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Biogeochemical Cycles Leyda
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Biogeochemical Cycles

Feb 24, 2016

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Biogeochemical Cycles. Leyda. Biogeochemical Cycles. Over 95% of the body is made of these elements: S P O N C H : Sulfur, Phosphorus, Oxygen, Nitrogen, Carbon, Hydrogen An ecosystem needs two things: A flow of Energy (goes one way through trophic levels and is lost along the way) - PowerPoint PPT Presentation
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Page 1: Biogeochemical Cycles

Biogeochemical CyclesLeyda

Page 2: Biogeochemical Cycles

Biogeochemical Cycles• Over 95% of the body is made of these elements:S P O N C H : Sulfur, Phosphorus, Oxygen, Nitrogen, Carbon, Hydrogen• An ecosystem needs two things:• A flow of Energy (goes one way through trophic levels and

is lost along the way)• Cycle of materials

Page 3: Biogeochemical Cycles

Water Cycle• Water = H2O• Cycles Hydrogen and Oxygen through the

biosphere• Water makes up to 70% of the mass of our bodies• Water is an important solvent for cell processes

Page 4: Biogeochemical Cycles

Water Cycle

Page 5: Biogeochemical Cycles

Water Cycle1. Precipitation: water falls to the Earth as rain, snow or ice

Page 6: Biogeochemical Cycles

Water Cycle2. Runoff: Water moves along the Earth’s surface into rivers, lakes, or streams

Page 7: Biogeochemical Cycles

Water Cycle3. Seepage: Water soaks through the soil and collects in pools underground.

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• Can be gradual or sudden

Page 9: Biogeochemical Cycles
Page 10: Biogeochemical Cycles

Sinkhole – Guatemala May 2010• After hurricane – 60 meters deep• http://www.youtube.com/watch?v=BoOHmdL2I9Y

Page 11: Biogeochemical Cycles

Water Cycle4. Evaporation: Water changes from a liquid to a gas (usually occurs at the surface of lakes and oceans)

Page 12: Biogeochemical Cycles

Water Cycle5. Transpiration: Water evaporates from the leaves of plants (the most evaporative)

Page 13: Biogeochemical Cycles

Water Cycle6. Condensation: Water changes from gas to liquid (occurs when warm, moist air rises and cools in the upper atmosphere)

Page 14: Biogeochemical Cycles

Carbon Cycle

Page 15: Biogeochemical Cycles

Carbon Cycle• Carbon is the main ingredient in all living things• Carbon makes up the 4 macromolecules of life:• Carbohydrates• Lipids• Proteins• Nucleic Acids

Page 16: Biogeochemical Cycles

Carbon Cycle1. Photosynthesis: Plants take in CO2 from the atmosphere and use it to make food.

Page 17: Biogeochemical Cycles

Carbon Cycle2. Feeding: Animals obtain carbon by eating plants.

Page 18: Biogeochemical Cycles

Carbon Cycle3. Respiration: Animals breathe out CO2 when they burn food to get energy.

Page 19: Biogeochemical Cycles

Carbon Cycle4. Deposition: When organisms decay, carbon is

trapped in sediments underground that eventually form rocks or fossil fuels.

Page 20: Biogeochemical Cycles

Carbon Cycle5. Human Activity: Burning fossil fuels in factories

and cars releases CO2 into the atmosphere.

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Carbon Cycle6. Decomposition: Energy-rich, carbon-based

compounds formed from the decaying bodies of buried organisms.

Page 22: Biogeochemical Cycles

Carbon Cycle – In the Ocean7. Photosynthesis: Phytoplankton are Producers

in the Ocean 8. Feeding: Phytoplankton (Producers) are eaten

by consumers.9. Respiration: CO2 is released when organisms

burn food.

Page 23: Biogeochemical Cycles

Carbon Cycle10. Erosion: Rocks break down, releasing carbon

into the soil or ocean where it can be used by organisms.

Page 24: Biogeochemical Cycles

Carbon Cycle11. Volcanic Activity: CO2 released into the

atmosphere

Page 25: Biogeochemical Cycles

Nitrogen Cycle

Page 26: Biogeochemical Cycles

Nitrogen Cycle• Nitrogen is important for making proteins and

DNA• Nitrogen makes up ¾ of our atmosphere• N2 (Nitrogen gas) cannot be used by living things until it

is changed into Nitrates, Nitrites, or Ammonia

Page 27: Biogeochemical Cycles

Nitrogen Cycle1. Fertilizers: Humans add usable nitrogen

directly to soil.

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Nitrogen Cycle2. Nitrogen Fixation: Bacteria in the roots of

plants change nitrogen gas (N2) into ammonia (NH3) so that plants can use it.

Page 29: Biogeochemical Cycles

Nitrogen Cycle3. Lightning: Changes nitrogen gas into nitrate

and nitrite.

Page 30: Biogeochemical Cycles

Nitrogen Cycle4. Uptake: Producers take up usable nitrogen from

the soil and ocean.

Page 31: Biogeochemical Cycles

Nitrogen Cycle5. Consumers: Obtain nitrogen by eating plants.

Page 32: Biogeochemical Cycles

Nitrogen Cycle6. Excretion: Urine returns nitrogen to the soil. Decomposition: When organisms decay, nitrogen

is returned to the soil.

Page 33: Biogeochemical Cycles

Nitrogen Cycle7. Denitrification: Some bacteria change usable

nitrogen back into nitrogen gas (N2) which goes back into the atmosphere.

Page 34: Biogeochemical Cycles

Nitrogen Cycle1. What are two ways nitrogen cycle allows nitrogen

to be taken out of the atmosphere and made usable for plants and animals?Nitrogen fixing bacteria, lightning, man

made fertilizer2. What are the three ways that ammonia (NH3) are formed?Nitrogen fixing bacteria, decomposition,

excretion, deposition

Page 35: Biogeochemical Cycles

Phosphorus Cycle1. What is phosphorus used for in living things?

2. What form is phosphorus frequently found in?

3. What part of the biosphere is phosphorus not found in, that carbon, water and nitrogen are found in?

ATP (Energy), DNA (Phosphate Group)

Rocks, sediments, soil minerals

Atmosphere