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Discovery of the southwest Dongsha Island mud volcanoes amid the northern margin of the South China Sea
Institution:1. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, Faculty of Resources, China University of Geosciences (CUG), Wuhan, Hubei 430074, PR China;2. Department of Marine Science and Engineering, Faculty of Resources, China University of Geosciences (CUG), Wuhan, Hubei 430074, PR China;3. MARUM — Center for Marine Environmental Sciences, University of Bremen, 28359, Bremen, Germany;4. Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, Guangdong 510301, PR China;5. Ghent University, Department of Geology and Soil Science, Renard Centre of Marine Geology, Krijgslaan 281 s8, B-9000 Ghent, Belgium;1. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;2. University of Chinese Academy of Sciences, Beijing 100049, China;3. School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK;4. MARUM, Center for Marine Environmental Sciences, University of Bremen, Bremen 28359, Germany;5. CNOOC, Research Institute, Beijing 100027, China
Abstract:The Dongsha Basin, circling Dongsha Island that is amid the northern margin of the South China Sea, is characterized by thin (~0.5 km) Cenozoic sediments veneering on thick (up to 5 km) Mesozoic strata. Recently, several geophysical and geological surveys, including multiple channel reflection seismic, sub-bottom profiling and benthic dredging, have been conducted on the slope southwest to the Dongsha Island, where the water depth varies from 400 m to 2000 m. A novel discovery is numerous submarine mud volcanoes of various sizes over there, typically 50–200 m high and 0.5–5 km wide. Geophysical profiles document their unusual features, e.g., roughly undulating seafloor, high-amplitude seabed reflectivity, foggy hyperbolic diffractions up to 50 m in water column above seabed, and internal reflection chaos and wipe-out down to 2–3 km level or deeper below the seabed. Benthic dredging from the mud volcanoes gives abundant faunas of high diversity, e.g., scleractinian (stony coral), gorgonian, black coral, thiophil tubeworm, glass sponge, bryozoan etc., indicating booming chemosynthetic community, among which the Lophelia pertusa-like coral and the Euretidae-like glass sponges are the first reports in the South China Sea. Concomitantly with them, there are also abundant authigenic carbonate nodules and slabs, raw, brecciated and breccias with bio-clasts congregation. Besides, there coexist massive mudflows and allogenic coarse-grained quartz, feldspar and tourmaline most likely brought out by mud volcanism. Geochemical analysis of the bottom water samples give dissolved methane concentration up to 4 times higher than the background average. These results lend comprehensive evidences for the ongoing and historical mud volcanism. The escaping methane gas is inferred to source mainly from the Mesozoic strata. Occupying a large province of the deep water slope, ca. 1000 km2 or more, the mud volcanoes is prospective for gas hydrate and natural gas for the Dongsha Basin.
Keywords:SW Dongsha Island mud volcanoes  The northern margin of the South China Sea  Geophysical image  Authigenic carbonate  Chemosynthetic community  Active methane seepage  Mesozoic Erathem  Gas prospect
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