{"refrec":{"BRefID":209766,"RR":"<b>Laruelle, G. G.; Roubeix, V.; Sferratore, A.; Brodherr, B.; Ciuffa, D.; Conley, D. J.; Dürr, H. H.; Garnier, J.; Lancelot, C.; Le Thi Phuong, Q.; Meunier, J.-D.; Meybeck, M.; Michalopoulos, P.; Moriceau, B.; Longphuirt, S. Ni.; Loucaides, S.; Papush, L.; Presti, M.; Ragueneau, O.; Regnier, P.; Saccone, L.; Slomp, C. P.; Spiteri, C.; Van Cappellen, P.</b> (2009). Anthropogenic perturbations of the silicon cycle at the global scale: Key role of the land-ocean transition. <i>Global Biogeochem. Cycles 23(GB4031)</i>: 17 pp. <a href=\"http://dx.doi.org/10.1029/2008GB003267\" target=\"_blank\">dx.doi.org/10.1029/2008GB003267</a>","BEntID":201738,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Global Biogeochem. Cycles 23(GB4031)</i>: 17 pp. <a href=\"https://dx.doi.org/10.1029/2008GB003267\" target=\"_blank\">https://dx.doi.org/10.1029/2008GB003267</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Laruelle, G. G.; Roubeix, V.; Sferratore, A.; Brodherr, B.; Ciuffa, D.; Conley, D. J.; Dürr, H. H.; Garnier, J.; Lancelot, C.; Le Thi Phuong, Q.; Meunier, J.-D.; Meybeck, M.; Michalopoulos, P.; Moriceau, B.; Longphuirt, S. Ni.; Loucaides, S.; Papush, L.; Presti, M.; Ragueneau, O.; Regnier, P.; Saccone, L.; Slomp, C. P.; Spiteri, C.; Van Cappellen, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Laruelle, G. G. <i>et al.</i>","Englishabstract":"Silicon (Si), in the form of dissolved silicate (DSi), is a key nutrient in marine and continental ecosystems. DSi is taken up by organisms to produce structural elements (e.g., shells and phytoliths) composed of amorphous biogenic silica (bSiO<sub>2</sub>). A global mass balance model of the biologically active part of the modern Si cycle is derived on the basis of a systematic review of existing data regarding terrestrial and oceanic production fluxes, reservoir sizes, and residence times for DSi and bSiO<sub>2</sub>. The model demonstrates the high sensitivity of biogeochemical Si cycling in the coastal zone to anthropogenic pressures, such as river damming and global temperature rise. As a result, further significant changes in the production and recycling of bSiO<sub>2</sub> in the coastal zone are to be expected over the course of this century.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Anthropogenic perturbations of the silicon cycle at the global scale: Key role of the land-ocean transition","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:01.897972","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2014-11-06","DateCreate":"2011-11-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000273255500001","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2008GB003267"},"refs":null,"anarec":{"AnaID":209766,"PubliDate":2009,"Pagination":"17 pp.","XtraPublOfAnaID":null,"ISBN":null,"Volume":"23","Issue":"GB4031","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45841,"SerRR":"Global Biogeochemical Cycles. 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