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

Show simple item record

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


Files in this item

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record