{"refrec":{"BRefID":98306,"RR":"<b>Andersen, T.; Andersen, F.Ø.; Pedersen, O.</b> (2006). Increased CO<sub>2</sub> in the water around <i>Littorella uniflora</i> raises the sediment O<sub>2</sub> concentration. <i>Aquat. Bot. 84(4)</i>: 294-300. <a href=\"http://dx.doi.org/10.1016/j.aquabot.2005.11.006\" target=\"_blank\">http://dx.doi.org/10.1016/j.aquabot.2005.11.006</a>","BEntID":93661,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Aquat. Bot. 84(4)</i>: 294-300. <a href=\"https://dx.doi.org/10.1016/j.aquabot.2005.11.006\" target=\"_blank\">https://dx.doi.org/10.1016/j.aquabot.2005.11.006</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Andersen, T.; Andersen, F.Ø.; Pedersen, O.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Andersen, T. <i>et al.</i>","Englishabstract":"n the present study, we set up laboratory experiments with the isoetid plant <i>Littorella uniflora</i> to test whether higher water column CO<sub>2</sub> concentrations affect (1) O<sub>2</sub> concentrations in leaves and sediment, and (2) nutrient dynamics in the porewater. The experiments showed that at 175&nbsp;&#x3bc;M CO<sub>2</sub> in the water column, which is 10-fold atmospheric equilibrium, a higher biomass of <i>L. uniflora</i> developed (from 302&nbsp;&#xb1;&nbsp;51 to 390&nbsp;&#xb1;&nbsp;86&nbsp;g&nbsp;dry&nbsp;wt&nbsp;m<sup>&#x2212;2</sup>) and there were higher O<sub>2</sub> concentrations in the leaves (from 120 up to 160% of air saturation) and in the porewater of the sediment (1.7-fold higher). The O<sub>2</sub> concentration in particular increased in the upper 10&#x2013;30&nbsp;mm of the sediment at the elevated CO<sub>2</sub> concentrations. The increase in biomass of <i>L. uniflora</i> mostly derived from a significant increase in the leaf biomass (from 97&nbsp;&#xb1;&nbsp;14 to 137&nbsp;&#xb1;&nbsp;21&nbsp;g&nbsp;DW&nbsp;m<sup>&#x2212;2</sup>), while root biomass at high CO<sub>2</sub> (253&nbsp;&#xb1;&nbsp;82&nbsp;g&nbsp;dry&nbsp;wt&nbsp;m<sup>&#x2212;2</sup>) was similar to that of plants growing at low CO<sub>2</sub> (205&nbsp;&#xb1;&nbsp;40&nbsp;g&nbsp;dry&nbsp;wt&nbsp;m<sup>&#x2212;2</sup>). This implied that the increase in O<sub>2</sub> concentration in the sediment was a result of increased O<sub>2</sub> production in the leaves rather than of increased root biomass. Porewater samples from three sediment depths (20, 70 and 120&nbsp;mm) showed reduced NO<sub>3</sub><sup>&#x2212;</sup> concentrations at high CO<sub>2</sub> concentration, especially at 20&nbsp;mm depth layer (mean values for low CO<sub>2</sub> ranged from 25 to 60&nbsp;&#x3bc;M while they were below 25&nbsp;&#x3bc;M at high CO<sub>2</sub>), presumably as a result of uptake by <i>L. uniflora</i>. NH<sub>4</sub><sup>+</sup> concentrations increased with depth (from nearly 0 up to 100&nbsp;&#x3bc;M) but were not significantly related to the CO<sub>2</sub> concentration. The PO<sub>4</sub><sup>3&#x2212;</sup> concentrations were low (less than 0.5&nbsp;&#x3bc;M) and similar at both low and high CO<sub>2</sub> treatments at all three depths. The study showed that photosynthesis of <i>L. uniflora</i> is limited by CO<sub>2</sub> at ambient concentrations and that higher CO<sub>2</sub> concentrations result in higher O<sub>2</sub> release to the sediment which is important for the cycling and retention of nutrients in sediments of oligotrophic softwater lakes.