Reference Type | Journal (article/letter/editorial) |
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Title | A new lower Cambrian eodiscoid trilobite fauna from Swedish Lapland and its implications for intercontinental correlation |
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Journal | Geological Magazine |
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Authors | AXHEIMER, NIKLAS | Author |
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AHLBERG, PER | Author |
CEDERSTRÖM, PETER | Author |
Year | 2007 (November) | Volume | 144 |
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Issue | 6 |
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Publisher | Cambridge University Press (CUP) |
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DOI | doi:10.1017/s0016756807003597Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 260096 | Long-form Identifier | mindat:1:5:260096:7 |
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GUID | 0 |
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Full Reference | AXHEIMER, NIKLAS, AHLBERG, PER, CEDERSTRÖM, PETER (2007) A new lower Cambrian eodiscoid trilobite fauna from Swedish Lapland and its implications for intercontinental correlation. Geological Magazine, 144 (6) 953-961 doi:10.1017/s0016756807003597 |
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Plain Text | AXHEIMER, NIKLAS, AHLBERG, PER, CEDERSTRÖM, PETER (2007) A new lower Cambrian eodiscoid trilobite fauna from Swedish Lapland and its implications for intercontinental correlation. Geological Magazine, 144 (6) 953-961 doi:10.1017/s0016756807003597 |
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In | (2007, November) Geological Magazine Vol. 144 (6) Cambridge University Press (CUP) |
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Abstract/Notes | AbstractA lower Cambrian eodiscoid trilobite fauna and an associated holmiid trilobite, Holmia sp., are described from a bioclastic limestone at the top of the Torneträsk Formation in the Luobákti section, south of Lake Torneträsk, northern Sweden. Other associated polymerid trilobites include Orodes? lapponica and Strenuaeva inflata. The precise age of the trilobite fauna cannot be determined, but its generic composition and stratigraphical position at the top of the lower Cambrian suggest that it was recovered from the Ornamentaspis? linnarssoni Assemblage Zone. Two species of eodiscoids are present: Neocobboldia aff. dentata and Chelediscus acifer. The latter species is known previously from England and southeastern Newfoundland, and provides a novel link between upper lower Cambrian successions in Baltica and Avalonia. |
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