{"refrec":{"BRefID":368685,"RR":"<b>Dämmer, L.K.; Ivkic, A.; de Nooijer, L.; Renema, W.; Webb, A.E.; Reichart, G.-J.</b> (2023). Impact of dissolved CO2 on calcification in two large, benthic foraminiferal species. <i>PLoS One 18(8)</i>: e0289122. <a href=\"https://dx.doi.org/10.1371/journal.pone.0289122\" target=\"_blank\">https://dx.doi.org/10.1371/journal.pone.0289122</a>","BEntID":366411,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>PLoS One 18(8)</i>: e0289122. <a href=\"https://dx.doi.org/10.1371/journal.pone.0289122\" target=\"_blank\">https://dx.doi.org/10.1371/journal.pone.0289122</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dämmer, L.K.; Ivkic, A.; de Nooijer, L.; Renema, W.; Webb, A.E.; Reichart, G.-J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Dämmer, L.K. <i>et al.</i>","Englishabstract":"Rising atmospheric CO <sub>2</sub> shifts the marine  inorganic carbonate    system and decreases seawater pH, a process often  abbreviated to ‘ocean    acidification’. Since acidification decreases the  saturation state for    crystalline calcium carbonate (e.g., calcite and  aragonite), rising    dissolved CO <sub>2</sub> levels will either increase  the energy demand for    calcification or reduce the total amount of CaCO <sub>3</sub> precipitated.    Here we report growth of two large benthic photosymbiont-bearing    foraminifera, <i>Heterostegina depressa</i> and    <i>        Amphistegina  lessonii    </i>    , cultured at four different ocean acidification scenarios (400,  700, 1000    and 2200 ppm atmospheric <i>p</i>CO<sub>2</sub>). Using the  alkalinity    anomaly technique, we calculated the amount of calcium carbonate    precipitated during the incubation and found that both species produced the    most carbonate at intermediate CO <sub>2</sub> levels. The chamber addition    rates for each of the conditions were also determined and matched the    changes  in alkalinity. These results were complemented by micro-CT scanning    of selected  specimens to visualize the effect of CO <sub>2</sub> on growth.    The  increased chamber addition rates at elevated CO <sub>2</sub>    concentrations  suggest that both foraminifera species can take advantage of    the increased  availability of the inorganic carbon, despite a lower    saturation state. This  adds to the growing number of reports showing the    variable response of  foraminifera to elevated CO <sub>2</sub>    concentrations, which is likely a  consequence of differences in    calcification mechanisms.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Impact of dissolved CO2 on calcification in two large, benthic foraminiferal species","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":2023,"MonPub":null,"DateUpdate":"2023-11-15","DateCreate":"2023-11-15","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:001051734600022","VABBcode":null,"OpenAcc":1,"DOI":"10.1371/journal.pone.0289122"},"refs":null,"anarec":{"AnaID":368685,"PubliDate":2023,"Pagination":"e0289122","XtraPublOfAnaID":null,"ISBN":null,"Volume":"18","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123954,"SerRR":"PLoS One. 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