10.14
The carbon cycle describes the movement of carbon through Earth's biotic and abiotic components.
Carbon exists in oxidized forms, such as carbon dioxide, and in reduced forms, such as methane and organic matter, for example, plant litter.
Photosynthetic microbes, like cyanobacteria in aquatic habitats, absorb carbon dioxide under aerobic conditions and convert it into organic compounds using sunlight.
In low-oxygen, light-exposed environments, some microbes fix carbon via anoxygenic photosynthesis, while chemolithoautotrophs in sediments fix carbon using energy from inorganic chemical reactions rather than light.
On the other hand, heterotrophic microbes decompose organic matter, returning carbon to the atmosphere.
In aerobic soils, microbial respiration produces carbon dioxide, while methanogens in anaerobic environments generate methane.
The released methane is then converted to carbon dioxide by methanotrophs in oxygen-rich environments.
Microbial decomposition also releases carbon dioxide along with ammonia, linking the carbon and nitrogen cycles.
Obieg węgla to podstawowy proces na Ziemi obejmujący transfer węgla pomiędzy biosferą, litosferą, atmosferą i hydrosferą. Odgrywa kluczową rolę w regu…
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