Cited by 217Methane Hydrates and Related PhenomenaMicrobial Community Ecology and PhysiologyPaleontology and Stratigraphy of Fossils

Kinetics of microbial sulfate reduction in estuarine sediments

Pallud, Céline, Van Cappellen, Philippe·2006·Geochimica et Cosmochimica Acta

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Crossref · 10.1016/j.gca.2005.11.002

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  • δ34S evidence indicates that sulfate concentrations within the sediments were sufficiently low to affect the rate and extent of microbial sulfate reduction.

    “Furthermore, δ34S evidence indicates that sulfate concentrations within the sediments were sufficiently low to affect the rate and extent of microbial sulfate reduction (32).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [32]

  • Background intervals are characterized by light δ34S values (average -6.0 ± 0.6‰) that display relatively high fractionations of 30-40‰ from Cambrian seawater (ca. +30‰), indicating that microbial sulfate reduction was not impeded in these intervals.

    “Background intervals are characterized by light δ34S values (average -6.0 ± 0.6‰) that display relatively high fractionations of 30–40‰ (30) from Cambrian seawater (ca. +30‰; ref. 31), indicating that microbial sulfate reduction was not impeded in these intervals (32).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [32]

  • Diffusion-limited conditions would have slowed the typical processes of microbial degradation in sediments by restricting the efficiency of sulfate reduction, thereby shifting the primary microbial pathways for degradation of labile carbon to the less efficient processes of methanogenesis and fermentation.

    “Diffusion-limited conditions would have slowed the typical processes of microbial degradation in sediments by restricting the efficiency of sulfate reduction, thereby shifting the primary microbial pathways for degradation of labile carbon to the less efficient processes of methanogenesis and fermentation (11, 32).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [32]

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Authors
Pallud, C., & Van Cappellen, P.
Affiliations
Utrecht University (NL)
Corresponding author
Pallud, Céline
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2006-03
Volume
70
Issue
5
Pages
1148-1162
ISSN
0016-7037 (ISSN-L)
OpenAlex
W2036953839
Cited by
217
References
0
Citations by year
2026: 9 · 2025: 4 · 2024: 7 · 2023: 10 · 2022: 13 · 2021: 15 · 2020: 9 · 2019: 14 · 2018: 11 · 2017: 13 · 2016: 9 · 2015: 9 · 2014: 9 · 2013: 18 · 2012: 14
FWCI
9.57
Type
journal article
Language
en
Open access
closed
Locations
Geochimica et Cosmochimica Acta (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Methane Hydrates and Related Phenomena
  • Physical Sciences › Environmental Science › Ecology › Microbial Community Ecology and Physiology
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
microbial sulfate reduction, estuarine sediments, intertidal sediments, Scheldt estuary, Michaelis-Menten kinetics, sulfate-reducing bacteria, salinity gradient, transport limitations, organic matter quality, lactate supplementation, sediment porosity, temperature effects

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