{"refrec":{"BRefID":207166,"RR":"<b>Cai, W.-J.</b> (2011). Estuarine and coastal ocean carbon paradox: CO<sub>2</sub> sinks or sites of terrestrial carbon incineration?, <b><i>in</i></b>: Carlson, C.A. <i>et al.</i> <i>Ann. Rev. Mar. Sci. 3. Annual Review of Marine Science,</i> 3: pp. 123-145. <a href=\"https://dx.doi.org/10.1146/annurev-marine-120709-142723\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-120709-142723</a>","BEntID":199225,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Carlson, C.A. <i>et al.</i> <i>Ann. Rev. Mar. Sci. 3. Annual Review of Marine Science,</i> 3: pp. 123-145. <a href=\"https://dx.doi.org/10.1146/annurev-marine-120709-142723\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-120709-142723</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cai, W.-J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cai, W.-J.","Englishabstract":"Estuaries are a major boundary in the land-ocean interaction zone where organic carbon (OC) and nutrients are being processed, resulting in a high water-to-air carbon dioxide (CO<sub>2</sub>) flux (∼0.25 Pg C y<sup>−1</sup>). The continental shelves, however, take up CO<sub>2</sub> (∼0.25 Pg C y<sup>−1</sup>) from the atmosphere, accounting for approximately 17% of open ocean CO<sub>2</sub> uptake (1.5 Pg C y<sup>−1</sup>). It is demonstrated here that CO<sub>2</sub> release in estuaries is largely supported by microbial decomposition of highly productive intertidal marsh biomass. It appears that riverine OC, however, would bypass the estuarine zone, because of short river-transit times, and contribute to carbon cycling in the ocean margins and interiors. Low-latitude ocean margins release CO<sub>2</sub> because they receive two-thirds of the terrestrial OC. Because of recent CO<sub>2</sub> increase in the atmosphere, CO<sub>2</sub> releases from low latitudes have become weaker and CO<sub>2</sub> uptake by mid- and high-latitude shelves has become stronger, thus leading to more dissolved inorganic carbon export to the ocean.","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Estuarine and coastal ocean carbon paradox: CO<sub>2</sub> sinks or sites of terrestrial carbon incineration?","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"air-sea CO2 exchange; carbon flux; dissolved inorganic carbon dynamics; estuary; salt marsh; continental shelf","OtherDescriptors":null,"Notes":null,"AnaPub":2011,"MonPub":null,"DateUpdate":"2022-03-23","DateCreate":"2011-08-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000286638700005","VABBcode":null,"OpenAcc":0,"DOI":"10.1146/annurev-marine-120709-142723"},"refs":null,"anarec":{"AnaID":207166,"PubliDate":2011,"Pagination":"123-145","XtraPublOfAnaID":null,"ISBN":"978-0-8243-4503-7","Volume":"3","Issue":null,"BRefMon":350592,"BRefMonRR":"<b>Carlson, C.A.; Giovannoni, S.J.</b> (2011). 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