Early Cambrian organophosphatic brachiopods from the Xinji Formation, at Shuiyu section, Shanxi Province, North China

被引:18
作者
Pan, Bing [1 ,2 ,3 ,4 ]
Skovsted, Christian B. [4 ,5 ]
Brock, Glenn A. [6 ]
Topper, Timothy P. [4 ,5 ]
Holmer, Lars E. [5 ,7 ]
Li, Luo-Yang [4 ,5 ]
Li, Guo-Xiang [1 ,2 ]
机构
[1] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
[3] Univ Sci & Technol China, Hefei 230026, Peoples R China
[4] Swedish Museum Nat Hist, Dept Palaeobiol, Box 50007, SE-10405 Stockholm, Sweden
[5] Northwest Univ, Dept Geol, Shaanxi Key Lab Early Life & Environm, State Key Lab Continental Dynam, Xian 710069, Peoples R China
[6] Macquarie Univ, Dept Biol Sci, Sydney, NSW 2109, Australia
[7] Uppsala Univ, Inst Earth Sci, Palaeobiol, SE-75236 Uppsala, Sweden
基金
中国国家自然科学基金; 瑞典研究理事会;
关键词
Cambrian Series 2; North China; Organophosphatic; Brachiopod; Mickwitziid; Lingulida; East Gondwana; SMALL SHELLY FOSSILS; 3 GORGES AREA; SERIES; SOUTH-AUSTRALIA; AMADEUS BASIN; SHAANXI PROVINCE; FLINDERS RANGES; MICKWITZIA; FAUNA; TRILOBITES;
D O I
10.1016/j.palwor.2019.07.001
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Abundant and diverse small shelly fossils have been reported from Cambrian Series 2 in North China, but the co-occurring brachiopods are still poorly known. Herein, we describe seven genera, five species and two undetermined species of organophosphatic brachiopods including one new genus and new species from the lower Cambrian Xinji Formation at Shuiyu section, located on the southern margin of North China Platform. The brachiopod assemblage comprises one mickwitziid (stem group brachiopoda), Paramickwitzia boreussinaensis n. gen. n. sp., a paterinide, Askepasma toddense Laurie ; 1986, an acrotretoid, Eohadrotreta cf. zhenbaensis Li and Holmer. 2004, a botsfordiid, Schizopholis yorkensis (Holmer and Ushatinskaya in Gravestock et al., 2001) and three linguloids, Spinobolus sp., Eodicellomus cf. elkaniiformis Holmer and Ushatinskaya in Gravestc-i-et al., 2001 and Eoobolus sp. This brachiopod assemblage suggests a late Age 3 to early Age 4 for the Xinji Formation and reveals a remarkably strong connection with coeval faunas from East Gondwana, particularly the Hawker Group in South Australia. The high degree of similarity (even at species level) further supports a close palaeogeographic position between the North China Platform and Australian East Gondwana during the early Cambrian as indicated by small shelly fossil data. (C) 2019 Elsevier Ireland Ltd Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
引用
收藏
页码:512 / 533
页数:22
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