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Spectroscopic studies of wood fossils from the Crato Formation, Cretaceous Period

2013; Elsevier BV; Volume: 115; Linguagem: Inglês

10.1016/j.saa.2013.06.042

1873-3557

J.H. da Silva, P.T.C. Freire, B.T.O. Abagaro, J.A.F. Silva, G.D. Saraiva, Flaviana Jorge de Lima, Olga Alcântara Barros, Renan Alfredo Machado Bantim, Antônio Álamo Feitosa Saraiva, Bartolomeu C. Viana,

Botanical Research and Applications

In this work we study two types of wood fossils (Gymnosperms, Araucariaceae) from the Crato Formation of Araripe Basin in Brazil, from the Cretaceous Period. The samples were characterized by Raman and infrared spectroscopies, X-ray diffraction and scanning electron microscopy. The results obtained by different techniques showed that although the rocks surrounding the fossils have predominantly the same constitution - calcite - however, the formation processes of these types of wood fossils are quite different. One of the fossils, denominated as light wood, is predominantly composed of gypsum, while the other fossil, the dark wood, is rich in amorphous carbon, possibly the kerogen type. Implications relative to the environment where the plants lived millions years ago are also given. Finally, the results highlight the constitution of one of the most important paleontological sites of the Cretaceous Period in the South America.