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This deck focuses on Describe Matter Movement In Ecosystems, giving you a quick way to review the definitions, rules, and examples that matter most for Biology.
Study Describe Matter Movement In Ecosystems in Biology with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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What is the correct term for the total mass of living organic matter in a given area?
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Biomass. Measures the total amount of living organic matter present.
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This deck focuses on Describe Matter Movement In Ecosystems, giving you a quick way to review the definitions, rules, and examples that matter most for Biology.
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: Biomass. Measures the total amount of living organic matter present.
Answer: The movement of nitrogen among atmosphere, soil, water, and organisms. Nitrogen moves between air, soil, water, and living organisms.
Answer: Biogeochemical cycle. Elements move through biological, geological, and chemical processes.
Answer: Decomposers convert organic nitrogen to NH3$/NH_4^+$. Releases nitrogen from dead organisms back to the soil.
Answer: Long-term storage of carbon in biomass, soils, oceans, or rocks. Carbon is removed from active cycling and stored long-term.
Answer: Precipitation. Water vapor condenses and falls as rain, snow, or other forms.
Answer: Sedimentary rocks and carbonate minerals. These geological formations hold carbon for millions of years.
Answer: N2 → fixation → NH4+$/NO_3^-$ → assimilation. Shows nitrogen conversion from atmospheric gas to bioavailable form to organic compounds.
Answer: Precipitation. Water vapor condenses and falls as rain, snow, or other forms.
Answer: Low oxygen (anaerobic) soils or sediments. Denitrifying bacteria use nitrate as an electron acceptor without oxygen.
Answer: N2 → fixation → NH4+$/NO_3^-$ → assimilation. Shows nitrogen conversion from atmospheric gas to bioavailable form to organic compounds.
Answer: Evaporation. Solar energy converts liquid water to water vapor.
Answer: Ammonification (mineralization). Bacteria break down organic nitrogen compounds to release ammonium.
Answer: A storage location for matter, such as soil, biomass, or atmosphere. These pools hold matter temporarily during biogeochemical cycles.
Answer: Decomposers consume O2 during decomposition. Bacterial decomposition of dead algae consumes dissolved oxygen rapidly.
Answer: Nitrification. Bacteria oxidize ammonium to nitrate in well-oxygenated soil.
Answer: Accumulation in food webs; it is not a nutrient cycle. Toxins concentrate up food chains rather than cycling through ecosystems.
Answer: Decomposition and humification. Decomposers break down organic matter and form stable soil carbon.
Answer: The movement of carbon among atmosphere, biosphere, oceans, and rocks. Carbon moves between living and nonliving reservoirs on Earth.
Answer: Ammonification (mineralization). Bacteria break down organic nitrogen compounds to release ammonium.
Answer: Phosphate is scarce and has no large atmospheric reservoir for rapid replacement. Limited supply and slow replacement make phosphorus growth-limiting.
Answer: Release of water vapor from plant stomata to the atmosphere. Plants lose water vapor during gas exchange for photosynthesis.
Answer: Dead organisms and organic waste (feces, leaf litter). Non-living organic matter that serves as food for decomposers.
Answer: Bacterial conversion of NH4+ to NO2− then NO3−. Oxidizes ammonia to nitrites then nitrates in aerobic conditions.
Answer: Excess nutrients cause algal blooms and oxygen depletion in water. Nutrient pollution stimulates excessive plant growth and ecosystem disruption.
Answer: Nitrogen-fixing bacteria (free-living or in root nodules). They have the enzyme nitrogenase that converts atmospheric N2.
Answer: Decomposition and excretion. Death and waste products release phosphate back to the environment.
Answer: They convert inorganic matter into organic biomass. They build organic compounds from simple inorganic molecules like CO2.
Answer: Denitrification. Bacteria reduce nitrate to nitrogen gas in oxygen-poor conditions.
Answer: Decomposition and respiration releasing CO2. Decomposer respiration releases carbon stored in wood as CO2.
Answer: Conversion of atmospheric N2 into ammonia (NH3)/NH4+. Breaks the strong triple bond in N2 to make bioavailable nitrogen.
