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Storrs, Glenn W. (1991) Note on a second occurrence of thalattosaur remains (Reptilia: Neodiapsida) in British Columbia. Canadian Journal of Earth Sciences, 28 (12) 2065-2068 doi:10.1139/e91-186

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Reference TypeJournal (article/letter/editorial)
TitleNote on a second occurrence of thalattosaur remains (Reptilia: Neodiapsida) in British Columbia
JournalCanadian Journal of Earth Sciences
AuthorsStorrs, Glenn W.Author
Year1991 (December 1)Volume28
Issue12
PublisherCanadian Science Publishing
DOIdoi:10.1139/e91-186Search in ResearchGate
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Mindat Ref. ID481187Long-form Identifiermindat:1:5:481187:3
GUID0
Full ReferenceStorrs, Glenn W. (1991) Note on a second occurrence of thalattosaur remains (Reptilia: Neodiapsida) in British Columbia. Canadian Journal of Earth Sciences, 28 (12) 2065-2068 doi:10.1139/e91-186
Plain TextStorrs, Glenn W. (1991) Note on a second occurrence of thalattosaur remains (Reptilia: Neodiapsida) in British Columbia. Canadian Journal of Earth Sciences, 28 (12) 2065-2068 doi:10.1139/e91-186
In(1991, December) Canadian Journal of Earth Sciences Vol. 28 (12) Canadian Science Publishing
Abstract/Notes A fragmentary thalattosaur specimen from the Late Triassic Pardonet Formation of northeastern British Columbia is the second reported occurrence of such animals in Canada. The group was previously known with certainty only from the Hosselkus Limestone of California, the Monte San Giorgio region shales of Italy and Switzerland, the Natchez Pass Formation of Nevada, and most recently, the Sulphur Mountain Formation of British Columbia. As such, the described material, which is indeterminate to genus, represents a slight geographic range extension of the Thalattosauria. The Norian age of this material represents a significant temporal range extension for the Thalattosauria, and it is the geologically youngest material known of this taxon.


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