| Reference Type | Journal (article/letter/editorial) |
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| Title | In situ lingulids from deep-water carbonates of the Middle Ordovician Table Head Group of Newfoundland and the Trenton Group of Quebec |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Pickerill, R. K. | Author |
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| Harland, T. L. | Author |
| Fillion, D. | Author |
| Year | 1984 (February 1) | Volume | 21 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e84-021Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 478181 | Long-form Identifier | mindat:1:5:478181:7 |
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| GUID | 0 |
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| Full Reference | Pickerill, R. K., Harland, T. L., Fillion, D. (1984) In situ lingulids from deep-water carbonates of the Middle Ordovician Table Head Group of Newfoundland and the Trenton Group of Quebec. Canadian Journal of Earth Sciences, 21 (2) 194-199 doi:10.1139/e84-021 |
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| Plain Text | Pickerill, R. K., Harland, T. L., Fillion, D. (1984) In situ lingulids from deep-water carbonates of the Middle Ordovician Table Head Group of Newfoundland and the Trenton Group of Quebec. Canadian Journal of Earth Sciences, 21 (2) 194-199 doi:10.1139/e84-021 |
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| In | (1984, February) Canadian Journal of Earth Sciences Vol. 21 (2) Canadian Science Publishing |
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| Abstract/Notes | Specimens of in situ lingulids have been discovered in carbonates of the Middle Ordovician Table Head Group of northwestern Newfoundland and Trenton Group of the St. Lawrence Lowland of Quebec. The discoveries have two important implications regarding Palaeozoic lingulid ecology. First, they represent one of the few recordings of in situ lingulids in carbonate substrates of Palaeozoic age and, second, they occur mainly in outer shelf and upper slope sediments (Grondines Member of Neuville Formation, Trenton Group, and Table Cove Formation, Table Head Group), deposited in presumed considerable water depths. Caution must be observed with the use in the fossil record of lingulids as palaeo-environmental indicators. |
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