Maria Simonet Roda
The evolution of thecideide microstructures and textures: traced from Triassic to Holocene
Simonet Roda, Maria; Griesshaber, Erika; Angiolini, Lucia; Harper, David A.T.; Jansen, Ulrich; Bitner, Maria Aleksandra; Henkel, Daniela; Manzanero, Eloy; Müller, Tamás; Tomašových, Adam; Eisenhauer, Anton; Ziegler, Andreas; Schmahl, Wolfgang W.
Authors
Erika Griesshaber
Lucia Angiolini
David Harper david.harper@durham.ac.uk
Emeritus Professor
Ulrich Jansen
Maria Aleksandra Bitner
Daniela Henkel
Eloy Manzanero
Tamás Müller
Adam Tomašových
Anton Eisenhauer
Andreas Ziegler
Wolfgang W. Schmahl
Abstract
Thecideide brachiopods are an anomalous group of invertebrates. In this study, we discuss the evolution of thecideide brachiopods from the Triassic to the Holocene and base our results and conclusions on microstructure and texture measurements gained from electron backscatter diffraction (EBSD). In fossil and Recent thecideide shells, we observe the following mineral units: (1) nanometric to small granules; (2) acicles; (3) fibres; (4) polygonal crystals; and (5) large roundish crystals. We trace for thecideide shells the change of mineral unit characteristics such as morphology, size, orientation, arrangement and distribution pattern. Triassic thecideide shells contain extensive sections formed of fibres interspersed with large, roundish crystals. Upper Cretaceous to Pleistocene thecideide hard tissues consist of a matrix of minute to small grains reinforced by acicles and small polygonal crystals. Recent thecideide species form their shell of mineral units that show a wide range of shapes, sizes and arrangements. We find from Late Triassic to Recent a gradual decrease in mineral unit size, regularity of mineral unit morphology and orientation and the degree of calcite co‐orientation. While crystallite co‐orientation is the highest for fibrous microstructures, it is strikingly low for taxa that form their shell out of nanogranular to acicular mineral units. Our results indicate that Upper Jurassic species represent transitional forms between ancient taxa with fibrous shells and Recent forms that construct their shells of acicles and granules. We attribute the observed changes in microstructure and texture to be an adaptation to a different habitat and lifestyle associated with cementation to hard substrates.
Citation
Simonet Roda, M., Griesshaber, E., Angiolini, L., Harper, D. A., Jansen, U., Bitner, M. A., Henkel, D., Manzanero, E., Müller, T., Tomašových, A., Eisenhauer, A., Ziegler, A., & Schmahl, W. W. (2021). The evolution of thecideide microstructures and textures: traced from Triassic to Holocene. Lethaia: An International Journal of Palaeontology and Stratigraphy, 54(4), 558-577. https://doi.org/10.1111/let.12422
Journal Article Type | Article |
---|---|
Acceptance Date | Jan 22, 2021 |
Online Publication Date | Apr 3, 2021 |
Publication Date | 2021-10 |
Deposit Date | Apr 3, 2021 |
Publicly Available Date | Apr 7, 2021 |
Journal | Lethaia |
Print ISSN | 0024-1164 |
Electronic ISSN | 1502-3931 |
Publisher | Scandinavian University Press |
Peer Reviewed | Peer Reviewed |
Volume | 54 |
Issue | 4 |
Pages | 558-577 |
DOI | https://doi.org/10.1111/let.12422 |
Public URL | https://durham-repository.worktribe.com/output/1244801 |
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http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
Early View © 2021 The Authors. Lethaia published by John Wiley & Sons Ltd on behalf of Lethaia Foundation
This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made
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