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Transitional Ediacaran-Cambrian small skeletal fossil assemblages from South China and Kazakhstan: Implications for chronostratigraphy and metazoan evolution
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文摘

Transitional Ediacaran–Cambrian ​skeletal fauna found in South China and Kazakhstan.

New fauna first occurs in basal Cambrian cherty sediments (Daibu and Aksai members).

Cloudinids (Cloudina and Rajatubulus gen. nov.) persisted into the early Cambrian.

New fauna reveals a less abrupt faunal change at the Pc–C boundary than thought.

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