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沙钱属 Mellita 的系统地理学研究:沿美洲海岸的隐存物种形成。

Phylogeography of the sand dollar genus Mellita: cryptic speciation along the coasts of the Americas.

机构信息

Smithsonian Tropical Research Institute, Box 0843-03092, Balboa, Panama.

出版信息

Mol Phylogenet Evol. 2013 Dec;69(3):1033-42. doi: 10.1016/j.ympev.2013.05.028. Epub 2013 Jun 20.

DOI:10.1016/j.ympev.2013.05.028
PMID:23792155
Abstract

Sand dollars of the genus Mellita are members of the sandy shallow-water fauna. The genus ranges in tropical and subtropical regions on the two coasts of the Americas. To reconstruct the phylogeography of the genus we sequenced parts of the mitochondrial cytochrome oxidase I and of 16S rRNA as well as part of the nuclear 28S rRNA gene from a total of 185 specimens of all ten described morphospecies from 31 localities. Our analyses revealed the presence of eleven species, including six cryptic species. Sequences of five morphospecies do not constitute monophyletic molecular units and thus probably represent ecophenotypic variants. The fossil-calibrated phylogeny showed that the ancestor of Mellita diverged into a Pacific lineage and an Atlantic+Pacific lineage close to the Miocene/Pliocene boundary. Atlantic M. tenuis, M. quinquiesperforata and two undescribed species of Mellita have non-overlapping distributions. Pacific Mellita consist of two highly divergent lineages that became established at different times, resulting in sympatric M. longifissa and M. notabilis. Judged by modern day ranges, not all divergence in this genus conforms to an allopatric speciation model. Only the separation of M. quinquiesperforata from M. notabilis is clearly due to vicariance as the result of the completion of the Isthmus of Panama. The molecular phylogeny calibrated on fossil evidence estimated this event as having occurred ~3 Ma, thus providing evidence that, contrary to a recent proposal, the central American Isthmus was not completed until this date.

摘要

砂金钱属 Mellita 是浅海沙生动物的成员。该属分布于美洲东西两岸的热带和亚热带地区。为了重建该属的系统地理学,我们从总共 31 个地点的 185 个形态种标本中,对线粒体细胞色素氧化酶 I 和 16S rRNA 的部分序列以及核 28S rRNA 基因的部分序列进行了测序。我们的分析揭示了存在 11 个物种,包括 6 个隐种。五个形态种的序列不构成单系分子单位,因此可能代表生态表型变体。经过化石校准的系统发育树表明,Mellita 的祖先在中新世/上新世边界附近分为太平洋谱系和大西洋+太平洋谱系。大西洋 M. tenuis、M. quinquiesperforata 和两个未描述的 Mellita 物种的分布没有重叠。太平洋 Mellita 由两个高度分化的谱系组成,它们在不同的时间建立,导致了同域的 M. longifissa 和 M. notabilis。根据现代的分布范围,该属的所有分化并不都符合异域物种形成模型。只有 M. quinquiesperforata 从 M. notabilis 的分离显然是由于巴拿马地峡的形成导致的隔离,因为这是巴拿马地峡形成的结果。基于化石证据进行校准的分子系统发育树估计这一事件发生在约 300 万年前,这为一个与最近的提议相反的观点提供了证据,即中美洲地峡直到这个时候才完成。

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