Cytogenetic analysis of the neotropical spider Nephilengys cruentata (Araneomorphae, tetragnathidae): standard staining, NORs, C-bands and base-specific fluorochromes

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Diversidade de Phytophthora parasitica isolados de Citrus usando seqüências de nucleotídeos da região ITS-5.8S rDNA

Realizou-se estudo para caracterização e verificação da diversidade genética de Phytophthora parasitica, agente causador da gomose dos citros. Quatorze isolados de Phytophthora parasitica, provenientes do Estado de São Paulo, foram seqüenciados a partir das regiões internas transcritas (ITS1 e ITS2) do gene 5.8S. Obtiveram-se seqüências de 812 pb a 860 pb que foram comparadas com seqüências de outras espécies de Phytophthora spp depositadas no NCBI. Foram feitos estudos filogenéticos, utilizando-se o método neighbor-joining com 1000 bootstrap e construído o dendrograma mais representativo. Obtiveram-se os resultados de 98,88% a 100% de similaridade genética entre os 14 isolados paulistas, e 99,5% a 98,8% entre estes e a seqüência de P. nicotianae (gi| 8927482) obtida do GenBank NCBI.

Reconhecimento de seqüências de atividades funcionais em pacientes com acidente cascular encefálico

During the motor rehabilitation of patients with neurological pathologies, there are many factors that have an influence on the therapeutical process. It is possible that the demonstration using videotapes or photographs of movements that will be learned can assist the codification, classification and reorganization of the elements of the task in familiar diagrams and thus facilitate the process of motor rehabilitation. The aim of this study was to analyze the performance in the test of recognition of sequences of functional activities such as water drinking and hair combing presented partially (by photos) and completely (by video) to the patients with encephalic vascular accident . The sample was generated from 12 patients (62 ± 8 years) and 10 healthy subjects (53 ± 5 years), of both sex, divided in two groups for which 5 functional activities were presented partially and completely, in 4 sequences that varied between reached and not reached objectives and correct and incorrect movements, during 24 trials. The test t'Student was applied to verify differences in the recognition time between the groups, and to compare the performance between the tests carried through at 9:00 am and retests at 9:00 am and 4:00 pm. To compare the frequency between the types of reply, the test Qui-square was used. It was verified that the patients presented a greater recognition time and a lower number of correct answers than the healthy subjects, and had better performances in the recognition of the complete sequence than the partial one. Bigger frequency was observed in the reply that the objective and the movement were being presented correctly, however the healthy subjects had soon indicated the correct reply in the first trials. An improvement tendency was observed in the performance, when the stages of tests and retests had been carried through in the same schedule. According to the results, it is suggested that the patients with stroke can better recognize the correct movements of a functional activity when it is presented completely in video form, what can influence the choice of the therapeutical strategy during the process of motor rehabilitation

Reconhecimento de seqüências de atividades funcionais em pacientes com acidente cascular encefálico

During the motor rehabilitation of patients with neurological pathologies, there are many factors that have an influence on the therapeutical process. It is possible that the demonstration using videotapes or photographs of movements that will be learned can assist the codification, classification and reorganization of the elements of the task in familiar diagrams and thus facilitate the process of motor rehabilitation. The aim of this study was to analyze the performance in the test of recognition of sequences of functional activities such as water drinking and hair combing presented partially (by photos) and completely (by video) to the patients with encephalic vascular accident . The sample was generated from 12 patients (62 ± 8 years) and 10 healthy subjects (53 ± 5 years), of both sex, divided in two groups for which 5 functional activities were presented partially and completely, in 4 sequences that varied between reached and not reached objectives and correct and incorrect movements, during 24 trials. The test t'Student was applied to verify differences in the recognition time between the groups, and to compare the performance between the tests carried through at 9:00 am and retests at 9:00 am and 4:00 pm. To compare the frequency between the types of reply, the test Qui-square was used. It was verified that the patients presented a greater recognition time and a lower number of correct answers than the healthy subjects, and had better performances in the recognition of the complete sequence than the partial one. Bigger frequency was observed in the reply that the objective and the movement were being presented correctly, however the healthy subjects had soon indicated the correct reply in the first trials. An improvement tendency was observed in the performance, when the stages of tests and retests had been carried through in the same schedule. According to the results, it is suggested that the patients with stroke can better recognize the correct movements of a functional activity when it is presented completely in video form, what can influence the choice of the therapeutical strategy during the process of motor rehabilitation

