{"refrec":{"BRefID":215788,"RR":"<b>Røy, H.; Kallmeyer, J.; Adhikari, R.R.; Pockalny, R.A.; Jørgensen, B.B.; D'Hondt, S.</b> (2012). Aerobic microbial respiration in 86-million-year-old deep-sea red clay. <i>Science (Wash.) 336(6083)</i>: 922-925. <a href=\"http://dx.doi.org/10.1126/science.1219424\" target=\"_blank\">http://dx.doi.org/10.1126/science.1219424</a>","BEntID":207544,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 336(6083)</i>: 922-925. <a href=\"https://dx.doi.org/10.1126/science.1219424\" target=\"_blank\">https://dx.doi.org/10.1126/science.1219424</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Røy, H.; Kallmeyer, J.; Adhikari, R.R.; Pockalny, R.A.; Jørgensen, B.B.; D'Hondt, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Røy, H. <i>et al.</i>","Englishabstract":"Microbial communities can subsist at depth in marine sediments without fresh supply of organic matter for millions of years. At threshold sedimentation rates of 1 millimeter per 1000 years, the low rates of microbial community metabolism in the North Pacific Gyre allow sediments to remain oxygenated tens of meters below the sea floor. We found that the oxygen respiration rates dropped from 10 micromoles of O-2 liter(-1) year(-1) near the sediment-water interface to 0.001 micromoles of O-2 liter(-1) year(-1) at 30-meter depth within 86 million-year-old sediment. The cell-specific respiration rate decreased with depth but stabilized at around 10(-3) femtomoles of O-2 cell(-1) day(-1) 10 meters below the seafloor. 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