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TEACHER GUIDE AND CURRICULUM HANDBOOK
CREATED BY: ISHA SANGHVI | ALICE MA | RYAN LEE
v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOKStemnova is a 501(c)(3) nonprofit founded in California with the mission to increase educational equity across the community. Our fundamental belief is that every child is deserving of a hands-on, experimental, enriching curriculum to help immerse them into the vast field of STEM. Stemnova has volunteered at local elementary schools and low-income housing centers, mentored middle school budding Science OlympiadTM teams, hosted science competitions drawing students from all across the state of California, and created an open-source curriculum to ensure our mission of educational equity will be achieved. With this curriculum, we hope teachers will be empowered with ample resources to inspire the next generation of scientists.
The teaching guide is filled with lesson transcripts that coincide with corresponding presentations for teachers to use with their students. The lesson transcript has been perfected after years of actual implementation in classrooms and schools. This handbook is also filled with activities, experiments, and worksheets to ensure that students are able to apply the knowledge learnt in lessons into actual real-world simulations.
We thank you for your vested interest in sparking a love for science in the next generation.
v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOKTABLE OF CONTENTSASTRONOMY
The Scale of Space 4
Our Solar System 10
Star Formation 18
Hertzsprung Russell Diagram 23
Life of a Star 31
Space Exploration 35
BIOLOGY
Macromolecules 46
Cells and Organization 57
Photosynthesis 67
Cellular Respiration 78
The Cell Cycle 84
Cancer and Biomarkers 90
Genetics 93
v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOKTABLE OF CONTENTSEPIDEMIOLOGY
Introduction to Epidemiology 101
Types of Epidemics 108
Spectrum of Disease 116
The Immune System 125
Immune System Disorder 131
Analyzing Case Studies 138
Conclusion to Epidemiology 148
GEOLOGY
Geology 156
Ocean Movements 166
Ocean Currents 171
Marine Life 175
Humans & the Ocean 180
v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOK
ASTRONOMYThe following curriculum section is for Astronomy. It introduces students to the workings of the outer world including stars, the solar system, and galaxies. Students also apply concepts of math and unit conversion into problem-solving. With lessons on understanding the relationship between luminosity and temperature and the different characteristics of plants, students will have a solid understanding of astronomy. They will be able to also apply this knowledge to understand and decode the biggest question of all: Are other planets hospitable to life?
Lesson 1 The Scale of Space
Summary
1. Subject(s): units, measuring space, unit conversions
2. Topic or Unit of Study: using units in science
3. Grade/Level: all grades
4. Objective: teach students how to understand the scale of space and unit relations
Key Skills: Students should be able to define what units are, visualize the size of
space, and convert measurements in one unit to another.
5. Time Allotment: Minimum 30 minutes.
Powerpoint
https://docs.google.com/presentation/d/1ek8c0x5GHSyoJibcBALbtRoJfsKIdY9n6Hw5UG0-B9U/e
dit?usp=sharing
Vocabulary and Important Concepts
Important Vocabulary
Unit: a quantity chosen as a standard in terms of which other quantities may be expressed
● an inch is a unit of length; seconds and hours are units of time; pounds is a unit of
weight
● ask students what other units they know to measure length, time, and temperature? -
sample answer: centimeters/yards/miles, days/weeks/years, Celsius/Fahrenheit
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Unit conversion: conversion process between different units to express the same measurement
● give students this example: there are 60 minutes in an hour; given this how many minutes
are in two hours? - answer: there are 120 minutes in 2 hours
● emphasize that 2 hours and 120 minutes are in different units but they are the same
quantity (equal to each other)
● example: there are 12 inches in a feet; given this, a tree that is 10 feet tall is how many
inches tall? - answer: inches0 2 201 × 1 = 1
● example: there are 2.54 centimeters in an inch; given this, how many centimeters long is a
3 inch pencil? - ○ answer: centimeters.54 .623 × 2 = 7
Important Concepts
Light is the fastest thing in the universe: Light is actually made of tiny particles that move so fast
we cannot see them. For example, when we turn on a light, the room lights up instantly - so fast
we can’t see the light particles spread out from the lamp.
● in 1 second, light travels 186,282 miles or 299,792 kilometers - that’s 7.5 times around the
Earth in one second
Space is measured with different units: Because space is so big, using miles or kilometers to
measure distances just isn’t reasonable. Can you imagine measuring the distance to Japan using
centimeters or inches? That’d take forever!
For distances to stars and galaxies, objects outside the solar system, we use light years. One light
year is about 6 trillion miles (9.5 trillion km), or 5,878,625,373,183.6 miles to be exact. Light years
are called light years because light travels about 6 trillion miles in one year.
For distances between planets and the Sun, or objects inside the solar system, we use
astronomical units (au). One astronomical unit is about 93 million miles, which is the distance
between the Earth and the Sun. It takes light only 8 minutes and 20 seconds to travel from the
Sun to Earth.
● Critical Thinking Question: What’s bigger - one light year or one astronomical unit? Why
might scientists not use astronomical units to measure distances between the Sun and
another star?
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○ Answer: Light years are greater than astronomical units. Scientists wouldn’t use
astronomical units to measure the distance between the Sun and another star
because that distance is too large to be reasonably measured with au. Simply put,
that distance in terms of astronomical units would be a huge number, maybe too
big to fit on the page!
● Critical Thinking Question: We know light travels one astronomical unit in 8 minutes and
20 seconds. it takes sunlight about 17 minutes to reach an asteroid in the solar system;
what’s the distance between the sun and the asteroid in au?
○ Answer: If we know light travels 1 au in 8 minutes and 20 seconds, then it will take
light 16 minutes and 40 seconds to travel 2 au. 16 minutes and 40 seconds is
about 17 minutes, so the distance between the sun and asteroid is about 2
astronomical units.
The same distance can be expressed with different units: There are many different units to
measure the same thing. We use miles, centimeters, inches, and feet to measure length. We use
minutes, seconds, days, and years to measure time. Different units can be used to refer to the
same length; for example a 1 inch long stick is also 2.54 cm long and 1/12 feet long.
Lecture Transcript Slide 1: Unit Conversions
● emphasize that the same amount can be defined with different units
○ for example, one week of time is equal to seven days of time; one foot of length is
equal to 12 inches of length or ⅓ a yard of length
○ a unit conversion is a mathematical process in which you change one form of
measurement to another
■ you are not changing the measurement, you are just changing the unit;
example: when I convert two feet to 24 inches, the two lengths are still the
same (24 inches is neither longer nor shorter than 2 feet)
Slide 2: Simple Conversions
● fractions have a numerator and denominator
● a number without a denominator is still a fraction: the denominator is 1 (4 = )14
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● when you multiply fractions, you:
○ multiply the numerator and numerator, and the new numerator is the product
○ multiply the denominator and denominator, and the new denominator is the
product
○ ex: ⅓ x ⅓ = 91
● when you multiply fractions, you can also cancel out the same numbers or units if they are
on the opposite sides of the fraction bar
○ ex: x = ; the 2 in the denominator of one-half and the 2 in the numerator of21
52
51
two-fifths cancel out to one, so the resulting fraction is one-fifth
Slide 3: Simple Conversions
● emphasize how the unit conversion must be put as a fraction
● the final unit you want to convert to should be the numerator; that way, the starting unit is
canceled out since it appears in the original measurement and the denominator
● How many centimeters are in 3 inches?
○ the unit conversion of centimeters to inches is put as a fraction ○ inches and inch cancel out since one is in the denominator and one is in the
numerator
○ ● How many inches are in 67.82 centimeters?
○ write the unit conversation of inches to centimeters as a fraction
■ make sure that the starting unit (centimeters) cancels out, so that the target
unit (inches) remains
○
Slide 4: Multi Step Conversions
● sometimes more than one fraction is needed
Slide 5: Converting Light Years to Astronomical Units
● in the conversion of light years to astronomical units, we run into a problem: there is no
direct unit conversion for light years to astronomical units
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○ for feet to inches, we know one foot equals 12 inches; for liters to quarts, we know
one liter is equal to 4 quarts: these are direct conversions since we can convert
from our starting unit to our end unit with one fraction
○ for light years to astronomical units, we aren’t given a direct conversion; however,
we know 1 au is 93 million miles and 1 light year is 5.9 trillion miles
■ with these two conversions, we can set up 2 fractions and1 light year5,900,000,000,000 miles
; when we multiply these two fractions together, the “miles”93,000,000 miles1 astronomical unit
unit cancels out since it can be found in the numerator of the first fraction
and denominator of the second fraction
● now, let’s look at the problem given on the slide
○ there are 2 equations to represent 2 ways to approach the problem
■ Approach 1 (faster): We can set up individual fraction bars and cancel out
units before multiplying everything together.
■ Approach 2 (easier): We multiply all the numerators and multiply all the
denominators to make one big fraction. Then we cancel out units that are
in both the numerator and denominator, and in the end, we are left with
only “astronomical units”
Slide 6: Converting Astronomical Units to Light Years
● the process is the same - we need multiple fractions, and we’ll be cancelling out units
● ask students to spot the difference in the overall equation
○ answer: the fractions converting light years to miles and converting au to miles are
flipped: light years is in the numerator, miles is in the denominator; au is in the
denominator and miles is in the numerator
○ explanation: in this problem, we want light years to be in our numerator because
it’s our final unit. we want au to be in our denominator because we want the au in
80,200 au and the au in the denominator to cancel out. miles still cancel out
because they are on opposite sides of the fraction bar.
Activity Slide 7: More Practice
● for the easier problems, ask students to practice doing the problem with fractions: ask
students to come up to the board/front of class to write the fractions
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● Answers
○ How many days are in 4 weeks?
■ 1 week = 7 days
● 4 weeks = 28 days× 7 days1 week
○ How many seconds are in half an hour?
■ 1 hour = 60 minutes, 1 minute = 60 seconds
● 0.5 hour = 180 seconds× 1 hour 60 minutes × 1 minute
60 seconds
○ How many inches are in 20 feet?
■ 1 foot = 12 inches
● 20 feet = 240 inches× 1 foot 12 inches
○ How many centimeters are in 20 feet?
■ 1 foot = 12 inches, 1 inch = 2.54 centimeters
● 20 feet = 609.6 centimeters× 1 foot 12 inches × 1 inch
2.54 centimeters
○ How many astronomical units are in 3 light years?
■ 1 astronomical units (au) = 93 million miles, 1 light year = 5.9 trillion miles
● 3 light years = 198,723 au× 1 light year 5.9 trillion miles × 1 au
93 million miles
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Lesson 2 Our Solar System
Summary
1. Subject(s): inner/terrestrial planets, outer/gas planets, the sun, moon, tides,
asteroids, meteors, and comets
2. Topic or Unit of Study: Astronomy
3. Grade/Level: 4-6
4. Objective: Students will learn to understand our solar system and the celestial
bodies it contains.
Key Skills: Students should be able to describe the different bodies in the solar
system.
5. Time Allotment: 2-4 hours
Powerpoint
https://docs.google.com/presentation/d/1eLoe4x6K3iZ21N0CDnHo26-9mvMumuQcC9hL6ym2rr
Q/edit?usp=sharing
Lecture Transcript
Our Solar System
Slide 2
The image on slide 2 is not to scale, but it shows the planets in order from how far each is from
the Sun. Our Solar System has 8 planets and several dwarf planets, with the most notable being
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Pluto. Pluto’s planetary status has been in discussion since its discovery, but as of currently, it is
classified as a dwarf planet.
Slide 3
What is a solar system?
A solar system consists of a sun and the celestial bodies that orbit it; either directly, such
as planets around the sun, or indirectly, such as moons that orbit around planets
There are many solar systems in the universe, not just the one that the Earth inhabits.
● Ask Students — Do you know where our Solar System is located?
○ Answer — our Solar System is in the Milky Way galaxy. Galaxies are a
group of stars, planets, and other stellar matter gravitationally bound
together. There are billions of galaxies in the universe, and scientists aren’t
even sure of exactly how many there are.
Slide 4
Our Solar System
Our solar system has a history of over 4.5 billion years and includes the Sun, 8 planets
and their moons, dwarf planets, asteroids, meteors, comets, and various other celestial
bodies.
For a long time, scientists only studied our solar system and didn’t even know that others
existed. But now, scientists know that there are many, many other solar systems out in the
universe. Each star could have a solar system and we just don’t know yet.
Slide 5 and 6
Inner Planets
The inner planets occupy the space from the Sun to about 700 million kilometers
outwards. The space that they occupy is actually very little compared to the rest of the
solar system, in fact the total distance from the sun to the last of the inner planets is less
than the distance between Jupiter and Saturn.
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The inner planets are also called the terrestrial planets because they are dense and rocky
in composition, also because they are Earth-like. They are composed mostly of minerals
with crusts, mantles, and cores. The inner planets are much smaller than the outer, with
Earth being the largest inner planet. They also have very few moons.
● Ask Students: Why do you think the inner planets don’t have many moons?
○ Answer - Inner planets are very small compared to the other planets in our
solar system. The smaller a planet, the weaker its gravitational pull is, so
because the inner planets are small and have weak pulls, they don’t have
many moons.
Slide 7
Mercury
Mercury is the planet that is closest to the Sun and the smallest planet in the solar system.
It has no moons or natural satellites.
Mercury doesn’t have any moons because it is too small and also because it is too close
to the Sun. If Mercury were to have a moon, its moon would most likely be pulled away
from it by the force of the Sun’s much more powerful gravitational pull.
Slide 8
Venus
Venus is the second planet from the Sun and the closest in size to the Earth (Venus to
Earth is about 0.85 to 1). It is the hottest planet in the Solar System. Venus’s surface has
reached temperatures of 400 degrees C. Venus also has no moons.
● Ask Students: If Mercury is closer to the Sun than Venus is, then how come Venus
is hotter than Mercury?
○ Answer — Venus’s atmosphere is much thicker than Mercury’s. Venus’s
atmosphere also has gases that are called greenhouse gases, like
methane. Greenhouse gases are very good at trapping heat in and
keeping it from escaping. So, any heat that reaches Venus is kept in by
those gases in the atmosphere, raising the temperature of the planet.
Slide 9
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Earth
Earth is the only planet with life that we know of. It also has an atmosphere made up of
nitrogen, oxygen, and other gases. It is also the only planet with plate tectonics. It has one
natural satellite, the Moon.
Slide 10
Mars
Mars, the fourth planet from the Sun, is known for its red color that comes from iron oxide,
rust, in its soil. Its atmosphere is mostly made of carbon dioxide and its surface has
volcanoes and valleys. Mars has two tiny natural satellites, or moons.
Mars’ two satellites are named Phobos and Deimos.
Mars has been the target of many space missions and continues to be a destination for
many missions to come.
Slide 11 and 12
Outer Planets
The outer planets, Jupiter, Saturn, Uranus, and Neptune, occupy the outer solar system.
They are also known as gas giants because they are all composed of gases like helium
and hydrogen. All of the outer planets have rings, however only Saturn’s are easily seen
from Earth.
The outer planets are very large, with Jupiter and Saturn combined being 400 times the
size of Earth. Uranus and Neptune are not as large, about 20 times the size of Earth.
Slide 13
Jupiter
The largest planet in the solar system is Jupiter, and it has 69 known natural satellites and
moons, the largest of which are named Ganymede, Callisto, Io, and Europa. Jupiter is
composed of mainly helium and hydrogen and has very strong thermal heat. It’s thermal
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heat is responsible for much of its weather patterns, causing storm bands and its iconic
Great Red Spot.
Nine spacecrafts have visited Jupiter. Although Jupiter itself is not able to support life as
we know it, some of its moons have been predicted to possibly support life.
Slide 14
Saturn
Saturn is unique because of its rings. Saturn is very similar to Jupiter although only about
60% of its volume. Saturn is the only planet that is less dense than water and its rings are
made up of ice and rock particles. It has 62 known moons.
Saturn is the farthest planet to be discovered with just the naked human eye, so its been
known to humans since ancient times of the Greeks.
Slide 15
Uranus
Uranus is the lightest of all the outer planets and it is unique because it orbits the Sun on
its side. Its sideways rotation causes the planet to experience strange seasons, with
nights lasting up to 21 years in the winter and days lasting up to 21 years in the summer. It
is much colder than the other planets and emits very little heat. It has 27 known satellites.
Uranus was the first planet to be discovered using a telescope. In April 2017, scientists
discovered that the clouds surrounding Uranus contain hydrogen sulfide, a smelly gas
that has the odor of rotten eggs.
Slide 16
Neptune
Neptune is the furthest planet from the Sun, it is the only planet that is not visible to the
naked eye. It has 14 known satellites and its largest is Triton. Triton is geologically active
and has geysers of liquid nitrogen.
Neptune is the Solar System’s windiest planet, with winds that can reach up to 2000
km/hr. In comparison, winds on Earth have only reached up to 400 km/hr. Neptune’s
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atmosphere has been confirmed to contain a dark vortex, high pressure systems that can
cause gases to freeze into ice crystals.
Slide 17
Pluto — The Dwarf Planet
Pluto has been infamous for its reclassification as a dwarf planet rather than the ninth
planet of our Solar System. It was discovered in 1930, and was first determined to be the
ninth planet. However, recent findings have declared it to be a dwarf planet.
Pluto is about 1400 miles wide, which is about half the distance from Los Angeles to New
York City. Pluto’s orbit around the Sun is elliptical, so it is not always the same distance
away from the Sun. At certain points of its orbit, it comes much closer to the Sun, causing
its atmosphere to thaw. When it moves away from the Sun, its atmosphere refreezes.
The International Astronomical Union has three criteria for planetary status: it must orbit
the sun, be spherical, and clear its own orbit. According to the International Astronomical
Union, a planet must be large enough to clear its own orbit, which Pluto cannot do.
Because Pluto cannot clear its own orbit, it was reclassified as a dwarf planet in 2006.
Slide 18
The Sun, Moon, and Tides
Slide 19
The Sun
The Sun is the largest component in the solar system. It is the solar system’s star and is
made up of mainly helium. The heat that is Sun provides is made from nuclear fusion of
hydrogen to helium. The Sun gravitational pull keeps the planets and other celestial
bodies orbiting around it.
Slide 20
The Earth’s Moon
The Moon is the only permanent natural satellite of the Earth. It is believed that the Moon
formed when the Earth and another body collided, the debris compressed into the Moon.
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It takes a month’s time for the Moon to orbit around the Earth and that orbit affects the
Earth’s ocean tides.
Slide 21 and 22
How Does the Moon Affect the Earth’s Ocean Tides?
The ocean’s tides are pulled and pushed by the Moon’s gravitational pull against the
Earth. The Moon’s gravitational pull is only strong enough to pull the water on Earth’s
surface, so it creates tides. Water on the side of the Earth that faces the moon is pulled
the most, and causes a bulge that is high tide.
Earth itself is pulled harder by moon’s gravity than is the ocean on the side of Earth
opposite the moon. As a result, there is a bulge of water on the opposite side of Earth
which creates another high tide. With water bulging on two sides of Earth, there is less
water in between. This creates low tides on the other two sides of the planet.
Slide 23
Asteroids, Meteors, and Comets
Slide 24 and 25
Asteroids and Meteors
Asteroids are classified as small solar system bodies and are composed of rocky and
metallic minerals and some ice. Most asteroids range from a few meters to hundreds of
kilometers in size. Asteroids that are smaller than one meter are typically classified as
meteoroids. When a meteoroid or asteroid enters the Earth’s atmosphere, it becomes a
meteor.
Many asteroids in the solar system are found in the asteroid belt that separates the inner
and outer planets.
Slide 26
Comets
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Comets are small solar system bodies and are typically a few kilometers in size. Comets
are made up of volatile ice and when they enter the Solar System, its icy surface
sublimizes and forms a tail, a coma, that is visible to the naked eye.
Most short-lived comets only live for about two hundred years, while long-lived comets
can survive for up to thousands of years. When comets lose their ice, they eventually
become asteroids.
Activity
Have students imagine that two new planets have been discovered — one that is an inner planet,
and one that is an outer planet. Let students partner up, and each pair will pick one of the two
planets. They will need to come up with a realistic name, similar to how the existing planets are
named after ancient gods of Roman mythology. They will be making a “profile” for their planet,
including the number moons, the planet’s characteristics, its atmosphere, and any other
information. Make sure the students are brainstorming ideas that are feasible, and they should be
able to defend their ideas with facts and information they know about the other planets.
For example, students should be able to explain that their inner planet has only 1 moon because
other inner planets have little to no moons as well.
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Lesson 3 Star Formation
Summary
1. Subject(s): The process of star formation, protostars, differences in the formations
of low mass and high mass stars
2. Topic or Unit of Study: Astronomy
3. Grade/Level: All grades levels, suggested for 4-6 grades
4. Objective: Teach students about star formation and the different variations of
formation
Key Skills: Students should be able to describe the process of star formation and
know the differences between low and high mass star formations
5. Time Allotment: 1-3 hours
Powerpoint
https://docs.google.com/presentation/d/1XCk5qP01RssAfHxc3JfdeEkdJWSORNWIMLRncqSco9k/
edit?usp=sharing
Lecture Transcript
Slide 2
Stars
A star is a large ball of gas held together by gravity, with the center being extremely hot. The
center of a star produces energy which is emitted as visible light, which is why we see stars as
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glowing at night. The sun is the star in our solar system — a sun is a star with planets orbiting
around it.
Teacher’s Note — Make sure students understand the difference between a star and a planet -
planets are smaller than stars and are too small to emit energy to produce visible light
Slide 3 and 4
Star Formation
From Space Dust into Stars
Imagine a huge collection of dust and particles floating in outer space. Gravity will attempt to pull
the pieces close to each other and eventually, enough gas and dust has collected in the center of
the cloud. That center is under a lot of pressure from the gravity and all the particles pressing
together; the temperature steadily increases and nuclear fusion begins, forming a new star.
This new star goes through a series of stages as it becomes a full-fledged star.
Slide 5
Cloud Collapse
Cloud collapse is the first step in forming a star. A large cloud of gas, dust, and particles will
experience gravitational collapse, where the cloud becomes too big and condenses into a giant
dense ball.
However, not all the dust and particles in the cloud will become part of the star. Some may form
planets or asteroids, or even remain as dust.
Also, cloud collapse does not always occur at a steady pace, sometimes the collapse will be
stronger or weaker, as seen in 2004, with the a nebula discovered in the constellation Orion. A
nebula is a collection of dust and particles. Scientists noticed that the brightness of the nebula
seemed to increase and decrease occasionally, leading them to believe that it was undergoing
cloud collapse in an erratic fashion.
Slide 6 and 7
Protostar
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As the temperature and the pressure of the cloud becomes too great, the cloud will eventually
become a protostar. A protostar is the intermediate step before the star becomes a
main-sequence star. Main-sequence stars are the stars that are stable and what we see at night. As the temperature and pressure further increases, the core of the protostar begins to
experience hydrogen turning into helium in a process called nuclear fusion. This is when the
protostar becomes a main-sequence star.
Slide 8
Low Mass and High Mass Stars
Low mass stars are smaller than high mass stars. Because these stars have different sizes,
scientists believe that they are formed differently.
Slide 9
Low Mass Stars
Low mass stars are smaller and may be formed via cloud collapse, just like was what mentioned
above.
Slide 10
High Mass Stars
High mass stars, because they are much larger, are thought to be made from several low
mass stars collapsing at the same time. However, because it is difficult to observe such a
formation, many scientists are unable to do more research regarding the formation of
these stars. In fact, much of what is known today about star formation is speculation and
hard to predict.
Article
The following article is about a recent observation made by scientists that may point to
how high-mass stars are formed. The article was originally published by The Independent
on April 30, 2018, written by Andrew Griffin about a study published in Nature Astronomy.
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Stars aren’t formed in the way we thought, scientists reveal
Huge stars are forming in completely unexpected ways in our own galaxy and beyond, new
research suggests.
Scientists have long expected that larger stars form in much the same way as smaller ones. But a
new study suggests that something unexplained is happening to those high-mass stars, and they
are forming in a way that is vastly different to how we expected.
In lower-mass stars – which make up most of those we can see in detail – there seems to be a
simple relationship between the mass of the star-forming clouds of dust and gas, and the mass of
the star itself once it is born.
But the new study suggests that high-mass stars do not behave in that way. The findings add an
extra layer of mystery to the conundrum of what it is that makes stars grow to a certain mass.
The new findings will force researchers to rethink their understanding of how high-mass stars are
formed in the universe.
All across the known universe, huge molecular clouds made of dust and gas collapse and then
stick together in dense blobs. Those cores then collapse and heat up at temperatures so high
that they form into stars.
In our own galaxy, the mass of those cores seems to decide the mass of the stars that come out
of them. There seems to be a common pattern that can be seen in all such regions.
But scientists have now looked into a different region of clusters elsewhere in the universe, in an
attempt to find whether that relationship works in other places too.
They found that the simple relationship they had presumed would hold throughout the universe
appears to be wrong, and that the cores are behaving differently elsewhere.
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Using extremely sensitive telescopes, they gained an unprecedented insight into a distant
star-forming region named W43-MM1, that lies 18,000 light years away.
The team was able to observe star-forming cores with an extraordinary range, from those similar
to the mass of the Sun to ones 100 times more massive.
To their surprise, the distribution of star-forming cores was completely different to what had
previously been observed in nearby regions of the Milky Way.
In particular, they observed an abundance of extremely big stars with huge masses, but fewer
smaller stars that are more common within our galaxy.
Co-author of the study Dr Kenneth Marsh, from Cardiff University, said: "These findings were a
complete surprise and call into question the intricate relationship between the masses of
star-forming cores and the masses of the stars themselves, which has long been assumed.
"As a consequence, the community may need to revisit its calculations regarding the complex
processes that dictate how stars are born.
"The evolution of a core into a star involves many different physical interactions, and the results
of studies such as this should help us better understand how it all happens."
