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作 者:LIU Dengke SUN Xuefeng HU Xuzhi YI Liang GUO Xiaoqi WANG Yichao WANG Shejiang LU Huayu 刘登科;孙雪峰;胡旭芝;易亮;郭小奇;王逸超;王社江;鹿化煜(School of Geography and Ocean Science,Nanjing University,Nanjing 210023,China;School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,China;State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China;Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences,Institute of Vertebrate Paleontology and Paleoanthropology,CAS,Beijing 100044,China;CAS Center for Excellence in Life and Paleoenvironment,Beijing 100044,China)
机构地区:[1]School of Geography and Ocean Science,Nanjing University,Nanjing 210023,China [2]School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,China [3]State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China [4]Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences,Institute of Vertebrate Paleontology and Paleoanthropology,CAS,Beijing 100044,China [5]CAS Center for Excellence in Life and Paleoenvironment,Beijing 100044,China
出 处:《Journal of Geographical Sciences》2022年第2期358-374,共17页地理学报(英文版)
基 金:National Social Science Foundation of China,No.19ZDA225;National Natural Science Foundation of China,No.41972185;The Project of Zhengzhou University,No.XKZDJC202006。
摘 要:The Qinling Mountain Range(QMR)spans a large region in China and is an important area of hominin activities.Many Paleolithic sites are found in Bahe,South Luohe,and Hanjiang river valleys in the northern,eastern,and southern part of the range,respectively.The Danjiang River valley acts as a channel connecting these valleys and stretches from the north to the south of the QMR.The previous dating of the Paleolithic sites in the Danjiang valley mainly relied on geomorphologic comparison,stratigraphic correlation,fossil characteristics,and Paleolithic artifacts,indicating a lack of absolute data.In this study,we conducted a detailed geochronological investigation of the entire valley,and selected an ideal site—the Miaokou profile.Based on the identification of the loess-paleosol sequences,optically stimulated luminescence,and magnetostratigraphy,the Paleolithic artifacts of the Miaokou site located within the S5 and S6 layers of the profile belong to~0.6-0.7 Ma.This suggests that the Paleolithic site is an old site in the Danjiang River valley,and this period also witnessed a rapid increase in the number of hominin sites during the Middle Pleistocene.Combining our results with previous reports across the QMR,we propose that the Danjiang River valley might have been a corridor for hominin migration,and is worthy of further investigation.
关 键 词:Danjiang River valley Miaokou site loess-paleosol sequence MAGNETOSTRATIGRAPHY hominin routeway
分 类 号:P534.631[天文地球—第四纪地质学] Q981[天文地球—古生物学与地层学]
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