DICENTRODUS (CHONDRICHTHYES: XENACANTHIDA) FROM THE EARLY CARBONIFEROUS (VISEAN: UPPER ST LOUIS FORMATION) OF IOWA, USA
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dc.contributor.author | Hampe O. | |
dc.contributor.author | Johnson G.D. | |
dc.contributor.author | Turner S. | |
dc.date.accessioned | 2024-12-28T06:16:11Z | |
dc.date.available | 2024-12-28T06:16:11Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13690535 | |
dc.identifier.citation | Geological Magazine, 2006, 143, 4, 545-549 | |
dc.identifier.issn | 0016-7568 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/47137 | |
dc.description.abstract | Dicentrodus 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.subject | CARBONIFEROUS | |
dc.subject | IOWA | |
dc.subject | PALAEOGEOGRAPHY | |
dc.subject | SCOTLAND | |
dc.subject | XENACANTHIDA | |
dc.title | DICENTRODUS (CHONDRICHTHYES: XENACANTHIDA) FROM THE EARLY CARBONIFEROUS (VISEAN: UPPER ST LOUIS FORMATION) OF IOWA, USA | |
dc.type | Статья | |
dc.identifier.doi | 10.1017/S0016756806002093 | |
dc.subject.age | Paleozoic::Carboniferous | |
dc.subject.age | Палеозой::Каменноугольная |
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