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Lesson 4 Hertzsprung Russell Diagram
Summary
1. Subject(s): Hertzsprung Russell diagram and luminosity
2. Topic or Unit of Study: Astronomy
3. Grade/Level: 5th-6th grades
4. Objective: Understand the mechanism behind the Hertzsprung Russell diagram,
luminosity, and know how to read a Hertzsprung Russell Diagram
Key Skills: Students should be able to explain the reasoning behind the HR
diagram and be able to understand luminosity and read an HR diagram.
5. Time Allotment: 1 hour
Powerpoint
https://docs.google.com/presentation/d/1cI-Fk4cJj1ZAqDmf1XmTAKYgnRmmROlH5RgD845tzRA/
edit?usp=sharing
Vocabulary and Previous Concepts
Learning Context
Students should have a general idea of how to plot points on a graph of standard
Cartesian plane. Make sure students understand how to scale the axis of a plane and
understand how to graph and read a graph.
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Students should have a general idea of what a scatter plot is. A scatter plot is a graph
that shows the relationship between two different variables. The graph has points that
are not connected with others, such as line graphs.
Lecture Transcript
Slide 3
Luminosity
In astronomy, luminosity is the total amount of energy emitted by a star or other
astronomical object per unit of time. It is related to the brightness, which is the luminosity
of an object in a given region.
Hertzsprung Russell Diagram
Slide 5
What is a Hertzsprung Russell Diagram?
A Hertzsprung Russell Diagram, also called an H-R diagram or HRD, is a scatter plot that
shows the relationship between a star’s luminosity and its temperature.
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Teacher’s Note — Have students think of the H-R diagram as similar to the Periodic Table
to Elements. The Periodic Table shows all the known elements, organized in a way that is
easy for scientists to read and use. An H-R diagram is the same thing, just for stars instead
of elements.
An H-R diagram shows the luminosity of the stars on the vertical axis and the temperature
of the stars is on the horizontal axis.
Stars in the same general region of each other share similar characteristics. An H-R
diagram typically has four regions of stars — main sequence stars, white dwarfs, giants,
and supergiants. However, stars move from region to region as they change over time, so
an H-R diagram is not fixed, it’s more like a graph that shows the evolution of different
stars.
If scientists know the location of a star on the H-R diagram, they would be able to know
the type, color, mass, temperature, luminosity, chemical composition, age, and evolution
history of the star.
Slide 6
Main Sequence Stars
About 90 percent of all stars found in the universe are currently main sequence stars.
Main sequence stars are found in the center of the HRD, in a relatively linear formation.
These stars fuse hydrogen at their core and have a balance of outward pressure and
gravity pushing inwards. Our Sun is a main sequence star.
The amount of time a star spends in its main sequence phase depends on how big the
star is. The larger the star, the faster it burns out and becomes less stable. Smaller stars
can stay stable for much longer. Main sequence stars also vary in size, with larger nebulae
forming larger stars.
Slide 7
White Dwarfs
A white dwarf is what stars like our sun will eventually become. White dwarfs are
extremely dense, they can have half the mass of the sun, but only be as large as the
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Earth. The atmosphere of a white dwarf is thought to be strange because its surface
gravity can be up to 100,000 times that of Earth’s.
Slide 8
Giants
Giant stars are stars that are much brighter and larger than main sequence or dwarf stars,
however, they are about the same surface temperature. Most stars that are in the giant
star phase are nearing the end of their stellar existence.
Slide 9
Supergiants
Supergiants are a subcategory of giant stars, and they are larger and brighter, but still
have lower surface temperatures. On an H-R diagram, they are found in the upper central
region, being the brightest, but not the hottest.
Activity
Students will construct their own H-R diagrams with the information they learned in the
lesson. Students can work alone or in pairs. Their diagrams should have labels for where
the main sequence, white dwarf, giant, and supergiant stars are found. Also, have
students label the areas of the diagram with the following temperature and brightness
combinations — hot/bright, hot/dim, cool/bright. cool/dim, average temperature/average
brightness. Students should also be able to relate the types of stars to the types of
temperature/brightness combinations.
Article
The following article is about how scientists can determine the age of the universe using
technology like the Hertzsprung Russell Diagram. The article was originally published on
Scientific American, citing interviews from two distinguished scientists.
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How do scientists determine the ages of stars? Is the technique really accurate enough to use it
to verify the age of the universe?
Stephen A. Naftilan, professor of physics in the Joint Science Department of the Claremont
Colleges, responds:
"Astronomers usually cannot tell the age of an individual star. There are certain stars that we
know are very young, and others that are very old, but for most stars we cannot tell. When we
have a large group of stars, however, we can tell its age. This is possible because all of the stars
in a cluster are presumed to have begun their life at approximately the same time. After a
relatively brief time (in 'star time,' that is--we are talking thousands to millions of years here) stars
reach the adult phase of their life, which we call the main sequence phase. The length of time a
star spends in the main sequence phase depends on its mass.
"Constructing a plot, called the HR diagram, of the stars in the cluster, scientists can determine
the mass of the stars that are just ending this phase and moving on to the next phase of their life,
the red giant phase. Computer models allow us to predict how old a star of that mass must be to
be at that juncture of its life, and hence to estimate the age of the cluster. Recently, this
procedure has come under close scrutiny because that age it gives for the oldest star clusters in
our Milky Way seems to be older than the age of the universe derived from the most recent
Hubble Space Telescope data."
Peter B. Stetson, senior research officer at the Dominion Astrophysical Observatory in
Victoria, British Columbia, provides a more detailed reply:
"It is impossible to determine the age of a single star all by itself. The only real means we have to
determine stellar ages is through the study of star clusters. In our galaxy, the Milky Way, there are
two basic types of star cluster. Clusters of the first type are called 'globular clusters' because they
appear as huge, round globs containing anywhere from a few thousand to a few million stars.
Globular clusters are very old, and they are scattered around (not just within) the Milky Way;
these clusters seem to have originated near the time our galaxy started to form, when the
universe was quite young. Clusters of the second type used to be called 'galactic clusters'
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because we see them inside the body of our galaxy, but now it is more common to refer to them
as 'open clusters' because they are much looser and their stars more spread out on the sky than
are those in globular clusters. Open clusters can contain anywhere from a few dozen to a few
thousand stars, and they come in a wide range of ages. Apparently our galaxy started making
open clusters soon after it settled down to its present size and continues making them even
today.
"The stars in either type of star cluster were all formed at the same time and out of the same
material. The essential feature of a star cluster that lets us estimate its age is that each cluster
contains stars with a range of masses. When a cluster is born, it will contain many stars of about
the same size and mass as our sun, but there will also be numerous stars more massive than our
sun and many other stars less massive than our sun. For about 90 percent of its lifetime, a star
shines because nuclear reactions are converting hydrogen to helium in the star's center,
releasing vast amounts of energy. This energy works its way from the center of the star to the
surface and escapes the star in the form of light. The more massive a star is, the bigger the
furnace in the center, and the brighter and the hotter the star is in this stable stage of its life. The
most massive stars are very bright and blue-hot; a less massive star is somewhat fainter and
white-hot; a star like our sun is a bit fainter still and is yellow-hot; and the least massive stars are
very faint and merely red-hot. During this period of its life, a star hardly changes either in
brightness or in temperature.
"The duration of the stable, or 'main sequence,' phase depends on a star's mass. A star 10 times
as massive as the sun contains, clearly, 10 times as much fuel. It consumes that fuel roughly
10,000 times faster than the sun, however. As a result, it has a total lifetime 1,000 times shorter
than that of our sun. When the hydrogen fuel in the center of a massive star is exhausted--'the
center' representing about 10 percent of the star's total mass--it becomes increasingly unstable.
The star remains bright, but it quickly switches from being comparatively small and hot to being
huge and red for a while, then it briefly becomes smaller and bluer, then even larger and even
redder, and finally explodes as a supernova, spewing its nuclear ashes as well as its unburned
fuel back into space. Similarly, a star five times more massive than the sun has a lifetime roughly
100 times shorter than the sun before it becomes unstable and ends its active life. A star like our
sun is calculated to have a total stable life-span of around 10 billion years; the sun is now a bit
less than half that age (this age is very accurately determined from radioactive elements in
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meteorites), so we have another five billion years or so before we have to start looking for a new
home.
"In the case of a single star, its brightness and temperature don't tell us much. Because these
properties stay fairly constant for 90 percent of its lifetime, the star could be fairly young or fairly
old, and we wouldn't be able to tell the difference. In a star cluster, we have the advantage that
stars of all masses formed at about the same time. So all we have to do is look at the cluster and
determine how hot and how massive is the hottest, bluest, most massive star that has not yet
entered the late, unstable period of its life. The star's mass tells us how much fuel the star had
when it was born, and the star's brightness tells us how fast it is burning that fuel. We know that
the star is just about to start becoming unstable--after all, the stars that are more massive have
already started to become unstable. We also know that its fuel is just about exhausted. The ratio
of how much fuel the star had in the beginning to how fast it has been burning that fuel tells us
how long the star has been alive. (By analogy, if we know how much kerosene our hurricane
lamp contained when we lit it and how fast it consumes the kerosene, and if the lamp is just now
starting to go out, then we can deduce how long it has been lit.) Because all the stars in the
cluster are the same age, the age of that one star tells us the age of the entire cluster.
"The basic physics of how hydrogen is converted to helium in the centers of stars and the amount
of energy generated by this process is comparatively simple and well understood. For much of
the 20th century, the main limitation to our knowledge of stellar ages has been due to the
difficulty of measuring the distances to the clusters--especially the distances to the oldest
clusters, the globulars, which are comparatively far away. (We know how bright a star looks, but
to know how bright it really is, you have to know how far away it is: is it like a headlight a mile
away or an airport beacon 10 miles away? In the dark of the nighttime sky with no reference
points, it's pretty hard to tell.) Technical advances, such as the introduction of charge-coupled
devices to replace photographic plates for the measuring of stellar distances and brightnesses,
are making our observations more secure.
"Distance measurements have improved to the point at which other details needed to determine
the ages of star clusters--such as the fine details of how a star converts nuclear energy to visible
light--can no longer be ignored. How exactly does the energy get from the center of the star,
where it is generated, to the surface, where it becomes the light that we see? How important is
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convection as a means of transporting energy, and how efficient is the convection? The answer
to these questions has some effect on the inferred relationship between mass and surface
temperature. Just how much oxygen is in the stars, along with the hydrogen and helium? The
relative amount of oxygen present has a modest effect on the efficiency of the central furnace,
affecting the relation between mass and brightness and, hence, age.
"Taken together, the uncertainty in the observations and the uncertainty in the relevant
theoretical physics probably lead to an uncertainty of 10 percent to 20 percent in our estimate of
the absolute ages of the globular clusters. According to our best available estimates, stars having
about 90 percent of the sun's mass are just now starting to die in the globulars. These stars are
most probably around 15 billion years old, but they could conceivably be as young as 12 billion
years or as old as 18 billion years. It is very unlikely that most of them could be either younger or
older than this range. This estimate is already accurate enough to place some very interesting
limits on the age and life history of the universe."
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Lesson 5 Life of a Star
Summary
1. Subject(s): life of a star
2. Topic or Unit of Study: Astronomy
3. Grade/Level: 3-6 grades
4. Objective: Students will learn about the lifespan of a star and how they change.
Key Skills: Students should to able to describe what a black hole is and how they
are formed.
5. Time Allotment: 2 hours
Powerpoint
https://docs.google.com/presentation/d/1_VtfoIH5ysG-fIVB9otN36eSU1eL20XaZ7PPXIS1IzE/edit?
usp=sharing
Lecture Transcript
Slide 3
Main Sequence to White Dwarfs
Average stars become white dwarfs over time. Our sun will eventually become a white dwarf.
White dwarfs are about the size of Earth but can contain the mass of half the Sun. Gradually,
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some will cool down and fade away, however for white dwarfs that are extremely large, they may
become supernovas.
Slide 5
What is a Supernova?
A supernova is the explosion of a star. It is the largest explosion that takes place in space.
Slide 6
Where Do Supernovas Take Place?
Supernovas are often seen in other galaxies. But supernovas are difficult to see in our own Milky
Way galaxy because dust blocks our view. In 1604, Johannes Kepler discovered the last
observed supernova in the Milky Way. NASA’s Chandra telescope discovered the remains of a
more recent supernova. It exploded in the Milky Way more than a hundred years ago.
Slide 7 and 8
What Causes a Supernova?
A supernova happens where there is a change in the core, or center, of a star. A change can
occur in two different ways, with both resulting in a supernova.
The first type of supernova happens in binary star systems. Binary stars are two stars that orbit
the same point. One of the stars, a carbon-oxygen white dwarf, steals matter from its companion
star. Eventually, the white dwarf accumulates too much matter. Having too much matter causes
the star to explode, resulting in a supernova.
The second type of supernova occurs at the end of a single star’s lifetime, after it becomes a
white dwarf. As the star runs out of nuclear fuel, some of its mass flows into its core. Eventually,
the core is so heavy that it cannot withstand its own gravitational force. The core collapses, which
results in the giant explosion of a supernova. The sun is a single star, but it does not have enough
mass to become a supernova.
Slide 10
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Neutron Stars
If the supernova is extremely large, it may become a neutron star. A neutron star is extremely
dense because it has so much volume packed into such a small space. It also has magnetic fields
that can accelerate the particles near it to become rays of radiation.
Slide 11
The largest supernovas will eventually become black holes.
Slide 12
Black Holes
A black hole is a place in space where gravity pulls so much that even light can not get out. The
gravity is so strong because matter has been squeezed into a tiny space. This can happen when
a star is dying.
Because no light can get out, people can't see black holes. They are invisible. Space telescopes
with special tools can help find black holes. The special tools can see how stars that are very
close to black holes act differently than other stars.
Slide 13
How Big Are Black Holes?
Black holes can be big or small. Scientists think the smallest black holes are as small as just one
atom. These black holes are very tiny but have the mass of a large mountain.
The largest black holes are called "supermassive." These black holes have masses that are more
than 1 million suns together. Scientists have found proof that every large galaxy contains a
supermassive black hole at its center. The supermassive black hole at the center of the Milky
Way galaxy is called Sagittarius A. It has a mass equal to about 4 million suns and would fit inside
a very large ball that could hold a few million Earths.
Slide 14
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How Do Black Holes Form?
Scientists think the smallest black holes formed when the universe began. Some black holes may
have formed when stars collapsed and died. Some think supermassive black holes were made at
the same time as the galaxy they are in.
Slide 15
If Black Holes Are "Black," How Do Scientists Know They Are There?
A black hole can not be seen because strong gravity pulls all of the light into the middle of the
black hole. But scientists can see how the strong gravity affects the stars and gas around the
black hole. Scientists can study stars to find out if they are flying around, or orbiting, a black hole.
When a black hole and a star are close together, high-energy light is made. This kind of light can
not be seen with human eyes. Scientists use satellites and telescopes in space to see the
high-energy light.
Activity
Have students pair up or form groups of three. Give each group/pair a scenario of a star and have
them map out the remaining steps of the star’s life.
For example, if a pair was given the scenario of a medium sized main sequence star, they would
map out the star’s life as going from main sequence to white dwarf to eventually fading away. If
the scenario were an extremely large main sequence star, students could respond by saying that
the star will become a large white dwarf, which could become a supernova, that would become
either a neutron star or black hole.
Make sure students can support their decisions with information learned from the lesson about
the life of stars.
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Lesson 7 Space Exploration
Summary
1. Subject(s): History of space exploration
2. Topic or Unit of Study: Astronomy
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the history of space exploration.
Key Skills: Students should be able to briefly explain the history of space
exploration and research.
5. Time Allotment: 1-2 hours
Powerpoint
https://docs.google.com/presentation/d/1mLlJVFfXj517fNAiK7kb_z8UqJl24hwVshE56GzByz4/edit
?usp=sharing
Lecture Transcript
History of Space Exploration
Space exploration began in the 20th century, with scientists from the United States, Russia, and
Germany seeking to advance science and competing with each other to be the first ones in
space.
During World War II, countries began to entertain ideas of using long-range rockets to attack
belligerent countries and Nazi Germany was one of the first to attempt making such rockets.
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However, after the Nazi defeat in WWII, Germany fell out of the race to space, leaving only the
United States and Russia.
After World War II, both the United States and the Soviet Union created their own missile
programs. In the midst of the Cold War between the US and USSR, both countries sought to be
the first to accomplish space exploration for reasons of military advancement and national pride.
On October 4, 1957, the Soviets launched the first artificial satellite, Sputnik 1, into space. The first
U.S. satellite, Explorer 1, went into orbit on January 30, 1958. On April 12, 1969, Russian astronaut
Yuri Gagarin became the first human to orbit the Earth.
On July 20, 1969, American astronaut Neil Armstrong stepped onto the moon on the mission
Apollo 11. Following that success, six more Apollo missions were made to explore the moon.
In the 1960s, unmanned spacecrafts photographed and probed the moon before astronauts like
Armstrong ever set foot on the moon. By the early 1970s, orbiting communications and navigation
satellites were in use and NASA’s Mariner spacecraft was orbiting and examining Mars’ surface.
By the end of the decade, the Voyager spacecraft sent back detailed images of Jupiter and
Saturn.
Skylab, America’s first space station, was a human-spaceflight highlight of the 1970s. The Apollo
Soyuz Test Project became the world’s first internally crewed space mission with American and
Russian scientists.
Space systems will continue to become more and more integral to homeland defense, weather
surveillance, communication, navigation, imaging, and remote sensing for chemicals, fires, and
other disasters.
The International Space Station is a research laboratory in low Earth orbit. With many different
partners contributing to its design and construction, this laboratory has become a symbol of
cooperation in space exploration, with former competitors now working together.
Articles
The following article is part of the NASA Knows! Series about the Apollo space program.
What Was the Apollo Program?
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Apollo was the NASA program that resulted in American astronauts' making a total of 11
spaceflights and walking on the moon.
The first four flights tested the equipment used in the Apollo Program. Six of the other seven flights
landed on the moon. The first Apollo flight happened in 1968. The first moon landing took place in
1969. The last moon landing was in 1972.
A total of 12 astronauts walked on the moon. The astronauts conducted scientific research there.
They studied the lunar surface. They collected moon rocks to bring back to Earth.
What Spacecraft Were Used for the Apollo Program?
NASA designed the Apollo Command Module for this program. It was a capsule with room for three
astronauts. The astronauts rode in the Command Module on the way to the moon and back. It was
larger than the spacecraft used in the Mercury and Gemini programs. The astronauts had room to
move around inside the spacecraft. The crew area had about as much room as a car.
Another spacecraft, the Lunar Module, was used for landing on the moon. This spacecraft carried
astronauts from orbit around the moon to the moon's surface, then back into orbit. It could carry
two astronauts.
Two types of rockets were used for the Apollo program. The first flights used the smaller Saturn I (1)
B rocket. It was about as tall as a 22-story building. This rocket had two stages. That means it was
made of two parts. When the first part ran out of fuel, it dropped away from the other and burned
up in Earth's atmosphere. The second part continued flying. The Saturn IB rocket was used to test
the new Apollo capsule in Earth orbit.
The other flights used the more powerful Saturn V (5) rocket. This three-stage rocket sent the Apollo
spacecraft to the moon. It was about as tall as a 36-story building.
When Did Humans First Visit the Moon?
The first manned mission to the moon was Apollo 8. It circled around the moon on Christmas Eve in
1968. However, Apollo 8 did not land on the moon. It orbited the moon, then came back to Earth.
The crew was Frank Borman, Bill Anders and Jim Lovell.
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The first moon landing occurred on July 20, 1969, on the Apollo 11 mission. The crew of Apollo 11
was Neil Armstrong, Michael Collins and Buzz Aldrin. Armstrong and Aldrin walked on the lunar
surface while Collins remained in orbit around the moon. When Neil Armstrong became the first
person to walk on the moon, he said, "That's one small step for (a) man; one giant leap for
mankind."
The following missions flew humans during Apollo:
Apollo Flight 7
Date: Oct. 11-22, 1968
Mission: Tested the Command Module
Crew: Schirra, Eisele, Cunningham
Apollo Flight 8
Date: Dec. 21-27, 1968
Mission: First to orbit the moon
Crew: Borman, Lovell, Anders
Apollo Flight 9
Date: March 3-13, 1969
Mission: Tested the Lunar Module
Crew: McDivitt, Scott, Schweickart
Apollo Flight 10
Date: May 18-26, 1969
Mission: Tested the Lunar Module around the moon
Crew: Cernan, Young, Stafford
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Apollo Flight 11
Date: July 16-24, 1969
Mission: First to land on the moon
Crew: Armstrong, Aldrin, Collins
Apollo Flight 12
Date: Nov. 14-24, 1969
Mission: Landed on the moon
Crew: Conrad, Bean, Gordon
Apollo Flight 13
Date: April 11-17, 1970
Mission: Was supposed to land on the moon but had a malfunction
Crew: Lovell, Swigert, Haise
Apollo Flight 14
Date: Jan. 31-Feb. 9, 1971
Mission: Landed on the moon
Crew: Shepard, Mitchell, Roosa
Apollo Flight 15
Date: July 26-Aug. 7, 1971
Mission: Landed on the moon
Crew: Scott, Irwin, Worden
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Apollo Flight 16
Date: April 16-27, 1972
Mission: Landed on the moon
Crew: Young, Duke, Mattingly
Apollo Flight 17
Date: Dec. 7-19, 1972
Mission: Landed on the moon
Crew: Cernan, Schmitt, Evans
Apollo 13 is one of the more famous lunar missions. A movie was made about this flight. Apollo 13
was supposed to land on the moon. On the way there, the spacecraft had a problem. NASA had to
figure out how to bring the astronauts home safely. Apollo 13 flew all the way around the moon
before returning home. Despite the problem, they were able to land safely on Earth.
How Did Astronauts Land on the Moon?
The Apollo spacecraft were launched on top of the Saturn V rocket. The Saturn V was made of
three stages. The first two stages used up their fuel reaching orbit. The third stage was used to
push the Apollo Command Module and Lunar Module to the moon. Once the spacecraft reached
the moon, the two modules separated from each other. Two astronauts in the Lunar Module landed
on the lunar surface. The third astronaut stayed in the Command Module in orbit around the moon.
On the last three missions, astronauts drove on the moon with the lunar rover. Astronauts drove the
lunar rover to explore more of the moon's surface. The lunar rovers were made so they could be
folded to fit in a storage area on the Lunar Module. The lunar rovers were left on the moon.
When the two astronauts were finished working on the surface, they got back in the Lunar Module
and launched. It went back into orbit around the moon and connected with the Command Module.
The two astronauts got back into the Command Module. They left the Lunar Module behind and
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flew back to Earth. The Lunar Module crashed into the moon. The Command Module landed in the
ocean, and a ship picked up the astronauts.
Why Was the Apollo Program Important?
In 1961, President John F. Kennedy challenged the nation to land astronauts on the moon by the
end of the decade. NASA met that challenge with the Apollo program. It was the first time human
beings left Earth orbit and visited another world. These missions made it possible to explore more
distant worlds further in the future.
__
This following article is from the NASA Knows! series about the Hubble Space Telescope.
What Is the Hubble Space Telescope?
The Hubble Space Telescope is a large telescope in space. It was launched into orbit by space
shuttle Discovery on April 24, 1990. Hubble orbits about 547 kilometers (340 miles) above Earth. It
is the length of a large school bus and weighs as much as two adult elephants. Hubble travels
about 5 miles per second: That is like traveling from the eastern coast of the United States to the
western coast in 10 minutes. Hubble is solar-powered.
Hubble takes sharp pictures of objects in the sky such as planets, stars and galaxies. Hubble has
made more than one million observations. These include detailed pictures of the birth and death of
stars, galaxies billions of light years away, and comet pieces crashing into Jupiter's atmosphere.
Scientists have learned a lot about the universe from these pictures. Many of them are beautiful to
look at.
What Makes Hubble Different From Telescopes on Earth?
Earth’s atmosphere alters and blocks the light that comes from space. Hubble orbits above Earth’s
atmosphere, which gives it a better view of the universe than telescopes have at ground level.
Where Did the Name Hubble Come From?
Hubble is named after an American astronomer, Edwin P. Hubble. He made important discoveries
in the early 1900s. He showed that the galaxy containing the solar system -- the Milky Way -- was
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only one of many galaxies. His work helped show that the universe is expanding. This led to the
big-bang theory, which says that the universe began with an intense burst of energy and has been
expanding ever since.
What Instruments Are on Hubble?
As Hubble orbits Earth, the Fine Guidance Sensors lock onto stars. The Fine Guidance Sensors are
part of the Pointing Control System and aim Hubble in the right direction. The telescope can lock
onto a target that is one mile away without moving more than the width of a human hair.
Once the target is acquired, Hubble's primary mirror collects light. The mirror can collect about
40,000 times more light than the human eye. The light bounces off the primary mirror to the
secondary mirror. The secondary mirror focuses the light back through a hole in the primary mirror.
From there, the light shines to Hubble's scientific instruments. Each instrument has a different way
of interpreting the light.
Hubble has five scientific instruments which include cameras and spectrographs. A spectrograph is
an instrument that splits light into its individual wavelengths .
The Wide Field Camera 3 is Hubble’s main camera. It studies everything from the formation of
distant galaxies to the planets in the solar system. The camera can see three different kinds of light:
near-ultraviolet, visible and near-infrared. But Hubble can only see each kind of light one at a time.
Human eyes can see visible light. Near-ultraviolet and near-infrared are just beyond what our eyes
can see.
The Advanced Camera for Surveys captures images of large areas of space. These images have
helped scientists study some of the earliest activity in the universe.
The Cosmic Origins Spectrograph reads ultraviolet light. This spectrograph studies how galaxies,
stars and planets formed and changed.
The Space Telescope Imaging Spectrograph helps scientists determine the temperature, chemical
composition, density and motion of objects in space. It also has been used to detect black holes.
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The Near Infrared Camera and Multi-Object Spectrometer, or NICMOS, sees objects in deep space
by sensing the heat they emit. It captures images and it is also a spectrograph. NICMOS helps
scientists study how stars, galaxies and planetary systems form.
What Are Hubble's Most Important Discoveries?
