The Tunggurian stage of the continental Miocene in China | |
Deng Tao; Hou Sukuan; Wang Hongjiang | |
2007-10-01 | |
发表期刊 | ACTA GEOLOGICA SINICA-ENGLISH EDITION |
卷号 | 81期号:5页码:709-721 |
文章类型 | Article |
摘要 | The Tunggurian Age was nominated in 1984, and the Second National Commission on Stratigraphy of China formally suggested establishing the corresponding chronostratigraphic unit, the Tunggurian Stage, based on the Tunggurian Age in 1999. The name of this stage comes from a lithostratigraphic unit, the Tunggur Formation, and the stratotype section is located at the Tunggur tableland, 15 km southeast of Saihan Gobi Township, Sonid Left Banner, Inner Mongolia. The Tunggurian Age is correlated to the Astaracian of the European land mammal ages, and they share the same definition of the lower boundary at the base of the paleomagnetic Chron C5Bn.1r with an age of 15.0 Ma. In the Tairum Nor section on the southeastern edge of the Tunggur tableland, this boundary is situated within the successive deposits of reddish-brown massive mudstone of the lower part of the Tunggur Formation, with a distance of 7.6 m from the base of the grayish-white sandstones in the middle part of the section. The Tunggurian is approximately correlated to the upper part of the marine Langhian and the marine Serravallian in the International Stratigraphical Chart. The Tunggurian Stage includes two Neogene mammal faunal units, i.e. NMU 6 (MN 6) and NMU 7 (MN 7/8). The Tairum Nor fauna from the Tairum Nor section corresponds to NMU 6, and the Tunggur fauna (senso stricto) from the localities on the northwestern edge of the Tunggur tableland, such as Platybelodon Quarry, Wolf Camp and Moergen, corresponds to NMU 7. Among the Middle Miocene mammalian faunas in China, the Laogou fauna from the Linxia Basin, Gansu, the Quantougou fauna from the Lanzhou Basin, Gansu, the Halamagai fauna from the northern Junggar Basin, Xinjiang, and the Dingjiaergou fauna from Tongxin, Ningxia correspond to NMU 6. |
关键词 | Tunggurian Miocene Stratotype Biostratigraphic Unit Paleomagnetic Age China |
WOS标题词 | Science & Technology ; Physical Sciences |
关键词[WOS] | NORTHERN TIBETAN PLATEAU ; HISPANOTHERIUM-MATRITENSE ; MIDDLE MIOCENE ; LINXIA BASIN ; NEOGENE ; GANSU ; BIOSTRATIGRAPHY ; SUBDIVISION ; SEQUENCE ; SPAIN |
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:000250766700005 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.205/handle/311034/2037 |
专题 | 古哺乳动物研究室 |
作者单位 | 1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China 3.Stn Cultural Relic Protect & Management Xilin Gol, Xilinhot 026000, Inner Mongolia, Peoples R China |
推荐引用方式 GB/T 7714 | Deng Tao,Hou Sukuan,Wang Hongjiang. The Tunggurian stage of the continental Miocene in China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2007,81(5):709-721. |
APA | Deng Tao,Hou Sukuan,&Wang Hongjiang.(2007).The Tunggurian stage of the continental Miocene in China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,81(5),709-721. |
MLA | Deng Tao,et al."The Tunggurian stage of the continental Miocene in China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 81.5(2007):709-721. |
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