The Tunggurian stage of the continental Miocene in China

IVPP-IR > 中科院古脊椎所（2000年以后）

	The Tunggurian stage of the continental Miocene in China
	Deng Tao(邓涛); Hou SuKuan(侯素宽); Wang Hongjiang; Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
	2007
发表期刊	ACTA GEOLOGICA SINICA-ENGLISH EDITION
ISSN	1000-9515
卷号	81 期号:5 页码:709—721
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.
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/3301
专题	中科院古脊椎所（2000年以后）
通讯作者	Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
推荐引用方式 GB/T 7714	Deng Tao,Hou SuKuan,Wang Hongjiang,et al. 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,&Deng, T .(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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