EGU2020-21996
https://doi.org/10.5194/egusphere-egu2020-21996
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Nanostructure of biogenic aragonite: a study of otoliths and bivalve shells from a freshwater environment

Zsombor Molnár1, Péter Pekker2, Miklós Jakab3, István Dódony1, Zoltán Vitál4, and Mihály Pósfai1,2
Zsombor Molnár et al.
  • 1University of Pannonia, Department of Earth and Environmental Sciences, 8200 Veszprém, Egyetem st. 10 Hungary (molnarzs1994@gmail.com)
  • 2Research Institute of Biomolecular and Chemical Engineering, Nanolab, 8200 Veszprém, Egyetem st. 10 Hungary
  • 3University of Pannonia, Institute of Material Engineering, 8200 Veszprém, Egyetem st. 10 Hungary
  • 4Balaton Limnological Institute, Fish and Conservation Research Group, 8237 Tihany, Klebelsberg Kunó st. 3.

There are numerous similarities between the otolith (an acellular calcium carbonate aggregate in the inner ears of fishes) and the shells of freshwater bivalves. Since both grow during a lifetime of the individuals, and show small increments or growth zones (in daily or subdaily periods), they are excellent time-keepers. By this capability they provide information about both the life history of the individuals and the geochemical evolution of their environments (Schulz-Mirbach et al., 2018; Cerrato, 2000). Changes of major and trace elements between the different growth zones have been studied thoroughly, but structural features, particularly those of otoliths, are not well known. We used scanning and scanning transmission electron microscopy (SEM and STEM) to study oriented ion-milled sections of an otolith and samples of Dreissena shells from Lake Balaton, a large, shallow lake in Hungary. SEM observations confirm that the growth zones within the otolith are built up of small increments, and they have a radially asymmetric appearance, whereas STEM images show that the small increments are terminated by tiny holes. Selected-area electron diffraction (SAED) patterns and HRTEM images show that the aragonite material of both samples is highly defective, with dense arrays of planar defects occurring in distinct areas, and grains joining along low-angle boundaries (around 1°). In addition, areas with multiple (double and triple) periodicities along the [110]* directions occur in both samples. Based on these preliminary observations, nanostructural features could provide important details about the growth of biogenic aragonite and the structural properties of distinct growth zones.



Cerrato R. M. (2000): What fish biologist should know about bivalve shells, Fisheries Research, 46, 39-49.

Schulz-Mirbach T., Ladich F., Plath M., Heß M. (2018): Enimgatic ear stones: what we know about the functional role and evolution of the fish otoliths, Biological Reviews, 94 (2), 457-482.

Acknowledgments: The research was supported by the ÚNKP-19-3 new national excellence program of the ministry for innovation and technology. 

How to cite: Molnár, Z., Pekker, P., Jakab, M., Dódony, I., Vitál, Z., and Pósfai, M.: Nanostructure of biogenic aragonite: a study of otoliths and bivalve shells from a freshwater environment, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21996, https://doi.org/10.5194/egusphere-egu2020-21996, 2020

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