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The evolution of thecideide microstructures and textures: traced from Triassic to Holocene

Simonet Roda, Maria and Griesshaber, Erika and Angiolini, Lucia and Harper, David A.T. and Jansen, Ulrich and Bitner, Maria Aleksandra and Henkel, Daniela and Manzanero, Eloy and Müller, Tamás and Tomašových, Adam and Eisenhauer, Anton and Ziegler, Andreas and Schmahl, Wolfgang W. (2021) 'The evolution of thecideide microstructures and textures: traced from Triassic to Holocene.', Lethaia. .

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.

Item Type:Article
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Available under License - Creative Commons Attribution Non-commercial No Derivatives 4.0.
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Status:Peer-reviewed
Publisher Web site:https://doi.org/10.1111/let.12422
Publisher statement:© 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
Date accepted:22 January 2021
Date deposited:07 April 2021
Date of first online publication:03 April 2021
Date first made open access:07 April 2021

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