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A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

Published online by Cambridge University Press:  26 December 2018

Xiangdong Wang ,
Mohammad N. Gorgij  and
Le Yao
Xiangdong Wang*
Affiliation:
Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing 210023, China; and Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
Mohammad N. Gorgij
Affiliation:
Geology Department, Faculty of Sciences, University of Sistan and Baluchestan, Zahedan, Iran
Le Yao*
Affiliation:
Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
*
*Corresponding author
*Corresponding author
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Abstract

Twelve rugose coral species belonging to seven genera are described and discussed based on 70 thin sections of 32 specimens collected from the Anarak section, northeast of Nain, Esfahan Province, Yazd Block, central Iran. These species include two new colonial rugose coral species, Antheria fedorowskii and Antheria robusta, and five previously named species of colonial rugose corals, Antheria lanceolata and Streptophyllidium scitulum, and solitary rugose corals, Arctophyllum jiangsiense, Caninophyllum cf. somtaiense, and Pseudotimania delicata. Five species are left in open nomenclature: Antheria sp., Arctophyllum sp., Caninophyllum sp., Nephelophyllum sp., and Yakovleviella sp. These Iranian corals are associated with the fusulinids Rauserites (several species) and Ultradaixina bosbytauensis, indicating a latest Carboniferous age (Gzhelian age). All the described genera and named species belong to the families Aulophyllidae, Bothrophyllidae, Cyathopsidae, and Kepingophyllidae, among which the family Kepingophyllidae has been previously documented only from China and Indochina. They are typical representatives of the Cathaysian rugose fauna, which was widely developed around the South China and Indochina blocks near the paleoequator and was absent from the Gondwanan and Cimmerian continents in high latitudes during the Late Pennsylvanian. Hence, the occurrence of the Cathaysian fauna from central Iran in the latest Carboniferous suggests that it may have had a close biogeographical connection with China and Indochina, which further implies its latitudinal position intermediate between the Gondwanan continent and South China and Indochina blocks during this time.

UUID: http://zoobank.org/5257d2bb-1346-4dee-8f3e-f4b1b33ba5a9

Type
Articles
Information
Journal of Paleontology , Volume 93 , Issue 3 , May 2019 , pp. 399 - 415
Copyright
Copyright © 2018, The Paleontological Society 

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