Biogeochemical Cycles: Carbon Cycle Flashcards

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These vocabulary flashcards cover the storage, fluxes, biological processes, and chemical reactions involved in the Earth's carbon cycle as described in the BIO 2207 lecture notes.

Last updated 2:46 PM on 6/14/26
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18 Terms

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Carbon Cycle

The biogeochemical cycle by which carbon is exchanged among the biosphere, lithosphere, hydrosphere, and atmosphere of Earth.

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Major Sources of Carbon

The three primary sources include atmospheric CO2CO_2, CO2CO_2 dissolved in water bodies (H2CO3H_2CO_3), and Methane (CH4CH_4).

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Atmospheric CO2CO_2 Quantity

The atmosphere contains 700×109700 \times 10^9 metric tonnes of CO2CO_2, with an average of about 66 tonnes of carbon as CO2CO_2 over each acre of Earth.

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Hydrosphere CO2CO_2 Quantity

Water bodies contain 35000×10935000 \times 10^9 metric tonnes of CO2CO_2.

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Deep Ocean Carbon Storage

The deep ocean acts as a massive reservoir, storing 38,10038,100 Gigatonnes of Carbon (GtCGtC).

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Photosynthesis Reaction

Performed by plants, algae, and phytoplankton in the presence of light: 6CO2+6H2OC6H12O6+6O26CO_2 + 6H_2O \rightarrow C_6H_{12}O_6 + 6O_2.

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Respiration Reaction

The process of utilizing biomolecules for cellular energy: C6H12O6+6O26CO2+6H2O+E(ATP)C_6H_{12}O_6 + 6O_2 \rightarrow 6CO_2 + 6H_2O + E (ATP), which transfers carbon through successive trophic levels.

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Aerobic Decomposition

The breakdown of complex organic matter by microbes and fungi in the presence of oxygen, releasing CO2CO_2; example reaction: (C6H10O5)+nO2nH2O+nCO2+C14H12O8+heat(C_6H_{10}O_5) + nO_2 \rightarrow nH_2O + nCO_2 + C_{14}H_{12}O_8 + heat.

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Fulvic Acid (C14H12O8C_{14}H_{12}O_8)

A product formed, along with water and carbon dioxide, when cellulose is broken down during aerobic decomposition.

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Hydrolysis (Anaerobic Decomposition Step 1)

The process where complex molecules like starch are broken down into constituent monomers like glucose: (C6H10O5)+nH2OnC6H12O6(C_6H_{10}O_5) + nH_2O \rightarrow nC_6H_{12}O_6, facilitated by Clostridium.

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Acidogenesis (Anaerobic Decomposition Step 2)

The process where glucose is converted to alcohol, hydrogen, and carbon dioxide: C6H12O6+2H2O2CO2+4H2+ROHC_6H_{12}O_6 + 2H_2O \rightarrow 2CO_2 + 4H_2 + R-OH, facilitated by Clostridium.

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Acetogenesis (Anaerobic Decomposition Step 3)

The process where alcohol is converted into acetic acid, hydrogen, and carbon dioxide: ROH+nH2OnCO2+nH2+CH3COOHR-OH + nH_2O \rightarrow nCO_2 + nH_2 + CH_3COOH, facilitated by Acetobacter.

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Methanogenesis (Anaerobic Decomposition Step 4)

The process where acetic acid is converted to methane and carbon dioxide by Methanobacter: CH3COOHCO2+CH4CH_3COOH \rightarrow CO_2 + CH_4.

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Fossil Fuel Formation

Dead tissue undergoes partial decomposition to form coal (from plants) or natural gas and petroleum (from marine organisms), remaining out of circulation for thousands of years.

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Combustion of Methane

A chemical reaction that transfers carbon from fossil fuels to the atmosphere: CH4+2O22H2O+CO2+heatCH_4 + 2O_2 \rightarrow 2H_2O + CO_2 + heat.

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Carbonic Acid Formation

Carbon dioxide in the atmosphere reacts with water in a reversible reaction to form a weak acid: H2O+CO2H2CO3H_2O + CO_2 \rightleftharpoons H_2CO_3.

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Calcium Carbonate Shell Formation

Sea animals use dissolved ions like Ca++Ca^{++} and bicarbonate liberated from rock weathering to create shells: 2HCO3+Ca++CaCO3+H2O+CO22HCO_3 + Ca^{++} \rightarrow CaCO_3 + H_2O + CO_2.

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Limestone Metamorphosis

Carbon is returned to the atmosphere when limestone shell accumulations react with silicon dioxide under deep-sea heat and pressure: CaCO3+SiO2CaSiO3+CO2CaCO_3 + SiO_2 \rightarrow CaSiO_3 + CO_2.