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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Format: | Report |
Language: | English |
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Woods Hole Oceanographic Institution
2007
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Online Access: | https://doi.org/10.2172/969330 https://digital.library.unt.edu/ark:/67531/metadc929343/ |