Methane hydrate-bearing seeps as a source of aged dissolved organic carbon to the oceans
作者： John W. Pohlman , James E. Bauer , William F. Waite , Christopher L. Osburn , N. Ross Chapman
DOI: 10.1038/NGEO1016
关键词:
摘要: Marine sediments contain large quantities of carbon, primarily in the form gas hydrate. Isotopic analyses suggest that carbon derived from fossil methane accounts for up to 28% dissolved organic sea water overlying hydrate-bearing seeps northeastern Pacific Ocean.
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