This horizon lies within the transitional interval between the lower clastic-dominated member and the upper carbonate-rich member ( Figure 1 c), a position that may be significant for understanding the taphonomic context of the fossil. 3.
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First Occurrence of <i>Wronascolex</i> sp. (Palaeoscolecida, Priapulida) in the Cambrian Tianpeng Formation (Wuliuan Stage), Southeastern Yunnan, South China: Implications for a New Burgess Shale-Type Lagerstätte.
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