Abstract

Hydrothermal vents are chemosynthetically driven ecosystems and one of the most extreme environments on Earth. Vent communities exhibit remarkable taxonomic novelty at the species and supra-species levels, and over 80% of vent species are endemic. Here, we used mitochondrial DNA to identify the biogeographic distribution of Munidopsis lauensis and the heme-binding regions of A1-type COX1 from six species (including M. lauensis) to investigate whether genetic variation in the protein structure affects oxygen-binding ability. We verified the identity of Indian Ocean specimens by comparing sequences from the barcoding gene mitochondrial cytochrome oxidase subunit 1 (COI) with known M. lauensis sequences from the NCBI database. The data show that these are the first recorded specimens of M. lauensis in the Indian Ocean; previously, this species had been reported only in the southwest Pacific. Our findings support the hypothesis that vent fauna in the Pacific and Indian Oceans can interact via active ridges. In the case of the mitochondrial DNA-binding site, the arrangement of heme-binding ligands and type A1 motif of M. lauensis was identical to that in other species. Moreover, our findings suggest that the mechanism of oxygen binding is well conserved among species from terrestrial organisms to hydrothermal extremophiles. Overall, dispersal of the same species to geologically separated hydrothermal vents and conserved heme-binding regions in mitochondrial proteins suggest that hydrothermal species might have evolved from shallow sea organisms and became distributed geographically using a dispersion corridor.

Highlights

  • Driven hydrothermal vents are among the harshest ecosystems on the planet, having temperatures as high as 390 ◦C, low oxygen levels, and enriched concentrations of hydrogen sulfide (H2S), methane (CH4), and heavy metals, including iron, zinc, and copper [1]

  • We investigated the biogeographic distribution of Munidopsis lauensis and tested a hypothesis that the Indian Ocean is a dispersal corridor connecting the hydrothermal vent fauna of the Atlantic and Pacific Oceans

  • On 1 July 2019, eighteen samples of M. lauensis were collected at the Onnuri Vent Field (OVF; latitude: 11◦14 58.6 S; longitude: 66◦15 14.4 E) in the Indian Ocean using a TeleVision-grab (TV-grab) device mounted on the Research Vessel (R/V) ISABU

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Summary

Introduction

Driven hydrothermal vents are among the harshest ecosystems on the planet, having temperatures as high as 390 ◦C, low oxygen levels, and enriched concentrations of hydrogen sulfide (H2S), methane (CH4), and heavy metals, including iron, zinc, and copper [1]. This unique environment makes vent species susceptible to geological settings and local ecosystems because they produce chemical-rich fluids that support the food web, generating a patchwork seafloor habitat. Hydrothermal vents are found at mid-ocean spreading centers in the Atlantic, Arctic, Indian, and eastern Pacific Oceans, and back-arc basins of the western Pacific Ocean [4]. Numerous vent communities have been reported along active margins in the Atlantic [5,6], Pacific [7,8], and Indian Oceans [9,10]

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