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

IF 3.2 2区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
Anna Sancho Vaquer*, Erika Griesshaber, Julie Meilland, Lurdes Fernández-Díaz, Xiaofei Yin, Jeraldine Lastam, Lennart de Nooijer, Michal Kucera and Wolfgang W. Schmahl, 
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引用次数: 0

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.

有孔虫Ca-Carbonate的微观结构和结构:Rotaliida, Robertinida和mililiida的不同生物矿化策略
我们报道了Neogloboquadrina dutertrei (Rotaliida)、Hoeglundina elegans (Robertinida)、Pyrgo murrhina、Triloculina sp.和Quinqueloculina sp. (milolida)的壳方解石和文石晶体学和晶体组织的差异。利用电子背散射衍射(EBSD)和高分辨率场发射扫描电镜(FE-SEM)对晶体进行了研究。Rotaliid和robertinid晶体具有枝状分形形态,具有强烈的指间性和孪晶。最初形成的方解石为原纤维。这些排列形成束,并演变成密集矿化的晶体实体。最初形成的秀丽隐杆线虫文石结晶为颗粒状。它们成核形成膜状模板,并演化成条状和波状层状。后者平行堆叠,形成圆形晶体单元。秀丽隐杆文石和杜特雷方解石在模板上成核时具有轴向晶体结构。对于秀丽隐杆线虫来说,后者是在整个外壳中维持的。对于白豆,轴晶纹理向远端壳表面转变为单晶纹理。对于N. duterte来说,晶体结构的变化受晶体生长过程和生长竞争的控制。在秀丽隐杆线虫文石或千粒方解石中没有观察到受生长竞争控制的晶体生长。千粒方解石不是孪生的。它是由纳米尺寸的单晶棒组成的网状结构,由纳米尺寸的单晶菱形体点缀。在近端壳表面,杆没有优选取向。在远端壳表面,方解石呈颗粒状,共取向,有织构。对于所有被调查的物种,方解石/文石的c轴随壳曲率旋转。尽管有孔虫壳的晶体结构有明显的差异,但我们发现晶体成核是相似的。尽管如此,对于所研究的物种,晶体生长是由不同的生长决定因素调节的。
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来源期刊
Crystal Growth & Design
Crystal Growth & Design 化学-材料科学:综合
CiteScore
6.30
自引率
10.50%
发文量
650
审稿时长
1.9 months
期刊介绍: The aim of Crystal Growth & Design is to stimulate crossfertilization of knowledge among scientists and engineers working in the fields of crystal growth, crystal engineering, and the industrial application of crystalline materials. Crystal Growth & Design publishes theoretical and experimental studies of the physical, chemical, and biological phenomena and processes related to the design, growth, and application of crystalline materials. Synergistic approaches originating from different disciplines and technologies and integrating the fields of crystal growth, crystal engineering, intermolecular interactions, and industrial application are encouraged.
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