J
Junming Zhang
Researcher at Chinese Academy of Sciences
Publications - 14
Citations - 1794
Junming Zhang is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Doushantuo Formation & Chemostratigraphy. The author has an hindex of 13, co-authored 14 publications receiving 1521 citations. Previous affiliations of Junming Zhang include Academia Sinica.
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Integrated Ediacaran (Sinian) chronostratigraphy of South China
TL;DR: In this article, the Yangtze Platform of South China has been investigated for the purpose of constructing a framework for global chronostratigraphic correlation of Ediacaran strata, and the results indicated that the earliest known metazoan biotas do not constitute two temporally separate evolutionary lineages preceding the Cambrian explosion of animal life.
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Doushantuo embryos preserved inside diapause egg cysts
TL;DR: The discovery of embryo-like Doushantuo fossils inside large, highly ornamented organic vesicles (acritarchs) indicates that these organisms were eukaryotic, and most probably early cleavage stage embryos preserved within diapause egg cysts.
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Sinian-Cambrian stratigraphic framework for shallow- to deep-water environments of the Yangtze Platform: an integrated approach
TL;DR: In this paper, the authors investigated the early Cambrian shallow-to-deep-water sequences of the Yangtze Platform and proposed a high-resolution stratigraphic framework for multidisciplinary analyses of the Cambrian explosion.
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U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in south China: Constraints on late Neoproterozoic glaciations
Shihong Zhang,Ganqing Jiang,Junming Zhang,Biao Song,Martin J. Kennedy,Nicholas Christie-Blick +5 more
TL;DR: In this paper, two distinctive volcanic ash beds were found in the terminal Proterozoic Doushantuo Formation in south China, yielding a U-Pb zircon age of 621 6 7 Ma, providing the closest upper limit for a correlative of the Marinoan glaciation.
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Carbon isotope chemostratigraphy and sedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei, South China
Maoyan Zhu,Miao Lu,Junming Zhang,Fangchen Zhao,Guoxiang Li,Yang Aihua,Xin Zhao,Xin Zhao,Meijuan Zhao,Meijuan Zhao +9 more
TL;DR: The Doushantuo Formation of South China, consisting of intercalated siliciclastic and carbonate rocks which exhibit considerable variation in thickness and sedimentary facies, is one of the key sedimentary units in the world for understanding Ediacaran geobiological processes as mentioned in this paper.