Lipid compositions of
sediments recovered during Ocean Drilling Program Leg 175 in the eastern South
Atlantic reflect a variety of oceanographic and climatological environments.
Most of the identified lipids can be ascribed to marine sources, notably
haptophytes, eustigmatophytes, dinoflagellates, archaea, and diatoms. Elevated
concentrations of cholesterol suggest zooplankton herbivory, characteristic for
sites influenced by upwelling. At these sites, sulfurized highly branched
isoprenoids from diatoms are also present in high amounts. Sterols, sterol
ethers, hopanoids, and midchain hydroxy fatty acids could also be detected.
Terrigenous lipids are n-alkanes,
fatty acids, n-alcohols,
and triterpenoid compounds like taraxerol and -amyrine.
n-Alkanes,
fatty acids, and n-alcohols
are derived from leaf waxes of higher land plants and transported to the sea by
airborne dust or fresh water. Triterpenoid compounds are most probably derived
from mangroves and transported solely by rivers. Lipid compositions below the
Congo low-salinity plume are strongly influenced by terrigenous material from
the Congo River. Elevated organic carbon contents and predominantly marine lipid
distributions at the Angola margin may indicate a highly productive plankton
population, probably sustained by the Angola Dome. Sedimentary lipids in the
Walvis Basin contain an upwelling signal, likely transported by the Benguela
Current. Sedimentary lipids off Lüderitz Bay and in the southern Cape Basin are
dominated by plankton lipids in high to intermediate amounts, reflecting
persistent and seasonal upwelling, respectively.
1Schefuss, E., Versteegh G.J.M, Jansen, J.H.F, and Sinninghe Damsté, J.S., 2001. Marine and terrigenous lipids in southeast Atlantic sediments (Leg 175) as paleoenvironmental indicators: initial results. In Wefer, G., Berger, W.H., and Richter, C. (Eds.), Proc. ODP, Sci. Results, 175 [Online]. Available from World Wide Web: <http://www-odp.tamu.edu/publications/175_SR/chap_10/chap_10.htm>. [Cited YYYY-MM-DD]
2Netherlands Institute for Sea Research, PO Box 59, 1790 AB Den Burg, Texel, The Netherlands. Correspondence author: schefuss@nioz.nl
3Utrecht University, Institute of Earth Sciences, PO Box 80021, 3508 TA Utrecht, The Netherlands.
Initial
receipt: 21 February 2000
Accepted: 14 September 2000
Web publication: 10 April 2001
Ms 175SR-228