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景观演化在中国南方一种溪流鱼类遗传多样性中的作用。

The role of landscape evolution in the genetic diversification of a stream fish from Southern China.

作者信息

Li Mingyue, Yang Xishu, Ni Xiaomin, Fu Cuizhang

机构信息

Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, Coastal Ecosystems Research Station of the Yangtze River Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China.

出版信息

Front Genet. 2023 Jan 6;13:1075617. doi: 10.3389/fgene.2022.1075617. eCollection 2022.

Abstract

(Cypriniformes: Gobionidae) is a stream fish which is endemic to sub-tropical coastal drainages in southern China, thus offering a valuable model for understanding how genetic divergence arises in stream-adapting freshwater fishes in this region. Using the mitochondrial Cyt gene, integrative analyses of phylogeny, population demography, and ancestral area and paleo-drainage reconstructions are carried out to explicitly explore the role of landscape evolution in genetic diversification of . The time-calibrated phylogeny of indicates the splitting of two major lineages (A and B) at ∼3.66 Ma. Lineage A inhabits the Poyang Lake sub-drainage of the middle Yangtze River, Han River and Pearl River, and can be split into two sub-lineages (A-I and A-II), where sub-lineage A-II can be further sub-divided into three infra-sub-lineages (A-IIa, A-IIb and A-IIc). Except for the infra-sub-lineage A-IIc, which is restricted to the Han River and Pearl River, the other sub-lineages and infra-sub-lineages live exclusively in the Poyang Lake sub-drainage. Lineage B lives in the lower Yangtze River, Qiantang River, Jiaojiang River and Ou River, displaying close genetic relationships among the drainages. Rapid population expansion has occurred since the Late Pleistocene. Our findings indicate that the splitting of lineages A and B could be attributed to geographic isolation due to the Zhe-Min Uplift, acting as a biogeographic barrier before the late Early Pleistocene. Furthermore, the strong genetic divergence within Lineage A could be explained by the isolation role of the Nanling Mountains and Poyang Lake acting as an ecological barrier; while the lack of phylogenetic structure within Lineage B may have been the result of paleo-drainage connections or episodic freshwater connections during the eustatic low stand of sea level in the late Middle-Late Pleistocene.

摘要

(鲤形目:鲤科)是一种溪流鱼类,为中国南方亚热带沿海流域特有,因此为理解该地区适应溪流的淡水鱼类如何发生遗传分化提供了宝贵模型。利用线粒体Cyt基因,开展了系统发育、种群动态、祖先区域及古水系重建的综合分析,以明确探讨景观演化在[该鱼类名称]遗传多样化中的作用。[该鱼类名称]的时间校准系统发育表明,两个主要谱系(A和B)在约366万年前发生分裂。谱系A栖息于长江中游的鄱阳湖子流域、汉江和珠江,可分为两个亚谱系(A-I和A-II),其中亚谱系A-II可进一步细分为三个次亚谱系(A-IIa、A-IIb和A-IIc)。除了局限于汉江和珠江的次亚谱系A-IIc外,其他亚谱系和次亚谱系仅生活在鄱阳湖子流域。谱系B生活在长江下游、钱塘江、椒江和瓯江,各流域间显示出密切的遗传关系。自晚更新世以来发生了快速的种群扩张。我们的研究结果表明,谱系A和B的分裂可能归因于早更新世晚期之前作为生物地理屏障的浙闽隆起导致的地理隔离。此外,谱系A内强烈的遗传分化可由南岭山脉和鄱阳湖作为生态屏障的隔离作用来解释;而谱系B内缺乏系统发育结构可能是中晚更新世晚期海平面下降期间古水系连接或间歇性淡水连接的结果。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5ae1/9853433/dc68a48fa643/fgene-13-1075617-g001.jpg

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