FN Archimer Export Format PT J TI Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments BT AF D'HONDT, Steven INAGAKI, Fumio ZARIKIAN, Carlos Alvarez ABRAMS, Lewis J. DUBOIS, Nathalie ENGELHARDT, Tim EVANS, Helen FERDELMAN, Timothy GRIBSHOLT, Britta HARRIS, Robert N. HOPPIE, Bryce W. HYUN, Jung-Ho KALLMEYER, Jens KIM, Jinwook LYNCH, Jill E. MCKINLEY, Claire C. MITSUNOBU, Satoshi MORONO, Yuki MURRAY, Richard W. POCKALNY, Robert SAUVAGE, Justine SHIMONO, Takaya SHIRAISHI, Fumito SMITH, David C. SMITH-DUQUE, Christopher E. SPIVACK, Arthur J. STEINSBU, Bjorn Olav SUZUKI, Yohey SZPAK, Michal TOFFIN, Laurent URAMOTO, Goichiro YAMAGUCHI, Yasuhiko T. ZHANG, Guo-liang ZHANG, Xiao-Hua ZIEBIS, Wiebke AS 1:1,2;2:1,3;3:1,4;4:5;5:1,6;6:1,7;7:1,4;8:1,8;9:1,9;10:1,10;11:1,11;12:1,12;13:1,13;14:1,14;15:1,15;16:16;17:1,17;18:1,3;19:1,18;20:2;21:2;22:1,19;23:1,20;24:1,2;25:1,21;26:1,2;27:1,22;28:1,23;29:1,24;30:1,25;31:1,3;32:1,23;33:1,26;34:1,27;35:1,28; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:PDG-REM-EEP-LMEE;31:;32:;33:;34:;35:; C1 Integrated Ocean Drilling Program Expedit 329 Shi, Tokyo, Japan. Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA. Japan Agcy Marine Earth Sci & Technol, Kochi Inst Core Sample Res, Nankoku, Kochi 7838502, Japan. Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA. Univ N Carolina, Ctr Marine Sci, Wilmington, NC 28409 USA. Swiss Fed Inst Aquat Sci & Technol, CH-8600 Dubendorf, Switzerland. Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Meeres, D-26129 Oldenburg, Germany. 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Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1130033, Japan. Dublin City Univ, Sch Chem Sci, Dublin 9, Ireland. Inst Francais Rech Exploitat Mer, Ctr Bretagne, F-29280 Plouzane, France. Chinese Acad Sci, South China Sea Inst Oceanol, Qingdao 266071, Peoples R China. Ocean Univ China, Coll Marine Life Sci, Qingdao 266003, Peoples R China. Univ So Calif, Dept Biol Sci, Los Angeles, CA 90089 USA. C2 IODP, JAPAN UNIV RHODE ISL, USA JAMSTEC, JAPAN UNIV TEXAS A&M, USA UNIV N CAROLINA, USA EAWAG, SWITZERLAND UNIV OLDENBURG, GERMANY MAX PLANCK INST MARINE, GERMANY UNIV AARHUS, DENMARK UNIV OREGON STATE, USA UNIV MINNESOTA, USA UNIV HANYANG, SOUTH KOREA GFZ GERMAN RES CTR GEOSCI, GERMANY UNIV YONSEI, SOUTH KOREA UNIV MELBOURNE, AUSTRALIA UNIV TEXAS A&M, USA UNIV SHIZUOKA, JAPAN UNIV BOSTON, USA UNIV TSUKUBA, JAPAN UNIV HIROSHIMA, JAPAN NOC, UK UNIV BERGEN, NORWAY UNIV TOKYO, JAPAN UNIV DUBLIN CITY, IRELAND IFREMER, FRANCE CHINESE ACAD SCI, CHINA UNIV OCEAN CHINA, CHINA UNIV CALIF LOS ANGELES, USA SI AUTRE BREST SE AUTRE PDG-REM-EEP-LMEE UM BEEP-LM2E IN WOS Ifremer jusqu'en 2018 copubli-europe copubli-int-hors-europe copubli-sud IF 12.508 TC 163 UR https://archimer.ifremer.fr/doc/00255/36658/35265.pdf LA English DT Article AB The depth of oxygen penetration into marine sediments differs considerably from one region to another. In areas with high rates of microbial respiration, O2 penetrates only millimetres to centimetres into the sediments, but active anaerobic microbial communities are present in sediments hundreds of metres or more below the sea floor. In areas with low sedimentary respiration, O2 penetrates much deeper but the depth to which microbial communities persist was previously unknown. The sediments underlying the South Pacific Gyre exhibit extremely low areal rates of respiration. Here we show that, in this region, microbial cells and aerobic respiration persist through the entire sediment sequence to depths of at least 75 metres below sea floor. Based on the Redfield stoichiometry of dissolved O2 and nitrate, we suggest that net aerobic respiration in these sediments is coupled to oxidation of marine organic matter. We identify a relationship of O2 penetration depth to sedimentation rate and sediment thickness. Extrapolating this relationship, we suggest that oxygen and aerobic communities may occur throughout the entire sediment sequence in 15–44% of the Pacific and 9–37% of the global sea floor. Subduction of the sediment and basalt from these regions is a source of oxidized material to the mantle. PY 2015 PD APR SO Nature Geoscience SN 1752-0894 PU Nature Publishing Group VL 8 IS 4 UT 000352082300021 BP 299 EP 304 DI 10.1038/NGEO2387 ID 36658 ER EF