Microbial sequestration of phosphorus in anoxic upwelling sediments
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Under anoxic and oxic conditions, sulfide-oxidizing bacteria accumulated 33P, with more accumulation in oxic conditions and no detectable 33P incorporation into dead control cells.
“They noted that under anoxic and oxic conditions these sulfide-oxidizing bacteria accumulated 33P, with more accumulation in oxic conditions and no detectable 33P incorporation into the dead (control) cells.”
From A Review of Phosphate Mineral Nucleation in Biology and Geobiology (2013) · cites this paper as [86]
Modern phosphorite formation has been associated with two species of sulfide-oxidizing bacteria that inhabit microbial mats within marine sediment: Beggiatoa and Thiomargarita namibiensis.
“Modern phosphorite formation has also been associated with two species of sulfide-oxidizing bacteria that inhabit microbial mats within the marine sediment: Beggiatoa [85, 86] and Thiomargarita namibiensis [79, 87].”
From A Review of Phosphate Mineral Nucleation in Biology and Geobiology (2013) · cites this paper as [86]
Authigenic apatite containing 33P formed most rapidly under anoxic conditions, while no apatite was formed in control experiments with dead cells.
“Authigenic (locally formed) apatite containing 33P formed most rapidly under anoxic conditions, while no apatite was formed in the control experiments with dead cells.”
From A Review of Phosphate Mineral Nucleation in Biology and Geobiology (2013) · cites this paper as [86]
Authigenic apatite formation required the presence of living cells such as Thiomargarita and Beggiatoa, and these cells accumulated phosphate as polyphosphate and released inorganic phosphate under anoxic conditions.
“The authors concluded that authigenic apatite formation required the presence of living cells such as Thiomargarita and Beggiatoa, and that these cells accumulated phosphate as polyP and released Pi under anoxic conditions [86].”
From A Review of Phosphate Mineral Nucleation in Biology and Geobiology (2013) · cites this paper as [86]
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- Authors
- Goldhammer, T., Brüchert, V., Ferdelman, T. G., & Zabel, M.
- Affiliations
- University of Bremen (DE)
- Stockholm University (SE)
- Corresponding author
- Goldhammer, Tobias
- Brüchert, Volker
- Venue
- Nature Geoscience
- Published
- 2010-07-18
- Volume
- 3
- Issue
- 8
- Pages
- 557-561
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2028366108
- Cited by
- 276
- References
- 34
- Citations by year
- 2026: 20 · 2025: 19 · 2024: 15 · 2023: 16 · 2022: 7 · 2021: 18 · 2020: 10 · 2019: 16 · 2018: 33 · 2017: 14 · 2016: 15 · 2015: 17 · 2014: 20 · 2013: 17 · 2012: 11
- FWCI
- 12.63
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- Max Planck Digital Library (submittedVersion)
- MPG.PuRe (Max Planck Society) (submittedVersion)
- Funders
- Deutsche Forschungsgemeinschaft
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- phosphorus sequestration, apatite formation, phosphate rock, organic phosphorus, sulfide-oxidizing bacteria, anoxic bottom water, Benguela upwelling, phosphate mineralization, oxygen minimum zone, marine phosphorus cycle, ocean primary productivity
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