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

Earth and Planetary Science Letters

Volumn 317-318, Issue , 2012, Pages 374-385

  Noble, Taryn L ^a,e   Piotrowski, Alexander M ^a   Robinson, Laura F ^b,f   McManus, Jerry F ^c   Hillenbrand, Claus Dieter ^d   Bory, Aloys J M ^c,g  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c Department of Earth and Environmental Sciences   (United States)

^d BRITISH ANTARCTIC SURVEY   (United Kingdom)

^e UNIVERSITY OF TASMANIA   (Australia)

^f UNIVERSITY OF BRISTOL   (United Kingdom)

^g UNIV LILLE   (France)

Author keywords

Detritus; Flux; Patagonia; Provenance; Radiogenic isotopes; Southern Ocean

Indexed keywords

DETRITUS; PATAGONIA; PROVENANCE; RADIOGENIC ISOTOPES; SOUTHERN OCEAN;

FLUXES; GLACIAL GEOLOGY; ISOTOPES; LEAD; OCEAN CURRENTS; SEDIMENTOLOGY; STRONTIUM; SUBMARINE GEOLOGY;

ANOXIC SEDIMENTS;

CLIMATE VARIATION; DETRITUS; HOLOCENE; ISOTOPIC COMPOSITION; LAST GLACIAL MAXIMUM; LEAD ISOTOPE; MARINE SEDIMENT; NEODYMIUM ISOTOPE; OCEAN DRILLING PROGRAM; POINT SOURCE; PROVENANCE; RECONSTRUCTION; SEDIMENT CHEMISTRY; SEDIMENT TRANSPORT; STRONTIUM ISOTOPE;

ANTARCTIC CIRCUMPOLAR CURRENT; PATAGONIA; SOUTHERN OCEAN;

EID: 84855426310     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.10.007     Document Type: Article

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