Middle Ordovician shallow-water gastropods from southern Xizang (Tibet), China

被引:1
|
作者
Li, Wen-Jie [1 ,2 ]
Fang, Xiang [1 ,2 ]
Yu, Shen-Yang [3 ]
Burrett, Clive [4 ]
Zhen, Yong Yi [5 ]
Huang, Jia-Yuan [1 ,2 ,6 ]
Zhang, Yuan-Dong [1 ,2 ,6 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
[3] Qufu Normal Univ, Sch Geog & Tourism, Rizhao 276826, Peoples R China
[4] Mahasarakham Univ, Palaeontol Res & Educ Ctr, Maha Sarakham 44150, Thailand
[5] Geol Survey New South Wales, Londonderry, NSW 2753, Australia
[6] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Maclurites; Hormotoma; Himalaya; Darriwilian; Palaeoecology; Palaeogeography; MOUNT JOLMO LUNGMA; STRATIGRAPHY; CONODONTS; GEOCHRONOLOGY; PALEOECOLOGY; BIOGEOGRAPHY; HIMALAYAN; BIVALVES; REGION;
D O I
10.1016/j.palwor.2022.08.003
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Many new specimens (36 in total) of gastropods were collected from the Ordovician Alai Formation of the Chiatsun Group at Jiacun village, Nyalam County, southern Xizang (Tibet). These gastropods comprise five species assigned to two genera, including Maclurites parviumbilicatus Yu, M . cf. nyalamensis Yu, M . cf. xizangensis Yu, M . cf. subconicus Yu, and " Hormotoma " ordosensis Yu, forming a Maclurites -" Hormotoma " association. All the species are described in detail herein, and some of which are redefined. This fauna is of middle to late Darriwilian age, and palaeoecologically characterised by species of shallow-water within the photic zone. A comparison of the Maclurites community with the contemporary gastropod fauna from the Zhuozishan Formation exposed along the west margin of the North China Block shows a close palaeogeographical affinity. The occurrences of Ordovician gastropods from China are analyzed biogeographically and the results reveal that the peri-Gondwana gastropod faunal turnover event was initiated during the Middle to Late Ordovician transition. The coincident faunal turnover and the lithofacies changes in the Himalaya and western margin of North China suggest that tectonic activities and relative sea-level changes may account for the biogeographical affinities of some specific fossil groups in peri-Gondwanan regions. (c) 2023 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
引用
收藏
页码:532 / 545
页数:14
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