2022
DOI: 10.37520/fi.2022.021
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Late Bashkirian ammonoids from the Mospyne Formation of the Donets Basin, Ukraine

Abstract: Eleven late Bashkirian ammonoid taxa (Anthracoceratites sp., Cymoceras sp., Melvilloceras rotaii (Librovitch in Popov, 1979), Gastrioceras angustum Patteisky, 1964, G. lupinum Popov, 1979, G. kutejnikovense Popov, 1979, ?Agastrioceras sp., Bisatoceras sp., ?Owenoceras sp., Branneroceras sp. A, and Branneroceras sp. B), are described from the Mospyne Formation of the Donets Basin, eastern Ukraine. Representatives of the genera Cymoceras, Agastrioceras, Bisatoceras are first recorded from the Carboniferous of th… Show more

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Cited by 3 publications
(5 citation statements)
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“…(see Fig. 5, b) and some unidentified ammonoids, as well as the trace fossils Planolites and Chondrites (Dernov, 2016(Dernov, , 2022b.…”
Section: Studied Fossil Sitesmentioning
confidence: 93%
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“…(see Fig. 5, b) and some unidentified ammonoids, as well as the trace fossils Planolites and Chondrites (Dernov, 2016(Dernov, , 2022b.…”
Section: Studied Fossil Sitesmentioning
confidence: 93%
“…In the study area (upper reaches of the Velyka Kamianka river), the upper boundary is located in the stratigraphic interval corresponding to the lower half of the coal-bearing Mospyne Formation (early late Bashkirian) (Dernov, 2022b). This area is characterised by rapid lateral replacement of the Dyakove Group in the northern and northwestern directions by the coal-bearing Amvrosiyivka, Mandrykyne and Mospyne formations (see Fig.…”
Section: Geological Settingmentioning
confidence: 99%
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“…The Mospyne Formation corresponds to the lower part of the Zuyivkian Horizon (lower half of the Kayalian Regional Stage) of the Regional Stratigraphic Scheme of the Dnipro-Donets Downwarp (Poletaev et al, 2011;Nemyrovska & Yefimenko, 2013). This formation contains remains of typical Langsettian terrestrial plants (Novik, 1974;Dernov & Udovychenko, 2019a) and ammonoids (Popov, 1979;Dernov, 2022b), the non-marine bivalves of the upper part of the lenisulcata Zone and the lower part of the communis Zone (Dernov, 2022a), the late Bashkirian conodonts (Nemyrovska, 1999), and other marine and terrestrial biota, such as miospores, foraminifers, corals, bryozoans, brachiopods, scaphopods, gastropods, horseshoe crabs, millipedes, insects and fishes.…”
Section: Geological Setting and Materialsmentioning
confidence: 99%
“…Rocks of the Mospyne Formation contain remains of typical Langsettian terrestrial plants (Novik 1974, Dernov andUdovychenko 2019, etc. ) and ammonoids (Popov 1979, Dernov 2022c), non-marine bivalves of the upper part of the lenisulcata Zone and lower part of the communis Zone (Dernov 2022b), late Bashkirian conodonts (Nemyrovska 1999), and other marine and terrestrial biota, e.g., miospores, foraminifers, corals, bryozoans, brachiopods, scaphopods, gastropods, trilobites, horseshoe crabs, millipedes, insects, and fishes.…”
Section: Geological Settingsmentioning
confidence: 99%