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Chapter 55: Ecosystems and Energy

Chapter 55: Ecosystems and Energy - ahschools.us fileChapter 55: Ecosystems and Energy. Ecosystems Ecosystem = sum of all the organisms living within its boundaries (biotic community)

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Chapter 55: Ecosystems and Energy

Ecosystems

Ecosystem = sum of all the organisms living

within its boundaries (biotic community) + abiotic

factors with which they interact

Involves two unique processes:

1. Energy flow

2. Chemical cycling

Overview of energy & nutrient dynamics

Energy Flow in an Ecosystem

• Energy cannot be recycled must be constantly

supplied to an ecosystem (mostly by SUN)

• The autotrophs (“self feeders”) are the primary

producers, and are usually photosynthetic (plants

or algae).

▫ They use light energy to synthesize sugars and other

organic compounds.

• Heterotrophs (“other feeders”) – can’t make own

food

• Heterotrophs are

at trophic levels

above the primary

producers and

depend on their

photosynthetic

output.

▫ Herbivores that eat primary producers are

called primary consumers.

▫ Carnivores that eat herbivores are called

secondary consumers.

▫ Carnivores that eat secondary consumers are

called tertiary consumers.

▫ Another important group of heterotrophs is the

detritivores, or decomposers.

They get energy from detritus, nonliving

organic material, and play an important role

in material cycling.

Main decomposers:

fungi & prokaryotes

Primary Production

• Primary production = amt. of light energy that

is converted to chemical energy

• Gross primary production (GPP): total primary

production in an ecosystem

• Net primary production (NPP) = gross primary

production minus the energy used by the

primary producers for respiration (R):

▫ NPP = GPP – R

• NPP = storage of chemical energy available to

consumers in an ecosystem

Open ocean

Continental shelf

Upwelling zones

Extreme desert, rock, sand, ice

Swamp and marsh

Lake and stream

Desert and semidesert scrub

Tropical rain forest

Temperate deciduous forest

Temperate evergreen forest

Tropical seasonal forest

Savanna

Cultivated land

Estuary

Algal beds and reefs

Boreal forest (taiga)

Temperate grassland

Woodland and shrubland

Tundra

0.4

0.4

1.0

1.3

1.5

1.6

1.7

1.8

2.4

2.7

2.9

3.3

3.5

4.7

0.3

0.1

0.1

5.2

65.0

Freshwater (on continents)

Terrestrial

Marine

Key Percentage of Earth’ssurface area

Average net primary

production (g/m2/yr)

6050403020100 2,5002,0001,5001,0005000

Percentage of Earth’s net

primary production

2520151050

125

2,500

360

1,500

500

3.0

90

900

600

800

2,200

600

250

1,600

1,200

1,300

2,000

700

140

0.3

7.9

9.1

9.6

5.4

3.5

0.6

7.1

4.9

3.8

2.3

24.4

5.6

1.2

0.9

0.1

0.04

0.9

22

Net primary production of different ecosystems

Primary production factors in:

•Aquatic ecosystems:

▫ Light availability (↑ depth, ↓ photosynthesis)

▫ Nutrient availability (N, P in marine env.)

•Terrestrial ecosystems:

▫ Temperature & moisture

•A nutrient-rich lake that supports algae growth is

eutrophic.

Energy transfer between trophic levels is

typically only 10% efficient

• Production efficiency:

only fraction of E stored

in food

• Energy used in

respiration is lost as heat

• Energy flows (not cycle!)

within ecosystems

Pyramid of Energy:

10% transfer of

energy from one

level to next

Ecological pyramids give insight to food chains

Pyramid of Numbers

Pyramid of Biomass

• Loss of energy limits #

of top-level carnivores

• Most food webs only

have 4 or 5 trophic

levels

Trophic level

Secondary

consumers

Primary

consumers

Primary

producers

The dynamics of energy through ecosystems have

important implications for the human population

Matter Cycles in Ecosystem

• Biogeochemical cycles: nutrient cycles that

contain both biotic and abiotic components

• organic inorganic parts of an ecosystem

• Nutrient Cycles: water, carbon, nitrogen,

phosphorus

Water Cycle

Water Cycle

1. Evaporation – liquid water becomes a gas

▫ Transpiration – evaporating off plants

2. Condensation – water changing from gas to liquid

3. Precipitation – water falling to Earth from

atmosphere

4. Run-off – water running over the land

▫ collect in the oceans, lakes or rivers

5. Infiltration – water seeping into the ground

– Ground Water- stored in underground caverns

and porous rock

– Provides water for the soil, streams, rivers, and

oceans

Watersheds

• The area of land that contributes water to a river system is called a watershed.