Images taken by Hubble have helped scientists estimate the age and size of the universe. Scientists
believe the universe is almost 14 billion years old. Hubble has helped scientists understand how
planets and galaxies form. An image called "Hubble Ultra Deep Field" shows the farthest galaxies
ever seen.
Hubble has detected black holes, which suck in everything around them, including light. The
telescope has played a key role in the discovery of dark energy, a mysterious force that causes the
universe to expand faster and faster as time goes on. And it has revealed details of gamma-ray
bursts -- powerful explosions of energy that occur when massive stars collapse.
Hubble has also studied the atmospheres of planets revolving around stars similar to Earth’s sun.
Where Do the Colors in Hubble's Images Come From?
Hubble transmits about 140 gigabytes of science data every week back to Earth. That's equal to
about 45 two-hour, HD-quality movies or about 30,000 mp3 songs. The digital signals are relayed
to satellites, then to a ground station, then to NASA's Goddard Space Flight Center, and finally to
the Space Telescope Science Institute. The STScI translates the data into images and information
we can understand.
Hubble pictures start out as shades of black and white. The Space Telescope Science Institute
adds colors to the pictures for different reasons. Sometimes colors are chosen to show how an
object might look to the human eye. Other times colors are used to highlight an important detail. Or
they can be used to show details that would otherwise be invisible to the human eye.
What Is the Future of Hubble?
Hubble is more than 25 years old! Engineers designed Hubble so that it could be repaired and
upgraded as needed. Since the telescope's launch, five space shuttle missions have carried
astronauts to Hubble to repair and upgrade it. The last mission was in 2009. Hubble was upgraded
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so that it is better than ever. The telescope will not be repaired or upgraded again. But it is
expected to continue to work until 2020 and beyond.
Meanwhile, NASA and its international partners are preparing the James Webb Space Telescope to
launch in early 2021. The Webb is an infrared telescope that will be larger than Hubble and will be
able to see through clouds and dust in space. Instead of orbiting Earth, this telescope will orbit the
Sun from a point beyond the Moon. Webb will send back amazing images like Hubble does, and it
will help astronomers unlock more of the biggest mysteries of the universe.
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v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOK
BIOLOGYThe following curriculum section is for Biology. It introduces students to the small cellular mechanisms working on our bodies everyday. In addition to understanding metabolic processes and organelles, students are able to learn about some of the most researched diseases, such as cancer. The curriculum guide includes activities which allow students to research different cancer therapies. Through this event, students will be able to apply their knowledge of the cell to understand how this knowledge can be used to create future treatments.
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Lesson 1 Macromolecules
Summary
1. Subject(s): Polymers, monomers, four main macromolecules - carbohydrates, lipids,
proteins, nucleic acids
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: teach students about the four main groups of organic macromolecules
Key Skills: Students should be able to explain what makes up a macromolecule and be
able to describe the function and structure of carbohydrates, lipids, proteins, and nucleic
acids. Students should also be to classify macromolecules into their correct categories.
5. Time Allotment: 1-2 hours
Powerpoint
https://drive.google.com/open?id=1nwuya2Vl_pCFxfaJi80rZiXKhG2oNaqmptjCOGefZsc
Lecture Transcript
Macromolecules
Slide 2 — What Are Macromolecules?
Macromolecules are very large molecules that are made up of numerous smaller units. The word
“macromolecule” hints at its definition, as “macro” means large in Greek. Macromolecules can
also be called polymers, and the smaller units that make them up are called monomers.
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Teacher’s Note: To explain to students what a molecule is or what a macromolecule is, draw the
following conceptual diagram on the board:
Each individual bead/circle is a monomer meaning one molecule. The polymer is a string of all of
the monomers connected to make one HUGE chain or a polymer.
In this lesson, we will be looking at the four main groups of macromolecules, carbohydrates,
lipids, proteins, and nucleic acids. However, of the four, lipids are not considered to be true
polymers because it is not made up of the same small unit combined into one larger molecule.
Ask Students — why might lipids be classified into the same category as the others if they are
not the same. The answer is that lipids, like the other three macromolecules, are essential to all
life and scientists classify them together to make for simplicity.
These four macromolecules are organic and are absolutely essential for all living things to have.
Without them, living things could not survive.
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Slide 4
Slide 3 shows examples of the four types of molecules.
Teacher’s Note: Draw the above diagram on the board (preferably the carbohydrate and lipid
diagrams to show the difference between polymers and non-polymers. Circle the individual
monomers to show how the different subunits contribute to the larger chain: polymer. Together,
the individual circles add up to be one big polymer. But for the lipids, there’s only one circle
because it is not made up of individual subunits.
Slides 5-11: Carbohydrates
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Carbohydrates are biological molecules that are made up of carbon, hydrogen, and oxygen
atoms joined together. They are a main source of energy and are also known as saccharides,
which means “sugars.” Some examples of carbohydrates include: grains, pasta, bread, rice etc.
Ask Students — What are some examples of carbohydrates you ate today?
Slide 6
The main function of carbohydrates is to provide energy. They are the main source of fuel,
necessary for physical functions, brain operations, and organ function. All cells in the body
require carbohydrates.
Slide 7-8
Carbohydrates are polymers that are made up of monomers of sugar. There are three main
categories of carbohydrates — monosaccharides, disaccharides, and polysaccharides.
Slides 9-11
Monosaccharides only contain one unit of sugar. Common monosaccharides include glucose,
fructose, and galactose. Glucose is an extremely important monosaccharide and carbohydrate
because it is the main carbohydrate that the human body processes. It is also the sugar that is
referred to when you hear “blood sugar”
Disaccharides are made up of two monosaccharides linked together. Di, the prefix, often means
two. Common disaccharides include maltose (made up of two glucose molecules), sucrose (made
up of glucose and fructose), and lactose (made up of galactose and glucose).
Polysaccharides are made up of more than two monosaccharides of glucose. Most
polysaccharides contain hundreds or thousands of glucose units.
Slides 12-13
Lipids
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Lipids are the only molecule of the four we will talk about that is not considered to be a true
macromolecule or polymer. The reason that lipids are not true macromolecules or polymers is
because it is not made up of several smaller identical units. Carbohydrates are made up of units
of sugars that are identical, making them polymers. However lipids are not.
Ask Students — What are some examples of lipids you ate today?
Slide 14
Lipids are made up of carbon, hydrogen, oxygen, and nitrogen atoms. Common lipids include
fats, waxes, and sterols. Lipids are unique in their inability to dissolve in water. If you put a lipid
into water and stir, no matter what happens, it will not dissolve. For example, if you mix oil, a lipid,
and water, the two will eventually separate into two individual layers.
Teacher’s Note: In order to cement the idea that lipids are unable to dissolve in water, show them
a demonstration of mixing oil in water or play this video:
https://www.youtube.com/watch?v=neS6Tm_HXKE
The basic composition of a lipid consists of a glycerol molecule with fatty acid tails. A lipid
molecule with three fatty acid tails is called a triglyceride.
Teacher’s Note: The picture on slide 12 is an example of a triglyceride. Point out that the three
tails are not the same, which is part of the reason why lipids are not macromolecules. The only
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way lipids can be macromolecules is if the tails are always identical, but that’s not the case.
Slide 15
The main function of lipids is to store energy, act as signals between cells, and make up cellular
membranes. Lipids store energy that is unneeded so that the body can use this stored energy
when it needs to. Lipids are also messengers that move between cells and locations throughout
the body to act as signals. Lipids are also the main component of cell membranes. Cell
membrane lipids will be touched upon in future lessons.
Slides 16-17
Proteins
Proteins are polymers that are made up of monomers of amino acids. Proteins perform a huge
array of different function within the body, including those of catalyzing metabolic reactions,
transporting molecules, replicating DNA, and responding to stimuli.
Proteins differ from each other in their basic amino acid sequence. There are 20 amino acids in
total, and the combinations that they come together forms different proteins with different
functions. Proteins have varying lifespans, some ranging from a few minutes to several years.
Ask Students — what analogy can they think of for proteins and amino acids. Examples could
include letters that make up words. With only 26 letters, the way that we arrange them and how
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many we use allows us to make an infinite number of words, just like how amino acids arrange to
form different proteins.
Proteins, like all other macromolecules, are essential for the survival of cells. They participate in
almost all cellular activities and help to regulate bodily functions.
Slide 18
Protein structure is split into four distinct categories — primary, secondary, tertiary, and
quaternary structure. The primary structure of a protein is the line of the amino acids.
Primary protein structure is essentially a string of amino acids. Secondary structure contains
alpha-helix and beta-sheets and they are the regularly repeating local structures. Secondary
structures can be thought of as how the individual primary strands are connected. Tertiary
structure is the overall structure of the entire protein. Quaternary structure is a structure that is
made up of several proteins, unusually forming a single protein complex.
Teacher’s Note: Remind students that the amino acids are like letters from the the alphabet.
When we put the different letters together, they form millions of different words. In the same way,
when the line the different amino acids together, they form words. The primary structure is a
word made up letters. The secondary structure involves the chain of amino acids put together.
This is similar to putting together the words to make a phrase. The tertiary structure is when the
structure of the amino acid chains twist and fold together to make a protein, similar to phrases
coming together to make a sentence. The quaternary structure is when all of the different
proteins come together to make a protein complex. Think of a sentence as a protein and a
paragraph as a protein complex.
Draw the following diagram on the board to help the students relate this important concept:
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Slide 19
Diagrams of the four different protein structures.
Teacher’s Note: Ask students to identify which step is which.
Slide 20
The most common protein function is enzymes. Enzymes help to speed up chemical reactions.
For example, a chemical reaction may take days to take place without an enzyme, but with, the
reaction may only take a few hours. Enzymes are extremely specific, with each enzyme only
matching with one specific reaction. The enzyme is similar to a lock and key. You can only open a
door if you have the exact key for the door. In the same way, the reaction can only be sped up if
you have the exact enzyme for it. For that reason, the human body can make numerous different
enzymes to cater to each and every reaction that needs an enzyme.
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Teacher’s Note: Give this analogy to students. Imagine you need to run a mile/kilometer. It will
usually take you fifteen minutes to run the mile. But, if you are given a special set of sneakers,
you can run the mile in ten minutes. Ask students, what is sneaker represent in the analogy? It represents the enzyme because it speeds up reactions.
Slide 21-22
Nucleic Acids
Nucleic acids are composed of monomers called nucleotides. Nucleic acids have the function of
having to create, encode, and store the information that is found in the nuclei of all cells in every
organism.
The encoded information is made using different sequences of nucleotides. There are five
distinct nucleotides — adenine, thymine, guanine, cytosine, and uracil.
Teacher’s Note: In the same way monomer amino acids can string together to create very unique
proteins, different sequences of the nucleotides can come together to create very different DNA
strands. The DNA codes for traits like your hair color, your skin color, your earlobes, etc. Draw
this diagram on the board for them to understand the structure of DNA.
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BioNinja
Ask students to identify a pattern. Which bases pair with one another? Adenine (A) bonds with
Thymine (T) and Guanine (G) pairs with Cytosine (C). These are the rules of DNA in a way. A
bonds with T and C bonds with G.
Slide 23
There are two types of nucleic acids, DNA and RNA.
Slide 24
DNA has two strands and has a double helix structure. It is made up of four nucleotides, adenine,
thymine, cytosine, and guanine. DNA’s main purpose is to house specific coded information of
genes.
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Slide 25
RNA has only one strand and is made up of four nucleotides, with uracil taking the place of
thymine. The other three nucleotides are the same as DNA. RNA contains encoded information
for protein synthesis.
Emphasize to students: the central dogma of Biology or the basic theory of biology is that DNA is
turned into RNA. RNA is then turned into proteins through protein synthesis. The proteins help
determine what characteristics a person has. While DNA has the code for your traits, only the
protein can actually show your traits (hair color, skin color etc).
Activity
For an activity to best cement the idea of DNA base pairs, have the children play DNA basketball! Set up
four different baskets, each labeled A, C, T, or G. Each student has a letter tag on them as an identifier.
They can either be Adenine (A), Cytosine (C), Guanine (G), or Thymine (T).
All of the adenine and thymine children are on the same team, while all of the cytosine and guanine
children are on the same team. Each person has the objective of scoring a basket in the base pair that
matches theirs. For example, a student with a C tag should score in the G basket.
Every correct match earns 2 points to the respective team. Every incorrect match (for example a student
with a C tag shoots in the A basket) results in the loss of 4 points.
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Lesson 2 Cells and Organization
Summary
1. Subject(s): cells, tissues, organs, organ systems; animal and plant cells; cell organelles;
unique cell organelles to plant and animal cells
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6
4. Objective: Teach students about the organizational system of cells, animal and plant cells,
and cell organelles
Key Skills: Explain the purpose and way of organization of cells; explain the differences in
plant and animal cells; identify and name the functions of basic organelles
5. Time Allotment: 2-4 hours
Vocabulary and Previous Concepts
Learning Context
Teacher’s Note: Remind students about the basic concept of macromolecules. In the same way
monomers build together to make polymers, often known as macromolecules (with the exception
of lipids), these macromolecules can also build upon one another to make bigger objects. One of
these examples are cells: macromolecules such as lipids, DNA, and protein combine to make
cells.
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Powerpoint
https://docs.google.com/presentation/d/1vuXoCfmkUWvomKr_RdKTRrTrg8Nekj-G89GIuaKnfxc/edit?usp=
sharing
Lecture Transcript
Cellular Organization
What Are Cells?
Cells are the basic units of life. The cell theory explains that cells are the basic building blocks of
life. Cell theory states three points:
1. All living organisms are composed of one or more cells. All of us, you and me, are made
of millions and billions of cells.
2. The cell is the basic unit of structure and organization in organisms. In the same way the
amino acid is the monomer of proteins, the cell is like a monomer of the body. It is the
small unit in which we study the body.
3. Cells come from already existing cells. Cells do not come from thin air. Instead, cells make
other cells through a process called cellular division.
How Are Tiny Cells Organized Into a Whole Organism?
Teacher’s Note: To give students a perspective for how small the cells are, show students this
online module which compares the cell to other commonly known items:
http://learn.genetics.utah.edu/content/cells/scale/
Cells are organized into organisms through a precise process. A group of similar cells with
common purposes form a tissue. For example, muscle tissue is formed by muscle cells. A group
of tissues then form a complete organ, like your heart. And finally, a several organs can come
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together to form an organ system. For example, your stomach, intestines and other organs for
your digestive system. These systems can then form an entire organism.
Teacher’s Note: Have students simulate the process of organization in the body. Have each
student represent a tiny cell. Ask students to form tissues where students must link arms to make
a tissue. Three students represent one tissue because the cells have joined together. Then, ask
the students to form an organ. This involves 2 tissues coming together. The two groups of three
students come together and huddle to form an organ. To form an organ system all of the different
organs in the classroom (groups of six) must come together to arrange in a line with one another.
Eukaryotes and Prokaryotes
There are two types of cells — eukaryotes and prokaryotes. In the same way each of you
students is representing a cell, each cell is unique and has different characteristics. For example,
we can split all of the students into 2 groups: boy/girl, shorts/full-length pants etc. The two groups
represent prokaryotic versus eukaryotic cells. While all of you are cells, some of you have more
similarities with one another.
Prokaryotes
Prokaryotes are considered to be the more basic form of cells when compared to eukaryotes.
Prokaryotes are different from eukaryotes in the fact that they do not contain a nucleus or any
membrane-bound organelles. Prokaryotes are extremely simple and most often are found in
single celled organisms such as bacteria.
Teacher’s Note: A nucleus is the “brain” of the cell. It contains all of the DNA and genetic material
in the cell. Because the prokaryote does not carry a nucleus, it instead has the DNA floating
around inside the cell.
Eukaryotes
Eukaryotes have nuclei and contain membrane-bound organelles. They are much more
complicated and compartmentalized, which allows for each cell to have multiple activities going
on at once.
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Plant and Animal Cells
There are two types of eukaryotic cells that we will talk about in this lesson, plant and animal
cells. The two types of cells have some different organelles and different functions.
Teacher’s Note: An organelle is like a mini-organ for a cell. In the same way your body needs to
carry out certain processes using your organs like the heart or lungs, your cell also has
organelles that help the cell carry out certain processes.
Plant Cells
Plant cells are found in plants and are filled with the necessary means to perform photosynthesis,
which is the way that plants make food.
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Tell students - Remember, while you can go to the store or a restaurant to eat food, plants
cannot buy food. Instead, they have to make food themselves. And not like cook food, but
actually make all of the ingredients. The way the plant makes food is through photosynthesis.
Using sunlight, water and carbon dioxide, the plant makes a carbohydrate called glucose. Using
this glucose, the plant grows taller.
Animal Cells
Animal cells, found in animals, do not have the ability to photosynthesize; however, they do have
unique properties that are not found in plant cells. The animal does not make their own food.
Instead animals like lions catch food and then break it down. They do not need to use
photosynthesis to make food.
Organelles
What Are Organelles?
An organelle is a cellular structure, similar to an organ. It has a specific job and purpose and each
is differentiated to be able to perform its function. Organelles are found embedded in a cell’s
cytoplasm.
Organelles Found in All Eukaryotic Cells
Cytoplasm
The cytoplasm is not actually considered to be an organelle. It is a jelly-like substance that fills a
cell. The cytoplasm is found in all cells and it keeps each organelle in place and is also the place
for many cellular chemical reactions.
Nucleus
A cell’s nucleus contains the cell’s genetic information, in the form of DNA. The nucleus is
surrounded by the nuclear envelope, which contains small pores to allow materials to go in and
out of the nucleus. Every eukaryotic cell contains and nucleus and is essential for cells to
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function. In prokaryotic cells, the genetic material is found in the center of the cell and gathered
in a group, not a specific organelle.
Cell Membrane
The cell membrane is found in all cells as well. It surrounds the cell and is made up of lipids. The
cell membrane is considered to be selectively permeable, meaning that is only allows certain
materials in and out of the cell.
The cell membrane is made up of phospholipids. The phospholipids are composed in a way that
makes the portion of the membrane touching the outside and the inside of the cell to be
hydrophilic, meaning that it dissolves in water. The area of the cell membrane that is sandwiched
between the hydrophilic part is hydrophobic.
Cell Wall
The cell wall is something that is only found in plant cells. It is responsible for making the plant
cell seem rigid. The cell wall is found outside of the cell membrane and serves to keep plants
upright. The strength of tree trunks is because of numerous cell walls forming together to make
the tree so strong.
Ribosomes
Ribosomes are the site of protein synthesis and they are also found in both eukaryotes and
prokaryotes. Ribosomes use RNA to put together proteins for the cell to use or to transport to
other locations. Structurally, ribosomes are made up of several subunits that are put together to
form the entire organelle.
There are two types of ribosomes — free-floating ribosomes and attached ribosomes. Free
floating ribosomes typically make proteins that will remain within the cell, for the cell to use while
attached ribosomes typically make proteins that will be sent outside to cell to other parts of the
organism.
Vacuoles
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Vacuoles are found only in eukaryotes and are in both plant and animal cells. The main purpose
of vacuoles is to store water, food, waste, or any other materials. In plant cells, there is only one,
large, central vacuole; typically found in the center of the cell. In animal cells, there are several
smaller vacuoles found scattered throughout the cytoplasm.
Mitochondria
The mitochondria is found in both plant and animal cells, but not in prokaryotes because it
contains a membrane. The mitochondria is known to be the powerhouse of the cell. It is
responsible for the process of cellular respiration that breaks down glucose into energy for the
cell and the body. Mitochondria contain a double membrane that allows for cellular respiration to
occur within the organelle. Cellular respiration and more about the structure of the mitochondria
will be discussed in later lessons.
Chloroplast
The chloroplast is found only in plant cells, and it is the organelle that is responsible for a plant’s
ability to produce its own food using sunlight. The chloroplast is the location of photosynthesis
and is essential to a plant cell’s survival. Chloroplasts also contain chlorophyll, which is a green
pigment that allows the organelle to absorb sunlight for the chloroplast to use. More about the
chloroplast and photosynthesis in later lessons.
Endoplasmic Reticulum
The endoplasmic reticulum, ER, is split into two types — smooth ER and rough ER. The rough ER
is known as rough because it has ribosomes connected to it. The purpose of the rough ER si for
protein synthesis, which is also the reason why it has so many ribosomes connected to it.
However, unlike free floating ribosomes, the protein that is created on the rough ER is packaged
and sent to outside of the cell usually to another location in the body.
The smooth ER’s function is to detoxify and to regulate the production of lipids and hormones. It
also helps to transport materials in and out of the cell.
Golgi Apparatus
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The Golgi apparatus, sometimes called the Golgi body, is a collection of membranes that has the
purpose of taking the proteins created by the rough ER, modifying and packaging them for
transport outside of the cell.
Lysosomes
Lysosomes are found in all eukaryotic cells and they are the waste disposal centers of cells.
Lysosomes are small sacs that are capable of breaking down waste.
Centrioles
Centrioles are typically only found in animal cells, but can sometimes be in plant cells. The main
purpose of centrioles is for cell division. They assist in dividing the cell when it is time for it to
reproduce. More about centrioles and their function when talking about cell division.
Teacher’s Note: Because this lesson has so much information about the different types of
organelles and the cell itself, have students do the worksheet as a refresher for the next class or
as a reviewer for the end of the class. The best method is to have students watch a recap video
of all of the organelles and take notes on the organizational sheet to help students best
conceptualize the actual categorization of the organelles. Then, have students do the
project/activity to best cement their understanding. They should use the organizational sheet to
help guide them while doing the activity.
Show this video for a better understanding of all of the cell organelles:
https://www.youtube.com/watch?v=URUJD5NEXC8 Have students fill out the organizational
sheet while watching the video/afterwards.
For a review and a more interactive way of looking at the construction of a cell, students can also
use this online simulator: http://sepuplhs.org/high/sgi/teachers/cell_sim.html.
Activity
For this activity, have students make an art project/analogy to the cell. Using poster paper, they can
make an analogy of the different organelles.
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For example, a student can compare the cell to a city, where the local government is the nucleus
because they direct all of the orders and is the brain of the cell. The mitochondria can be the energy
plant or coal plant which burns coal to create energy (even though that is not a sustainable energy
source and is bad for the environment). The lysosomes can be the disposal facility or the garbage trucks
and so on.
The students should have a written or verbal explanation of why each specific organelle is chosen to be
a specific object in the comparison. Have them present to the class so students better make connections
and are able to remember the role of each of the organelles.
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Lesson 3 Photosynthesis
Summary
1. Subject(s): Structure and function of parts of the chloroplast; light dependent and
independent reactions; photosynthesis adaptations
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the specific processes of photosynthesis and
the structure of the chloroplast. Students will also be able to distinguish between
different adaptations of plants regarding photosynthesizing.
Key Skills: Students should be able to explain the processes of photosynthesis
and their relationships to the chloroplast. Students will also be able to explain
reasons and functions of different adaptations of photosynthesis.
5. Time Allotment: 2-3 hours
Vocabulary and Previous Concepts
Learning Context
Teacher’s Note: This lesson focuses mainly on a specific organelle introduced in the
previous lecture: the chloroplast. Before you go very in depth regarding the process of
photosynthesis, remind students about the chloroplast and its structure to better immerse
the students into it.
To go over the structure (which is not a focus of the previous lesson on organelle), draw
this image on the board:
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This is a diagram of a chloroplast which like we know about most eukaryotic organelles, is
double-membraned. It has an outer and inner membrane, with the intermembrane space
being between the two membranes. Inside the chloroplast is jelly-like liquid (similar to the
cytoplasm), except is called the stroma. Inside the stroma are stacks of little disks known
as thylakoids.
Ask students to draw a chloroplast of their own in their notebooks/papers so they
understand the structure.
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Powerpoint
https://docs.google.com/presentation/d/1LcRPqKsWL2YhiTQc9UqGSk0JfeZrUJumvQ4_0tMTGKY
/edit?usp=sharing
Lecture Transcript
Chloroplasts
Where Does Photosynthesis Take Place?
The process of photosynthesis takes place within the chloroplast. The chloroplast is an organelle
that is only found in plant cells. It has a double membrane that surrounds the interior of the
chloroplast. Inside, the chloroplast contains small, round, flat circles called thylakoids. Thylakoids
are stacked into groups called granums. The entire chloroplast contains an aqueous solution,
comparable to the cytoplasm in cells, called stroma.
Photosynthetic Pigments
In order for photosynthesis to occur, the chloroplast needs to have specific pigments that will
allow light to be absorbed.
A pigment is a color. Take for example, your clothes have certain pigments. If I’m wearing a red
shirt, my shirt has pigments that reflect the color red. The pigment absorbs visible light as well as
reflects visible light. The light that is not absorbed is reflected onto the viewer.
Teacher’s Note: To connect this concept of light and pigments to the students (this is a
fundamental concept of the entire process of photosynthesis), draw this diagram on the
board. The sun gives off white light (which is a combination of all of the light colors). The
light is full of different wavelengths. Each wavelength of light corresponds to a different
color. So, for example, we see the leaf as green because it reflects only green light and
absorbs all the other wavelengths of light.
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Ask students, what wavelength of light (color) is absorbed/reflected off of a red bug.
Fun Science
Have a group of three students stand up. Ask one to wave their hands in small waves,
medium waves, and large waves. Based on the visible light spectrum below, ask
students to determine which student would be which color. (The small waves would
represent the purple, medium waves would represent the green, and the large waves
would represent the red).
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ORCA Grow Film
The most common pigment in the chloroplast is chlorophyll, which reflects green. Chlorophyll is
the reason for why plant leaves are typically green.
Photosynthesis
Photosynthesis is the process in which plants make their own food. Imagine a plant catching after
an insect for food! It is impossible (unless of course you have a Venus Flytrap) so instead plants
make their own food inside of themselves using certain ingredients. The ingredients are: sunlight,
carbon dioxide, and water to make sugar. The plant takes in water through the roots and carbon
dioxide through the stomata (little holes at the bottom of the leaves). A byproduct of this
production of food, in the form of sugar, is oxygen.
