KMS Institute of Vertebrate Paleontology and Paleoanthropology
Paleomagnetic age and palaeobiological significance of hominoid fossil strata of Yuanmou Basin in Yunnan | |
Yue, LP; Zhang, YX; Qi, GQ; Heller, FA; Wang, JQ; Yang, LR; Zhang, R; Yue, LP (reprint author), Northwest Univ, Ley Lab Continental Dynam, Minist Educ China, Dept Geol, Xian 710069, Peoples R China. | |
2004-05-01 | |
发表期刊 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES |
ISSN | 1006-9313 |
卷号 | 47期号:5页码:405-411 |
文章类型 | Article |
摘要 | The two sections containing hominoid fossils in the Yuanmou Basin, Yunnan Province have been studied by means of magnetostratigraphy. The results are as follows. The Xiaohe section records over 8 polarity zones corresponding to Cande-Kent95 time scale, including C3Br.1n, C3Br.1r, C3Br.2n, C3Br.2r, C4n.1n, C4n.1r, C4n.2n and C4n.2r, attaching to Late Miocene. This section comprises two layers of hominoid fossils: the lower layer (the 1st layer in fig. 4) which records the lower portion of C4n.2r with paleornagnetic age of 8.20-8.10 Ma and the upper layer (the 16th layer in fig. 4) which records C3Br.1r with paleornagnetic age of 7.20-7.15 Ma. So the age of hominoid fossils in the Xiaohe section is about 8.20-7.15 Ma. The Leilao section records over 11 polarity zones corresponding to Cande-Kent95 time scale, including C3Br, C3Br.1n, C3Br.1r, C3Br.2n, C3Br.2r, C4n.1n, C4n.1r, C4n.2n, C4n.2r, C4n.3n and C4n.3r, attaching to Late Miocene. This section also consists of two layers of hominoid fossils: the lower layer (the 3rd layer in fig. 3) which records C4n.2r with the age of 8.20-8.10 Ma and the upper layer(the 19th layer in fig. 3) which records the middle portion of C3Br with the age of 7.15-7.1 Ma. So the age of hominoid fossils in the Leilao section is about 8.20-7.10 Ma. Sedimentary environments reflected in both sections are extremely similar, and the ages of hominoid fossils are of correspondency. The age of the lower and upper fossil layers is 8.20-8.10 Ma and 7.20-7.10 Ma respectively, which probably imply that hominoids living in Xiaohe and Leilao basins have uniform activity areas. There were hominoids activities all along during 8.00-7.00 MaBP in this field.; The two sections containing hominoid fossils in the Yuanmou Basin, Yunnan Province have been studied by means of magnetostratigraphy. The results are as follows. The Xiaohe section records over 8 polarity zones corresponding to Cande-Kent95 time scale, including C3Br.1n, C3Br.1r, C3Br.2n, C3Br.2r, C4n.1n, C4n.1r, C4n.2n and C4n.2r, attaching to Late Miocene. This section comprises two layers of hominoid fossils: the lower layer (the 1st layer in fig. 4) which records the lower portion of C4n.2r with paleornagnetic age of 8.20-8.10 Ma and the upper layer (the 16th layer in fig. 4) which records C3Br.1r with paleornagnetic age of 7.20-7.15 Ma. So the age of hominoid fossils in the Xiaohe section is about 8.20-7.15 Ma. The Leilao section records over 11 polarity zones corresponding to Cande-Kent95 time scale, including C3Br, C3Br.1n, C3Br.1r, C3Br.2n, C3Br.2r, C4n.1n, C4n.1r, C4n.2n, C4n.2r, C4n.3n and C4n.3r, attaching to Late Miocene. This section also consists of two layers of hominoid fossils: the lower layer (the 3rd layer in fig. 3) which records C4n.2r with the age of 8.20-8.10 Ma and the upper layer(the 19th layer in fig. 3) which records the middle portion of C3Br with the age of 7.15-7.1 Ma. So the age of hominoid fossils in the Leilao section is about 8.20-7.10 Ma. Sedimentary environments reflected in both sections are extremely similar, and the ages of hominoid fossils are of correspondency. The age of the lower and upper fossil layers is 8.20-8.10 Ma and 7.20-7.10 Ma respectively, which probably imply that hominoids living in Xiaohe and Leilao basins have uniform activity areas. There were hominoids activities all along during 8.00-7.00 MaBP in this field. |
关键词 | Yuanmou Basin Hominoid Paleomagnetism Chronology |
WOS标题词 | Science & Technology ; Physical Sciences |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000222583800003 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.205/handle/311034/3657 |
专题 | 中科院古脊椎所(2000年以后) |
通讯作者 | Yue, LP (reprint author), Northwest Univ, Ley Lab Continental Dynam, Minist Educ China, Dept Geol, Xian 710069, Peoples R China. |
作者单位 | 1.Northwest Univ, Ley Lab Continental Dynam, Minist Educ China, Dept Geol, Xian 710069, Peoples R China 2.Chinese Acad Sci, State Key Lab Loess & Quanternary Geol, Inst Earth Environm, Xian 710075, Peoples R China 3.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 4.ETH, Inst Geophys, CH-8093 Zurich, Switzerland |
推荐引用方式 GB/T 7714 | Yue, LP,Zhang, YX,Qi, GQ,et al. Paleomagnetic age and palaeobiological significance of hominoid fossil strata of Yuanmou Basin in Yunnan[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2004,47(5):405-411. |
APA | Yue, LP.,Zhang, YX.,Qi, GQ.,Heller, FA.,Wang, JQ.,...&Yue, LP .(2004).Paleomagnetic age and palaeobiological significance of hominoid fossil strata of Yuanmou Basin in Yunnan.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,47(5),405-411. |
MLA | Yue, LP,et al."Paleomagnetic age and palaeobiological significance of hominoid fossil strata of Yuanmou Basin in Yunnan".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 47.5(2004):405-411. |
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