Molecular isotopic tracing of carbon flow and trophic relationships in a methane‐supported benthic microbial community

By J. Werne, M. Baas, J. S. Sinninghe Damsté. 2002

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A Microbial Mat of a Large Sulfur Bacterium Preserved in a Miocene Methane-Seep Limestone (2004, background): “Their distribution, mass spectra and retention characteristics indicate that they comprise fossil counterparts of DAGE identified by Pancost et al. (2001, series II) and Werne et al. (2002) in modern methane-rich sediments from Eastern Mediterranean mud volcanoes.”
ECOLOGY OF COLD SEEP SEDIMENTS: INTERACTIONS OF FAUNA WITH FLOW, CHEMISTRY AND MICROBES (2005, background): “Werne et al. (2002) present molecular isotopic evidence that bacterivorous ciliates are feeding primarily on methane-derived carbon from archaea and bacteria at the Kazam mud volcano in the Mediterranean Sea, based largely on the isotopic signatures of tetrahymenol, a lipid biomarker produced by…”
Characterization of Specific Membrane Fatty Acids as Chemotaxonomic Markers for Sulfate-Reducing Bacteria Involved in Anaerobic Oxidation of Methane (2003, background): “This feature enables the evaluation of the activity of specific microbial populations involved in AOM and carbon flow further on into the benthic community (Levin and Michener 2002; Werne et al. 2002).”