Paleontologic, paleogeographic, and sedimentologic controls on the spatial-temporal distribution of Permian sponge reefs in South China
文献类型：期刊论文
| 作者 | Tian, Xuesong1,2,3; Liang, Kun2 ; Vinn, Olev4; Chen, Dishu1,3,5; Zhang, Feng6; Cao, Rui6; Wang, Yue2,7
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| 刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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| 出版日期 | 2024-11-15 |
| 卷号 | 654页码:20 |
| 关键词 | Permian sponge reef South China Frame-building hypercalcified sponge Time-spaced distribution Geological controlled factors Two reef-forming intervals |
| ISSN号 | 0031-0182 |
| DOI | 10.1016/j.palaeo.2024.112472 |
| 通讯作者 | Vinn, Olev(olev.vinn@ut.ee) ; Chen, Dishu(cds1003chengdu@163.com) ; Wang, Yue(yuewang@nigpas.ac.cn) |
| 英文摘要 | The Permian sponge reefs belong to several distinct types, and their taxonomic composition and distribution vary. Their development and succession depend both on intrinsic and extrinsic control mechanisms. The well- documented outcrops in South China, encompassing Permian sponge reefs have been sampled and investigated in aspects of palaeontology, stratigraphy, sedimentology, and paleogeography. Two major reef-forming intervals, namely the Roadian to Capitanian and the late Wuchiapingian to Changhsingian, were recorded mainly in the Maokou and Changxing formations. The sponge reefs in these formations could be morphologically subdivided into three types: fringing reef, patch reef, and barrier reef. From the Roadian to Capitanian, fringing reefs developed near a littoral clastic shelf, and barrier reefs mainly presented on the margin of the isolated carbonate platforms within the Dian-Qian-Gui Basin. These reefs were dominated by frame-building hyper- calcified sponges, including Amblysiphonella, , Tebagathalamia, , Rhabdactinia, Intrasporeocoelia, and Cystothalamia of sphinctozoa and Peronidella, , Stellispongia, , Guangxinella and Grossotubenella of inozoa. From late Wuchiapingian to Changhsingian, patch reefs distributed on the middle-upper Yangtze Platform and on the isolated platforms within the North Yangtze Basin and Dian-Qian-Gui Basin. The barrier reefs located on the margin of the Yangtze Platform facing the North Yangtze and Jiangnan basins and on the margin of the isolated platforms within the Dian-Qian-Gui Basin. Frame-building hypercalcified sponges were dominated by Amblysiphonella, , Sollasia, Lichuanospongia, Intrasporeocoelia of sphinctozoa, and Peronidella of inozoa. . The highly diversified and abundant hypercalcified sphinctozoans and inozoans, as well as massive microencrusters and binders made great contributions to the formation of sponge reefs. The subtidal high-energy shoal and the stable carbonate platform environment at the low-latitudes provided the favorable habitat for the growth of sponge reefs. Once these conditions could not be met simultaneously, sponge reefs would rapidly decrease and disappear, as it happened during the latest Capitanian and the latest Changhsingian. |
| WOS关键词 | MASS EXTINCTION ; PANLONGDONG SECTION ; OCEANIC CONDITIONS ; NANPANJIANG BASIN ; WESTERN HUBEI ; LAIBIN AREA ; END ; BOUNDARY ; PLATFORM ; COUNTY |
| 资助项目 | National Natural Science Foundation of China[41830323] ; National Natural Science Foundation of China[42302027] ; Natural Science Foundation of Chongqing[CSTB2022NSCQ-MSX1221] ; Open Fund of State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS)[193127] ; China Geological Survey[DD20221829] ; Gas Production Plant 5 of PetroChina Changqing Oilfield Company[CQWC-2023-201] |
| WOS研究方向 | Physical Geography ; Geology ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:001333961400001 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Foundation of China ; Natural Science Foundation of Chongqing ; Open Fund of State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) ; China Geological Survey ; Gas Production Plant 5 of PetroChina Changqing Oilfield Company |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/44422]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Vinn, Olev; Chen, Dishu; Wang, Yue |
| 作者单位 | 1.Chongqing Inst Geol & Mineral Resources, Minist Nat Resources, Key Lab Shale Gas Explorat, Chongqing 401120, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Key Lab Palaeobiol & Petr Stratig, Nanjing 210008, Peoples R China 3.Chongqing Huadi Resources & Environm Technol Co LT, Chongqing 401120, Peoples R China 4.Univ Tartu, Dept Geol, Ravila 14A, EE-50411 Tartu, Estonia 5.China Univ Geosci Wuhan, Sch Earth Resources, Wuhan 430074, Peoples R China 6.Chongqing Geol & Mineral Resource Explorat & Dev, Hydrogeol & Engn Geol Team 208, Chongqing 400070, Peoples R China 7.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Tian, Xuesong,Liang, Kun,Vinn, Olev,et al. Paleontologic, paleogeographic, and sedimentologic controls on the spatial-temporal distribution of Permian sponge reefs in South China[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2024,654:20. |
| APA | Tian, Xuesong.,Liang, Kun.,Vinn, Olev.,Chen, Dishu.,Zhang, Feng.,...&Wang, Yue.(2024).Paleontologic, paleogeographic, and sedimentologic controls on the spatial-temporal distribution of Permian sponge reefs in South China.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,654,20. |
| MLA | Tian, Xuesong,et al."Paleontologic, paleogeographic, and sedimentologic controls on the spatial-temporal distribution of Permian sponge reefs in South China".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 654(2024):20. |
入库方式： OAI收割
来源：南京地质古生物研究所
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