Callovian Marine Reptiles of European Russia

Author:

Zverkov Nikolay1,Arkhangelsky Maxim23,Gulyaev Denis4,Ippolitov Alexey156ORCID,Shmakov Alexey7

Affiliation:

1. Geological Institute of the Russian Academy of Sciences, Pyzhevsky Lane 7, Moscow 119017, Russia

2. Department of General Geology and Minerals, Saratov State University, Astrakhanskaya Str. 83, Saratov 410012, Russia

3. Department of Oil and Gas, Saratov State Technical University, Politekhnicheskaya Str. 77, Saratov 410054, Russia

4. Commission on Jurassic System of the Interdepartmental Stratigraphical Committee (ISC) of Russia, Chekhova St., 25/7, Yaroslavl 150054, Russia

5. School of Geography, Environment and Earth Sciences, Victoria University of Wellington Te Herenga Waka, 21 Kelburn Parade, Wellington 6012, New Zealand

6. Institute of Geology and Petroleum Technologies, Kazan Federal University, Kremlevskaya St., 18, Kazan 420008, Russia

7. Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya St., 123, Moscow 117997, Russia

Abstract

Our knowledge of marine reptiles of the Callovian age (Middle Jurassic) is majorly based on the collections from the Oxford Clay Formation of England, which yielded a diverse marine reptile fauna of plesiosaurians, ichthyosaurians, and thalattosuchians. However, outside of Western Europe, marine reptile remains of this age are poorly known. Here, we survey marine reptiles from the Callovian stage of European Russia. The fossils collected over more than a century from 28 localities are largely represented by isolated bones and teeth, although partial skeletons are also known. In addition to the previously described rhomaleosaurid and metriorhynchids, we identify pliosaurids of the genera Liopleurodon and Simolestes; cryptoclidid plesiosaurians, including Cryptoclidus eurymerus, Muraenosaurus sp., and cf. Tricleidus, and ophthalmosaurid ichthyosaurians, including the iconic Ophthalmosaurus icenicus. These findings expand the ranges of several Callovian marine reptile taxa far to the Eastern Europe, and support the exchange of marine reptile faunas between Western and Eastern European seas in the middle to late Callovian. However, some specimens from the lower Callovian of European Russia show differences from typical representatives of the middle Callovian Oxford Clay fauna, possibly representing the earlier stages of evolution of some of these marine reptiles not yet recorded in Western Europe or elsewhere.

Funder

Geological Institute

Kazan Federal University Strategic Academic Leadership Program

Publisher

MDPI AG

Reference145 articles.

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4. Andrews, C.W. (1910). A Descriptive Catalogue of the Marine Reptiles of the Oxford Clay. Part 1, British Museum (Natural History).

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