Abstract.
290 Million years old petrifactions from the Lower Permian Rotliegend of Chemnitz were examined by analytical X-ray microscopy to determine their chemical composition. Mappings show the inhomogeneous distribution of the involved elements, which may reflect the former plant anatomy, as well as some contemporaneous processes of permineralization (with silica and fluorite) and agate-formation. Most prominent advantages of the analytical X-ray microscopy are the low preparation expense of the museum samples, the analysis scanning range and the X-ray spot diameter suitable with the dimension of the fossil plants.
Similar content being viewed by others
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Dietrich, D., Frosch, G., Rößler, R. et al. Analytical X-Ray Microscopy on Psaronius sp. – A Contribution to Permineralization Process Studies. Mikrochim Acta 133, 279–283 (2000). https://doi.org/10.1007/s006040070105
Issue Date:
DOI: https://doi.org/10.1007/s006040070105