Early Carboniferous spiriferoid brachiopods from the Qaidam Basin, Northwest China: Taxonomy, biostratigraphy and biogeography

被引:6
|
作者
Shi, G. R. [1 ]
Chen, Zhong-Qiang [2 ]
Lee, Sangmin [1 ]
Zhan, Li-Pei [3 ]
机构
[1] Deakin Univ, Sch Life & Environm Sci, Burwood Campus, Geelong, Vic, Australia
[2] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[3] Chinese Acad Geol Sci, Inst Geol, Beijing, Peoples R China
基金
澳大利亚研究理事会;
关键词
Spiriferoid brachiopods; Lower Carboniferous; Palaeobiogeography; Qaidam Basin; Qaidamospirifer; Triangulospirifer; GONDWANA; FAUNAS; PYRENEES; GENERA;
D O I
10.1016/j.palwor.2016.07.003
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Six Early Carboniferous brachiopod species in four genera of the Superfamily Spiriferoidea are described from the Qaidam Basin, northwestern China, including a new genus, Qaidamospirifer, and two new species: Grandispirifer qaidamensis and Qaidamospirifer elongatus. Additionally, a new genus, Triangulospirifer, is also proposed to replace Triangularia Poletaev, 2001 that was preoccupied by a Devonian molluscan genus. On the basis of the new material as well as published information, we have reviewed the taxonomic composition and the stratigraphic and palaeobiogeographic distributions of the three previously established genera from the viewpoint of palaeobiogeography. The study reveals that Grandispirifer has a relatively long stratigraphic range from the late Tournaisian to Serpukhovian. During this interval, the genus attained a wide geographical distribution, reaching Northwest China, western Yunnan of West China, Japan, as well as Iran and North Africa. Angiospirifer first occurred in western Europe in the Visean, and later migrated to North Africa during the late Visean. In the Serpukhovian, it migrated eastward, reaching the Donets Basin of Ukraine and the Qaidam Basin in Northwest China. Anthracothyrina evolved from Brachythyrina in North Africa in late Visean, then dispersed north-westward to western and eastern Europe and, further eastward to the Qaidam Basin during the Serpukhovian. (C) 2016 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
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页码:581 / 599
页数:19
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