Abstract
The preservation of fossils depends on several interactions of organic
and inorganic chemical processes. The hard parts, which are more
suitable for fossilization, might record valuable information of
hiogenic processes, while the taphonomic characteristics supply
information on postmortem chemical transformation. Here, X-ray
fluorescence, X-ray diffraction, and infrared spectroscopy analyses were
carried out in Early Eoholocene fragments of bones collected from the
subsurface at Gruta do Urso Fossil, Ubajara National Park, northeast of
Ceara State in Brazil. It is suggested a lower degree of decomposition,
a preservation of the original mineral composition, along with some
incidence of encrustation, and the occurrence of different animal
species are analyzed. These preliminary data serve as a basis for future
studies involving fossil biota from the deposits of Grata do Urso Fossil
using spectroscopic techniques.
Users
Please
log in to take part in the discussion (add own reviews or comments).