Abstract
The study of ostracods from sedimentary successions exposed in the east portion of the Grajau Basin, Maranhao State, related to Codo Formation, revealed a Neoaptian lacustrine fauna characterized exclusively by Harbinia and Candona represented by the species Candona sp., Harbinia micropapillosa (Bate), Harbinia angulata (Krommelbein & Weber), Harbinia sinuata (Krommelbein & Weber), Harbinia sp. aff. H. symmetrica (Krommelbein & Weber), Harbinia salitrensis (Krommelbein & Weber) and Harbinia sp. The stratigraphical distribution patterns of the ostracod palaeocommunities in the studied sections confirmed the occurrence of a cyclic depositional lacustrine environment, as assumed by previous faciological studies. These cycles are associated with events of expansion and contraction of the lake, characterized mainly as hipersaline, with shallow-water and very low oxygen levels. The sudden environmental changes caused by these events produced a monospecific occurrence of some resilient species, followed by a mass death.
Cite
CITATION STYLE
Ramos, M. I. (2006). Caracterização e significado paleoambiental da fauna de ostracodes da Formação Codó (Neoaptiano), leste da bacia de Grajaú, MA, Brasil. Revista Brasileira de Paleontologia, 9(3), 339–348. https://doi.org/10.4072/rbp.2006.3.09
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