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Plant Stomata Encyclopedia
Teacher’s Note: For the students who are familiar with chemistry and understand
molecular formulas, you can show them this chemical formula for the reaction of
photosynthesis. But, if students have not learnt chemistry yet, we recommend not
showing them this formula as it might intimidate them.
ight 6CO 6H O H O Ol + 2 + 2 → C6 12 6 + 6 2
Photosynthesis can be split into two parts, light dependent reactions and light independent
reactions. As you can imagine, the light dependent reactions depend on light, while the light
independent reactions do not need light and instead can operate in the dark and light.
Light Dependent Reactions
Light dependent reactions are a part of photosynthesis that requires sunlight to occur. The
reaction requires sunlight and water to produce its products. It takes place in the thylakoid
membrane or the outside coverage of the thylakoid. When sunlight hits the chlorophyll in the
thylakoid, a chain reaction is triggered as electrons are passed from one molecule to another.
Think of it is a domino effect. Once the first molecule of chlorophyll is struck by sunlight,
water is split to create electrons are sent from one molecule to another. The light dependent
reactions result in the formation of ATP, a molecule called NADPH, and oxygen. ATP is an
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important molecule because it able to store energy. NADPH is also able to store energy but not
as much as ATP. The oxygen is released into the environment as a byproduct.
In simple terms, during the light dependent reaction, the light is used to split up up water. In
splitting up water, two energy forms are created which are later used to make sugar. When water
is split up, oxygen is released.
Light Independent Reaction - Calvin Cycle
The light independent reaction is also known as the Calvin cycle and it does not need sunlight to
be available to occur. The Calvin cycle takes place in the stroma of the chloroplast. The Calvin
cycle requires the products of the light dependent reaction (ATP and NADPH) and carbon
dioxide. The cycle results in the production of a sugar molecule, glucose, which is considered to
be the plant’s food.
Teacher’s note: For a more visual description of the Calvin cycle, show your students this video:
https://www.youtube.com/watch?v=0UzMaoaXKaM&vl=en. The actual names of enzymes and
proteins are not important, but it helps to connect the dots between ATP/NADPH and sugar!
Plant Adaptations of Photosynthesis
Certain plants the live in different environments have their own ways to optimize their production
of food. For example, some plants live in dry, hot environments with little rain such as deserts.
Other plants live in environments with too much rain. As a result, each plant species has different
adaptations.
Teacher’s note: Ask the class to brainstorm other adaptations for other animals to help them
connect the dots between evolution and adaptation of organisms. For example, giraffes have
evolved into having long necks to eat leaves at the top of trees no other animal can reach. Or,
think of chameleons which have developed chamoflague to avoid being eaten by predators.
C4 plants and CAM plants are two different adapted plants that have made changes to the typical
process of photosynthesis. C3 plants are plants that that are normal/regular plants.
C4 Plants
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C4 plants have their Calvin cycle in a different part of the leaf compared to typical plants.
Sometimes there is a shortage of carbon dioxide in the environment, so the adapted plant must
find a way to “stick” to the carbon dioxide. In regular plants, the Calvin Cycle happens in a certain
cell called the mesophyll cell. For the C4 plant, a carbon intermediate is made in the mesophyll
cell and then shipped to the bundle sheath cell where the Calvin Cycle happens. The reason why
the Calvin Cycle happens in the bundle sheath cell is because it is easier to stick to the carbon
dioxide.
CAM Plants
CAM plants are typically found in deserts and they have the special adaptation of keeping carbon
dioxide in a different form during the day. They do not want to lose too much water in the
daytime. The plants wait until night time to turn the carbon dioxide into sugars, thus conserving
their water during the heat of the day.
Teacher’s note: Remind students that the process of photosynthesis requires water as a reactant
or an ingredient to make a sugar. But, when there is a lot less water in the environment, often
times the plant loses water to the environment when trying to take water in.
Article Teacher’s note: Highlighted information/sentences should be emphasized to students
while reading it as a class or asking students to read independently. Stemnova’s
comments are written in red and are not to be confused with the statement of Hannah
Devlin or The Guardian. This article has effectively shown the bridge between genetics
and photosynthesis.
Plants Modified to Boost Photosynthesis Produce Greater Yields, Study
Shows By Hannah Devlin
Genetically modified (GM) plants (Every organism has genetic material inside of them. Remember, in the earlier lesson, we explained that in eukaryotic cells, the genetic information or DNA is found in the nucleus. In a prokaryotic cell, the DNA is found floating in the cytoplasm. A
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genetically modified organism has its DNA modified to make the organism stronger or more adapted to the environment) designed to use light more efficiently produced a 20% greater yield in a study that could have significant implications for global food supplies.
The field trial, which used tobacco plants, is the first to show that GMtechniques can be used to boost the basic efficiency of photosynthesis, potentially offering substantial gains across almost all food crops in the future. Until now many scientists had doubted this would be possible.
The scientists believe the finding could help meet the global demand for food, which is projected by the UN to rise by 70% by 2050 (this statistic indicates that there is a need for more production of food/plants for the world).
Professor Stephen Long, who led the work at the University of Illinois, said: “We don’t know for certain this approach will work in other crops, but because we’re targeting a universal process that is the same in all crops, we’re pretty sure it will.” (Other genetically engineering tactics target unique characteristics in each organism such as the way they attract bees for pollination or absorb water through the roots. After all, there are different ways to execute such tasks. For example, if I ask two student to complete a project, they would both do it in drastically different ways. So, the genetic engineering targets a process EACH plant does.)
Previously, GM (genetic modified) techniques have been used to produce crops that are pest-resistant, disease-resistant or less sensitive to herbicides, but this is one of the first demonstrations of a crop’s basic efficiency being improved.
Professor Jonathan Jones, who works on GM crops at the Sainsbury Laboratory in Norwich and was not involved in the latest study, said the size of the gains reported were impressive. “That’s not the kind of thing you normally see,” he said.
Long’s team started out by simulating the entire process of photosynthesis, the process that converts sunlight into chemical energy, to identify where potential gains could be made. They decided to target a process that plants use to shield themselves from bright sunlight.
“Crop leaves exposed to full sunlight absorb more light than they can use,” Long said. “If they can’t get rid of this extra energy, it will actually bleach the leaf.”
Chemical changes within the leaf allow the excess energy to be dissipated as heat, in a process called nonphotochemical quenching (NPQ). (Explain to students that NPQ is a process by which plants turn the excess light into heat so that bleaching does not occur). While plants switch on the quenching mechanism almost instantaneously – similar to the way in which the pupil in the human eye contracts in bright light – it takes much longer for it to switch off again.
“When a cloud crosses the sun, or a leaf goes into the shade of another, it can take up to half an hour for that NPQ process to relax,” Long said. “In the shade, the lack of light limits
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photosynthesis, and NPQ is also wasting light as heat.” (This is the specific problem. The “half an hour” in which we are losing light as heat).
Computer simulations suggested that the energy wasted after quenching reduces overall crop productivity drastically, by 7.5 to 30%, depending on the plant type and sunlight conditions. The scientists modified three genes with the aim of increasing the levels of three proteins that could help ramp up the efficiency of photosynthesis more quickly after exposure to bright sunlight.
They grew seedlings from multiple experiments and selected the three best strains, based on how they responded to changes in light conditions. These were then grown in several field plots alongside standard tobacco plants.
Two of the GM strains consistently showed 20% higher yields and the third was 14% higher, in terms of the weight of dry leaves harvested. The plants also had bigger leaves, were taller and had heavier roots. (Ask students why they think bigger leaves and heavier roots would increase the amount of sugar/growth for plants.)
The team have now been funded by the Gates Foundation to introduce similar modifications in major food crops, starting with rice, soya bean and cassava.
If a relatively simple gene modification can improve the efficiency of photosynthesis, it might appear surprising that plants have not just evolved this genetic trait by themselves. However, outside agricultural settings, photosynthesis is not the factor that limits plants growth, according to Jones. “Most plants grew in an environment where the limiting factor was nitrogen available, not photosynthesis,” he said.
Questions
1. What is the specific problem scientists are targeting in the plant through genetic
engineering?
The specific problem is that there is a process in the plant which turns excess light into heat to
prevent bleaching. And while it is quick to turn on, it is hard to turn off. Which means during the
time it takes for the process to turn off, there is wasted sunlight that the plant could have used to
perform photosynthesis.
2. Have the experiments of genetic engineering shown signs of success in the plants?
Here are specific statistics/quotes stated by the article:
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● Computer simulations suggested that the energy wasted after quenching reduces overall
crop productivity drastically, by 7.5 to 30%
● Two of the GM strains consistently showed 20% higher yields and the third was 14%
higher, in terms of the weight of dry leaves harvested.
● The plants also had bigger leaves, were taller and had heavier roots.
3. Why is it important that the scientists try to create bigger leaves and heavier roots (as
mentioned by the article)?
Bigger leaves mean more surface area to take in carbon dioxide through. With more carbon
dioxide, there is more of a raw ingredient to make sugar and have plants that grow stronger.
Strong and heavier roots mean roots that are more capable of taking in and absorbing water,
another raw ingredient for a strong plant.
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Lesson 4 Cellular Respiration
Summary
1. Subject(s): Structure and function of the mitochondria; aerobic respiration —
glycolysis, Krebs cycle, electron transport chain; anaerobic respiration — lactic
acid and alcoholic fermentation
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about cellular respiration and the organelle in which
it takes place
Key Skills: Students should be able to describe a mitochondrion and its structure
and function. Students should also be able to distinguish between aerobic and
anaerobic respiration and the factors associated with both.
5. Time Allotment: 1-3 hours
Vocabulary and Previous Concepts
Learning Context
Teacher’s Note: It’s important to remind students that while only plants carry out
photosynthesis (because they are producers of food), every organism carries out
respiration in order to break down the food they have already ingested or eaten. Plants,
humans, lions, and bugs all carry out cellular respiration. While plants carry out cellular
respiration to break down the sugar they themselves made, animals carry out cellular
respiration to break down food they caught or bought (in the case of humans).
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Additionally, it is important to remind students that there is a difference between the term
“respiration” and “cellular respiration.” Respiration refers to the bodily process by which
humans and animals take in oxygen and release carbon dioxide through breathing.
Cellular respiration, instead, involves breaking down sugars. It does however require
oxygen so in a sense respiration gets the oxygen needed to start cellular respiration.
Powerpoint
https://docs.google.com/presentation/d/1zMmYyFzeM4zGznIgeZ1ol1dPMVeebItUFmQHQnh9PAM
/edit?usp=sharing
Lecture Transcript
Cellular Respiration Overview
Cellular respiration is the process of taking food in the form of sugar, glucose, and turning it into
energy, in the form of ATP. The process also uses water and oxygen and produces carbon
dioxide as a byproduct.
Teacher’s Note: Ask students, how is cellular respiration similar to the process of
photosynthesis? Cellular respiration is the opposite of photosynthesis in the sense that
the products of photosynthesis (oxygen and sugar) are the reactants or ingredients
needed to start cellular respiration. In the same way, the reactants of photosynthesis
(energy in the form of light, carbon dioxide, and water) are the products of cellular
respiration (except the energy is not in the form of light but instead allows you to carry out
bodily processes).
Mitochondria
Where Does Cellular Respiration Take Place?
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Teacher’s Note: Before going into the specifics of what the actual process of cellular
respiration is, you should introduce to students the structure of the mitochondria, the
cellular organelle involved in producing energy. Draw the following structure on the board
to help students to get familiarized with the structure.
Cellular respiration takes place in the mitochondria and cytoplasm of the cell. The mitochondria is
an organelle with two membranes. The inner membrane contains folds called cristae. These folds
increase the amount of surface area of the mitochondria and allow for multiple different
processes to take place at once. The space enclosed by the inner membrane is called the matrix.
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Aerobic Respiration
What is Aerobic Respiration?
Aerobic respiration is the form of cellular respiration that requires oxygen to be present. It uses
oxygen to turn glucose into energy and carbon dioxide. Aerobic indicates that there is a need for
oxygen because in latin, aero- means air (often associated with oxygen). We as humans, along
with other organisms, mainly carry out aerobic respiration. There are other organisms who carry
out anaerobic respiration and we will talk about them later (they are the exception).
1. Glycolysis
Glycolysis is the first step of cellular respiration. It takes place in the cytoplasm of the cell. It
involves breaking down the sugar (mainly glucose) into smaller parts and molecules which can
then later on be broken down to release energy in the form of ATP. Glycolysis actually does not
need oxygen to occur, however, in the presence of oxygen, it will produce two pyruvate
(3-carbon molecules) and four molecules of ATP. These products will be moved into the
mitochondria, to the next step of aerobic respiration.
2. Krebs Cycle
The Krebs cycle takes place in the matrix of the mitochondria or the
space inside the inner membrane. The Krebs cycle, also called the
citric acid cycle, takes the pyruvate and ATP from glycolysis and uses it
to make NADH and FADH2. Remember from the photosynthesis
lesson, NADH is a type of energy intermediate. FADH2 is similar in this
sense in that it is an energy intermediate (it will later be used to turn
into ATP). The Krebs cycle is a series of 8 steps that turns the pyruvate
into NADH and FADH2. These molecules will be sent to the third and
final step of aerobic respiration. In the process of the Krebs cycle,
carbon dioxide gas is released as a waste product.
3. Electron Transport Chain
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The electron transport chain (ETC) takes place along the inner membrane of the mitochondria.
The ETC takes NADH and FADH2 from the Krebs cycle and turns it into the final product of ATP.
The NADH and FADH2 can be turned into less energy forms and in the process, this excess
energy can be used to turn the ATP synthase (making ATP). Wikipedia
Anaerobic Respiration
What is Anaerobic Respiration?
Anaerobic respiration is cellular respiration that takes place without oxygen. It occurs in some
bacteria cells. It also occurs in our cells and our bodies when we do not have enough oxygen at
the time.
Lactic Acid Fermentation
Our bodies will undergo lactic acid fermentation if there is not enough oxygen present. In lactic
acid fermentation, the product of glycolysis is not pyruvate, rather it is lactic acid. This process
can create a net production of 2 molecules of ATP for the body to use. However, the lactic acid
will build up within the cell.
Teacher’s Note: While lactic acid fermentation creates energy in the form of 2 ATP
molecules, compared to actual cellular respiration which produces 36 ATP molecules, it is
not energy efficient. This is because it does not have the oxygen needed for the electron
transport chain, so the pyruvate will not be broken down.
When you run, you often feel your legs burning. The burning sensation comes from lactic acid
fermentation, what you’re feeling is the lactic acid being built up within your muscles.
Alcoholic Fermentation
Yeast is a type of bacteria that undergoes alcoholic fermentation. This type of fermentation is the
reason for how bread rises when you add yeast to it. Alcoholic fermentation produces ethanol
and carbon dioxide; ethanol is the alcohol. Carbon dioxide is what allows bread to rise.
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Photosynthesis and Cellular Respiration Connection
Teacher’s Note: Draw this diagram on the board to connect photosynthesis and
respiration and explain why the processes are often called opposite reactions.
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Lesson 5 The Cell Cycle
Summary
1. Subject(s): cell cycle and its phases, including cell division; regulation of the cell cycle;
cancer cells and cyclin and CDK
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the cell cycle and its different phases. They will also
learn about what happens when the cell cycle fails to operate properly.
Key Skills: Students should be able to explain the cell cycle and its phases, including
mitosis and cell division. Students should also be able to articulate what will happen when
the cycle fails to regulate itself and how cancer forms.
5. Time Allotment: 2-3 hours
Powerpoint
https://drive.google.com/open?id=1210ucfm6Cuk1WB0E3Qzt8aDFjHEAgDY5Eg42Xe-5qjY
Lecture Transcript
Cell Cycle
What is the Cell Cycle?
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Have you ever gotten a cut before? And then days later, you notice a scab forming over and finally, it is
good as new! Somehow, new cells appeared over the cut to heal. Where do these new cells come from?
These cells come from a process known as the cell cycle.
The cell cycle is essentially the life of a cell. It is a series of events that eventually lead up to the cell
reproducing by splitting into two identical cells. The only way living things can grow bigger is if they have
cell division and the cell cycle. Otherwise, if we have one cell that grows bigger and bigger, this would
create an ineffective and inefficient system of getting in nutrients and disposing of waste. The cycle is
split up into three main phases — interphase, mitosis, and cytokinesis.
Interphase
Interphase is the time of which the cell will grow and develop. It’s the time from when a new cell forms to
when that cell is ready to go through mitosis to produce new cells.
Interphase is further divided into three phases — , S, and .G1 G2
In the phase, the cell grows and develops. Think of representing growth 1 or the first phase ofG1 G1
growth. This is the time when the cell does its job, whatever it was meant to do. For example, a muscle
cell at phase will go through cellular respiration and create ATP.G1
The next phase is the S phase. During the S phase, the cell begins to prepare for cell division and will
replicate all of its DNA. The cell must replicate all of its DNA to create two copies such that there is the
same amount of DNA in each of the cells after they split into two.
Teacher’s Note: The process of cellular replication is complicated and should be taught to students who
in the upper age ranges. However, a simplified explanation using the image below can also be taught to
all age ranges of students. When teaching this process, draw the following diagram on the board and
draw the steps of replication to simplify the process.
First Step: The DNA strands should be separated from one another from a protein enzyme called:
helicase. While the name is unimportant, just now an enzyme breaks the strands apart. The enzyme
breaks all of the hydrogen bonds between the different bases so that the two strands can separate from
one another.
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Leaving Certificate Biology
Second Step: DNA polymerase, another enzyme, matches up the strand with the corresponding DNA
bases.
Teacher’s Note: Ask students to write the corresponding string of bases for both the left and right-hand
strands (for the left-hand strand, it would be: C-T-T-G-T-A, for the right-hand strand, it would be:
G-A-A-C-A-T). Guide students to what should be a revelation: the two new created strands are the exact
same to the parent strand. This is the process of DNA replication.
The last phase is , where the cell will undergo more growth and prepare further for division. TheseG2
are the final stages of preparation before the cell is ready to divide. This involves creating specific
organelles and microtubules necessary for the division of the cell.
Mitotic Phase
The mitotic phase is when the cell goes from a single cell, with one nucleus, to two conjoined cells each
with their own nucleus. However, the products of mitosis, the two daughter cells, are identical to that of
the parent cell. This means that the stomach cell daughter cell will be exactly identical to the parent
stomach cell.
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Teacher’s Note: Remind students that this process of cellular division can be a blessing and a curse.
Imagine if there is a cell in the body with a specific mutation. Because of cellular division, all of the cells
in the body would have that specific mutation or problem in the DNA. This means that the body as a
whole is unable to function properly.
Mitosis has a total of four steps that results in two identical daughter cells.
Teacher’s Note: Draw the following diagram on the board to explain to students how the cell is broken
into two identical cells.
Wikipedia
In summary, the DNA coils up from its chromatin form to become into condensed chromosome form. All
of the chromosomes line up at the center of the cell’s equator or metaphase plate. Then they are
separated from one another and moved to opposite sides of the cell in order to form two distinct cells.
Cytokinetic Phase
The last stage of mitosis occurs at around the same time as cytokinesis. Cytokinesis is the splitting of the
cell, when the two conjoined cells will separate into two separate cells.
In animal cells, cytokinesis occurs with a cleavage furrow, when the cell membrane will begin to pinch
around the middle and splits the cells. In plant cells, cytokinesis occurs with the growth of a cell plate
which is part of the cell wall. It will grow between the two nuclei and separate them, eventually causing
the single cell to become two individual cells.
Think of this process as creating a barrier around each of the new cells as a way to mark them as finally
an individual, completed daughter cell. Because animals do not have cell walls, the process of
cytokinesis is easier through the formation of a cleavage furrow. However, the plant cell has a cell wall
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and thus it takes more time for the wall to form around each daughter cell. Observe the following image
to see the difference between the cleavage furrow and the plant cell plate.
Dev.biologists.com (Cleavage Furrow) Visual’s Unlimited (Cell Plate)
Regulating the Cell Cycle
The cell cycle is complicated and must be regulated to ensure that the cell produces the correct
daughter cells. There are several different ways of regulating the cell cycle to ensure that it occurs
correctly and without any disruptions.
PhaseG0
phase is a resting phase. When the cell realizes that something within the cell cycle has gone wrong,G0
it automatically goes into phase. In phase, the cell does not divide and it will not create anyG0 G0
daughter cells. Think of the resting phase as the sidelines/bench of when a player is playing a sport. If
the player is injured, the coach will call for the player to be removed from the game and then put onto
the sideline bench until they feel ready enough to play again. Some cells spend most of their lives in G0
phase, especially cells that do not divide, such as liver cells.
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Cyclins and CDK
Cyclins and CDK are two types of regulatory molecules that help with keeping the cell cycle running
smoothly. These two molecules will detect the phase of which a cell is in and ensure that it is in the
proper phase and doing the correct things in that phase.
If the molecules recognize a mistake or an error in the cell cycle, they will force the cell into phase inG0
order to keep it from producing the wrong daughter cells. Think of them as the coach who puts the
player onto the field if they notice an error or that the player is not well enough to play.
Cancer
Unfortunately, even with these regulators, there are still mistakes that occur in the cell cycle that go
unnoticed. Sometimes these mistakes are extremely dangerous and can cause cancer. Cancer is a
problem in which there is uncontrolled cell growth, often because of mutations (or changes in the DNA)
of organisms. In humans, a defect in the p53 gene is often associated with an increased level of cancer
because they can manipulate with the growth regulators.
How Does Cancer Form?
Cancer forms when a cell begins to multiple uncontrollably, forming a tumor. Sometimes tumors can be
harmless and will simply be removed from the body through surgery or otherwise. However, sometimes,
the tumors can be extremely dangerous and will require a lot of treatment.
Teacher’s Note: Have students watch the following video about the mechanism of cancer:
https://www.youtube.com/watch?annotation_id=annotation_385640765&feature=iv&src_vid=f-ldPgEfAHI
&v=lpAa4TWjHQ4
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Supplemental Lesson 5a Cancer and Biomarkers
Summary
1. Subject(s): cancer cells and cyclin and CDK; cancer therapy; immunotherapy and
chemotherapy
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the current research practices of cancer therapy.
They will also learn about other mechanisms that are still in the beta/testing stage.
Key Skills: Students will be able to understand research and scientific diction as well as
apply what they have learnt the past 5 lessons to real-world research.
5. Time Allotment: 1-2 hours
Biomarkers
Biomarkers are short for biological markers. Every organism’s cells have markers on them or unique
biological tags that can identify them. Think of them as the luggage tag you place on your suitcase with
your identification on it. By looking at that tag, you can understand what kind of luggage it is as well as
who the luggage belongs to. In the same sense, biomarkers are molecules that help signal whether or
not the cell is abnormal, normal, or even belongs to the body in the first place.
Teacher’s Note: Draw the following diagram on the board to explain to students what biomarkers
are:
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Biomarkers can be DNA, RNA, proteins, and hormones. They are produced by both healthy and
unhealthy cells. While biomarkers are most studied in relation to cancer therapy, there are
particular biomarkers for all sorts of diseases: from neurodegenerative diseases to cardiovascular
diseases. These biomarkers are unique to certain diseases and the appearance of specific
biomarkers can help create therapy options that are unique to the specific patient, not just the
idea of the disease. Biomarkers are not the same thing as an individual’s genes. Instead these
biomarkers are basically little tags for the tumors to help scientists and doctors know more about
the characteristics of the bad guys in your body (rather than your body itself)!
Biomarkers are most studied in relation to cancer. Here is one example of a common biomarker:
HER2. HER2 is used to monitor cell growth similar to how CDK and cyclin helps to control the cell
cycle. But sometimes, your body might make too much of HER2. If there is too much of it, that
means that more cells are made than usual, allowing the cell growth to become rapid and
uncontrollable and often end up as a tumor. In this sense, HER2 is a biomarker. If scientists and
doctors can prescribe treatment that targets the HER2 pathway if the patient shows too much of
the biomarker, then this treatment would uniquely help them.
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Genetic Engineering and Biotechnology News
In the past, cancer therapy has been generalized to cancer and not the actual patient. Using the
novel approach of biomarkers, scientists are able to create therapies unique to the patient itself.
Using biomarkers, scientists know what specific cells not to target. For example, if you know all of
the villains or bad guys have a specific tags on them. Instead of setting off an alarm that catches
all of the people good and bad, you can specifically target the bad guys only. This is how
biomarkers have helped guide the new research methods for cancer and other diseases.
For example, biomarkers have been linked with virotherapy. Virotherapy is a type of therapy that
uses viruses and genetically modifies them to be good and beneficial biological agents, instead
of carrying disease-causing DNA/RNA. By genetically engineering viruses to target cells with
cancer biomarkers, these viruses can then kill those specific cells.
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Lesson 6 Genetics
Summary
1. Subject(s): DNA, genes, chromosomes, genetic inheritance and heredity
2. Topic or Unit of Study: Biology
3. Grade/Level: 4-6 grades
4. Objective: Students will learn the basics of genetics, including DNA, genes,
chromosomes, and heredity.
Key Skills: Students should be able to explain the basics of genetics.
5. Time Allotment: 1-2 hours
Powerpoint
https://drive.google.com/open?id=1x083g1f-rMX55eD05kJ-EveB2nQboJabRa4PKxJCMy8
Lecture Transcript
Introduction to Genetics
Genetics is a field of biology that studies how traits are passed from parents to their offspring. The passing of traits from parents to offspring is known as heredity, therefore, genetics is the study of heredity. In simple terms, genetics is the study of how you inherited your dad’s hair color or how you inherited your mom’s ear lobes.
Genetics is built around molecules called DNA. DNA molecules hold all the genetic information for an organism. It provides cells with the information they need to perform tasks that allow an
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organism to grow, survive and reproduce. A gene is one particular section of a DNA molecule that tells a cell to perform one specific task.
U.S. National Library of Medicine
Heredity is what makes children look like their parents. During reproduction, DNA is replicated and passed from a parent to their offspring. This inheritance of genetic material by offspring influences the appearance and behavior of the offspring. The environment that an organism lives in can also influence how genes are expressed.
