4.7 Article

Hydrogen-isotopic variability in lipids from Santa Barbara Basin sediments

Journal

GEOCHIMICA ET COSMOCHIMICA ACTA
Volume 73, Issue 16, Pages 4803-4823

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2009.05.056

Keywords

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Funding

  1. National Science Foundation [EAR-0311824]

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We conducted an extensive survey of hydrogen-isotopic compositions (D/H ratios) of diverse sedimentary lipids from the Santa Barbara Basin (SBB), offshore southern California. The main goal of this Survey was to assess the diversity of D/H ratios in lipids from marine sediments, in order to provide a more detailed understanding of relevant biological and geochemical factors impacting lipid isotopic variability. A total of 1182 individual delta D values are reported from two stations in SBB, one located in the suboxic basin depocenter and the other on the fully oxic flank of the basin. Sediments collected from the basin depocenter span a depth of similar to 2.5 m and reach the methanogervic zone. Lipids that were analyzed include n-alkanes, n-alkanols and alkenols, short- and long-chain fatty acids, linear isoprenoids, steroids, and hopanoids, and exhibit several systematic patterns. First, there are no significant differences in delta D values between the two sampling locations, nor with increasing depth for most lipids, indicating that degradation does not influence sedimentary lipid delta D values. Second, relatively large differences in delta D values among differing molecular structures are observed in all samples. n-Alkyl lipids of probable marine origin have typical delta D values between -150 and -200%omicron, those from terrestrial leaf waxes and aquatic plants range from -80 to -170%omicron, while petroleum n-alkanes are typically -90 to -150%omicron. Third, lipids inferred to derive from bacteria (branched fatty acids and hopanols) living at the sediment surface or in the water column tend to be D-enriched relative to similar algal products by 30%omicron or more. At the same time, several other lipids have delta D values that decrease strongly with depth, presumably as a result of in situ production by anaerobic bacteria. This dichotomy in isotopic compositions of bacterial lipids is inconsistent with a nearly constant D/H fractionation during lipid biosynthesis, and likely reflects significant variations associated with metabolism. (C) 2009 Elsevier Ltd. All rights reserved.

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