中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin and evolution of the Early Ordovician conodont genus Prioniodus Pander, 1856-New evidence from South China

文献类型:期刊论文

作者Zhen, Yong Yi1; Zhang, Yuan-Dong2; Chen, Zhong-Yang2; Wang, Long-Wu3
刊名MARINE MICROPALEONTOLOGY
出版日期2023-08-01
卷号183页码:16
ISSN号0377-8398
关键词Conodonta Ramiform-pectiniform apparatus Origination Evolution
DOI10.1016/j.marmicro.2023.102269
通讯作者Zhen, Yong Yi(yong-yi.zhen@regional.nsw.gov.au)
英文摘要A conodont fauna of late Tremadocian to early Floian age (Early Ordovician) is documented from the Yinchufu Formation of Zhejiang Province, South China. It is characterized by the occurrence of two species of Prioniodontidae, a new species of Prioniodus and Acodus triangularis. Prioniodus antiquus sp. nov. may represent the most primitive species of Prioniodus, which is one of the earliest conodont genera with a ramiform-pectiniform apparatus. Based on the review of nearly 200 species originally assigned to Prioniodus, six multielement species are confirmed to belong to this genus. Morphological changes of these six species shows that they form an evolutionary lineage directly evolved from an adentate species, likely Acodus triangularis which has been reported from South China, Australia and from the Precordillera of western Argentina. Origination of the ramiform pectiniform apparatuses as represented by the appearances of Prioniodus through late Tremadocian to Floian of the Early Ordovician might be a major response of the 'conodont animals' to occupy and adapt to the increasingly diversified environments in the shelf and slope settings. The biofacies distribution of the six Prioniodus species indicates that Prioniodus might have originated in deep-water slope settings and progressively spread into distal and then interior shelves in the late Tremadocian and diversified in the Floian, with Prioniodus amadeus possibly representing a relict species that survived into the Middle Ordovician and was restricted to shallow water environments.
WOS关键词HONGHUAYUAN FORMATION ; BIOSTRATIGRAPHY ; CORDILLERA ; GUIZHOU ; FAUNA ; BIODIVERSIFICATION ; BIOGEOGRAPHY ; AUSTRALIA ; SYSTEM ; BASIN
资助项目National Natural Science Foundation of China[XDB26000000] ; Strategic Priority Research Program of the Chinese Academy of Sciences ; [42030510]
WOS研究方向Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:001054959100001
资助机构National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences
源URL[http://ir.nigpas.ac.cn/handle/332004/42647]  
专题中国科学院南京地质古生物研究所
通讯作者Zhen, Yong Yi
作者单位1.WB Clarke Geosci Ctr, Geol Survey New South Wales, 947-953 Londonderry Rd, Londonderry, NSW 2753, Australia
2.Chinese Acad Sci, State Key Lab Paleobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
3.Zhejiang Inst Geol Survey, Hangzhou 311203, Peoples R China
推荐引用方式
GB/T 7714
Zhen, Yong Yi,Zhang, Yuan-Dong,Chen, Zhong-Yang,et al. Origin and evolution of the Early Ordovician conodont genus Prioniodus Pander, 1856-New evidence from South China[J]. MARINE MICROPALEONTOLOGY,2023,183:16.
APA Zhen, Yong Yi,Zhang, Yuan-Dong,Chen, Zhong-Yang,&Wang, Long-Wu.(2023).Origin and evolution of the Early Ordovician conodont genus Prioniodus Pander, 1856-New evidence from South China.MARINE MICROPALEONTOLOGY,183,16.
MLA Zhen, Yong Yi,et al."Origin and evolution of the Early Ordovician conodont genus Prioniodus Pander, 1856-New evidence from South China".MARINE MICROPALEONTOLOGY 183(2023):16.

入库方式: OAI收割

来源:南京地质古生物研究所

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