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  1. Jul 11, 2024 · carbon cycle, in biology, circulation of carbon in various forms through nature. Carbon is a constituent of all organic compounds, many of which are essential to life on Earth. The source of the carbon found in living matter is carbon dioxide (CO 2) in the air or dissolved in water. Algae and terrestrial green plants (producers) are the chief ...

    • The Editors of Encyclopaedia Britannica
  2. en.wikipedia.org › wiki › Carbon_cycleCarbon cycle - Wikipedia

    The carbon cycle is that part of the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of Earth. Other major biogeochemical cycles include the nitrogen cycle and the water cycle. Carbon is the main component of biological compounds as well as a major component of many ...

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  3. Oct 19, 2023 · The movement of carbon from reservoir to reservoir is known as the carbon cycle. Carbon can be stored in a variety of reservoirs, including plants and animals, which is why they are considered carbon life forms. Carbon is used by plants to build leaves and stems, which are then digested by animals and used for cellular growth.

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    Carbon is the backbone of life on Earth. We are made of carbon, we eat carbon, and our civilizationsour economies, our homes, our means of transportare built on carbon. We need carbon, but that need is also entwined with one of the most serious problems facing us today: global climate change.

    Forged in the heart of aging stars, carbon is the fourth most abundant element in the Universe. Most of Earths carbonabout 65,500 billion metric tonsis stored in rocks. The rest is in the ocean, atmosphere, plants, soil, and fossil fuels.

    On very long time scales (millions to tens of millions of years), the movement of tectonic plates and changes in the rate at which carbon seeps from the Earths interior may change the temperature on the thermostat. Earth has undergone such a change over the last 50 million years, from the extremely warm climates of the Cretaceous (roughly 145 to 65...

    Through a series of chemical reactions and tectonic activity, carbon takes between 100-200 million years to move between rocks, soil, ocean, and atmosphere in the slow carbon cycle. On average, 1013 to 1014 grams (10100 million metric tons) of carbon move through the slow carbon cycle every year. In comparison, human emissions of carbon to the atmo...

    Only 80 percent of carbon-containing rock is currently made this way. The remaining 20 percent contain carbon from living things (organic carbon) that have been embedded in layers of mud. Heat and pressure compress the mud and carbon over millions of years, forming sedimentary rock such as shale. In special cases, when dead plant matter builds up f...

    Chemistry regulates this dance between ocean, land, and atmosphere. If carbon dioxide rises in the atmosphere because of an increase in volcanic activity, for example, temperatures rise, leading to more rain, which dissolves more rock, creating more ions that will eventually deposit more carbon on the ocean floor. It takes a few hundred thousand ye...

    However, the slow carbon cycle also contains a slightly faster component: the ocean. At the surface, where air meets water, carbon dioxide gas dissolves in and ventilates out of the ocean in a steady exchange with the atmosphere. Once in the ocean, carbon dioxide gas reacts with water molecules to release hydrogen, making the ocean more acidic. The...

    In the meantime, winds, currents, and temperature control the rate at which the ocean takes carbon dioxide from the atmosphere. (See The Oceans Carbon Balance on the Earth Observatory.) It is likely that changes in ocean temperatures and currents helped remove carbon from and then restore carbon to the atmosphere over the few thousand years in whic...

    Carbon plays an essential role in biology because of its ability to form many bondsup to four per atomin a seemingly endless variety of complex organic molecules. Many organic molecules contain carbon atoms that have formed strong bonds to other carbon atoms, combining into long chains and rings. Such carbon chains and rings are the basis of living...

    The bonds in the long carbon chains contain a lot of energy. When the chains break apart, the stored energy is released. This energy makes carbon molecules an excellent source of fuel for all living things. On the other hand, carbon dioxide is essential for plant and phytoplankton growth. An increase in carbon dioxide could increase growth by ferti...

    Shifts in Earths orbit are happening constantly, in predictable cycles. In about 30,000 years, Earths orbit will have changed enough to reduce sunlight in the Northern Hemisphere to the levels that led to the last ice age.

    Today, changes in the carbon cycle are happening because of people. We perturb the carbon cycle by burning fossil fuels and clearing land.

    All of this extra carbon needs to go somewhere. So far, land plants and the ocean have taken up about 55 percent of the extra carbon people have put into the atmosphere while about 45 percent has stayed in the atmosphere. Eventually, the land and oceans will take up most of the extra carbon dioxide, but as much as 20 percent may remain in the atmos...

    It is significant that so much carbon dioxide stays in the atmosphere because CO2 is the most important gas for controlling Earths temperature. Carbon dioxide, methane, and halocarbons are greenhouse gases that absorb a wide range of energyincluding infrared energy (heat) emitted by the Earthand then re-emit it. The re-emitted energy travels out in...

    Because scientists know which wavelengths of energy each greenhouse gas absorbs, and the concentration of the gases in the atmosphere, they can calculate how much each gas contributes to warming the planet. Carbon dioxide causes about 20 percent of Earths greenhouse effect; water vapor accounts for about 50 percent; and clouds account for 25 percen...

    Rising carbon dioxide concentrations are already causing the planet to heat up. At the same time that greenhouse gases have been increasing, average global temperatures have risen 0.8 degrees Celsius (1.4 degrees Fahrenheit) since 1880.

    Warmer oceansa product of the greenhouse effectcould also decrease the abundance of phytoplankton, which grow better in cool, nutrient-rich waters. This could limit the oceans ability to take carbon from the atmosphere through the fast carbon cycle.

    With more atmospheric carbon dioxide available to convert to plant matter in photosynthesis, plants were able to grow more. This increased growth is referred to as carbon fertilization. Models predict that plants might grow anywhere from 12 to 76 percent more if atmospheric carbon dioxide is doubled, as long as nothing else, like water shortages, l...

    • Holli Riebeek
    • 2011
  4. Feb 1, 2019 · Carbon is the chemical backbone of life on Earth. Carbon compounds regulate the Earth’s temperature, make up the food that sustains us, and provide energy that fuels our global economy. The carbon cycle. (Image credit: NOAA) Most of Earth’s carbon is stored in rocks and sediments. The rest is located in the ocean, atmosphere, and in living ...

  5. The carbon cycle is an essential part of How the Earth System Works. Click the image on the left to open the Understanding Global ChangeInfographic. Locate the carbon cycle icon and identify other Earth system processes and phenomena that cause changes to, or are affected by, the cycling of carbon.

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