首页> 美国卫生研究院文献>PLoS Clinical Trials >Living in the Past: Phylogeography and Population Histories of Indo-Pacific Wrasses (Genus Halichoeres) in Shallow Lagoons versus Outer Reef Slopes
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Living in the Past: Phylogeography and Population Histories of Indo-Pacific Wrasses (Genus Halichoeres) in Shallow Lagoons versus Outer Reef Slopes

机译:过去的生活:浅礁湖与外礁坡的印太平古藻类植物的系统志和种群史

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摘要

Sea level fluctuations during glacial cycles affect the distribution of shallow marine biota, exposing the continental shelf on a global scale, and displacing coral reef habitat to steep slopes on oceanic islands. In these circumstances we expect that species inhabiting lagoons should show shallow genetic architecture relative to species inhabiting more stable outer reefs. Here we test this expectation on an ocean-basin scale with four wrasses (genus Halichoeres): H. claudia (N = 194, with ocean-wide distribution) and H. ornatissimus (N = 346, a Hawaiian endemic) inhabit seaward reef slopes, whereas H. trimaculatus (N = 239) and H. margaritaceus (N = 118) inhabit lagoons and shallow habitats throughout the Pacific. Two mitochondrial markers (cytochrome oxidase I and control region) were sequenced to resolve population structure and history of each species. Haplotype and nucleotide diversity were similar among all four species. The outer reef species showed significantly less population structure, consistent with longer pelagic larval durations. Mismatch distributions and significant negative Fu’s F values indicate Pleistocene population expansion for all species, and (contrary to expectations) shallower histories in the outer slope species. We conclude that lagoonal wrasses may persist through glacial habitat disruptions, but are restricted to refugia during lower sea level stands. In contrast, outer reef slope species have homogeneous and well-connected populations through their entire ranges regardless of sea level fluctuations. These findings contradict the hypothesis that shallow species are less genetically diverse as a consequence of glacial cycles.
机译:冰川周期中的海平面波动会影响浅海生物区系的分布,使大陆架在全球范围内暴露,并使珊瑚礁栖息地向大洋洲的陡坡转移。在这种情况下,我们期望相对于居住在更稳定的外部礁石上的物种而言,居住在泻湖中的物种应显示出较浅的遗传结构。在这里,我们在海盆尺度上用四个濑鱼(Halichoeres属)检验了这种期望:H。claudia(N = 194,在整个海洋分布)和H. ornatissimus(N = 346,夏威夷特有种)栖息在海礁暗礁上,而H. trimaculatus(N = 239)和H. margaritaceus(N = 118)居住在整个太平洋的泻湖和浅层栖息地。对两个线粒体标记(细胞色素氧化酶I和控制区)进行了测序,以解析每个物种的种群结构和历史。在所有四个物种中,单倍型和核苷酸多样性相似。外礁物种显示出明显较少的种群结构,与更长的上层幼体持续时间一致。不匹配的分布和显着的Fu负F值表明所有物种的更新世种群都在扩张,并且(与预期相反)外坡物种的历史较浅。我们得出的结论是,泻湖濑鱼可能会因冰川生境破坏而持续存在,但在海平面下降时仅限于避难所。相反,无论海平面如何波动,礁石外坡物种在其整个范围内的种群均一且联系紧密。这些发现与以下假说相反:由于冰川循环,浅层物种的遗传多样性较少。

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