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Ecology - Carbon cycling

Grade 12IBBiology

Review the key concepts, formulae, and examples before starting your quiz.

🔑Concepts

Autotrophs convert atmospheric carbon dioxide into carbohydrates and other carbon compounds through the process of carbon fixation during photosynthesis (6CO2+6H2OC6H12O6+6O26CO_2 + 6H_2O \rightarrow C_6H_{12}O_6 + 6O_2).

In aquatic ecosystems, carbon is present as dissolved CO2CO_2 and hydrogen carbonate ions (HCO3HCO_3^-). The CO2CO_2 dissolves in water to form carbonic acid (H2CO3H_2CO_3), which dissociates to lower the pH.

Carbon dioxide diffuses from the atmosphere or water into autotrophs, moving down a concentration gradient created as autotrophs use CO2CO_2 for photosynthesis.

Carbon dioxide is produced by the respiration of all organisms (producers, consumers, and decomposers) and diffuses out of cells into the atmosphere or water.

Methane (CH4CH_4) is produced from organic matter in anaerobic conditions by methanogenic archaeans; it typically diffuses into the atmosphere or accumulates in the ground.

Methane is oxidized to carbon dioxide and water in the stratosphere (CH4+2O2CO2+2H2OCH_4 + 2O_2 \rightarrow CO_2 + 2H_2O), which explains why atmospheric CH4CH_4 concentrations remain relatively low despite constant production.

Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils, trapping carbon for long periods.

Partially decomposed organic matter from past geological eras was converted into oil and gas in porous rocks or into coal; combustion of this fossilized organic matter releases CO2CO_2.

Reef-building corals and mollusks have hard parts composed of calcium carbonate (CaCO3CaCO_3) that can become fossilized in limestone rock, acting as a major carbon sink.

📐Formulae

6CO2+6H2OlightC6H12O6+6O26CO_2 + 6H_2O \xrightarrow{light} C_6H_{12}O_6 + 6O_2

CO2+H2OH2CO3H++HCO3CO_2 + H_2O \rightleftharpoons H_2CO_3 \rightleftharpoons H^+ + HCO_3^-

CH4+2O2CO2+2H2OCH_4 + 2O_2 \rightarrow CO_2 + 2H_2O

Ca2++2HCO3CaCO3+CO2+H2OCa^{2+} + 2HCO_3^- \rightarrow CaCO_3 + CO_2 + H_2O

💡Examples

Problem 1:

Explain how the formation of limestone from the shells of marine organisms acts as a carbon sink and how ocean acidification affects this process.

Solution:

Marine organisms like corals use Ca2+Ca^{2+} and CO32CO_3^{2-} to build CaCO3CaCO_3 shells. When they die, these shells settle on the ocean floor and are compressed into limestone. However, increased atmospheric CO2CO_2 dissolves in the ocean to form H+H^+, which reacts with carbonate: H++CO32HCO3H^+ + CO_3^{2-} \rightarrow HCO_3^-.

Explanation:

The reduction in available CO32CO_3^{2-} ions due to increased acidity makes it difficult for organisms to synthesize CaCO3CaCO_3, potentially dissolving existing coral reefs and slowing the sequestration of carbon into limestone.

Problem 2:

Given that a specific forest has a gross primary productivity (GPPGPP) of 2.5 kg C m2 yr12.5\text{ kg C m}^{-2}\text{ yr}^{-1} and the autotrophic respiration (RaR_a) is 1.2 kg C m2 yr11.2\text{ kg C m}^{-2}\text{ yr}^{-1}, calculate the Net Primary Productivity (NPPNPP).

Solution:

NPP=GPPRa=2.51.2=1.3 kg C m2 yr1NPP = GPP - R_a = 2.5 - 1.2 = 1.3\text{ kg C m}^{-2}\text{ yr}^{-1}

Explanation:

NPPNPP represents the actual amount of carbon stored as biomass in the producers after accounting for the carbon lost through their own cellular respiration.

Carbon cycling - Revision Notes & Key Diagrams | IB Grade 12 Biology