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Research Article

Unusual plesiosaur vertebrae from the Lower Jurassic Posidonia Shale of Germany

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Received 15 Apr 2023, Accepted 26 Jul 2023, Published online: 17 Aug 2023
 

ABSTRACT

The Toarcian (upper Lower Jurassic) strata of the world-renowned Posidonia Shale of Central Europe have yielded diverse assemblages of marine vertebrates. Some of them, such as those of the Holzmaden area in southwestern Germany, are among the best-preserved specimens of Lower Jurassic vertebrate taxa. Here, we provide a reassessment of ‘Plesiosaurus’ bavaricus, a long-overlooked plesiosaur taxon from the Posidonia Shale of northern Bavaria (southern Germany), established based upon two isolated cervical centra and a caudal vertebra. The cervical material exhibits an intriguing character combination, providing evidence for the presence of a distinct plesiosaur taxon in the upper Lower Jurassic of the Posidonia Shale of Germany. Additionally, we report another isolated cervical vertebra, likewise from the Posidonia Shale of Bavaria, that shows striking similarities to the type cervicals of ‘P’. bavaricus. Following our study of the Bavarian specimens, we hypothesise that, despite their substantial incompleteness, it seems likely that the material belonged to the same taxon, either species or a group of species, distinct from other plesiosaurs known from the Posidonia Shale.

Acknowledgments

We would like to express our gratitude to Thomas Voigt (IGJ) for access to specimens under his care and to Stefan Eggmaier (Urwelt-Museum Oberfranken, Bayreuth, Germany) for information about the historical fossil locality Creez. Oliver Rauhut (BSPHG) is thanked for providing details on the lost syntype specimens of ‘Plesiosaurusbavaricus and Glenn Storrs (Cincinnati Museum Center, Cincinnati, Ohio, USA) kindly provided a copy of Zarnik's (1925) rare publication. We also thank Cristian David Benavides-Cabra and an anonymous reviewer for their helpful comments.

Disclosure statement

No potential conflict of interest was reported by the author(s).

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