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

We 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.

Authors

Institutions

Publication Details

Journal
Crystal Growth & Design
Published
2025-05-06
DOI
https://doi.org/10.1021/acs.cgd.4c01531
Citations
1
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
4.33

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

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

Lennart de Nooijer, Wolfgang W. Schmahl, Julie Meilland, Jeraldine Lastam et al.
1 citations
Crystal Growth & Design
Paleontology and Stratigraphy of Fossils
4.33
article

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

Lennart de Nooijer, Wolfgang W. Schmahl, Julie Meilland, Jeraldine Lastam, Lurdes Fernández-Dı́az, Michal Kučera, Erika Griesshaber, Xiaofei Yin, Anna Sancho Vaquer
article en
1 citations

Abstract

We 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.

Crystal Growth & DesignVol. 25(10)
Universidad Complutense de Madrid (ES), Forschungszentrum Jülich (DE), University of Bremen (DE), Bruker (United States) (US), LMU Klinikum (DE), Royal Netherlands Institute for Sea Research (NL), Applied Nano Surfaces (Sweden) (SE), Marine Research Centre (MV), Advanced Materials and Devices (United States) (US), Instituto de Geociencias (ES), Ludwig-Maximilians-Universität München (DE)
Ministerio de Ciencia, Innovación y Universidades, Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 9%
Paleontology and Stratigraphy of Fossils
4.33
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.