KMS Nanjing Institute of Geology and Palaeonotology,CAS
A typical Euramerican floral element from the Shanxi Formation (Cisuralian, lower Permian) in the Wuda Coal Field, Inner Mongolia, North China | |
Wan, Mingli (万明礼)1,2,3![]() ![]() ![]() | |
2016-12-01 | |
发表期刊 | PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS
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ISSN | 1867-1594 |
卷号 | 96期号:4页码:507-515 |
摘要 | Autunia conferta (Sternberg) Kerp is one of the best known, earliest and most widespread callipterids in Euramerica during the Cisuralian. Unambiguous A. conferta foliage is for the first time recorded from Cathaysia in the Shanxi Formation of Wuda, Inner Mongolia, North China. Together with the find of Autunia naumannii (Gutbier) Kerp in the lowermost Permian strata of the same region, it proves that the radiation and spatio-temporal distribution of peltasperms was apparently not hampered by the floral provincialism, and it also indicates a mutual migration of floral elements between Cathaysia and Euramerica. Their long stratigraphic range, from the Cisuralian to the Lopingian, demonstrates that callipterids played an important role in the palaeotropical landscape and had a long history in North China during the Permian. The nearly absence of callipterids in typical Cisuralian wetland floras indicates their preference for well-drained settings and uplands. It is inferred that A. conferta lived contemporaneously with the wetland floral elements in Cathaysia during the Cisuralian, but commonly outside the window of preservation. |
关键词 | Autunia Conferta (Sternberg) Kerp Peltasperm Early Permian Wuda Cathaysia Flora North China |
DOI | 10.1007/s12549-016-0246-z |
语种 | 英语 |
关键词[WOS] | Paleobotany ; Peltasperms ; Palynology ; Western ; Plant ; Reclassification ; Paleoecology ; Brongniart ; Cathaysia ; Foliage |
资助项目 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18030404] ; Basic Project of State Key Laboratory of Palaeobiology and Stratigraphy ; National Nature Science Foundation of China[41502006] ; National Nature Science Foundation of China[41530101] ; National Nature Science Foundation of China[41372011] ; National Nature Science Foundation of China[41372010] ; National Nature Science Foundation of China[J1210006] ; National Nature Science Foundation of China[41472005] ; China Scholarship Council |
WOS研究方向 | Biodiversity & Conservation ; Paleontology |
WOS类目 | Biodiversity Conservation ; Paleontology |
WOS记录号 | WOS:000388113300001 |
项目资助者 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Basic Project of State Key Laboratory of Palaeobiology and Stratigraphy ; National Nature Science Foundation of China ; China Scholarship Council |
出版者 | SPRINGER HEIDELBERG |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/12659 |
专题 | 中国科学院南京地质古生物研究所 中国科学院南京地质古生物研究所 其他 |
通讯作者 | Wang, Jun (王军) |
作者单位 | 1.Chinese Acad Sci, Dept Palaeobotany & Palynol, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 3.Missouri Univ Sci & Technol, Geol & Geophys Program, Rolla, MO 65409 USA 4.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Peoples R China 5.Anhui Geol Museum, Hefei 230031, Peoples R China |
第一作者单位 | 中国科学院南京地质古生物研究所 |
通讯作者单位 | 中国科学院南京地质古生物研究所 |
推荐引用方式 GB/T 7714 | Wan, Mingli ,Zhou, Weiming ,He, Xuezhi ,et al. A typical Euramerican floral element from the Shanxi Formation (Cisuralian, lower Permian) in the Wuda Coal Field, Inner Mongolia, North China[J]. PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS,2016,96(4):507-515. |
APA | Wan, Mingli ,Zhou, Weiming ,He, Xuezhi ,Liu, Lujun ,&Wang, Jun .(2016).A typical Euramerican floral element from the Shanxi Formation (Cisuralian, lower Permian) in the Wuda Coal Field, Inner Mongolia, North China.PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS,96(4),507-515. |
MLA | Wan, Mingli ,et al."A typical Euramerican floral element from the Shanxi Formation (Cisuralian, lower Permian) in the Wuda Coal Field, Inner Mongolia, North China".PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS 96.4(2016):507-515. |
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