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Dengying Formation
Geologic formation in China From Wikipedia, the free encyclopedia
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The Dengying Formation is an upper Ediacaran (551-541 Ma[2]) fossiliferous geologic formation found in South China. It was deposited on a shallow marine carbonate platform.[3]
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Members
Listed by ascending age:
- The Hamajing Member is characterized by light grey, medium- to thick-bedded dolomite, intercalated with thin layers of chert.[3]
- The Shibantan Member is interpreted to represent a subtidal environment and is composed of dark grey, thin-bedded bituminous limestone. It is the most fossiliferous of the Dengying Formation members and has yielded several trace fossils, such as Lamonte,[4] as well as possible lobopodian trackways. [5]
- The Baimatuo Member consists of light grey, thick-bedded dolomite.[3]
Traditionally, the Tianzhushan Member was considered to be the uppermost unit of the Dengying Formation. However, its small shelly fossils and Micrhystridium-like acritarchs are a shared characteristic with the Cambrian Yanjiahe Formation.[3] The Kuanchuanpu Formation also is occasionally placed as a member of the Dengying Formation,[6] however it is likely separate for the same reasons.
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Paleobiota
Summarize
Perspective
The Dengying formation is unique from other Ediacaran formations in that its top is almost right up against the Ediacaran - Cambrian boundary, with more recent organisms being described that have striking similarities with Cambrian fauna, like Alienum. There are also a lot of ichnogenera in the form of burrows, something that is common in younger Ediacaran rocks the closer to the Cambrian boundary they are.
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Notes Uncertain or tentative taxa are in small text; |
Proarticulata
Petalonamae
Trilobozoa
Porifera
incertae sedis
Flora
Microorganisms
Ichnogenera
Undescribed
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See also
- List of fossiliferous stratigraphic units in China
- Ediacaran biota
References
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