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Oct 19, 2006Astronomy 230 Fall 2006
Astronomy 230This class (Lecture 16):
Biological EvolutionBiological Evolution
Vlad Nicolaescu
Brandon Roel
Jake Szczepaniak
Next Class:
Biological EvolutionBiological Evolution
Tom Patterson
Tim Ferencak
Jeffery Lipsey
Oct 26:
Fred Knecht:
William Kormos
Adam Molski: Music: Spaceboy – Smashing Pumpkins
Oct 19, 2006Astronomy 230 Fall 2006
HW #3
• Jeff Ungrund:http://www.unsolvedmysteries.com/usm95137.html
• Joel Bonasera:http://www.anomalies-unlimited.com/WTC_UFO.html
• Natalya Sholomyansky:http://www.msss.com/http/ps/life/life.html
Oct 19, 2006Astronomy 230 Fall 2006
Presentations
• Vlad Nicolaescu: Extreme Life
• Brandon Roel:
Alien Probes: Monoliths in Hiding
• Jake Szczepaniak:
UFO Conspiracy Theories
Oct 19, 2006Astronomy 230 Fall 2006
Outline
• Life in our Solar System?
– Saturn (Titan)
• Two types of cell life: Eukaryotes and Prokaryotes.
• All life can be divided into 3 types:
– Bacteria
– Archaea
– Eukarya
Oct 19, 2006Astronomy 230 Fall 2006
Earth – Saturn comparison
Equatorial radius 9.45 Earth
Cloud-top gravity 1.07 Earth
Mass 95.2 Earth
Distance from Sun 9.53 AU
Year 29.5 Earth years
Solar day (equator) 10 hours 14 minutes
It floats. The least
spherical planet.
Oct 19, 2006Astronomy 230 Fall 2006
Saturn’s Atmosphere
• Composition similar to Jupiter
– Mostly hydrogen and helium
• Atmosphere more “spread out”
– Less gravity
– Contrast of cloud bands reduced
• Wind speeds fastest at the equator
– 1000 km per hour!
Oct 19, 2006Astronomy 230 Fall 2006
Driving Saturn’s Weather
• As on Jupiter, Saturn’s internal heat drives weather
– Saturn radiates 80% more heat than it receives from the Sun
– Like Jupiter, Saturn is still contracting!
– As is contracts, heat is produced
• As on Jupiter, storms are produced between cloud bands
– No long lasting storm like the Great Red Spot
Oct 19, 2006Astronomy 230 Fall 2006
Saturn’s Interior
• Similar structure to
Jupiter’s
– But Saturn is less massive
– The interior is less
compressed
• Liquid metallic hydrogen
creates a magnetic field
– 30% weaker than Earth’s
Oct 19, 2006Astronomy 230 Fall 2006
Saturn’s Rings
• Two main rings
– Several fainter rings
– Each ring is divided
into ringlets
• The rings are thin
– Only a few tens of
meters thick– razor thin!
Oct 19, 2006Astronomy 230 Fall 2006
Makeup of the Rings
• The rings of Saturn
are not solid rings
– Made of icy rocks
– 1cm to 10m across
• New Cassini data shows
ring particle size varies
with distance from Saturn
– Note the gap is filled with
small particles
Oct 19, 2006Astronomy 230 Fall 2006
Saturn’s Moons
• Saturn has a large number of moons– At least 30
• Only Titan is comparable to Jupiter’s Galilean moons
• Smaller moons are mostly ice, some rock
Oct 19, 2006Astronomy 230 Fall 2006
Saturn’s Odd
Moons• Mimas - Crater two-thirds its
own radius
• Enceladus - Fresh ice surface, water volcanoes?
• Hyperion –Irregularly shaped
• Iapetus - Half its surface is 10x darker than the other half
• Phoebe - Orbits Saturn backwards
Mimas
PhoebeHyperion
Oct 19, 2006Astronomy 230 Fall 2006
Titan
Titan’s atmosphere
• Saturn’s largest moon– bigger than Mercury.
