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Volumn 230, Issue 3-4, 2005, Pages 301-317

Late Pleistocene to Holocene composite speleothem 18O and 13C chronologies from South Island, New Zealand - Did a global Younger Dryas really exist?

Author keywords

Climate change; New Zealand; Palaeoclimate; Quaternary; Speleothems; Stable isotopes

Indexed keywords

ANTARCTIC COLD REVERSAL (ACR); STALAGMITES; THERMAL IONIZATION MASS SPECTROMETRY (TIMS); YOUNGER DRYAS (YD);

EID: 12744253992     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2004.10.024     Document Type: Article
Times cited : (103)

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