Abstract
All living organisms contribute to the biogeochemical cycles, but microorganisms, due to their high abundance, their tremendous metabolic capacities and adaptation potential, play a key role in the functioning and the evolution of biogeochemical cycles. Consequently, they are keyplayers in adaptation, resistance and resilience of ecosystems. The role of microorganisms in the main biogeochemical cycles (carbon, nitrogen, sulfur, phosphorus, silicon, metals), in soils, freshwater and marine ecosystems is presented. Microbial processes involved in the turnover of biogeochemical cycles are discussed from gene to ecosystem (natural and anthropogenic ecosystems), at global, regional and local scales, as well as in targeted microenvironments (such as particles or microniches). The biodiversity of microorganisms is highlighted and their metabolic pathways on which are based exchanges and biotransformations of organic and mineral components within ecosystems are described in details. The impacts of human activities on the microbial actors and processes of biogeochemical cycles, and the cascading ecological effects (greenhouse gas emissions, acid rains, dystrophic crises, etc.), are also discussed.
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Notes
- 1.
The chemical element phosphorus (31P) exists in waters only in forms of phosphates (oxidation degree V), organic or mineral, particulate or dissolved, non-reducible under natural conditions. It is then preferable to talk about the phosphate cycle instead of the phosphorus cycle.
- 2.
Enzyme excreted by the cell and remaining attached to the outer membrane (or in the periplasmic space of gram-negative bacteria). Prokaryotic heterotrophic microorganisms, prokaryotic autotrophic (cyanobacteria) and single-celled eukaryotes (flagellates, diatoms) have for some species the genetic ability to produce ectoenzymes such as the alkaline phosphatase or the phosphonatase. The production of these enzymes is usually induced by mineral phosphate deficiency, and enables hydrolyze the phospho-ester (C-O-P) or the phosphonate (C–P) bonds of organic molecules of the DOP. The mineral phosphate released can then be incorporated by microorganisms.
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Bertrand, JC. et al. (2015). Biogeochemical Cycles. In: Bertrand, JC., Caumette, P., Lebaron, P., Matheron, R., Normand, P., Sime-Ngando, T. (eds) Environmental Microbiology: Fundamentals and Applications. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-9118-2_14
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