• 2nd largest moon in the solar system after
Ganymede.
• Discovered in 1655 by Christiaan Huygens
• Only moon to have a dense atmosphere
– Dense nitrogen/methane atmosphere
– Small greenhouse effect
– 85% nitrogen
– Much like ancient Earth!
Oct 19, 2006Astronomy 230 Fall 2006
Titan
Titan’s atmosphere
• Atmospheric pressure is 1.5 times Earth’s
• Liquid/ice hydrocarbons?
• Organic compounds – life?
• Probably not – too cold: 95 K
• May be a “deep freeze” of the chemical
composition of ancient Earth
Oct 19, 2006Astronomy 230 Fall 2006
Piercing the Smog
• Cassini has special infrared
cameras to see through Titan’s
smog
• Green areas are water ice
• Yellow-orange areas are
hydrocarbon ice
• White area is a methane cloud
over the south pole
Oct 19, 2006Astronomy 230 Fall 2006
Huygens Probe
descent to Titan
Jan 14, 2005
Arrival at Saturn
July 1, 2004
Cassini-Huygens
Oct 19, 2006Astronomy 230 Fall 2006
Mapping Titan
Oct 19, 2006Astronomy 230 Fall 2006
Mapping Titan
Oct 19, 2006Astronomy 230 Fall 2006
Mapping Titan
http://esamultimedia.esa.int/multimedia/esc/esaspacecast001.mp4
Oct 19, 2006Astronomy 230 Fall 2006
Titan• N2 came from ammonia (NH3) – common in outer solar system
• Second most abundant component is methane (natural gas)
- One option is UV + methane � hydrocarbons (e.g., ethane)
- Then, ethane condenses and rains down on Titan’s surface
• So, it might have liquid ethane or methane lakes/oceans?
• Many organic compounds should be in atmosphere– reducing
atmosphere.
• If life exists here, then it will change our water–chauvinistic ideas.
Oct 19, 2006Astronomy 230 Fall 2006
A Possible Past
• The probe floating in the ethane sea of Titan (didn’t happen)
• Mountains in the distance (weren’t there).
http://saturn.jpl.nasa.gov/cgibin/gs2.cgi?path=../multimedia/images/artwork/images/ Oct 19, 2006Astronomy 230 Fall 2006
Conclusion
• No conclusive evidence exists for life in our solar system
besides on Earth
• But, possibilities exist for life
– Venus’s clouds may have migrated life.
– Mars may have some microbial history linked to water, and
perhaps some subsurface life.
– Jupiter’s reducing atmosphere may harbor sinkers.
– Europa’s sub-crustal oceans may harbor life, even fish-like life.
– Titan is still very interesting
• Thick atmosphere
• Reducing chemistry
Oct 19, 2006Astronomy 230 Fall 2006
No Intelligent Life
• We might find evidence of some sort of life in the
next decade, but very unlikely to find complexity
needed for intelligent and communicative life.
• Apparently in our system, Earth’s conditions are
necessary.
• Other planets may have microbial forms of life,
and maybe complex fish-like organisms, but we
don’t expect communicative beings.
Oct 19, 2006Astronomy 230 Fall 2006
How to search for life?
• How do we search for life in our Solar System and beyond?
• What test will indicate life exclusively?
• Remember the Viking problems on Mars.– Need flexibility to test interpretations.
• But, it is difficult to anticipate fully the planet conditions.
Oct 19, 2006Astronomy 230 Fall 2006
How to search for life?
• Is is apparent that future missions need to land as near as possible to sites of subsurface water or other solvents.
• On Titan, what are the important tests for determining biological signatures of non-water life?
• What if the life is still in the protolife stage? Can we detect that?
• The boundary between chemical and biological processes is difficult to distinguish.
Oct 19, 2006Astronomy 230 Fall 2006
Decision Trees– Search for Life
• Wait for it to come to us via meteorites or comets.
