Vol. 34 No. 1 (2012): Boletín de Geología
Articles

¿FOSSIL BONE OR SIMPLE ROCK? SPECTROSCOPY FTIR AND CRITERIATO FOSSILIZED BONE STRUCTURES IDENTIFICATION

Javier H. Jerez-Jaimes
Universidad Industrial de Santander
Bio
Silvia Elizabeth García-Gómez
Universidad Industrial de Santander
Bio
Luis Enrique Cruz-Guevara
Universidad Industrial de Santander
Bio

Published 2012-08-24

How to Cite

Jerez-Jaimes, J. H., García-Gómez, S. E., & Cruz-Guevara, L. E. (2012). ¿FOSSIL BONE OR SIMPLE ROCK? SPECTROSCOPY FTIR AND CRITERIATO FOSSILIZED BONE STRUCTURES IDENTIFICATION. Boletín De Geología, 34(1). Retrieved from https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/2717

Abstract

Fossil record of marine vertebrates is very important to the reconstruction of systematic phylogenies,evolutionary and ecological studies, for this reason, any taphonomic element must be analyzed with quick and simple technical before it is discarded. In this study, was evaluated the biological origin of a similar structure to the vertebrae with Infrared spectroscopy analysis FTIR. The structure was collected in the Paja Formation(Cretaceous: Aptian) of the municipality of La Mesa de los Santos (Santander, Colombia). Samples of the outerlayer and the filling matrix were extracted using a microdrill. Along cow´s bone (Bos taurus) was used as a control sample to determine the spectrum of calcium phosphate. FTIR spectra allowed identification of differences inthe composition of the outer layer and the internal structure of the specimen. A response was found in the absorption ranges to calcium phosphate in the outer layer. The internal layer showed a greater composition ofcalcium carbonate. The FTIR technique allowed the recognition of calcium phosphate in this taphonomic entity.Current paleontological criteria determine that the morphology and the spectra IR not support the recognition of this element like fossil ossified structure due to the absence of the characteristic microstructure.

Keywords: Aptian, Marine Reptile, Pseudofossil, Paja Formation.

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