Uma investigação das sequências de fase Hebbianas descritas como grafos de assembleias neuronais

Hebb proposed that synapses between neurons that fire synchronously are strengthened, forming cell assemblies and phase sequences. The former, on a shorter scale, are ensembles of synchronized cells that function transiently as a closed processing system; the latter, on a larger scale, correspond to the sequential activation of cell assemblies able to represent percepts and behaviors. Nowadays, the recording of large neuronal populations allows for the detection of multiple cell assemblies. Within Hebb’s theory, the next logical step is the analysis of phase sequences. Here we detected phase sequences as consecutive assembly activation patterns, and then analyzed their graph attributes in relation to behavior. We investigated action potentials recorded from the adult rat hippocampus and neocortex before, during and after novel object exploration (experimental periods). Within assembly graphs, each assembly corresponded to a node, and each edge corresponded to the temporal sequence of consecutive node activations. The sum of all assembly activations was proportional to firing rates, but the activity of individual assemblies was not. Assembly repertoire was stable across experimental periods, suggesting that novel experience does not create new assemblies in the adult rat. Assembly graph attributes, on the other hand, varied significantly across behavioral states and experimental periods, and were separable enough to correctly classify experimental periods (Naïve Bayes classifier; maximum AUROCs ranging from 0.55 to 0.99) and behavioral states (waking, slow wave sleep, and rapid eye movement sleep; maximum AUROCs ranging from 0.64 to 0.98). Our findings agree with Hebb’s view that neuronal assemblies correspond to primitive building blocks of representation, nearly unchanged in 10 the adult, while phase sequences are labile across behavioral states and change after novel experience. The results are compatible with a role for phase sequences in behavior and cognition

Estratigrafia de sequências do intervalo aptiano ao albino na Bacia do Araripe, NE do Brasil

This study has as a main objective to make a detailed stratigraphic analysis of the Aptian-Albian interval in the east part of Araripe Basin, NE of Brazil which correspond, litostratigraphically, to Rio Da Batateira, Crato, Ipubi and Romualdo formations. The stratigraphic analysis was based on three different stages, the 1D, 2D and 3D analysis; these ones were adapted to the sequence stratigraphy concepts in order to create a chronostratigraphic framework for the study area within the basin. The database used in the present study contains field and well information, wells that belong to Santana Project, carried out by the Ministério de Minas e Energia- DNPM- CPRM from 1977 to 1978. The analysis 1D, which was done separately for each well and outcrop allowed the recognition of 13 sedimentary facies, mainly divided based on predominant litologies and sedimentary structures. Such facies are lithologically represented by pebble, sandstones, claystones, margas and evaporates; these facies are associated in order to characterize different depositional systems, that integrate from the continental environment (fluvial system and lacustre), paralic system (delta system and lagunar) to the marine environment (shelfenvironment). The first one, the fluvial system was divided into two subtypes: meandering fluvial system, characterized by fill channel and floodplain deposits; the facies of this system are associated vertically according to the textural thinning upward cycles (dirting-up trend pattern in well logs). Lacustrine environment is mainly related with the lithotypes of the Crato Formation, it shows a good distribution within the basin, been composed by green claystone deposits and calcareous laminated. Deltaic System represented by prodelta and delta front deposits which coarsening upward tendency. Lagunar system is characterised by the presence of anhydrite and gypsum deposits besides the black claystone deposits with vegetal fragments which do not contain a fauna typically marine. The marine platform system is composed by successions of black and gray claystone with fossiliferous fauna of Dinoflagellates (Spiniferites Mantell, Subtilisphaera Jain e Subtilisphaera Millipied genre) typical of this kind of depositional system. The sedimentary facies described are vertically arranged in cycles with progradational patterns which form textural coersening upward cycles and retrogradational, represented by textural thinning dowward cycles. Based in these cycles, in their stack pattern and the vertical change between these patterns, the systems tracks and the depositional sequences were recognized. The Low System Track (LST) and High System Track (HST) are composed by cycles with progradational stack pattern, whereas the Trangessive System Track (TST) is composed by retrogradational stack pattern cycles. The 2D stratigraphic analysis was done through the carrying out of two stratigraphic sections. For the selection of the datum the deepest maximum flooding surface was chosen, inside the Sequence 1, the execution of these sections allowed to understand the behaviour of six depositional systems along the study area, which were interpreted as cycles of second order or supercycles (cycles between 3 and 10 Ma), according to the Vail, et al (1977) classification. The Sequence 1, the oldest of the six identified is composed by the low, transgressive and high systems tracks. The first two system tracks are formed exclusively by fluvial deposits of the Rio da Batateira Formation whereas the third one includes deltaic and lacustrine deposits of the Crato Formation. The sequences 2 and 3 are formed by the transgressive systems tracks (lake spreading phase) and the highstand system track (lake backward phase). The TST of these sequences are formed by lacustrine deposits whereas HST contains deltaic deposits, indicating high rates of sedimentary supply at the time of it s deposition. The sequence 4 is composed by LST, TST and HST, The TST4 shows a significant fall of the lake base level, this track was developed in conditions of low relation between the creation rate of space of accommodation and the sedimentary influx. The TST4 marks the third phase of expansion of the lacustrine system in the section after the basin´s rift, the lacustrine system established in the previous track starts a backward phase in conditions that the sedimentary supply rate exceeds the creation rate of space accommodation. The sequence 5 was developed in two different phases, the first one is related with the latest expansion stage of the lake, (TST5), the basal track of this sequence. In this phase the base level of the lake rose considerably. The second phase (related to the TST5) indicates the end of the lacustrine domain in the Araripe Basin and the change to lagunar system ant tidal flat, with great portions in the supratidal. These systems were formed by restricted lagoons, with shallow level of water and with intermittent connections with the sea. This, was the phase when the Araripe Basin recorded the most several arid conditions of the whole interval studied, Aptian Albian, conditions that allow the formation of evaporitic deposits. The sequence 6 began its deposition after a significant fall of the sea (LST6). The sequence 6 is without any doubtlessly, the sequence that has deposits that prove the effective entrance of the sea into the Araripe Basin. The TST6, end of this sequence, represents the moment which the sea reaches its maximum level during the Aptian Albian time. The stratigraphic analysis of the Aptian Albian interval made possible the understanding that the main control in the development of the depositional sequences recognized in the Araripe Basin were the variations of the local base level, which are controlled itself by the climate changes

