Revision of Middle Devonian stromatoporoid Climacostroma from South China
Huang, Jia-Yuan4,5; Kershaw, Stephen1,2,3; Liang, Kun4,5; Li, Yue4,5; Qie, Wen-Kun4,5
刊名PALAEOWORLD
2024-03-01
卷号33期号:1页码:92-104
关键词Syringostromatid stromatoporoid Climacostroma skeletal feature systematic revision three-dimensional reconstruction
ISSN号1871-174X
DOI10.1016/j.palwor.2022.12.013
通讯作者Qie, Wen-Kun(wkqie@nigpas.ac.cn)
英文摘要Climacostroma Yang and Dong, 1979, an endemic stromatoporoid genus, originally discovered in central Guangxi, South China, has remained enigmatic for over 40 years. Its validity and systematic position in the Order Stromatoporida (hypercalcified sponges) is here reinterpreted. In this study, the original collections of Climacostroma (including holotypes of C. guangxiense, C. microlaminatum and C. facetum) by Yang and Dong (1979) were re-examined, with improved images of the internal skeletons. We show that this genus is diagnostically characterized by thin microlaminae, dominant cassiculate structures between microlaminae, and distinct acosmoreticular to orthoreticular microstructures. Prior studies revealed similarities of Climacostroma with Stromatopora, Lineastroma, Ferestromatopora, Arctostroma, Habrostroma, and Parallelostroma. However, Climacostroma is markedly different from Stromatopora and Lineastroma by possessing thin microlaminae and microreticulate microstructure. Climacostroma is distinguished from Ferestromatopora and Arctostroma by the lack of dominant oblique or arched structures. Habrostroma differs from Climacostroma by the absence of prominent cassiculate structures. We found that Parallelostroma is most similar to Climacostroma in having dominant cassiculate structures between microlaminae and orthoreticular microstructure. Thus, we propose that Climacostroma is combined with Parallelostroma, and is reclassified under the Family Parallelostromatidae of the Order Syringostromatida, instead of its current position in the Family Stromatoporidae of the Order Stromatoporida. The three original species are here revised as two valid species, namely, P. guangxiense and P. microlaminatum. (c) 2022 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
资助项目Chinese Academy of Sciences[XDB26000000] ; National Natural Science Foundation of China[41772004] ; China Scholarship Council[202104910277]
WOS关键词REEF
WOS研究方向Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:001170029100001
资助机构Chinese Academy of Sciences ; National Natural Science Foundation of China ; China Scholarship Council
内容类型期刊论文
源URL[http://ir.nigpas.ac.cn/handle/332004/43424]  
专题中国科学院南京地质古生物研究所
通讯作者Qie, Wen-Kun
作者单位1.Nat Hist Museum, Earth Sci Dept, Cromwell Rd, London SW7 5BD, England
2.Brunel Univ, Dept Life Sci, Kingston Lane, Uxbridge UB8 3PH, England
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China
5.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
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Huang, Jia-Yuan,Kershaw, Stephen,Liang, Kun,et al. Revision of Middle Devonian stromatoporoid Climacostroma from South China[J]. PALAEOWORLD,2024,33(1):92-104.
APA Huang, Jia-Yuan,Kershaw, Stephen,Liang, Kun,Li, Yue,&Qie, Wen-Kun.(2024).Revision of Middle Devonian stromatoporoid Climacostroma from South China.PALAEOWORLD,33(1),92-104.
MLA Huang, Jia-Yuan,et al."Revision of Middle Devonian stromatoporoid Climacostroma from South China".PALAEOWORLD 33.1(2024):92-104.
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