{"refrec":{"BRefID":291266,"RR":"<b>Sulu-Gambari, F; Hagens, M.; Behrends, T; Seitaj, D.; Meysman, F.J.R.; Middelburg, J.; Slomp, C.P.</b> (2018). Phosphorus cycling and burial in sediments of a seasonally hypoxic marine basin. <i>Est. Coast. 41(4)</i>: 921–939. <a href=\"https://dx.doi.org/10.1007/s12237-017-0324-0\" target=\"_blank\">https://dx.doi.org/10.1007/s12237-017-0324-0</a>","BEntID":283309,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Est. Coast. 41(4)</i>: 921–939. <a href=\"https://dx.doi.org/10.1007/s12237-017-0324-0\" target=\"_blank\">https://dx.doi.org/10.1007/s12237-017-0324-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Sulu-Gambari, F; Hagens, M.; Behrends, T; Seitaj, D.; Meysman, F.J.R.; Middelburg, J.; Slomp, C.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Sulu-Gambari, F <i>et al.</i>","Englishabstract":"Recycling of phosphorus (P) from sediments contributes to the development of bottom-water hypoxia in many coastal systems. Here, we present results of a year-long assessment of P dynamics in sediments of a seasonally hypoxic coastal marine basin (Lake Grevelingen, the Netherlands) in 2012. Sequential phosphorus extractions (SEDEX) and X-ray absorption spectroscopy (XAS) indicate that P was adsorbed to Fe-(III)-(oxyhydr)oxides when cable bacteria were active in the surface sediments in spring. With the onset of summer hypoxia, sulphide-induced dissolution of the Fe-(III)-(oxyhydr)oxides led to P release to the pore water and overlying water. The similarity in authigenic Ca-P concentrations in the sediment and suspended matter suggest that Ca-P is not formed in situ. The P burial efficiency was ≤ 32%. Hypoxia-driven sedimentary P recycling had a major impact on the water-column chemistry in the basin in 2012. Water-column monitoring data indicate up to ninefold higher surface water concentrations of phosphate in the basin in the late 1970s and a stronger hypoxia-driven seasonal P release from the sediment. The amplified release of P from the sediment in the past is attributed to the presence of a larger pool of Fe-bound P in the basin prior to the first onset of hypoxia. Given that P is not limiting, primary production in the basin has not been affected by the decadal changes in P availability and recycling over the past 40 years. The changes in P dynamics on decadal time scales were ","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Phosphorus cycling and burial in sediments of a seasonally hypoxic marine basin","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":"Phosphorus; Recycling; Burial efficiency; Benthic flux; Cable bacteria ","OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2018-06-27","DateCreate":"2017-12-05","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000430990300001","VABBcode":null,"OpenAcc":1,"DOI":"10.1007/s12237-017-0324-0"},"refs":null,"anarec":{"AnaID":291266,"PubliDate":2018,"Pagination":"921–939","XtraPublOfAnaID":null,"ISBN":null,"Volume":"41","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":101945,"SerRR":"Estuaries and Coasts. 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