New data on the Carboniferous corals of the Donets Basin

Ogar, V.V.

doi:10.1016/j.palwor.2010.08.001

Cited by 10 publications

(14 citation statements)

References 2 publications

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“…Pennsylvanian, Novaya Zemlya and Moscow Basin, Russia (Chwieduk, 2014); lower Gzhelian, Donets Basin, Ukraine (Ogar, 2010); Gzhelian–lower Permian, Spitsbergen, Norway (Chwieduk, 2014).…”

Section: Systematic Paleontologymentioning

confidence: 99%

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

Wang¹,

Gorgij

Yao

2018

J. Paleontol.

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Twelve rugose coral species belonging to seven genera are described and discussed based on 70 thin sections of 32 specimens collected from the Anarak section, northeast of Nain, Esfahan Province, Yazd Block, central Iran. These species include two new colonial rugose coral species,Antheria fedorowskiiandAntheria robusta, and five previously named species of colonial rugose corals,Antheria lanceolataandStreptophyllidium scitulum, and solitary rugose corals,Arctophyllum jiangsiense,Caninophyllumcf.somtaiense, andPseudotimania delicata. Five species are left in open nomenclature:Antheriasp.,Arctophyllumsp.,Caninophyllumsp.,Nephelophyllumsp., andYakovleviellasp. These Iranian corals are associated with the fusulinidsRauserites(several species) andUltradaixina bosbytauensis, indicating a latest Carboniferous age (Gzhelian age). All the described genera and named species belong to the families Aulophyllidae, Bothrophyllidae, Cyathopsidae, and Kepingophyllidae, among which the family Kepingophyllidae has been previously documented only from China and Indochina. They are typical representatives of the Cathaysian rugose fauna, which was widely developed around the South China and Indochina blocks near the paleoequator and was absent from the Gondwanan and Cimmerian continents in high latitudes during the Late Pennsylvanian. Hence, the occurrence of the Cathaysian fauna from central Iran in the latest Carboniferous suggests that it may have had a close biogeographical connection with China and Indochina, which further implies its latitudinal position intermediate between the Gondwanan continent and South China and Indochina blocks during this time.UUID:http://zoobank.org/5257d2bb-1346-4dee-8f3e-f4b1b33ba5a9

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“…Pennsylvanian, Novaya Zemlya and Moscow Basin, Russia (Chwieduk, 2014); lower Gzhelian, Donets Basin, Ukraine (Ogar, 2010); Gzhelian–lower Permian, Spitsbergen, Norway (Chwieduk, 2014).…”

Section: Systematic Paleontologymentioning

confidence: 99%

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

Wang¹,

Gorgij

Yao

2018

J. Paleontol.

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“…Considering the morphological similarity Corphalia simplex (Perna, 1923) and Dorlodotia pseudovermiculare (McCoy, 1849) as well their distribution in the adjacent horizons of the Tournaisian and Viséan on the eastern slope of the Southern Urals (Kachanov, 1965) and the Donets Basin (Ogar, 2010), the phylogenetic relationships of these species is very probable. In this case Corphalia simplex could be an ancestor of acolumellate Dorlodotia as suggested by .…”

Section: Phylogenymentioning

confidence: 99%

“…The stratigraphic distribution of corals taxa in the Tournaisian strata is highly heterogeneous. Most corals are found in the middle part of the Tournaisian (C 1 t c Zone) (Ogar, 2010). In the lower and upper parts of the Tournaisian, corals are much rarer.…”

Section: Introductionmentioning

confidence: 99%

New Rugose corals and refinements of the Tournaisian biostratigraphy of the Donets Basin (Ukraine)

Ogar¹

2016

Geol. Belg.

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ABSTRACT. Specimens collected by Vassilyuk from the lower part of the Tournaisian strata of the southern Donets Basin and described as Campophyllum caninoides Sibly are re-examined. These specimens re-attributed to the Conilophyllum priscum (Münster, 1840), which is a well-known species in the lower part of the Lower Tournaisian of Western and Eastern Europe, Kazakhstan, North America and China (Junggar). Corphalia simplex (Perna, 1923) is for the first time identified at the top of Tournaisian in the Donets Basin. This species was described at similar stratigraphic levels on the eastern slope of the Southern Urals and in Belgium. The application of described species for interregional correlation of the Tournaisian subdivisions is discussed herein. Evolutionary relations between Corphalia and Dorlodotia near the Tournasian-Viséan boundary have been confirmed indirectly.

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“…All regions under consideration possess one or the other but never both species. S. junceum is the typical small-sized species in the Western Europe Province of Sando (1990) while S. asiaticum has a wide distribution through the Hill (1938Hill ( -1941, ; Nova Scotia: Lewis (1935) and Poty (2002) Said et al 2013); Sahara: Semenoff-Tian-Chansky (1985), Aretz (2011), Aretz et al (2013); Poland: Khoa (1977); Donets Basin: Vassiljuk (1960), Ogar (2010); Ural Mountains and Novaya Zemlya: Gorsky (1938Gorsky ( , 1978Russian Platform: Dobroljubova (1958);Kuznetsk: Fomichev (1931), Dobroljubova et al (1966); Kazakhstan: Bykova (1966), Volkova (1941);Siberia and Omolon: Ivanowski (1967), Onoprienko (1976), Conil et al (1982); S China and Thailand: Yü (1933), Fan et al (2003), Lin et al (2012), Fontaine et al (1991). …”

Section: Phylogenymentioning

confidence: 99%

Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bartın (NW Turkey)

Denayer¹

2014

Bull. Geosci.

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New data on the Carboniferous corals of the Donets Basin

Cited by 10 publications

References 2 publications

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

New Rugose corals and refinements of the Tournaisian biostratigraphy of the Donets Basin (Ukraine)

Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bartın (NW Turkey)

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New data on the Carboniferous corals of the Donets Basin

Cited by 10 publications

References 2 publications

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

New Rugose corals and refinements of the Tournaisian biostratigraphy of the Donets Basin (Ukraine)

Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bart&#305;n (NW Turkey)

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Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bartın (NW Turkey)