Email. The water cycle. Carbon can be stored in a variety of reservoirs, including plants and animals, which is why they are considered carbon life forms. The geologic component of the carbon cycle operates slowly in comparison to the other parts of the global carbon cycle. This is the currently selected item. The Geological Carbon Cycle. The carbon cycle . The carbon cycle. Learn how carbon moves through Earth's ecosystems and how human activities are altering the carbon cycle. The global carbon cycle is driven by geologic processes and by photosynthesis and the respiration of plants and animals (Figure 2.24). The movement of carbon from reservoir to reservoir is known as the carbon cycle. Carbon is used by plants to build leaves and stems, which are then digested by animals and used for cellular growth. Mouseover the words on the picture to learn more "In the geological carbon cycle, carbon moves between rocks and minerals, seawater, and the atmosphere. Plants take up CO 2 from the atmosphere and convert it to carbon in plant tissue and oxygen. The carbon cycle is tied to the availability of other elements and compounds. This mineral is then dissolved by rainwater and carried to the oceans. Intro to biogeochemical cycles. Once in the ocean, carbon dioxide gas reacts with water molecules to release hydrogen, making the ocean more acidic. Most of the earth's carbon is stored inertly in the earth's lithosphere. The water cycle. Biogeochemical cycles. However, the slow carbon cycle also contains a slightly faster component: the ocean. Plants also respire to generate energy for life. Google Classroom Facebook Twitter. 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. It is one of the most important determinants of the amount of carbon in the atmosphere, and thus of global temperatures. The nitrogen cycle. The carbon cycle. During photosynthesis, plants take carbon dioxide from the air and used it to make glucose (stored carbon), while releasing oxygen. Biogeochemical cycles overview. For example, the carbon cycle is tied to the availability of oxygen in the atmosphere. Carbon dioxide in the atmosphere reacts with some minerals to form the mineral calcium carbonate (limestone).
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