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Adrain, Jonathan M., Kloc, Gerald J. (1997) Lower Devonian aulacopleuroidean trilobites from Oklahoma. Journal of Paleontology, 71 (4) 703-712 doi:10.1017/s0022336000040154

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Reference TypeJournal (article/letter/editorial)
TitleLower Devonian aulacopleuroidean trilobites from Oklahoma
JournalJournal of Paleontology
AuthorsAdrain, Jonathan M.Author
Kloc, Gerald J.Author
Year1997 (July)Volume71
Issue4
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000040154Search in ResearchGate
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Mindat Ref. ID417369Long-form Identifiermindat:1:5:417369:8
GUID0
Full ReferenceAdrain, Jonathan M., Kloc, Gerald J. (1997) Lower Devonian aulacopleuroidean trilobites from Oklahoma. Journal of Paleontology, 71 (4) 703-712 doi:10.1017/s0022336000040154
Plain TextAdrain, Jonathan M., Kloc, Gerald J. (1997) Lower Devonian aulacopleuroidean trilobites from Oklahoma. Journal of Paleontology, 71 (4) 703-712 doi:10.1017/s0022336000040154
In(1997, July) Journal of Paleontology Vol. 71 (4) Cambridge University Press (CUP)
Abstract/NotesNew aulacopleuroidean trilobites from the Lochkovian of Oklahoma include the otarionine Cyphaspis carrolli new species from the Haragan Formation, and the brachymetopid Cordania wessmani new species from the overlying Bois d'Arc Formation. Cyphaspis carrolli is the first record of the genus from the North American Devonian. It is a highly plesiomorphic species, dissimilar to contemporaries from Europe, but closely related to Silurian species from Northern Laurentia and England. Cordania wessmani had previously been interpreted as a possible sexual dimorph of Cordania falcata Whittington, 1960, but new material and information shows that the forms occur separately with no stratigraphic overlap. New information on trilobite occurrence in the Haragan and Bois d'Arc Formations does not support previous hypotheses of trilobite sexual dimorphism, but rather indicates the presence of distinct, stratigraphically successive faunas.


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