{"refrec":{"BRefID":77834,"RR":"<b>Andersson, J.H.; Wijsman, J.W.M.; Herman, P.M.J.; Middelburg, J.J.; Soetaert, K.; Heip, C.H.R.</b> (2004). Respiration patterns in the deep ocean. <i>Geophys. Res. Lett. 31(3)</i>: L03304 (1-4). <a href=\"https://dx.doi.org/10.1029/2003GL018756\" target=\"_blank\">https://dx.doi.org/10.1029/2003GL018756</a>","BEntID":73371,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 31(3)</i>: L03304 (1-4). <a href=\"https://dx.doi.org/10.1029/2003GL018756\" target=\"_blank\">https://dx.doi.org/10.1029/2003GL018756</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Andersson, J.H.; Wijsman, J.W.M.; Herman, P.M.J.; Middelburg, J.J.; Soetaert, K.; Heip, C.H.R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Andersson, J.H. <i>et al.</i>","Englishabstract":"The biological pump affects atmospheric CO<sub>2</sub> levels and fuels most heterotrophic activity in the deep ocean. The efficiency of this pump depends on the rate of carbon fixation, export out of the euphotic zone and the depth of respiration. Here we study the depth dependence of respiration patterns, hence particulate carbon flux, using a compiled data set of sediment oxygen consumption rates. We show that the depth relationship can best be described by a double exponential model. 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