biogeochemical cycles

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Biogeochemi cal Cycles Unit 6-2 Notes Mr. Hefti - Pulaski Biology

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Biogeochemical Cycles. Unit 6-2 Notes Mr. H efti - Pulaski Biology. You’ve seen this before – what does it mean?. Earth has a finite supply of resources * Bio = life * Geo = earth * Chemical = having to do w/ atoms. Layers of Earth. Lithosphere: Rocks / soils Hydrosphere: Water - PowerPoint PPT Presentation

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Page 1: Biogeochemical Cycles

Biogeochemical Cycles

Unit 6-2 NotesMr. Hefti - Pulaski Biology

Page 2: Biogeochemical Cycles

You’ve seen this before – what does it mean?

Page 3: Biogeochemical Cycles

Earth has a finite supply of resources

*Bio = life

*Geo = earth

*Chemical = having to do w/ atoms

Page 4: Biogeochemical Cycles

Layers of Earth

• Lithosphere: Rocks / soils • Hydrosphere: Water• Atmosphere: Air• Biosphere: Any place there is life

Page 5: Biogeochemical Cycles

Phosphorus Cycle

• P released from weathered rocks and decaying organisms

• Why is it important?– P holds DNA molecule together– Used to make ATP

Page 6: Biogeochemical Cycles

The

Phos

phor

us C

ycle

Soil decomposers

Rot

Page 7: Biogeochemical Cycles

Water Cycle

• H2O supply replenishes itself through:– Evaporation (and transpiration) – Condensation – Precipitation – Runoff

• Why is it important?– Earth would dry out without the water cycle

Page 8: Biogeochemical Cycles

Condensation

Precipitation

Runoff

Evaporation

Ground water

LakeSoil

Ocean

The Water Cycle

Page 9: Biogeochemical Cycles

Carbon Cycle

• C gets transformed through:– Photosynthesis– Respiration– Burning of fossil fuels

• Why is it important?– Needed to make glucose

Page 10: Biogeochemical Cycles

CO2 in the atmosphere

Used to make glucose during photosynthesis

Plants eaten by animals

Decaying plants make

C in rotting tissue

C in fossil fuels

CO2 released to atmosphere during

respiration

CO2 released to atmosphere when

fossil fuels are burned

The Carbon Cycle

Page 11: Biogeochemical Cycles

Nitrogen Cycle

• Life requires N-compounds but atmospheric nitrogen (N2) unusable to most living things

• Nitrogen-fixing bacteria important!

• Why is it important?– Needed to make proteins

Page 12: Biogeochemical Cycles

Nitrogen in atmosphere

Nitrogen in animal proteins

Nitrogen in plant proteins

The

Nitr

ogen

Cyc

le

Nitrogen in decaying tissues

Soil bacteria “fix” nitrogen for use by plants

Page 13: Biogeochemical Cycles

Oxygen Cycle

• Living things need O2

• Needed for release of energy

• Why is it important?– Cellular respiration

Page 14: Biogeochemical Cycles

At night, plants take in O2 and give off CO2

During day, plants take in CO2 and give off O2

Animals take in O2 and give off CO2

The Oxygen Cycle

Page 15: Biogeochemical Cycles

The Water Cycle The Water Cycle

Page 16: Biogeochemical Cycles

The Carbon Cycle The Carbon Cycle

Page 17: Biogeochemical Cycles

The Nitrogen Cycle The Nitrogen Cycle

Page 18: Biogeochemical Cycles

The Oxygen Cycle The Oxygen Cycle

Page 19: Biogeochemical Cycles

The Phosphorus Cycle The Phosphorus Cycle