SOuza

Rev. bras. paleontol. 13(1):57-66, Janeiro/Abril 2010
© 2010 by the Sociedade Brasileira de Paleontologia doi:10.4072/rbp.2010.1.07 PALINOLOGIA DA FORMAÇÃO PIAUÍ, PENSILVANIANO DA BACIA DO
PARNAÍBA: BIOCRONOESTRATIGRAFIA DE INTERVALO SELECIONADO DO
POÇO 1-UN-09-PI (CAXIAS, MA, BRASIL)
PAULO ALVES DE SOUZA
Laboratório de Palinologia, DPE, IGeo, Programa de Pós-graduação em Geociências, UFRGS, Av. Bento Gonçalves, 9500,
91540-000, Porto Alegre, RS, Brasil. [e-mail]

LUCAS THETINSKI MATZEMBACHER
Laboratório de Palinologia, DPE, IGeo, UFRGS, Av. Bento Gonçalves, 9500, 91540-000, Porto Alegre, RS, Brasil. [e-mail] MARINA ABELHA & LEONARDO BORGHI
Laboratório de Geologia Sedimentar, CCMN, IGeo, UFRJ, Av. Athos da Silveira Ramos, 274, 21941-916,
Rio de Janeiro, RJ, Brasil. [e-mail], [e-mail]

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ABSTRACT – PALYNOLOGY OF THE PIAUÍ FORMATION, PENNSYLVANIAN OF THE PARNAÍBA BASIN:
BIOCHRONOSTRATIGRAPHY OF A SELECTED INTERVAL WITHIN THE BOREHOLE 1-UN-09-PI (CAXIAS,
MA, BRAZIL). The Pennsylvanian Piauí Formation, basal unit of the Balsas Group, is constituted by sandstones, shales and limestones, with scarce palynological records. This unit is interpreted mainly as continental to shorefacies in origin.
This paper presents the palynostratigraphical results obtained for the interval between 110.60 m and 178.12 m of the borehole 1-UN-09-PI, located in Caxias, Maranhão State, which corresponds to the upper microclastic portion of this unit in the borehole. Most part of the twelve core samples studied furnished palynological associations. Among the continental palynomorphs, saccate pollen grains are dominant, mainly taeniate bisaccate and non tateniate monosaccate species. Taking into account that there is no available palynological zonation of the Pennsylvanian-Permian interval of this basin, the scheme erected for the neighboring Amazonas Basin was used for comparisons.