Fossil marine vertebrates (Chondrichthyes, Actinopterygii, Reptilia) from the Upper Cretaceous of Akkermanovka (Orenburg Oblast, Southern Urals, Russia)

• Published in: Cretaceous research Vol. 155; p. 105779
• Main Authors: Jambura, Patrick L, Solonin, Sergey V, Cooper, Samuel L A, Mychko, Eduard V, Arkhangelsky, Maxim S, Türtscher, Julia, Amadori, Manuel, Stumpf, Sebastian, Vodorezov, Alexey V, Kriwet, Jürgen
• Format: Journal Article
• Language: English
• Published: England 01.03.2024
• Subjects: Santonian–?early Campanian; Elasmobranchii; Polycotylidae; Lepisosteidae; Mosasauridae; Teleostei
• ISSN: 0195-6671; 1095-998X
• DOI: 10.1016/j.cretres.2023.105779

Upper Cretaceous coastal marine deposits are widespread in the Southern Urals with a number of marine vertebrates previously reported from this region. However, previous studies on the vertebrate faunas in this region often lack detailed taxonomic descriptions and illustrations, rendering comparisons to other faunal assemblages difficult. A new diverse vertebrate assemblage comprising cartilaginous and bony fishes, as well as marine reptiles, is described here from the Orenburg region near Akkermanovka (Southern Urals, Russia). Thirty five taxa are identified, including three holocephalans ( sp., , Chimaeroid indet.), two hybodontiform sharks ( sp., cf. sp.), 17 neoselachians ( cf. sp., sp., ex gr. . cf. ), a holostean (Lepisosteidae indet.), nine teleosts ( sp., Saurodontidae indet., cf. sp., Pachyrhizodontidae indet., . cf. . spp., Alepisauroidei indet.), two plesiosaurs (Polycotylidae indet., Plesiosauria indet.), and one mosasaurid (Tylosaurinae indet.). Based on the faunal assemblage, a Santonian-?early Campanian age is proposed. Lamniform sharks are the best represented group in terms of taxic diversity and relative abundance, probably reflecting the peak in diversity this group experienced following the Cenomanian radiation in the Late Cretaceous. The faunal assemblage of Akkermanovka exhibits significant taxonomic overlaps with assemblages reported from Asia and North America, but not from Southern Hemisphere continents, indicating east-west dispersal of several marine taxa during the Late Cretaceous.