biogeochemical cycle by which carbon is exchanged among the biosphere
The carbon cycle is the process by which carbon moves between the air, living things, and Earth's systems through natural exchanges. Understanding this cycle matters because carbon is a fundamental element that flows through all life and the environment, affecting how ecosystems function.
AI-generated from the Wikipedia summary — may contain errors.
Carbon cycle schematic showing the movement of carbon between land, atmosphere, and oceans in billions of tons (gigatons) per year. Yellow numbers are natural fluxes, red are human contributions, and white are stored carbon. The effects of the slow (or deep) carbon cycle, such as volcanic and tectonic activity are not included.
The carbon cycle is a part of the biogeochemical cycle where 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 rocks such as limestone. The carbon cycle comprises a sequence of events that are key to making Earth capable of sustaining life. It describes the movement of carbon as it is recycled and reused throughout the biosphere, as well as long-term processes of carbon sequestration (storage) to and release from carbon sinks. At 422.7 parts per million (ppm), the global average atmospheric carbon dioxide has set a new record high in 2024.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).