What this deck covers
This deck focuses on The Carbon Cycle, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study The Carbon Cycle in AP Environmental Science with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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Which cycle describes the movement of carbon through living organisms and the environment?
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The carbon cycle. Movement of carbon between atmosphere, biosphere, and geosphere.
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This deck focuses on The Carbon Cycle, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Work through these flashcards in short sessions. Try to answer each prompt before flipping the card, then revisit any cards you miss until the explanation feels automatic.
Answer: The carbon cycle. Movement of carbon between atmosphere, biosphere, and geosphere.
Answer: Burning of fossil fuels. Human activities like coal, oil, and gas combustion.
Answer: Decomposition. Bacteria and fungi break down dead material, releasing carbon.
Answer: Outgassing. Volcanic activity releases CO2 stored in Earth's interior.
Answer: Respiration. Cellular process breaking down glucose and releasing CO2.
Answer: Carbon fixation. The process where plants convert atmospheric CO2 into organic molecules.
Answer: Degassing. Warmer water releases dissolved CO2 back to atmosphere.
Answer: Decompose organic matter, releasing CO2. Bacteria and fungi break down dead material, returning carbon to atmosphere.
Answer: Carbon dioxide (CO2). Makes up about 0.04% of atmospheric gases by volume.
Answer: Photosynthesis. Light-driven process converting CO2 and water into glucose.
Answer: Respiration. Cellular process where organisms break down glucose and release CO2.
Answer: They sequester carbon in shells and skeletons. Build calcium carbonate shells that store carbon long-term.
Answer: Dissolved inorganic carbon. Bicarbonates and carbonates dissolved in ocean water.
Answer: Decreases pH (acidification). Dissolved CO2 forms carbonic acid, lowering ocean pH.
Answer: Bicarbonate ions (HCO3−). Most oceanic carbon exists as dissolved bicarbonate ions.
Answer: Dissolution. CO2 dissolves in seawater forming carbonic acid and bicarbonates.
Answer: Fossilization. Dead organisms buried under sediments form coal, oil, and gas over time.
Answer: Burning fossil fuels. Combustion releases stored carbon from coal, oil, and natural gas.
Answer: Enhances plant growth due to more photosynthesis. CO2 fertilization effect increases photosynthetic rates.
Answer: Absorb CO2 during photosynthesis. Marine algae fix atmospheric carbon through photosynthesis.
Answer: Fossilization. Dead organisms buried under sediments form coal, oil, and gas over time.
Answer: Calcium carbonate (CaCO3). Carbonate mineral formed from marine organisms' shells over time.
Answer: From decomposed organic matter under pressure. Heat and pressure transform buried organic material over millions of years.
Answer: Calvin cycle. Light-independent reactions that fix CO2 into sugar molecules.
Answer: Photosynthesis. Plants remove atmospheric CO2 and convert it to biomass.
Answer: Photosynthesis. Light-driven process converting CO2 and water into glucose.
Answer: They sequester carbon in shells and skeletons. Build calcium carbonate shells that store carbon long-term.
Answer: From decomposed organic matter under pressure. Heat and pressure transform buried organic material over millions of years.
Answer: Bicarbonate ions (HCO3−). Most oceanic carbon exists as dissolved bicarbonate ions.
Answer: Carbon. Fossil fuels are primarily carbon compounds like hydrocarbons.
Answer: Calcium carbonate (CaCO3). Carbonate mineral formed from marine organisms' shells over time.
Answer: Photosynthesis. Plants remove atmospheric CO2 and convert it to biomass.
Answer: The carbon cycle. Movement of carbon between atmosphere, biosphere, and geosphere.
Answer: Geological carbon. Carbon stored in coal, oil, and natural gas deposits.
Answer: Enhanced greenhouse effect. More heat trapped leads to rising global temperatures.
Answer: CO2. One carbon atom bonded to two oxygen atoms.
Answer: Global warming. More atmospheric CO2 enhances the greenhouse effect.
