DICENTRODUS (CHONDRICHTHYES: XENACANTHIDA) FROM THE EARLY CARBONIFEROUS (VISEAN: UPPER ST LOUIS FORMATION) OF IOWA, USA

dc.contributor.authorHampe O.
dc.contributor.authorJohnson G.D.
dc.contributor.authorTurner S.
dc.date.accessioned2024-12-28T06:16:11Z
dc.date.available2024-12-28T06:16:11Z
dc.date.issued2006
dc.description.abstractDicentrodus possessed bicuspid teeth with a flat base and nonserrated or finely serrated, labio-lingually compressed, highly unequal cusps. Originally known from the late Visean-early Serpukhovian of Scotland (D. bicuspidatus), it is now known also to occur in the middle Visean of North America. This is the earliest occurrence of a xenacanthid yet reported from North America; its presence is based on incomplete teeth, which are easily distinguished from other xenacanthid genera. The cross-continental distribution of Dicentrodus, like that of other xenacanthid genera, can be explained by an increasing body of data that intimate that xenacanthids were euryhaline sharks and not restricted to a freshwater habitat. © 2006 Cambridge University Press.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13690535
dc.identifier.citationGeological Magazine, 2006, 143, 4, 545-549
dc.identifier.doi10.1017/S0016756806002093
dc.identifier.issn0016-7568
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/47137
dc.subjectCARBONIFEROUS
dc.subjectIOWA
dc.subjectPALAEOGEOGRAPHY
dc.subjectSCOTLAND
dc.subjectXENACANTHIDA
dc.subject.agePaleozoic::Carboniferous
dc.subject.ageПалеозой::Каменноугольная
dc.titleDICENTRODUS (CHONDRICHTHYES: XENACANTHIDA) FROM THE EARLY CARBONIFEROUS (VISEAN: UPPER ST LOUIS FORMATION) OF IOWA, USA
dc.typeСтатья

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