Abstract
The Ipubi and Romualdo Formations are Cretaceous units of the Araripe
Basin (Santana Group). The first and most ancient was deposited in a
lake environment, and some fossils were preserved in shales deposited
under blackish conditions. The second was deposited in a marine
environment, preserving a rich paleontological content in calcareous
concretions. Considering that these two environments preserved their
fossils under different processes, in this work we investigated the
chemical composition of two fossilized specimens, one from each of the
studied stratigraphic units, and compared them using vibrational
spectroscopy techniques (Raman and IR), X-ray diffraction and
large-field energy-dispersive X-ray spectroscopy (EDS) mappings. Calcite
was observed as the dominant phase and carbon was observed in the
fossils as a byproduct of the decomposition. The preservation of
hydroxide calcium phosphate (Ca-10(PO4)(6)(OH)(2), hydroxyapatite) was
observed in both fossils. In addition, it was observed that there was a
smaller amount of pyrite (pyritization) in the Romualdo Formation sample
than in the Ipubi one. Large-field EDS measurements showed the major
presence of the chemical elements calcium, oxygen, iron, aluminum and
fluoride in the Ipubi fossil, indicating a greater influence of
inorganic processes in its fossilization. Our results also suggest that
the Romualdo Formation fossilization process involved the substitution
of the hydroxyl group by fluorine, providing durability to the fossils.
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