Paleontology and Microfacies of the Serpukhovian in the Verkhnyaya Kardailovka Section, South Urals, Russia: potential candidate for the GSSP for the Visean-Serpukhovian boundary

Nikolaeva, Svetlana; Kulagina, Elena I.; Pazukhin, V. N.; Kochetova, N. N.; Konovalova, V. A.

doi:10.1127/0078-0421/2009/0043-0165

Cited by 48 publications

(44 citation statements)

References 13 publications

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“…Tournaisian; SERP. Serpukhovian et al 2006;Nikolaeva et al 2009;Korn and Titus 2011). The South Urals show very diverse latest Viséan ammonoid assemblages, which at the generic and species level outnumber all of the other regions and thus possess a unique position (Ruzhencev and Bogoslovskaya 1971a).…”

Section: Viséanmentioning

confidence: 92%

“…In other areas, such as the NW Territories of Canada (Nassichuk 1975), the western United States (Youngquist 1949;Titus 2000;Titus and Manger 2001), the American Midcontinent (Gordon 1965;Saunders 1973;Saunders et al 1977;Manger and Saunders 1980), the Cantabrian Mountains (Kullmann 1962), Novaya Zemlya (Kusina and Yatskov 1999), the South Urals Bogoslovskaya 1971a, 1978;Nikolaeva et al 2009), Karaganda (Ruzhencev and Bogoslovskaya 1971a), the Pamirs of Tajikistan (Nikolaeva 1994(Nikolaeva , 1995, Kyrgyzstan and Uzbekistan (Pitinova 1974;Ruzhencev and Bogoslovskaya 1978), Xinjiang (Liang and Wang 1991) and South China (Yang 1978;Ruan 1981a;Ruan and Zhou 1987), stratigraphical subdivisions operate also with advanced goniatitid and glaphyritid ammonoids.…”

Section: Serpukhovian Bashkirianmentioning

confidence: 97%

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Paleozoic Ammonoid Biostratigraphy

Korn

Klug

2015

Topics in Geobiology

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Section: Viséanmentioning

confidence: 92%

Section: Serpukhovian Bashkirianmentioning

confidence: 97%

Paleozoic Ammonoid Biostratigraphy

Korn

Klug

2015

Topics in Geobiology

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“…Although the genus Plectostaffella has been reported from the Upper Serpukhovian of Urals and Tien-Shan (Einor 1996;Kulagina and Sinitsyna 2003;Orlov-Labkovsky 2005;Nikolaeva et al 2009), these two species are reliable markers of the base of Pennsylvanian in most places in the eastern hemisphere.…”

Section: Mid-carboniferous Boundarymentioning

confidence: 96%

“…ikensis. The range of the latter species is reported elsewhere to terminate just below the mid-Carboniferous boundary (Vdovenko et al 1990;Vachard and Maslo 1996;Altıner and Ö zgül 2001;Nikolaeva et al 2001). The midCarboniferous boundary is drawn locally at the base of the sample 27, coincident with the boundary between the Eostaffella ex gr.…”

Section: Mid-carboniferous Boundarymentioning

confidence: 98%

Foraminiferal biostratigraphy and sequence stratigraphy across the mid-Carboniferous boundary in the Central Taurides, Turkey

