RESUMEN
Genetic deviation between two deep-sea snailfishes, Careproctus pellucidus from the Pacific Ocean and Careproctus rastrinus from the Okhotsk Sea, of the Careproctus rastrinus species complex was analyzed, based on the nucleotide sequences of the mitochondrial cytochrome b (Cytb) gene. Our sampling revealed the occurrence of individuals with C. rastrinus-type Cytb genes off northeastern Japan, in the northwestern Pacific. Most of these individuals were collected from an area off Miyagi Prefecture, while few individuals were collected from areas to its north (off Iwate Prefecture) and south (off Fukushima and Ibaraki Prefectures). Phylogeographic analyses based on nucleotide sequences of the first intron region of the nuclear S7 ribosomal protein gene (S7) and 11 microsatellite loci indicated little genetic deviation between individuals with C. pellucidus-type and C. rastrinus-type Cytb genes in the area off Miyagi Prefecture. Significant genetic differences between the Pacific Ocean and the Okhotsk Sea populations may be attributed to unidirectional migration due to a greater current from the latter to the former. In addition, peritoneum and stomach colors of 10 and 17 specimens collected from the Pacific Ocean and the Okhotsk Sea, respectively, were evaluated quantitatively. The colors were significantly different for the two populations; however, they appeared to overlap. Although only one Pacific individual with a C. rastrinus-type Cytb gene was available for color evaluation, it was more similar to Pacific individuals than to Okhotsk Sea individuals. These results suggest inbreeding between C. pellucidus and C. rastrinus in the Pacific Ocean, off Miyagi Prefecture.
Asunto(s)
Distribución Animal , Peces/genética , Variación Genética , Hibridación Genética , Animales , Citocromos b/genética , Peces/anatomía & histología , Peces/fisiología , Regulación Enzimológica de la Expresión Génica , Repeticiones de Microsatélite , Océano Pacífico , Especificidad de la EspecieRESUMEN
Calibration of the molecular rate is one of the major challenges in marine population genetics. Although the use of an appropriate evolutionary rate is crucial in exploring population histories, calibration of the rate is always difficult because fossil records and geological events are rarely applicable for rate calibration. The acceleration of the evolutionary rate for recent coalescent events (or more simply, the time dependency of the molecular clock) is also a problem that can lead to overestimation of population parameters. Calibration of demographic transition (CDT) is a rate calibration technique that assumes a post-glacial demographic expansion, representing one of the most promising approaches for dealing with these potential problems in the rate calibration. Here, we demonstrate the importance of using an appropriate evolutionary rate, and the power of CDT, by using populations of the sandy beach amphipod Haustorioides japonicus along the Japanese coast of the northwestern Pacific Ocean. Analysis of mitochondrial sequences found that the most peripheral population in the Pacific coast of northeastern Honshu Island (Tohoku region) is genetically distinct from the other northwestern Pacific populations. By using the two-epoch demographic model and rate of temperature change, the evolutionary rate was modeled as a log-normal distribution with a median rate of 2.2%/My. The split-time of the Tohoku population was subsequently estimated to be during the previous interglacial period by using the rate distribution, which enables us to infer potential causes of the divergence between local populations along the continuous Pacific coast of Japan.
Asunto(s)
Crustáceos/genética , Evolución Molecular , Fósiles , Genética de Población/métodos , Algoritmos , Animales , Biodiversidad , Biomasa , Calibración , Crustáceos/fisiología , ADN Mitocondrial/genética , Genética de Población/normasRESUMEN
Many coastal barnacles are introduced to non-native regions. However, data are lacking on cryptic invasion, which is defined as an invasion that remains unrecognised because the invader is mistaken for a native or previously introduced species or clade. In this work, cryptic invasions of an intertidal barnacle, Semibalanus cariosus, between Japan and the north-eastern Pacific were evaluated based on population genetic analyses. A significant genetic differentiation was found between the Japanese and north-eastern Pacific populations, suggesting a limited introduction of non-native genotypes between these regions. Haplotype frequencies did not differ significantly between the past (museum samples collected in 1971 from Hokkaido, Japan) and present Japanese populations, implying the rare occurrence of human-mediated migration from the north-eastern Pacific to Japan. Migrate-n analysis revealed a low level of directional gene flow in S. cariosus from the north-eastern Pacific to Japan, possibly by natural stepping-stone dispersal via directional water currents or human-mediated transport.
Asunto(s)
Especies Introducidas , Thoracica/crecimiento & desarrollo , Thoracica/genética , Animales , Haplotipos , Japón , Océano Pacífico , Filogenia , Movimientos del AguaRESUMEN
Recent studies have revealed the impact of the drastic climate change during the last glacial period on coastal marine and anadromous species in the marginal seas of the northwestern Pacific Ocean; however, its influence on deep-sea species remains poorly understood. To compare the effects of the last glacial period on populations from the Sea of Japan and the Sea of Okhotsk, we examined the mitochondrial control region and cytochrome b gene sequences of Lycodes matsubarai, a deepsea demersal fish that inhabits these two seas. Our results showed clear genetic differentiation of populations between the two seas. The populations may have diverged during the last glacial period, probably as a result of vicariance due to the drastic sea level change. The population in the Sea of Okhotsk was larger than that in the Sea of Japan, but suddenly decreased after the last glacial period. However, the Sea of Japan population expanded after the last glacial period, coincident with high levels of oxygenation in deep-sea areas. These results elucidate regional-scale impacts of climate change on deep-sea organisms.