Orbitolinopsis cenomaniensis n. sp., a new larger benthic foraminifera (Orbitolinidae) from the middle-?late Cenomanian of the Sarvak Formation (SW Iran, Zagros Zone): a regional marker taxon for the Persian Gulf area and Oman
{"title":"Orbitolinopsis cenomaniensis n. sp., a new larger benthic foraminifera (Orbitolinidae) from the middle-?late Cenomanian of the Sarvak Formation (SW Iran, Zagros Zone): a regional marker taxon for the Persian Gulf area and Oman","authors":"Felix Schlagintweit , Mohsen Yazdi-Moghadam","doi":"10.1016/j.revmic.2020.100413","DOIUrl":null,"url":null,"abstract":"<div><p>A new orbitolinid is described as <em>Orbitolinopsis cenomaniensis</em><span> n. sp. from the middle-?late Cenomanian of the Sarvak Formation, Zagros Zone, SW Iran. It is characterized by a high-conical test, a simple embryo consisting of proloculus and deuteroconch in subapical position, a rather narrow marginal zone and a prominent central zone with cupules that can present a jagged outline. The regular occurrence of one short rafter is considered a species characteristic of the species, one case that is also encountered in other dictyoconid taxa (e.g., </span><em>Montseciella</em>, <em>Paracoskinolina</em>, <em>Simplorbitolina</em>, <em>Valserina</em><span>). Single sporadic rafters have been reported from the early Albian </span><em>Orbitolinopsis ajoensis</em> Schlagintweit et al. demonstrating a distinct trend towards an increasing in morphological complexity. The Iranian find represents the first record of <em>Orbitolinopsis</em><span> from the Cenomanian. Like several other taxa of larger benthic foraminifera (agglutinating and porcelaneous), </span><em>O. cenomaniensis</em><span> is here considered an endemic taxon for the Arabian Plate.</span></p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.7000,"publicationDate":"2020-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2020.100413","citationCount":"13","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"REVUE DE MICROPALEONTOLOGIE","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0035159820300118","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
引用次数: 13
Abstract
A new orbitolinid is described as Orbitolinopsis cenomaniensis n. sp. from the middle-?late Cenomanian of the Sarvak Formation, Zagros Zone, SW Iran. It is characterized by a high-conical test, a simple embryo consisting of proloculus and deuteroconch in subapical position, a rather narrow marginal zone and a prominent central zone with cupules that can present a jagged outline. The regular occurrence of one short rafter is considered a species characteristic of the species, one case that is also encountered in other dictyoconid taxa (e.g., Montseciella, Paracoskinolina, Simplorbitolina, Valserina). Single sporadic rafters have been reported from the early Albian Orbitolinopsis ajoensis Schlagintweit et al. demonstrating a distinct trend towards an increasing in morphological complexity. The Iranian find represents the first record of Orbitolinopsis from the Cenomanian. Like several other taxa of larger benthic foraminifera (agglutinating and porcelaneous), O. cenomaniensis is here considered an endemic taxon for the Arabian Plate.
期刊介绍:
La Revue de micropaléontologie publie 4 fois par an des articles de intérêt international, consacrés à tous les aspects de la micropaléontologie. Les textes, en anglais ou en français, sont des articles originaux, des résultats de recherche, des synthèses et mises au point, des comptes rendus de réunions scientifiques et des analyses de ouvrages. La revue se veut résolument ouverte à tous les aspects de la micropaléontologie en accueillant des travaux traitant de la systématique des microfossiles (et de leurs équivalents actuels), des bactéries aux microrestes de vertébrés, et de toutes leurs applications en sciences biologiques et géologiques.