Geographic provenance of aeolian dust in East Antarctica during Pleistocene glaciations: preliminary results from Talos Dome and comparison with East Antarctic and new Andean ice core data

Quaternary Science Reviews

Volumn 29, Issue 1-2, 2010, Pages 256-264

  Delmonte, B ^a   Andersson, P S ^b   Schoberg H ^b   Hansson, M ^c   Petit, J R ^d   Delmas, R ^d   Gaiero, D M ^e   Maggi, V ^a   Frezzotti, M ^f  

^a UNIVERSITY OF MILANO BICOCCA   (Italy)

^b SWEDISH MUSEUM OF NATURAL HISTORY   (Sweden)

^c STOCKHOLM UNIVERSITY   (Sweden)

^d UNIV GRENOBLE ALPES   (France)

^e UNIVERSIDAD NACIONAL DE CÓRDOBA   (Argentina)

^f ENEA   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

ANTARCTIC ICE CORE; ANTARCTIC PLATEAU; ANTARCTICA; ATMOSPHERIC CIRCULATION PATTERNS; CIRCULATION PATTERNS; DUST PRODUCTION; ICE CORE; ISOTOPIC COMPOSITION; ISOTOPIC DATA; ISOTOPIC SIGNATURES; LONG DISTANCES; MINERAL AEROSOLS; MINERAL PARTICLES; PATAGONIA; PLEISTOCENE; PLEISTOCENE GLACIAL; POLAR ICE CORE; QUATERNARY CLIMATE; SOURCE DATA; SOUTH AMERICA;

CLIMATOLOGY; DOMES; GLACIAL GEOLOGY; ICE; ISOTOPES; NEODYMIUM; SILICATE MINERALS; STRONTIUM; SWITCHING CIRCUITS;

DUST;

CIRCULATION; DOME; EOLIAN DEPOSIT; GLACIATION; HYPOTHESIS TESTING; ICE CORE; ISOTOPIC ANALYSIS; ISOTOPIC COMPOSITION; LAST INTERGLACIAL; PROVENANCE; RUBIDIUM-STRONTIUM DATING; SEDIMENT TRANSPORT;

ANTARCTICA; EAST ANTARCTICA; PATAGONIA;

EID: 73549116307     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2009.05.010     Document Type: Article

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