Microstructure and Texture of Foraminiferal Ca-Carbonate: The Different Biomineralization Strategies of Rotaliida, Robertinida, and Miliolida

dc.contributor.authorSancho Vaquer, Anna
dc.contributor.authorGriesshaber, Erika
dc.contributor.authorMeilland, Julie
dc.contributor.authorFernández Díaz, María Lourdes
dc.contributor.authorYin, Xiaofei
dc.contributor.authorLastam, Jeraldine
dc.contributor.authorDe Nooijer, Lennart
dc.contributor.authorKucera, Michal
dc.contributor.authorSchmahl, Wolfgang W.
dc.date.accessioned2025-06-02T18:10:35Z
dc.date.available2025-06-02T18:10:35Z
dc.date.issued2025
dc.description.abstractWe report differences for shell calcite and aragonite crystallography and crystal organization for Neogloboquadrina dutertrei (Rotaliida), Hoeglundina elegans (Robertinida), Pyrgo murrhina, Triloculina sp., and Quinqueloculina 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 N. dutertrei calcite crystallites are fibrils. Arrays of these form bundles and evolve into densely mineralized crystal entities. First-formed H. elegans 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. H. elegans aragonite and N. dutertrei calcite have an axial-crystal-texture at nucleation onto the template. For H. elegans, the latter is maintained for the entire shell. For N. dutertrei, the axial-crystal-texture transforms to a single-crystal-texture toward distal shell surface. For N. dutertrei, 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 H. elegans 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 c-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.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipDeutsche Forschungsgemeinschaft
dc.description.sponsorshipMinisterio de Ciencia e Innovación (España)
dc.description.statuspub
dc.identifier.citationSancho Vaquer, A., Griesshaber, E., Meilland, J., Fernández-Díaz, L., Yin, X., Lastam, J., De Nooijer, L., Kucera, M., & Schmahl, W. W. (2025). Microstructure and texture of foraminiferal ca-carbonate: The different biomineralization strategies of rotaliida, robertinida, and miliolida. Crystal Growth & Design, 25(10), 3274-3297. https://doi.org/10.1021/acs.cgd.4c01531
dc.identifier.doi10.1021/acs.cgd.4c01531
dc.identifier.essn1528-7505
dc.identifier.issn1528-7483
dc.identifier.officialurlhttps://doi.org/10.1021/acs.cgd.4c01531
dc.identifier.relatedurlhttps://pubs.acs.org/doi/full/10.1021/acs.cgd.4c01531
dc.identifier.urihttps://hdl.handle.net/20.500.14352/120795
dc.issue.number10
dc.journal.titleCrystal Growth & Design
dc.language.isoeng
dc.page.final3297
dc.page.initial3274
dc.publisherAmerican Chemical Society
dc.relation.projectIDGR 9/1234, SCHM 930/11–2
dc.relation.projectIDEXC-2077, Project 390741603
dc.relation.projectIDPID2021–125467NB-I00
dc.rights.accessRightsrestricted access
dc.subject.cdu548
dc.subject.keywordCalcite
dc.subject.keywordCrystal structure
dc.subject.keywordCrystallization
dc.subject.keywordCrystallography Crystals
dc.subject.ucmMineralogía (Geología)
dc.subject.unesco2506.11 Mineralogía
dc.titleMicrostructure and Texture of Foraminiferal Ca-Carbonate: The Different Biomineralization Strategies of Rotaliida, Robertinida, and Miliolida
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number25
dspace.entity.typePublication
relation.isAuthorOfPublication5283531a-5de9-4e87-bcc7-1c218b2d3a89
relation.isAuthorOfPublication.latestForDiscovery5283531a-5de9-4e87-bcc7-1c218b2d3a89

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