Nihewan Basin

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The Nihewan Basin or the Nihewan Depression is located in the transition area between the North China Lowlands and the Inner Mongolia Plateau about 200 km west of Beijing in the border area of ​​the Hebei and Shanxi provinces .

It is after the village Nihewan in China named Hebei Province, the most Sanggan River in the east of the circle Yang Yuan of prefecture-level city of Zhangjiakou is.

The basin belongs to the Shanxi rift system that formed as a series of intermontane basins in the Middle to Late Pleistocene. It is filled with late Pliocene to Holocene lacustric , fluvial and wind-transported sediments . The Nihewan Formation comprises the entire fluvio-lacustric sequence in the Nihewan Basin, which is overlaid by wind-blown loess sediments of the Holocene and / or the last Ice Age and / or the Warm Period and underlaid with late Pliocene red clay of Aeolian origin.

Determining the time sequence of the Nihewan Formation of the Nihewan Basin, rich in mammalian faunas and Paleolithic sites (see main article Nihewan ), is crucial for an understanding of a number of important questions about early human adaptability to extreme environmental conditions in high northern latitudes, the filling process of the Nihewan Basin. Basin and the chronological order of the Nihewan fauna .

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Individual evidence

  1. Chinese   泥 河湾 盆地 , Pinyin Nihewan pendi , English Nihewan Basin
  2. Chinese   泥 河灣  /  泥 河湾 , Pinyin Níhéwān , W.-G. Ni-ho-wan / Nihowan
  3. Dennell 2009, 167 after Li et al. 1998
  4. According to Zhu Rixiang, Deng Chenglong, Pan Yongxin (see web link under Ref.).

Coordinates: 40 ° 15 ′ 22 "  N , 114 ° 37 ′ 51.1"  E