SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers.
Gaia Crippa1, Erika Griesshaber2, Antonio G Checa3
1Università degli Studi di Milano, Dipartimento di Scienze della Terra 'A. Desio', via Mangiagalli 34, Milano 20133, Italy.
Data in Brief
|December 9, 2020
Summary
This study details the microstructural and crystallographic orientation patterns in modern Glycymeris shells. The findings offer a reference for detecting diagenetic alteration in fossils and understanding bivalve shell formation.
Area of Science:
- Geology
- Paleontology
- Materials Science
Background:
- Bivalve shells exhibit complex microstructures crucial for their mechanical properties and fossil record.
- Understanding aragonite crystallite orientation in modern shells provides a baseline for paleoenvironmental studies.
Purpose of the Study:
- To present detailed data on the microstructure and texture of aragonite crystallites in various layers of modern Glycymeris shells.
- To analyze crystallite orientation patterns and their transitions between shell layers.
- To establish a reference dataset for Glycymeris shells to aid in the interpretation of fossil analogs.
Main Methods:
- Scanning Electron Microscopy (SEM) for microstructural identification.
- Electron Backscatter Diffraction (EBSD) for crystallographic texture analysis.
- Laser confocal microscopy and Field Emission SEM (FE-SEM) for detailed imaging and organic matrix visualization.
Main Results:
- Comprehensive dataset on aragonite crystallite orientation in crossed-lamellar, fibrous prismatic, and myostracal shell layers.
- Characterization of texture at layer transitions, highlighting similarities and differences.
- Visualization of organic matrix distribution within the outer crossed-lamellar layer.
Conclusions:
- The provided data serve as a modern reference for assessing diagenetic alteration in fossil Glycymeris shells.
- This research enhances comprehension of the mechanisms underlying bivalve shell biomineralization and structural development.
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