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SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers
Here, we provide the dataset associated with the research article “Orientation patterns of aragonitic crossed-lamellar, fibrous prismatic and myostracal microstructures of modern Glycymeris shells” [1]. Based on several tools (SEM, EBSD, laser confocal microscopy and FE-SEM) we present original data...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Elsevier
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7701352/ https://www.ncbi.nlm.nih.gov/pubmed/33294532 http://dx.doi.org/10.1016/j.dib.2020.106547 |
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author | Crippa, Gaia Griesshaber, Erika Checa, Antonio G. Harper, Elizabeth M. Simonet Roda, Maria Schmahl, Wolfgang W. |
author_facet | Crippa, Gaia Griesshaber, Erika Checa, Antonio G. Harper, Elizabeth M. Simonet Roda, Maria Schmahl, Wolfgang W. |
author_sort | Crippa, Gaia |
collection | PubMed |
description | Here, we provide the dataset associated with the research article “Orientation patterns of aragonitic crossed-lamellar, fibrous prismatic and myostracal microstructures of modern Glycymeris 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 Glycymeris 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 Glycymeris reference to detect diagenetic alteration in fossil analogs used for paleoenvironmental reconstructions, are useful to better comprehend the mechanisms of bivalve shell formation. |
format | Online Article Text |
id | pubmed-7701352 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Elsevier |
record_format | MEDLINE/PubMed |
spelling | pubmed-77013522020-12-07 SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers Crippa, Gaia Griesshaber, Erika Checa, Antonio G. Harper, Elizabeth M. Simonet Roda, Maria Schmahl, Wolfgang W. Data Brief Data Article Here, we provide the dataset associated with the research article “Orientation patterns of aragonitic crossed-lamellar, fibrous prismatic and myostracal microstructures of modern Glycymeris 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 Glycymeris 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 Glycymeris reference to detect diagenetic alteration in fossil analogs used for paleoenvironmental reconstructions, are useful to better comprehend the mechanisms of bivalve shell formation. Elsevier 2020-11-19 /pmc/articles/PMC7701352/ /pubmed/33294532 http://dx.doi.org/10.1016/j.dib.2020.106547 Text en © 2020 The Authors http://creativecommons.org/licenses/by-nc-nd/4.0/ This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). |
spellingShingle | Data Article Crippa, Gaia Griesshaber, Erika Checa, Antonio G. Harper, Elizabeth M. Simonet Roda, Maria Schmahl, Wolfgang W. SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title | SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title_full | SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title_fullStr | SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title_full_unstemmed | SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title_short | SEM, EBSD, laser confocal microscopy and FE-SEM data from modern Glycymeris shell layers |
title_sort | sem, ebsd, laser confocal microscopy and fe-sem data from modern glycymeris shell layers |
topic | Data Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7701352/ https://www.ncbi.nlm.nih.gov/pubmed/33294532 http://dx.doi.org/10.1016/j.dib.2020.106547 |
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