中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Effects of drainage reorganization on phytogeographic pattern in Sino-Himalaya

文献类型:期刊论文

作者Sun,Hang; Li,Zhimin; Landis,Jacob B.; Qian,Lishen; Zhang,Ticao; Deng,Tao
刊名ALPINE BOTANY
出版日期2022
卷号132期号:1页码:141-151
ISSN号1664-2201
关键词Sino-Himalaya Paleo Red River Valley plants Drainage reorganization Biogeographic evolution TERMINALIA-FRANCHETII COMBRETACEAE MEKONG-SALWEEN DIVIDE TANAKA-KAIYONG LINE RIVER-CAPTURE HENGDUAN MOUNTAINS GENETIC-STRUCTURE SOUTHWEST CHINA CYTOCHROME-B PHYLOGEOGRAPHY EVOLUTION
DOI10.1007/s00035-021-00269-4
英文摘要The Sino-Himalaya region is located in the southeast margin of the Qinghai-Tibetan Plateau (QTP) with several Asian rivers in this area, namely the Yarlung Zangbo River (YZR), Salween, Mekong, and Jinshajiang River and their tributaries. All these rivers currently flow independently into the Indian Ocean, the South China Sea (Pacific Ocean) and the East China Sea (Pacific Ocean). In geologic history, however, these rivers flowed southward into the Paleo-Red River (PRR), forming a huge drainage system, which then flowed into the South China Sea. From the end of the Neogene to the beginning of the Quaternary, with further uplift of the QTP, the monsoon climate was formed and strengthened bringing abundant precipitation leading to river erosion, rapid undercutting and a series of river capture events resulting in modern drainage systems and the beheading of the huge PRR. The reorganization of the PRR led to changes in the spatial pattern of river systems, subsequently affecting the geographical distribution of plants in the river valley. This paper reviews the effects of drainage evolution on the genetic structure and geographical pattern of plants in this region, and summarizes the resulting four types of discontinuous distribution patterns observed, namely: (1) the discontinuous distribution pattern between the Three River Valleys (TRV) (Salween, Mekong, Jinshajiang and their tributaries) and the Red River Basin (RRB); (2) the discontinuity between the Yarlung Zangbo River and the TRV-RRB; (3) the discontinuity among the TRV, and (4) the discontinuity between the east and west ends of the QTP. The conclusions from this review, while providing botanical evidence supporting and confirming the drainage evolution in Sino-Himalaya China, are the following: (1) the reorganization of drainage systems made the original continuous distribution pattern discontinuous, forming unique genetic and biogeographical characteristics, promoting the genetic differentiation of species and the formation of new taxa; (2) river capture events link different river systems together, bringing together the genetic diversity of different river valley species, increasing the richness of genetic diversity and the exchange of genes among populations; (3) the reorganization of river systems impacts the evolutionary history of valley plants and shapes their modern distribution patterns.
WOS记录号WOS:000692632700001
源URL[http://ir.kib.ac.cn/handle/151853/73294]  
专题中国科学院昆明植物研究所
作者单位1.Landis, Jacob B.] Cornell Univ, Sch Integrat Plant Sci, Sect Plant Biol & L H Bailey Hortorium, Ithaca, NY USA
2.Yunnan Univ Chinese Med, Sch Chinese Mat Med, Kunming 650500, Yunnan, Peoples R China
3.Chinese Acad Sci, Kunming Inst Bot, CAS Key Lab Plant Div & Biogeog East Asia, Kunming 650201, Yunnan, Peoples R China
4.Yunnan Normal Univ, Sch Life Sci, Kunming 650500, Yunnan, Peoples R China
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Sun,Hang,Li,Zhimin,Landis,Jacob B.,et al. Effects of drainage reorganization on phytogeographic pattern in Sino-Himalaya[J]. ALPINE BOTANY,2022,132(1):141-151.
APA Sun,Hang,Li,Zhimin,Landis,Jacob B.,Qian,Lishen,Zhang,Ticao,&Deng,Tao.(2022).Effects of drainage reorganization on phytogeographic pattern in Sino-Himalaya.ALPINE BOTANY,132(1),141-151.
MLA Sun,Hang,et al."Effects of drainage reorganization on phytogeographic pattern in Sino-Himalaya".ALPINE BOTANY 132.1(2022):141-151.

入库方式: OAI收割

来源:昆明植物研究所

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