Cited by 457Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisMethane Hydrates and Related Phenomena

Large Sulfur Bacteria and the Formation of Phosphorite

Schulz, Heide N., Schulz, Horst D.·2005·Science

Abstract

Phosphorite deposits in marine sediments are a long-term sink for an essential nutrient, phosphorus. Here we show that apatite abundance in sediments on the Namibian shelf correlates with the abundance and activity of the giant sulfur bacterium Thiomargarita namibiensis , which suggests that sulfur bacteria drive phosphogenesis. Sediments populated by Thiomargarita showed sharp peaks of pore water phosphate (≤300 micromolar) and massive phosphorite accumulations (≥50 grams of phosphorus per kilogram). Laboratory experiments revealed that under anoxic conditions, Thiomargarita released enough phosphate to account for the precipitation of hydroxyapatite observed in the environment.

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Crossref · 10.1126/science.1103096

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  • Polyphosphate hydrolysis caused the increase in marine sediment pore water inorganic phosphate concentration, leading to biologically induced hydroxyapatite precipitation.

    “It was concluded that polyP hydrolysis caused the increase in marine sediment pore water Pi concentration, leading to biologically induced hydroxyapatite precipitation [79].”
  • 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].”
  • Incubation of these bacteria in the laboratory demonstrated inorganic phosphate release under anoxic conditions.

    “Incubation of these bacteria in the laboratory demonstrated Pi release under anoxic conditions [79].”
  • In situ inorganic phosphate concentrations of up to 300 μM were measured within ocean sediment composed of about 25% hydroxyapatite and populated by Thiomargarita.

    “In situ Pi concentrations of up to 300 μM were measured within ocean sediment composed of ~25 % hydroxyapatite and populated by Thiomargarita [79].”
  • Organisms can concentrate and store inorganic phosphate from their environment and then release it to survive periodic anaerobic environments or after death.

    “It was later proven that organisms can concentrate and store Pi from their environment [78] and then release Pi to survive periodic anaerobic environments [79] or after death [75, 80].”

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Authors
Schulz, H. N., & Schulz, H. D.
Affiliations
Leibniz University Hannover (DE)
Corresponding author
Schulz, Heide N.
Venue
Science
Published
2005-01-21
Volume
307
Issue
5708
Pages
416-418
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2078012795
Cited by
457
References
0
Citations by year
2026: 22 · 2025: 21 · 2024: 19 · 2023: 53 · 2022: 14 · 2021: 23 · 2020: 15 · 2019: 25 · 2018: 31 · 2017: 27 · 2016: 29 · 2015: 21 · 2014: 26 · 2013: 25 · 2012: 17
FWCI
10.07
Type
journal article
Language
en
Open access
closed
Locations
  • Science (publishedVersion)
  • PubMed (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Environmental Science › Environmental Chemistry › Methane Hydrates and Related Phenomena
Keywords
sulfur bacteria, phosphorite formation, phosphogenesis, apatite, hydroxyapatite precipitation, phosphate release, anoxia, marine sediment, Namibian continental shelf, phosphorus cycling
MeSH terms
Aerobiosis, Anaerobiosis, Diffusion, Energy Metabolism, Hydroxyapatites, Minerals, Nitrates, Oxidation-Reduction, Phosphates, Polyphosphates, Chemical Precipitation, Seawater, Sulfides, Thermodynamics, Geologic Sediments, Thiotrichaceae

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