DNA
DNA is the cornerstone of genetics and is the perfect place to start for an introduction to genetics. DNA stands for deoxyribonucleic acid and it is the molecule that holds the genetic information for a cell and an organism.
A DNA molecule contains a code that can be used by a cell to express certain genes. Specific sections of a DNA molecule provides the information to build specific proteins which can then be used by a cell to express the desired gene.
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DNA molecules are replicated during cell division. When a cell divides, the two new cells contain all the same DNA that the original cell had.
Teacher’s Note: Students should be familiar with the process of DNA replication. Review
the process by having students draw the mechanism on the board or have a quick class
discussion about it.
In sexual reproduction with two parents, half of the DNA of the offspring is provided by each of the parents. The genetic material of a child is made from 50% of their mother’s DNA and 50% their father’s DNA. This is because we inherit one chromosome from the mother and one chromosome from the father to create a chromosome pair. There are 23 pairs of chromosomes or 46 chromosomes in all (23 from our mom and 23 from our dad).
Genes
A gene is a specific segment of a DNA molecule that holds the information for one specific protein. DNA molecules have a unique code for each gene which codes for their specific protein. Some organisms can have more than 100,000 different genes so they will have 100,000 unique sequences of DNA ‘code’.
Genes are the basic unit of heredity. The genes of an individual are determined by their parent or parents. A bacteria that is born by one parent cell splitting into two cells and has the exact same genes as their one parent cell.
A human, on the other hand, has two copies of each gene – one set from their mother and a second set from their father. Different forms of the same gene are called alleles. For each gene, a human can have two different alleles or two of the same alleles – one from each parent.
For example, if the gene codes for hair color. One allele could be for blonde hair, the other for brown hair, and the other for green hair! Of course, it is not as simple as that. Let’s say for example, we inherit an allele for blue hair and red hair? Do we end up having purple hair? Sometimes but most of the time, no. The allele can be dominant or recessive. If the allele is dominant that means that no matter what it will be expressed. In this case, if the red hair allele is dominant, no matter what, if I inherit the red hair allele, I will have red hair. The recessive allele is
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one that is only expressed if there is NO dominant allele. So, in this case, if the blue hair is recessive, the only way I can have blue hair is if I inherit a blue hair allele from my mom and a blue hair allele from my dad.
Physical traits such as eye color or height are often determined by the combination of multiple genes. The environment an individual lives in also impacts how genes are expressed.
Chromosomes
A chromosome is a structure made from tightly packed strands of DNA and proteins called histones. Strands of DNA are tightly wrapped around the histone proteins and form into long worm-shaped structures called ‘chromatids’. Two chromatids join together to form a chromosome.
Chromosomes are formed in the nucleus of a cell when a cell is dividing. It is possible to see chromosomes under an ordinary light microscope if the cell is in the right stage of cell division.
The number of chromosomes varies between species. Humans have 46 chromosomes. Some species can have many more than 100 chromosomes while others can have as little as two.
Genetic Inheritance
Inheritance is the backbone of genetics and is an important topic to cover in an introduction to genetics. Long before DNA had been discovered and the word ‘genetics’ had been invented, people were studying the inheritance of traits from one generation to the next.
Genetic inheritance occurs both in sexual reproduction and asexual reproduction. In sexual reproduction, two organisms contribute DNA to produce a new organism. In asexual reproduction, one organism provides all the DNA and produces a clone of themselves. In either, genetic material is passed from one generation to the next.
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Experiments performed by a monk named Gregor Mendel provided the foundations of our current understanding of how genetic material is passed from parents to their offspring.
Activity
Engineer an Animal
For this game, have the class work together to create a new organism.
Read this prompt aloud: You are a group of scientists at the AnimCorps Lab (purely fictional). You are ordered to create a new organism to register in the international log of organisms. To ensure that this organism is purely unique, you must randomly select traits and register them in the following table.
Draw the table on the board:
Characteristic Description
Hair
Nose
Feet
Body shape
Wings
Neck
Fur
Scales
Horns
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Cut the following page into little slips. After doing so, place the slips (of the same characteristic category) in a little container. Both of the hair slips should be in the container at the same time. Then draw the slips one by one. The first slip you draw is dominant, while the second slip you draw is recessive. If for example, you draw the red hair slip first and the green hair slip last, the red hair allele would be dominant, while the green hair recessive.
Mark the different characteristics of the organism (the dominant allele as only that will be expressed) in the table to create an organism. Name the organism and draw it on the board!
YELLOW HAIR
GREEN HAIR
TRIANGLE NOSE
CIRCLE NOSE
WEBBED FEET
TWO-TOED FEET
OVALULAR BODY
SPHERICAL BODY
WINGS
NO WINGS
BLOCK SHORT NECK
LONG NECK
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LONG FUR
SHORT FUR
NO SCALES
SCALES
THREE HORNS
MANY HORNS ALONG THE SPINE
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v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOK
EPIDEMIOLOGYThe following section is for Epidemiology or the study of diseases. Students will be exposed to the different types of diseases, the biological and environmental causes of epidemics, the functions of the immune system, statistical measures scientists use themselves to analyze epidemics, and current experimental solutions to some of the world’s biggest diseases. Not only will students be able to intertwine math and biology into one subject, they will also be able to better understand the world around them.
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Lesson 1 Introduction to Epidemiology
Summary
1. Subject(s): Types of epidemiology and types of studies performed in fields of
epidemiology
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will learn about the field of epidemiology, including the types of
studies that are performed.
Key Skills: Students should be able to briefly explain about the topic of epidemiology.
5. Time Allotment: 2-3 hours
Vocabulary and Previous Concepts
Learning Context
Pathogens: infectious agent such as a virus, bacteria, protozoa, prion, a fungus, or other
microorganism (organism that causes diseases)
Incidence: number of new cases during specific period time
Prevalence: number of cases at any specific time frame or point in time
Powerpoint
https://docs.google.com/presentation/d/1t52IzrtDnqgM37TE7mbwYqYRPk_sR6a0-HnYIPpwQiQ/edit?usp
=sharing
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Lecture Transcript
Teaching Note: This lesson is very important to establishing a basic understanding of how studies
and experiments are conducted, as well as teaching students about the different elements that
are studied as part of epidemiology. Because the lesson will have new vocabulary, make sure to
go slowly and share the analogies listed in the document.
Slide 3: What is the definition of Epidemiology?
As according to the Center of Disease Control and Prevention, the United States’s Governmental
Organization in charge of dealing with disease outbreaks, the definition of epidemiology is “the study of
the distribution and determinants of health-related states and events in specified populations.” When we
break this down, distribution means the frequency and pattern of the disease. Frequency means how
often populations or people experience the disease and pattern can refer to the people, time, place of
the disease. Determinants are known as the causes and factors that relate to the disease itself.
Health-related states and events are more commonly understood as states of disorder or diseases.
Ask students: Why do you think epidemiologists call disorders, health-related states and events, rather
than diseases? The answer is that often times we think diseases are when individuals are suffering from
a physical illness or are feeling very ill. Instead, diseases and disorders are when people’s state of being
is not healthy. It does not need to be extreme or caused by a physical factor.
Ask students: What are some examples of health-related states and events that are not caused by or
have physical symptoms? Examples include depression where people are very sad for long periods of
time and often lose the will to live or Post Traumatic Stress Disorder. This disorder is often associated
with war soldiers who have had traumatic experiences, so when they come home from the war, they
have high levels of anxiety and terror because of these horrible memories.
Slide 4: Simplifying Definition of Epidemiology
A simpler definition of epidemiology is the study and analysis of health and disease.
Slide 5: Types of Epidemiology
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Epidemiology can be classified into many types. The main difference between all of these types is what
data is being collected and the application of this data to solving/preventing similar outbreaks in the
future.
Slide 6: Types of Epidemiology
Classical Epidemiology - population oriented, studies community origins of health problems related to
nutrition, environment, human behavior, and the psychological, social, and spiritual state of a population.
This is the most common approach to epidemiology because it involves scientists looking at populations
to determine why certain diseases arose and spread within the population.
Share this example: The H1N1 flu or swine flu has broken out in the town Pigville (swine is another word
for pig). Epidemiologists use classical epidemiology to understand why the flu spread from 1 person to 48
people and to compare the characteristics of each person infected. They identified a pattern or
distribution of swine flu in which very young or very old people in the population had swine flu.
Slide 7: Clinical Epidemiology
Clinical Epidemiology - studies patients in health care settings in order to improve the diagnosis and
treatment of various diseases and the prognosis for patients already affected by a disease. In other
words, after scientists collect information about the disease in the population, they can use this
information to create medicines and solutions for the disease.
Share with students: The definition of prognosis is the likely course or pathway of a disease illness and
ailment.
Slide 8: Descriptive Epidemiology
Descriptive Epidemiology is used to create a hypothesis of what could have caused the disease based
on researching about the who, when, where of the outbreak or analyzing the person, time, place.
Slide 9: Analytical Epidemiology
Analytical Epidemiology is used to test out hypothesis using experimental or observational studies. This
is because it involves looking at the what or why of the disease.
Share this with students: An easy way of remembering the difference between Descriptive and
Analytical Epidemiology is that description involves details, while analytical means analyzing. Thus the
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details of the outbreak include who, when, and where. But, by analyzing the details of the outbreak, we
can determine the what and why of the outbreak.
Slide 10: Types of Studies in Epidemiology
In order to collect data about diseases and disorders, we must carry out studies or experiments. There
are a lot of different studies scientists can perform and sometimes, if epidemiologists (scientists who
study epidemiology) want to find a solution to the disease, they can use experiments.
Slide 11: Ecological Study
Ecological - study of the interactions between environment and pathogen and host. As one can see in
the slide, the image of the mosquito represents an ecological study because it measures the interactions
between the host of mosquitos and the parasite of the Plasmodium bacterium.
Slide 12: Cross Sectional Study
Cross Sectional - a survey, health questionnaire, "snapshot in time". Cross sectional studies are focused
on prevalence or how many people have a disorder rather than then the time in which they got the
disorder. It is a known measure of descriptive epidemiology rather than analytical epidemiology.
Ask students: why would a cross-sectional study, such as a survey about diets and heart attacks, be a
measure of descriptive epidemiology rather than analytical epidemiology? Descriptive epidemiology
focuses on the who, where, and when rather than establishing a cause of the disease which is often
through analytical epidemiology. The survey would help us find more information about the types of
people who have heart disease but it would not be able to confirm the cause of the heart disease.
Slide 13: Case Control Study
Case-Control - compare people with and without disease to find common exposures or causes. For
example, if you want to identify the cause of a bad stomach illness going throughout the school, you
would find a sample group of people. Then, you would split them up into a group of people who has the
stomach illness and the other group is made of people who do not have the stomach illness.
Ask students: Who is the control group and who is the case group in this instance? The control group is
always the group without the disease, so in this case is the group of people without the stomach illness.
The case group is the group with the disease or the group of people with the stomach illness.
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After splitting them up, you would interview each person in each group to figure out what could have
caused the stomach illness. You can then identify a common cause by comparing answers to find a
pattern. For example, if a lot of people with the stomach illness ate some spoiled vegetables sold in the
cafeteria, we can infer that the spoiled vegetables was the cause of the stomach illness.
Slide 14: Cohort Study
Cohort - compare people with and without exposures to see what happens to each. By splitting up the
group into a group of people who have been exposed to the pathogen (for example, have eaten the
spoiled vegetables) and a group of people who have not been exposed, scientists can track the two
different groups over time. If the group with the higher exposure had more people the disease than the
group with no exposure, then scientists can say the pathogen caused the disease.
Share this analogy: The pathogen is a mosquito. A group of 50 students who have just returned from
the camping trip are split into two groups. One group is those with mosquito bites (exposed to
mosquitos) and the other group is those without mosquito bites (unexposed to mosquitos). The students
are tracked by the school’s epidemiologist who finds that out of the exposed group of 25 students, 10 of
them developed malaria-symptoms. However, in the unexposed group, only 1 student developed
malaria. Thus, the epidemiologist concluded that the mosquito was the cause of the disease and was
carrying malaria.
Slide 15: Experiment
In studies, scientists do not actively try to change anything. Instead, they collect data and make
observations. In the case of the experiments, scientists give one group with the disease a possible
treatment. This group is the experimental group. The other group with the disease does not receive
treatment and is known as the control group. They are used as a comparison to the experimental group.
While the other studies we talked about before are mainly about finding out a cause for the
disorder/disease, experiments are about finding medicine and treatment that work.
Slide 16: Characteristics of a Good Experiment
Blind: The participants do not know which group they are in. This way they are not subconsciously forced
to act in a certain way, according to their group. For example, if you were placed in the experimental
group and was aware that the experimental group would receive a drug that caused increased stomach
pain, you might be more likely to report stomach pain.
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Double Blind: The researcher does not know which group the participants are in. Instead, a third-party,
unbiased person or group conducts the experiment and gives the data to the researcher. This ensures
that the researcher does not prime the participants into acting a certain way.
Prime means to influence.
Randomized: This means that placement of people into a control or experimental group is random.
Placebo: The control group will receive a placebo. For example, if the experimental group is getting a pill
to alleviate stomach aches, the control group will receive a pill that does nothing except give the
impression to the control group that it is doing something. This makes sure that the results are because
of the experiment itself and not because of the feeling the solution has towards the experimental group.
Activity
Experimental and Study Design
Teacher’s Note: The following activity will allow students to apply their knowledge of experiments
and types of studies into an actual scenario. In this process, students will be able to work with
groups of other children as well as present in front of the class. Often times, students learn better
from other students, and this ensures that students understand the information from all
perspectives.
1. Split students up into groups of 3-4
2. Assign each group a type of study from the following (Preferably make it a secret so each
group has to guess what the other group has been assigned): Case-Control, Cohort,
Experiment, Cross-Sectional (It is okay for more than one group to have the same type of
study)
3. Read to the students the following prompt or write the prompt on the board:
Teacher’s Note: You can custom-tailor the prompt to be more interesting to the students you are
teaching. In the classrooms Stemnova has taught in, most students find the following prompt
engaging. If you would like to use a more challenging prompt, please refer to Prompt #2.
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Prompt #1: In the fictional school of Hogwarts, Professor Albus Dumbledore notices students are
increasingly more sleepy after the Hogsmeade Season starts. During this season, students go to
the neighboring town, where many students drink Butterbeer, a non-alcoholic sugary drink.
Dumbledore begins to wonder if the Butterbeer has an effect on student’s academic
performance or drowsiness. He asks top student, Hermione Granger, to devise a set of
experiments to answer the question: Does Butterbeer cause low academic performance in
students?
Prompt #2: Botulism has become more prevalent in the town of Diseasneyland. The symptoms
of this disease include drooping eyelids, double vision, difficulty swallowing, and respiratory
problems. Epidemiologists suspect a recently opened restaurant, Stemnova Cafe, in the center
of the town is responsible for the outbreak. However, they must carry out studies before they
request for the restaurant to be shut down. Their studies are set to answer the question: Is the
recently-opened restaurant responsible for the increased prevalence of botulism?
4. Give students 15 to 20 minutes to develop their ideas and write down how they plan to
carry out the study.
Teacher’s Note: Go around to each group while they are preparing their ideas to ensure that they
are on the right track. For students who are stuck (especially for cross-sectional), prompt them
with questions like, “What do cross-sectional studies measure?” and “Based on what they usually
measure, what would they be designed to measure in this scenario?”
5. One by one, have the groups come up in front of the class to talk about their study. Have
students guess which type of study that group was instructed to design.
6. Ask students about the strengths and weaknesses of the study and any improvements
they might have.
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Lesson 2 Types of Epidemics
Summary
1. Subject(s): Types of epidemics and how to read Epi Curves
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will learn about the different types of epidemics and how to read Epi
Curves.
Key Skills: Students should be able to read an Epi Curve.
5. Time Allotment: 1-2 hours
Vocabulary and Previous Concepts
Learning Context
Teacher Note: Start the lecture by having students talk about what pathogens are. Because
epidemics are caused by pathogens, it is important that the students understand what pathogens
are in the first place. After a discussion with the students, give them the formal definition.
Pathogen: infectious agent such as a virus, bacteria, protozoa, prion, a fungus, or other microorganism
(organism that causes diseases)
Powerpoint
https://docs.google.com/presentation/d/1N-xogUOqthWewX3HbZClWxJ1BJk-71awKNA5WRib380/edit?us
p=sharing
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Lecture Transcript
Slide 3: What is an epidemic?
An epidemic is when a large number of people over a wide geographical area are affected by the same
disease or sickness. Additionally, the number of people affected by the sickness is more than usual. The
usual number of people who are affected by the disease is For example, even if 100 individuals in the
community have the flu in December, we cannot say it is an epidemic unless we are able to compare this
number to the usual amount of people who have the flu in the community. After more data collection, we
find out that usually only 15 people in the community have the flu in December, then we can say that
there is a flu epidemic occurring. Another example is when 500 individuals in the community have
malaria. However, the usual number of people who have malaria in the community is 496. Thus, this
cannot be classified as a malaria outbreak because there is not a significant increase in the number of
cases. Diseases that are very common, in this case: malaria, are known referred to as endemic to the
area.
Epidemics are not just used to describe contagious diseases or diseases that spread from person to
person. Instead, epidemics can be used to describe all types of diseases. Recall from Lesson 1, the
Center for Disease Control and Prevention defined disease as being anything that causes a person to
not be healthy. In the United States, increased numbers of people are dying from overdosing on opioids,
a prescription drug given to them by their doctors. These opioids are painkillers, but taking too many of
them can cause addiction and oddly enough, more pain. Thus, an opioid epidemic has been declared in
America. On the other hand, contagious diseases can also be referred to as epidemics.
Ask students: Why would contagious diseases be more likely to be epidemics than noncontagious
diseases? Contagious diseases spread from person to person. This means that the number of people
who have the disease increase rapidly, causing a large amount of people to suffer from the disease.
Noncontagious diseases do not spread from person to person, so it is harder for a larger amount of
people to have the disease.
Slide 4: How are Epidemics Caused Part 1
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Because an epidemic is when more people have a disease than normally, there must be a reason why
the prevalence and incidence of the disease has increased.
Concept Check: Ask students what is the difference between incidence and prevalence? Incidence is
the number of new cases that have occurred during a timeframe, while prevalence is the total number of
cases regardless of the time.
The first cause behind epidemics is an increased amount of pathogens. Haemophilus influenzae is the
one of the many bacteria that causes the flu. If more of the Haemophilus influenzae bacteria become
present in the community, then of course more people are going to become sick with the flu, causing an
epidemic.
The second cause is when the pathogen is introduced into a new environment altogether. In the image,
you can see the Haemophilus influenzae bacteria was once in India (The Taj Mahal) but now has moved
to China (Great Wall of China). China will now experience a flu epidemic because some of the population
will be exposed to the bacteria for the first time and will contract the flu.
Slide 5: How are Epidemics Caused Part 2
The final causes of Epidemics involve people who contract the disease themselves. If people have an
increased susceptibility (vulnerable or likely to contract the disease) to the disease, then it is more likely
that their body’s immune system will not be able to fight off the pathogen. Then, the individual will
contract the disease.
Share this analogy with students: Imagine a beautiful house with a garden. After a terrible storm, the
side window of the house is broken. We can call this an increased susceptibility because now the house
is more likely to be broken into by the burglar bacteria. Ask students to relate analogy to people. If the
population has a weaker immune system or a person has an increased vulnerability to the disease, then
it is more likely that they and other people in the population will contract the disease.
Slide 7: Types of Epidemics and Epi Curves
An epi-curve is a histogram that shows the course of an outbreak by plotting the number of cases of a
condition according to the time of onset.
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Slide 8: Types of Epidemics - Breakdown
There are two main types of epidemics and their respective Epi Curves. Common Source Epidemics can
be broken up into Point Source Epidemic and Continuous Common Source Epidemic. The other
classification of Epidemics is Propagated Epidemics.
Slide 9: Common Source Epidemics
Common Source epidemics are those in which people are exposed to the same pathogen or cause.
Thus, it is a common source. For example, if raw meat is served at a picnic and most of the attendees
develop salmonella, the type of epidemic would be common source. Often times, common source
epidemics are food related epidemics and involve diseases that are not contagious. There are two types
of common source epidemics.
Slide 10/11: Point Source Epidemics
Point source epidemics occur when people are exposed to the same exposure over a limited, well
define period of time. The shape of the curve commonly rises rapidly and contains a definite peak,
followed by a gradual decline.
Slide 12/13: Continuous Common Source Epidemics
Continuous common source epidemics occur when the exposure to the source is prolonged over an
extended period of time and may occur over more than one incubation period. The down slope of the
curve may be very sharp if the common source is removed. If the common source is not removed, then
the outbreak may continue to increase or decrease gradually once the outbreak exhausts itself.
Slide 14: Characteristics of Common Source Epidemics, Epi-Curve
Teaching Note: Draw the following diagrams and have students identify what type of epi-curve
you have drawn. When they answer, have them explain the reasons behind their answer (ideally,
relating to the characteristics on the slide).
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Slide 14
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The first one is point source because it has a steep increase then a gradual decline in the number
of cases indicating that people developed the disease from a source at one point of time. The
second case is a common continuous source epidemic because the number of cases do not
decrease suddenly and instead gradually slope off after a long period of time. There are also
successive large peaks meaning that people are continuing to develop the disease because of
continued exposure.
Slide 15/16: Propagated Epidemics
Propagated (progressive source) epidemics occur when a case of disease serves later as a source of
infection for subsequent cases and those subsequent cases, in turn, serve as sources for later cases.
The shape of this curve usually contains a series of successively larger peaks, reflective of the increasing
number of cases caused by person-to-person contact, until the pool of those susceptible is exhausted or
control measures are implemented.
Slide 16/17: Drawing Epi-Curves
The first step is to draw and label the axis with appropriate units. The x-axis represents time so the units should be days, weeks, or months. The y-axis represents the number of cases of the diseases. After establishing the axis, plot the points in the coordinate form of (Time, number of cases) on the graph. Draw the bar up to the point and shade in. After drawing the bar for each point in time, identify the trend in the Epi-Curve and determine what type of Epidemic it is.
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Activity
Materials & Resources
Teaching Note: To reinforce the skills of drawing epi-curves and recognizing trends, give
students the following data points and ask them to construct an epi-curve. Then, have them
identify the type of epidemic using keywords, incubation period, time duration of epidemic,
successive peaks, and slope.
Time Jan. 2 Jan. 9 Jan. 16 Jan. 23 Jan. 30 Feb. 6
Cases 2 3 9 12 23 11
Time Feb. 13 Feb. 20 Feb. 27 Mar. 6 Mar. 13 Mar. 20
Cases 7 4 1 0 0 7
Time Mar. 27 Apr. 2 Apr. 9 Apr. 16 Apr. 23 Apr. 30
Cases 15 22 18 10 7 3
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The epi-curve when graphed should resemble the graph below. Make sure students label the
axes with appropriate units and include a title. The epi-curve resembles the trend of the
propagated epidemic because of: 1) increasingly larger successive peaks (the peak number of
cases in the first set of outbreaks is less than the peak number of cases in the second set of
outbreaks), 2) gaps between each peak. These gaps indicate the time taken for the disease to
spread from one group of people to another.
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Lesson 3 Spectrum of Disease
Summary
1. Subject(s): Etiology, pathogens, and environmental and societal causes of
diseases
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will learn about the causes of diseases.
Key Skills: Students should be able to explain the causes of diseases.
5. Time Allotment: 1-2 hours
Vocabulary and Previous Concepts
Learning Context
Genes: information we inherit from our parents that controls all of our traits including hair
color, the shape of our ears, and whether or not we may have some genetic diseases
Powerpoint
https://docs.google.com/presentation/d/1mlpVmcoJbclD9sw4vq2x8mpudN_Ek_FzZPVGyNj94kU/
edit?usp=sharing
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Lecture Transcript
Slide 2: What is Etiology?
In epidemiology, etiology refers to the study of the causes of diseases. It also can simply mean
cost. For example, I can say the etiology of the rash on my hand is poison oak (The cause of the
rash on my hand is poison oak).
Slide 3: Etiology continued
Scientists determine etiology of diseases by using experiments and studies. Remember that in
the first lesson, we talked about the various types of studies that scientists use to determine what
the cause of the disease was.
Ask students: what are some examples of studies you remember? Cohort studies are when you
divide a group of people by whether or not they are exposed to a certain pathogen. Then, you
track them over time to see whether they develop the disease. Case-control studies are when
you divide a group of people by those who are sick and those who are not. By asking the sick
people about why they may be sick, you can determine common causes.
There are different types of factors that cause etiology. A predisposing factor is a factor that you
cannot control. For example, your age, gender, and genes (refer to vocabulary section) are all
things you cannot control. But these qualities may increase your risk of contracting a disease. For
example, girls are more likely than boys to develop breast cancer. Thus, gender would be a
predisposing factor of breast cancer. A precipitating factor, however, is more in your control
because it involves being exposed to the pathogen in the first place. For example, if you have
been bitten by a mosquito which carries the pathogen for malaria, Plasmodium, then you are
likely to contract malaria. This is a precipitating factor.
Teaching Note: If students are still confused about the difference, share with them this
technique of remembering. Precipitation is like rain. The more rain that falls on you, the
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more wet you become. Similarly, the more exposed you are to a bacteria, the more likely
you are to get the disease.
Slide 3: Predisposing vs. Precipitating
Ask students: Why is the image on the right the precipitating factor, but the image on the left
is a predisposing factor? A predisposing factor is a factor outside of your control. Genes are
inherited from parents so they are out of the person’s control, making them a predisposing factor.
On the other hand, if a person is bitten by a mosquito, that is more in their control, and this is
direct exposure to a pathogen (found inside in mosquito). Thus, the image on the left is a
predisposing factor.
Slide 5: What Are Pathogens?
Pathogens are microscopic things that can cause disease. There are four different categories of
pathogens — bacteria, viruses, fungi, and protozoa. Some pathogens can cause a lot of damage,
while other pathogens are less severe.
