Dimorphoceratidae From the Upper Visean Shales of County Leitrim, Eire

Moore, E. W. J.

doi:10.1144/pygs.31.3.219

Cited by 6 publications

(8 citation statements)

References 2 publications

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“…-Metadimorphoceras richardsi belongs to the simple-sutured species of the genus (Manger 1988), showing a degree of complexity comparable to the late Asbian (British P 1 a Zone) M. pseudodiscrepans (Moore, 1939), which, however, already shows a further subdivision of the external lobe. A similar complexity stage, but also with a weak tertiary subdivision of the external lobe, is visible in the early Brigantian M. hodsoni Moore, 1958. This shows that M. richardsi obviously represents a very early stage in the diversification of the genus Metadimorphoceras.…”

Section: Metadimorphoceras Richardsi Sp Novmentioning

confidence: 56%

“…The genus ranges through a large part of the late Viséan (Asbian and early Brigantian equivalent) and has been reported from the European North Variscan basins such as the British Isles (e.g. Bisat 1924Bisat , 1934Bisat , 1952Moore 1936Moore , 1946Moore , 1952Moore , 1958Hodson & Moore 1959), the Rhenish Mountains (e.g. Brüning 1923;Schmidt 1925;Nicolaus 1963;Korn 1988Korn , 1990Korn , 1997a, the Ardennes (e.g.…”

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confidence: 99%

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Goniatites Zone (middle Mississippian) ammonoids of the Antler Foreland Basin (Nevada, Utah)

Korn¹,

Titus²

2011

Bull. Geosci.

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The ammonoid faunas from the Goniatites Zone (Late Viséan; Mississippian) of the Camp Canyon Member (Chainman Formation) are described for the first time. The assemblage shows close relationships to time equivalent occurrences in Alaska and the American Midcontinent, but differs markedly from occurrences in Europe, North Africa, and the South Urals. Seven successive ammonoid biozones are proposed for this interval in North America, in ascending order: (1) Calygirtyoceras confusionense Ammonoid Biozone, (2) Calygirtyoceras arcticum Ammonoid Biozone, (3) Girtyoceras primum Ammonoid Biozone, (4) Girtyoceras gordoni Ammonoid Biozone, (5) Goniatites deceptus Ammonoid Biozone, (6) Goniatites eganensis Ammonoid Biozone, and (7) Goniatites multiliratus Ammonoid Biozone. The following ammonoid species are revised or newly described: Bollandoceras occidentale sp. nov., Entogonites burbankensis sp. nov., Entogonites borealis (Gordon, 1957), Entogonites acus sp. nov., Calygirtyoceras confusionense sp. nov., Calygirtyoceras arcticum Gordon, 1957, Girtyoceras primum sp. nov., Girtyoceras gordoni sp. nov., Girtyoceras hamiltonense sp. nov., Dimorphoceras worki sp. nov., Dimorphoceras rileyi sp. nov., Metadimorphoceras mangeri sp. nov., Metadimorphoceras richardsi sp. nov., Kazakhoceras bylundi sp. nov., Goniatites americanus Gordon, 1971, Goniatites deceptus sp. nov., Goniatites eganensis sp. nov., Goniatites sowerbyi sp. nov., and Praedaraelites loeblichi (Miller and Furnish, 1940)

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Section: Metadimorphoceras Richardsi Sp Novmentioning

confidence: 56%

mentioning

confidence: 99%

Goniatites Zone (middle Mississippian) ammonoids of the Antler Foreland Basin (Nevada, Utah)

Korn¹,

Titus²

2011

Bull. Geosci.

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“…pseudodiscrepans (Moore, 1939): with incipient subdivision of the E1 lobe; M. hodsoni (Moore, 1958): with bifid, narrow E1 lobe; M. wiswellense (Moore, 1939): with denticulation of the E1 lobe; M. moorei (Hodson, 1954): with bifid, wide E1 lobe.…”

Section: Sulcogirtyoceras Ruzhencev 1960mentioning

confidence: 99%

The Early Carboniferous (Mississippian) ammonoids from the Chebket el Hamra (Jerada Basin, Morocco)

Korn

Ebbighausen²

2008

Fossil Record

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Five Late Viséan ammonoid assemblages of North Variscan provenance are described from the locality Chebket el Hamra (Jerada Basin, north‐eastern Morocco). These assemblages are composed of 27 species of the genera Eoglyphioceras, Girtyoceras, Sulcogirtyoceras, Metadimorphoceras, Goniatites, Arnsbergites, Hibernicoceras, Paraglyphioceras, Lusitanoceras, Sudeticeras, Neoglyphioceras, Lusitanites, Ferganoceras, Praedaraelites, and Pronorites. The new subfamily Arnsbergitinae is described, as well as the thirteen new species Eoglyphioceras minutum n. sp., Girtyoceras ibnkhaldouni n. sp., Metadimorphoceras anguinosum n. sp., Arnsbergites ferrus n. sp., Arnsbergites proiecturus n. sp., Arnsbergites rufus n. sp., Hibernicoceras touissitense n. sp., Hibernicoceras artilobatum n. sp., Paraglyphioceras celeris n. sp., Lusitanoceras zirari n. sp., Sudeticeras ibnbajjahi n. sp., Sudeticeras horoni n. sp., and Pronorites owodenkoi n. sp. (© 2008 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)

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“…Superfamily Dimorphoceratoidea Hyatt, 1884Family Dimorphoceratidae Wedekind, 1918 Metadimorphoceras Moore, 1958 Type species. Goniatites splendidus Brown, 1841.…”

Section: Figure 11mentioning

confidence: 99%

The Early Carboniferous (Mississippian) ammonoids from the Chebket el Hamra (Jerada Basin, Morocco)

Korn

Ebbighausen²

2008

Foss. Rec.

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Dimorphoceratidae From the Upper Visean Shales of County Leitrim, Eire

Cited by 6 publications

References 2 publications

Goniatites Zone (middle Mississippian) ammonoids of the Antler Foreland Basin (Nevada, Utah)

Goniatites Zone (middle Mississippian) ammonoids of the Antler Foreland Basin (Nevada, Utah)

The Early Carboniferous (Mississippian) ammonoids from the Chebket el Hamra (Jerada Basin, Morocco)

The Early Carboniferous (Mississippian) ammonoids from the Chebket el Hamra (Jerada Basin, Morocco)

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