Petrographic approach to the study of organic microfossils from the Irati Subgroup (Permian, Parana Basin, Brazil)


Autoria(s): Calca, Cleber Pereira; Fairchild, Thomas Rich
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

24/10/2013

24/10/2013

2012

Resumo

Early diagenetic chert, infrequently exploited in Phanerozoic micropaleontology, was examined for organic-walled microfossils in petrographic thin sections of silicified dolostones from diverse levels and localities of the Assistencia Formation (Permian, Parana Basin) in the state of Sao Paulo, Brazil. In contrast to previous palynological studies of this formation, the use of thin sections allowed direct observation in three dimensions of common palynomorphs, as well as benthic microbial mats preserved in situ in various stages of their life cycles and degradation. As in palynological residues from the more wellknown shale of this formation, the chert contains wind-dispersed pollen grains and phytoclasts derived from terrestrial sources and planktonic cryptarchs (unornamented coccoidal unicellular or colonial palynomorphs). However, only in the chert is it possible to see much more delicate microfossils, such as abundant cyanobacteria of the in situ benthic microbiota as well as chlorophycean microalgae of the microphytoplankton. Post-depositional processes affecting the formation have destroyed all but the most resistant organic remains in the other lithologies, such that only rare, degraded pollen grains are seen in the unsilicified dolostone of the formation, and in the shale the vast majority of microfossils have been compacted to flattened disks. On the other hand, early silicification not only preserved organic remains at an incipient stage of decomposition but also impeded significant further degradation due to compaction, recrystallization, and oxidation. Thus, the petrographic study of such chert can complement traditional palynological investigations in Phanerozoic rocks by furnishing hitherto unavailable information, especially with regard to benthic organic microfossils and fragile organic-walled phytoplankton normally absent from organic residues. (C) 2011 Elsevier Ltd. All rights reserved.

FAPESP (Fundacao de Amparo a Pesquisa de Sao Paulo)

Fundacao de Amparo a Pesquisa de Sao Paulo (FAPESP)

FAPESP

FAPESP

CAPES (Coordenadoria de Apoio ao Aperfeicoamento de Professores do Ensino Superior, Brazil)

CAPES (Coordenadoria de Apoio ao Aperfeicoamento de Professores do Ensino Superior, Brazil)

Identificador

JOURNAL OF SOUTH AMERICAN EARTH SCIENCES, OXFORD, v. 35, n. 9, supl. 4, Part 1, pp. 51-61, APR, 2012

0895-9811

http://www.producao.usp.br/handle/BDPI/35904

10.1016/j.jsames.2011.10.005

http://dx.doi.org/10.1016/j.jsames.2011.10.005

Idioma(s)

eng

Publicador

PERGAMON-ELSEVIER SCIENCE LTD

OXFORD

Relação

JOURNAL OF SOUTH AMERICAN EARTH SCIENCES

Direitos

restrictedAccess

Copyright PERGAMON-ELSEVIER SCIENCE LTD

Palavras-Chave #PALYNOLOGY #PETROGRAPHY #MICROPALEONTOLOGY #CHERT #IRATI SUBGROUP #PERMIAN #PALEOENVIRONMENTAL DISTRIBUTION #EXPERIMENTAL SILICIFICATION #PROTEROZOIC MICROFOSSILS #FOSSIL RECORD #CHERT #MICROORGANISMS #STROMATOLITES #CYANOBACTERIA #SPITSBERGEN #PALYNOLOGY #GEOSCIENCES, MULTIDISCIPLINARY
Tipo

article

original article

publishedVersion