Abstract

Cretoxyrhina mantelli was a large pelagic lamniform shark geographically widespread during the Late Cretaceous, and well known because of several nearly complete skeletons from the Western Interior Seaway of North America. Here we report 15 partial skeletons belonging to lamniform sharks from the ‘lastame’ lithozone of the Upper Cretaceous Scaglia Rossa Formation of the Lessini Mountains (northeastern Italy). Seven partial but articulated skeletons include tooth sets that allow a confident attribution to Cretoxyrhina mantelli based on dental morphologies. We review the taxonomic history of C. mantelli, evidencing that the taxon was erected by Agassiz (1835) and tracing back four of the original syntypes. Based on calcareous plankton biostratigraphy, the rock in which the Italian skeletal remains are embedded is constrained to the middle-upper Turonian. Total length estimates of the specimens suggest that the sample includes the largest specimen of Cretoxyrhina mantelli (615–650 cm estimated total length) known to date. The placoid scale morphology indicates that C. mantelli most likely was a fast swimmer with a similar ecology as the extant white shark, Carcharodon carcharias. The associated skeletal elements of the specimens represent large chondrichthyan deadfalls and the cadavers decayed on the seafloor where they remained exposed for several months, as indicated by bioerosional traces, some of which are interpreted as a product of bone-eating worm activities and other bioerosional traces with Gastrochaenolites-like structure. The Cretoxyrhina mantelli remains described herein provide new information about the ʻlastameʼ vertebrate assemblage, which seemingly was strongly dominated by chondrichthyans, especially lamniform sharks.

Highlights

  • Theginsushark, Cretoxyrhina mantelli (Agassiz), is probably one of the best known and ecologically relevant top predators of the Late Cretaceous seas

  • Isolated teeth are so far the most common remains of C. mantelli reported from Italy (e.g., Bassani, 1876; D’Erasmo, 1922), some partial skeletons were found in the Scaglia Rossa

  • The goal of this paper is to provide an overview of all the skeletal remains of C. mantelli discovered in northeastern Italy, and to discuss their paleobiological, stratigraphic and taphonomical implications

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Summary

Introduction

Theginsushark, Cretoxyrhina mantelli (Agassiz), is probably one of the best known and ecologically relevant top predators of the Late Cretaceous seas Isolated teeth of this shark have been reported from many localities all around the world Chalk Member of the Niobrara Chalk in the Western Interior Seaway of North America (Bourdon, Everhart, 2011; Shimada, 1993a,b, 1994a-c, 1997a-e, 2008; Shimada et al, 2006) These skeletons indicate that Cretoxyrhina mantelli had a general morphology close to that of the white shark (Carcharodon carcharias Linnaeus, 1758) (Shimada, 1997b; Shimada et al, 2006), being similar or even larger in size. The majority of these skeletal remains consist of teeth associated with calcified vertebral centra and fragments of calcified cranial cartilage; in some cases, they include placoid scales

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