Spiny frogs (Paini) illuminate the history of the Himalayan region and Southeast Asia

CORC > 昆明动物研究所 > 昆明动物研究所 > 遗传资源与进化国家重点实验室 > 分子进化基因组学

	Spiny frogs (Paini) illuminate the history of the Himalayan region and Southeast Asia
	Che J 1,2; Zhou WW 1; Wake DB[]2; Zhang YP[]1,4; Hu JS 1,3; Yan F 1; Papenfuss TJ 2
刊名	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
	2010
卷号	107 期号:31 页码:13765-13770
关键词	China nuclear DNA phylogeography Tibet tribe Paini
通讯作者	wakelab@berkeley.edu ; zhangyp@mail.kiz.ac.cn
合作状况	其它
英文摘要	Asian frogs of the tribe Paini (Anura: Dicroglossidae) range across several first-order tectono-morphological domains of the Cenozoic Indo-Asian collision that include the Tibetan Plateau, the Himalayas, and Indochina. We show how the tectonic events induced by the Indo-Asian collision affected the regional biota and, in turn, how the geological history of the earth can be viewed from a biological perspective. Our analysis of a concatenated dataset comprising four nuclear gene sequences of Paini revealed two main radiations, corresponding to the genera Nanorana (I) and Quasipaa (II). Five distinct clades are recognized: Tibetan plateau clade (I-1), Himalaya clade (I-2), environs of Himalaya-Tibetan plateau clade (I-3), South China clade (II-1), and Indochina clade (II-2). This pattern of relationships highlights the significance of geography in shaping evolutionary history. Building on our molecular dating, ancestral region reconstruction, and distributional patterns, we hypothesize a distinct geographic and climatic transition in Asia beginning in the Oligocene and intensifying in the Miocene; this stimulated rapid diversification of Paini. Vicariance explains species formation among major lineages within Nanorana. Dispersal, in contrast, plays an important role among Quasipaa, with the southern Chinese taxa originating from Indochina. Our results support the tectonic hypothesis that an uplift in the Himalaya-Tibetan plateau region resulting from crustal thickening and lateral extrusion of Indochina occurred synchronously during the transition between Oligocene and Miocene in reaction to the Indo-Asian collision. The phylogenetic history of Paini illuminates critical aspects of the timing of geological events responsible for the current geography of Southeast Asia.
收录类别	SCI
资助信息	This work conducted in the laboratoryof Y.P.-Z.wassupportedbygrantsfromtheNationalBasicResearch Program of China (973 Program, Grant 2007CB411600), the National Natural Science Foundation of China, and the Bureau of Science and Technology of Yunnan Province. General support to the laboratory of D.B.W. was received from the US National Science Foundation AmphibiaTree of Life program (Grant EF-0339439).
语种	英语
内容类型	期刊论文
源URL	[http://159.226.149.26:8080/handle/152453/9605]
专题	昆明动物研究所_分子进化基因组学昆明动物研究所_遗传资源与进化国家重点实验室昆明动物研究所_两栖爬行类多样性与进化
作者单位	1.State Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming 650223, People’s Republic of China 2.Department of Integrative Biology, Museum of Vertebrate Zoology, University of California, Berkeley, CA 94720 3.College of Life Sciences,Yunnan University, Kunming 650091, People’s Republic of China 4.Laboratory for Conservation and Utilization of Bioresources, Yunnan University, Kunming 650091, People’s Republic of China
推荐引用方式 GB/T 7714	Che J,Zhou WW,Wake DB[*],et al. Spiny frogs (Paini) illuminate the history of the Himalayan region and Southeast Asia[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2010,107(31):13765-13770.
APA	Che J.,Zhou WW.,Wake DB[].,Zhang YP[].,Hu JS.,...&Papenfuss TJ.(2010).Spiny frogs (Paini) illuminate the history of the Himalayan region and Southeast Asia.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,107(31),13765-13770.
MLA	Che J,et al."Spiny frogs (Paini) illuminate the history of the Himalayan region and Southeast Asia".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 107.31(2010):13765-13770.