1) Doushantuoian
陡山沱期
1.
Megascopic Biota from the Doushantuoian of the Neoproterozoic (Ediacaran) in Guizhou and Zhongqing, South China
黔—渝地区新元古代伊迪卡拉纪陡山沱期宏体生物群
2.
Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance
华南陡山沱期晚期宏体生物生态系统的出现及其意义
2) Late Doushantuoian
陡山沱晚期
1.
Preliminary discussion on ecological characteristics and buried environments of Miaohe-type Biota during the Late Doushantuoian of Sinian in northeastern Guizhou Province;
黔东北震旦纪陡山沱晚期庙河型生物群的生态特征及埋藏环境初探
3) Doushantuo formation
陡山沱组
1.
Macroscopic Algae from the Ediacaran Doushantuo Formation in Northeast Guizhou, South China;
黔东北伊迪卡拉纪陡山沱组的宏体藻类
2.
Geochemistry and petrogenesis of the cap dolostones at the bottom of the Doushantuo Formation in northwestern Fanjing Mountains,Guizhou;
贵州梵净山西北陡山沱组底部白云岩帽地球化学特征及成因探讨
3.
Sedimentary Successions and Environment of the Sinian Doushantuo Formation in Jiangkou,Guizhou Province;
贵州江口震旦系陡山沱组沉积层序和沉积环境分析
4) Doushantuo Formation phosphate rocks
陡山沱组磷块岩
1.
Plenty of multicellular alage, sponge and embryos have been discovered in the upper Sinian system Doushantuo Formation phosphate rocks(580 million years) in Weng’an county, Guizhou Province.
在贵州省瓮安县上震旦统陡山沱组磷块岩（距今５８０ Ｍａ）中，发现有大量的多细胞藻类、海绵和动物胚胎化石。
5) Doushantuo Formation Dengying Formation boundary layer
陡山沱组-灯影组界线层
1.
Abundant microspherulites have been recently discovered first in the Doushantuo Formation Dengying Formation boundary layer of the Miaohe Sinian section in Zigui, Hubei.
在湖北秭归庙河震旦系剖面陡山沱组-灯影组界线层内首次发现了微球粒。
6) Doushantuo formation Dengying formation boundary
陡山沱组灯影组界线
1.
The Doushantuo formation Dengying formation boundary section at Miaohe in the eastern Yangtze Gorges in China is studied.
我们研究了峡东庙河陡山沱组灯影组界线剖面，获得ＲＥＥ及其它微量元素异常和大量微球粒等灾变事件的证据，从而判定庙河生物群的大绝灭是由于陡山沱期末的一次地球灾变事件的结果。
补充资料：立陡陡
1.直立貌。
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