Arquitetura deposicional e evolução tectono-estratigráfica das sequências pré-rifte e rifte, na porção central do Vale do Cariri, Bacia do Araripe, NE do Brasil

A complex depositional history, related to Atlantic rifting, demonstrates the geological evolution during the late Jurassic and early Neocomian periods in the Araripe Basin NE Brazil. Based on outcrop, seismic and remote sensing data, a new model of the tectono-stratigraphic evolution of the section that covers the stages Dom João, Rio da Serra and Aratu (Brejo Santo, Missão Velha and Abaiara formations) is presented in this paper. In the stratigraphic section studied, ten sedimentary facies genetically linked to nine architectural elements were described, representing depositional systems associated with fluvial, aeolian and deltaic environments. Based on the relationship between the rates of creation of accommodation space and sediment influx (A / S) it was possible to associate these depositional systems with High and Low accommodation system tracks. These system tracks represent two tectono-sequences, separated by regional unconformities. The Tectono-sequence I, which includes lithotypes from the Brejo Santo Formation and is related to the pre-rift stage, is bounded at the base by the Paleozoic unconformity. This unit represents only a High Accommodation System Track, composed by a succession of pelitic levels interbedded with sandstones and limestones, from a large fluvial floodplain origin, developed under arid climatic conditions. The Tectono-sequence II, separated from the underlying unit by an erosional unconformity, is related to the rift stage, and is composed by the Missão Velha and Abaiara Formation lithotypes. Changes in depositional style that reflect variations in the A / S ratio, and the presence of hydroplastic deformation bands, make it possible to divide this tectonosequence into two internal sequences. Sequence IIA, which includes the lower portion of the Missão Velha Formation and sequence IIB, is composed by the upper section of the Missão Velha and Abaiara Formations The Sequence IIA below, composed only by the Low Accommodation System Track, includes crossbedding sandstones interbedded with massive mudstones, which are interpreted as deposits of sandy gravel beds wandering rivers. Sequence IIB, above, is more complex, showing a basal Low Accommodation System Track and a High Accommodation System Track at the top, separated by an expansion surface. The lower System Track, related to the upper portion of the Missão Velha Formation, is composed by a series of amalgamated channels, separated by erosion surfaces, interpreted as deposits of a belt of braided channels. The High Accommodation System Track, correlated with the Abaiara Unit, is marked by a significant increase in the A / S, resulting in the progradation of a system of braided river deltas with aeolic influence. Regarding tectonic evolution, the stratigraphic study indicates that the Tectonosequence Rift in the Araripe basin was developed in two phases: first characterized by a beginning of rifting, related to Sequence IIA, followed by a phase of syndepositional deformation, represented by sequence IIB. The first phase was not influenced by the development of large faults, but was influenced by a sharp and continuous decrease of accommodation space that permitted a change in depositional patterns, establishing a new depositional architecture. In turn, the stage of syndepositional deformation allowed for the generation of enough accommodation space for the preservation of fluvial-lacustrine deposits and conditioned the progradation of a braided river-dominated delta system.

