中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Plant dispersal in the Devonian world (c. 419-359 Ma)

文献类型:期刊论文

作者Liu, Bing-Cai2,3,4; Wang, Kai2,3,4; Bai, Jiao2,3,4; Wang, Yao1,3,4; Huang, Bing3,4; Xu, Hong-He3,4
刊名PALAEONTOLOGY
出版日期2024-05-01
卷号67期号:3页码:16
关键词plant dispersal Devonian biogeography macroevolution deep time
ISSN号0031-0239
DOI10.1111/pala.12699
通讯作者Huang, Bing(bhuang@nigpas.ac.cn) ; Xu, Hong-He(hhxu@nigpas.ac.cn)
英文摘要Dispersal, whether active or passive, plays a crucial role in biogeography by facilitating the movement of propagules away from their original location. Botanical geographical zonation, resulting from the co-evolution of plants and their environment, has been established since the remarkable plant diversification during the Devonian Period (c. 419-359 Ma). However, a significant knowledge gap exists in understanding plant dispersal between living and fossil organisms due to the rarity of opportunities for tracing plant dispersal in geological history. In this study, we present evidence of two plant dispersal routes and verify their occurrence through the examination of geographical zonation, changes in plant diversity, and latitudinal and longitudinal gradients during the Devonian. We analyse global occurrence data from widely-distributed and extensively-studied Devonian plants. The two dispersal routes, namely clockwise and anticlockwise, connect the South China and Euramerica-Siberia realms. These routes clearly demonstrate inland and inter-land dispersal models, closely linked to Devonian sea-land topography and dispersal vectors such as wind and ocean currents. Moreover, these models probably apply to all Devonian plants. Our comprehensive synthesis of plant dispersal in deep time reveals that propagule diversity and dispersal vectors have progressively increased and become more complex over time, facilitating plant colonization and diversity changes. Importantly, our study unveils the dispersal models of fossil plants, demonstrating the equivalent models observed in extant plants that have been established since the Devonian Period.
WOS关键词MIDDLE ORDOVICIAN ; SEED DISPERSAL ; WEST JUNGGAR ; LAND PLANTS ; CHINA ; DIVERSITY ; EVOLUTION ; PATTERNS ; XINJIANG ; PALEOBIOGEOGRAPHY
资助项目National Key R&D Program of China ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences[CAS-WX2021SF-0205] ; Big Science Program ; [2022YFF0800200]
WOS研究方向Paleontology
语种英语
WOS记录号WOS:001218246300001
出版者WILEY
资助机构National Key R&D Program of China ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences ; Big Science Program
源URL[http://ir.nigpas.ac.cn/handle/332004/43743]  
专题中国科学院南京地质古生物研究所
通讯作者Huang, Bing; Xu, Hong-He
作者单位1.Qufu Normal Univ, Sch Geog & Tourism, Rizhao 276826, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China
4.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
推荐引用方式
GB/T 7714
Liu, Bing-Cai,Wang, Kai,Bai, Jiao,et al. Plant dispersal in the Devonian world (c. 419-359 Ma)[J]. PALAEONTOLOGY,2024,67(3):16.
APA Liu, Bing-Cai,Wang, Kai,Bai, Jiao,Wang, Yao,Huang, Bing,&Xu, Hong-He.(2024).Plant dispersal in the Devonian world (c. 419-359 Ma).PALAEONTOLOGY,67(3),16.
MLA Liu, Bing-Cai,et al."Plant dispersal in the Devonian world (c. 419-359 Ma)".PALAEONTOLOGY 67.3(2024):16.

入库方式: OAI收割

来源:南京地质古生物研究所

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