Multiple Orbitoides d’Orbigny lineages in the Maastrichtian? Data from the Central Sakarya Basin (Turkey) and Arabian Platform successions (Southeastern Turkey and Oman)
-
Published:2021-04-19
Issue:1
Volume:140
Page:
-
ISSN:1664-2376
-
Container-title:Swiss Journal of Palaeontology
-
language:en
-
Short-container-title:Swiss J Palaeontol
Author:
Özcan ErcanORCID, Yücel Ali Osman, Catanzariti Rita, Kayğılı Sibel, Okay Aral I., Simmons Michael D., Pignatti Johannes, Abbasi İftikhar Ahmed, Erbil Ümitcan
Abstract
AbstractThe standard reconstruction of species of Orbitoides d’Orbigny into a single lineage during the late Santonian to the end of the Maastrichtian is based upon morphometric data from Western Europe. An irreversible increase in the size of the embryonic apparatus, and the formation of a greater number of epi-embryonic chamberlets (EPC) with time, is regarded as the main evolutionary trends used in species discrimination. However, data from Maastrichtian Orbitoides assemblages from Central Turkey and the Arabian Platform margin (Southeastern Turkey and Oman) are not consistent with this record. The Maastrichtian Besni Formation of the Arabian Platform margin in Southeastern Turkey yields invariably biconvex specimens, with small, tri- to quadrilocular embryons and a small number of EPC, comparable to late Campanian Orbitoides medius (d’Archiac). The upper Maastrichtian Taraklı Formation from the Sakarya Basin of Central Turkey contains two distinct, yet closely associated forms of Orbitoides, easily differentiated by both external and internal features. Flat to biconcave specimens possess a small, tri- to quadrilocular embryonic apparatus of Orbitoides medius-type and a small number of EPC, whereas biconvex specimens possess a large, predominantly bilocular embryonic apparatus, and were assigned to Orbitoides ex. interc. gruenbachensis Papp–apiculatus Schlumberger based on morphometry. The flat to biconcave specimens belong to a long overlooked species Orbitoides pamiri Meriç, originally described from the late Maastrichtian of the Tauride Mountains in SW Turkey. This species is herein interpreted to be an offshoot from the main Orbitoides lineage during the Maastrichtian, as are forms that we term Orbitoides ‘medius’, since they recall this species, yet are younger than normal occurrence with the accepted morphometrically defined lineage. The consistent correlation between the external and internal test features in O. pamiri implies that the shape of the test is not an ecophenotypic variation, but appears to be biologically controlled. We, therefore, postulate that more than one lineage of Orbitoides exists during the Maastrichtian, with a lineage that includes O. ‘medius’ and O. pamiri displaying retrograde evolutionary features.
Funder
Türkiye Bilimsel ve Teknolojik Araştirma Kurumu Sultan Qaboos University
Publisher
Springer Science and Business Media LLC
Reference65 articles.
1. Abdelghany, O. (2003). Late Campanian-Maastrichtian foraminifera from the Simsima Formation on the western side of the northern Oman Mountains. Cretaceous Research, 24, 391–405. 2. Albrich, S., Frijia, G., Parente, M., & Caus, E. (2014). The evolution of the earliest representatives of the genus Orbitoides: implications for the Upper Cretaceous biostratigraphy. Cretaceous Research, 51, 22–34. 3. Altıner, D., Koçyiğit, A., Farinacci, A., Nicosia, U., & Conti, M. A. (1991). Jurassic-Lower Cretaceous stratigraphy and paleogeographic evolution of the southern part of north-western Anatolia (Turkey). Geologica Romana, 27, 13–80. 4. Barrier, E., Vrielynck, B., Brouillet, J.-F., & Brunet, M.-F. (2018). Atlas of Paleotectonic reconstruction of the Central Tethyan Realm. Tectono-sedimentary-palinspastic maps from late Permian to Pliocene. 5. Baumfalk, Y. A. (1986). The evolution of Orbitoides media (Foraminiferida) in the Late Campanian. The Journal of Foraminiferal Research, 16, 293–312.
Cited by
11 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|