首页|期刊导航|地质学报(英文版)|High-Resolution Records of the Holocene Paleoenvironmental Variation Reflected by Carbonate and Its Isotopic Compositions in Bosten Lake and Response to Glacial Activities

High-Resolution Records of the Holocene Paleoenvironmental Variation Reflected by Carbonate and Its Isotopic Compositions in Bosten Lake and Response to Glacial ActivitiesOA

High-Resolution Records of the Holocene Paleoenvironmental Variation Reflected by Carbonate and Its Isotopic Compositions in Bosten Lake and Response to Glacial Activities

英文摘要

The Early Holocene paleoclimate in Bosten Lake on the northern margin of the Tarim Basin, southern Xinjiang, is reconstructed through an analysis of a 953 cm long core (BSTC2000) taken from Bosten Lake. Multiple proxies of this core, including the mineral components of carbonate, carbonate content, stable isotopic compositions of carbonate, Ca/Sr, TOC and C/N and C/S of organic matter, are used to reconstruct the climatic change since 8500 a B.P. The chronol…查看全部>>

ZHANG Chengjun;ZHENG Mianping;Alexander PROKOPENKO;Steffen MISCHKE;GOU Xiaohui;YANG Qili;ZHANG Wanyi;FENG Zhaodong

School of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, Gansu, ChinaCenter of Saline Lake and Epithermal Deposit, Chinese Academy of Geological Sciences, Beijing 100037, ChinaCenter of Saline Lake and Epithermal Deposit, Chinese Academy of Geological Sciences, Beijing 100037, ChinaUniversity of South Carolina, Columbia, SC, 29205, USAFreie University Berlin, Berlin, 12249, GermanySchool of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, Gansu, ChinaSchool of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, Gansu, ChinaSchool of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, Gansu, China

地质学

carbonate isotopic composition glacial activity paleoenvironmental variation Bosten Lake

carbonate isotopic composition glacial activity paleoenvironmental variation Bosten Lake

《地质学报(英文版)》 2009 (6)

1101-1115,15

This work was co-supported by the National Natural Science Foundation of China (grant Nos. 40773064, 40331012 and 40041004) and "973" Program of China (No. G1999043501).

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