Vester Formation

The Vester Formation is a geologic formation in Oregon. It preserves fossils dating back to the Triassic period. The partial skeleton of a new genus of basal thalattosaur has been recovered from the Brisbois Member of this formation.[1] The Brisbois Member, which dates to between the Carnian and Norian, is a marine sequence primarily composed of fine-grained clastic sedimentary rocks with fissile mudstones of black, green or gray variety broken up by widely spaced intervals of calcirudite beds and calcareous conglomerate.[2] The formation formed between two parallel island arcs, that of the Baker Terrane and the Olds Ferry Terrane. The formation is mostly consists of reworked chert grains from the Baker Terrane.[3] In addition to the remains of the basal thalattosaur, fragmentary and undescribed remains exist of an ichthyosaur, archosaur, and a hybodontid shark as well as many invertebrate fossils.[1]

Vester Formation
Stratigraphic range: Ladinian - Norian
TypeFormation
Unit ofOlds Ferry Terrane
Sub-unitsBrisbois Member
AreaCentral Oregon
Location
Coordinates44.118° N, 119.483° W
RegionOregon
CountryUnited States

See also

References

  1. Metz, Eric T. (2019). Description, phylogenetic analysis and taphonomy of a new Thalattosaur from the Brisbois member of the Vester Formation (Carnian/Norian) of central Oregon (ms thesis). University of Alaska Fairbanks.
  2. Dickinson and Vigrass, 1965
  3. Dorsey and LaMaskin, 2007

Sources

  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.
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