作者: Xiangzhong Li , Xiangjun Liu , Yuxin He , Weiguo Liu , Xin Zhou
DOI: 10.1016/J.GLOPLACHA.2017.11.016
关键词:
摘要: Holocene climatic and environmental changes on the northeastern Tibetan Plateau (TP) have been widely discussed based on the climatic records from sedimentary cores. However, differences in the reconstructed climatic history from various studies in this region still exist, probably due to influence of climatic proxies from multiple factors and the chronological uncertainties in lacustrine sediments. Here we present records of terrestrial plant δ 13 C, soil color and total organic carbon content over the past 8400 years from a well …