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Dynamic variation of Middle to Late Ordovician cephalopod provincialism in the northeastern peri-Gondwana region and its implications
Fang, Xiang (方翔)1,2; Burrett, Clive3,4; Li, Wenjie2,5,6; Zhang, Yunbai (张允白)1,2; Zhang, Yuandong (张元动)2,5,6; Chen, Tingen (陈挺恩)1,2; Wu, Xuejin2,5,7
2019-05-01
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
Volume521Pages:127-137
Abstract

Middle to Late Ordovician cephalopod occurrence data from South China and adjacent terranes in the northeastern peri-Gondwana region are used to define biogeographic provinces. Several multivariate methods are adopted for biogeographic analysis, including cluster analysis, non-metric multidimensional scaling and network analysis. During the Middle Ordovician, three biogeographic provinces in this region are recognized, the Australia, the North China-Tibet-Sibumasu (NTS) and the South China-Altun (SA) provinces. In the Late Ordovician, three provinces with modified geographic ranges may also be recognized, as the cephalopods of the Tibetan region and Sibumasu terrane changed significantly and accordingly they have been included with South China-Altun to form a South China-Tarim-Tibet-Sibumasu Province (STTS), while the other two Late Ordovician provinces are the Australia and the North China provinces. The dynamic variation of cephalopod provincialism in the northeastern peri-Gondwana region, may have been controlled by the changing palaeolatitude and differentiated movement of these plates or terranes from the Middle through Late Ordovician.

KeywordPalaeobiogeography Cluster Analysis Non-metric Multidimensional Scaling Network Analysis Palaeolatitude Plate Movement
DOI10.1016/j.palaeo.2019.02.015
Language英语
WOS KeywordBoda Limestone ; Paleogeography ; China ; Paleobiogeography ; Reconstructions ; Diversification ; Paleoecology ; Diversity ; Zircons ; Faunas
Funding ProjectChinese Academy of Sciences[XDB26000000] ; Chinese Academy of Sciences[XDB10010100] ; Chinese Ministry of Science and Technology[2013FY111000] ; Chinese Ministry of Science and Technology[2017ZX05036-001-004] ; National Natural Science Foundation of China[41772005] ; IGCP projects[653] ; IGCP projects[668]
WOS Research AreaPhysical Geography ; Geology ; Paleontology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS IDWOS:000463291900010
Funding OrganizationChinese Academy of Sciences ; Chinese Ministry of Science and Technology ; National Natural Science Foundation of China ; IGCP projects
PublisherELSEVIER SCIENCE BV
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/15809
Collection中国科学院南京地质古生物研究所
其他
Corresponding AuthorFang, Xiang (方翔)
Affiliation1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Jiangsu, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing, Jiangsu, Peoples R China
3.Univ Tasmania, Sch Phys Sci, Hobart, Tas, Australia
4.Mahasarakham Univ, Palaeontol Res & Educ Ctr, Maha Sarakham, Thailand
5.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, CAS Key Lab Econ Stratig & Palaeogeog, Nanjing, Jiangsu, Peoples R China
6.Univ Chinese Acad Sci, Beijing, Peoples R China
7.Univ Sci & Technol China, Hefei, Anhui, Peoples R China
Recommended Citation
GB/T 7714
Fang, Xiang ,Burrett, Clive,Li, Wenjie,et al. Dynamic variation of Middle to Late Ordovician cephalopod provincialism in the northeastern peri-Gondwana region and its implications[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2019,521:127-137.
APA Fang, Xiang .,Burrett, Clive.,Li, Wenjie.,Zhang, Yunbai .,Zhang, Yuandong .,...&Wu, Xuejin.(2019).Dynamic variation of Middle to Late Ordovician cephalopod provincialism in the northeastern peri-Gondwana region and its implications.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,521,127-137.
MLA Fang, Xiang ,et al."Dynamic variation of Middle to Late Ordovician cephalopod provincialism in the northeastern peri-Gondwana region and its implications".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 521(2019):127-137.
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