Aquifers

• Aquifer – Layer of permeable rock or sediment.

• “recharged” by precipitation filtering into permeable soils

• Water Table – Boundary at the top of the groundwater zone.

Human impacts on water cycle

• Removing forests and vegetation – increases runoff and erosion, reduces transpiration and lowers water tables

• Damming rivers increases evaporation and infiltration

• Emitting pollutants = acid precipitation

• Most threatening : overdrawing groundwater▫ Agriculture, watering, etc.

Lake Mead

White Bear Lake

http://www.wblcd.org/wl/images/articles/PDF/Million_dollar_question_meansWBP102616.pdf

http://www.wblcd.org/wl/images/articles/PDF/TheupsanddownsofWBL_ST052216.pdf

Carbon Cycle

• CO2 removed by

photosynthesis,

added by burning

fossil fuels

Ways carbon moves

• Photosynthesis – moves from environment to plants

• Respiration- moves from living things back to the environment

• Decomposition/Decay- moving from dead organisms back to the environment

• Combustion- Burning releases carbon back into the atmosphere

Carbon in the

Atmosphere

• Greenhouse effect

▫ Trapping of heat by molecules (water, methane,

CO2,)

Human Impact

• Fossil fuels

▫ Releases stores of carbon

• Deforestation and Habitat Destruction

▫ Fewer plants mean less CO2 removed from

atmosphere

• Methane release

▫ Agriculture and animal, wetlands, leakages during

natural gas extraction, transportation, use

Humans affect the carbon cycle

• Today’s atmospheric carbon dioxide reservoir is the largest in the past 800,000 years

Photo from IPCC

The Keeling Curve

Effects of Climate ChangeEcosystem change

• Ranges being shifted

▫ Some butterflies, foxes, and alpine plants have

moved farther north or to higher, cooler areas

• Flowering earlier

• Loss of species▫ Polar Bears, penguins, golden toad

• Climate Change: marine ecosystems

Glaciers are melting

Why artic sea ice matters

1. It reflects sunlight

2. It influences ocean and air currents

3. Keeps methane locked away

4. It limits severe weather

5. It supports native people and wildlife

IPCC (2007)

Other Effects

• Sea Level Rise

▫ Melting of ice sheets

▫ Expansion of heated (warm) sea water

▫ Flooding of coastal communities

• Spread of diseases

• Increase of extreme weather events

• Precipitation has increased across the globe, on

averagehttp://news.nationalgeographic.com/2015/12/151229-before-after-earth-features/

Nitrogen Cycle• Nitrogen fixation:

▫ N2 plants by bacteria

• Nitrification:

▫ ammonium nitrite

nitrate

▫ Absorbed by plants

• Denitrification:

▫ Release N to atmosphere

Nitrogen Cycle• Nitrogen is used for proteins, DNA

• Nitrogen is found in atmosphere and is unusable

▫ Converted to a useable form through nitrogen

fixation

Special organisms/bacteria that convert

legumes

Lightning

▫ Animals get nitrogen from eating plants

• Returned to soil when animals urinates/dies

▫ Denitrification – nitrogen is converted back to gas

Humans affect the nitrogen cycle

• Fertilizers and animal waste

• Excess Nitrogen can cause Eutrophication

▫ causes aquatic life to die due to low levels of oxygen

Decreasing Nitrogen Pollution

• Decrease fertilizer use

• Using new farming methods

• MN Buffer law

• Maintaining wetlands

Phosphorus Cycle

https://www.youtube.com/watch?v=2D7hZpIYlCA