THE GONIATITES OF THE
 BEYRICHOCERAS
 ZONE IN THE NORTH OF ENGLAND

Bisat, W. S.

doi:10.1144/pygs.22.4.280

Cited by 47 publications

(16 citation statements)

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“…Recent collecting at this locality by David M. Work and ALT has secured the previously reported Bollandites greencastlensis (Miller & Gurley, 1896), Bollandites phillipsi (Bisat, 1934) and Prolecanites americanus Miller & Garner, 1953 (P. serpentinus of Knapp 1965), along with a crenistriate variety of Goniatites (cf. G. americanus ) and primitive Kazakhoceras that are the earliest known records for the latter genus in the world.…”

Section: Illinois Basinsupporting

confidence: 53%

“…-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%

“…Genevieve Formation (earliest Chesterian) and contain essentially the same assemblage. Knapp (1965) reviewed the Greencastle assemblage, added Bollandites phillipsi (Bisat, 1934) and Prolecanites serpentinus (Phillips, 1836) to the species list, and concluded that Goniatites greencastlensis, owing to its widely umbilicate juvenile stage and narrow ventral lobe of the suture, doesn't belong in Goniatites. We currently see no reason why Goniatites greencastlensis Miller & Gurley, 1896 should not be referred to the genus Bollandites, even though it is one of the widest shelled species in the generic complex.…”

Section: Illinois Basinmentioning

confidence: 99%

“…-Beyrichoceras submicronotum Bisat, 1934 (original designation); subjective junior synonym of Bollandoceras micronotum (Phillips, 1836).…”

Section: Genus Bollandoceras Bisat 1952mentioning

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.…”

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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: Illinois Basinsupporting

confidence: 53%

Section: Global Correlationsmentioning

confidence: 98%

Section: Illinois Basinmentioning

confidence: 99%

“…-Beyrichoceras submicronotum Bisat, 1934 (original designation); subjective junior synonym of Bollandoceras micronotum (Phillips, 1836).…”

Section: Genus Bollandoceras Bisat 1952mentioning

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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Correlation of Mississippian (Upper Viséan) foraminiferan, conodont, miospore and ammonoid zonal schemes, and correlation with the Asbian–Brigantian boundary in northwest Ireland

Cózar¹,

Somerville

Mitchell

et al. 2006

Geological Journal

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The microbiota of the upper Viséan (Asbian-Brigantian) rocks in the Lough Allen Basin in northwest Ireland is analysed. The Middle Mississippian sequence studied extends from the upper part of the Dartry Limestone/Bricklieve Limestone formations of the Tyrone Group to the Carraun Shale Formation of the Leitrim Group. The rocks have been traditionally dated by ammonoid faunas representing the B 2a to P 2c subzones. The Meenymore Formation (base of the Leitrim Group) also contains conodont faunas of the informal partial-range Mestognathus bipluti zone. The upper Brigantian Lochriea nodosa Conodont Zone was recognized by previous authors in the middle of the Carraun Shale Formation (Ardvarney Limestone Member), where it coincides with upper Brigantian ammonoids of the Lusitanoceras granosus Subzone (P 2a ). Foraminifera and algae in the top of the Dartry Limestone Formation are assigned to the upper Cf6 Foraminifera Subzone (highest Asbian), whereas those in the Meenymore Formation belong to the lower Cf6 Foraminifera Subzone (lower Brigantian). The Dartry Limestone FormationMeenymore Formation boundary is thus correlated with the Asbian-Brigantian boundary in northwest Ireland. For the first time, based on new data, a correlation between the ammonoid, miospore, foraminiferan and conodont zonal schemes is demonstrated. The foraminiferans and algae, conodonts and ammonoids are compared with those from other basins in Ireland, northern England, and the German Rhenish Massif. Historically, the Asbian-Brigantian boundary has been correlated with several levels within the P 1a Ammonoid Subzone. However, the new integrated biostratigraphical data indicate that the AsbianBrigantian boundary in northwest Ireland is probably located within the B 2a Ammonoid Subzone and the NM Miospore Zone, but the scarcity of ammonoids in the Tyrone Group precludes an accurate placement of that boundary within this subzone.

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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 GONIATITES OF THE BEYRICHOCERAS ZONE IN THE NORTH OF ENGLAND

Cited by 47 publications

References 0 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)

Correlation of Mississippian (Upper Viséan) foraminiferan, conodont, miospore and ammonoid zonal schemes, and correlation with the Asbian–Brigantian boundary in northwest Ireland

The lower carboniferous rocks of ireland

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