THE CARBONIFEROUS GONIATITE GENERA
 GIRTYOCERAS
 AND
 EUMORPHOCERAS

Moore, E. W. J.

doi:10.1144/pygs.25.6.387

Cited by 25 publications

(8 citation statements)

References 7 publications

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“…-Equivalent successions in North England contain rich, well-preserved ammonoid faunas in thick basinal shale sequences that have been well documented over the years by Bisat (1924Bisat ( , 1934Bisat ( , 1952 and Moore (1936Moore ( , 1946. They were summarized by Riley (1993) and updated by Korn & Tilsley (2006).…”

Section: Global Correlationsmentioning

confidence: 98%

“…23C). C. arcticum has a wider conch than C. platyforme (Moore, 1946), C. moorei (Nicolaus, 1963), and C. zrigatense Korn & Ebbighausen, 2006, but is more slender than C. darkaouaense Korn, Klug & Mapes, 1999. Type species.…”

Section: B C Amentioning

confidence: 99%

“…Calygirtyoceras zrigatense Korn & Ebbighausen, 2006, also known from Morocco, as well as the European species C. platyforme (Moore, 1946) and C. moorei (Nicolaus, 1963) Gordon,p. 50,pl.…”

Section: B Cmentioning

confidence: 99%

“…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.…”

mentioning

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: Global Correlationsmentioning

confidence: 98%

Section: B C Amentioning

confidence: 99%

“…Calygirtyoceras zrigatense Korn & Ebbighausen, 2006, also known from Morocco, as well as the European species C. platyforme (Moore, 1946) and C. moorei (Nicolaus, 1963) Gordon,p. 50,pl.…”

Section: B Cmentioning

confidence: 99%

mentioning

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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“…This species is associated with the B, forms Goniatites masimus Bisat and Bollandites phillipsi (Bisat) in the B, zone at Wedber Brow, Malham, and with Beyrichoceras on Hill Langerton (Bisat 1934, p. 298). Moore (1946) suggested Sagittoceras to be synonymous with Girfyoceras and referred a specimen from Higher Clough (Cowdale Clough), Barnoldswick, to Girtyoceras cf. discus, stating its horizon (40 ft below a faunal band in P , 3 to be high B, (op.…”

Section: The Unconformity Below the Bowland Shales In The Ashnott-newmentioning

confidence: 99%

The relationship of the Bowland shales to the pendleside limestone in the Clitheroe, Slaidburn and Sykes Anticlines

Parkinson¹

1964

Geological Journal

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The lower carboniferous rocks of ireland

Turner¹

1951

Geological Journal

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Following introductory notes on the historical aspect of the subject, this revicw of Irish Carboniferous Limestone and associated beds discusses the distribution of the principal lithological types in Ireland. The zonal -tigraphy is then reviewed throughout the island, opportunity being taken to incorporate certain unpublished results of recent work. Then follows a A u m f of the history of the period from the palaeogeographical point of view. Detailed bibliographies (a) by counties, (b) of more general papers, are predwed to the paper.

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THE CARBONIFEROUS GONIATITE GENERA GIRTYOCERAS AND EUMORPHOCERAS

Cited by 25 publications

References 7 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 relationship of the Bowland shales to the pendleside limestone in the Clitheroe, Slaidburn and Sykes Anticlines

The lower carboniferous rocks of ireland

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