Early Bashkirian Rugosa (Anthozoa) from the Donets Basin, Ukraine. Part 4. Cordibia, a new protocolonial genus

Fedorowski, Jerzy; Ogar, V.V.

doi:10.2478/agp-2013-0014

Cited by 16 publications

(28 citation statements)

References 2 publications

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“…The Bashkirian recorded the recovery of the rugose corals with the first re-diversification of corals, mainly from solitary species that survived the Serpukhovian extinctions (Fedorowski, 1981;Kossovaya, 1996). The genera are well documented in the Ural Mts and Moscow Basin (Ogar, 1985(Ogar, , 1990Kossovaya, 1996Kossovaya, , 2002, Donets Basin (Fedorowski, 2009a,b, Fedorowski & Vassiljuk 2011, Fedorowski & Ogar, 2013, North America (Armstrong, 1972;Sando, 1985;Stevens, 2012;Fedorowski et al, 2014a,b) and China (Wu & Zhao, 1989;Zhang et al, 2009Zhang et al, , 2010. However, they are poorly known in time-equivalent assemblages from the southern Tethys from northern Africa (Semenoff-Tian-Chansky, 1974;Rodriguez et al, 2013) and East central Iran (Flügel, 1974(Flügel, , 1975(Flügel, , 1994.…”

Section: Introductionmentioning

confidence: 99%

Fasciculate Kleopatrinid corals from the Bashkirian (late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran)

Badpa¹,

Poty²,

Ashouri³

et al. 2016

Rev. bras. paleontol.

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-In the East-Central Iran, the Sardar Formation (upper Visean-Moscovian) consists of shallow-water limestone with intercalations of shale containing rugose corals, tabulate corals and brachiopods. Ten sections were sampled in the Ozbak-kuh Mountains, from north to south. Among the rugose corals, an assemblage of fasciculate Kleopatrinidae has been collected. The latter contains the species: Paraheritschioides antoni antoni, P. antoni minor, P. gracilis and two new species for the genera Fomichevella and Heintzella. Heintzella is described from Iran for the first time. However, its age, as determined by conodonts and foraminifers, is early to middle Bashkirian (early late Carboniferous). The most similar, time-equivalent faunal associations are that of the Ellesmere Island, Sverdrup Basin in Arctic Canada, Alexander terrane and Brooks Range in southeastern Alaska and eastern Klamath terrane in northern California, where similar tropical warm water conditions have been identified during the Bashkirian in the northern hemisphere. During these times central Iran block and Northern provinces, characterized by a dominant carbonate facies and more diversified colonial coral faunas.Key words: Iran, Ozbak-kuh, Sardar, Bashkirian, rugose corals. RESUMO -A Formação Sardar (Viseano superior-Moscoviano) no Irã Central-Leste é caracterizada por calcários de ambientes pouco profundos com intercalações de folhelhos que contêm corais rugosos, tabulados e braquiópodes. Foram estudadas dez amostras das montanhas Ozbak-kuh, de norte a sul. Entre os corais rugosos foi amostrada uma associação de Kleopatrinidae fasciculados, que contém as espécies Paraheritschioides antoni antoni, P. antoni minor, P. gracilis e duas novas espécies novas para os gêneros Fomichevella e Heintzella. O gênero Heintzella é descrito pela primeira vez para o Irã. Contudo, a sua idade, determinada por conodontes e foraminíferos, é Bashkiriano inicial-médio (Neocarbonífero). As associações faunísticas contemporâneas mais semelhantes são as da Ilha de Ellesmere, bacia Sverdrup no Canadá Ártico, Terreno Alexander e Cordilheira Brooks no sudeste de Alasca, e o Terreno Klamath mais a leste na Califórnia setentrional, onde condições de águas quentes tropicais foram identificadas durante o Bashkiriano no hemisfério norte. O bloco central iraniano e as provincias setentrionais, durante este tempo, foram caracterizadas por facies calcárias dominantes e faunas coralinas coloniais diversificadas.

