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Naobaogou Formation
Geological formation in Daqing Mountains, China From Wikipedia, the free encyclopedia
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The Naobaogou Formation is a geological formation in the Daqing Mountains of China. It is likely of Lopingian (Late Permian) age. It consists of three rhythms of sediment, labeled members I-III primarily of purple siltstone, but each with a thick basal conglomerate bed. It is notable for its fossil content, producing one of the most diverse Late Permian vertebrate faunas outside Russia and South Africa.[1]
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Vertebrate fauna
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References
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