Cited by 276Paleontology and Stratigraphy of FossilsMarine and coastal ecosystemsGeochemistry and Elemental Analysis

Microbial sequestration of phosphorus in anoxic upwelling sediments

Goldhammer, Tobias, Brüchert, Volker, Ferdelman, Timothy G., Zabel, Matthias·2010·Nature Geoscience

Integrity signals

Registry

Crossref · 10.1038/ngeo913

Cites

34 of 34 references verified0 citation errors · 0 not checkable

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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.”
  • 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].”
  • 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.”
  • 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].”

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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
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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