Solovievaia nomen novum for Ovatella Solovieva pre-occupied and revision of this fossil Foraminifera (Fusulinida, Profusulinellidae)

Vachard, Daniel; Coze, François Le

doi:10.26879/858

Cited by 5 publications

(1 citation statement)

References 2 publications

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“…The Arkhangelskian has an enormous diversity of fusulinid assemblages in the Hadim Nappe sections. In the studied sections, in addition to the previously noted genera, advanced fusulinids such as Solovievaia Vachard and Le Coze, 2018; Aljutovella Rauzer-Chernousova in Rauzer-Chernousova et al, 1951; Tikhonovichiella Solovieva in Rauzer-Chernousova et al, 1996; and Verella Dalmatskaya, 1951 first appear in the Arkhangelskian Substage. The species of the latter two genera, Tikhonovichiella tikhonovichi (Rauzer-Chernousova in Rauzer-Chernousova et al, 1951) and Verella spicata Dalmatskaya, 1951, are the index taxa of the Arkhangelskian Substage.…”

Section: Biostratigraphymentioning

confidence: 61%

Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian) successions from the Hadim Nappe, Central Taurides, southern Turkey

Akbaş

Okuyucu

2021

J. Paleontol.

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The Hadim Nappe, which is one of the allochthonous tectonic units in the Tauride Belt, in southern Turkey, includes a continuous stratigraphic succession from the Middle(?)–Late Devonian to Late Cretaceous. A relatively complete succession of the upper Serpukhovian to Bashkirian is exposed in the Central Taurides, where two sections (Yassıpınar and Gölbelen) have been selected for detailed biostratigraphic investigations. The Mississippian-Pennsylvanian boundary in these sections was determined by the first appearance datum of the Plectostaffella jakhensis and located in the oolitic limestone facies indicating a shallow-water depositional environment. The uppermost Serpukhovian and regional Bashkirian substages (Syuranian, Akavasian, Askynbashian, and Arkhangelskian) were determined by index taxa, namely Plectostaffella jakhensis, P. bogdanovkensis, P. varvariensis, Pseudostaffella antiqua, Staffellaeformes staffellaeformis, Tikhonovichiella tikhonovichi, and Verella spicata. Fifty fusulinid species belonging to fourteen genera were determined in two sections, in which two species are new: Depratina turani Akbaş new species and Tikhonovichiella praetikhonovichi Akbaş new species. The taxonomic positions of two fusulinid species (Depratina convoluta n. comb. and Staffellaeformes parva robusta n. comb.) are revised. The studied fusulinid assemblages correlate with fusulinid assemblages from the southern Urals, Russian Platform, Donetz Basin, Darvaz, Spain, central Iran, and some other regions of the Tethyan Realm. UUID: http://zoobank.org/bcbb6c72-f6f9-4e77-9cf9-3572bd731ff3

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Section: Biostratigraphymentioning

confidence: 61%

Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian) successions from the Hadim Nappe, Central Taurides, southern Turkey

Akbaş

Okuyucu

2021

J. Paleontol.

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Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development

Ueno¹

2021

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This paper proposes a synthesis of the taxonomy, phylogeny, palaeogeographic distribution, regional biostratigraphy, and palaeobiogeographic faunal development of Carboniferous fusuline foraminifers. They appeared in the latest Tournaisian and comprised a small-sized, morphologically conservative taxonomic group during the Mississippian. Fusulines became larger and prevailed in Pennsylvanian foraminiferal assemblages. Carboniferous fusulines consist of Ozawainellidae, Staffellidae, Schubertellidae, Fusulinidae, and Schwagerinidae, in which 95 genera are considered as valid taxonomically. Upsizing their shells throughout the Pennsylvanian is likely related to symbiosis with photosynthetic microorganisms, which was accelerated by the acquisition of a keriothecal wall in Late Pennsylvanian schwagerinids. Regional fusuline succession data from 40 provinces provide a refined biostratigraphy, enabling zonation and correlation with substage- or higher-resolution precision in the Pennsylvanian. Their spatio-temporal faunal characteristics show that fusulines had a cosmopolitan palaeobiogeographic signature in Mississippian time, suggesting unrestricted faunal exchange through the palaeoequatorial Rheic Ocean. After the formation of Pangea, Pennsylvanian fusulines started to show provincialism, and their distributions defined the Ural-Arctic Region in the Boreal Realm, Palaeotethys, Panthalassa, and North American Craton regions in the Palaeoequatorial Realm, and Western Gondwana and Eastern Peri-Gondwana regions in the Gondwana Realm. The Western Palaeotethys and East European Platform Subregions maintained higher generic diversity throughout the Pennsylvanian.

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The Russian School of Foraminiferology

Mikhalevich

Bugrova

Basov

et al. 2020

Journal of Foraminiferal Research

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Russian foraminiferal research began in the late 19th century and has continued to the present. Micropaleontology was prominent at two main branches of Soviet research institutions, that in St. Petersburg, known as the Petersburgian (Leningrad) and in Moscow as the Russian foraminiferal school. These two collaborated in well-coordinated cooperative work all around the country. This combined school of foraminiferology included many accomplished scientists whose main achievements are summarized, including highlights of the leadership and the contributions of A. V. Fursenko, G. A. Dutkevich, D. M. Rauser-Chernousova, N. N. Subbotina, and A. Gerke. The sustained focus on evolutionary history and its significance for taxonomy resulted in the revision of higher-level taxonomy and new understanding of the phylogeny of the Foraminifera, as well as positive elaborations of the systematics, biostratigraphy and ecology of the Foraminifera.

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Solovievaia nomen novum for Ovatella Solovieva pre-occupied and revision of this fossil Foraminifera (Fusulinida, Profusulinellidae)

Abstract: It is replaced here by Solovievaia Vachard and Le Coze nomen novum. Following this nomenclatural modification, a revision of this profusulinellid genus is proposed.

Cited by 5 publications

References 2 publications

Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian) successions from the Hadim Nappe, Central Taurides, southern Turkey

Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian) successions from the Hadim Nappe, Central Taurides, southern Turkey

Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development

The Russian School of Foraminiferology

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