Literature DB >> 26221982

Paleolimnological inferences based on Oligocene ostracods (Crustacea: Ostracoda) from Tremembé Formation, Southeast Brazil.

Cristianini T Bergue1, Maria da Saudade A S Maranhão2, Gerson Fauth1.   

Abstract

Non-marine Oligocene ostracods from Tremembé Formation (Taubaté Basin, Southeast Brazil) are studied for the first time. The study reveals rich assemblages which are probably composed of many new taxa, two of which are described here. The sixteen ostracod species registered are classified in the generaCypretta Vávra, Strandesia Stuhlmann,Potamocypris Brady, Heterocypris Claus,Eucypris Vávra, Herpetocypris Brady and Norman, Cytheridella Daday and LimnocythereBrady. Two new species of the latter are herein proposed: L. mandubi sp. nov. and L. katu sp. nov. The succession of ostracod assemblages along the studied core changes conspicuously in composition, abundance and preservation, and are characterized by the following associations: Herpetocypris-Cytheridella (lower), Limnocythere-Cypretta (middle) andPotamocypris-Heterocypris (upper). It is assumed that these associations represent different ecological phases of the paleolake Taubaté which is in accordance to previous stratigraphic and paleontological studies in the basin. The results from this pioneering taxonomic and paleoecological study on ostracods from Tremembé Formation reinforce the potential of these fossils for paleolimnological researches in Brazilian Cenozoic deposits.

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Year:  2015        PMID: 26221982     DOI: 10.1590/0001-3765201520140366

Source DB:  PubMed          Journal:  An Acad Bras Cienc        ISSN: 0001-3765            Impact factor:   1.753


  1 in total

1.  Limnological response from high-altitude wetlands to the water supply in the Andean Altiplano.

Authors:  Ignacio García-Sanz; Inger Heine-Fuster; José A Luque; Héctor Pizarro; Rodrigo Castillo; Matías Pailahual; Manuel Prieto; Pablo Pérez-Portilla; Adriana Aránguiz-Acuña
Journal:  Sci Rep       Date:  2021-04-08       Impact factor: 4.379

  1 in total

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