Interação entre o gene TKN2 (KNOX-type I) e o miR156 node durante a transição de fase vegetativa para reprodutiva em tomateiro (Solanum lycopersicum)

Pós-graduação em Ciências Biológicas (Genética) - IBB

Análise estratigráfica em depósitos lacustres maastrichtianos da Formação Yacoraite (Bacia de Salta - Argentina): definição e rastreabilidade de sequências de alta resolução

Pós-graduação em Geologia Regional - IGCE

Produção de biohidrogênio a partir de soro de leite em AnSBBR com recirculação da fase líquida

O presente estudo investigou a aplicação de dois tipos de AnSBBR (reatores anaeróbio com biofilme e operados em batelada e batelada alimentada sequenciais: com recirculação da fase líquida e com agitação) para produção de biohidrogênio tratando água residuária sintética (a base de soro de leite e lactose, respectivamente). O AnSBBR com recirculação da fase líquida, que foi o estudo principal do presente trabalho, apresentou problemas na produção de hidrogênio utilizando soro de leite como substrato. Algumas alternativas, como adaptação da biomassa com substratos puros de degradação mais fácil, controle do pH em valores muito baixos e diferentes formas de inoculação foram testadas, entretanto, sem obtenção de sucesso. A solução do problema foi obtida ao refrigerar o meio de alimentação a 4ºC para evitar a fermentação no frasco de armazenamento, retirar a ureia e a suplementação de nutrientes, e realizar lavagens periódicas do material suporte para retirada de parte da biomassa. Dessa forma eliminaram-se indícios de produção de H2S por possível ação de bactérias redutoras de sulfato (BRS) e atingiu-se uma produção estável de hidrogênio sem, entretanto, eliminar completamento o metano, que foi produzido em baixas concentrações. Depois de atingida a estabilidade, investigou-se a influência da concentração afluente de substrato, do tempo de enchimento e da temperatura na produção de biohidrogênio no AnSBBR com recirculação da fase líquida tratando soro de leite. O estudo da concentração afluente apresentou um ponto ótimo para a concentração de 5400 mgDQO.L-1, atingindo valores de 0,80 mol H2.mol-1 lactose e de 660 mL H2.L-1.d-1. O estudo do tempo de enchimento apresentou resultados similares para as condições analisadas. Com relação à temperatura, os melhores resultados foram obtidos com a temperatura mais baixa testada de 15ºC (1,12 mol H2.mol lactose-1 e 1080 mL H2.L-1.d-1), sendo que na temperatura mais alta testada (45°C) não ocorreu produção de hidrogênio. Para o AnSBBR com agitação mecânica, que foi um estudado complementar realizado pelo fato da lactose ser o principal complemento do soro de leite, o desempenho do biorreator foi avaliado de acordo com influência conjunta do tempo de ciclo (tC – 2, 3 e 4 h), da concentração afluente (CSTA – 3600-5400 mgDQO.L-1) e da carga orgânica volumétrica aplicada (COAV – 9,3, 12,3, 13,9, 18,5 e 27,8 mgDQO.L-1.d-1). Foram obtidos excelentes resultados: consumos de carboidratos (lactose), com valores médios sempre acima de 90% e uma produção estável de biohidrogênio em todas as condições estudadas, com metano em baixas concentrações apenas na condição de maior COAV. A diminuição do tC apresentou tendência clara de melhora sobre o RMCRC,n (rendimento molar entre hidrogênio produzido e carboidrato removido) apenas para as condições com menor concentração CSTA, havendo uma relação direta entre CSTA, e RMCRC,n em todos os valores de tC, exceto para o tempo de ciclo de 3 h, exatamente onde ocorreu produção de metano. O melhor valor de RMCRC,n obtido na operação com lactose (1,65 mol H2.mol Carboidrato-1) foi superior aos obtidos em outros trabalhos utilizando a mesma configuração de reator e sacarose como substrato. As análises filogenéticas mostraram que a maioria dos clones analisados foi semelhante à Clostridium. Além destes, clones filogeneticamente semelhantes com a Família Lactobacilaceae, especificamente Lactobacillus rhamnosus foram observados em menor porcentagem no reator, assim como clones com sequências semelhantes a Acetobacter indonesiensis.