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Section: Introductionmentioning

confidence: 99%

Fasciculate Kleopatrinid corals from the Bashkirian (late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran)

Badpa¹,

Poty²,

Ashouri³

et al. 2016

Rev. bras. paleontol.

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“…The history of the recognition and content of the Bashkirian Stage is available from the earliest of a series of papers dealing with the rugose corals of the Donets Basin (Fedorowski 2009a). Detailed descriptions, faunal contents and some historical details of the Mississippian, Pennsylvanian and lower Permian (Cisuralian) stratotypes in that basin have been pub- Text- fig.…”

Section: Geological Settingmentioning

confidence: 99%

“…Whereas the series of my papers dealing with the rugose corals from the Donets Basin (Fedorowski 2009a(Fedorowski , b, 2016Fedorowski and Vassilyuk 2011;Fedorowski and Ogar 2013) were devoted chiefly to the early Bashkirian taxa, corals investigated in this paper also include a latest Serpukhovian specimen (holotype of Bothrophyllum berestovensis Vassilyuk, 1960) and some earliest Zhuyevskian specimens (Bothrophyllum gorbachevensis sp. nov. and Cystilophophyllum kalmiussi Fomichev, 1953).…”

Section: Introductionmentioning

confidence: 99%

Early Bashkirian Rugosa (Anthozoa) from the Donets Basin (Ukraine). Part 5. The Family Bothrophyllidae Fomichev, 1953

Fedorowski¹

2017

Acta Geologica Polonica

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The taxonomic value of the microstructure of the septa and the necessity for a distinction between that character and diagenetic alterations; 2. Depositional conditions, under which the rugose coral skeletons were deposited; 3. The similarity of skeletal constructions vs. relationships in some taxa of the Subfamily Dibunophyllinae Wang, 1950 and the Family Bothrophyllidae Fomichev, 1953. The lack of final conclusions in the matter of the relationships is due to the incompleteness and restricted number of specimens studied herein and the incomplete investigations of a great majority of the earlier described bothrophyllid taxa.

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“…Most of his conclusions concerning genera, except for the synonymy of Antiphyllum with Claviphyllum are accepted here. Also, an emended diagnosis is introduced combining the main characters of both earlier diagnoses, and the Antiphyllidae are treated as an independent family both here and in earlier papers (Fedorowski, 2009b(Fedorowski, , c, 2010a). …”

Section: Systematic Palaeontology Subclass Rugosa Milne Edwards and Hmentioning

confidence: 99%

On three rugose coral genera from Serpukhovian strata in the Upper Silesian Coal Basin, Poland

Fedorowski¹

2012

Acta Geologica Polonica

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ABSTRACT:Fedorowski, J. 2012. On three rugose coral genera from Serpukhovian strata in the Upper Silesian Coal Basin, Poland. Acta Geologica Polonica, 62 (1), 1-33. WarszawaThe rugose coral specimens included by Schindewolf (1952) in the genera Claviphyllum Hudson, 1942, Fasciculophyllum Thomson, 1883 and Pentaphyllum (Tachylasma) Grabau, 1922 are revised on the basis of the original collection. The first two taxa are included in Antiphyllum Schindewolf, 1952, either in its original sense or in its newly introduced subgenus Antiphyllites. The new genus Effigies is introduced for Pentaphyllum (Tachylasma) silesiacum Schindewolf, 1952. The reasons for placing individual genera within given families and suborders are discussed. New, detailed descriptions of species are supplemented by text-figures in order to document their intraspecific variability and phylogenetic relationships.

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Early Bashkirian Rugosa (Anthozoa) from the Donets Basin, Ukraine. Part 4. Cordibia, a new protocolonial genus

Cited by 16 publications

References 2 publications

Fasciculate Kleopatrinid corals from the Bashkirian (late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran)

Fasciculate Kleopatrinid corals from the Bashkirian (late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran)

Early Bashkirian Rugosa (Anthozoa) from the Donets Basin (Ukraine). Part 5. The Family Bothrophyllidae Fomichev, 1953

On three rugose coral genera from Serpukhovian strata in the Upper Silesian Coal Basin, Poland

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