Answer: Bacterial conversion of NO3− to atmospheric N2 (and N2O). Returns nitrogen to the atmosphere, completing the cycle.
Answer: Evaporation. Solar energy converts liquid water to water vapor.
Answer: They break down detritus and recycle nutrients to the environment. They return nutrients to soil and water for producer uptake.
Answer: Use of nitrogen fertilizers and runoff into waterways. Fertilizers introduce excess nitrogen that can overstimulate plant growth.
Answer: Matter is incorporated into hawk biomass and released as waste and CO2. Matter is either assimilated into tissues or excreted as waste.
Answer: Decomposers consume O2 during decomposition. Bacterial decomposition of dead algae consumes dissolved oxygen rapidly.
Answer: Biogeochemical cycle. Elements move through biological, geological, and chemical processes.
Answer: Decomposers convert organic nitrogen to NH3$/NH_4^+$. Releases nitrogen from dead organisms back to the soil.
Answer: Release of water vapor from plant stomata to the atmosphere. Plants lose water vapor during gas exchange for photosynthesis.
Answer: Excess nutrients cause algal blooms and oxygen depletion in water. Nutrient pollution stimulates excessive plant growth and ecosystem disruption.
Answer: A pathway where detritus is consumed and nutrients are recycled. It processes dead matter and returns nutrients to ecosystem pools.
Answer: Burning fossil fuels (combustion). Releases stored carbon from fossil fuels into the atmosphere.
Answer: They break down detritus and recycle nutrients to the environment. They return nutrients to soil and water for producer uptake.
Answer: Matter is incorporated into hawk biomass and released as waste and CO2. Matter is either assimilated into tissues or excreted as waste.
Answer: Phosphate ions (PO43−) from weathered rock/soil. Rock weathering releases phosphate ions that plants can uptake.
Answer: A pathway where detritus is consumed and nutrients are recycled. It processes dead matter and returns nutrients to ecosystem pools.
Answer: Water (H2O) absorbed from soil by roots. Plants absorb water through roots for the light-dependent reactions.
Answer: Cellular respiration. All organisms break down organic compounds and release CO2.
Answer: Decomposition and humification. Decomposers break down organic matter and form stable soil carbon.
Answer: Accumulation in food webs; it is not a nutrient cycle. Toxins concentrate up food chains rather than cycling through ecosystems.
Answer: Movement of water from the surface into soil and groundwater. Water soaks into soil and recharges underground water supplies.
Answer: Uptake of NO3− or NH4+ to build organic nitrogen compounds. Plants absorb inorganic nitrogen to synthesize proteins and nucleic acids.
Answer: Sedimentary rocks and carbonate minerals. These geological formations hold carbon for millions of years.
Answer: Bacterial conversion of NO3− to atmospheric N2 (and N2O). Returns nitrogen to the atmosphere, completing the cycle.
Answer: Uptake of NO3− or NH4+ to build organic nitrogen compounds. Plants absorb inorganic nitrogen to synthesize proteins and nucleic acids.
Answer: Weathering and erosion. Physical and chemical breakdown of rocks makes phosphate available.
Answer: Biomass. Measures the total amount of living organic matter present.
Answer: Nitrate (NO3−) or ammonium (NH4+) in soil. These are the bioavailable forms of nitrogen that plant roots can absorb.
Answer: They convert inorganic matter into organic biomass. They build organic compounds from simple inorganic molecules like CO2.
Answer: Carbon dioxide (CO2) from the atmosphere. Plants fix atmospheric CO2 during photosynthesis to make glucose.
Answer: Nitrogen-fixing bacteria (free-living or in root nodules). They have the enzyme nitrogenase that converts atmospheric N2.
Answer: The rate of movement of matter between reservoirs. Measures how fast matter moves from one pool to another.
Answer: Use of nitrogen fertilizers and runoff into waterways. Fertilizers introduce excess nitrogen that can overstimulate plant growth.
Answer: The movement of water among ocean, atmosphere, land, and organisms. Water moves through different reservoirs driven by solar energy.
Answer: CO2 → grass → rabbit → wolf. Shows carbon moving through a complete food chain from producer to tertiary consumer.
