Fossilization results from several physical-chemical-geological
processes. Original labile and non-bioclastic structures rarely survive
throughout this process. In particular, the Crato Formation (Araripe
Basin) is one of the most significant Cretaceous Konservat-Lagerstatten
due to its well-preserved invertebrates, mainly three-dimensional
insects. In general, Crato insects exhibit brown-orange color,
constituted by goethite or hematite replacements. In this context, we
used the scanning electron microscopy coupled to energy dispersive
spectrometer and Raman spectroscopy to analyze Araripeblatta
dornellesae, a 115 million-years-old fossil from Crato Formation,
Araripe Basin. Our results show that a dark-color material rather than
the brown-orange pattern preserve this specimen. The carbon is
restricted to the fossil imprint, indicating some retention of the
original organic remains. In addition, the presence of original organic
components allowed to approach the biochemical aspects further than
simple morphology, as well as to elucidate the taphonomical complexity
involved in this preservation style.
%0 Journal Article
%1 WOS:000455151100005
%A Bezerra, Francisco Irineudo
%A da Silva, Joao Herminio
%A de Paula, Amauri Jardim
%A Oliveira, Naiara Cipriano
%A Paschoal, Alexandre Rocha
%A Freire, Paulo Tarso C
%A Neto, Bartolomeu Cruz Viana
%A Mendes, Marcio
%C PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL
%D 2018
%I SOC BRASILEIRA PALEONTOLOGIA
%J REVISTA BRASILEIRA DE PALEONTOLOGIA
%K Crato Cretaceous; Electron Formation; Lagerstiitten; Lower Microscopy} Scanning components; organic {taphonomy;
%N 3
%P 245-254
%R 10.4072/rbp.2018.3.05
%T THROWING LIGHT ON AN UNCOMMON PRESERVATION OF BLATTODEA FROM THE CRATO
FORMATION (ARARIPE BASIN, CRETACEOUS), BRAZIL
%V 21
%X Fossilization results from several physical-chemical-geological
processes. Original labile and non-bioclastic structures rarely survive
throughout this process. In particular, the Crato Formation (Araripe
Basin) is one of the most significant Cretaceous Konservat-Lagerstatten
due to its well-preserved invertebrates, mainly three-dimensional
insects. In general, Crato insects exhibit brown-orange color,
constituted by goethite or hematite replacements. In this context, we
used the scanning electron microscopy coupled to energy dispersive
spectrometer and Raman spectroscopy to analyze Araripeblatta
dornellesae, a 115 million-years-old fossil from Crato Formation,
Araripe Basin. Our results show that a dark-color material rather than
the brown-orange pattern preserve this specimen. The carbon is
restricted to the fossil imprint, indicating some retention of the
original organic remains. In addition, the presence of original organic
components allowed to approach the biochemical aspects further than
simple morphology, as well as to elucidate the taphonomical complexity
involved in this preservation style.
@article{WOS:000455151100005,
abstract = {Fossilization results from several physical-chemical-geological
processes. Original labile and non-bioclastic structures rarely survive
throughout this process. In particular, the Crato Formation (Araripe
Basin) is one of the most significant Cretaceous Konservat-Lagerstatten
due to its well-preserved invertebrates, mainly three-dimensional
insects. In general, Crato insects exhibit brown-orange color,
constituted by goethite or hematite replacements. In this context, we
used the scanning electron microscopy coupled to energy dispersive
spectrometer and Raman spectroscopy to analyze Araripeblatta
dornellesae, a 115 million-years-old fossil from Crato Formation,
Araripe Basin. Our results show that a dark-color material rather than
the brown-orange pattern preserve this specimen. The carbon is
restricted to the fossil imprint, indicating some retention of the
original organic remains. In addition, the presence of original organic
components allowed to approach the biochemical aspects further than
simple morphology, as well as to elucidate the taphonomical complexity
involved in this preservation style.},
added-at = {2022-05-23T20:00:14.000+0200},
address = {PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL},
author = {Bezerra, Francisco Irineudo and da Silva, Joao Herminio and de Paula, Amauri Jardim and Oliveira, Naiara Cipriano and Paschoal, Alexandre Rocha and Freire, Paulo Tarso C and Neto, Bartolomeu Cruz Viana and Mendes, Marcio},
biburl = {https://www.bibsonomy.org/bibtex/247a97523ae825ff1c196d57becb5708b/ppgfis_ufc_br},
doi = {10.4072/rbp.2018.3.05},
interhash = {f55ed5097466d0527b1225e017a2b384},
intrahash = {47a97523ae825ff1c196d57becb5708b},
issn = {1519-7530},
journal = {REVISTA BRASILEIRA DE PALEONTOLOGIA},
keywords = {Crato Cretaceous; Electron Formation; Lagerstiitten; Lower Microscopy} Scanning components; organic {taphonomy;},
number = 3,
pages = {245-254},
publisher = {SOC BRASILEIRA PALEONTOLOGIA},
pubstate = {published},
timestamp = {2022-05-23T20:00:14.000+0200},
title = {THROWING LIGHT ON AN UNCOMMON PRESERVATION OF BLATTODEA FROM THE CRATO
FORMATION (ARARIPE BASIN, CRETACEOUS), BRAZIL},
tppubtype = {article},
volume = 21,
year = 2018
}