Anna Sancho Vaquer*, Erika Griesshaber, Julie Meilland, Lurdes Fernández-Díaz, Xiaofei Yin, Jeraldine Lastam, Lennart de Nooijer, Michal Kucera and Wolfgang W. Schmahl,
{"title":"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","authors":"Anna Sancho Vaquer*, Erika Griesshaber, Julie Meilland, Lurdes Fernández-Díaz, Xiaofei Yin, Jeraldine Lastam, Lennart de Nooijer, Michal Kucera and Wolfgang W. Schmahl, ","doi":"10.1021/acs.cgd.4c0153110.1021/acs.cgd.4c01531","DOIUrl":null,"url":null,"abstract":"<p >We report differences for shell calcite and aragonite crystallography and crystal organization for <i>Neogloboquadrina dutertrei</i> (Rotaliida), <i>Hoeglundina elegans</i> (Robertinida), <i>Pyrgo murrhina</i>, <i>Triloculina</i> sp., and <i>Quinqueloculina</i> 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 <i>N. dutertrei</i> calcite crystallites are fibrils. Arrays of these form bundles and evolve into densely mineralized crystal entities. First-formed <i>H. elegans</i> 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. <i>H. elegans</i> aragonite and <i>N. dutertrei</i> calcite have an axial-crystal-texture at nucleation onto the template. For <i>H. elegans</i>, the latter is maintained for the entire shell. For <i>N. dutertrei</i>, the axial-crystal-texture transforms to a single-crystal-texture toward distal shell surface. For <i>N. dutertrei</i>, 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 <i>H. elegans</i> 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 <i>c</i>-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.</p>","PeriodicalId":34,"journal":{"name":"Crystal Growth & Design","volume":"25 10","pages":"3274–3297 3274–3297"},"PeriodicalIF":3.2000,"publicationDate":"2025-05-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Microstructure and Texture of Foraminiferal Ca-Carbonate: The Different Biomineralization Strategies of Rotaliida, Robertinida, and Miliolida\",\"authors\":\"Anna Sancho Vaquer*, Erika Griesshaber, Julie Meilland, Lurdes Fernández-Díaz, Xiaofei Yin, Jeraldine Lastam, Lennart de Nooijer, Michal Kucera and Wolfgang W. Schmahl, \",\"doi\":\"10.1021/acs.cgd.4c0153110.1021/acs.cgd.4c01531\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >We report differences for shell calcite and aragonite crystallography and crystal organization for <i>Neogloboquadrina dutertrei</i> (Rotaliida), <i>Hoeglundina elegans</i> (Robertinida), <i>Pyrgo murrhina</i>, <i>Triloculina</i> sp., and <i>Quinqueloculina</i> 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 <i>N. dutertrei</i> calcite crystallites are fibrils. Arrays of these form bundles and evolve into densely mineralized crystal entities. First-formed <i>H. elegans</i> 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. <i>H. elegans</i> aragonite and <i>N. dutertrei</i> calcite have an axial-crystal-texture at nucleation onto the template. For <i>H. elegans</i>, the latter is maintained for the entire shell. For <i>N. dutertrei</i>, the axial-crystal-texture transforms to a single-crystal-texture toward distal shell surface. For <i>N. dutertrei</i>, 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 <i>H. elegans</i> 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 <i>c</i>-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.</p>\",\"PeriodicalId\":34,\"journal\":{\"name\":\"Crystal Growth & Design\",\"volume\":\"25 10\",\"pages\":\"3274–3297 3274–3297\"},\"PeriodicalIF\":3.2000,\"publicationDate\":\"2025-05-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Crystal Growth & Design\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://pubs.acs.org/doi/10.1021/acs.cgd.4c01531\",\"RegionNum\":2,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"CHEMISTRY, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Crystal Growth & Design","FirstCategoryId":"92","ListUrlMain":"https://pubs.acs.org/doi/10.1021/acs.cgd.4c01531","RegionNum":2,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, MULTIDISCIPLINARY","Score":null,"Total":0}
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.
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.