4.7 Article

Mercury proxy for hydrothermal and submarine volcanic activities in the sediment cores of Central Indian Ridge

Journal

MARINE POLLUTION BULLETIN
Volume 159, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.marpolbul.2020.111513

Keywords

Mercury speciation; Hydrothermal proxy; Submarine volcano; Mid-Ocean ridge; Central Indian Ocean

Funding

  1. Ministry of Oceans and Fisheries, Korea [20170411]
  2. National Research Foundation of Korea (NRF) - Ministry of Science and ICT of Korean government [2019R1F1A1059106]
  3. National Research Foundation of Korea [2019R1F1A1059106] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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Hydrothermal vent is the one of the main natural Hg sources to the deep ocean. Thus, we investigated which Hg speciation in the sediment core can be the past records for geothermal activities in mid-ocean ridges of the Central Indian Ocean. The result showed that the hydrothermal Hg in the core sediments was mainly associated with Fe-Mn oxides with the elevated concentrations of other hydrothermal-derived trace metals [Co + Zn + Cu]. In addition, the [Sm]/[Nd] and [Rb]/[Sr] ratios and eNdCHUR and Sr-87/Sr-86 isotopic values supported that the extremely high Hg concentrations were possibly originated from the hydrothermal vent. However, the Hg emitted from submarine volcano was mainly associated with sulfides-organic matters because the volcanos did not release Fe and Mn. Thus, our results showed that the sedimentary Hg is an independent toll for reconstruction of paleodynamics of hydrothermal and/or volcanic activities in deep sea basin of the Central Indian Ocean.

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