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• W1931377114 endingPage "2458" @default.
• W1931377114 startingPage "2441" @default.
• W1931377114 abstract "Summary The anoxic sediments of the W hite O ak R iver estuary comprise a distinctive sulfate–methane transition zone ( SMTZ ) and natural enrichment of the archaea affiliated with the M iscellaneous C renarchaeotal G roup ( MCG ). Archaeal biphytanes were generally depleted in 13 C , with δ 13 C values being less than –35‰, indicative of production by active sedimentary archaeal populations. Multivariate analysis of the downcore distributions of 63 lipid biomarkers identified three major groups of lipids that were enriched in the surface, SMTZ or subsurface depths. Intact polar lipids with phosphatidylglycerol headgroups and glycerol dibiphytanyl glycerol tetraethers containing one, two or three cyclopentane rings were enriched at the base of the SMTZ and likely represent the accumulated product of a small but active ANME ‐1 community. The recently identified butanetriol dibiphytanyl glycerol tetraethers ( BDGT ), which increased relatively to other lipids with depth, were correlated with the relative abundance of MCG in archaeal 16 S rRNA clone libraries, and were 13 C depleted throughout the depth profile, suggesting BDGT lipids as putative biomarkers of an MCG community that may either be autotrophic or feeding on 13 C ‐depleted organic substrates transported by porewater." @default.
• W1931377114 created "2016-06-24" @default.
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• W1931377114 date "2015-02-11" @default.
• W1931377114 modified "2023-09-27" @default.
• W1931377114 title "The archaeal lipidome in estuarine sediment dominated by members of the Miscellaneous Crenarchaeotal Group" @default.
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• W1931377114 doi "https://doi.org/10.1111/1462-2920.12716" @default.
• W1931377114 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/25403417" @default.
• W1931377114 hasPublicationYear "2015" @default.
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