In the past years we carried out further stratigraphy division in field and it is found that rich stone artifacts can be found in fluvial-shallow lake-alluvial sediments on the terrace Ⅱ of Biangou River, in Shuidong...In the past years we carried out further stratigraphy division in field and it is found that rich stone artifacts can be found in fluvial-shallow lake-alluvial sediments on the terrace Ⅱ of Biangou River, in Shuidonggou site, Ningxia and they are SDG1, 2 and 7. More luminescence and AMS 14C dating in laboratory show that Paleolithic culture develops during the Upper Paleolithic period with ages of 35―20 ka. The Paleolithic culture of SDG 1 is a little earlier than that of SDG 2 similar to SDG 7. The sandy sediments on terrace Ⅱ of Biangou River deposits in the past 72―18 ka, corresponding to Last Glacial. SDG2 has a stable sedimentary environment, resulting in the continuous stratigraphy, thickest deposits and rich environment and culture information, which can be regarded as the important and classic paleoanthropological section of Late Pleistocene in this region.展开更多
Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains,animal fossils,abundant sporopollen and unique geological sequence,it is the type site for Lat...Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains,animal fossils,abundant sporopollen and unique geological sequence,it is the type site for Late Pleistocene to Holocene human occupation and environmental change in the Ningxia-Inner Mongolia region. Many scholars suggest that the site should be named the "Shuidong-gou Formation" of Late Pleistocene in North China. Dating results indicate that ancient human activities at the site took place 30―24 ka (Marine Isotope Stage MIS 3). The climate at that time was warmer and moister than present day,and adequate precipitation led to the formation of water pack depressions where broad-leaf trees and sparse forest vegetations,as well as herbivorous animals flourished,mak-ing the area suitable for early human hunting,gathering and survival. The Neolithic human occupation happened 9―5 ka at the site,while similar environmental conditions with MIS3 occurred. The absence of human activity record in the region during the Last Glacial Maximum (MIS2) suggests that the envi-ronment was too harsh for humans to live there.展开更多
基金Supported by the National Basic Research Program of China(Grant No. 2006CB806400)Basic Scientific Special Program of MST of China (Grant No. 2007FY110200)National Natural Science Foundation of China (Grant No. 40602020)
文摘In the past years we carried out further stratigraphy division in field and it is found that rich stone artifacts can be found in fluvial-shallow lake-alluvial sediments on the terrace Ⅱ of Biangou River, in Shuidonggou site, Ningxia and they are SDG1, 2 and 7. More luminescence and AMS 14C dating in laboratory show that Paleolithic culture develops during the Upper Paleolithic period with ages of 35―20 ka. The Paleolithic culture of SDG 1 is a little earlier than that of SDG 2 similar to SDG 7. The sandy sediments on terrace Ⅱ of Biangou River deposits in the past 72―18 ka, corresponding to Last Glacial. SDG2 has a stable sedimentary environment, resulting in the continuous stratigraphy, thickest deposits and rich environment and culture information, which can be regarded as the important and classic paleoanthropological section of Late Pleistocene in this region.
基金the Major Basic Research Projects (Grant No. 2006CB806400) of MST of Chinathe National Natural Science Foundation of China-General Program (Grant No. 40472016)
文摘Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains,animal fossils,abundant sporopollen and unique geological sequence,it is the type site for Late Pleistocene to Holocene human occupation and environmental change in the Ningxia-Inner Mongolia region. Many scholars suggest that the site should be named the "Shuidong-gou Formation" of Late Pleistocene in North China. Dating results indicate that ancient human activities at the site took place 30―24 ka (Marine Isotope Stage MIS 3). The climate at that time was warmer and moister than present day,and adequate precipitation led to the formation of water pack depressions where broad-leaf trees and sparse forest vegetations,as well as herbivorous animals flourished,mak-ing the area suitable for early human hunting,gathering and survival. The Neolithic human occupation happened 9―5 ka at the site,while similar environmental conditions with MIS3 occurred. The absence of human activity record in the region during the Last Glacial Maximum (MIS2) suggests that the envi-ronment was too harsh for humans to live there.
