Open AccessOrganic matter in river‐influenced continental margin sediments: The land‐ocean and climate linkage at the Late Quaternary Congo fan (ODP Site 1075)
Author(s) -
Holtvoeth Jens,
Wagner Thomas,
Schubert Carsten J.
Publication year - 2003
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2003gc000590
Subject(s) - terrigenous sediment , geology , upwelling , organic matter , total organic carbon , fluvial , oceanography , geochemistry , sedimentary rock , environmental chemistry , paleontology , ecology , chemistry , structural basin , biology
Late Quaternary sections (1.2 Ma) of ODP‐Site 1075 from the Congo deep‐sea fan are investigated to reconstruct variations of terrigenous organic matter supply to the eastern equatorial Atlantic. To characterize the organic matter (OM) with regard to marine and terrigenous amounts we used elemental analysis (C, N, S), stable carbon isotopes (bulk δ 13 C org ), Rock‐Eval pyrolysis, and terrigenous biomarkers (lignin phenols from CuO oxidation). The records of total organic carbon (TOC) contents, C org /N tot ratios, bulk OM degradation rates (C org /C org *), and the ratios of hydrocarbons (HC) from low‐mature versus HC from high‐mature OM (lm/hm) reveal pronounced cyclic changes in OM abundance, preservation, and reactivity that are closely related to the precessional controlled record of insolation, and thus, to variations in upwelling intensity and fluvial run‐off. Primary productivity off the Congo is stimulated by both, enhanced nutrient supply in response to trade‐induced upwelling during arid African climates (insolation minima) and fluvial nutrient delivery during humid stages (following insolation maxima), especially due to the contribution of dissolved silica that is taken up preferably by diatoms. However, results stemming from a multiparameter approach reveal that the fluvial supply of degraded OM and black carbon (BC) associated with fine‐grained sediments from soil erosion is a decisive factor for the preservation of marine OM and, in addition, significantly influences the geochemical signature of bulk and terrigenous OM. Riverine and eolian supply of C 4 plant matter, as well as enhanced concentrations of BC, during arid and arid‐to‐humid transitional climate stages, may lead to a severe underestimation of terrigenous organic carbon, if its amount is calculated from bulk isotopic ratios using binary end‐member models. During the humid stages, it is the massive supply of 13 C‐enriched soil OM with low C org /N tot ratios that may suggest a mainly marine composition of bulk OM. In fact, terrigenous OM governs bulk OM geochemical signatures in the sediments of the Congo deep‐sea fan, a result that is contradictory to earlier studies, especially to the conventional interpretation of the bulk δ 13 C org signal.