| Reference Type | Journal (article/letter/editorial) |
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| Title | Lingulid brachiopods and Lingulichnus from a Silurian shelf–slope carbonate sequence, Delorme Group, Mackenzie Mountains, Northwest Territories |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Over, D. Jeffrey | Author |
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| Year | 1988 (March 1) | Volume | 25 |
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| Issue | 3 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e88-047Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 479940 | Long-form Identifier | mindat:1:5:479940:9 |
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| GUID | 0 |
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| Full Reference | Over, D. Jeffrey (1988) Lingulid brachiopods and Lingulichnus from a Silurian shelf–slope carbonate sequence, Delorme Group, Mackenzie Mountains, Northwest Territories. Canadian Journal of Earth Sciences, 25 (3) 465-471 doi:10.1139/e88-047 |
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| Plain Text | Over, D. Jeffrey (1988) Lingulid brachiopods and Lingulichnus from a Silurian shelf–slope carbonate sequence, Delorme Group, Mackenzie Mountains, Northwest Territories. Canadian Journal of Earth Sciences, 25 (3) 465-471 doi:10.1139/e88-047 |
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| In | (1988, March) Canadian Journal of Earth Sciences Vol. 25 (3) Canadian Science Publishing |
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| Abstract/Notes | Structures assigned to the ichnogenus Lingulichnus, commonly containing the burrow-forming brachiopod, were collected from an argillaceous unit in a Silurian shelf dolostone sequence (Delorme Group). The sediments, benthic fauna, and inclined orientation of all lingulid burrows indicate the presence of a bottom current and restricted conditions on the margin of the Selwyn Basin. High-abundance–low-diversity faunas of lingulids and Lingulichnus are indicative of limiting conditions at the substrate surface. Under low-energy conditions, they seem to be indicative of the Zoophycos ichnofacies. |
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