Аннотация
The Araripe Sedimentary Basin is known by the excellence of its fossils,
regarding the preservation, diversity, and quantity. Here, we present a
spectroscopic analysis using several experimental techniques (X-ray
energy dispersion spectroscopy, Fourier-transform infrared spectroscopy)
as well as X-ray diffraction and thermogravimetric analysis applied in
small fragments of bones from the posterior members of a theropod
dinosaur. The results agree regarding the different composition of the
stone matrix and the fossilized bone, indicating a partial substitution
of the material by elements present in the depositional environment.
However, differently from what is believed to occur, there is evidence
that pyritization is not the only mechanism of fossilization for a
specimen of Ipubi formation, but calcification, additionally, plays an
important role in the fossil production of this Formation.
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