THE PERMIAN FORAMINIFERAL FAMILY PSEUDOVIDALINIDAE AND THE GENUS<i>ALTINERIA</i>EMEND. HEREIN

Vachard, Daniel; Rettori, R; Altıner, Demir; Gennari, Valerio

doi:10.2113/gsjfr.47.3.279

Cited by 6 publications

(2 citation statements)

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“…A first emendation of Pseudovidalina was provided by Zaninetti et al (), Loeblich and Tappan (), Altiner (), Vachard in Vachard and Beckary (), and Pinard and Mamet (), who suggested that the wall was bilayered and not unilayered. Furthermore, Altiner () introduced the genus Angelina (renamed as Altineria Özdikmen, because Angelina was pre‐occupied; see Vachard et al, in press), also described as bilayered but with a completely evolute test. On the other hand, many authors, in China and Russia, do not follow these emendations of Pseudovidalina and preferred to denominate the taxon as Eolasiodiscus Reitlinger, or Eolasiodiscus ?, whereas in the USA, it was generally renamed as Raphconilia Brenckle and Wahlman, .…”

Section: Systematic Paleontologymentioning

confidence: 99%

“…Another lineage that might exist in the Capitanian–Wuchiapingian with Pseudovidalina sensu stricto is – Xingshandiscus complaniformis Lin, – X. jianyangensis Zheng, – Altineria . Anyway, Xingshandiscus and Altineria represent, among the lasiodiscids, the homeomorphs of the most advanced stages of archaediscids (i.e., the tenuis and evolutus stages; Vachard et al, in press).…”

Section: Systematic Paleontologymentioning

confidence: 99%

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The uppermost Carboniferous (Gzhelian)–Lower Permian (Asselian–Sakmarian) stratigraphy and smaller foraminifers of the Ozbak‐Kuh region (Tabas Block, east central Iran)

Yarahmadzahi

Vachard

2017

Geological Journal

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The uppermost Carboniferous (Gzhelian)–Lower Permian (Asselian to Sakmarian) Anarak Group of the Zaladou section in central Iran is more than 180‐m thick and includes thick units of shale, calcareous sandstone, fusulinid limestone, sandy limestone, and dolomite. The Zaladou and Tigh‐e‐Madanu formations of this group were dated as Gzhelian to Sakmarian. A review of the smaller foraminifers of the Zaladou section is presented. Five foraminiferal subzones grouped in three biozones are proposed in this work: The first assemblage zone (I) is Gzhelian; the second zone (II) corresponds to the Gzhelian–Asselian boundary interval, and the third biozone (III) is Asselian in age. Biozone I is subdivided informally into two subzones: the Hemigordius spirilliniformis‐Bradyina cf. samarica subzone IA (probably early Gzhelian in age) and the Raphconilia modificata and Globivalvulina spp. subzone IB (middle to late Gzhelian); biozone II is the Nodosinelloides spp. zone; biozone III is subdivided informally into two subzones: IIIA with Pseudoacutella partoazari‐Bradyina lucida and IIIB with Planoendothyra persica n. sp.‐Rectogordius sp. The studied assemblages are correlated with those from the Carnic Alps (Austria–Italy), East European Platform of Russia, the Urals (Russia), Darvas (Uzbekistan), the northern and central Pamirs (Tajikistan), northern Iran (Alborz), northern Afghanistan, and other classical regions of the Tethyan realm. The genera Raphconilia and Planoendothyra are revised, and Planoendothyra persica n. sp. is described.

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Section: Systematic Paleontologymentioning

confidence: 99%

Section: Systematic Paleontologymentioning

confidence: 99%