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采用贝叶斯二项式 MCMC 分析探讨中国拟鲿(鲤科)的潜在殖民历史。

The potential colonization histories of Opsariichthys bidens (Cyprinidae) in China using Bayesian binary MCMC analysis.

机构信息

The Key Laboratory of Aquatic Biodiversity and Conservation of Chinese Academy of Sciences, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan, Hubei 430072, China; Pearl River Fisheries Research Institute, Chinese Academy of Fishery Sciences, Guangzhou, Guangdong 510380, China.

The Key Laboratory of Aquatic Biodiversity and Conservation of Chinese Academy of Sciences, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan, Hubei 430072, China.

出版信息

Gene. 2018 Nov 15;676:1-8. doi: 10.1016/j.gene.2018.07.019. Epub 2018 Jul 7.

Abstract

Vicariance and/or long-distance dispersal shape the distribution patterns of many extant taxa, and orogenesis and/or climate fluctuations are key factors that drive the events of vicariance and/or dispersal. In this study, we yielded biogeographical inferences from Bayesian binary MCMC (BBM) analysis to explore the potential colonization histories of Opsariichthys bidens in China and to identify potential factors responsible for the colonization histories. Many vicariance and dispersal events were identified. The results suggested that O. bidens seemed to have originated from the Yangtze River and/or the Pearl River and experienced a Yangtze River-Pearl River split at 7.04 million years ago (Ma). BBM analysis revealed that the Pearl River populations had undergone expansions to the Hainan drainages, the Lancangjiang River (upper Mekong) and the Nanpanjiang River (upper branch of the Pearl River) at 0.74 Ma. Meanwhile, the Yangtze River populations expanded to the northeastern drainages during the Early Pleistocene. Subsequently, the northeastern drainages dispersed to the Yellow River during the Middle Pleistocene. More recently, the northeastern drainage populations also dispersed to the Huaihe River and back to the Yangtze River. A portion of the Pearl River populations originated from the Yangtze River dispersed to the Jiulongjiang River during the Middle Pleistocene. These time scales fit well with the uplift of the Qinghai-Tibet Plateau and Pleistocene glacial cycles, indicating the two factors played vital roles in shaping the colonization histories of O. bidens.

摘要

地理隔离和/或远距离扩散塑造了许多现存生物类群的分布模式,造山运动和/或气候波动是驱动地理隔离和/或扩散事件的关键因素。在这项研究中,我们通过贝叶斯二分 MCMC(BBM)分析得出生物地理学推论,以探讨中国间臀鮈的潜在殖民历史,并确定导致其殖民历史的潜在因素。我们识别出了许多地理隔离和扩散事件。结果表明,间臀鮈似乎起源于长江和/或珠江,在 704 万年前经历了长江-珠江的分裂。BBM 分析表明,珠江种群在 740 万年前经历了向海南水系、澜沧江(上湄公河)和南盘江(珠江上游支流)的扩张。同时,长江种群在更新世早期向东北水系扩张。随后,东北水系在更新世中期扩散到黄河。最近,东北水系的种群也扩散到淮河,并返回长江。一部分来自长江的珠江种群在更新世中期扩散到九龙江。这些时间尺度与青藏高原的隆升和更新世冰期循环非常吻合,表明这两个因素在塑造间臀鮈的殖民历史中发挥了重要作用。

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