
biogeochemistry
Sign in to savethumb|right|300px| Cyanobacterial Microbial mat|mat dominated by [[Anabaena sp. (heterocystous) in the Mayotte lagoon at 14 m depth. These cyanobacteria fix nitrogen and influence redox conditions, contributing to biogeochemical cycling in marine environments.]]
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11 sectionsContents
- History
- Early Greek
- 18th-19th centuries
- 20th century
- Biogeochemical cycles
- Research
- Evolutionary Biogeochemistry
- See also
- References
- Representative books and publications
- External links
thumb|right|300px| Cyanobacterial Microbial mat|mat dominated by [[Anabaena sp. (heterocystous) in the Mayotte lagoon at 14 m depth. These cyanobacteria fix nitrogen and influence redox conditions, contributing to biogeochemical cycling in marine environments.]]
Biogeochemistry is the scientific discipline that involves the study of the chemical, physical, geological, and biological processes and reactions that govern the composition of the natural environment (including the biosphere, the cryosphere, the hydrosphere, the pedosphere, the atmosphere, and the lithosphere). In particular, biogeochemistry is the study of biogeochemical cycles, the cycles of chemical elements such as carbon and nitrogen, and their interactions with and incorporation into living things transported through earth scale biological systems in space and time. The field focuses on chemical cycles which are either driven by or influence biological activity. Particular emphasis is placed on the study of carbon, nitrogen, oxygen, sulfur, iron, and phosphorus cycles. Biogeochemistry is a systems science closely related to systems ecology.