HR: 0800h
AN: PP41A-0622    [Abstracts]
TI: Glacial/Interglacial Terrigenous Provenance in the Southeastern Atlantic Ocean
AU: * Latimer, J C
EM: jlatimer@indstate.edu
AF: Indiana State University, 159 Science Building, Terre Haute, IN 47809 United States
AU: Filippelli, G M
EM: gfilippe@iupui.edu
AF: Indiana Univ.-Purdue Univ. Indianapolis, 723 W. Michigan Street, Indianapolis, IN 46202 United States
AU: Hendy, I L
EM: ihendy@umich.edu
AF: University of Michigan, 2534 C.C. Little Bldg, Ann Arbor, MI 48109 United States
AU: Gleason, J D
EM: jdgleaso@umich.edu
AF: University of Michigan, 2534 C.C. Little Bldg, Ann Arbor, MI 48109 United States
AU: Blum, J D
EM: jdblum@umich.edu
AF: University of Michigan, 2534 C.C. Little Bldg, Ann Arbor, MI 48109 United States
AB: Identifying terrigenous sources in deep sea sediments may reveal temporal trends in paleo-circulation and the relative role of eolian, upwelled, and hemipelagic Fe sources to surface waters. Bulk and isotopic geochemistry of deep sea sediments recovered during Ocean Drilling Program Leg 177 in the southeastern Atlantic sector of the Southern Ocean reveal several important aspects of paleo-circulation and terrigenous provenance. The sites studied span 43-53 S and represent different oceanographic settings relative to regional hydrography and sediment type. Bulk sediment geochemistry indicates that terrigenous provenance varied considerably over the past 600 kyr. Site 1089, the northernmost site, exhibits clear glacial/interglacial variability in provenance, while provenance appears to vary irrespective of climate state at the more southerly sites (Site 1093 and 1094). Nd and Sr isotopes and Sm/Nd ratios of the terrigenous fraction indicate that study sites have geochemically distinguishable provenance. Nd and Sr isotopes further suggest that Sites 1089 and 1094 both contain detrital components that originated in South America over the past 30 kyr, however, Site 1089 is also influenced by southern African sources and the strength of the Agulhas Current. Additionally, the δNd data supports a more hemipelagic source for the terrigenous material rather than an eolian source based on comparisons with Antarctic ice core data.
DE: 1040 Radiogenic isotope geochemistry
DE: 1051 Sedimentary geochemistry
DE: 1065 Major and trace element geochemistry
SC: Paleoceanography and Paleoclimatology [PP]
MN: Fall Meeting 2005