Atakul‐Özdemir

Altıner

Özkan-Altıner

et al. 2011

Facies

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The Aladag Unit is one of the main tectonic units in the Tauride Belt, located in southern Turkey. It includes a continuous Paleozoic carbonate sequence encompassing the mid-Carboniferous boundary, with outcrops being especially well exposed in the Hadim region. The boundary succession lithology is mainly composed of carbonates with intercalated quartz arenitic sandstone layers. Based on foraminifers, four biostratigraphic zones have been defined in the interval from the Upper Serpukhovian to the Lower Bashkirian. These zones are, in ascending order: the Eostaffella ex gr. ikensis-E. postmosquensis Zone (Zapaltyubinsky Horizon, Upper Serpukhovian); the Plectostaffella jakhensis-P. bogdanovkensis Zone, and the Millerella marblensis Zone (Bogdanovsky Horizon, lower Bashkirian); and the Semistaffella sp. Zone (Syuransky Horizon, lower Bashkirian). The mid-Carboniferous boundary occurs between the Eostaffella ex gr. ikensis-E. postmosquensis Zone and the Plectostaffella jakhensis-P. bogdanovkensis Zone. Boundary beds are characterized by eight, repeatedly occurring microfacies types, namely: (1) coated crinoidal packstone; (2) coated bioclastic grainstone; (3) oolitic grainstone; (4) oolitic packstone-grainstone; (5) intraclastic grainstone; (6) mudstone-wackestone; (7) quartz-peloidal packstone; and 8) quartz arenitic sandstone. Based on microfacies stacking patterns, various types of shallowing-upward cycles have been recognized. Depositional sequences and sequence boundaries are correlatable with those described from North America and Russia and Carboniferous global sea-level curves. The duration of cycles has been estimated as 100 ky, suggesting that cycle periodicities correspond to the Milankovitch eccentricity band.

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“…Two principle candidate GSSPs are currently being considered for the base of the Serpukhovian Stage; the Verkhnyaya Kardailovka Section in the southern Urals, Russia (Nikolaeva et al . ) and Naqing (formerly Nashui) in southern China (Qi et al . , , ; Groves et al .…”

Section: Mississippian (Carboniferous) Chronostratigraphymentioning

confidence: 99%

Conodonts of the genus Lochriea in Ireland and the recognition of the Viséan–Serpukhovian (Carboniferous) boundary

Barham

Murray

Sevastopulo

et al. 2015

LET

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Conodonts of the genus Lochriea offer high‐resolution biostratigraphical differentiation of the upper Mississippian (Carboniferous). In particular, L. ziegleri is regarded as the most suitable index taxon for recognition of a revised Viséan–Serpukhovian boundary and selection of a Global Stratotype Section and Point. Mixed carbonate‐siliciclastic Carboniferous sections from western Ireland demonstrate that gradual morphological evolution is expressed within the Lochriea lineage, evidenced by P1‐elements with progressively more complex ornament appearing in a pulsed fashion in the Late Viséan. Significant diversification of the Lochriea conodonts occurs below the currently recognized base of the Namurian (identified by ammonoids), with which the basal Serpukhovian has been correlated in the past. The First Appearance Datum (FAD) of L. ziegleri in the Lugasnaghta Section of western Ireland is apparently coincident with the FAD's of other complexly ornamented Lochriea species (e.g. L. cruciformis) and corresponds with the Irish and British P2a ammonoid biozone and the lower part of the upper Cf6δ (MFZ15) foraminiferal biozone. The FAD of L. ziegleri in Ireland is closely related to other Lochriea morphotypes with complex ornament, which are difficult to identify to species level using current species definitions. These forms, recorded from the three sections examined (St Brendan's Well, Kilnamona and Lugasnaghta), may partly be explained as abnormal growth histories, evolutionary intermediate forms, etc. In some instances, however, the apparently consistent and novel morphotypes suggest that current Lochriea taxonomy needs to be re‐examined. Furthermore, given the close association of the morphologies with asymmetric complex ornament and L. ziegleri, these taxa may hold significance as biostratigraphical tools in their own right.

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Paleontology and Microfacies of the Serpukhovian in the Verkhnyaya Kardailovka Section, South Urals, Russia: potential candidate for the GSSP for the Visean-Serpukhovian boundary

Cited by 48 publications

References 13 publications

Paleozoic Ammonoid Biostratigraphy

Paleozoic Ammonoid Biostratigraphy

Foraminiferal biostratigraphy and sequence stratigraphy across the mid-Carboniferous boundary in the Central Taurides, Turkey

Conodonts of the genus Lochriea in Ireland and the recognition of the Viséan–Serpukhovian (Carboniferous) boundary

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