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Molecular phylogeny of the Notostraca

机译:线虫的分子系统发育

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We used a combined analysis of one nuclear (28S rDNA) and three mitochondrial markers (COI, 12S rDNA, 16S rDNA) to infer the molecular phylogeny of the Notostraca, represented by samples from the six continents that are inhabited by this group of branchiopod crustaceans. Our results confirm the monophyly of both extant notostracan genera Triops and Lepidurus with good support in model based and maximum parsimony analyses. We used branchiopod fossils as a calibration to infer divergence times among notostracan lineages and accounted for rate heterogeneity among lineages by applying relaxed-clock models. Our divergence date estimates indicate an initial diversification into the genera Triops and Lepidurus in the Mesozoic, most likely at a minimum age of 152.3-233.5. Ma, i.e., in the Triassic or Jurassic. Implications for the interpretation of fossils and the evolution of notostracan morphology are discussed. We further use the divergence date estimates to formulate a biogeographic hypothesis that explains distributions of extant lineages predominantly by overland dispersal routes.We identified an additional hitherto unrecognised highly diverged lineage within Lepidurus apus lubbocki and three additional previously unknown major lineages within Triops. Within T. granarius we found deep differentiation, with representatives distributed among three major phylogenetic lineages. One of these major lineages comprises T. cancriformis, the T. mauritanicus species group and two hitherto unrecognised T. granarius lineages. Samples that were morphologically identified as T. granarius diverged from the most basal nodes within this major lineage, and divergence dates suggested an approximate age of 23.7-49.6. Ma for T. cancriformis, indicating the need for a taxonomic revision of Triassic and Permian fossils that are currently attributed to the extant T. cancriformis. We thus elevate T. cancriformis minor to full species status as Triops minor Trusheim, 1938 and include in this species the additional Upper Triassic samples that were attributed to T. cancriformis. We further elevate T. cancriformis permiensis to full species status as Triops permiensis Gand et al., 1997.
机译:我们结合使用了一个核(28S rDNA)和三个线粒体标记(COI,12S rDNA,16S rDNA)的组合分析来推断Notostraca的分子系统发育,这是由六大洲的这一类io足类甲壳动物所居住的样品代表的。我们的研究结果证实了现存的诺托斯坎人Triops和Lepidurus的单系性在基于模型和最大简约分析中具有良好的支持。我们使用支脚足类化石作为标定来推断诺斯塔坎谱系之间的发散时间,并通过应用宽松时钟模型解释了谱系之间的速率异质性。我们的离异日期估计表明,中生代最初进入了Triops和Lepidurus属,最可能的年龄是152.3-233.5。马,即在三叠纪或侏罗纪。讨论了对化石的解释和Notstrastracan形态演变的意义。我们进一步使用发散日期估计来制定生物地理假说,该假说主要通过陆上散布路线来解释现存谱系的分布。我们在Lepidurus apus lubbocki内发现了另外一个迄今未被认可的高度发散谱系,并在Triops内发现了另外三个以前未知的主要谱系。在T. granarius内,我们发现了深度分化,其代表分布在三个主要的系统发育谱系之间。这些主要血统中的一个包括坎氏锥虫(T. cancriformis),毛利氏锥虫(T. mauritanicus)物种组和两个迄今未获认可的格兰氏锥虫(T. granarius)血统。在形态上被鉴定为颗粒状T. granarius的样品与该主要谱系中最基础的节不同,并且分歧日期表明其年龄约为23.7-49.6。 Ma代表T. cancriformis,表明需要对三叠纪和二叠纪化石进行分类学修订,而目前归因于现存的T. cancriformis。因此,我们将未成年人T. cancriformis提升为全物种状态,即Triops minor Trusheim,1938年,并在该物种中加入了归因于Cancriformis的其他上三叠纪样品。我们将T. cancriformis permiensis进一步提升为Triops permiensis Gand等人,1997年的完整物种地位。

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