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Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas
Deng, Tao; Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
2006
发表期刊GEODIVERSITAS
ISSN1280-9659
卷号28期号:3页码:499-516
文章类型Article
摘要Both China and Greece have abundant fossils of the late Miocene Hipparion fauna. The habitat of the Hipparion fauna in Greece was a sclerophyllous evergreen woodland. The Chinese late Miocene Hipparion fauna is represented respectively in the Guonigou fauna (MN 9), the Dashengou fauna (MN 10), and the Yangjiashan fauna (MN 11) from Linxia, Gansu, and the Baode fauna (MN 12) from Baode, Shanxi. According to the evidence from lithology, carbon isotopes, paleobotany, taxonomic framework, mammalian diversity and faunal similarity, the paleoenvironment of the Hipparion fauna in China was a subarid open steppe, which is different from that of Greece. The red clay bearing the Hipparion fauna in China is windblown in origin, i.e. eolian deposits. Stable carbon isotopes from tooth enamel and paleosols indicate that C-3 plants dominated the vegetation during the late Miocene in China. Pollens of xerophilous and sub-xerophilous grasses show a signal of steppe or dry grassland. Forest mammals, such as primates and chalicotheres, are absent or scarce, but grassland mammals, such as horses and rhinoceroses, are abundant in the Chinese Hipparion fauna. The species richness of China and Greece exhibits a similar trend with a clear increase from MN 9 to MN 12, but the two regions have low similarities at the species level. The entry of Hipparion led to a comparable radiation in China and Greece, but their dietary evolution is different. In conclusion, the ecosystems of the Chinese and Greek Hipparion faunas have an obvious dissimilarity in the late Miocene.; Both China and Greece have abundant fossils of the late Miocene Hipparion fauna. The habitat of the Hipparion fauna in Greece was a sclerophyllous evergreen woodland. The Chinese late Miocene Hipparion fauna is represented respectively in the Guonigou fauna (MN 9), the Dashengou fauna (MN 10), and the Yangjiashan fauna (MN 11) from Linxia, Gansu, and the Baode fauna (MN 12) from Baode, Shanxi. According to the evidence from lithology, carbon isotopes, paleobotany, taxonomic framework, mammalian diversity and faunal similarity, the paleoenvironment of the Hipparion fauna in China was a subarid open steppe, which is different from that of Greece. The red clay bearing the Hipparion fauna in China is windblown in origin, i.e. eolian deposits. Stable carbon isotopes from tooth enamel and paleosols indicate that C-3 plants dominated the vegetation during the late Miocene in China. Pollens of xerophilous and sub-xerophilous grasses show a signal of steppe or dry grassland. Forest mammals, such as primates and chalicotheres, are absent or scarce, but grassland mammals, such as horses and rhinoceroses, are abundant in the Chinese Hipparion fauna. The species richness of China and Greece exhibits a similar trend with a clear increase from MN 9 to MN 12, but the two regions have low similarities at the species level. The entry of Hipparion led to a comparable radiation in China and Greece, but their dietary evolution is different. In conclusion, the ecosystems of the Chinese and Greek Hipparion faunas have an obvious dissimilarity in the late Miocene.
关键词Hipparion Fauna Late Miocene Paleoecology China Greece
WOS标题词Science & Technology ; Life Sciences & Biomedicine
关键词[WOS]LOESS PLATEAU ; MAMMALIAN FAUNAS ; DENTAL MICROWEAR ; PRELIMINARY MAGNETOSTRATIGRAPHY ; NORTHERN GREECE ; SEQUENCE ; FOSSIL ; EVOLUTION ; PLIOCENE ; LINGTAI
收录类别SCI
语种英语
WOS研究方向Paleontology
WOS类目Paleontology
WOS记录号WOS:000241576900007
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3483
专题中科院古脊椎所(2000年以后)
古哺乳动物研究室
通讯作者Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
作者单位Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
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Deng, Tao,Deng, T . Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas[J]. GEODIVERSITAS,2006,28(3):499-516.
APA Deng, Tao,&Deng, T .(2006).Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas.GEODIVERSITAS,28(3),499-516.
MLA Deng, Tao,et al."Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas".GEODIVERSITAS 28.3(2006):499-516.
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