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  1. www.khanacademy.org › science › biologyThe carbon cycle (article) | Ecology | Khan Academy

    Jun 10, 2016 · On land, carbon is stored in soil as organic carbon from the decomposition of living organisms or as inorganic carbon from weathering of terrestrial rock and minerals. Deeper under the ground are fossil fuels such as oil, coal, and natural gas, which are the remains of plants decomposed under anaerobic—oxygen-free—conditions.

  2. biologydictionary.net › decomposerDecomposer - Definition, Function and Examples | Biology ...

    Apr 28, 2017 · When an organism dies and decomposers do the work of decomposition, the organism’s remains go through five stages of decomposition: fresh, bloat, active decay, advanced decay, and dry/remains. There are two main processes that occur in a decomposing organism: autolysis and putrefaction.

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  4. www.khanacademy.org › science › hs-biologyThe carbon cycle (article) | Khan Academy

    The decomposition of dead organisms and other nonliving organic matter also returns CO A 2 to the atmosphere. Organic matter that is not immediately broken down accumulates and is buried. Given enough time and pressure, this matter turns into fossil fuel deposits and rock, which brings us to the geological carbon cycle. Geological carbon cycle.

  5. bio.libretexts.org › Bookshelves › Introductory_and8.3.3: Energy Flow through Ecosystems - Biology LibreTexts

    Energy is acquired by living things in three ways: photosynthesis, chemosynthesis, and the consumption and digestion of other living or previously living organisms by heterotrophs.

  6. www.snexplores.org › article › recycling-deadRecycling the dead - Science News Explores

    Sep 27, 2014 · The decomposition that follows the death of every organism sets the stage for new life. It’s nature’s way of recycling. Eventually, all living things die. And except in very rare cases, all of those dead things will rot. But that’s not the end of it. What rots will wind up becoming part of something else.

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  7. www.encyclopedia.com › science-and-technologyFossils | Encyclopedia.com

    May 29, 2018 · In the modern sense, which dates from the late seventeenth century, the remains of a once-living organism, generally one that lived prior to the last glacial period, i.e. fossils are older than 10 000 years. They include skeletons, tracks, impressions, trails, borings, and casts.

  8. bio.libretexts.org › Courses › Gettysburg_College20.3: The Carbon Cycle - Biology LibreTexts

    Jan 20, 2024 · Carbon can enter the soil as a result of the decomposition of living organisms, the weathering of rocks, the eruption of volcanoes, and other geothermal systems. The Carbon Cycle Carbon, the second most abundant element in living organisms.

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