DICENTRODUS (CHONDRICHTHYES: XENACANTHIDA) FROM THE EARLY CARBONIFEROUS (VISEAN: UPPER ST LOUIS FORMATION) OF IOWA, USA
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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.
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Geological Magazine, 2006, 143, 4, 545-549