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1)  Weng an fauna
瓮安动物群
1.
REE characteristics of Doushantuo phosphorites indicate a pronounced paleoredox condition change from the lower to the upper ore bed when Weng an fauna, most probably the earliest metazoan fauna, emerged.
这种南沱冰期之后的环境变化可能为瓮安动物群的大爆发提供了必要的条件。
2)  Weng'an Biota
瓮安生物群
1.
Sedimentary Geochemistry Research on the Radiation of Weng'an Biota and the Formation of the Phosphorite Ore Deposit,Guizhou;
贵州瓮安生物群和磷矿形成的沉积地球化学研究
2.
New data of phosphatized globular fossils from Weng'an biota in the Ediacaran Doushantuo Formation and the problem concerning their affinity
埃迪卡拉纪陡山沱期瓮安生物群中磷酸盐化球状化石新材料及其问题讨论
3)  Weng an biota
瓮安生物群
1.
New Evidences of Sponge Fossils in the Weng an Biota;
瓮安生物群中海绵化石的新证据
2.
The Study on the Spheroidal Fossils in Weng an Biota and Kuanchuanpu Biota;
宽川铺生物群与瓮安生物群中的球形类化石研究
3.
Microscopic observation indicates that the walls of the vase-shaped fossils from both Weng an biota .
报道了产自贵州瓮安新元古代陡山沱期磷块岩中的瓶状微化石2属3种,进一步证实瓮安生物群中已具有最早的能分泌硬体的原生动物存在。
4)  Wenghui biota
瓮会生物群
1.
The Wenghui biota, which is found in the Ediacaran Doushantuo Formation in Northeast Guizhou, is composed mainly of macroalgae (18 species of 15 genera, one unnamed macroalgae, and macroalgal holdfast forms described herein), and contains macroscop.
产自于黔东北伊迪卡拉系陡山沱组的瓮会生物群生活环境应在贫氧的、透光性良好的浅海低能环境,以宏体藻类为主,共描述15属18种(其中包括3个新属、5个新种、2个修定属和4个修定种)和1个未命名藻以及不明藻类固着器,另包含有宏体后生动物,可能的后生动物以及遗迹化石。
5)  "Weng'an mass incident"
瓮安群体事件
6)  Weng an
瓮安
1.
The Geochemistry of Phosphorite of Doushantuo Formation in Weng an,China: Insights from Trace Elements and REE;
贵州瓮安磷矿陡山沱组地层元素地球化学特征
补充资料:黑瓮瓮
1.犹黑洞洞。
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