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Lenz, Alfred C. (2013) Early Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada. Canadian Journal of Earth Sciences, 50 (11) 1097-1115 doi:10.1139/cjes-2013-0057

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Reference TypeJournal (article/letter/editorial)
TitleEarly Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada
JournalCanadian Journal of Earth Sciences
AuthorsLenz, Alfred C.Author
Year2013 (November)Volume50
Issue11
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2013-0057Search in ResearchGate
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Mindat Ref. ID484891Long-form Identifiermindat:1:5:484891:6
GUID0
Full ReferenceLenz, Alfred C. (2013) Early Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada. Canadian Journal of Earth Sciences, 50 (11) 1097-1115 doi:10.1139/cjes-2013-0057
Plain TextLenz, Alfred C. (2013) Early Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada. Canadian Journal of Earth Sciences, 50 (11) 1097-1115 doi:10.1139/cjes-2013-0057
In(2013, November) Canadian Journal of Earth Sciences Vol. 50 (11) Canadian Science Publishing
Abstract/Notes The Early Devonian graptolite fauna of the Arctic Islands comprises the highest species content (17 species) in the world. In spite of this richness, no new species have been recognized; instead already-existing species, scattered around the then-known continents, suggest that relatively complete cosmopolitanism held sway for graptolites. Canadian Arctic biozonation is very similar to schemes elsewhere, consisting of the uniformis and hercynicus biozones in the Lochkovian, falcarius in the lower Pragian, and an expanded yukonensis Biozone in the upper Pragian and the lower Emsian. Three genera and 17 species are recognized: “Monograptus” (microdon cf. microdon, microdon curvatus); Neomonograptus (cf. atopus, aequabilis, bardoensis, falcarius, notoaequabilis); and Uncinatograptus (birchensis, craigensis, hercynicus, langgunensis, parangustidens, subhercynicus, telleri, thomasi, uniformis, yukonensis).


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