VIII.—<i>Descriptions of the type-specimens of some carboniferous corals of the genera</i>“Diphyphyllum,” “Stylastræa,” Aulophyllum,<i>and</i>Chætetes

Smith, Stanley G.; Lang, W. D.

doi:10.1080/00222933008673118

Cited by 12 publications

(8 citation statements)

References 7 publications

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“…Our form does not differ greatly from Caninia gophiae Heritsch (1936e) from the Permian of the Carnic Alps, Caninia juddi Thomson, emended by Lewis (1924), common in the Visean of Britain, and Caninia sp. described by Smith (1935) from Permian of Canada, and somewhat similar forms in the Upper Carboniferous of Central Russia, the Urals and Timan (see Stuckenberg 1895Stuckenberg , 1904. HoRIZON Two transverse sections have been cut not far apart in the proximal part.…”

Section: "L No 2]mentioning

confidence: 88%

“…the genotype see Carruthers (1908), and for description and figures of Carboniferous species of Caninia, see Salée (1910) and Lewis (1924), and of Permian species of Caninia, see Stuckenberg (1895,1904), Heritsch (1936c) and Smith (1935). DEScRIPTION.…”

Section: Remarks the Present Species Differs From The Wesleo Form Inmentioning

confidence: 99%

“…This suggests that it belongs to the genus Amygdalophyllurn but the specimen is too imperfect to make exact specific determination. HORIZON The coral Waagenophyllum is considered as a characteristic genus of the Middle and Upper Permian and as evidence of a Tethyau facies through recently studied by Reed (1925), Smith (1935), Heritach (1933b, 1933c, 1936, Huang (1932*), Grabau (1931), Douglas (1936) and others.…”

Section: The Genus Was Found By Dun and Benson (1920) For A Lowermentioning

confidence: 99%

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Permian Corals from South‐Eastern Yunnan^*

1938

Bulletin of the Geological Society of China

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Section: "L No 2]mentioning

confidence: 88%

Section: Remarks the Present Species Differs From The Wesleo Form Inmentioning

confidence: 99%

Section: The Genus Was Found By Dun and Benson (1920) For A Lowermentioning

confidence: 99%

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Permian Corals from South‐Eastern Yunnan^*

1938

Bulletin of the Geological Society of China

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“…Dimorphism has been suspected but not always convincingly demonstrated in numerous rugose coral species. Appropriate in this regard is reference to the "genomorph concept" of Smith and Lang (1930) which was based upon Carboniferous coral genera in which aberrant corallites or parts of corallites have the appearance of another genus. Critical reviews (Rozkowska, 1960;Wilson, 1963;Oliver, 1968) have not encouraged use of genomorph in a taxonomic sense as advocated by its authors.…”

Section: Growth Changes and Reproductive Featuresmentioning

confidence: 99%

Lower and lower Middle Devonian rugose corals of the central Great Basin

Merriam¹

1974

Professional Paper

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“…It provided the type material for the genus Corwenia and for figured examples of Orionastraea phillipsi (cited as Phillipsastraea radiatus in earlier lists) and Diphyphyllum (e.g. Smith and Ryder, ; Smith and Lang, ; Kato and Mitchell, ). Earlier reviews of the North Wales Visean succession (e.g.…”

Section: Previous Researchmentioning

confidence: 99%

The Corwen Outlier and its implications for the Mid Mississippian palaeogeography of North Wales, UK

Davies

Riley

Wilson³

2013

Geol. J.

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The isolated outlier of Visean (Mid Mississippian) limestones and sandstones near Corwen, North Wales, UK, provides a critical constraint on regional tectonic and palaeogeographical models. The late Asbian to Brigantian succession comprises a series of shoaling-upwards cycles (parasequences). These were the product of forced, glacioeustatic regressions and have boundaries that testify to emergence, karstic dissolution and soil formation on a low gradient carbonate platform prior to flooding and the resumption of marine deposition. The recognition of two of the main marker beds within the North Wales Visean succession (Main Shale and Coral Bed) together with a newly applied foraminiferal and algal biozonation allow the outlier succession to be correlated with other Visean outcrops in the region and more widely throughout the British Isles. In revealing regional thickness and facies variations, these comparisons show that the outlier succession was deposited landward of the early Asbian shoreline in a region of enhanced subsidence localized along the Bala Lineament. The Corwen Outlier suggests that, within narrow gulfs associated with the region's major tectonic lineaments, Mississippian carbonate facies extended farther south into the contemporary hinterland of older rocks and that, in response to Brigantian climate change, these topographic features likely also influenced fluvial catchments supplying siliciclastic sediment to the platform's landward margin and, subsequently, Namurian deltas. Contrary to earlier suggestions, Visean outcrop patterns, facies distributions and thicknesses in the vicinity of the Bala Lineament can be explained without the need to invoke extensive post-depositional lateral displacements. BGS ? NERC 2013. Geological Journal ? John Wiley & Sons Ltd.Peer reviewe

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VIII.—Descriptions of the type-specimens of some carboniferous corals of the genera“Diphyphyllum,” “Stylastræa,” Aulophyllum,andChætetes

Cited by 12 publications

References 7 publications

Permian Corals from South‐Eastern Yunnan^*

Permian Corals from South‐Eastern Yunnan^*

Lower and lower Middle Devonian rugose corals of the central Great Basin

The Corwen Outlier and its implications for the Mid Mississippian palaeogeography of North Wales, UK

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VIII.—Descriptions of the type-specimens of some carboniferous corals of the genera“Diphyphyllum,” “Stylastræa,” Aulophyllum,andChætetes

Cited by 12 publications

References 7 publications

Permian Corals from South‐Eastern Yunnan*

Permian Corals from South‐Eastern Yunnan*

Lower and lower Middle Devonian rugose corals of the central Great Basin

The Corwen Outlier and its implications for the Mid Mississippian palaeogeography of North Wales, UK

Contact Info

Product

Resources

About

Permian Corals from South‐Eastern Yunnan^*

Permian Corals from South‐Eastern Yunnan^*