
New light on the trophic ecology of Carcharodon hastalis from teeth embedded in Miocene cetacean vertebrae from Calvert Cliffs in Maryland, USA
Stephen J. Godfrey, Victor J. Perez, Marcus Jones, Phillip F. Chapman, Nathan Spencer, and Jason E. Osborne
Recent isotopic analyses of the teeth of the extinct lamnid Carcharodon hastalis showed that it fed at a comparable trophic level as was the fossil and modern great white shark, Carcharodon carcharias. Although there are many examples of shark bite marks on marine mammal bones, there have not been any publications documenting the presence of C. hastalis teeth embedded in the bones of marine mammals. Here we report on the first C. hastalis teeth found embedded in vertebrae of two Miocene cetaceans. These teeth represent unequivocal evidence of trophic interactions between this shark and cetaceans. It is not known if these interactions were the result of active predation or scavenging. These embedded C. hastalis teeth offer supporting evidence to the aforementioned isotopic findings. The finding of C. hastalis teeth embedded in cetacean vertebrae demonstrate that in the Carcharodon lineage, serrated teeth were not a prerequisite to feeding on marine mammals. Carcharodon hastalis may have fed on marine mammals for millions of years prior to the evolution of lightly serrated teeth in its chronospecific descendent, Carcharodon hubbelli. The behavioral adaptation to mammalophagy in the Carcharodon lineage, regardless as to how inefficient it might have been without serrated teeth, appears to have occurred for millions of years prior to the evolution of fully serrated teeth in Carcharodon carcharias. That feeding behavior may well have given natural selection sufficient time to develop and hone the serrated teeth now seen in extant great white sharks (C. carcharias). Given that competition for high trophic resources between the Carcharodon and Otodus lineages seemingly existed for millions of years prior to the extinction of Otodus megalodon, it seems that competition alone is likely not the only explanation for why O. megalodon went extinct.
Key words: Elasmobranchii, Carcharodon hastalis , Cetacea, cetacean vertebrae, trophic interaction, Miocene, Maryland.
Stephen J. Godfrey [Stephen.Godfrey@calvertcountymd.gov; ORCID: https://orcid.org/0000-0002-7916-8791], Maryland Paleontology Collection and Research Center, Calvert Marine Museum, P.O. Box 97, Solomons, Maryland, 20688 USA. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC, 20013-7012 USA; Vertebrate Paleontology, Natural History Museum of Los Angeles, 900 Exposition Boulevard, Los Angeles, California, 90007 USA. Victor J. Perez [vjperez@smcm.edu; ORCID: https://orcid.org/0000-0002-0041-7151], St. Mary’s College of Maryland, St. Mary’s City, Maryland, 20686 USA; Maryland Paleontology Collection and Research Center, Calvert Marine Museum, P.O. Box 97, Solomons, Maryland, 20688 USA. Marcus Jones [paleomarcjones@gmail.com; ORCID: https://orcid.org/0009-0003-9012-1438], Maryland Paleontology Collection and Research Center, Calvert Marine Museum, P.O. Box 97, Solomons, Maryland, 20688 USA. Phillip F. Chapman [phillip.f.chapman@dartmouth.edu; ORCID: https://orcid.org/0009-0001-9810-1736], Materials Science and Engineering, Johns Hopkins University, Baltimore, Maryland. Thayer School of Engineering, Dartmouth College, 15 Thayer Drive, Hanover, New Hampshire, 03755 USA (current address). Nathan Spencer [Nathan@syGlass.io; ORCID: https://orcid.org/0009-0001-9917-4670] and Jason E. Osborne [Jason@ syGlass.io; ORCID: https://orcid.org/0009-0008-4748-4352], syGlass, 1405 Earl Core Road PMB 1070, Morgantown, West Virginia, 26506 USA.
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