As relações entre tectonismo e seqüências deposiconais no rifte potiguar - porção SW do Graben de Umbuzeiro, bacia potiguar emersa

Through an integrated approach, using litho, chrono and biostratigraphic data, the relative importance of climate variations and tectonics were recognized in rift sediments of the onshore Potiguar Basin, Northeast Brazil. Concepts of sequence stratigraphy were applied as a template to integrate sedimentological and geochemical data (oxygen isotopes), as well as quantitative palynologic methods to address and recognize the main depositional patterns produced in a rift basin. The main objective was to address the relative importance of climate changes and tectonics to the resultant stratigraphic architecture. The results of computer simulations of sedimentary basin fills of rift basins were quite useful to test working hypothesis and mimic the process of filling a half graben during a rift event. The studied section includes a neovalanginian-eobarremian (Lower Cretaceous) rift interval from the Pendência Formation, located in the southwestern portion of Umbuzeiro Graben, in the offshore Potiguar Basin. The depositional setting is interpreted as progradational deltaic system entering a lake from its flexural margin. Sismoestratigraphyc and well logs analyses allowed to interpret two regressive intervals (Green and Yellow Sequences), separated by a broad transgressive interval (Orange Sequence), known as the Livramento Shale. The depositional history encompass three stages: two tectonically active phases, during the deposition of the Green and Yellow Sequences, and a tectonically quiescent phase, during the deposition of the Orange Sequence. Paleoclimatic interpretation, based on quantitative palynology and geochemical data (��18O), suggests a tendency to arid conditions during the tectonically active phases and wet conditions during the tectonically quiescent phase. Stratigraphic modeling and backstripping techniques, supported by paleoclimatic/paleoecologic interpretations provide a powerful methodology to evaluate the tectonic and climatic controls on tectonic lakes

Formação de classes ordinais após a aprendizagem de seqüências independentes

A aquisição de relações ordinais entre estímulos arbitrários é uma importante habilidade comportamental, requisito para a aprendizagem de comportamentos acadêmicos, especialmente a alfabetização. O propósito deste estudo foi investigar o efeito do ensino de seqüências de dois termos com sobreposição na emergência de relações ordinais com mais de dois estímulos. A sobreposição ocorre quando o último estímulo em uma seqüência de dois estímulos é o primeiro de outra seqüência (e.g., S1 -> S2 e S2 ->S3, onde S2 é o estímulo sobreposto). Nas Etapas 1 e 2 de um experimento conduzido com cinco estudantes do ensino fundamental foram ensinadas seqüências de dois termos com os cinco estímulos de um conjunto A (A1 -> A2, A2 -> A3, A3 -> A4, A4 ->A5) e os cinco de um conjunto B (B1 -> B2, B2 ->B3, B3 -> B4, B4 -> B5). Estabelecida essa linha de base, foram conduzidos testes da emergência de relações ordinais com três, quatro e cinco termos dos conjuntos A e B, separadamente. A Etapa 3 avaliou se estímulos das seqüências ensinadas eram mutuamente substituíveis, com base na mesma função ordinal (primeiro, secundo, etc.). Os estudantes compuseram as relações ordinais ensinadas e apresentaram relações ordinais emergentes com estímulos dos conjuntos A e B, separadamente. Três estudantes também realizaram a substituição mútua entre estímulos dos conjuntos A e B na Etapa 3. Esses resultados sugerem a formação de cinco classes de estímulos (A1B1, A2B2, etc.), cada uma consistindo de estímulos que ocuparam a mesma função ordinal em diferentes seqüências. Os resultados têm implicações para a análise de comportamento simbólico complexo. Merecem consideração, também, aspectos metodológicos que favoreceram a aprendizagem relacional e a emergência de comportamento novo.

