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The squamation of “Ctenacanthus” costellatus (Chondrichthyes: Ctenacanthiformes) from the Carboniferous of Lublin area, south-eastern Poland

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EN
Abstrakty
EN
A sample of late Viséan limestone from the Włodawa IG-4 borehole, east of Lublin, Poland, yielded a piece of a tooth and a few hundred well-preserved scales comparable to those of “Ctenacanthus” costellatus Traquair, 1884 from Glencartholm, Scotland, UK. Most of the scales are typical compound body scales of the ctenacanthid type. Their crowns are composed of several separate odontodes whose distal ends are turned backwards and bases are characterised by concave undersides. In the material, there are also sparse scales with similar crowns but with flat or convex bulbous bases, as well as ornamented plates and single, star-like denticles, probably from the head region. The taxonomic status of “Ctenacanthus” costellatus was analysed and a new generic name for that species, viz. Glencartius gen. nov., is proposed.
Rocznik
Strony
571--582
Opis fizyczny
Bibliogr. 41 poz., rys.
Twórcy
  • Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland
  • Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland
Bibliografia
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  • 23. Maisey, J.G. 1981. Studies on the Paleozoic selachian genus Ctenacanthus Agassiz: No. 1. Historical review and revised diagnosis of Ctenacanthus, with a list of referred taxa. American Museum Novitates, 2718, 1-26.
  • 24. Maisey, J.G. 1982. Studies on the Paleozoic selachian genus Ctenacanthus Agassiz: No. 2. Bythiacanthus St. John and Worthen, Amelacanthus, new genus, Eunemacanthus St. John and Worthen, Sphenacanthus Agassiz, and Wodnika Münster. American Museum Novitates, 2722, 1-24.
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  • 32. Reif, W.-E. 1978. Types of morphogenesis of the dermal skeleton in fossil sharks. Paläontologische Zeitschrift, 52, 110-128.
  • 33. Shvetsov, M.S. and Birina, L.M. 1935. On the petrology and origin of the Oka Limestone in the Mikhailov-Aleksin region. Trudy Moskovskogo Geologicheskogo Tresta, 10, 1-86. [In Russian]
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  • 35. Skompski, S. 1996. Stratigraphic position and facies significance of the limestone bands in the subsurface Carboniferous succession of the Lublin Upland. Acta Geologica Polonica, 46, 171-268.
  • 36. Traquair, R.H. 1884. Description of a fossil shark (Ctenacanthus costellatus) from the Lower Carboniferous rocks of Eskdale, Dumfrieshire. Geological Magazine, (3), 1, 3-8.
  • 37. Waksmundzka, M.I. 2010. Sequence stratigraphy of Carboniferous paralic deposits in the Lublin Basin (SE Poland). Acta Geologica Polonica, 60, 557-597.
  • 38. Waksmundzka, M.I. 2013. Carboniferous coarsening-upward and non-gradational cyclothems in the Lublin Basin (SE Poland): Palaeoclimatic implications. Geological Society Special Publication, 376, 141-175.
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Uwagi
PL
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-159a5a08-8306-4529-975b-b53e3a39d82d
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