Biomarker and 16S rDNA evidence for anaerobic oxidation of methane and related carbonate precipitation in deep-sea mud volcanoes of the Sorokin Trough, Black Sea

Author:

Stadnitskaia A.,Muyzer G.,Abbas B.,Coolen M.J.L.,Hopmans E.C.,Baas M.,van Weering T.C.E.,Ivanov M.K.,Poludetkina E.,Sinninghe Damsté J.S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference102 articles.

1. Methane-related authigenic carbonates of eastern Mediterranean Sea mud volcanoes and their possible relation to gas hydrate destabilization;Aloisi;Earth Planet. Sci. Lett.,2000

2. CH4-consuming microorganisms and the formation of carbonate crusts at cold seeps;Aloisi;Earth Planet. Sci. Lett.,2002

3. Geochemical observations supporting anaerobic methane oxidation;Alperin,1984

4. Inhibition experiments on anoxic marine sediments suggests methane is not directly oxidized by sulfate-reducing bacteria;Alperin,1985

5. Methane production and consumption in anoxic marine sediments;Barnes;Geology,1976

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