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Increased CO<sub>2</sub> in the water around <i>Littorella uniflora</i> raises the sediment O<sub>2</sub> concentration","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":"Littorella uniflora; softwater lakes; increasing atmospheric CO2;isoetids; oxygen; sediment","OtherDescriptors":null,"Notes":null,"AnaPub":2006,"MonPub":null,"DateUpdate":"2018-05-17","DateCreate":"2006-04-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000236617300003","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":98306,"PubliDate":2006,"Pagination":"294-300","XtraPublOfAnaID":null,"ISBN":null,"Volume":"84","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42195,"SerRR":"Aquatic Botany. Elsevier Science: Tokyo; Oxford; New York; London; Amsterdam.  ISSN 0304-3770; e-ISSN 1879-1522","StandardTitleSer":"Aquatic Botany","ISSN":"0304-3770","AbbrevSer":"Aquat. Bot.","StandardTitleMon":null,"StartPage":294,"Pages":7,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":{"Line1":"University of Southern Denmark","Email":"foa@biology.sdu.dk","Line2":null,"EnvName":"Denmark"},"othpubs":null,"ownerships":null,"authors":[{"AutName":"Andersen","Firstname":"Troels","Initials":"T.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":93661,"AutID":64929,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Andersen","Firstname":"Frede","Initials":"F.Ø.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":93661,"AutID":51518,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Pedersen","Firstname":"Ole","Initials":"O.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":93661,"AutID":55945,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":null,"litstyles":null,"thespers":null,"arch2discl":null,"SERpubls":[{"PublName":"Elsevier Science","City":"Tokyo; Oxford; New York; London; Amsterdam"}],"MONpubls":null,"pictures":[],"thestermsPath":[{"ThesaurusTerm":"Oxygen","ThestID":5926,"Acronym":"ASFA","ThesTermPath":"Chemical elements > Nonmetals > Atmospheric gases > Oxygen"},{"ThesaurusTerm":"Sediments","ThestID":7403,"Acronym":"ASFA","ThesTermPath":"Sediments"}],"thestermsASFA":[{"ThesaurusTerm":"Oxygen"},{"ThesaurusTerm":"Sediments"}],"taxtermsASFA":null,"geotermsASFA":null,"collections":null,"conf":null,"proj":null,"Physdatasets":null,"spcols":null,"doi":null,"publs":null,"serparttypes":null,"monauthors":null,"MParts":null,"SParts":null,"hLibs":null,"langs":[{"BEntID":93661,"AbstractFlag":-1,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"},{"BEntID":93661,"AbstractFlag":0,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"}],"urls":null,"thesterms":[{"ThesaurusTerm":"Oxygen","ThestID":5926,"Acronym":"ASFA","ThesTypID":1,"ThesType":"ASFA Thesaurus List"},{"ThesaurusTerm":"Sediments","ThestID":7403,"Acronym":"ASFA","ThesTypID":1,"ThesType":"ASFA Thesaurus List"}],"taxterms":null,"geoterms":null,"othterms":null,"asfacodes":null,"asfa2codes":null,"thestermsFRIS":[{"ThesaurusTerm":"Oxygen","DutchTerm":"Zuurstof","ThestID":5926,"Acronym":"ASFA","ThesTypID":1,"ThesType":"ASFA Thesaurus List"},{"ThesaurusTerm":"Sediments","DutchTerm":"Sedimenten","ThestID":7403,"Acronym":"ASFA","ThesTypID":1,"ThesType":"ASFA Thesaurus List"}],"taxtermsFRIS":null,"geotermsFRIS":null,"othtermsFRIS":null,"resmessage":"","complete":1,"sessions":{"newSesName":"Chisala, Chilekwa, C.","newSesDate":{"date":"2006-04-25 12:44:16.043000","timezone_type":3,"timezone":"Europe/Brussels"},"updSesName":"Lyssens, Liesbeth, L.","updSesDate":{"date":"2018-05-17 21:28:56.790000","timezone_type":3,"timezone":"Europe/Brussels"}}}
