Geobiology & Biogeochemistry

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Geobiology & Biogeochemistry Chapter 11

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Geobiology & Biogeochemistry. Chapter 11. Biogeochemical Terms. Stromatolites Bacteria Archaea Eukaryota Phosphorus Cycle Sulfur Cycle Carbon Cycle Nitrogen Cycle. Tree of Life. Archaea. Archaea (ancient ones) - PowerPoint PPT Presentation

Transcript of Geobiology & Biogeochemistry

Page 1: Geobiology & Biogeochemistry

Geobiology & Biogeochemistry

Chapter 11

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Biogeochemical Terms• Stromatolites• Bacteria• Archaea• Eukaryota• Phosphorus Cycle• Sulfur Cycle• Carbon Cycle• Nitrogen Cycle

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Tree of Life

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Archaea

• Archaea (ancient ones) • Archaea, like bacteria, are

prokaryote micro-organisms that lack a membrane-bound organelle such as a nucleus.

• They were discovered in extreme environments and defined on RNA phylogentics.

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Bacteria

• Bacteria are micro-organisms that lack a membrane-bound nucleus.

• There are 10 times as many bacterial cells in your body as human cells.

• Bacteria are ubiquitous in all terrestrial environments from high atmosphere to several km underground

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Eukarya

• Eukaryotes are organisms with a cytoskeleton and cell nuclei .

• Eukaryotes include:– Animals– Plants– Fungi– Diatoms & dinoflagellates

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Your Family Tree

Based on RNA phylogenetics

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Div

ersi

ty o

f org

anis

ms

Age (Ma)0200400600

800

0

200

400

600

Cambrianradiation

429 MaMass

extinction364 MaMass

extinction

End-Permianmass extinction

208 MaMass extinction

End-Cretaceousmass extinction

The end-Cretaceous extinction includedthe demise of dinosaurs.

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Stromatolites

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Stromatolites

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Stromatolites

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Stromatolites• Stromatolites are bacterial mats

that precipitate calcite from seawater.

• These carbonates are preserved directly as fossils.

• Earliest stromatolites are 3.5 Gy• These are the earliest true fossils on

Earth

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Biogeochemical Cycles

• Some biogeochemical cycles may leave distinctive isotopic signatures that permit them to be identified in very ancient rocks.

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Biogeochemical Cycles• Phosphorus P5+ (no oxidation) • Sulfur S2-, S6+

• Carbon C0, C4+ (CO2, CH4)

• Nitrogen: N3-,N0, N2+, N5+

• ‘Reduction’ means decrease in valence.

• ‘Oxidation’ means increase in valence.

• Reduction / oxidation (redox) reactions provide

energy for biology.

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THE PHOSPHORUS CYCLE

Tectonic processesuplift rock to the surface.

Wind and rain erodephosphorus-richrocks.

Plants usephosphorusfrom soil.

Animals eatplants.

Decomposersreturn phosphorusto soil.

Phosphorus leaches from the soil into water.

Runoff of phosphate-bearing compounds in fertilizers.

Sediment accumulatesto form phosphate-rich sedimentary rocks.

Runoff carries sediment to rivers, lakes, and oceans.

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Phosphorus Cycle:(your teeth and bones)

• Ca5(PO4)3(OH) Apatite in rocks• H(PO4)- in soils• Phosphorus is essential for plant

growth.• P is a limiting nutrient in oceans• P in runoff causes algal blooms and

eutrophication (oxygen depletion in water)

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Sulfur Cycle• S2- (sulfide) to S6+O3• S6+O3 + H2O = H2SO4• S6+ reduced to S2- • Acid mine drainage• Eutrophication removes S• Operates by oxidation/reduction• Sulfur isotopes fractionated

–Ancient biological activity may leave isotopic signature.

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Carbon Cycle• Photosynthesis (reduction of

atmospheric CO2)• CO2 (atmosphere) = C + O2• Carbon traps

–CH4 (methane)–Organic hydrocarbons

• Wood, Coal, gas, petroleum–Ocean & biogenic calcite–Magnesite (MgCO3)

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Carbon Cycle• Photosynthesis (reduction of

atmospheric CO2)• CO2 (atmosphere) = C + O2• Atmosphere is ~390 ppm CO2• We do not know where all the CO2 is

going.– 2/3 of total emission is removed– 1/3 of total accumulates in atmosphere

• Very active area of research.

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Carbon Cycle

• How much increase in 50 years?

• 395-315 = 80 ppm• 80 / 315 = ~ 25% in 50 years

• What are you going to do?

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Nitrogen Cycle• N3-H4

+, N20, NO2-, NO3

-

• N2 (atmosphere) • NH4

+ (ammonia) in soils• NH4

+ can also be in minerals• Nitrogen isotopes fractionated

–Ancient biological activity may leave N isotopic signature.

• 14N (99.7%); 15N (0.3%)

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Sediment accumulatesto form phosphate-rich sedimentary rocks.

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Nitrogen Cycle

• Haber Process (1914)– CH4 (methane) + H2O = CO + 3H2

– N2 + 3H2 = 2 NH3

• Sustains about 1/3 human population– Can also be used for explosives

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Clicker Question• Which of the major divisions of life-forms

on Earth has membrane-divided organelles and a cytoskeleton?– A. Bacteria– B. Archaea– C. Eukarya– D. Viruses– E. They all do

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Clicker Question• Which of the major divisions of life-forms

on Earth has membrane-divided organelles and a cytoskeleton?– A. Bacteria– B. Archaea– C. Eukarya– D. Viruses– E. They all do

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Clicker Question• Which of the major divisions of life-forms

on Earth includes both multi-celled plants and animals?– A. Bacteria– B. Archaea– C. Eukarya– D. Viruses– E. They all do

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Clicker Question• Which of the major divisions of life-forms

on Earth includes both multi-celled plants and animals?– A. Bacteria– B. Archaea– C. Eukarya– D. Viruses– E. They all do

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Clicker Question• Which of the major bio-geochemical

cycles (S, C, P, N) does not involve oxidation-reduction.– A. Sulfur– B. Carbon– C. Nitrogen– D. Phosphorus– E. They all do

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Clicker Question• Which of the major bio-geochemical

cycles (S, C, P, N) does not involve oxidation-reduction.– A. Sulfur– B. Carbon– C. Nitrogen– D. Phosphorus– E. They all do

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Clicker Question• The oldest true fossils on Earth are

stromatolites. The oldest of these are about:– A. 6000 years– B. 550 million years– C. 2000 million years– D. 3500 million years– E. 4550 million years

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Clicker Question

• The oldest true fossils on Earth are stromatolites. The oldest of these are about:– A. 6000 years– B. 550 million years– C. 2000 million years– D. 3500 million years– E. 4550 million years

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Tree of Life based on phylogenetics(Biochemistry)

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Biogeochemical Terms• Stromatolites• Bacteria• Archaea• Eukarya• Phosphorus Cycle• Sulfur Cycle• Carbon Cycle• Nitrogen Cycle