Mid-Cretaceous Rudist Assemblage from the Lhasa Block, Tibet (China)

被引:1
作者
Rao, Xin [1 ,2 ]
Skelton, Peter W. [3 ]
Sano, Shin-ichi [4 ]
Sha, Jingeng [1 ,2 ]
Wan, Bin [1 ,2 ]
机构
[1] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, 39 East Beijing Rd, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, 39 East Beijing Rd, Nanjing 210008, Peoples R China
[3] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England
[4] Univ Toyama, Grad Sch Sci & Engn Res, Dept Earth Syst Sci, 3190 Gofuku, Toyama, Toyama 9308555, Japan
来源
PALEOBIODIVERSITY AND TECTONO-SEDIMENTARY RECORDS IN THE MEDITERRANEAN TETHYS AND RELATED EASTERN AREAS | 2019年
关键词
Lhasa block; Sangzugang Formation; Langshan Formation; Rudist; SW Asian/Pacific faunal province; RADIOLITID RUDIST;
D O I
10.1007/978-3-030-01452-0_22
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A total of four rudist taxa had been distinguished from the Sangzugang Formation and the Langshan Formation of the Lhasa block, Tibet by Rao et al. [4, 5]. They are Auroradiolites biconvexus [5], Magallanesia rutogensis [5], Eoradiolites cf. hedini and Sellaea sp. The genus Auroradiolites was established for a group of SW Asian to the Pacific endemic radiolitids that featured by an entirely compact outer shell layer. The geological range of this rudist assemblage is Late Aptian to Albian. The mid-Cretaceous SW Asian-Pacific province was recognized based on the occurrence of endemic rudist taxa Auroradiolites and the accompanying polyconitid lineage, Horiopleura haydeni-Praecaprotina-Magallanesia.
引用
收藏
页码:91 / 94
页数:4
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