Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Av. Ciudad Universitaria 3000, C.P. 04510 Coyoacán, Ciudad de México, Mexico; Instituto Nacional de Biodiversidad (INABIO), Colección de Peces Calle Rumipamba 341, Av. De los Shyris, Parque "La Carolina", Quito, Ecuador.
CONACYT-Laboratorio de Zoología, Facultad de Ciencias Naturales, Universidad Autónoma de Querétaro, Av. De las Ciencias s/n, Juriquilla, C.P 76230. Delegación Santa Rosa Jáuregui, Santiago de Querétaro, Mexico.
Mol Phylogenet Evol. 2022 Aug;173:107496. doi: 10.1016/j.ympev.2022.107496. Epub 2022 May 17.
The Panamic Clingfish Gobiesox adustus is widely distributed in the Tropical Eastern Pacific (TEP), from the central Gulf of California, Mexico to Ecuador, including the oceanic Revillagigedo Archipelago, and Isla del Coco. This cryptobenthic species is restricted to very shallow rocky-reef habitats. Here, we used one mitochondrial and three nuclear DNA markers from 155 individuals collected across the distribution range of the species in order to evaluate if geographically structured populations exist and to elucidate its evolutionary history. Phylogenetic analyses recovered a monophyletic group, with four well-supported, allopatric subgroups. Each subgroup corresponded to one of the following well-known biogeographic regions/provinces: 1) the Revillagigedo Archipelago, 2) the Cortez + Mexican provinces (Mexico), 3) the Panamic province (from El Salvador to Ecuador), and 4) Isla del Coco. A molecular-clock analysis showed a mean date for the divergence between clade I (the Revillagigedos and Cortez + Mexican provinces) and clade II (Panamic province and Isla del Coco) in the Pliocene, at ca. 5.33 Mya. Within clade I, the segregation between the Revillagigedos and Cortez + Mexican province populations was dated at ca. 1.18 Mya, during the Pleistocene. Within clade II, the segregation between samples of Isla del Coco and the Panamic province samples was dated at ca. 0.77 Mya, during the Pleistocene. The species tree, Bayesian species delimitation tests (BPP and STACEY), the Φ, AMOVA, and the substantial genetic distances that exist between those four subgroups, indicate that they are independent evolutionary units. These cladogenetic events seem to be related to habitat discontinuities, and oceanographic and geological processes that produce barriers to gene flow for G. adustus, effects of which are enhanced by the intrinsic ecological characteristics of this species.
巴拿马吸盘鱼(Gobiesox adustus)广泛分布于热带东太平洋(TEP)地区,从墨西哥加利福尼亚湾中部到厄瓜多尔,包括大洋中的拉维加吉多群岛和可可岛。这种穴居底栖物种仅限于非常浅的岩石礁栖息地。在这里,我们使用了来自该物种分布范围内的 155 个个体的一个线粒体和三个核 DNA 标记,以评估是否存在地理结构种群,并阐明其进化历史。系统发育分析回收了一个单系群,有四个支持良好的、异域的亚群。每个亚群对应于以下一个著名的生物地理区域/省份:1)拉维加吉多群岛,2)科尔特斯+墨西哥省(墨西哥),3)巴拿马省(从萨尔瓦多到厄瓜多尔),和 4)可可岛。分子钟分析显示,在渐新世,支系 I(拉维加吉多群岛和科尔特斯+墨西哥省)和支系 II(巴拿马省和可可岛)之间的分歧的平均日期约为 533 万年前。在支系 I 内,拉维加吉多群岛和科尔特斯+墨西哥省种群的分离发生在更新世,约为 118 万年前。在支系 II 内,可可岛和巴拿马省样本之间的分离发生在更新世,约为 77 万年前。种系发生树、贝叶斯物种界定测试(BPP 和 STACEY)、Φ、AMOVA 以及这四个亚群之间存在的大量遗传距离表明,它们是独立的进化单位。这些分支事件似乎与栖息地不连续性以及产生 G. adustus 基因流障碍的海洋学和地质过程有关,这些效应因该物种的内在生态特征而增强。