Answer: Movement of water from the surface into soil and groundwater. Water soaks into soil and recharges underground water supplies.
Answer: Cellular respiration. All organisms break down organic compounds and release CO2.
Answer: Conversion of atmospheric N2 into ammonia (NH3)/NH4+. Breaks the strong triple bond in N2 to make bioavailable nitrogen.
Answer: The movement of nitrogen among atmosphere, soil, water, and organisms. Nitrogen moves between air, soil, water, and living organisms.
Answer: Decomposition and respiration releasing CO2. Decomposer respiration releases carbon stored in wood as CO2.
Answer: Phosphorus cycles via rocks/soil; it has no major atmospheric gas phase. Phosphorus lacks a gaseous form and moves only through solid/liquid phases.
Answer: The movement of carbon among atmosphere, biosphere, oceans, and rocks. Carbon moves between living and nonliving reservoirs on Earth.
Answer: Macronutrients are needed in larger amounts; micronutrients in trace amounts. Macronutrients like carbon and nitrogen are needed in large quantities.
Answer: CO2 → grass → rabbit → wolf. Shows carbon moving through a complete food chain from producer to tertiary consumer.
Answer: Nitrification. Bacteria oxidize ammonium to nitrate in well-oxygenated soil.
Answer: Phosphorus cycles via rocks/soil; it has no major atmospheric gas phase. Phosphorus lacks a gaseous form and moves only through solid/liquid phases.
Answer: Dead organisms and organic waste (feces, leaf litter). Non-living organic matter that serves as food for decomposers.
Answer: Carbon dioxide (CO2) from the atmosphere. Plants fix atmospheric CO2 during photosynthesis to make glucose.
Answer: They transfer matter by eating and assimilating biomass. They move organic matter through food webs by consuming other organisms.
Answer: The rate of movement of matter between reservoirs. Measures how fast matter moves from one pool to another.
Answer: They transfer matter by eating and assimilating biomass. They move organic matter through food webs by consuming other organisms.
Answer: Decomposition and excretion. Death and waste products release phosphate back to the environment.
Answer: A storage location for matter, such as soil, biomass, or atmosphere. These pools hold matter temporarily during biogeochemical cycles.
Answer: Phosphate is scarce and has no large atmospheric reservoir for rapid replacement. Limited supply and slow replacement make phosphorus growth-limiting.
Answer: Phosphate ions (PO43−) from weathered rock/soil. Rock weathering releases phosphate ions that plants can uptake.
Answer: Burning fossil fuels (combustion). Releases stored carbon from fossil fuels into the atmosphere.
Answer: Denitrification. Bacteria reduce nitrate to nitrogen gas in oxygen-poor conditions.
Answer: The movement of water among ocean, atmosphere, land, and organisms. Water moves through different reservoirs driven by solar energy.
Answer: Photosynthesis. Plants convert atmospheric CO2 into organic carbon compounds.
Answer: Macronutrients are needed in larger amounts; micronutrients in trace amounts. Macronutrients like carbon and nitrogen are needed in large quantities.
Answer: Surface flow of water into streams, rivers, lakes, and oceans. Water flows over land surfaces back to water bodies.
Answer: Weathering and erosion. Physical and chemical breakdown of rocks makes phosphate available.
Answer: Combustion. Burning organic matter or fossil fuels oxidizes carbon to CO2.
Answer: Nitrate (NO3−) or ammonium (NH4+) in soil. These are the bioavailable forms of nitrogen that plant roots can absorb.
Answer: Photosynthesis. Plants convert atmospheric CO2 into organic carbon compounds.
Answer: Bacterial conversion of NH4+ to NO2− then NO3−. Oxidizes ammonia to nitrites then nitrates in aerobic conditions.
Answer: Water (H2O) absorbed from soil by roots. Plants absorb water through roots for the light-dependent reactions.
Answer: Combustion. Burning organic matter or fossil fuels oxidizes carbon to CO2.
Answer: Surface flow of water into streams, rivers, lakes, and oceans. Water flows over land surfaces back to water bodies.