{"refrec":{"BRefID":330802,"RR":"<b>Roepert, A.; Polerecky, L.; Geerken, E.; Reichart, G.-J.; Middelburg, J.</b> (2020). Distribution of chlorine and fluorine in benthic foraminifera. <i>Biogeosciences 17(18)</i>: 4727-4743. <a href=\"https://doi.org/10.5194/bg-17-4727-2020\" target=\"_blank\">https://doi.org/10.5194/bg-17-4727-2020</a>","BEntID":324412,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Biogeosciences 17(18)</i>: 4727-4743. <a href=\"https://doi.org/10.5194/bg-17-4727-2020\" target=\"_blank\">https://doi.org/10.5194/bg-17-4727-2020</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Roepert, A.; Polerecky, L.; Geerken, E.; Reichart, G.-J.; Middelburg, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Roepert, A. <i>et al.</i>","Englishabstract":"Over the last few decades, a suite of inorganic proxies based on    foraminiferal calcite have been developed, some of which are now widely    used for palaeoenvironmental reconstructions. Studies of foraminiferal    shell chemistry have largely focused on cations and oxyanions, while much    less is known about the incorporation of anions. The halogens fluoride and    chloride are conservative in the ocean, which makes them candidates for    reconstructing palaeoceanographic parameters. However, their potential as a    palaeoproxy has hardly been explored, and fundamental insight into their    incorporation is required. Here we used nanoscale secondary ion mass    spectrometry (NanoSIMS) to investigate, for the first time, the    distribution of Cl and F within shell walls of four benthic species offoraminifera. In the rotaliid species <i>Ammonia tepida</i> and    <i>Amphistegina lessonii</i>, Cl and F were distributed highly    heterogeneously within the shell walls, forming bands that were co-located    with the bands observed in the distribution of phosphorus (significant    positive correlation of both Cl and F with P; <i>p</i>&lt;0.01). In the    miliolid species <i>Sorites marginalis</i> and <i>Archaias angulatus</i>,    the distribution of Cl and F was much more homogeneous without discerniblebands. In these species, Cl and P were spatially positively correlated (    <i>p</i>&lt;0.01), whereas no correlation was observed between Cl and F or    between F and P. Additionally, their F content was about an order of    magnitude higher than in the rotaliid species. The high variance in the Cl    and F content in the studied foraminifera specimens could not be attributed    to environmental parameters. Based on these findings, we suggest that Cl    and F are predominately associated with organic linings in the rotaliid    species. We further propose that Cl may be incorporated as a solid solution    of chlorapatite or may be associated with organic molecules in the calcite    in the miliolid species. The high F content and the lack of a correlation    between Cl and F or P in the miliolid foraminifera suggest a fundamentally    different incorporation mechanism. Overall, our data clearly show that the    calcification pathway employed by the studied foraminifera governs the    incorporation and distribution of Cl, F, P, and other elements in their    calcite shells.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Distribution of chlorine and fluorine in benthic foraminifera","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-11-11","DateCreate":"2020-11-11","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000576666000001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/bg-17-4727-2020"},"refs":null,"anarec":{"AnaID":330802,"PubliDate":2020,"Pagination":"4727-4743","XtraPublOfAnaID":null,"ISBN":null,"Volume":"17","Issue":"18","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":68092,"SerRR":"<b>Gattuso, J.P.; Kesselmeier, J. (Ed.)</b> Biogeosciences. Copernicus Publications: Göttingen.  ISSN 1726-4170; e-ISSN 1726-4189","StandardTitleSer":"Biogeosciences","ISSN":"1726-4170","AbbrevSer":"Biogeosciences","StandardTitleMon":null,"StartPage":4727,"Pages":17,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Roepert","Firstname":"Anne","Initials":"A.","Affiliation":"Univ Utrecht, 3508 TA, Dept Earth Sci Geochem, Fac Geosci, POB 80-021, NL-3508 TA Utrecht, Netherlands.","Discriminator":null,"CorporateFlag":0,"BEntID":324412,"AutID":305505,"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":"Polerecky","Firstname":"Lubos","Initials":"L.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":324412,"AutID":416209,"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":"Geerken","Firstname":"Esmee","Initials":"E.","Affiliation":"OCS","Discriminator":null,"CorporateFlag":0,"BEntID":324412,"AutID":324698,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"OCS","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; 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