A human parietal fossil found at the Shuidonggou site, Ningxia, China
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概要
- 論文の詳細を見る
The morphological features of the first human parietal fossil found at the Shuidonggou site of Ningxia, China are described and compared with other specimens. Our results show that most of the features of the Shuidonggou parietal resemble those of modern humans. On the other hand, this specimen was found in situ adjacent to the erosional surface of the late Pleistocene stratum and exhibits a certain degree of fossilization. There are two features which are different from modern humans and similar to those of fossil hominids. One of the features is the strong ridges between the striae parietalis suggesting that the temporalis muscles were more developed than in modern humans. The second feature is the lack of a sigmoid sulcus at the mastoid angle of the Shuidonggou parietal which is similar to the situation seen in Homo erectus of Zhoukoudian. Given the similarities of many morphological features between late Pleistocene and modern humans, it is impossible to set the age or evolutionary status of the fossil accurately just from skeletal morphology of a fragmentary parietal. Nevertheless, taking the specimen’s fossilization and the background information of the site into consideration, we believe that the parietal likely comes from the late Pleistocene human populations that lived in this area.
- 日本人類学会の論文
- 2004-04-01
著者
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Liu W
Institute Of Vertebrate Paleontology And Paleoanthropology Chinese Academy Of Sciences
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WU XIUJIE
Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences
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WU LIU
Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences
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WANG ZHAOXIAN
Culture and Relic Office
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Liu Wu
Institute Of Vertebrate Paleontology And Paleoanthropology Chinese Academy Of Sciences
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Wu Xiujie
Institute Of Vertebrate Paleontology And Paleoanthropology Chinese Academy Of Sciences
関連論文
- A human parietal fossil found at the Shuidonggou site, Ningxia, China
- Comparisons of tooth size and morphology between the late Miocene hominoids from Lufeng and Yuanmou, China, and their implications