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Paleobiota of the Liushu Formation information


An artist's illustration of the Paleobiota and environment of the upper part of the Liushu formation

The Liushu formation is a geological formation in the Gansu province of China that spans up to 100 m thick and is widely distributed within the Linxia Basin, with a paleomagnetic age of between 11 and 6.4 Mya (Upper/Late Miocene).

The formation is divided into three parts which represent three different ages, generally referred to as the "upper part" (youngest, at 6-7 mya), the "middle part" (intermediate, at 9 to 7.6 mya. Also known as the Dashengou fauna, and the "lower part" (oldest).[1][2]

  1. ^ "Vertebrata PalAsiatica, Vol. 42, 2004----Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences". english.ivpp.cas.cn. Retrieved 2020-12-21.
  2. ^ Cite error: The named reference :0 was invoked but never defined (see the help page).

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Paleobiota of the Liushu Formation

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The Liushu formation is a geological formation in the Gansu province of China that spans up to 100 m thick and is widely distributed within the Linxia...

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