Release of Methane from Bering Sea Sediments During the Last Glacial Period
Several lines of evidence suggest that during times of elevated methane flux the sulfate-methane transition zone (SMTZ) was positioned near the sediment-water interface. We studied two cores (from 700 m and 1457 m water depth) from the Umnak Plateau region. Anomalously low d13C and high d18O in bent...
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Language: | unknown |
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2010
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Online Access: | http://www.osti.gov/servlets/purl/969330 https://www.osti.gov/biblio/969330 https://doi.org/10.2172/969330 |