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1995
DOI: 10.1016/s0016-6995(95)80137-5
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Middle/Late Devonian Phoebodontbased ichthyolith zonation

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Cited by 17 publications
(19 citation statements)
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“…A diverse Frasnian microvertebrate fauna has also been recorded by Trinajstic and George (2009) with scales of the thelodont Australolepis seddoni Turner and Dring, 1981 recorded as occurring with conodont elements and phoebodont teeth for the first time, thus allowing the age of A. seddoni to be constrained to MN 4-10 CZ. The phoebodont teeth were also correlated to the known phoebodont based zonation of Ginter and Ivanov (1995a).…”
Section: Horse Springmentioning
confidence: 99%
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“…A diverse Frasnian microvertebrate fauna has also been recorded by Trinajstic and George (2009) with scales of the thelodont Australolepis seddoni Turner and Dring, 1981 recorded as occurring with conodont elements and phoebodont teeth for the first time, thus allowing the age of A. seddoni to be constrained to MN 4-10 CZ. The phoebodont teeth were also correlated to the known phoebodont based zonation of Ginter and Ivanov (1995a).…”
Section: Horse Springmentioning
confidence: 99%
“…Furthermore, a Late Devonian zonation scheme based on phoebodont sharks has been established from the Frasnian to the end Famennian Jones and Turner 2000;Young and Turner 2000). Where known, the Devonian shark fauna of Western Australia (Trinajstic and George 2009;Trinajstic et al 2014) has been correlated to the Frasnian phoebodont zonation of Ginter and Ivanov (1995a). However, to date little work has been published on Famennian shark taxa from Western Australia.…”
mentioning
confidence: 99%
“…C. A South Urals specialty is Ph. latus Ginter and Ivanov, 1995, which predominates in the lower part of the Upper Frasnian and then gradually gives way to Ph. bifurcatus.…”
Section: Discussionmentioning
confidence: 99%
“…thomasi Turner resulted in its identification as Cladodoides wildungensis Jaekel. Ginter and Ivanov (1995) proposed a zonal scale based on Phoebodus representatives, which was tested in many regions of the world. The investigations in the Kuznetsk coal basin made it possible to specify this scale (Ivanov and Rodina, 2002), which is now accepted as a zonal scale on sharks (Becker et al, 2012).…”
Section: Geological Reviewmentioning
confidence: 99%
“…Bar is 0.1 mm. (1) Nanicella tchernyshevae Lipina, Sample T041 4/1, thin section 3; (2, 3) Nanicella porrecta E. Bykova: (2) Sample T041 5/3, thin section 9; (3) Sample T041 1/61, thin section 14; (4) Semitextularia minuta E. Bykova, Sam ple T041 1/2, thin section 1; (5-7) Nanicella tchernyshevae Lipina: (5) Sample T041 6/1, thin section 1; (6) Sample T041 5/1, thin section 4; (7) Sample T041 7/1, thin section 3; (8) Nanicella sp., Sample T041 1/1, thin section 1; (9) Multiseptida corallina E. Bykova, Sample T041 3/7, thin section 4; (10-13) Eonodosaria evlanensis Lipina: (10) Sample T041 7/3, thin section 8; (11) Sample T041 9/1, thin section 8; (12) Sample T041 7/3, thin section 12; (13) Sample T041 4/2, thin section 6; (14) Eono dosaria sp., Sample T041 4/1, thin section 1; (15-18) Eogenitzina devonica Lipina: (15) Sample T041 11/1, thin section 1; (16) Sample T041 4/1, thin section 1; (17) Sample T041 7/2, thin section 9; (18) Sample T041 7/2, thin section 11; Ginter and Ivanov (1995) were the first to propose a zonal scale based on the distribution of Devonian Elasmobranchii remains belonging to the genus Phoe bodus in pelagic facies of Poland, the Southern Urals, and the Timan Range. This zonal succession was sub sequently specified owing to data on the distribution of Chondrichthyes remains in the Kuznetsk coal basin (Ivanov and Rodina, 2002).…”
Section: Famennian Stage Diplosphaerina Magna Zonementioning
confidence: 99%