{"refrec":{"BRefID":437447,"RR":"<b>Sancho Vaquer, A.; Griesshaber, E.; Meilland, J.; Fernández-Díaz, L.; Yin, X.; Lastam, J.; de Nooijer, L.J.; Kucera, M.; Schmahl, W.W.</b> (2025). Microstructure and texture of foraminiferal Ca-Carbonate: The different biomineralization strategies of Rotaliida, Robertinida, and Miliolida. <i>Crystal Growth & Design 25(10)</i>: 3274-3297. <a href=\"https://dx.doi.org/10.1021/acs.cgd.4c01531\" target=\"_blank\">https://dx.doi.org/10.1021/acs.cgd.4c01531</a>","BEntID":435278,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Crystal Growth & Design 25(10)</i>: 3274-3297. <a href=\"https://dx.doi.org/10.1021/acs.cgd.4c01531\" target=\"_blank\">https://dx.doi.org/10.1021/acs.cgd.4c01531</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Sancho Vaquer, A.; Griesshaber, E.; Meilland, J.; Fernández-Díaz, L.; Yin, X.; Lastam, J.; de Nooijer, L.J.; Kucera, M.; Schmahl, W.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Sancho Vaquer, A. <i>et al.</i>","Englishabstract":"<span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">We report differences for shell calcite and aragonite crystallography and crystal organization for </span><i>Neogloboquadrina dutertrei</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> (Rotaliida), </span><i>Hoeglundina elegans</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> (Robertinida), </span><i>Pyrgo murrhina</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">, </span><i>Triloculina</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> sp., and </span><i>Quinqueloculina</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> sp. (Miliolida). Crystals were investigated with electron backscatter diffraction (EBSD) and high-resolution field-emission SEM (FE-SEM) imaging. Rotaliid and robertinid crystals have dendritic-fractal morphologies, interdigitate strongly, and are twinned. First-formed </span><i>N. dutertrei</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> calcite crystallites are fibrils. Arrays of these form bundles and evolve into densely mineralized crystal entities. First-formed </span><i>H. elegans</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> aragonite crystallites are granules. These nucleate onto a membranous template and evolve into laths and undulated laminae. The latter are stacked in parallel and generate round-shaped crystal units. </span><i>H. elegans</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> aragonite and </span><i>N. dutertrei</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> calcite have an axial-crystal-texture at nucleation onto the template. For </span><i>H. elegans</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">, the latter is maintained for the entire shell. For </span><i>N. dutertrei</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">, the axial-crystal-texture transforms to a single-crystal-texture toward distal shell surface. For </span><i>N. dutertrei</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">, the change in crystal texture is controlled by the crystal growth process and growth competition. Crystal growth controlled by growth competition is not observed for </span><i>H. elegans</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\"> aragonite or miliolid calcite. Miliolid calcite is not twinned. It is a meshwork of nanometer-sized single-crystal rods, interspersed by nanometer-sized single-crystal rhombohedra. At the proximal shell surface, the rods do not have preferred orientation. At the distal shell surface, the calcite is rather granular, co-oriented, and textured. For all investigated species, calcite/aragonite </span><i>c</i><span style=\"background-color:rgb(255,255,255);color:rgb(21,21,21);\">-axis rotates with shell curvature. Despite distinct foraminiferal shell crystallographic-structural differences, we find similarity for crystal nucleation. Nonetheless, for the investigated species, crystal growth is modulated by different growth determinants.</span>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Microstructure and texture of foraminiferal Ca-Carbonate: The different biomineralization strategies of Rotaliida, Robertinida, and Miliolida","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-02-09 01:32:45.714484","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Calcite; Crystal structure; Crystallization; Crystallography; Crystals","OtherDescriptors":null,"Notes":null,"AnaPub":2025,"MonPub":null,"DateUpdate":"2026-02-02","DateCreate":"2026-02-02","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1021/acs.cgd.4c01531"},"refs":null,"anarec":{"AnaID":437447,"PubliDate":2025,"Pagination":"3274-3297","XtraPublOfAnaID":null,"ISBN":null,"Volume":"25","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":266531,"SerRR":"Crystal Growth & Design. 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