Multidisciplinary study of the Mechetlino Quarry section (Southern Urals, Russia) — The GSSP candidate for the base of the Kungurian Stage (Lower Permian)

Palaeoworld ◽  
2020 ◽  
Vol 29 (2) ◽  
pp. 325-352 ◽  
Author(s):  
Valery V. Chernykh ◽  
Galina V. Kotlyar ◽  
Boris I. Chuvashov ◽  
Ruslan V. Kutygin ◽  
Tatiana V. Filimonova ◽  
...  
Keyword(s):  
Southern Urals ◽  
Lower Permian ◽  
Multidisciplinary Study ◽  
Kungurian Stage

scholarly journals New representatives of the species Kerpia samarica from the location Novyi Kuvak (kazanian stage, Samara Region)

2016 ◽  
Vol 5 (2) ◽  
pp. 11-15
Author(s):  
Liubov Mikhailovna Bukhman ◽  
Nikolay Sergeevich Bukhman
Keyword(s):  
New Species ◽  
Southern Urals ◽  
Species Level ◽  
Middle Urals ◽  
The Southern Urals ◽  
Kazanian Stage ◽  
New Findings ◽  
The One ◽  
Kungurian Stage ◽  
A New Species

The article is devoted to the study of new representatives of the genus Kerpia Naugolnykh from Novyi Kuvak located in Shentalinsky district (northeast of Samara region). The genus Kerpia for ginkgo similar leaves was set by S.V. Naugolnykh in 1995 on the material from the Kungurian stage of the Middle Urals. Typical species of this genus is Kerpia macroloba Naugolnykh. In the diagnosis of the genus S.V. Naugolnykh showed the most important signs of this genus: presence of lobes and sinuses of the 1st and 2nd order, distinct petiole and two veins included in lamina from the petiole. Later, in 2001, from the sediments of Kazanian stage of the Southern Urals S.V. Naugolnykh described a new species Kerpia belebeica Naugolnykh. In 2013 in Novyi Kuvak location we found impressions of ginkgo similar leaves with on the one hand a great similarity with the known members of the genus Kerpia ( Kerpia macroloba and Kerpia belebeica ), but on the other hand they are clearly not identical to this representative at the species level. According to the results of the study of these impressoins in 2014 we described a new species of the genus Kerpia - Kerpia samarica N.S. Bukhman et L.M. Bukhman, 2014. In this paper we give description of both known and new findings of species Kerpia samarica and a comparison of this species with other species of the genus Kerpia .

scholarly journals ORTHOPTERA FROM THE LOWER PERMIAN VORKUTA LOCALITY (RUSSIA: KOMI REPUBLIC; KUNGURIAN STAGE)

2020 ◽  
Vol 410 ◽  
pp. 17-20
Author(s):  
D. S. Aristov ◽  
◽  
A. V. Gorochov ◽  
◽  
Keyword(s):  
Komi Republic ◽  
Lower Permian ◽  
Kungurian Stage

scholarly journals Zircons of the Permian age (280–290 Ma) from intrusive magmatic rocks in Riphean structure of the Southern Urals

LITOSFERA ◽  
2021 ◽  
Vol 21 (5) ◽  
pp. 601-608
Author(s):  
A. A. Krasnobaev ◽  
V. N. Puchkov ◽  
N. D. Sergeeva ◽  
S. V. Busharina
Keyword(s):  
Southern Urals ◽  
Lower Permian ◽  
The Urals ◽  
Shrimp Dating ◽  
The Southern Urals ◽  
Lower Paleozoic ◽  
Magmatic Rocks ◽  
Lower Riphean ◽  
Granite Complex ◽  
A Chain

Research subject. Magmatic complexes that are developed in the lower (volcanogenic-sedimentary) part of the Ai Formation of the Lower Riphean of the Taratash anticline in the Southern Urals. Results. For the frst time, the Lower Permian SHRIMP dating (288.6 ± 3.1 Ma by U-Pb method on zircon from monzogabbro) was obtained for a dike cutting the basalts of the Lower Paleozoic (420–450 Ma) age. Conclusions. On the eastern slope of the Urals there is a chain of massifs which are close in the age. The chain belongs to the Lower Permian Stepninsky monzogabbro-granosyenite-granite complex, represented by the Uiski, Vandyshevski, Biryukovski and Stepninski intrusions with the age of 281 ± 2, 280 ± 2 and 286 ± 2 Ma, correspondingly (U-Pb method after zircons, SHRIMP-II, VSEGEI) and earlier obtained dates 281 ± 4 Ma (Rb-Sr isochrone) and 283 ± 2 Ma (isotope Pb-Pb method after zircons). The Stepninsky complex was described earlier as plume-dependent. The monzogabbro dike, described in this paper, although being at a considerable distance from the Sepninsky complex, is situated at a strike of the chain of the stepninsky intrusions, is close to them by the composition and age and can be ascribed to the same plume episode. The idea of the plume character of the complex was ехрressed by us relatively long ago based on a superimposed character of the chain of the intrusions over the earlier, collisional Uralian structures. As for the geochemical character (monzogabbro) the dike conforms with one of two standard trends of the Stepninsky complex – monzonite (monzogabbro, monzodiorites, syenites).