Answer: Carbon dioxide (CO2). Absorbs infrared radiation, trapping heat in Earth's atmosphere.
Answer: Dissolution. CO2 dissolves in seawater forming carbonic acid and bicarbonates.
Answer: Carbon dioxide (CO2). Makes up about 0.04% of atmospheric gases by volume.
Answer: Enhances plant growth due to more photosynthesis. CO2 fertilization effect increases photosynthetic rates.
Answer: Biomass carbon. Carbon stored in living plant tissues and wood.
Answer: Enhanced greenhouse effect. More heat trapped leads to rising global temperatures.
Answer: Carbon sequestration. Long-term storage of carbon in geological formations.
Answer: Increases CO2 levels in the atmosphere. Removing trees reduces carbon sequestration and adds CO2 from burning.
Answer: Increased CO2 leads to global warming. Excess atmospheric carbon enhances greenhouse warming.
Answer: Sedimentary rocks. Contains limestone and other carbonate minerals storing most Earth's carbon.
Answer: Decomposition. Bacteria and fungi break down dead material, releasing carbon.
Answer: Carbon sequestration. Removing atmospheric carbon and storing it in solid forms.
Answer: Deforestation. Removing forests reduces carbon storage and increases emissions.
Answer: Deforestation. Removing forests reduces carbon storage and increases emissions.
Answer: Microbial respiration. Soil microbes decompose organic matter, releasing CO2.
Answer: Global warming. More atmospheric CO2 enhances the greenhouse effect.
Answer: Sedimentary rocks. Contains limestone and other carbonate minerals storing most Earth's carbon.
Answer: Dissolved inorganic carbon. Bicarbonates and carbonates dissolved in ocean water.
Answer: Increases CO2 levels in the atmosphere. Removing trees reduces carbon sequestration and adds CO2 from burning.
Answer: Carbon sequestration. Long-term storage of carbon in geological formations.
Answer: Soil respiration. Microorganisms in soil decompose organic matter, releasing CO2.
Answer: Respiration. Cellular process breaking down glucose and releasing CO2.
Answer: Outgassing. Volcanic activity releases CO2 stored in Earth's interior.
Answer: Carbon sequestration. Removing atmospheric carbon and storing it in solid forms.
Answer: Impairs shell formation in marine organisms. Lower pH dissolves carbonate shells and disrupts marine ecosystems.
Answer: Soil respiration. Microorganisms in soil decompose organic matter, releasing CO2.
Answer: Carbon dioxide (CO2). Absorbs infrared radiation, trapping heat in Earth's atmosphere.
Answer: Absorb CO2 during photosynthesis. Marine algae fix atmospheric carbon through photosynthesis.
Answer: Impairs shell formation in marine organisms. Lower pH dissolves carbonate shells and disrupts marine ecosystems.
Answer: Respiration. Cellular process where organisms break down glucose and release CO2.
Answer: Geological carbon. Carbon stored in coal, oil, and natural gas deposits.
Answer: Biomass carbon. Carbon stored in living plant tissues and wood.
Answer: Burning of fossil fuels. Human activities like coal, oil, and gas combustion.
Answer: Decreases pH (acidification). Dissolved CO2 forms carbonic acid, lowering ocean pH.
Answer: Decompose organic matter, releasing CO2. Bacteria and fungi break down dead material, returning carbon to atmosphere.
Answer: Calvin cycle. Light-independent reactions that fix CO2 into sugar molecules.
Answer: Carbon fixation. The process where plants convert atmospheric CO2 into organic molecules.
Answer: Microbial respiration. Soil microbes decompose organic matter, releasing CO2.
Answer: Increased CO2 leads to global warming. Excess atmospheric carbon enhances greenhouse warming.
Answer: Burning fossil fuels. Combustion releases stored carbon from coal, oil, and natural gas.
Answer: Degassing. Warmer water releases dissolved CO2 back to atmosphere.