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Evidence for anaerobic methane oxidation by archaea in euxinic waters of the Black Sea

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Evidence for anaerobic methane oxidation by archaea in euxinic waters of the Black Sea (English)

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Jaap Sinninghe Damsté

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Jaap S.Sinninghe Damsté

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3

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Stefan Schouten

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1

object named as

Stefan Schouten

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Stuart G. Wakeham

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2

object named as

Stuart G Wakeham

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publication date

October 2001

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published in

Organic Geochemistry

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volume

32

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issue

10

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page(s)

1277-1281

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cites work

A marine microbial consortium apparently mediating anaerobic oxidation of methane

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Biogeochemical aspects of atmospheric methane

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Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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Predictive isotopic biogeochemistry: hydrocarbons from anoxic marine basins

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

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Methane-consuming archaebacteria in marine sediments

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Ether lipids of planktonic archaea in the marine water column

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Archaeal dominance in the mesopelagic zone of the Pacific Ocean

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Massive expansion of marine archaea during a mid-Cretaceous oceanic anoxic event

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Carbon cycling and chronology of climate warming during the Palaeocene/Eocene transition

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Biomarker evidence for widespread anaerobic methane oxidation in Mediterranean sediments by a consortium of methanogenic archaea and bacteria. The Medinaut Shipboard Scientific Party

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Archaeal lipids in Mediterranean cold seeps: molecular proxies for anaerobic methane oxidation

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Structural characterization, occurrence and fate of archaeal ether-bound acyclic and cyclic biphytanes and corresponding diols in sediments

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Widespread occurrence of structurally diverse tetraether membrane lipids: evidence for the ubiquitous presence of low-temperature relatives of hyperthermophiles

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Effects of an oceanic anoxic event on the stable carbon isotopic composition of early Toarcian carbon

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Dibiphytanyl ether lipids in nonthermophilic crenarchaeotes

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10.1016/S0146-6380(01)00110-3

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(Q63972075)

Evidence for anaerobic methane oxidation by archaea in euxinic waters of the Black Sea

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