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

2016 ◽  
Vol 90 (6) ◽  
pp. 1049-1067 ◽  
Author(s):  
Olga L. Kossovaya ◽  
Matevž Novak ◽  
Dieter Weyer
Keyword(s):  
Southern Urals ◽  
Wide Distribution ◽  
Time Span ◽  
Lower Permian ◽  
New Taxon ◽  
Early Permian ◽  
The Southern Urals ◽  
Predominant Species ◽  
Large Numbers ◽  
Distinguishing Features

AbstractA new monospecific “caninioid” genus,Preisingerellan. gen., from the lower Permian of the Karavanke Mountains (Southern Alps, Slovenia) is erected. The type species isPreisingerella stegovnikensisn. sp. The new taxon can be differentiated from otherCaninia-type genera by its specific ontogeny and features of its dissepimentarium. Corals with such morphology had a wide distribution during the Carboniferous and early Permian, occurring in mostly shallow-water carbonate rocks. The phylogenetic relationships within this group are mostly unclear due to similarities in the adult stages. The earlier stages reveal the main distinguishing features that are decisive for a generic assignment, but these have rarely been well preserved and properly considered. The new taxon is compared with related genera of the Cyathopsidae and species ofCaninellaGorskiy, 1938 characterized by lateral dissepiments. Large numbers of specimens of the new species, representing a monospecific assemblage, have been collected from the Born Formation at Mt. Stegovnik. Sedimentological and microfacies characteristics, as well as macro- and microfossil assemblages, underline this correlation. The fusulinoidean assemblage of the Born Formation, withSphaeroschwagerina carniolica(Kahler and Kahler, 1937), as the predominant species, corresponds to the time span between theSphaeroschwagerina moelleri-Schwagerina fecundaandPseudofusulina moellerizones, indicating a late Asselian to early Sakmarian age in the Southern Urals.

scholarly journals New species of the genus Blattinopsis Giebel, 1867 (Insecta: Blattinopsida: Blattinopsidae) from the Permian of Taimyr Peninsula, Russia

2021 ◽  
pp. 6-9
Author(s):  
A.P. Rasnitsyn ◽  
◽  
D.S. Aristov ◽  
◽  
◽  
...  
Keyword(s):  
New Species ◽  
Western Siberia ◽  
Lower Permian ◽  
Taimyr Peninsula ◽  
North Western ◽  
Kungurian Stage

Blattinopsis indefinitus Rasnitsyn et Aristov, sp. n. is described from the Lower Permian Fokina locality (the upper Burgukla subhorizont of the upper Kungurian Stage) in North-Western Siberia. It is the latest record of the genus Blattinopsis Giebel, 1867.

The Carboniferous-Permian boundary and ammonoids from the Aidaralash section, southern Urals

1995 ◽  
Vol 69 (2) ◽  
pp. 288-301 ◽  
Author(s):  
M. F. Bogoslovskaya ◽  
T. B. Leonova ◽  
A. A. Shkolin
Keyword(s):  
Southern Urals ◽  
Late Carboniferous ◽  
Lower Permian ◽  
Profound Change ◽  
Stratigraphic Section ◽  
Northern Kazakhstan ◽  
Permian Ammonoid

The stratigraphic section at Aidaralash Creek, northern Kazakhstan, provides a complete and well-developed succession of strata across the Carboniferous–Permian boundary. This section, containing abundant and well-preserved ammonoid, fusulinacean, and conodont faunas, can serve well as the Carboniferous–Permian boundary stratotype. A profound change in ammonoid faunas, which occurs at the Orenburgian–Asselian boundary and which has been recognized by previous workers (e.g., Ruzhencev, 1950, 1951, 1952; Bogoslovskaya and Popov, 1986a, 1986b; Furnish, 1973; Glenister and Furnish, 1981), occurs in the Aidaralash Creek section, at the boundary between beds 19 and 20, and serves to mark the Carboniferous–Permian boundary. Additionally, Lower Permian strata at Aidaralash Creek mark the first appearance of widespread Permian ammonoid taxa, including representatives of Svetlanoceras, Juresanites, Prostacheoceras, Tabantalites, and Kargalites, that are preceded by the extinction of characteristic Late Carboniferous genera such as Prouddenites, Uddenites, Shumardites, Vidrioceras, Schistoceras, and Subkargalites.

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