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A new pterosaur (Pterodactyloidea, Tapejaridae) from the Early Cretaceous Jiufotang Formation of western Liaoning, China and its implications for biostratigraphy
Wang, XL; Zhou, ZH; Wang, XL (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
2003
发表期刊CHINESE SCIENCE BULLETIN
ISSN1001-6538
卷号48期号:1页码:16-23
文章类型Article
摘要In this article we describe a new and exceptionally well-preserved pterodactyloid pterosaur, Sinopterus dongi gen. et sp. nov. from the Jiufotang Formation in western Liaoning Province of northeast China. The new species is referred to the family Tapejaridae, representing its first record outside Brazil. It also represents the earliest occurrence as well as the most complete skeleton of the family. Some revisions are made about the family according to the morphological observations of the postcranial bones of Sinopterits. Two pterosaur assemblages appear to have existed in the Jehol Group, represented by the lower Yixian Formation and upper Jiufotang Formation, respectively. The lower pterosaur assemblage shows some resemblance to that of the Late Jurassic in Solnhofen (Tithonian) by sharing members of the Pterodactylidae and Anurognathidae. The upper one shows more resemblance to that of the Early Cretaceous Santana Formation (Aptian/Albian) by comprising only pterodactyloids such as the Tapejaridae. The age of the Yixian Formation is younger than that of the Solnhofen lithographic limestone, and the age of the Jiufotang Formation (Aptian) is slightly older than the Santana Formation.; In this article we describe a new and exceptionally well-preserved pterodactyloid pterosaur, Sinopterus dongi gen. et sp. nov. from the Jiufotang Formation in western Liaoning Province of northeast China. The new species is referred to the family Tapejaridae, representing its first record outside Brazil. It also represents the earliest occurrence as well as the most complete skeleton of the family. Some revisions are made about the family according to the morphological observations of the postcranial bones of Sinopterits. Two pterosaur assemblages appear to have existed in the Jehol Group, represented by the lower Yixian Formation and upper Jiufotang Formation, respectively. The lower pterosaur assemblage shows some resemblance to that of the Late Jurassic in Solnhofen (Tithonian) by sharing members of the Pterodactylidae and Anurognathidae. The upper one shows more resemblance to that of the Early Cretaceous Santana Formation (Aptian/Albian) by comprising only pterodactyloids such as the Tapejaridae. The age of the Yixian Formation is younger than that of the Solnhofen lithographic limestone, and the age of the Jiufotang Formation (Aptian) is slightly older than the Santana Formation.
关键词Pterodactyloidea Tapejaridae Sinopterus Jiufotang Formation Jehol Group Biostratigraphy Chaoyang Liaoning
WOS标题词Science & Technology
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关键词[WOS]YIXIAN FORMATION ; AGE ; DINOSAUR
收录类别SCI
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000180522700003
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3761
专题中科院古脊椎所(2000年以后)
古低等脊椎动物研究室
通讯作者Wang, XL (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
作者单位Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
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GB/T 7714
Wang, XL,Zhou, ZH,Wang, XL . A new pterosaur (Pterodactyloidea, Tapejaridae) from the Early Cretaceous Jiufotang Formation of western Liaoning, China and its implications for biostratigraphy[J]. CHINESE SCIENCE BULLETIN,2003,48(1):16-23.
APA Wang, XL,Zhou, ZH,&Wang, XL .(2003).A new pterosaur (Pterodactyloidea, Tapejaridae) from the Early Cretaceous Jiufotang Formation of western Liaoning, China and its implications for biostratigraphy.CHINESE SCIENCE BULLETIN,48(1),16-23.
MLA Wang, XL,et al."A new pterosaur (Pterodactyloidea, Tapejaridae) from the Early Cretaceous Jiufotang Formation of western Liaoning, China and its implications for biostratigraphy".CHINESE SCIENCE BULLETIN 48.1(2003):16-23.
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