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作 者:WANG Yuanqing TONG Yongsheng LI Qian
出 处:《Acta Geologica Sinica(English Edition)》2011年第2期443-451,共9页地质学报(英文版)
基 金:supported by the Basic Work Program (2006FY120300-15);the Major Basic Research Projects (2006CB806400) of the Ministry of Science and Technology of China;the National Natural Science Foundation of China (40532010)
摘 要:Recent paleontological, paleomagnetic and carbon isotopic investigations have provided new evidence supporting placement of the Chinese terrestrial Paleocene-Eocene boundary at the base of the Lingcha Formation in the Hengyang Basin, Hunan Province, and within the upper part of the Nomogen Formation in the Erlian Basin, Inner Mongolia. Based on mammalian and ostracod biostratigraphic data, the boundary can also be roughly correlated with the contacts between the Baoyue and Huayong formations in the Sanshui Basin of Guangdong, the Qingjiang and Xinyu formations of Jiangxi, the Fourth Formation of the Funing Group and the Dainan Formation in northern Jiangsu, and the Dabu and Shisanjianfang formations in the Turfan Basin of Xinjiang.Recent paleontological, paleomagnetic and carbon isotopic investigations have provided new evidence supporting placement of the Chinese terrestrial Paleocene-Eocene boundary at the base of the Lingcha Formation in the Hengyang Basin, Hunan Province, and within the upper part of the Nomogen Formation in the Erlian Basin, Inner Mongolia. Based on mammalian and ostracod biostratigraphic data, the boundary can also be roughly correlated with the contacts between the Baoyue and Huayong formations in the Sanshui Basin of Guangdong, the Qingjiang and Xinyu formations of Jiangxi, the Fourth Formation of the Funing Group and the Dainan Formation in northern Jiangsu, and the Dabu and Shisanjianfang formations in the Turfan Basin of Xinjiang.
关 键 词:Vertebrate/ostracod biostratigraphy Paleocene-Eocene boundary CORRELATION Hunan Province Inner Mongolia China
分 类 号:P534.613[天文地球—古生物学与地层学] Q911.6[天文地球—地质学]
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