Greater supply of Patagonian-sourced detritus and transport by the ACC to the Atlantic sector of the Southern Ocean during the last glacial period

被引:35
作者
Noble, Taryn L. [1 ]
Piotrowski, Alexander M. [1 ]
Robinson, Laura F. [2 ]
McManus, Jerry F. [3 ]
Hillenbrand, Claus-Dieter [4 ]
Bory, Aloys J. -M.
机构
[1] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England
[2] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA
[3] Columbia Univ, Lamont Doherty Earth Observ, Dept Earth & Environm Sci, Palisades, NY 10964 USA
[4] British Antarctic Survey, Cambridge CB3 0ET, England
关键词
radiogenic isotopes; detritus; flux; provenance; Patagonia; Southern Ocean; LATE QUATERNARY; ANTARCTIC PENINSULA; SEDIMENT REDISTRIBUTION; TERRIGENOUS SEDIMENT; GRAIN-SIZE; ICE-CORE; DEEP-SEA; DOME-C; ISOTOPIC CONSTRAINTS; EQUATORIAL PACIFIC;
D O I
10.1016/j.epsl.2011.10.007
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Reconstructing past detrital flux and provenance in the Southern Ocean provides information about changes in source regions associated with climate variations and transport pathways. We present a Last Glacial Maximum (LGM) to Holocene comparison of Th-230 normalised fluxes combined with sediment provenance data (Pb, Nd and Sr isotopes) from a latitudinal core transect in the eastern Atlantic sector of the Southern Ocean (ODP Leg 177 cores). We compare the radiogenic isotopic composition (IC) of detritus in these cores to that of cores proximal to potential source areas. We observe a well-defined latitudinal Holocene gradient in both detrital flux and provenance of sediment. High detrital fluxes in the north are associated with terrigenous material derived from southern Africa, while low detrital fluxes in the south are associated with supply from southern South America, West Antarctica and the South Sandwich Islands. The data suggest that this well-defined Holocene gradient in detrital flux and sediment provenance is controlled by the flow of the Antarctic Circumpolar Current (ACC) and the position of its frontal zones. The LGM is characterised by 2 to 6 times higher than modem detrital fluxes at most ODP Leg 177 sites. The LGM detrital fluxes do not show a latitudinal trend and suggest a greater supply of glaciogenic detritus sourced from southern South America. Glacial Patagonian outwash sediments (<5 mu m fraction) were analysed and compared to the bulk compositions of the marine sediments. The Pb IC of the Patagonian sediments is very similar to the glacial IC of sediments in the Scotia Sea and at similar to 49 degrees S latitude in the eastern Atlantic sector. We propose that the glacial IC of sediments is controlled by increased delivery of Patagonian detritus initially supplied by glaciers and then transported at depth via the ACC. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:374 / 385
页数:12
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