Slide 6: Types of Pathogens
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Bacteria are microscopic organisms that come in many shapes and sizes. But even the largest
ones are only 10 micrometres long - 1 micrometre = 1 millionth of a metre. Bacteria cause diseases
such as e.coli where people get diarrhea or respiratory diseases.
Viruses are many times smaller than bacteria. They consist of a fragment of genetic material
inside a protective protein coat. Viruses cause diseases such as influenza - flu.
Larger fungi include molds and mushrooms. Microscopic fungi can cause diseases such as
athlete’s foot.
Protozoa are single-celled organisms. Food contaminated with protozoa can cause infections
such as amoebic dysentery, of which severe diarrhoea is a symptom. Some protozoa are
parasites. These organisms live on, or inside, another organism and cause it harm. Malaria is a
disease caused by protozoa that live in the blood. It is passed to a person by an insect vector, the
mosquito.
Teaching Note: If students are confused about the differences between the pathogens,
have them practice the “Types of Pathogens” through the activity. Understanding the
types of pathogens is a more advanced skill and it is not necessary for the students to
understand the types of pathogens for them to understand the spectrum of disease.
Slide 7: Environmental and Societal Causes of Diseases
Environmental diseases are diseases that have be directly attributed to the environment, not
things like genetics or infections.
Environmental diseases are a direct result from the environment. This includes diseases caused
by substance abuse, exposure to toxic chemicals, and physical factors in the environment, like
UV radiation from the sun.
There are many different types of environmental disease including:
● Lifestyle disease such as cardiovascular disease, diseases caused by substance
abuse such as alcoholism, and smoking-related disease
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● Disease caused by physical factors in the environment, such as skin cancer caused by
excessive exposure to ultraviolet radiation in sunlight
● Disease caused by exposure to toxic or irritant chemicals in the environment such as
toxic metals
Slide 8/9: Chain of Infection
Now that we understand the causes of diseases and the organisms or social/environmental
causes behind them, it is important to understand the steps in which these pathogens can enter
the body. This process is known as the chain of infection.
Slide 10: Reservoir
A reservoir is known as the home of the pathogen or where the pathogen is before it infects a
new person or animal. The reservoir can be a living thing such as a plant, animal, or human.
Reservoirs can also be the environment such the soil. Toxic chemicals, for example, can be found
in the soil. If the reservoir is person, the person is referred to a carrier. Some carriers can be
described as asymptomatic, or not showing any symptoms.
Ask students: Why is it more difficult to avoid contracting a disease if carriers are
asymptomatic? It makes it more difficult to avoid contact with someone with the disease if the
person does not show any symptoms of the disease. They seem perfectly normal.
Slide 11: Portal of Exit
Portal of exit is how the pathogen leaves the reservoir in order to enter the new host. Think of it
as the door to the house that is the reservoir. In order for the pathogen to leave the reservoir
(house), it must cross through the portal of exit (door).
Slide 12: Mode(s) of Transmission
The mode of transmission is the bicycle for the pathogen or how the pathogen travels from one
organism to another. There are two main ways pathogens can travel.
Direct transmission involves direct contact with someone who is sick (through touching) or
droplet spread which is exposure to the germs through sneezing and coughing. Indirect
transmission usually means that there is something in the middle to carry the disease, rather than
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the person directly contracting it from someone who is sick. For example, indirect transmission
can be through touching an object such as a shirt of an infected person. Vector spread involves
an animal, like mosquitoes, that carry the pathogen and transport it. Airborne transmission is
similar to droplet spread but while droplet spread is close contact in the air, airborne transmission
is over a longer distance where dust or water droplets carry germs in the air.
Slide 13: Portal of Entry
Portal of entry is how the pathogen enters the new host. It is like a new door to a new house.
Sometimes though, it takes time for symptoms to appear. Think about it. The last time you fell
sick, was it immediately or did it take time for symptoms to show? This time period that it takes for
the disease to show symptoms is known as the incubation period.
Teaching Note: Share this unique way of understanding incubation period with your
students. Incubate means to grow so if you ever hear incubation period, think of a period
of growth. In this period, the pathogen is growing such that it will finally show symptoms.
Slide 14: Susceptible Host
The last step is the susceptible host itself. Think about it, would it be easier to enter a house with
an open door or a closed door? Of course, open door. The open door represents being
susceptible because your body’s defense or the immune system is not working so your body is
left open and vulnerable to pathogens.
Activity
Spectrum of Disease Game: How to contract a disease
Teacher’s Note: The following activity will allow students to act out the process of how
individuals acquire diseases, cementing key terms and relating the different terms to a
linear process. This also allows the students a chance to get up and get active, instead of
sitting down and listening to a lecture.
One of the students will be considered a reservoir. This individual will contain or carry the
disease (in this case, the disease can be anything from a teddy bear to a toy). The student
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with the pathogen (in this case, the toy) is trying to transmit the disease to the next
susceptible host.
Teacher’s Note: Ensure students understand that the reservoir is not always the person
with the disease. It is just the environment or location in which the pathogen normally
grows and reproduces. It does not need to be a person. We are just using a student to
model it.
The reservoir can pass the disease in one of two main modes of transmission. As the
game’s moderator, tell the students whether it will be direct or indirect transmission. If it is direct transmission, the reservoir must directly touch the student who is the susceptible
host.
Figure 1: Direct Transmission Game Set-Up:
The reservoir can also pass the disease through indirect transmission. There are two
main ways of indirect transmission. The first is vector-borne, where the pathogen is
transmitted to another organism who later transmits it onto the host. The second is
airborne transmission where the reservoir will throw the pathogen to the susceptible
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host. This models the fact that the pathogen does not need to be directly transmitted to
the host, but just transmitted through the air.
Figure 2: Indirect Transmission Game Set-Up
After the pathogen is transmitted, there are 3-4 students who act as guards for the host.
These students are acting as the immune system of the host. Ask the guards to try to
prevent the pathogen from reaching the host. However, at one point, ask the guards to let
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the pathogen in. At this point, the pathogen has found a portal of entry. Because the host
no longer has any guards, it becomes a susceptible host.
Repeat the simulation using the different types of transmission and cycle students so
each student has the opportunity to be each person. For bigger groups of students, have
the susceptible host continue the game by transmitting it to another person.
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Lesson 4 The Immune System
Summary
1. Subject(s): Lines of defense in the body, humoral and cell-mediated responses of the
immune system
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will learn about the immune system and the body’s response to
pathogens.
Key Skills: Students should have a brief understanding of the immune system and how it
works.
5. Time Allotment: 1-2 hours
Powerpoint
https://docs.google.com/presentation/d/1Z3cn-Iyen-PppBY7M3cAa3Xkjju1JB6QzHw1TTRoTBo/edit?usp=s
haring
Lecture Transcript
Slide 1: The Immune System
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The immune system is one of the most important body systems. It makes sure that your body is healthy
and it helps fight off pathogens if they enter your body. Without an immune system, you would be sick all
the time!
Slide 3: Functions of the Immune System
The immune system attacks, destroys, and remembers intruders or even cells inside our own body that
may have become abnormal or sick. The three main functions of the Immune System are:
1. Scavenge dead, dying body cells (Scavenge means to look for and collect. Think of a Scavenger
Hunt).
2. Destroy abnormal (cancerous) cells
3. Protect from pathogens & foreign molecules, such as parasites, bacteria, viruses
The immune system has 3 different lines of defense to protect against foreign pathogens. They are
divided into nonspecific defenses and specific defenses.
Slide 4: Nonspecific Defenses
Nonspecific defenses mean actions taken out by the immune system regardless of the type of pathogen.
As an analogy, let’s say you were a gardener and a lot of weeds have popped up in your garden,
threatening the (Ask students for the name of a flower) you planted. Some weeds need to be pulled
out, while other weeds need to be cut. Instead of doing these specific actions, you remind yourself that
the next time you plant flowers, you will spray Round-Up or Weed Killer so that none of the weeds pop
up in the first place.
Ask students: How do we relate this analogy to the nonspecific and specific defenses? The specific
defenses are the methods carried out specific to the weed. For example, one weed needed to be pulled,
while the other weed needed to be cut. The nonspecific defenses occurred when the gardener sprayed
the garden with Weed-Killer to prevent any type of weed from popping up. The action was not specific to
a type of weed. Similarly, while specific lines of defense depend on the type of pathogen (bacteria, virus,
fungi, protozoa) and where the pathogen is, the nonspecific line of defense applies to all pathogens,
regardless of type.
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The first line of defense is made of physical and chemical barriers that prevent pathogens from entering
the body. Some physical barriers are your skin while some chemical barriers are sweat and mucus.
These chemicals are very acidic, so they can kill off bacteria or other pathogens.
The second line of defense occurs when the pathogen slips through the first line of defense and enters
the body. The immune system detects the location of the pathogen and releases millions of white blood
cells to reach the site of the infection. Because so many blood cells are traveling to the infection, the
blood vessels expand, making the area swollen. The immune system also releases chemicals that
increase your body temperature. This is known as a fever. Think of the fever as a sauna to kill all the
bacteria.
Slide 5: First Line of Defense vs. Second Line of Defense
The first line of defense acts like a wall because it prevents pathogens from even entering the kingdom
of your body in the first place. The second line of defense acts like a security guard who finds the
intruder and them removes them.
Slide 6: Specific Defenses
Physical and chemical barriers form the first line of defense when the body is invaded. This system relies
on antigens, which are specific substances found in foreign pathogens. Most antigens are proteins that
serve as the stimulus to produce an immune response to destroy and protect against the pathogen.
The basis of the immune system consists of white blood cells that are able to help to defend the body
against pathogens. The two types of white blood cells that we will talk about are B and T cells.
Slide 7: Humoral Responses
The humoral response (or antibody-mediated response) involves B cells that recognize antigens or pathogens that are circulating in the lymph or blood (“humor” is a medieval term for body fluid). The B cells create plasma cells which create antibodies. These antibodies are very important. They fit the shape of the antigen, so antibodies are specific to the antigen.
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Think of antibodies as a key that fits into the lock of the antigen. You cannot open any lock with any key. You need a specific key to open a specific lock. The antibodies bind to the pathogen causing the pathogen to be unable to move and relocate. The pathogen will die out and the B cells create memory cells to remember the intruder pathogen in the future.
Ask students: Why is it important that B cells create memory cells to remember the intruder
pathogen? This way if the same pathogen returns in the future, the body will be able to get rid of it quickly because it already has antibodies made for the specific antigen.
Slide 9: Cell-Mediated Response
The cell-mediated response involves mostly T cells and responds to any cell that displays specific markers, including cells invaded by pathogens, tumor cells, or transplanted cells. Antibodies often cannot defeat pathogens inside the cell so we need T cells to defeat the infected cells. The T cells divide into all types of T cells. The killer T cell kills pathogens. The helper T cell helps make memory T cells. Memory T cells remember the antigen. The suppressor T cells suppress killer T cells and end cell-mediated response.
Slide 10: Specific Defenses in Pictures
The humoral response occurs when the pathogen is in the body fluid, while cell-mediated response occurs when the pathogen is inside the cell.
Slide 11: Recap of How Immune System Works
Teaching Note: Have students watch this highly informative video
(https://www.youtube.com/watch?v=24IYt5Z3eC4) about the way the Immune System Works.
The video goes over the immune system using an analogy where the body is a kingdom. Make
sure students make this connection and ask them: 1) What new pieces of information they learnt
and 2) What information was repeated from the lesson you gave them? If students are confused
about macrophages and lymphocytes, clarify that lymphocytes are what B and T cells are called.
Macrophages are responsible for the first function of the immune system: scavenging dying and
infected body cells. The macrophages “eat” these infected cells.
Slide 12: Types of Immunity
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Immunity is the ability for the body to fight off diseases and resist pathogens. There are several ways your body can develop immunity.
Slide 13: Active vs. Passive Immunity
Ask students: how do you think babies have immunity against certain pathogens? After all, if babies
did not have any immunity, they would fall sick all the time. Babies have a type of immunity known as passive immunity. They get antibodies from their mother while in her womb or during breastfeeding where antibodies are passed through breastmilk.
In addition to getting antibodies from your mom, individuals can also get antibodies injected into their bloodstream. For example, when someone is bit by an animal with rabies, they are given antibodies in their bloodstream to develop an immunity against the disease.
Active immunity is developed when an individual develops antibodies on their own. They can develop it on their own by having been exposed to the pathogen in the first place. One way of exposing people to a pathogen in a healthy amount is a vaccination.
Slide 14: Vaccinations
Vaccinations are one of the most important medical discoveries of all time. In fact, according to the World Health Organization, 17.1 million lives have been saved just from death by measles because of vaccines. It was invented by Edward Jenner around 220 years ago. He noticed that a lot of people were dying from smallpox, a deadly disease. Jenner noticed that people who had gotten cowpox however, did not fall sick from smallpox. This led him to believe that those who had cowpox in the past developed immunity to smallpox. He tested this hypothesis out by giving a small dose of a cowpox virus to a child. After the child developed cowpox and recovered, Jenner exposed him to smallpox. The child did not develop the disease proving Jenner right.
Vaccines work in that they introduce a small amount of the pathogen to the human body. The human body will then create memory T and B cells that will recognize the pathogen if it ever returns. You may think, isn’t it crazy to give someone a disease in the hopes of it making them strong enough to fight the disease off in the future? But, vaccines only give a very very very small amount of pathogens. It is so little that it will not cause any illness, but just trigger an immune response.
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Ask students: Now that you understand how vaccines work, why was Edward Jenner right? By giving a small amount of cowpox (a pathogen similar to the smallpox pathogen), the child developed memory lymphocytes. Then, in the future, when Jenner gave him smallpox, the child’s memory cells quickly defeated the pathogens before it could cause any real harm.
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Lesson 5 Immune System Disorder
Summary
1. Subject(s): Allergies, Immunodeficiency Diseases, AIDS, Autoimmune Diseases, Multiple
Sclerosis, Type 1 Diabetes
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will learn about the disorders of the Immune Systems as well as
possible solutions to these different disorders
Key Skills: Students should be able to classify different immune system disorders after
understanding mechanisms of the disorder, as well as explain the biology of the
disorders.
5. Time Allotment: 1-2 hours
Vocabulary and Previous Concepts
Learning Context
RNA: single-stranded molecule in which genetic information and genes are coded into
DNA: double-stranded molecule in which genetic information and genes are coded into
Powerpoint
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=sharing
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Lecture Transcript
Slide 1: Immune System Disorders
Like any system of the body, the Immune System is not perfect. It has weaknesses and can be
susceptible to diseases. Consider that some of the disorders of the Immune System is that the
Immune System destroys its own body cells. Through this lesson, we will learn about the different
disorders of the Immune System and how we can help solve them.
Slide 2/3: Allergies
Ask students: Do any of you have allergies? How do allergies feel like? Allergies are caused by
overreactions of the immune system to usually, non-threatening antigens. Antigens that cause
allergies are known as allergens.
Teaching Note: Write on board “Antigen + Allergy = Allergens” to help the word allergen and its
relation to allergies and antigens stick.
When an allergen such as dust or pollen (Ask students if they know any more) enters the body,
it attaches to a cell known as a mast cell. While the name of the cell is not very important, just
remember that these cells cause the inflammatory response we talked about while discussing
specific defenses of the Immune System.
Ask students: Does anyone remember what an inflammatory response is? An inflammatory
response is when a pathogen enters the body and white blood cells are released to the site of
the infection. Chemicals are released to increase body temperature and kill the pathogens.
Similarly, the allergens cause the mast cells to trigger inflammatory response. The cells release
chemicals known as histamines which cause sneezing, itchy eyes, etc. The solution to having an
allergic reaction is to take antihistamines or drugs that counteract the effects of histamines.
Slide 4: Serious Allergies
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Most allergies are not very life threatening, but an example of a life threatening allergy is asthma
where allergens, stress, or exercise cause the air pathways to contract. This makes it very hard to
breathe.
Ask students: If asthma attacks are caused by the tightening of muscles in the air pathway,
what do you think medications that help people with asthma do? The medications cause
smooth muscles in the air pathways to relax so that people can breathe properly.
Independence, Missouri
As you can see in this image, the air pathway of someone with asthma is very tight. By relaxing
the muscles of the pathway, we can prevent respiratory failure.
Slide 5: Immunodeficiency Diseases
Immunodeficiency diseases are when the immune system does not work well enough. There is a
“deficiency” in the ability for it to prevent diseases. This is in contrast to allergies where the
immune system works too much.
Slide 6: Immunodeficiency Diseases Cont.
Immunodeficiency Diseases make it very hard to protect the body against infection. Think of your
body as a kingdom. What would happen if your guards were sleepy all the time and refused to
fight off invading armies? Allergies on the other hand occur when your guards are so active that
they attack harmless people like mailmen or bakers.
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Immunodeficiency diseases can be congenital meaning the immune system has not developed
properly during when the person was in the womb of the mother. Acquired immunodeficiency
diseases are when the immune system has been destroyed by a disease.
Slide 7: Acquired Immune Deficiency Syndrome
This is the most deadly and common example of the acquired immune system disorder. It is
caused by the HIV or Human Immunodeficiency Virus. The reason why this virus is so dangerous
is because its genetic material is coded in RNA instead of DNA. When the DNA molecule
replicates itself, sometimes it makes mistakes. But, it has certain ways of correcting this mistakes,
making the original DNA molecule and the later DNA molecule very similar. However, when RNA
replicates, there is no way to check back against mistakes made through replication. Thus, HIV
mutates or has a lot of changes in its genetic sequence, making it hard to create medicine to
solve the HIV.
Teaching Note: If students are still confused by the importance of HIV being a retrovirus, explain
to them that in order to create medication, the medicine needs to be very specific to the
pathogen. If the pathogen keeps changing or mutating like the RNA molecule does, then it
becomes very hard to come up with a cure.
The virus attacks T cells in the body, specifically helper T cells.
Ask students: What do helper T cells do again? They help make memory T cells which protect
the body against the same pathogen in the future. HIV makes it hard for the body to remember
pathogens. Thus, people who have HIV often do not die because of the virus itself but because
they cannot protect themselves against simple diseases such as the flu.
Slide 8: T Cell Count and HIV Infection
Scientists are able to measure the progression of HIV by counting the number of helper T cells. If
the number of Helper T cells is very low, then the HIV has developed and is in later stages of
disease.
Slide 9/10: Autoimmune Diseases
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Autoimmune diseases occur when the immune system attacks body cells. In the same kingdom
analogy, imagine the guards of your kingdom started attacking other guards because they
thought the guards were intruders. Similarly, the immune system’s macrophages and
lymphocytes are not able to distinguish between invading cells and body cells. The most
common solution or treatment to these diseases is medication that suppresses immune
response. This way, the immune cells cannot attack other immune system cells.
Ask students: Can anyone think of a bad consequence of these immune-suppressing
medications? These medications may also suppress the immune system response when the
body's affected by an actual disease. For example, when the body is attacked by flu viruses,
immune suppressing medications will prevent T and B cells from attacking those viruses as well.
Slide 11: Type 1 Diabetes
Type 1 Diabetes occur when the immune system destroys insulin-producing cells in the pancreas.
The pancreas is (point to the pancreas on your own body; between stomach and liver). These
insulin producing cells produce insulin. Insulin is a hormone or a chemical that moves sugar into
the cell of your body. In the cell, sugar is broken down into energy.
Ask students: What happens if there is no insulin in the body? Sugar will not be converted to
energy and people with Diabetes will always be tired because there is no energy.
As you can see in the diagram below, the blood sugar of someone with Diabetes is almost
double that of the someone without Diabetes.
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OPTHER
A solution to Type 1 Diabetes is giving insulin injections to people. Think of this like passive
immunity where doctors inject antibodies inside the body. Except in this case, we are injecting
insulin.
Slide 12: Multiple Sclerosis
Multiple sclerosis is when the immune system cells, specifically macrophages, destroy the
covering of neurons (nerve cells in the brain and spinal cord).
Teaching Note: Draw the following diagram on the board so students understand the importance
of the myelin sheath.
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Self-Hacked
Myelin covers the axon of the neuron and it helps make messages sent by the brain quicker. If it
is destroyed, then messages are not sent and the body is slow at responding/moving/gathering
information from the environment.
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Lesson 6 Analyzing Case Studies
Summary
1. Subject(s): Case studies, Odds ratio, Relative Risk
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 6
4. Objective: Students will learn about the different statistical measures epidemiologists use
to measure distribution of disease in a population.
Key Skills: Students should be able to apply their understanding of relative risk and odds
ratio to different scenarios.
5. Time Allotment: 2-3 hours
Lecture Transcript Epidemiology is not just the study of diseases, but also the study of how to solve these diseases.
Epidemiologists use math and statistics to figure out how prevalent the disease is in within the
population and to determine if a particular pathogen is actually the cause of the disease.
Step 1: Collecting Information
Ask students: If you were an epidemiologist, what kind of information would you collect to
help you figure out what the cause of the disease was? Epidemiologists collect information
regarding:
● Characteristics of infected population (age, location, gender, pre-existing conditions)
○ Pre-existing conditions means any disease or disorder the individual had before
they contracted the new disease. Some diseases make it easier to contract other
diseases. Like we learnt last time, if someone has HIV, their immune system is so
vulnerable that they can contract the flu.
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● Number of people in the population who is infected/ not infected
● Potential cause of the infection as according to the infected population (obtained through
surveys and interviews)
● Symptoms of the disease/infection (Symptoms are specific to the pathogen and the
subsequent disease. By knowing the symptoms of the disease, scientists can hypothesize
the cause of the disease.)
Step 2: Sorting out Information
The information collected by the scientists is usually organized into a 2 by 2 table. This table is an
easy way of seeing relationships between data.
Teacher Note: Draw the following table on the board so students are able to see where different
pieces of information go.
Without Disease With Disease
Exposed/Group A A B
Unexposed/ Group B C D
Let’s now practice organizing data by sorting through the data from a hypothetical situation. Last
Friday, 400 students from Epidemiology University all went to the Epidemiology Bistro for lunch.
The restaurant was serving two lunch specials. The first special was a lettuce and tomato salad,
while the second special was a turkey and cheese sandwiches. 230 students ate the first special,
while 170 ate the second special. The next day, 200 students who ate the first special and 20
students who ate the second special reported diarrhea, vomiting, and cramps. Health examiners
suspect the produce (vegetables) in Special 1 was infected with the bacteria e.coli, but needs
your help to confirm it.
After sorting out the data, the table should look like:
Without Disease With Disease Total
Exposed/Special 1 30 200 230
Unexposed/Special 2 150 20 170
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Total 180 220 400
You should be able to check whether or not you are right by making sure the totals of the
exposed and the unexposed is equal to the sum of the groups with and without the disease.
Step 3: Calculating Odds Ratio
The odds ratio is used to tell what the odds are of getting a disease after being exposed to the
pathogen. The odds ratio is calculated using this pattern:
AB ÷ C
D = A×DB×C
If we apply this pattern, the odds ratio for the data we collected is:
030×20200×150 = 5
If the odds ratio is greater than 1, scientists can say 1 of two things.
Scientists can correctly say that the odds of getting the disease after being exposed to the
pathogen is greater than the odds of getting the disease if not exposed to the pathogen. Thus,
the pathogen is likely the cause of the disease. In this case, it is likely that the cause of the
symptoms reported by the students is the lettuce and tomato salad because the odds of getting
diarrhea after eating the salad is higher than the odds of getting diarrhea after eating the turkey
sandwich.
Step 4: Calculating Risk Ratio
The risk ratio is used to tell what the risk is of developing the disease after being exposed to the
pathogen. The risk ratio is very similar to the odds ratio, except is calculated in a different way.
Risk is the proportion of the cases of the disease to the total number of people exposed to the
pathogen.
BA+B ÷
DC+D = DA+DB
BC+BD
.42230200 ÷ 20
170 = 7
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Similar to the odds ratio, if the relative risk is greater than 1, scientists can say the risk of getting
the disease is greater when exposed to pathogen than if not exposed to the pathogen. This
indicates that the pathogen is likely the cause of the disease. In this case, since the risk ratio
gives us the value of 7.42, we can see that the cause of the disease must be Special 1.
Step 5: Figuring Out Solutions
After scientists correctly identify the cause of the disease, they can start administering solutions.
Solutions in the case of food-borne illnesses such as this one often include rest and lots of fluids
to flush out bacteria from the body. In the case of contagious diseases, scientists may prescribe
antibiotics or other medications to stop the disease from getting more severe or spreading to
other people.
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Worksheet 6
Analyzing Case Studies
The Epidemiology Organization hosted a dinner for all of its epidemiologists. At the dinner, 6500
scientists showed up to the event. Unfortunately, there was not enough space at Venue A to host
all of the epidemiologists. 2500 scientists were moved to Venue B, while 4000 of the scientists
remained at Venue A.
The menus for the Venues were following:
Venue A:
● Caesar salad
● Macaroni and cheese
● Strawberry cake
Venue B:
● Sweet and sour soup
● Deli turkey, lettuce, and tomato sandwich
● Chocolate brownies
Around 15 hours after the event, 230 epidemiologists from Venue A reported symptoms of
nausea, diarrhea, fever, and muscle aches. 295 epidemiologists from Venue B reported similar
symptoms. Using your understanding of the odds ratio and relative risk, determine the cause of
the symptoms and using information given to you, determine the illness itself to diagnose
medications.
1. Fill out the following chart using the appropriate information.
Without Disease With Disease Total
Exposed
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Unexposed
Total
2. Calculate the odds ratio.
3. What does the calculated value of the odds ratio tell us?
4. Calculate the relative risk.
5. What does the calculated value of relative risk tell us?
6. Using the relative risk and odds ratio, was the outbreak of pathogen greater in Venue A
or Venue B? Explain.
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7. Using the table of pathogens below and their respective symptoms, identify the most
likely pathogen that caused this disease.
