Phylogenetic reconstruction, divergence time estimations and ancestral range estimation were undertaken for 66% of the Afrotropical freshwater crab fauna (Potamonautidae) based on four partial DNA loci (12S rRNA, 16S rRNA, cytochrome oxidase one [COI], and histone 3). The present study represents the most comprehensive taxonomic sampling of any freshwater crab family globally, and explores the impact of paleodrainage interconnectivity on cladogenesis among freshwater crabs. Phylogenetic analyses of the total evidence data using maximum-likelihood (ML), maximum parsimony (MP), and Bayesian inference (BI) produced a robust statistically well-supported tree topology that reaffirmed the monophyly of the Afrotropical freshwater crab fauna. The estimated divergence times suggest that the Afrotropical Potamonautidae diverged during the Eocene. Cladogenesis within and among several genera occurred predominantly during the Miocene, which was associated with major tectonic and climatic ameliorations throughout the region. Paleodrainage connectivity was observed with specimens from the Nilo-Sudan and East African coast proving to be sister to specimens from the Upper Guinea Forests in West Africa. In addition, we observed strong sister taxon affinity between specimens from East Africa and the Congo basin, including specimens from Lake Tanganyika, while the southern African fauna was retrieved as sister to the Angolan taxa. Within the East African clade we observed two independent transoceanic dispersal events, one to the Seychelles Archipelago and a second to Madagascar, while we observe a single transoceanic dispersal event from West Africa to São Tomé. The ancestral area estimation suggested a West African/East African ancestral range for the family with multiple dispersal events between southern Africa and East Africa, and between East Africa and Central Africa The taxonomic implications of our results are discussed in light of the widespread paraphyly evident among a number of genera.

译文

:根据66个非热带淡水蟹类动物(Potamonautidae)的系统发育重建,发散时间估计和祖传范围估计,基于四个部分DNA基因座(12S rRNA,16S rRNA,细胞色素氧化酶1 [COI]和组蛋白3)。本研究代表了全球任何淡水蟹家族中最全面的生物分类学采样,并探讨了古排水互连对淡水蟹克拉德形成的影响。使用最大似然(ML),最大简约(MP)和贝叶斯推断(BI)对总证据数据进行的系统发育分析产生了可靠的统计上有力的树形拓扑结构,该拓扑结构再次证实了非嗜水淡水蟹类动物的单性。估计的发散时间表明,在始新世期间,非洲的Pot科(Potamonautidae)发生了发散。在中新世期间,几个属内和之中的新生发生主要发生在中新世,这与整个区域的主要构造和气候改善有关。在尼洛苏丹和东非海岸的标本中发现了古排水的连通性,事实证明它们与西非上几内亚森林的标本是姐妹的。此外,我们观察到东非和刚果盆地标本(包括坦Tang尼喀湖的标本)之间的姐妹分类群亲和力很强,而南部非洲动物群则被当作安哥拉分类群的姐妹而被发现。在东非进化枝中,我们观察到两次独立的越洋扩散事件,一次发生在塞舌尔群岛,第二次发生在马达加斯加,而我们观测到从西非到圣多美的一次越洋扩散事件。祖先面积估计表明该家族在南部非洲和东非之间以及东非和中非之间有多个分散事件的家庭的祖传范围是西欧/东非。一些属。

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