Abstract
A new archaeal lipid biomarker, C-20,C-25 sn-2, C-7 hydroxy isoprenoid glycerol diether, has been identified in methane-related carbonates from six methane seep locations. The molecular structure resembles that of sn-2 hydroxyarchaeol but the hydroxy group-bearing moiety at the sn-2 position comprises a regular C-25 instead of a C-20 isoprenoid chain. Compound specific stable carbon isotope measurements revealed delta C-13 values ranging from -96%, to -129%, which are similar to delta C-13 Values of sn-2 hydroxyarchaeol. This supports the origin of the novel compound from archaea involved in the anaerobic oxidation of methane. it also suggests a common source, i.e. archaea within the ANME-2 group, which is consistent with the previously reported 16S rDNA data for the same samples. The frequent appearance of the novel sn-2 isoprenoidal hydroxy glycerol diether in cold seepage sediments with high salinity environments, and its distinct Structural similarities with membrane lipids of halophilic and methanogenic microbes, suggests that ANME-2 methanotrophic archaea thriving at elevated salinity are the possible biological source for this specific lipid. (c) 2008 Elsevier Ltd. All rights reserved.
Original language | English |
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Pages (from-to) | 1007-1014 |
Number of pages | 8 |
Journal | Organic Geochemistry |
Volume | 39 |
Issue number | 8 |
DOIs | |
Publication status | Published - Aug 2008 |
Event | 23rd International Meeting on Organic Geochemistry - Torquay Duration: 9 Sept 2007 → 14 Sept 2007 |
Keywords
- Farnesylgeranyl diphosphate synthase
- Mediterranean mud volcanos
- Sulfate-reducing bacteria
- Methane oxidation
- Carbonate crusts
- Black-sea
- Marine-sediments
- Polar lipids
- Hyperthermophilic archaeon
- Aeropyrum-pernix