Pollen-based Miocene vegetation history from the Fotan Formation, SE China and its palaeoclimatic and palaeoenvironmental significances
文献类型：期刊论文
| 作者 | Yang, Yi1,2,3; Wang, Wei-Ming3 ; Shu, Jun-Wu3; Chen, Wei3; Shi, Gong-Le3
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| 刊名 | REVIEW OF PALAEOBOTANY AND PALYNOLOGY
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| 出版日期 | 2024-04-01 |
| 卷号 | 323页码:17 |
| 关键词 | Pollen Vegetation history Fotan Formation Miocene Southeastern China |
| ISSN号 | 0034-6667 |
| DOI | 10.1016/j.revpalbo.2024.105078 |
| 通讯作者 | Wang, Wei-Ming(wmwang@nigpas.ac.cn) |
| 英文摘要 | The Middle Miocene Zhangpu biota (similar to 14.7 Ma)-from the Fotan Formation in the Zhangpu area, southeastern China-indicates that the rainforest had reached at least 24.2 degrees N at that time. In this study, pollen analysis was carried out in six outcrop sections of this formation in the Zhangpu area. Based on the succession of palynoflora, three developmental stages of vegetation were recognized. From the late Early Miocene to the Middle Miocene Climatic Optimum (MMCO) (the first stage), the vegetation underwent frequent disturbances associated with the volcanic activities, in which two sub-stages are recognizable. During the earlier sub-stage (late Early Miocene), the vegetation was similar to the modern subtropical evergreen broad-leaved forest and exhibited a warming trend; then during the later sub-stage (MMCO), the tropical forest developed with the appearance of diverse tropical and subtropical taxa. The second stage, which was also within the MMCO, should be an intermission of volcanic eruptions, during which the tropical forest, especially the tropical montane rain forest, steadily developed without disruptions. And during the third stage (Middle to Late Miocene), the altitudinal vegetation belts of tropical montane rain forest significantly lowered which was accompanied by the occurrence of drought-tolerant taxa, implying the significant climatic cooling and moisture reduction. The above evolutionary phases of the vegetation in the Zhangpu area show a close relationship with the Miocene global climatic variations, which might be the main driving force of the vegetation changes in the southeast coast area of China during that period. |
| WOS关键词 | CLIMATE ; BASIN ; EVOLUTION ; MONSOON ; RECORD ; OLIGOCENE ; PLIOCENE ; FOREST ; CORES ; ROCKS |
| 资助项目 | Strategic Priority Research Program of Chinese Academy of Sciences[XDB26000000] ; National Natural Science Foundation of China[41472010] ; National Natural Science Foundation of China[41771219] |
| WOS研究方向 | Plant Sciences ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:001206354000001 |
| 出版者 | ELSEVIER |
| 资助机构 | Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/43651]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Wang, Wei-Ming |
| 作者单位 | 1.Chinese Acad Sci, CAS Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Xishuangbanna 666303, Peoples R China 2.Univ Sci & Technol China, Hefei 230026, Peoples R China 3.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yang, Yi,Wang, Wei-Ming,Shu, Jun-Wu,et al. Pollen-based Miocene vegetation history from the Fotan Formation, SE China and its palaeoclimatic and palaeoenvironmental significances[J]. REVIEW OF PALAEOBOTANY AND PALYNOLOGY,2024,323:17. |
| APA | Yang, Yi,Wang, Wei-Ming,Shu, Jun-Wu,Chen, Wei,&Shi, Gong-Le.(2024).Pollen-based Miocene vegetation history from the Fotan Formation, SE China and its palaeoclimatic and palaeoenvironmental significances.REVIEW OF PALAEOBOTANY AND PALYNOLOGY,323,17. |
| MLA | Yang, Yi,et al."Pollen-based Miocene vegetation history from the Fotan Formation, SE China and its palaeoclimatic and palaeoenvironmental significances".REVIEW OF PALAEOBOTANY AND PALYNOLOGY 323(2024):17. |
入库方式： OAI收割
来源：南京地质古生物研究所
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