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首页> 外文期刊>Molecular phylogenetics and evolution >Recent vicariant and dispersal events affecting the phylogeny and biogeography of East Asian freshwater crab genus Nanhaipotamon (Decapoda: Potamidae)
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Recent vicariant and dispersal events affecting the phylogeny and biogeography of East Asian freshwater crab genus Nanhaipotamon (Decapoda: Potamidae)

机译:影响东亚淡水蟹属Nanhaipotamon(十足目:Potamidae)东亚淡水蟹属的系统发育和生物地理的近期杀害和传播事件

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摘要

The molecular phylogeny and biogeography of the East Asian freshwater crabs of the genus Nanhaipotamon (Decapoda: Brachyura: Potamidae) were studied, using two mitochondrial (16S rRNA and cytochrome oxidase I) and one nuclear (28S rRNA) markers, and correlated with various vicariant and dispersal events which have occurred in this region. The results showed Nanhaipotamon to be a monophyletic taxon with four clades which correspond to the topography of the coastal region of southeastern China and Taiwan Island. Mountains appear to play an important role in the distribution. The genus occurs only from east of the Wuyishan Range (Zhejiang and Fujian) and south of the Nanling Range (Guangdong) in southern China, and is also present west of the Central Range in Taiwan. The molecular and geological data suggest that Nanhaipotamon originated in an area between the Wuyishan and Nanling Ranges. In this area, the main and earliest cladogenesis occurred at ~4.8 million years ago (mya), with speciation probably taking place at around 4. mya. The molecular evidence strongly supports the recent invasion of the genus into Taiwan Island from northeastern Fujian, via the paleo-Minjiang River on the landbridge of Taiwan Strait. The presence of the genus in Dongyin Island, however, is through invasion from southeastern Zhejiang, during the Pleistocene glaciation period. Nanhaipotamon reached Taiwan and Dongyin Island at ~1.0 and 0.4. mya, respectively. A small population of Nanhaipotamon formosanum from Penghu Islands (Pescadores) in the central Taiwan Strait has a slightly different genetic constitution and suggests it is a relict of past Pleistocene glaciations.
机译:使用两个线粒体(16S rRNA和细胞色素氧化酶I)和一个核仁(28S rRNA)标记,研究了南海波坦属(Nhaihaipotamon)(十足目:Brachyura:波坦科)的东亚淡水蟹的分子系统发育和生物地理学,并与各种变种相关和该地区发生的扩散事件。结果表明,南海波达蒙是具有四个进化枝的单一类群,对应于中国东南沿海地区和台湾岛的地形。山脉似乎在分布中起着重要作用。该属仅发生在中国南部的武夷山山脉以东(浙江和福建)和南岭山脉以南(广东),也存在于台湾中部山脉以西。分子和地质数据表明,南海波达蒙起源于武夷山山脉和南岭山脉之间的地区。在该地区,主要的和最早的成岩作用发生在约480万年前(mya),物种形成可能发生在大约4. mya。分子证据有力地支持了该属最近从福建东北部通过台湾海峡陆桥上的古闽江入侵台湾岛。然而,东银岛属的存在是由于在更新世冰期期间浙江东南部的入侵。南海波达蒙在〜1.0和0.4到达台湾和东银岛。分别台湾海峡中部澎湖群岛(Pescadores)的一小部分南海波塔蒙(Naihaipotamon)福尔摩沙的遗传组成略有不同,这表明它是过去更新世冰川的遗迹。

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