Carbon and oxygen stable isotope values and microfossiis at 41.4\-4.5 ka BP in Tai Co, Tibet, China, and their paleoclimatic significance

Acta Geologica Sinica (English Edition)

Volumn 85, Issue 5, 2011, Pages 1036-1056

  Zheng, Mianping ^a   Liu, Junying ^a,b   Ma, Zhibang ^a,c   Wang, Hailei ^a   Ma, Nina ^a  

^a INSTITUTE OF MINERAL RESOURCES   (China)

^b INSTITUTE OF GEOLOGY   (China)

^c INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

Late Pleistocene Holocene (41.4 4.5 ka BP); Paleoclimatic changes; Sedimentary environment index; Tai Co; Tibet

Indexed keywords

ARIDITY; CARBON ISOTOPE; CARBONATE; CHAROPHYTE; CLAY; CLIMATE VARIATION; GASTROPOD; LAST GLACIAL MAXIMUM; MICROFOSSIL; OSTRACOD; OXYGEN ISOTOPE; PALEOCLIMATE; PALEOECOLOGY; POSTGLACIAL; STABLE ISOTOPE;

CHINA; TAIHU LAKE; XIZANG;

CHARACEAE; GASTROPODA; OSTRACODA;

EID: 84863266073     PISSN: 10009515     EISSN: 17556724     Source Type: Journal    
DOI: 10.1111/j.1755-6724.2011.00539.x     Document Type: Article

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