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Ustʹ Pinega Formation
Geological formation in northwestern Russia From Wikipedia, the free encyclopedia
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64°9′0.000″N 41°55′59.988″E The Ustʹ Pinega Formation is an Upper Ediacaran geological formation exposed along the banks of the Syuzma and Onega Rivers in Arkhangelsk Oblast, northwestern Russia,[3] and spans from around 580 Ma to 550 Ma, with fossilferous stones restricted to between 565 and 555 Ma.
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It also preserves a wealth of rare Ediacaran fossils, like Zolotytsia, Ventogyrus and Bomakellia.
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Dating
The Ustʹ Pinega Formation is relatively large, and using zircon U-Pb dating, a date of 550±2 Ma had be recovered for the top of the formtion,[4] whilst the known base of the formation is restricted to 580±0 Ma.[4][1]
As for the lower and upper dates of the fossiliferous units within the formtaion, using the Rb–Sr dating method, the lowest fossiliferous unit of the Ustʹ Pinega Formation has been dated to 565±9 Ma,[1] whilst the upper-most fossiliferous unit was dated using zircon U-Pb dating, which had recovered a date of 555±3 Ma.[5]
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Paleobiota
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Perspective
The Ustʹ Pinega Formation is home to many rare and common Ediacaran fauna, from the well known motile forms such as Dickinsonia and Kimberella,[6] to the rarer, more elusive forms like Ventogyrus and Zolotytsia. All forms within this formation are preserved in layers of ash beds, which are not only good at preserving the fine exterior details of organisms, but also their internals, like Burykhia.[7]
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Notes Uncertain or tentative taxa are in small text; |
Proarticulata
Petalonamae
Trilobozoan
Cnidarian
Chordata
Annelida
incertae sedis
Flora
Ichnogenera
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See also
References
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