E. coli Listeria Salmonella
● Watery diarrhea,
abdominal
cramps, some
vomiting
● Incubation period
of 1-3 days
● Bacteria found in
undercooked
meat
● Fever, muscle
aches, nausea,
diarrhea
● Incubation period
of 9-28 hours
● Bacteria found in
ready to eat deli
meats,
unpasteurized
milk, soft
cheeses
● Diarrhea, fever,
abdominal
cramps, vomiting
● Incubation period
of 6-48 hours
● Bacteria found in
eggs, poultry,
meat, cheese,
raw fruits and
veggies
8. Give solutions or possible tips to prevent this outbreak from happening in the future.
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Worksheet 6 Analyzing Case Studies
The Epidemiology Organization hosted a dinner for all of its epidemiologists. At the dinner, 6500
scientists showed up to the event. Unfortunately, there was not enough space at Venue A to host
all of the epidemiologists. 2500 scientists were moved to Venue B, while 4000 of the scientists
remained at Venue A.
The menus for the Venues were following:
Venue A:
● Caesar salad
● Macaroni and cheese
● Strawberry cake
Venue B:
● Sweet and sour soup
● Deli turkey, lettuce, and tomato sandwich
● Chocolate brownies
Around 15 hours after the event, 80 epidemiologists from Venue A reported symptoms of
diarrhea, fever, and muscle aches. 295 epidemiologists from Venue B reported similar symptoms.
Using your understanding of the odds ratio and relative risk, determine the cause of the
symptoms and using information given to you, determine the illness itself to diagnose
medications.
1. Fill out the following chart using the appropriate information. (Hint: Epidemiologists are
confident the outbreak was in Venue B).
Without Disease With Disease Total
Exposed/Venue B 2205 295 2500
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Unexposed/Venue A 3920 80 4000
Total 6125 375 6500
1. Calculate the odds ratio.
R .556O = 2952205 ÷ 80
3920 = 6
2. What does the calculated value of the odds ratio tell us?
Because the calculated odds ratio is greater than 1, it tells us that the odds of getting the disease
from Venue B are 6 times the odds of getting the disease from Venue A. Thus, the outbreak is
larger in Venue A.
3. Calculate the relative risk.
R .900R = 2952500 ÷ 80
4000 = 5
4. What does the calculated value of relative risk tell us?
Because the relative risk is greater than 1, it tells us that the risk of getting the disease is higher in
Venue B than it is in Venue A. Specifically, the risk of getting the disease from Venue B is 5.9
times the risk of getting the disease in Venue A.
5. Using the relative risk and odds ratio, was the outbreak of pathogen greater in Venue A
or Venue B? Explain.
In both cases, the relative risk and the odds ratio was greater than 1, indicating that the risk of
getting the disease is higher in Venue B than in Venue A. This is because all of the calculations
assumed Venue B to be the exposure factor
6. Using the table of pathogens below and their respective symptoms, identify the most
likely pathogen that caused this disease.
E. coli Listeria Salmonella
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● Watery diarrhea,
abdominal
cramps, some
vomiting
● Incubation period
of 1-3 days
● Bacteria found in
undercooked
meat
● Fever, muscle
aches, nausea,
diarrhea
● Incubation period
of 9-28 hours
● Bacteria found in
unpasteurized
milk and soft
cheeses
● Diarrhea, fever,
abdominal
cramps, vomiting
● Incubation period
of 6-48 hours
● Bacteria found in
eggs, poultry,
meat, cheese,
raw fruits and
vegetables
Salmonella; The symptoms (all except for vomiting) all match that of Salmonella bacteria. The
incubation period of 15 hours (the time taken for the epidemiologists to contract the disease after
eating the dinner) fits within the range of incubation period of 6 to 48 hours. Additionally, it is
Salmonella because the foods of meat and raw vegetables were included in the Venue B menu. It
cannot be Listeria because there was no unpasteurized milk and cheese in the menu for Venue
B.
7. Give solutions or possible tips to prevent this outbreak from happening in the future.
Cook all meat and make sure to wash all vegetables thoroughly in the future. Epidemiologists
with Salmonellosis should take plenty of rest and lots of water to flush out the bacteria.
Additionally, doctors should prescribe antibiotics for the patients to help the body kill the
bacteria.
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Activity 7 Conclusion to Epidemiology
Summary
1. Subject(s): Study of epidemiology in present, current world
2. Topic or Unit of Study: Epidemiology
3. Grade/Level: 5-6 grades
4. Objective: Students will get an conclusion to what basic epidemiological terms mean in
the real world and how to make key connections.
Key Skills: Students should be able to use critical thinking to answer questions about the
article and how it connects to the lesson.
5. Time Allotment: 1 hour
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Article Teacher’s note: Highlighted information/sentences should be emphasized to students while
reading it as a class or asking students to read independently. Stemnova’s comments are written
in red and are not to be confused with the statement of Soumya Karlamangla or the Los Angeles
Times.
Severe flu brings medicine shortages, packed ERs and a rising death toll in California By Soumya Karlamangla (Courtesy of the Los Angeles Times)
So many people have fallen sick with influenza in California that pharmacies have run out of flu medicines, emergency rooms are packed, and the death toll is rising higher than in previous years.
Health officials said Friday that 27 people younger than 65 have died of the flu in California since October, compared with three at the same time last year. (This information proves that this is an epidemic because it is 24 more people who are affected by the flu. Endemics are the baseline number of how many people usually get the disease, while epidemics are much larger than this baseline number. Epidemiologists only declare emergency or focus attention on the outbreak if it is an epidemic.) Nationwide and in California, flu activity spiked sharply in late December and continues to grow.
The emergency room at UCLA Medical Center in Santa Monica typically treats about 140 patients a day, but at least one day this week had more than 200 patients — mostly because of the flu, said the ER’s medical director, Dr. Wally Ghurabi.
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“The Northridge earthquake was the last time we saw over 200 patients,” Ghurabi said. Experts say it’s possible that this year’s flu season is outpacing the last simply because it’s
peaking earlier. The flu season is typically worst around February, but can reach its height anytime from
October to April. Though influenza had only only killed three Californians at this time last year, it had taken 68 lives by the end of February, according to state data. (This is more evidence proving the epidemic level of the influenza virus).
Many California doctors, however, contend that the recent surge has been unusually severe.
“Rates of influenza are even exceeding last year, and last year was one of the worst flu seasons in the last decade,” said Dr. Randy Bergen, clinical lead of the flu vaccine program for Kaiser Permanente in Northern California.
State health officials said Friday that there was no region of the state where people were being spared from the flu. (This should indicate to the students that the flu is contagious and spreads from person to person. This is known as a propagated spread of disease. This should have been referenced in lesson 2).
In Riverside and San Bernardino counties, ambulance services have been severely strained because of the number of flu calls coming in, (example of a potential problem that epidemiologists can target for better healthcare and less fatalities or deaths) local health officials said.
Plus, emergency rooms are so crowded that ambulances arriving at hospitals can’t immediately unload their patients, (another example of a problem epidemiologists should target) so they’re unable to leave for incoming 911 calls, said Jose Arballo Jr., spokesman for the Riverside County Department of Public Health.
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“The ambulances have to wait … and if they’re waiting there, they can’t be out on calls,” Arballo said.
Most people in California and nationwide are catching a strain of influenza known as H3N2, (This is because influenza is a virus, a type of pathogen in which there is only genetic material and a protein coat. DNA and RNA change quickly, which means last year’s flu shot may not be able to stop this year’s flu. Take for example, a little puppy. At first, you buy them a pen that is very small, but then as they keep growing, that old pen may not work for them anymore. Then, you need to buy them a bigger house. In the same way, flu shots need to be made every time the DNA/RNA changes/mutates) which the flu vaccine typically doesn’t work as well against. National health officials say the vaccine might only be about 32% effective this year, which could be contributing to the high number of people falling ill.
H3N2 is also a particularly dangerous strain of the flu, experts say. “It tends to cause more deaths and more hospitalizations than the other strains,” said Dr.
Jeffrey Gunzenhauser, L.A. County’s interim health officer. Of extra concern this year are large numbers of older patients who are showing up at
hospitals with the flu and pneumonia, a potentially fatal combination. “You have no choice but to admit them and hydrate them on IV antibiotics to prevent --
God forbid -- a bad outcome,” Ghurabi said. Each year, the number of flu deaths reported by the state includes only people younger
than 65 and therefore underestimates the flu’s real toll, since elderly people are most likely to succumb to the illness, experts say. In Los Angeles County, 33 people have died of the flu this season and only a handful were under 65, Gunzenhauser said.
Dr. Matthew Mullarky, an emergency physician at St. Joseph Hospital in Orange, said that half of the patients he saw on a recent ER shift were so sick that he had to keep them in the hospital. Most of them were older than 85, with the flu and pneumonia.
“It’s incredibly scary,” he said. Doctors often prescribe the flu medication oseltamivir, known by the brand name Tamiflu,
to patients with the flu. But doctors and patients said this week that the drug was hard to find. (Tamiflu might be a good control measure for the epidemiologists to investigate. A control measure is a tactic scientists use to help stop the spread or prevent the epidemic from becoming a pandemic - going internationally. Scientists may want to increase production of the Tamiflu).
Caroline Bringenberg, who lives in Silver Lake, fell ill when she was visiting her family in Denver for the holidays. She had headache, fever and weakness.
“I don’t remember the last time I was this sick,” said Bringenberg, 25. When her doctor prescribed her Tamiflu on Wednesday, Bringenberg learned that a CVS
pharmacy in Glassell Park was out of the medicine. All the CVS pharmacies in the area had run out, the pharmacists there told her.
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Bringenberg then called a nearby independent pharmacy, but it also had exhausted its supply.
“I’ve just sort of given up,” said Bringenberg, through sniffles. “I think honestly it would make me feel worse to be in the car driving all over town, so I've just opted for ibuprofen and DayQuil.”
CVS spokeswoman Amy Lanctot said increased demand for Tamiflu in California may have led to some stores being temporarily out of stock. Other pharmacies reported that they were running low on the medicine or were out completely.
“They’re all on back order right now,” said Talia Dimaio, a pharmacy clerk at Rancho Park Compounding Pharmacy in West L.A. “We can’t get it.”
Bob Purcell, spokesman for the San Francisco-based pharmaceutical company Genentech, which makes Tamiflu, said there isn’t a national shortage of the medicine, suggesting that pharmacists’ shelves were emptied this week by a sudden surge in demand.
Marenna Bielman, right, takes Angelica Lara's blood pressure as she is treated for flu-like symptoms at St. Joseph Hospital in Orange.
Doctors say Tamiflu doesn’t eliminate the flu but lessens the severity of symptoms and how long they last. It works best if taken within 48 hours of when patients start to feel sick.
Nihar Mandavia, a pharmacist who owns the Druggist Pharmacy in Laguna Niguel, said he’s been ordering as much Tamiflu as possible from wholesalers and filling 25 prescriptions a day, compared with a typical one a day. He said out-of-stock pharmacies are referring patients to him.
“It’s been crazy,” he said. “And there’s still more -- we’re getting calls right now.” On Friday morning, Mandavia had enough left for only four more patients, he said. And
some of his wholesalers had run out too. Though flu season is underway, health officials say it’s not too late to get the flu shot. The
vaccine is recommended for everyone older than 6 months. “Even if you’re healthy, the downside of getting the flu vaccine is so low — it’s relatively
inexpensive. At the worst you’ll have a sore arm,” Gunzenhauser said. The vaccine can also mean not getting sick and then infecting someone who might not
recover so easily. Nationwide, 13 children have died of influenza this flu season. Dr. Greg Hendey, UCLA’s chair of emergency medicine, said people usually develop flu
symptoms two to three days after they’re exposed to the virus, (What is this time period called? Incubation period) but are most contagious the day before symptoms develop.
“So before you even know you’re sick you’re already spreading the virus,” he said. He recommended that people wash their hands often and avoid close contact with
anyone coughing or sneezing.
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Hendey said they’ve been trying to adjust staffing levels at the ER to keep up with the crowds, but there’s been an added challenge lately.
“Sometimes we don’t have our full complement of nurses because, they’re people too, they get sick,” he said.
Questions
1. How do epidemiologists know this is an epidemic and not just an endemic?
Highlighted references indicate that more people than usual are being affected by this strain of
the flu. This means that the number of cases are above the baseline level. By looking at the graph
presented in the article, we can see that the number of cases are clearly exceeding the usual average.
2. What type of spread is this illness?
Propagated; The spread is person to person, as the article states that “people usually develop flu
symptoms two to three days after they’re exposed to the virus, but are most contagious the day before
symptoms develop.” This means that people show symptoms and then spread the disease to others.
3. Name at least three symptoms of this H3N2 strain.
Headache, fever, sniffles, coughing, sneezing, weakness (muscle fatigue)
4. What is a problem regarding the influenza virus that occurs every year, not just this particular
time?
The virus mutates often, forcing scientists to continue researching newer and newer flu shots to prevent
the flu.
5. What are some possible control measures you as an epidemiologists would recommend for the
specific situation? List two.
● Increasing ambulance dispatch services (more ambulances and staff)
● Flu warnings to schools, workplaces to alert people to avoid those showing possible
symptoms
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● Increased production of Tamiflu to help decrease symptoms
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v vEPIDEMIOLOGYTEACHER GUIDE AND CURRICULUM HANDBOOK
GEOLOGYThe following curriculum section is for Geology. It introduces students to basic chemistry and ecology with an overlying focus on the interactions of these various science fields in the ocean. There is a stressed importance on current events: the mechanism of global warming. Along with explaining the impacts of global warming, we devote a section of the class to exploring different technologies that are currently being used to delay the onset of global warming. The curriculum also touches upon fossils and the use of landforms to give us insight about the Earth’s history.
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Lesson 1 Geology
Summary
1. Subject(s): Plate tectonics, Wilson cycle, where land meets sea, types of sediment
2. Topic or Unit of Study: Oceanography
3. Grade/Level: 4-6 grades
4. Objective: Students should learn a basic understanding of geology associated
with oceanography.
Key Skills: Students should be able to explain plate tectonics, the Wilson cycle, the
way that land and sea meet, and types of sediment.
5. Time Allotment: 2-3 hours
Powerpoint
Core Curriculum:
https://docs.google.com/presentation/d/1IDSokU09nyt8kebInwSv-Nk2_vAwAMJa_GJZZ1QrHAg/
edit?usp=sharing
Supplement Curriculum:
https://docs.google.com/presentation/d/1zujUzeJdPxl5HGXM5C2k0tCsAeP9sh1-KUf6-ALZ7oE/ed
it?usp=sharing
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Lecture Transcript (Core Curriculum)
Plate Tectonics
We tend to think of land on Earth as being fixed and unmoving, however, the land does move.
The movement is very, very slow, only about 1 to 5 inches per year. It takes over millions of years
for the movement to be noticable.
The part of the land that moves is called the lithosphere. The lithosphere is made up of the
Earth’s crust and a little more further down into the Earth. The lithosphere moves in big chunks
called plate tectonics. The plate tectonics are a little bit like giant puzzle pieces. There are 2
types of plates, continental and oceanic plates. Continental plates are the ones that form
continents, like the African Plate, Australian Plate, and South American Plate. Oceanic plates are
beneath oceans, like the Pacific Plate. The main difference between these 2 types of plates that
you need to know is that oceanic plates are denser.
There are three types of movements that the plates experience — convergent, divergent, and
transform.
Convergent
In the convergent type of plate movement, the plates move towards one another and give rise to
geographical structures like mountain ranges and volcanoes.
India and Asia collided into each other about 55 million years ago, which led to the formation of
the Himalayas, the highest mountain range on the earth.
Similarly, when the oceanic plates crash into each other deep trenches like the Mariana Trench in
the North Pacific Ocean and underwater volcanoes are formed.
Divergent
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In the divergent type of plate movement, the plates move apart.
The magma from the interior of the Earth surges toward the surface and pushes the tectonic
plates away from each other. Between oceanic plates, divergent boundaries are called
mid-ocean ridges. Between continental plates, divergent boundaries are called rift valleys.
One famous mid-ocean ridge is the Atlantic Mid-Ocean Ridge. This is the longest divergent
boundary in the world at 10,000 miles and occurs where the North and South American Plates
are moving away from the Eurasian and African Plates. Along this ridge, there are many
volcanoes and earthquake epicenters.
Additionally, scientists believe that millions of years from now, Eastern Africa will split apart from
the continent and form a new landmass. This divergent boundary is called the East African Rift
Valley, and it is one of the most volcanically active places in the world.
Transform
In the transform type of plate movement, two plates move sideways with respect to each other.
When the two plates rub against each other, a lot of energy is built up, and this energy is
sometimes released as earthquakes.
These movements do not produce spectacular geographical features like mountains or
oceans
Hotspots
Very different from the boundaries mentioned above, hotspots are found in the middle of
tectonic plates. Hotspots are regions where a lot of magma is rising to the surface, and
this magma often breaks through the plate, leading to volcanoes. A great example is
Yellowstone National Park. Right in the middle of the United States, Yellowstone National
Park is nowhere near a plate boundary, but there are still many signs of volcanic activity,
geysers, hot springs, minor earthquakes, and a humongous volcanic crater. This is
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because right below Yellowstone is a column of magma rising to the surface. This magma
brings heat and may eventually poke through.
The Wilson Cycle
The Wilson cycle is the cyclical opening and closing of ocean basins caused by movement of the
Earth’s plates. The Wilson cycle begins with a rising plume of magma and the thinning of the
overlying crust. As the crust continues to thin due to extensional tectonic forces, an ocean basin
forms and sediments accumulate along its margins. Subsequently subduction is initiated on one
of the ocean basin’s margins and the ocean basin closes up. When the crust begins to thin again,
another cycle begins.
The Wilson cycle comes in four stages:
Stage A — begins with a stable continental craton. A craton is a part of the lithosphere that is old
and stable. A hot spot rises up under the craton, heating it, causing it to swell upward, stretch and
thin like taffy, crack, and finally split into two pieces. This process not only splits a continent in
two it also creates a new divergent plate boundary.
Stage B – the one continent has been separated into two continents, east and west, and a new
ocean basin is generated between them. As the ocean basin widens the stretched and thinned
edges where the two continents used to be joined cool, become denser, and sink below sea
level. Wedges of divergent continental margins sediments accumulate on both new continental
edges.
Stage C – the ocean basin widens, sometimes to thousands of miles; this is comparable to the
Atlantic ocean today. As long as the ocean basin is opening we are still in the opening phase of
the Wilson cycle.
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Stage D – the closing phase of the Wilson Cycle begins when a subduction zone (new
convergent plate boundary) forms. The subduction zone may form anywhere in the ocean basin,
and may face in any direction.Once the subduction zone is active the ocean basin is doomed; it
will all eventually subduct and disappear.
Types of Sediment
There are three types of sediment — clastic, chemical, and biochemical sediments.
Clastic
Clastic sediments are composed of fragments or grains (or clasts) of other rocks and minerals.
We classify clastic sediments based on their grain size. Grain Size reflects the amount of bumping
and grinding that has occurred. For example, the largest clasts are generally found close to the
source of the sediment, since they are harder to transport. The farther away you go from the
source, the more grinding occurs between the clasts, and they become smaller and smoother
from the transportation process.
Chemical
Chemical sediments are not formed from the weathering and erosion of other rocks. They form
from the precipitation of minerals out of a solution. Most commonly, the solution is sea water, and
the precipitates are called evaporites.
Biochemical
At the end of the Cambrian era, marine organisms obtained the ability to form protective shells.
When these organisms die, their shells fall to the sea floor forming biochemical sediment. Much
of this material comes from microorganisms (organisms of microscopic size). The primary
biochemical rock is limestone. If the shells are not ground finely, the material may be called
bioclastic.
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Lesson Transcript (Supplement Curriculum)
The Rock Cycle
The rock cycle is a series of changes that circle around three types of rocks — igneous,
sedimentary, and metamorphic. These three types of rocks can change into one another through
the processes of the rock cycle. Before we jump into the specifics, let’s actually examine what the
three types of rocks are.
Igneous Rock
Igneous rock is formed from magma. Magma is lava that has come out of a volcano, it is an
extremely hot liquid that is made out of melted minerals. When magma cools, it forms igneous
rocks. Igneous rock can form above or below ground. Above ground, the magma cools very
quickly or suddenly, such as when it touches water. However, underground, the magma will cool
much slower. Igneous rocks that form from magma cooling above ground are called extrusive
rocks; igneous rocks that form from magma cooling below ground are called intrusive rocks.
Sedimentary Rock
Sedimentary rock is formed when sediments, small tiny pieces of rock, are packed together. Over
time, these sediments become cemented together and create sedimentary rock. If you look at
the picture at the left of conglomerate, a type of sedimentary rock, you can actually see the
smaller rock pieces packed together.
Metamorphic Rock
Metamorphic rock forms when rocks are heated to extremely high temperatures. When rocks
become buried deep underground, the temperature is very very high. The high temperature will
cause the rock to form crystals and become metamorphic rock. If you look at the picture at the
left, you will see that the rock has neat stripes across from left to right. If you see these stripes, it’s
usually a sign the rock is metamorphic since high pressures cause these patterns to form.
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How Does One Type of Rock Change Into A Different Type?
Igneous or sedimentary rock can change into metamorphic rock if they undergo extreme heat
and pressure underground. To get to igneous rock, both sedimentary rocks and metamorphic
rocks can be melted into magma. This magma then cools underground or above ground and
forms igneous rock. To get to sedimentary rock, both igneous rocks and metamorphic rocks can
be eroded into smaller pieces called sediments by wind, water, plants, and other natural forces.
Over time, these small sediments are packed together and cement to form new sedimentary
rock.
Dating Rocks
Today, scientists have plenty of ways to determine the ages of rock layers and fossils. There are
two general categories of rock and fossil dating - relative dating and absolute dating.
Relative Dating
Geological Principles
In relative dating, the general age of a rock layer or fossil is determined. Relative dating is the
method used most often to date fossils. One key principle to remember is the Law of
Superposition. This law basically states that in undisturbed rock layers, younger rock layers are
always on top of older ones. Sounds pretty obvious right? Based on the picture and the Law of
Superposition, one can safely assume that the yellow, lighter rock layers on top are older than
the redder rock layers on the bottom.
Relative Dating: The Process & Multiple Index Fossils
Simply put, relative dating is a method that compares a unknown rock layer or fossil’s age with
one that scientists already know. Scientists use index fossils to help determine the time frame of
other fossils and rock layers. Index fossils are fossils that are only known to occur in a certain
time period.
Now, relative dating can be used to date fossils or rock layers. For example, let’s say you have a
layer of sandstone you are trying to figure out the age of. In the layer of sandstone, you find a
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specific tree fossil, and you know that species of tree lived 3 million years ago. Based on this
information, you can probably guess safely that the mysterious sandstone is approximately 3
million years old. Here’s another example. Let’s say you discover a mysterious insect fossil in
clay. Based on previous studies, you know the clay is 20 million years old, so thus, the insect is
also probably around 20 million years old.
Sometimes multiple index fossils can be used. In a hypothetical example, a rock formation
contains fossils of a type of brachiopod known to occur between 410 and 420 million years. The
same rock formation also contains a type of trilobite that was known to live 415 to 425 million
years ago. Since the rock formation contains both types of fossils the ago of the rock formation
must be in the overlapping date range of 415 to 420 million years.
Absolute Dating
Half Life
Before we jump into absolute dating, it is important to understand the concept of the half life.
Essentially, as time passes, radioactive elements such as Uranium or Carbon-14 (a type of
carbon), break down into simpler elements through a process called radioactive decay. The
half-life of a radioactive element is the time it takes for half of the substance to decay. For
example, let’s say you have 100 grams of Element A, and you know Element A’s half-life is 500
years. That means that after 500 years, you will only have 50 grams of Element A. A more
realistic example is Carbon-14. Carbon-14 slowly decays into Nitrogen-14, a simpler element, and
its half-life is 5700 years. This means that if you have 100 grams of Carbon-14, after 5700 years,
you will only have 50 grams left.
Absolute Dating
Absolute dating uses radioactive dating to determine the exact time period of a fossil. It uses
radioactive materials, like elements we mentioned before, found in the fossil as a geological
clock. Again, certain radioactive elements leave traces of themselves over time and will decay
over time. By seeing how much of the element is remaining and how much has decayed to a
different element, scientists can determine the exact time period of a fossil.
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For example, we already know Carbon-14 decays into Nitrogen-14 over 5700 years. If I take an
old tree fossil and discover there are 2 grams of Carbon-14 and 2 grams of Nitrogen-14, I know
the ratio of Carbon to Nitrogen is 1 to 1. This means that half the total amount of substance is
Carbon and the other half is Nitrogen. Because I know Carbon-14’s half-life is 5700 years, this 1 to
1 ratio tells me the tree fossil is most likely 5700 years old. (Teacher’s Note: To better illustrate
this example, it might be best to draw a diagram on the board or utilize the slide as a visual
reference.)
Activity
Modeling Plate Tectonics
Teaching Note: The purpose of this activity is to give students a better conceptual
understanding of the structure of the Earth. Using common food items, students will
create a model of the Earth’s surface and then enjoy their masterpiece after.
Materials Needed: Different colored candies (M&Ms), crackers, white frosting (dye red if
possible), paper plates, plastic knives, marshmallows, and chocolate frosting/Nutella
1. To conserve materials, organize the students into pairs or groups of three. Each
group needs one paper plate, one spoonful of chocolate frosting, one spoonful of
vanilla frosting, a pack of M&Ms, one marshmallow, two graham crackers, and two
plastic knives.
2. Read the following prompt aloud: “You are a geologist hired by the kingdom of
Candyland to better understand the planet’s geography. Candyland has a very
similar structure to Earth except everything is edible. Use the following pieces of
information to construct a model of Planet Candyland”
3. Have each group spread the white frosting across the plate. Ask them what layer
of the planet the frosting represents and why? - Sample Answer: The frosting
represents the mantle beneath the crust. Like the mantle, the frosting is not rigid,
able to move around, and sticky.
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4. Have each group break the crackers into at least four pieces and lay them on top
of the frosting; two of the crackers should be spread with brown frosting. Let the
students know that each of the cracker pieces represent a plate, and ask them
what they the frosted crackers represent and why? - Sample Answer: The brown
crackers are oceanic plates since they are heavier and denser that the
non-frosted ones.
