Microbial carbon pump
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The microbial carbon pump (MCP) is a biological process in the ocean where microorganisms (primarily bacteria and archaea) transform dissolved organic carbon (DOC) into refractory dissolved organic carbon (RDOC), which is resistant to further microbial degradation. This process effectively sequesters carbon in the deep ocean for centuries to millennia, contributing significantly to long-term carbon storage and climate regulation.[1][2]
Microbes metabolize labile (easily degradable) DOC from phytoplankton or other sources, producing RDOC as a byproduct. RDOC is chemically stable and persists in the ocean, resisting breakdown. This contrasts with the biological carbon pump, which sequesters carbon via sinking particulate organic matter (e.g., dead organisms or fecal pellets). The microbial carbon pump locks away carbon in the form of RDOC, which can remain in the deep ocean for thousands of years, reducing atmospheric carbon dioxide levels over long timescales. Estimates suggest RDOC accounts for a significant portion of the ocean's ~700 billion tons of dissolved organic carbon, making the microbial carbon pump a critical component of the global carbon cycle.[1][2][3]
Diverse microbial communities, including bacteria like Prochlorococcus and Pelagibacter, drive the microbial carbon pump by transforming organic matter through metabolic processes. Environmental factors (e.g., nutrient availability, temperature) influence the efficiency of RDOC production. The microbial carbon pump helps regulate Earth's climate by storing carbon that would otherwise contribute to atmospheric carbon dioxide. It's particularly relevant in the context of climate change, as changes in ocean conditions (e.g., warming, acidification) could affect microbial activity and RDOC production.[1][2][3]
See also
[edit]References
[edit]- ^ a b c Jiao, Nianzhi; Herndl, Gerhard J.; Hansell, Dennis A.; Benner, Ronald; Kattner, Gerhard; Wilhelm, Steven W.; Kirchman, David L.; Weinbauer, Markus G.; Luo, Tingwei; Chen, Feng; Azam, Farooq (2010). "Microbial production of recalcitrant dissolved organic matter: long-term carbon storage in the global ocean". Nature Reviews Microbiology. 8 (8): 593–599. doi:10.1038/nrmicro2386. ISSN 1740-1526. PMID 20601964. Retrieved 2025-08-04.
- ^ a b c Jiao, N. and Azam, F., 2011. "Microbial carbon pump and its significance for carbon sequestration in the ocean" Microbial carbon pump in the ocean, 10, pp.43–5.
- ^ a b Legendre, Louis; Rivkin, Richard B.; Weinbauer, Markus G.; Guidi, Lionel; Uitz, Julia (2015). "The microbial carbon pump concept: Potential biogeochemical significance in the globally changing ocean". Progress in Oceanography. 134: 432–450. Bibcode:2015PrOce.134..432L. doi:10.1016/j.pocean.2015.01.008. Retrieved 2025-08-07.
- ^ "How much oxygen comes from the ocean?". NOAA's National Ocean Service. Retrieved 2025-07-17.
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