Deglacial dust provenance changes in the Eastern Equatorial Pacific and implications for ITCZ movement

Earth and Planetary Science Letters

Volumn 317-318, Issue , 2012, Pages 386-395

  Xie, Ruifang C ^a   Marcantonio, Franco ^a  

^a TEXAS A AND M UNIVERSITY   (United States)

Author keywords

Dust provenance; Eastern equatorial Pacific Ocean; ITCZ; Last deglaciation; Sr, Nd, Pb isotopes

Indexed keywords

ATMOSPHERIC CIRCULATION; AUSTRALIA; DEEP SEA SEDIMENT; DEGLACIAL; DUST SOURCES; EASTERN EQUATORIAL PACIFIC; EOLIAN DUST; HOLOCENES; INTERTROPICAL CONVERGENCE ZONE; ISOTOPIC FINGERPRINTING; ITCZ; LAST DEGLACIATION; LAST GLACIAL; LAST GLACIAL PERIOD; ND ISOTOPES; PB ISOTOPES; RADIOGENIC VALUES; SOUTHERN HEMISPHERE; SR ISOTOPE RATIO; TEMPORAL CHANGE;

ANOXIC SEDIMENTS; BARITE; CLIMATOLOGY; DUST; GLACIAL GEOLOGY; ISOTOPES; LEAD; NEODYMIUM; SOURCE SEPARATION;

STRONTIUM;

ATMOSPHERIC CIRCULATION; DEGLACIATION; DEPOSITIONAL ENVIRONMENT; DUST; EOLIAN DEPOSIT; HOLOCENE; INTERTROPICAL CONVERGENCE ZONE; ISOTOPIC RATIO; LAST GLACIATION; LEAD ISOTOPE; NEODYMIUM ISOTOPE; PALEOATMOSPHERE; PALEOENVIRONMENT; POINT SOURCE; PROVENANCE; SEDIMENT TRANSPORT; STRONTIUM ISOTOPE; TREND ANALYSIS; UPWELLING;

PACIFIC OCEAN; PACIFIC OCEAN (EQUATORIAL);

EID: 84855467960     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.11.014     Document Type: Article

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