Precambrian Ecosystem Laboratory (PEL), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Kanagawa, Japan.
PLoS One. 2012;7(3):e32965. doi: 10.1371/journal.pone.0032965. Epub 2012 Mar 14.
Indian Ocean hydrothermal vents are believed to represent a novel biogeographic province, and are host to many novel genera and families of animals, potentially indigenous to Indian Ocean hydrothermal systems. In particular, since its discovery in 2001, much attention has been paid to a so-called 'scaly-foot' gastropod because of its unique iron-sulfide-coated dermal sclerites and the chemosynthetic symbioses in its various tissues. Despite increasing interest in the faunal assemblages at Indian Ocean hydrothermal vents, only two hydrothermal vent fields have been investigated in the Indian Ocean. Here we report two newly discovered hydrothermal vent fields, the Dodo and Solitaire fields, which are located in the Central Indian Ridge (CIR) segments 16 and 15, respectively. Chemosynthetic faunal communities at the Dodo field are emaciated in size and composition. In contrast, at the Solitaire field, we observed faunal communities that potentially contained almost all genera found at CIR hydrothermal environments to date, and even identified previously unreported taxa. Moreover, a new morphotype of 'scaly-foot' gastropod has been found at the Solitaire field. The newly discovered 'scaly-foot' gastropod has similar morphological and anatomical features to the previously reported type that inhabits the Kairei field, and both types of 'scaly-foot' gastropods genetically belong to the same species according to analyses of their COI gene and nuclear SSU rRNA gene sequences. However, the new morphotype completely lacks an iron-sulfide coating on the sclerites, which had been believed to be a novel feature restricted to 'scaly-foot' gastropods. Our new findings at the two newly discovered hydrothermal vent sites provide important insights into the biodiversity and biogeography of vent-endemic ecosystems in the Indian Ocean.
印度洋热液喷口被认为代表了一个新的生物地理区系,是许多新型属和科动物的宿主,这些动物可能是印度洋热液系统的特有种。特别是自 2001 年发现以来,由于其独特的铁硫化物涂层真皮骨板以及其各种组织中的化能共生关系,一种所谓的“鳞足”腹足动物引起了广泛关注。尽管人们对印度洋热液喷口的动物群组合越来越感兴趣,但在印度洋只对两个热液喷口场进行了调查。在这里,我们报告了两个新发现的热液喷口场,即 Dodo 和 Solitaire 场,它们分别位于中央印度洋脊(CIR)的 16 和 15 段。Dodo 场的化能动物群落在大小和组成上都很瘦弱。相比之下,在 Solitaire 场,我们观察到的动物群落可能包含了迄今为止在 CIR 热液环境中发现的几乎所有属,甚至还发现了以前未报道的分类群。此外,在 Solitaire 场还发现了一种新的“鳞足”腹足动物形态型。新发现的“鳞足”腹足动物具有与先前报道的栖息在 Kairei 场的类型相似的形态和解剖特征,并且根据 COI 基因和核 SSU rRNA 基因序列分析,这两种类型的“鳞足”腹足动物在遗传上属于同一物种。然而,新形态型的骨板完全缺乏铁硫化物涂层,这曾被认为是“鳞足”腹足动物的一个独特特征。我们在这两个新发现的热液喷口地点的新发现为印度洋喷口特有生态系统的生物多样性和生物地理学提供了重要的见解。