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Lookup NU author(s): Dr Martin Cooke,
Dr Helen Talbot,
Professor Thomas Wagner
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The transport and deposition of terrestrially derived organic matter (TOM) into the ocean is an important but poorly constrained aspect of the modern global carbon cycle. A preliminary study of Late Quaternary sediments from the Congo deep sea fan (ODP leg 175, site 1075, 2 km water depth) and four surface samples from associated cores has confirmed the presence of proposed soil-specific bacteriohopanepolyol biomarkers (BHPs) including adenosylhopane, in samples to a depth of 89 m. Concentrations of soil marker BHPs are high in the upper sediment section (to 49 m) and the closest related surface sample (4913), supporting the case for these molecular markers as novel proxies for soil organic carbon (SOC) supply via riverine transport and subsequent burial. Distinct peaks for the markers at about 21, 34 and 60 m below surface level tentatively imply that the rate of TOM discharge from tropical Africa significantly increased at these times, possibly associated with periods of reduced soil stability in the Congo catchment. © 2008 Elsevier Ltd. All rights reserved.
Author(s): Cooke MP, Talbot HM, Wagner T
Publication type: Article
Publication status: Published
Journal: Organic Geochemistry
Print publication date: 01/08/2008
ISSN (print): 0146-6380
ISSN (electronic): 1873-5290
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