• Robotic one-way investigations– Mars rovers.
• Fetch and return with samples.
http://www.ibibli
o.org/wm/paint/a
uth/friedrich/tree
.jpg
Oct 19, 2006Astronomy 230 Fall 2006
Problems
• In the last 2 cases, we have the
problem of contamination by
Earth life.
• Organisms can live in Mars-like
conditions on Earth.
• If some Earth life survives the
space journey, it could colonize
Mars, possibly destroy any
Martian life. Think of Kudzu.
• Current missions must be
sterilized.http://www.hope.edu/academic/biology/faculty
/evans/images/Angiosperms/CoreEudicots/Eur
osidsI/Fabaceae/Kudzu.JPG
Oct 19, 2006Astronomy 230 Fall 2006
Biomarkers: How to look for extrasolar life.
• We need to decide how to search
for biomarkers or chemical
signatures of life.
• On Earth, methane and oxygen
are indicators. They normally
react. Something is keeping it
out of equilibrium. Sort of like
Venus disequilibrium.
• The Galileo spacecraft on its way
out to Jupiter, turned and looked
at the Earth.
• Did it detect life?
Oct 19, 2006Astronomy 230 Fall 2006
Biomarkers: Looking at Earth.
• Strong “red edge” from reflected light. Absorption from photosynthesis.
• Strong O2. Keeping oxygen rich atmosphere requires some process. It should slowly combine with rocks.
• Strong methane. Should oxidize. Replenished by life.
• Strange radio emissions that could be intelligent life.
• Recently, researchers have looked at the Earthshine from the moon.
• They agree with Galileo result. There is life on Earth. – Water
– Oxygen
– Tentative detection of “red edge”
http://epod.usra.edu/archive/epodviewer.php3?oid=56256
Oct 19, 2006Astronomy 230 Fall 2006
# of
advanced
civilizations
we can
contact in
our Galaxy
today
Drake Equation
N = R* × fp × ne × fl × fi × fc × LStar
formation
rate
Fraction
of stars
with
planets
# of
Earthlike
planets
per
system
Fraction
on which
life arises
Fraction
that evolve
intelligence
Fraction
that
commun-
icate
Lifetime of
advanced
civilizations
Frank
Drake
15
stars/
yr
0.5
systems/
star
2.7 x 0.134
= 0.36
planets/
system
0.095
life/
planet
intel./
life
comm./
intel.
yrs/
comm.
That’s 2.6 life-arising systems/decade
Oct 19, 2006Astronomy 230 Fall 2006
Evolution of Intelligence
• First, we will examine the diversity of life; the fossil record shows a huge diversity with time.
• Organisms range from bacteria to humans.
• 1.8 x 106 known species– Insects account for most (1.0 x 106)
– Estimated that only 10% are known.
– Bacteria are hard to classify– only 4000 species so far.
• Remember that all of these organisms use nearly identical genetic codes, so life descended from a common ancestor.
• Primary challenge of biology is to explain how life from a single type of organism, diversified so much.
• Evolution is the primary concept.
Oct 19, 2006Astronomy 230 Fall 2006
Life
If we took all the biomass of all the animals, and all
the biomass of all the viruses, bacteria, protozoa, and
fungi– who weighs more?
Around 90% of all biomass on the Earth is in the
smallest and simplest lifeforms.
Oct 19, 2006Astronomy 230 Fall 2006
Classification of Life
1. Prokaryotes – No cell nucleus– DNA floating
around
– Always single-cell creatures like bacterium
– Came first
– Outnumber and outweigh the second class (eukaryotes)
Oct 19, 2006Astronomy 230 Fall 2006
Classification of Life
2. Eukaryotes– Have a cell nucleus, a membrane
to protect the DNA
– Basis of all multi-cell creatures
– Also some single-cell creatures like amoebas.
– DNA arranged into chromosomes in nucleus– 23 pairs for humans.
