The back-and-forth movement of living and non-living matter used in the production of living matter is the biogeochemical cycle. It is a pathway by which a chemical substance moves through both biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) components of Earth.
Step-by-step explanation:
A biogeochemical cycle or material turnover or cycling of substances is a pathway by which a synthetic substance moves within biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) sections of Earth.The most significant biogeochemical cycles are the carbon cycle, nitrogen cycle, oxygen cycle, phosphorus cycle, and the water cycle. The biogeochemical cycles perpetually have a state of stability.