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Earthquake-enhanced dissolved carbon cycles in ultra-deep ocean sediments.
Chu, Mengfan; Bao, Rui; Strasser, Michael; Ikehara, Ken; Everest, Jez; Maeda, Lena; Hochmuth, Katharina; Xu, Li; McNichol, Ann; Bellanova, Piero; Rasbury, Troy; Kölling, Martin; Riedinger, Natascha; Johnson, Joel; Luo, Min; März, Christian; Straub, Susanne; Jitsuno, Kana; Brunet, Morgane; Cai, Zhirong; Cattaneo, Antonio; Hsiung, Kanhsi; Ishizawa, Takashi; Itaki, Takuya; Kanamatsu, Toshiya; Keep, Myra; Kioka, Arata; McHugh, Cecilia; Micallef, Aaron; Pandey, Dhananjai; Proust, Jean Noël; Satoguchi, Yasufumi; Sawyer, Derek; Seibert, Chloé; Silver, Maxwell; Virtasalo, Joonas; Wang, Yonghong; Wu, Ting-Wei; Zellers, Sarah.
Afiliação
  • Chu M; Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100, China.
  • Bao R; Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100, China. baorui@ouc.edu.cn.
  • Strasser M; University of Innsbruck, Institute of Geology, Innsbruck, Austria.
  • Ikehara K; National Institute of Advanced Industrial Science and Technology (AIST), Geological Survey of Japan, Institute of Geology and Geoinformation, Ibaraki, 305-8567, Japan.
  • Everest J; British Geological Survey, Lyell Centre, Edinburgh, EH14 4AP, UK.
  • Maeda L; Center for Deep Earth Exploration, Japan Agency for Marine-Earth Science and Technology, Kanagawa, 236-0001, Japan.
  • Hochmuth K; School of Geography, Geology and the Environment, University of Leicester, Leicester, UK.
  • Xu L; Australian Centre for Excellence in Antarctic Sciences, Institute for Marine and Antarctic Studies, University of Tasmania, 20 Castray Esplanade, Battery Point TAS, Churchill Ave, 7004, Australia.
  • McNichol A; NOSAMS Laboratory, Woods Hole Oceanographic Institution, Massachusetts, USA.
  • Bellanova P; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Massachusetts, USA.
  • Rasbury T; RWTH Aachen University, Institute of Neotectonics and Natural Hazards & Institute of Geology and Geochemistry of Petroleum and Coal, 52056, Aachen, Germany.
  • Kölling M; Stony Brook University, Department of Geosciences, New York, 11794, USA.
  • Riedinger N; MARUM - Center for Marine Environmental Science, University of Bremen, Bremen, 28359, Germany.
  • Johnson J; Boone Pickens School of Geology, Oklahoma State University, Oklahoma, 74078, USA.
  • Luo M; University of New Hampshire, Department of Earth Sciences, New Hampshire, 03824, USA.
  • März C; Shanghai Engineering Research Center of Hadal Science and Technology, College of Marine Sciences, Shanghai Ocean University, Shanghai, China.
  • Straub S; School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK.
  • Jitsuno K; Institute for Geosciences, University of Bonn, Nussallee 8, 53115, Bonn, Germany.
  • Brunet M; Lamont Doherty Earth Observatory, Geochemistry Division, New York, 10964, USA.
  • Cai Z; Department of Life Science and Medical Bioscience, Waseda University, Tokyo, 162-0041, Japan.
  • Cattaneo A; Univ Rennes, CNRS, Géosciences Rennes, UMR 6118, 35000, Rennes, France.
  • Hsiung K; Kyoto University, Department of Geology and Mineralogy, Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto, 606-8502, Japan.
  • Ishizawa T; Geo-Ocean, UMR 6538, Univ Brest, CNRS, Ifremer, Plouzané, F-29280, France.
  • Itaki T; Research Institute for Marine Geodynamics, JAMSTEC, Marine Geology and Geophysics Research Group, Subduction Dynamics Research Center, Kanagawa, 237-0061, Japan.
  • Kanamatsu T; International Research Institute of Disaster Science, Tohoku University, Sendai, 980-0845, Japan.
  • Keep M; National Institute of Advanced Industrial Science and Technology (AIST), Geological Survey of Japan, Institute of Geology and Geoinformation, Ibaraki, 305-8567, Japan.
  • Kioka A; Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute of Marine Geodynamics (IMG), Yokosuka, 237-0061, Japan.
  • McHugh C; The University of Western Australia, Department School of Earth Sciences, Perth, Australia.
  • Micallef A; Kyushu University, Department of Earth Resources Engineering, Fukuoka, 819-0395, Japan.
  • Pandey D; Queens College, City University of New York, School of Earth and Environmental Sciences, New York, 11367, USA.
  • Proust JN; GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, D-24148, Germany.
  • Satoguchi Y; National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Government of India, Goa, 403 804, India.
  • Sawyer D; Univ Rennes, CNRS, Géosciences Rennes, UMR 6118, 35000, Rennes, France.
  • Seibert C; Lake Biwa Museum, Shiga, 525-0001, Japan.
  • Silver M; The Ohio State University, School of Earth Sciences, Ohio, 43210, USA.
  • Virtasalo J; Lamont Doherty Earth Observatory, Marine geology and geophysics division, New York, 10964, USA.
  • Wang Y; Colorado School of Mines, Hydrologic Science and Engineering, Colorado, 80227, USA.
  • Wu TW; Geological Survey of Finland (GTK), Espoo, 02151, Finland.
  • Zellers S; Ocean University of China, Department of Marine Geosciences, Qingdao, 266100, China.
Nat Commun ; 14(1): 5427, 2023 Sep 11.
Article em En | MEDLINE | ID: mdl-37696798
ABSTRACT
Hadal trenches are unique geological and ecological systems located along subduction zones. Earthquake-triggered turbidites act as efficient transport pathways of organic carbon (OC), yet remineralization and transformation of OC in these systems are not comprehensively understood. Here we measure concentrations and stable- and radiocarbon isotope signatures of dissolved organic and inorganic carbon (DOC, DIC) in the subsurface sediment interstitial water along the Japan Trench axis collected during the IODP Expedition 386. We find accumulation and aging of DOC and DIC in the subsurface sediments, which we interpret as enhanced production of labile dissolved carbon owing to earthquake-triggered turbidites, which supports intensive microbial methanogenesis in the trench sediments. The residual dissolved carbon accumulates in deep subsurface sediments and may continue to fuel the deep biosphere. Tectonic events can therefore enhance carbon accumulation and stimulate carbon transformation in plate convergent trench systems, which may accelerate carbon export into the subduction zones.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Nat Commun Ano de publicação: 2023 Tipo de documento: Article
Texto completo
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PubMed Links
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Nat Commun Ano de publicação: 2023 Tipo de documento: Article