Nearest vent, dearest friend: biodiversity of Tiancheng vent field reveals cross-ridge similarities in the Indian Ocean

Author:

Sun Jin12ORCID,Zhou Yadong3,Chen Chong4ORCID,Kwan Yick Hang2ORCID,Sun Yanan2,Wang Xuyang5,Yang Lei6,Zhang Ruiyan3,Wei Tong2,Yang Yi2,Qu Lingyun1,Sun Chengjun1,Qian Pei-Yuan2

Affiliation:

1. Marine Bioresource and Environment Research Center, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, People's Republic of China

2. Department of Ocean Science, Division of Life Science and Hong Kong Branch of the Southern Marine Science and Engineering Guangdong Laboratory, The Hong Kong University of Science and Technology, Hong Kong, People's Republic of China

3. Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, People's Republic of China

4. X-STAR, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan

5. State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong University, Shanghai 200240, People's Republic of China

6. Marine Survey Research Center, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, People's Republic of China

Abstract

Biodiversity of hydrothermal vents in the Indian Ocean, particularly those on the Southwest Indian Ridge (SWIR), are still relatively poorly understood. The Tiancheng field on the SWIR was initially reported with only a low-temperature diffuse flow venting area, but here we report two new active areas, including a chimney emitting high-temperature vent fluids. Biological sampling in these new sites doubled the known megafauna and macrofauna richness reported from Tiancheng. Significantly, we found several iconic species, such as the scaly-foot snail and the first Alviniconcha population on the SWIR. Tiancheng shares a high proportion of taxa with vents on the Central Indian Ridge (CIR) and lacks a number of key taxa that characterize other vents investigated so far on the SWIR. Population genetics of the scaly-foot snail confirmed this, as the Tiancheng population was clustered with populations from the CIR, showing low connectivity with the Longqi field. Unlike the previously examined populations, scales of the Tiancheng scaly-foot snail were coated in zinc sulfide, although this results only from precipitation. The close connection between Tiancheng and CIR vents indicates that the dispersal barrier for vent endemic species is not the Rodriguez Triple Junction as previously suggested but the transformation faults between Tiancheng and Longqi, warranting further studies on deep currents in this area to resolve the key barrier, which has important implications for biological conservation.

Funder

China Ocean Mineral Resource R&D Association

Hong Kong Research Grants Council

Japan Society for the Promotion of Science Grant-in-Aid for Scientific Research

National Key Research and Development Program of China

Scientific Research Fund of the Second Institute of Oceanography

Hong Kong Branch of South Marine Science and Engineering Guangdong Laboratory

Publisher

The Royal Society

Subject

Multidisciplinary

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