Estratigrafia de seqüências das formações Taciba e Rio Bonito (Membro Triunfo) na região de Mafra/SC, leste da Bacia do Paraná

The Taciba and Rio Bonito (lower Triunfo Mbr) formations are divided into six depositional sequences based on cores, gamma-ray and electrical logs from shallow drillings from northern Santa Catarina State, Each sequence is formed by two systems tracts, a lower one, sandy (lowstand) and an upper one, shaly (highstand). The Taciba Formation has three sequences, S 0 to S 0 sequence S 0 has a thick turbidite sandstone at the base (Rio Segredo Member) that pinches out towards the eastern margin and even disappears in the Mafra outcrop area. Sequence S 1 varies from a thin fluvial-estuarine system to a thick turbidite sandstone of a channelized fan system; S 1 upper shaly system tract is marine in well PP-11, and it is glacially-influenced in well PP-10. Sequence S 2 is a thick sand-stone body of shallow marine origin, but restricted to one well (PP-11); its upper shaly tract is dominated by massive siltstones intercalated with thin, distal tempestites. The lower Triunfo Member (or Taciba-Triunfo transition) begins with the arrival of deltaic clastics of sequence S 3 lower tract, coarsening-up from medial- to proximal delta front sandstones. Sequence S 4 is quite similar to S 3, both showing sand-stone progradation from north to south, as opposed to the southwest-sourced transgressive diamictites. Sequence S 5 consists of fluvial deposits at well PP-12, and two transgressive cycles from wells PP-11 to PP-9, each one of them composed of fluvial-estuarine to marine systems. Well PP-10 is an exception, where the lower cycle presents deglaciation to marine deposits.

Ciclos e seqüências deposicionais das formações Rio da Batateira e Santana (Andar Alagoas), Bacia do Araripe, Brasil

The Rio da Batateira e Santana formations, the latter with Crato, Ipubi and Romualdo members (Alagoas Stage, Aptian), were studied in four cored and logged wells from the eastern portion of Araripe Basin, Northeastern Brazil. The investigated section is 230 m-thick, and PS-14 well is the most representative, because it is the only one which sampled the evaporites of Ipubi Member. Nine facies cycles were identified, being formed by siliciclastics (estuarine, deltaic and lacustrine), mixed lithologies (lacustrine), carbonates, black shales and marls (lacustrine), and gypsum-anhydrite (lacustrine evaporite). The ordering of facies cycles furnished six depositional sequences. They were formed by siliciclastic, regressive-transgressive R-T cycles (S1 and S4, corresponding to Rio da Batateira Formation and to Santana Formation/Romualdo Member), by siliciclastics and carbonates, R-T cycles (S2, S3.1 and S3.2, corresponding to Crato Member), and by siliciclastic-carbonate, R-T cycles followed by evaporitic cycles (S3.3, referred to Ipubi Member). The last cycles correspond to concentration-dilution, C-D cycles of marine brines, which precipitated gypsum in the restricted lacustrine basin.

Estratigrafia de seqüências das formações Serra Alta, Teresina e Rio do Rasto (permiano, Bacia do Paraná) na porção nordeste do Paraná e centro-sul de São Paulo

Pós-graduação em Geologia Regional - IGCE

Análise filogenética da subfamília Callichthyinae (Teleostei: Siluriformes: Callichthyidae) com base em seqüências de DNA nuclear e mitocondrial

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Análises moleculares na subfamília hypoptopomatinae (Siluriformes, Loricariidae): isolamento, caracterização e mapeamento cromossômico de sequências repetitivas

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Estratigrafia das seqüências deposicionais do grupo Guatá, borda leste da Bacia do Paraná

Pós-graduação em Geologia Regional - IGCE

Estratigrafia de seqüências do Grupo Itararé (Neocarbonifero-Eopermiano) na região de Rio Negro (PR) - Mafra (SC)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)