5. Have each group identify convergent, divergent, and transform boundaries - this
can be up to their choice. Students should line convergent boundaries with blue
candies, transform boundaries with yellow candies, and divergent boundaries with
red candies. Ask them, “Is it possible for a boundary between a frosted and
non-frosted cracker to be lined with red or yellow candies?” - Sample Answer: No;
because the oceanic plate is denser, it always sinks beneath the continental one,
creating a convergent boundary that should be lined with blue candies.
6. Read the following aloud: “Now we have the basic map of Planet Candyland.
However, we just got new data that there is a hotspot beneath one of the oceanic
plates.” Ask the students what a hotspot is, and have them represent the hotspot
with one marshmallow passed out.
7. With the orange M&Ms, have the students map out where they think volcanoes
should be. There should be orange candies near the marshmallow and along the
convergent and divergent boundaries. Ask them why there shouldn’t be
volcanoes allow the yellow transform boundaries and why there are volcanoes
near the hotspot.
8. Now, assign the following words to each group: friction, earthquakes and
tsunamis, land formation, and the Wilson Cycle. Groups should present their plates
and explain how the term they’ve been assigned relates to their map.
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Lesson 2 Ocean Movements
Summary
1. Subject(s): Ocean temperature, salinity, and density
2. Topic or Unit of Study: Oceanography
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about factors of temperature, salinity, and density in
the ocean
Key Skills: Students should be able to explain the ocean in relation to temperature,
salinity, and density.
5. Time Allotment: 1-2 hours
Powerpoint
https://docs.google.com/presentation/d/18XFUJ53k8AE1MpdMKJ-EMlKrKf9Btewg5qpgkKkKvz8/e
dit?usp=sharing
Lecture Transcript
Ocean Movements
The ocean is not a uniform body of water. The ocean is made up of many water masses that flow past each other. These distinct masses of water each have a characteristic density. Density is the relative heaviness of a substance; it is mass per unit volume. Dense water masses will sink while
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less dense ones will float above them. It is similar to density differences that lead to oil floating on top of water in a bottle of salad dressing. Water masses of different densities will similarly layer out. This layering is known as stratification in the ocean. There is no single perfect example of a "typical" stratification, though the link below is a neat graphic.
Density
Density of seawater is primarily determined by two factors: temperature and salinity. Warmer water is less dense than colder water. Therefore, warm water floats near the surface while cold water will sink toward the bottom. Salinity also affects density. Higher salinity (more salts in the water) leads to higher density. So salty water sinks while fresh water floats at the surface.
Anywhere in the ocean where water masses of different salinity and/or different temperature meet, the ocean will be stratified. There will be distinct layers of water found at different depths. The layer of the ocean where density increases the fastest is called the pycnocline.
Temperature
The major source of heat for the ocean is the sun. Therefore, it is only surface waters that get heated. Deep-ocean water is cold with temperatures hovering around 40C. The sun does not heat the surface of the ocean evenly. Polar regions receive very little, diffuse sunlight and even surface waters are cold there. Therefore the entire column of water from the surface to the bottom is cold; there is no thermal stratification. Tropical regions receive the most solar energy and tropical surface waters are warm. The warmer surface waters, with their low density, float on top of the colder deep water and the ocean is thermally stratified in the tropics. Temperate surface waters are cold in the winter but warm up in the spring and summer. Therefore, in these regions, there is no thermal stratification in the winter. It builds up as the seasons change and there is strong stratification in the summer months.
Plotting the change in temperature with depth, in the tropics for example, clearly shows that temperature does not just decrease uniformly with depth. Instead, there are three distinct layers or zones. The warm upper zone, known as the mixed or surface zone, is kept uniformly warm as waves and currents distribute the solar energy from the sun. The middle zone is a region where temperature decreases with depth; this is known as a thermocline. Within the thermocline, warm surface water mixes with cold deeper water. Below the thermocline is the deep layer, which is uniformly cold.
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Salinity
Salinity is a measure of the total amount of dissolved solids (salts) in the ocean. The average salinity in the ocean varies from about 33 – 37 parts per thousand (ppt or o/oo). Salinity can approach 0 (fresh water) where rivers enter the ocean and may be very high in areas where there is little rain and an excess of evaporation. The amount of rainfall, input from rivers and streams and the level of evaporation will all affect the salinity of the ocean in any area. Therefore, most salinity variation take place near the surface where these environmental influences occur.
Diffusion is the slow mixing that occurs due to random motion of molecules. The salts and water molecules in seawater are vibrating and this vibration causes them to bounce off each other and mix. Salts will slowly spread away from areas of high salinity and toward areas of low salinity due to diffusion and the salinity of those areas will change.
The salts dissolved in seawater are heavier than the water molecules themselves. Therefore increasing the salinity of water increases its density. Water with low salinity will float on top of water with a high salinity, as happens when river water flows into the ocean. Salinity, as temperature, does not increase uniformly with depth. A plot of salinity versus depth shows three distinct zones. The upper mixed zone is characterized by lower salinity. The middle zone is a zone where salinity increases with depth; this is known as a halocline. Below the halocline, the deep zone contains water of fairly uniform higher salinity.
Activity
Density Demonstration
Teaching Note: The purpose of this demonstration is to show how water masses of
differing densities interact with each other. Students will also receive a more in-depth look
of the thermocline.
Materials Needed: two 500-600 mL beakers per group (any large glass container works
as well as long as it is transparent), sea salt (NaCl), Epsom salt (MgSO4), hot water, cold
water, room temperature water, red food coloring, blue food coloring, one sheet of binder
paper per group, one thermometer per group
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Demonstration 1: Freshwater and Saltwater
1. Distribute two beakers to each group. In both beakers, pour room temperature
water. Dissolve sea salt and add blue food coloring to one of the beakers.
2. Have the students combine the contents of the two beakers and record their
observations on the binder paper.
3. Give the students 5 minutes to discuss and write down where this phenomenon
may occur - Sample Answer: Sea ice melting, rainfall, and river runoff all lead to
situations in which freshwater interacts with salt water.
Teaching Note: Between demonstrations, it is suggested to rinse the beakers of coloring.
Demonstration 2: Saltwater and Saltwater
1. Distribute two beakers to each group. In both beakers, pour room temperature
water. Dissolve sea salt in one and add blue food coloring. Dissolve Epsom salt in
the other and add red food coloring.
2. Have the students combine the contents of the two beakers and record their
observations on the binder paper.
3. Give the students 7 minutes to discuss and write down why this phenomenon
occurs and where this phenomenon may occur - Sample Answer: Epsom salt is
heavier than sea salt; thus, water with dissolved Epsom salt is denser and sinks to
the bottom. This may occur near underwater volcanoes that eject denser salts
and minerals into the ocean.
Demonstration 3: Warm Water and Cold Water
1. Distribute two beakers to each group. In one beaker, pour the cold water and dye
it blue. In the other beaker, pour the warm water and dye it red.
2. In the cold water beaker, have the students measure the temperature per
centimeter above the table. Plot this data in a table similar to the one below:
Centimeters from Bottom of Temperature of Water Layer
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Beaker
1 cm X degrees Celsius
2 cm Y degrees Celsius
... ...
3. Slowly add the warm water to the cold water beaker. Every centimeter of water
increase, remind the students to record the temperature and plot the data in the
data table on the binder paper.
4. When all the warm water has been added, record observations on the paper as
well as the water surface temperature.
5. Give the students ten minutes to plot the data from the table on a chart. The X-axis
should be Centimeters from Bottom of Beaker while the Y-axis is Temperature of
Water Layer. Afterwards, have the students circle the thermocline based on the
graph. If there is no visible thermocline, have students discuss and record 2
reasons why the experiment does not accurately represent what happens in the
oceans - Sample Answer: Ocean water masses are larger & this demonstration
does not account for salinity of water
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Lesson 3 Ocean Currents
Summary
1. Subject(s): thermohaline circulation, surface and coastal currents, and tides
2. Topic or Unit of Study: Oceanography
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about ocean currents, including thermohaline
circulation, surface currents, coastal currents, and tides
Key Skills: Students should be able to explain the differences between surface
and coastal currents, explain tides, and briefly explain thermohaline circulation.
5. Time Allotment: 2-3 hours
Powerpoint
https://docs.google.com/presentation/d/1mVMzADn93rJiExvX7VYOTMyiWS9K0fk4KBY7A5cTo4o
/edit?usp=sharing
Lecture Transcript Thermohaline Circulation (Slides 2,3,4)
Winds drive ocean currents in the upper 100 meters of the ocean’s surface. However, ocean
currents also flow thousands of meters below the surface. These deep-ocean currents are driven
by differences in the water’s density, which is controlled by temperature (thermo) and salinity
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(haline). This process is known as thermohaline circulation.
In the Earth's polar regions ocean water gets very cold, forming sea ice. As a consequence the
surrounding seawater gets saltier, because when sea ice forms, the salt is left behind. As the
seawater gets saltier, its density increases, and it starts to sink. Surface water is pulled in to
replace the sinking water, which in turn eventually becomes cold and salty enough to sink. This
initiates the deep-ocean currents driving the global conveyor belt.
Surface Currents (Slides 5,6,7)
The water at the ocean surface is moved primarily by winds that blow in certain patterns.
Surface ocean currents flow in a regular pattern, but they are not all the same. Some currents are
deep and narrow. Other currents are shallow and wide. Currents are often affected by the shape
of the ocean floor. Some move quickly while others move more slowly. A current can also change
somewhat in depth and speed over time. Surface currents form large circular systems called
gyres.
Surface ocean currents carry heat from place to place in the Earth system. This affects regional
climates. The Sun warms water at the equator more than it does at the high latitude polar regions.
The heat travels in surface currents to higher latitudes. A current that brings warmth into a high
latitude region will make that region’s climate less chilly.
Tides (Slides 8,9,10)
Tides are actually waves, the biggest waves on the planet, and they cause the sea to rise and fall
along the shore around the world. Tides exist thanks to the gravitational pull of the moon and the
sun, but vary depending on where the moon and sun are in relation to the ocean as the earth
rotates on its axis. The moon and sun’s pull cause two bulges or high tides in the ocean on
opposite sides of the earth. The moon, being so much closer, has more power to pull the tides
than the sun and therefore is the primary force creating the tides.
However, when the sun and moon reinforce each other’s gravitational pulls, they create
larger-than-normal tides called spring tides. The opposite of this—when the gravitational forces of
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the sun and moon pull from opposite sides of the earth and cancel each other out—is called a
neap tide and results in a smaller-than-usual tidal range.
Coastal Currents (Slide 11,12,13,14)
Along the coast, there are also different currents that operate on the smaller scale. There are
three types of coastal currents - upwelling, longshore currents, and rip currents.
Upwelling is probably the most important of all coastal currents. Upwelling is defined as the rising
of colder, deep water to the ocean surface. If you recall from previous lessons, isn’t colder water
denser, so why does it rise to the surface? This phenomenon happens because near coastlines,
winds are typically very strong. These strong winds blow on the ocean surface and actually push
the surface water away from the shore. Because the surface water has been displaced, there is
now a “gap” on the ocean surface. Thus, the deeper, colder water rises to fill the “gap”.
Upwelling is especially important since plankton and nutrients are more commonly found in
deeper, colder waters. This means that upwelling supports fish populations that survive on
plankton and, thus, human fishermen.
Longshore currents are powerful currents that run parallel to the shore. Because these currents
are so close to the shoreline, they transport large amounts of sand and other sediments and
deposit the load elsewhere. This transport is called longshore drift. Longshore drift is especially
bad for beachside buildings because over time, the ground under the building can actually be
eroded away too, causing the house to collapse. Where this sand is deposited, different features
form. A spit is a stretch of sand connected to the mainland that extends into the ocean. A barrier
or barrier island is a sand dune not connected to the mainland.
Rip currents are the most dangerous coastal current. Rip currents happen on beaches. If you’ve
ever gone to beach, when you watch the waves, do you ever see the water recede once it
contacts the sand. The water doesn’t remain on the beach forever - it flows backwards towards
the ocean again. On some beaches, this backwards flowing is extremely powerful, and that is
when a rip current forms. Many swimmers have died from being trapped in rip currents, so next
time, pay attention to any warnings. If you ever see foam or debris floating away from the beach
rapidly, it’s probably a rip current.
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Worksheets
Teacher’s Note: The purpose of this worksheet is to teach students the different types of
tides and how tidal patterns are factored into decisions that actually affect us.
Worksheet:
https://drive.google.com/file/d/0B8yQoHxsmWNxVnh2WTI2ODNDSmc/view?usp=sharing
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Lesson 4 Marine Life
Summary
1. Subject(s): Ocean layers and different ocean ecosystems
2. Topic or Unit of Study: Oceanography
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the different ocean layers and the ecosystems
associated with them.
Key Skills: Students should be able to explain the different layers of the ocean and
the various ocean ecosystems.
5. Time Allotment:
Powerpoint
https://docs.google.com/presentation/d/1sGRK60X-dmE9AWaoWOL162Gu_LZ3RIxAqpqQlnrgHR
Q/edit?usp=sharing
Lecture Transcript
Marine Life Overview
The oceans are a habitat teeming with life. Filled with millions of animals, plants, and other
organisms, marine ecosystems account for 50 to 80 percent of all life on Earth. Even though 1.5
million species have already been discovered, much of the ocean is still uncharted territory:
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scientists estimate there are still 2 to 50 million life forms left to find. From the shallowest tide
pools to the deepest trenches, you will always find something living.
This marine life is fragile, however. As you will see later on, these organisms are valuable to us,
but human activities such as overfishing and littering have put them under attack. It’s our
responsibility to make sure oceans remain beautiful and lively.
Ocean Life Building Blocks
Plankton form the building blocks of ocean habitats. Plankton are tiny, tiny organisms we can’t
see that float with ocean currents. They are important because they are a major food source for
ocean animals - everything from small shrimps and anemones to the largest whales feed on
plankton. From an ecological standpoint, plankton for the bottom of the food chain.
There are 2 types of plankton. Zooplankton are animal planktons - to survive, they feed on
smaller planktons. Phytoplankton are plant planktons - to survive, they convert energy from the
sunlight to their own food source.
Surprisingly, plankton enjoy cold water. You will find more plankton in the near freezing waters of
the Arctic than the tropical beaches of Hawaii. Plankton enjoy cold waters because they usually
have more nutrients. The abundance of plankton near the Arctic and Antarctic is what allows
marine life to thrive there.
Light and the Oceans
Not all regions of the ocean receive light. The deeper you go, the less sunlight reaches that
region of the ocean.
The upper 200 meters, about 650 feet, of ocean is called the euphotic zone, or - more easy to
remember - the sunlight zone. This zone has sunlight, so it is warmer and supports phytoplankton
(remember? phytoplankton need sunlight to produce their own food).
The middle zone, called the twilight or disphotic zone, receives very little sunlight and extends
from 660 feet to nearly 3000 feet. Here animals are adapted to darkness and high pressure. Fish
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have larger eyes, and some smaller organisms can glow in the dark. Some animals here include
zooplankton, octopi, krill, lobsters and crabs, eels, grey whales, sperm whales, squids, and some
large fish species.
The deepest zone, called the midnight or aphotic zone, is all regions of the ocean deeper than
3300 feet. The environment here is basically pitch black. Animals in this zone are the most
unique. First, at this zone, scientists refer to a phenomenon called a “rain of death” - essentially,
all organisms that die in the sunlight and twilight zones fall to the midnight zone. These carcasses
and dead plankton serve as the primary food sources for many organisms.
Another interesting thing to take note of is underwater volcanoes. Near mid-ocean ridges, there
are special underwater volcanoes called hydrothermal vents that eject different chemicals and
minerals from the Earth. Despite the extreme conditions, some organisms such as tube worms
and crabs actually survive here, relying on the chemicals ejected by the volcanoes to produce
food. Yes, even at the deepest depths and hottest temperatures, you will still discover life.
Habitat Focus: Coral Reefs
There are so many habitats in the ocean, but one key ecosystem everyone must understand is
coral reefs. Coral reefs can be found in tropical waters, and they are a home to 25% of all marine
species. Humans rely on reefs for fishing and tourism, and in places where storms are common,
coral reefs act as crucial wave breakers.
Contrary to common belief, corals are not plants. Corals are made out of individual units called
polyps. Polyps are small and look like upside-down jellyfish. Like jellyfish, polyps also have
stinging tentacles they use to catch floating plankton, and some glow in the dark. What gives
corals their beautiful colors is the algae. Algae called zooxanthellae actually live in the polyps;
these microscopic algae help produce extra food for the coral by converting sunlight to food,
while the polyp provides a home. This cooperation is called symbiotic mutualism, a relationship
where both the coral polyp and algae benefit. (The following slide of pictures depicts polyps and
a diagram of a polyp and algae. In the rightmost image, the orange-brown dots are actually
zooxanthellae living in the polyp)
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Reefs are huge structures. The Great Barrier Reef by Australia is the largest living structure in the
world at 1400 miles long. Reefs take millions of years to grow because coral grow so slow. Hard
corals form the backbone of the reef. Hard corals are special because their polyps secrete
calcium carbonate, a very hard mineral. Over time, the calcium carbonate accumulates, giving
more space for polyps to grow.
Because coral reefs grow so slowly, they are considered very fragile ecosystems. Any changes in
the environment can kill the coral. When the water becomes too warm or too cold, the
zooxanthellae actually escape the polyp; this causes the polyp to lose color in an event called
bleaching and eventually starve to death. If there is pollution in the water, this not only poisons
the polyp, but it can block sunlight and prevent the algae from making food. Finally, powerful
storms can completely destroy reefs if waves are powerful enough. The greatest threat to coral
reefs today is humans. Our littering, pollution, fishing practices, and contributions to climate
change harm reefs. For instance, in some countries, fishermen use dynamite to blow up entire
reefs to catch dead fish. Right here in the US, irresponsible boaters drag their boats through
reefs, destroying hard corals If we do not change our ways, more than 90% of our coral reefs will
die by 2050.
Activity
Ecosystem Modeling
Teaching Note: The purpose of this activity is to ensure students conceptually and visually
understand the diversity of marine ecosystems.
Materials: plain clay, cardboard, construction paper, toothpicks, paint, Internet access,
glue, tape
1. Distribute clay, construction paper, toothpicks, glue, tape, cardboard, and paint to
each group. Assign each group one of the following marine ecosystems: kelp
forests, tide pools, coral reefs, seagrass beds, hydrothermal vents, and deep sea
reefs.
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2. With the materials and online research, students should recreate a model of the
ecosystem they have been assigned.
3. After the models have set, have each group present the following information
about their specific ecosystem: location, 4 unique organisms, importance to
humans, how it relates to another group’s ecosystem, and 1 fun fact.
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Lesson 5 Humans & The Oceans
Summary
1. Subject(s): Human activities and their impacts on the oceans.
2. Topic or Unit of Study: Oceanography
3. Grade/Level: 4-6 grades
4. Objective: Students will learn about the different ocean layers and the ecosystems
associated with them.
Key Skills: Students should be able to explain the different layers of the ocean and
the various ocean ecosystems.
5. Time Allotment:
Powerpoint
https://docs.google.com/presentation/d/1hC5x3GuzOfO9N11Cju04-m9wUK8lNVD4BmP_24Bb_Y
M/edit?usp=sharing
Lecture Transcript
Global Warming & Climate Change (Slide 2,3)
By now, most of us know global warming and climate change are two immense problems we
have to face. But before we can think of solutions, we must first understand how global warming
and climate change works in the first place.
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99% of scientists agree that humans are responsible for the impending climate disaster. But what
is it that we do that has such large impacts? There are three main fossil fuels that humans depend
on - coal, natural gas, and oil. Almost every part of our lives involves burning these fuels. When
we drive, our cars burn gasoline, which comes from oil. When we turn on the lights, the nearest
power plant is probably burning coal to generate power. When we cook or heat our homes, our
stoves and heaters burn natural gas. All this burning has severe consequences as greenhouse
gases are released into the air. Greenhouse gases include carbon dioxide (CO2), methane, and
sulfur dioxide. These greenhouse gases are invisible, and when they reach our atmosphere, they
form a blanket around the Earth that traps in heat from the Sun. Usually, the heat the Earth
receives from the Sun is reflected back into space, but with this layer of greenhouse gases in our
atmosphere, heat is reflected back onto the Earth’s surface and is trapped for a long time. This
trapped heat is what’s responsible for the phenomenon we call global warming.
Global Temperature Trend (Slide 4)
Global warming has been observed since the early 1900s. The 1800s and 1900s were when
humans first started burning massive amounts of fossil fuels. If you look at the graph from NASA,
you can see that global average temperatures have been on a rise since then.
Direct Ecological Impacts (Slide 5)
This increase in temperatures has direct impacts on the ocean’s ecosystems. First, because
water temperatures are dramatically warming with the atmosphere’s temperatures, many fish
species can no longer bear living in their original environments. This has caused them to move
northward or southward towards the poles in search of cooler environments. In their new
environments, these fish disrupt the balance of Arctic and Antarctic marine ecosystems by
outcompeting the species that originally lived there. If you look at the diagram at the left, you can
clearly see how Arctic fishes’ habitats, the regions outlined in purple, have shrunk over the past
thirty years while the habitats of temperate fish, the regions outlined in orange and red, have
expanded. Fish migrations have also threatened fishermen. These days, fishermen have to travel
farther and farther just to get a catch.
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Another direct ecological impact is the death of coral. From the previous lesson on marine
ecosystems, we know that coral reefs are extremely fragile ecosystems, and that even small
ocean temperature increases can kill coral. That’s exactly what’s happening right now in many
parts of the world - coral and the species that depend on them are dying due to rising
temperatures. Even the Great Barrier Reef, the largest coral reef in the world, has suffered greatly
from unusually warm waters.
Sea Level Rise (Slide 6)
One serious long term impact of global warming is sea level rise. Most of us already know that
sea level rise is partially caused by the melting of land ice. As glaciers and ice caps in the Arctic,
Antarctic, and Greenland continue to fragment and melt, this meltwater is entering the ocean and
causing sea levels to increase. Greenland’s melting ice is one of the greatest concerns for
scientists. If all of Greenland’s ice melted, sea levels would increase by 22 feet - that’s the height
of a two story building. Right now, Greenland’s melting contributes to a 1 millimeter increase in
sea levels every year, but if temperatures continue to warm, this rate will only increase. The
second cause behind sea level rise is thermal expansion. When water is warmer, it actually takes
up more volume. That means, that as the oceans have been getting warmer and warmer, they
have also been getting larger and larger.
There are several impacts to sea level rise. Right now, NASA reports that by 2100, sea levels may
rise by 11 to 78 inches, depending on whether or not we change our greenhouse gas emissions.
Higher sea levels means bigger storm surges during hurricanes and typhoons that can wipe out
entire towns and cities. In fact, up to 650 million people globally are at risk for increased flooding
due to sea level rise. If all these people are forced to move due to natural disasters and become
climate refugees, that would be a huge humanitarian crisis.
Ocean Acidification - Diagram (Slide 7)
Often overlooked, ocean acidification is another serious threat to our ocean’s health. Not directly
caused by higher temperatures, ocean acidification is actually a result of greater CO2 levels in
the air. Before we jump into why this is serious, let’s get a brief overview of how our oceans are
growing more and more acidic. When the oceans absorb CO2 from the air, the carbon dioxide
reacts with water molecules and carbonate ions to form bicarbonate ions. This process is
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detrimental since it decreases the pH of the oceans - the lower the pH, the more acidic the
oceans are.
Ocean Acidification - Impacts (Slide 8)
Let’s take some time to imagine why ocean acidification is problematic. Imagine putting a tooth in
soda - soda is acidic by the way. If you wait several weeks, you’ll see the tooth will be completely
dissolved. The bottom line is acidic solutions with lower pH values break down things like bones
and skeleton, especially if they contain calcium (an element that is used to build calciums and we
obtain it from milk). As we’ve touched upon before when we discussed sediments and coral
reefs, hundreds of marine organisms rely on calcium carbonate, a compound containing calcium,
to build their shells and internal skeletons. Because oceans are becoming more and more acidic,
these organisms’ shells and skeletons are literally slowly dissolving. If you take a look at the
image on the left, you can see the effects of ocean acidification very clearly. In the 2005
snapshot, the coral are thriving. In the 2010 snapshot, the corals don’t even exist anymore;
there’s barely a trace of them since their skeletons have all dissolved away.
Activity
Solutions Debate
Teaching Note: The purpose of this activity is for students to better understand how
human needs and activities often conflict with the health of our oceans. Through debates,
students should have a sharper grasp of how important oceans are to our survival.
1. Give each group a sheet of paper, and ten minutes per debate to discuss/research
solutions and arguments. Refer to the following prompts for guidance, and assign
sides to make the debate even more challenging!
a. In many poorer coastal communities, fishermen depend on fishing from
coral reefs to survive. However, these fishing practices are often
destructive - some fishermen overfish while others use dynamite to kill
hundreds of organisms at the same time. Should governments respond to
this issue? How should governments approach this issue?
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b. Today, much of our understanding of ocean currents comes from an
accident that happened many years ago. After a shipment of rubber ducks
fell into the ocean, scientists were able to track the floating plastic ducks to
see where the surface currents took them. Should more of these
investigations be carried out, even if they involve polluting the oceans?
c. Tidal energy and offshore wind farms are two rapidly developing
renewable energy sources. One downside to these sources is that they
often damage local ecosystems. Assign one group to defend the
construction of these structures and assign the other group to defend the
prohibition of these structures.
d. The Earth currently has a freshwater crisis - many countries are running out
of water. Some coastal nations have turned to constructing desalination
plants. Desalination plants are essentially buildings that convert seawater
to freshwater by filtering the salt and dumping it back into the ocean. This
salt destroys surrounding organisms and affects ocean circulation patterns.
What should be done about this conflict?
2. While each pair of groups debates, remind students to take notes. At the end of
each debate, ask the class for their input on the situation.
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