Oct 19, 2006Astronomy 230 Fall 2006
Prokaryotes
Divided into 2 domains:
1. Eubacteria or “true” bacteria
2. Archaea
– Thought to be oldest life forms.
– Often found in harsh environments:
hot springs, undersea vents, salty
seashores, etc, which were probably
more common on the early Earth.
– Some live deep underground, and
may represent a significant fraction
of the Earth’s biomass.
– Some evidence that ancient
organisms were heat-lovers (maybe)
Oct 19, 2006Astronomy 230 Fall 2006
Eukaryotes
• All animals, plants, and
fungi.
Oct 19, 2006Astronomy 230 Fall 2006
3 Domains of Life
• Genetically speaking,
Archaea and Eukarya
are more similar to one
another than are
Bacteria and Archaea
• Implies that Archaea
and Bacteria split and
then all Eukarya split
from Archaea
• A major implication for
the evolution of life on
Earth
The old “kingdom”
classification is no longer really
used, such as plant kingdom or
animal kingdom
Oct 19, 2006Astronomy 230 Fall 2006
Genetic Relations• This is a major change from the old
methods of assigning groups based on
outward form and anatomy.
• Instead based on studies of the genetic
code.
• Surprise: Human and chimpanzees
share about 99% of the same DNA, and
about 97% with mice.
• Surprise: 2 species of fruit fly look very
much alike, but only share about 25%.
Some of this differences is due to junk
DNA.
http://www.uglybug.org/index00.shtml
http://www.pritchettcartoons.com/fruitfly.htm
Oct 19, 2006Astronomy 230 Fall 2006
Changes?
• Today’s view: evolution is the most important and
unifying property of life.
• Anaximander (c. 610−547 BC): life arose in water and
gradually became more complex
• Empedocles (c. 492−432 BC): survival of the fittest (but,
“a good idea stated within an insufficient theoretical frame
loses its explanatory power and is forgotten” by Hans
Reichenbach )
• Aristotle (384−322 BC): species are fixed and independent
of each other → evolution discarded for 2000 years
• Fossil record: slowly broke down the Aristotelian theory
Oct 19, 2006Astronomy 230 Fall 2006
For the Species Survival
• Darwin (1809−1882) & Malthus(1766-1834):
– Populations can grow faster than food sources can support them.
– Creates a struggle for survival that can wipe out competitors.
– Individual variations has advantages or disadvantages in the struggle for survival
– Natural selection can create unequal reproductive success
Oct 19, 2006Astronomy 230 Fall 2006
Filling the Niche with Finch
• Other Evidence:– Adapted species in
the GalápagosIslands, in particular finches
– Artificial breeding of house/farm animals and vegetables
• DNA is really the mechanism of natural selection, but evolution requires both heredity and environment
Oct 19, 2006Astronomy 230 Fall 2006
Mutant Sex
• Mutations from changes in the bases of DNA.
• Usually copying errors, but also radiation–
radioactivity, cosmic rays, chemical agents, or UV
light.
• About 3 mutations per person per generation.
• Most mutations are neutral, changes in the junk
DNA.
• Why is sex important to this class?
http://www.mutantx.net/features/press_vw_sexy.html
Oct 19, 2006Astronomy 230 Fall 2006
Mutant Sex
• Sexual reproduction leads to greater genetic diversity– a difference between prokaryotes and eukaryotes?
• Asexual reproduction does not allow 2 new and beneficial mutations to combine.
• Blackberries have not changed much in 10 millions years, but sexual plants have produced: raspberries, thimbleberries, cloudberries, dewberries, etc.
• Sex is useful in the process, but the mutations are still key.
http://www.alcasoft.com/arkansas/blackberry.html
Oct 19, 2006Astronomy 230 Fall 2006
Does it take a long time?
Cabbage, kale, kohlrabi, brussels sprouts, cauliflower and broccoli have same common ancestor– wild mustard. All bred by humans on a very short time scale.
Or domestic lap dogs from
wolves in about 5000 years.
This is
selective
breeding, but
still the
potential is in
the DNA.