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A juvenile anuran from the Lower Cretaceous Jiufotang Formation, Liaoning, China
Wang, Yuan; Jones, Marc E. H.; Evans, Susan E.; Wang, Y (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
2007-04-01
发表期刊CRETACEOUS RESEARCH
ISSN0195-6671
卷号28期号:2页码:235-244
文章类型Article
摘要A disarticulated partial skeleton of a juvenile anuran is reported from the Lower Cretaceous Jiufotang Formation, Jehol Group, in Liaoning Province, China. The individual has a premaxilla with a tall, wide bifurcate alary process and a well-defined palatine process; a maxilla without pre- or postorbital processes; and no contact between the squamosal and the maxilla. The centra of the presacral vertebrae are notochordal. The urostyle (with transverse processes) and the pelvic girdle are proportionally short, and the hind limbs are long (including proportionally long femur, fibiofibula, and proximal tarsals), and the tibiotibula is considerably longer than the femur. Comparison with other frogs suggests the hindlimb proportions of the Jiufotang frog are similar to those of anurans that are primarily saltatory. Although body proportions and other osteological features distinguish the Jiufotang anuran from other Jehol taxa, its immaturity and fragmentary preservation preclude detailed discussion of its systematic position. Nonetheless, this frog documents not only the first fossil anuran from the Aptian Jiufotang Formation of China, but also the most recent Mesozoic anuran currently known from China. (C) 2006 Elsevier Ltd. All rights reserved.; A disarticulated partial skeleton of a juvenile anuran is reported from the Lower Cretaceous Jiufotang Formation, Jehol Group, in Liaoning Province, China. The individual has a premaxilla with a tall, wide bifurcate alary process and a well-defined palatine process; a maxilla without pre- or postorbital processes; and no contact between the squamosal and the maxilla. The centra of the presacral vertebrae are notochordal. The urostyle (with transverse processes) and the pelvic girdle are proportionally short, and the hind limbs are long (including proportionally long femur, fibiofibula, and proximal tarsals), and the tibiotibula is considerably longer than the femur. Comparison with other frogs suggests the hindlimb proportions of the Jiufotang frog are similar to those of anurans that are primarily saltatory. Although body proportions and other osteological features distinguish the Jiufotang anuran from other Jehol taxa, its immaturity and fragmentary preservation preclude detailed discussion of its systematic position. Nonetheless, this frog documents not only the first fossil anuran from the Aptian Jiufotang Formation of China, but also the most recent Mesozoic anuran currently known from China. (C) 2006 Elsevier Ltd. All rights reserved.
关键词Anura Early Cretaceous Jiufotang Formation Jehol Biota China Development Limb Proportions
WOS标题词Science & Technology ; Physical Sciences ; Life Sciences & Biomedicine
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关键词[WOS]SKELETAL DEVELOPMENT ; CRANIAL OSSIFICATION ; MESOZOIC ANURANS ; FROG ; OSTEOLOGY ; AMPHIBIA ; LEPTODACTYLIDAE ; DISCOGLOSSIDAE ; ONTOGENY ; SEQUENCE
收录类别SCI
语种英语
WOS研究方向Geology ; Paleontology
WOS类目Geology ; Paleontology
WOS记录号WOS:000246762700010
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3365
专题中科院古脊椎所(2000年以后)
通讯作者Wang, Y (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
2.UCL, Dept Anat & Dev Biol, London WC1E 6BT, England
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Wang, Yuan,Jones, Marc E. H.,Evans, Susan E.,et al. A juvenile anuran from the Lower Cretaceous Jiufotang Formation, Liaoning, China[J]. CRETACEOUS RESEARCH,2007,28(2):235-244.
APA Wang, Yuan,Jones, Marc E. H.,Evans, Susan E.,&Wang, Y .(2007).A juvenile anuran from the Lower Cretaceous Jiufotang Formation, Liaoning, China.CRETACEOUS RESEARCH,28(2),235-244.
MLA Wang, Yuan,et al."A juvenile anuran from the Lower Cretaceous Jiufotang Formation, Liaoning, China".CRETACEOUS RESEARCH 28.2(2007):235-244.
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