Title | Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada-stratigraphic and paleobiogeographic implications |
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Author | Fedorowski, J; Bamber, E W; Richards, B C |
Source | Acta Palaeontologica Polonica vol. 64, 4, 2019 p. 851-870, https://doi.org/10.4202/app.00636.2019 Open Access |
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Year | 2019 |
Alt Series | Natural Resources Canada, Contribution Series 20200158 |
Publisher | Inst Paleobiologii Pan |
Document | serial |
Lang. | English |
Media | paper; on-line; digital |
File format | pdf |
Province | Canada |
Lat/Long WENS | -126.0000 -123.0000 61.5000 60.0000 |
Subjects | environmental geology; Nature and Environment; stratigraphy; Science and Technology; taxonomy; paleogeography; fossils; stratigraphic analyses; paleobiology; Mattson Formation; Liard Basin;
Pennsylvanian; Carboniferous |
Illustrations | location maps; lithologic sections; sections |
Released | 2019 12 05 |
Abstract | Colonies of the rugose corals Nemistium liardense sp. nov. and Heritschioides simplex sp. nov. were collected from limestone in the upper member of the Mattson Formation in the Liard Range in the
Northwest Territories and are the only known identifiable coral species from the Mattson Fm. The Mattson Fm., deposited in the Liard Basin west of the syndepositional Bovie reverse fault, comprises sandstone with subordinate shale and carbonates
deposited during several delta cycles. The close morphological similarity and identical mode of offsetting in N. liardense colonies from the Mattson Fm. and the allochthonous Stikine Terrane of British Columbia indicate they belong in the same
species. This and the morphological similarity between H. simplex and the late Serpukhovian to early Bashkirian H. columbicum allow assignment of the coral-bearing part of the upper Mattson Fm. to Bashkirian Foraminiferal Biozone 20. Widespread
occurrence of the genus Nemistium confirms open communication between the Liard Basin region and the western European and northern African seas. |
GEOSCAN ID | 326570 |
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