Abstract Benthic foraminifera, ostracods and pteropods are reliable paleoenvironmental indicators in Quaternary deposits. However, in the Ceará Basin, on the Brazilian Equatorial Margin, these microfossils are poorly studied. This paper investigates environmental changes during the Pleistocene–Holocene transition in the Icaraí subbasin based on micropaleontological analysis of the core ANP 1011. Seventy-four taxa of benthic foraminifera, represented predominantly by Globocassidulina, Uvigerina, Pyrgo and Melonis, have been identified. The ostracod assemblages are composed mainly by the families Macrocyprididae, Cytheruridae, Trachyleberididae, Pontocyprididae and Krithidae, of which the genus Krithe was the most abundant. The composition of the ostracod assemblages identified in this study area differs somewhat from other regions of the Brazilian Margin. The assemblages of foraminifera and ostracod characterize a typical bathyal paleoenvironment. The occurrence of pteropods and dominance of epifaunal foraminifera taxa, mainly Pyrgo sp. and Miliolinella sp. in the lower portion of the core (Pleistocene), indicates higher phytodetritus input and oxygen concentration. A conspicuous environmental change was observed in the upper portion of the core, which corresponds to the Holocene, where the increase of infaunal foraminifera (e.g., Uvigerina, Globocassidulina and Melonis) suggests reduction in the organic matter input and, probably, increased bacterial density and depletion in dissolved oxygen in the sediment. deposits However Basin Margin studied PleistoceneHolocene Pleistocene Holocene 1011 Seventyfour Seventy four Uvigerina Melonis Macrocyprididae Cytheruridae Trachyleberididae Krithidae abundant paleoenvironment sp Pleistocene, , (Pleistocene) concentration e.g., eg e g (e.g. probably sediment 101 (Pleistocene e.g. (e.g 10 e.g 1

Abstract A study of macro and microfacies, palynoflora and palynofacies of the non-marine Cerro Negro Formation at President Head Peninsula, Snow Island, northwest of the Antarctic Peninsula, was developed. Two assemblages were recognized: Palynofacies assemblage 1 (P1) at the base of the section with a dominance of fern spores and conifer pollen grains, and facies association consisting of a clastic layer, with the predominance of mudstones; and Palynofacies assemblage 2 (P2) at the top of the section, with remarkable abundance of AOM/Pseudoamorphous particles, associated with facies that includes tuffs. The complete section shows in some levels the presence of freshwater algae and translucent phytoclasts. The integrated data characterizes a fluvial-lacustrine environment, what is reinforced by the occurrence of freshwater algae (Botryococcus) in some levels of P1 and P2. We could verify an increase in volcanic activity towards the top of the section that apparently has played an important role in the collapse of the palynoflora. The occurrence of the spore species Muricingulisporis annulatus, Sotasporites elegans, S. triangularis, Foraminisporis wonthaggiensis, and F. asymmetricus in the Cerro Negro Formation allows the correlation with sections in South America and Australia, suggesting an Aptian age for these deposits.

Análises paleoecológicas são ferramentas importantes para a reconstrução de paleoambientes. Este trabalho teve como objetivo utilizar análises de associação de ostracodes e microfácies carbonáticas de um poço (Carbomil) e um afloramento (Ponto Quixeré) da Formação Jandaíra, Bacia Potiguar, a fim de verificar como estes métodos corroboram e complementam um ao outro. Dois paleoambientes para o Poço Carbomil (associações 1 e 2, respectivamente, ambiente marinho e mixo-halino) e um para o Ponto Quixeré (associação 3, ambiente marinho) foram identificados por meio da análise das associações de ostracodes. O estudo das seções petrográficas permitiu a identificação de duas fácies diferentes para o Poço Carbomil, packstonesa wackstonesbioclásticas, representando um sistema marinho salobro ou marinho restrito; grainstonesa packstonesbioclásticas, indicando um sistema marinho raso normal). As amostras do Ponto Quixeré parecem apontar para um ambiente de pouca energia. Em geral, as informações provenientes da análise das microfácies carbonáticas corroboram e complementam os dados fornecidos pelas assembleias de ostracodes, o que permitiu um maior grau de precisão na análise paleoambiental.

Paleoecological analyses are important tools for the reconstruction of paleoenvironments. This paper had the objective of using analysis of ostracode assemblages and carbonate microfacies of a well (Carbomil) and an outcrop (Quixeré) from the Jandaíra Formation, Potiguar Basin, in order to verify how they corroborate and complement the other. Two paleoenvironments for Carbomil Well (assemblages 1 and 2, respectively marine and brackish to neritic environments) and one for Quixeré Outcrop (assemblage 3, marine environment) were identified through the ostracode assemblage analysis. Thin section analysis allowed the identification of two different facies for Carbomil Well, i.e. bioclastic packstones to wackstones, a marine brackish or restricted marine system; and bioclastic grainstones to packstones, a normal, shallow marine system. High levels of alteration on the samples prevented an adequate analysis of Quixeré Outcrop; however, it seems to point towards a low-energy environment. Overall, information provided by the thin sections corroborate and complement data of the ostracode assemblages, which allowed a higher degree of certainty for the paleoenvironmental analysis.