Department of Marine Ecosystems Dynamics, Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba, Japan.
Division of Marine Science and Conservation, Nicholas School of the Environment, Duke University, Beaufort, North Carolina, United States of America.
PLoS One. 2020 Sep 29;15(9):e0239784. doi: 10.1371/journal.pone.0239784. eCollection 2020.
The Southwest Pacific represents an independent biogeographic province for deep-sea hydrothermal vent fauna. Different degrees of genetic connectivity among vent fields in Manus, North Fiji and Lau Basins have been reported for various molluscan and crustacean species, presumably reflecting their different levels of dispersal ability as swimming larvae. The present study investigates the population connectivity of the hydrothermal vent limpet Shinkailepas tollmanni (family Phenacolepadidae) in the Southwest Pacific. Our analyses using mitochondrial COI-gene sequences and shell morphometric traits suggest a panmictic population structure throughout its geographic and bathymetric ranges, spanning 4,000 km from the westernmost Manus Basin (151ºE; 1,300 m deep) to the easternmost Lau Basin (176ºE; 2,720 m). The measurements of its embryonic and larval shells demonstrate that the species hatches as a planktotrophic veliger larva with an embryonic shell diameter of 170-180 μm and settles at the vent environment with the larval shell diameter of 750-770 μm. This substantial growth as a feeding larva, ca. 80 times in volume, is comparable or even greater than those of confamilial species in the hydrothermal-vent and methane-seep environments in the Northwest Pacific and Atlantic Oceans. Large pigmented eyes in newly settled juveniles are another common feature in this and other phenacolepadids inhabiting the chemosynthetic environments. These results put together suggest that the larvae of S. tollmanni migrate vertically from deep-sea vents to surface waters to take advantages of richer food supplies and faster currents and stay pelagic for an extended period of time (> 1 year), as previously indicated for the confamilial species.
西南太平洋是深海热液喷口动物的一个独立生物地理区。已报道曼努斯、北斐济和劳盆地的各个软体动物和甲壳动物物种的喷口场之间存在不同程度的遗传连通性,这可能反映了它们作为游泳幼虫的不同扩散能力水平。本研究调查了西南太平洋深海热液喷口帽贝 Shinkailepas tollmanni(Phenacolepadidae 科)的种群连通性。我们使用线粒体 COI 基因序列和壳形态特征分析的结果表明,在其地理和水深范围内存在泛种群结构,从最西端的曼努斯盆地(151°E;1300 米深)到最东端的劳盆地(176°E;2720 米深),跨越了 4000 公里。其胚胎和幼虫壳的测量表明,该物种以浮游幼虫的形式孵化,胚胎壳直径为 170-180 μm,在喷口环境中定居时幼虫壳直径为 750-770 μm。这种作为摄食幼虫的大量生长,体积约增加 80 倍,与西北太平洋和大西洋热液喷口和甲烷渗漏环境中的近缘种相当,甚至更大。新定居的幼体中较大的色素化眼睛是栖息在化学合成环境中的这种帽贝和其他 Phenacolepadidae 的另一个共同特征。这些结果表明,S. tollmanni 的幼虫垂直从深海喷口迁移到海面,以利用更丰富的食物供应和更快的海流,并在浮游期停留更长时间(>1 年),正如之前对近缘种的研究所示。