Carbon and oxygen isotope records and paleoclimate reconstruction (140-250 ka B.P.) from a stalagmite of Shuinan Cave, Guilin, China

The time sequence of paleoclimatic changes from 245.2 to 147.9 ka B.P. has been established by high precision U-series dating by Thermal Ionization Mass Spectrometry and the analysis of the oxygen isotopes from a stalagmite of Shuinan Cave in Guilin. The oxygen isotope pattern is divided into three...

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Veröffentlicht in:	Environmental earth sciences 2006-03, Vol.49 (5), p.752-764
Hauptverfasser:	Meiliang, Zhang, Hai, Cheng, DaoXian, Yuan, Xiaoyan, Zhu, Yushi, Lin, Jiaming, Qin, Edwards, R. L
Format:	Artikel
Sprache:	eng
Schlagworte:	Carbon isotopes Climate change Climate studies Climate system Earth sciences Earth, ocean, space Exact sciences and technology Geochronology Guilin, China Ionization Isotope geochemistry. Geochronology Isotope records Isotopes Marine and continental quaternary Mass spectrometry Oxygen isotopes Palaeo-climate reconstruction Paleoclimate Pleistocene Shuinan Cave Stalagmite Surficial geology TIMS-U series ages
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