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Cited by 527

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Methane Production in the Interstitial Waters of Sulfate-Depleted Marine Sediments

Martens, Christopher S., Berner, Robert A.·1974·Science

Abstract

Methane in the interstitial waters of anoxic Long Island Sound sediments does not reach appreciable concentrations until about 90 percent of seawater sulfate is removed by sulfate-reducing bacteria. This is in agreement with laboratory studies of anoxic marine sediments sealed in jars, which indicate that methane production does not occur until dissolved sulfate is totally exhausted. Upward diffusion of methane or its production in sulfate-free microenvironments, or both, can explain the observed coexistence of measurable concentrations of methane and sulfate in the upper portions of anoxic sediments.

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Metadata

Authors
Martens, C. S., & Berner, R. A.
Venue
Science
Published
1974-09-27
Volume
185
Issue
4157
Pages
1167-1169
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2000621691
Cited by
527
References
0
FWCI
13.35
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Methane Production in the Interstitial Waters of Sulfate-Depleted Marine Sediments. https://app.cochat.ai/papers/10.1126/science.185.4157.1167
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Martens, C. S., & Berner, R. A. (1974). Methane Production in the Interstitial Waters of Sulfate-Depleted Marine Sediments. Science. https://doi.org/10.1126/science.185.4157.1167

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.