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THE ANATOMY OF THE SULFATE-METHANE INTERFACE IN A METHANE-RICH CORE FROM THE GULF OF MEXICOD

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The sulfate-methane interface (SMI) is becoming recognized as a fundamental biogeochemical boundary in methane-rich and gas-hydrate-bearing marine sediments worldwide. The SMI separates sulfate-bearing sediment above from sulfate-depleted, methane-rich sediments below. The SMI is a zone of intense methane oxidation mediated by anaerobic methane oxidizing archaea. During this process methane and sulfate are consumed and dissolved inorganic carbon (DIC) and hydrogen sulfide (HS-) are produced; excess HS- and DIC form solid mineral phases.

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Last Updated September 29, 2016, 15:06 (LMT)
Created September 29, 2016, 15:06 (LMT)
Citation USSLER, William III1, PAULL, Charles K.1, HALLAM, Steven1, DELONG, Ed1, CHEN, Yifeng2, MATSUMOTO, Ryo2, LORENSON, Thomas3, and WINTERS, William J.4, ---- Roy Long, THE ANATOMY OF THE SULFATE-METHANE INTERFACE IN A METHANE-RICH CORE FROM THE GULF OF MEXICOD, 2016-09-29, https://edx.netl.doe.gov/dataset/the-anatomy-of-the-sulfate-methane-interface-in-a-methane-rich-core-from-the-gulf-of-mexicod
Netl Product yes
Poc Email Roy.long@netl.doe.gov
Point Of Contact Roy Long
Program Or Project KMD
Publication Date 2003-11-5