| Reference Type | Journal (article/letter/editorial) |
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| Title | Chitinozoaires de l'Arenig supérieur (Zone D) de la Formation de Lévis, Québec, Canada |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Achab, A. | Author |
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| Year | 1982 (June 1) | Volume | 19 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e82-110Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477543 | Long-form Identifier | mindat:1:5:477543:4 |
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| GUID | 0 |
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| Full Reference | Achab, A. (1982) Chitinozoaires de l'Arenig supérieur (Zone D) de la Formation de Lévis, Québec, Canada. Canadian Journal of Earth Sciences, 19 (6) 1295-1307 doi:10.1139/e82-110 |
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| Plain Text | Achab, A. (1982) Chitinozoaires de l'Arenig supérieur (Zone D) de la Formation de Lévis, Québec, Canada. Canadian Journal of Earth Sciences, 19 (6) 1295-1307 doi:10.1139/e82-110 |
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| In | (1982, June) Canadian Journal of Earth Sciences Vol. 19 (6) Canadian Science Publishing |
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| Abstract/Notes | The Shumardia limestone that forms the upper part of the Levis Formation (Zone D) yields well preserved assemblages of chitinozoans.These assemblages seem to be characterized by a new species: Conochitina pirum. They also contain Fustichitina langei, Conochitina poumoti, and Conochitina cf. C. kryos species, which permit a comparison with Arenig microfaunas from Spitsbergen and Australia.The paleontological data, especially those given by graptolites, indicate that Zone D is of late Arenig age. This age determination is corroborated by the absence of lower Llanvirn chitinozoans in the samples studied. |
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