{"refrec":{"BRefID":107793,"RR":"<b>Gattuso, J.P.; Pichon, M.; Frankignoulle, M.</b> (1995). Biological control of air-sea CO<sub>2</sub> fluxes: effect of photosynthetic and calcifying marine organisms and ecosystems. <i>Mar. Ecol. Prog. Ser. 129(1-3)</i>: 307-312. <a href=\"https://dx.doi.org/10.3354/meps129307\" target=\"_blank\">https://dx.doi.org/10.3354/meps129307</a>","BEntID":102608,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Mar. Ecol. Prog. Ser. 129(1-3)</i>: 307-312. <a href=\"https://dx.doi.org/10.3354/meps129307\" target=\"_blank\">https://dx.doi.org/10.3354/meps129307</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gattuso, J.P.; Pichon, M.; Frankignoulle, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gattuso, J.P.; Pichon, M.; Frankignoulle, M.","Englishabstract":"A simple expression enables prediction of the effect of photosynthetic and calcifying systems on air-sea CO<sub>2</sub> exchange at all spatial scales (from organism to ecosystem). Input data are: gross primary production (P<sub>g</sub>), respiration (R), net calcification (G) and the ratio of CO<sub>2</sub> released to CaCO<sub>3</sub> precipitated ( psi ); the output is the amount of dissolved inorganic carbon (F<sub>CO2</sub> which needs to be exchanged with the atmosphere to balance biologically mediated changes in the concentration of dissolved inorganic carbon in an open sea water system: F<sub>CO2</sub> = -P<sub>g</sub> + R + psi G. Coral reef data were used in the model to illustrate the relative influence of organic and inorganic carbon metabolism on ocean-atmosphere CO<sub>2</sub> cycling. A coral reef comprised of calcareous and non-calcareous organisms can be shown to act as a sink for atmospheric CO<sub>2</sub> when excess (= net) production is high and CaCO<sub>3</sub>  precipitation is low. These characteristics are not typical of actively developing reef systems which typically exhibit a nearly balanced organic carbon metabolism (P<sub>g</sub>/R similar to 1) and relatively high rates of calcification. In these circumstances, reef communities can be expected to cause CO<sub>2</sub> evasion to the atmosphere. This prediction is confirmed by the only existing measurement of air-sea CO<sub>2</sub> flux in a coral reef system.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Biological control of air-sea CO<sub>2</sub> fluxes: effect of photosynthetic and calcifying marine organisms and ecosystems","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-22 01:31:35.117948","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1995,"MonPub":null,"DateUpdate":"2014-08-12","DateCreate":"2007-02-19","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1995TP66400030","VABBcode":null,"OpenAcc":1,"DOI":"10.3354/meps129307"},"refs":null,"anarec":{"AnaID":107793,"PubliDate":1995,"Pagination":"307-312","XtraPublOfAnaID":null,"ISBN":null,"Volume":"129","Issue":"1-3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43354,"SerRR":"Marine Ecology Progress Series. 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