{"refrec":{"BRefID":223356,"RR":"<b>Smith, A.M.; Garden, C.J.</b> (2013). Being a bimineralic bryozoan in an acidifying ocean, <b><i>in</i></b>: Ernst, A. <i>et al.</i> <i>Bryozoan Studies 2010. Lecture Notes in Earth System Sciences,</i> 143: pp. 327-337. <a href=\"http://dx.doi.org/10.1007/978-3-642-16411-8_22\" target=\"_blank\">http://dx.doi.org/10.1007/978-3-642-16411-8_22</a>","BEntID":215080,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Ernst, A. <i>et al.</i> <i>Bryozoan Studies 2010. Lecture Notes in Earth System Sciences,</i> 143: pp. 327-337. <a href=\"http://dx.doi.org/10.1007/978-3-642-16411-8_22\" target=\"_blank\">http://dx.doi.org/10.1007/978-3-642-16411-8_22</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Smith, A.M.; Garden, C.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Smith, A.M.; Garden, C.J.","Englishabstract":"Strongly controlled calcification by bryozoans means that some species maintain complex skeletons formed of more than one mineral. Whether they are mainly intermediate-Mg calcitic with up to 50% aragonite, mainly aragonitic with small amounts of high-Mg calcite (&gt;8 wt.% MgCO<sub class=\"a-plus-plus\">3</sub>), or formed of both high- and low-Mg calcites, preservation of sediments formed of these bimineralic bryozoan skeletons may be more at risk from ocean acidification than the majority of bryozoan sediments formed of monomineralic skeletons. An acid-bath immersion experiment on seven species reveals that three (<em class=\"a-plus-plus\">Adeonella</em> sp., <em class=\"a-plus-plus\">Adeonella patagonica</em>, and <em class=\"a-plus-plus\">Adeonellopsis</em> sp.) are more resistant to dissolution than the other four. Skeletal carbonate mineralogy appears to influence dissolution history very little: the most soluble aragonite and high-Mg calcite species, <em class=\"a-plus-plus\">Adeonellopsis</em> sp., was more highly resistant to dissolution than species dominated by low-Mg calcite. In the context of ocean acidification, it is likely that bryozoan skeletons with high surface area and small delicate morphologies are at greatest risk of dissolution, irrespective of mineralogical composition.","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Being a bimineralic bryozoan in an acidifying ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:32:52.928458","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Experimental dissolution","OtherDescriptors":null,"Notes":null,"AnaPub":2013,"MonPub":null,"DateUpdate":"2013-03-06","DateCreate":"2013-03-06","SecASFANote":null,"ConfID":null,"PeerRev":null,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1007/978-3-642-16411-8_22"},"refs":null,"anarec":{"AnaID":223356,"PubliDate":2013,"Pagination":"327-337","XtraPublOfAnaID":null,"ISBN":"978-3-642-16410-1","Volume":"143","Issue":null,"BRefMon":222875,"BRefMonRR":"<b>Ernst, A.; Schäfer, P.; Scholz, J. (Ed.)</b> (2013). Bryozoan Studies 2010. <i>Lecture Notes in Earth System Sciences</i>, 143. Springer: Berlin. ISBN 978-3-642-16410-1. viii, 463 pp. <a href=\"https://dx.doi.org/10.1007/978-3-642-16411-8\" target=\"_blank\">https://dx.doi.org/10.1007/978-3-642-16411-8</a>","BRefXtra":null,"BRefXtraRR":null,"SerBRefID":222874,"SerRR":"Lecture Notes in Earth System Sciences. Springer: Heidelberg; Berlin.  ISSN 2193-8571; e-ISSN 2193-858X","StandardTitleSer":"Lecture Notes in Earth System Sciences","ISSN":"2193-8571","AbbrevSer":"Lect. notes earth syst. sci. (Print)","StandardTitleMon":"Bryozoan Studies 2010","StartPage":327,"Pages":11,"ToPubliDate":null,"BRefBibLvlCode":"MS","SerNotes":null,"AutString":"Ernst, A.; Schäfer, P.; Scholz, J. (Ed.)"},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Smith","Firstname":"Abigail","Initials":"A.M.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":215080,"AutID":43722,"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":"Garden","Firstname":"Christopher","Initials":"C.J.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":215080,"AutID":158882,"OrderNr":2,"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":null,"MONpubls":[{"PublName":"Springer","Place":"Berlin"}],"pictures":[],"thestermsPath":[{"ThesaurusTerm":"Acidification","ThestID":60,"Acronym":"ASFA","ThesTermPath":"Acidification"},{"ThesaurusTerm":"Aragonite","ThestID":527,"Acronym":"ASFA","ThesTermPath":"Minerals > Carbonate minerals > Aragonite"},{"ThesaurusTerm":"Calcite","ThestID":1273,"Acronym":"ASFA","ThesTermPath":"Minerals > Carbonate minerals > Calcite"},{"ThesaurusTerm":"Oceans","ThestID":5716,"Acronym":"ASFA","ThesTermPath":"Water bodies > Oceans"}],"thestermsASFA":[{"ThesaurusTerm":"Acidification"},{"ThesaurusTerm":"Aragonite"},{"ThesaurusTerm":"Calcite"},{"ThesaurusTerm":"Oceans"}],"taxtermsASFA":[{"TaxTerm":"Bryozoa"}],"geotermsASFA":null,"collections":null,"conf":null,"proj":null,"Physdatasets":null,"spcols":null,"doi":null,"publs":null,"serparttypes":null,"monauthors":[{"AutName":"Ernst","Initials":"A.","CorporateFlag":0,"BEntID":214601,"AutID":81180,"OrderNr":1,"DegrID":null,"EditorFlag":1,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"AutStrTrunc":"Ernst, A.; Schäfer, P.; Scholz, J. 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