Crippa Gaia, Griesshaber Erika, Checa Antonio G, Harper Elizabeth M, Simonet Roda Maria, Schmahl Wolfgang W
Università degli Studi di Milano, Dipartimento di Scienze della Terra 'A. Desio', via Mangiagalli 34, Milano 20133, Italy.
Department für Geo- und Umweltwissenschaften, Ludwig-Maximilians Universität München, Munich, Germany.
Data Brief. 2020 Nov 19;33:106547. doi: 10.1016/j.dib.2020.106547. eCollection 2020 Dec.
Here, we provide the dataset associated with the research article "Orientation patterns of aragonitic crossed-lamellar, fibrous prismatic and myostracal microstructures of modern shells" [1]. Based on several tools (SEM, EBSD, laser confocal microscopy and FE-SEM) we present original data relative to the microstructure and texture of aragonite crystallites in all shell layers (crossed-lamellar, complex crossed-lamellar, fibrous prismatic and pedal retractor and adductor myostraca) and address texture characteristics at the transition from one layer to the other, identifying similarities and differences among the different layers. Shells were cut transversely, obliquely and longitudinally in order to obtain different orientated sections of the outer and inner layer and of the myostraca. The identification of major microstructural elements was provided by detailed SEM and laser confocal microscopy images. Microstructure and texture characterization was based on EBSD measurements presented as band contrast images and as color-coded crystal orientation maps with corresponding pole figures. Crystal co-orientation was measured with the MUD value. Finally, the distribution of the organic matrix occluded within the outer crossed-lamellar layer was revealed using FE-SEM. These data, besides providing a modern unaltered reference to detect diagenetic alteration in fossil analogs used for paleoenvironmental reconstructions, are useful to better comprehend the mechanisms of bivalve shell formation.
在此,我们提供与研究论文《现代贝壳文石质交叉层状、纤维柱状和肌肉痕微结构的取向模式》[1]相关的数据集。基于多种工具(扫描电子显微镜、电子背散射衍射、激光共聚焦显微镜和场发射扫描电子显微镜),我们展示了与所有贝壳层(交叉层状、复杂交叉层状、纤维柱状以及足缩肌和闭壳肌肌肉痕)中霰石微晶的微观结构和织构相关的原始数据,并探讨了从一层到另一层过渡时的织构特征,识别不同层之间的异同。贝壳被横向、斜向和纵向切割,以获取外层、内层和肌肉痕不同取向的截面。主要微观结构元素的识别由详细的扫描电子显微镜和激光共聚焦显微镜图像提供。微观结构和织构表征基于电子背散射衍射测量结果,以带衬度图像以及带有相应极图的彩色编码晶体取向图呈现。晶体共取向用MUD值测量。最后,用场发射扫描电子显微镜揭示了外层交叉层状层中封闭的有机基质的分布。这些数据除了为检测用于古环境重建的化石类似物中的成岩蚀变提供一个未改变的现代参考外,还有助于更好地理解双壳类贝壳形成的机制。