Factores bióticos de mortalidad en la fase vegetativa del maíz en época seca y lluviosa y su respuesta a carbofuran

Se realizó este estudio para evaluar el efecto que tiene Carbofuran sobre el complejo de especies de insectos que atacan al maíz antes de la emergencia y durante los primeros 30 DDE. La siembra se realizó el 9 de marzo de 1986 utilizando la variedad NB-6 en la época seca, y el 22 de junio de 1986 utilizando la variedad NB-3 para la época lluviosa. El trabajo se realizó en el Centro Nacional de Investigación de granos básicos San Cristóbal, Departamento de Managua. Se realizaron dos ensayos evaluando la aplicación de Carbofuran al momento de la siembra y un tratamiento sin aplicación de insecticida, con seis repeticiones. En el muestreo de suelo en la época seca se encontraron larvas de Phillophaga sp con un promedio de 0.2 larvas/pts2, Aeolus sp con promedio de 0.3 larvas/pie2. Aeolus sp con promedio de 0.2 larvas/pie2, y Epitregus sp con promedio de 0.08 larvas/pie2. A los 5, 10, 15, 20, 25 y 30 días después de la emergencia se encontraron plantas que presentaban síntomas de marchitamiento en el cogollo y perforaciones en la base del tallo, en estas plantas se encontraron larvas de S. frugiperda y D. linneclete y plantas con perforaciones, sin encontrarse presentes estas larvas, esto ocurrió en la época seca. En la época lluviosa se encontraron en las plantas los mismos síntomas que en época seca, conteniendo larvas de S frugiperda, Aeolus sp y Listronotus sp. Con la aplicación de Carbofuran al momento de la siembra no se observó reducción en el porcentaje de plantas muertas por las especies de insectos reportadas, mientras se observó una diferencia significativa entre ciclo sobre el porciento de plantas muertas, encontrándose que para la época seca hubo un total de 7.41% de plantas muertas y en la época lluviosa se encontró un total de 3.5%.

Evaluación de diferentes alternativas quimicas y no quimicas para el manejo de patógenos de suelo en fase de semillero y campo en el cultivo del tomate (Licopersicum esculentum L.)

Con el fin de evaluar y seleccionar las mejores opciones para manejo de patógenos del suelo, que sean rentables económicamente para los productores y que preserven la calidad del medio ambiente y la salud humana, se realizó el presente estudio durante época de primera de 1995, en la finca del productor Pablo Maltéz, San Isidro de la Cruz Verde, Managua del 5 de junio al 7 de septiembre de 1995. El experimento se dividió en dos fases: de semillero y campo. En la fase de semillero, se evaluó el efecto de: Cal, Ceniza, Mezcla de cal y ceniza, Agua hirviendo, Vitavax-300 y un testigo sin aplicación, sobre la pudrición radical y del tallo, usando las variedades UC-82 y VF-134. Las variables a medir fueron: Porcentaje de incidencia de plantas enfermas por "Damping off” y el efecto de éstas alternativas sobre patógenos del suelo. En la fase de campo, se evaluó el efecto que tienen la mezcla de cal y ceniza, vitavax-300 y un testigo sin aplicación. Se evaluó la variedad UC-82 y se tornó la variable: Porcentaje de incidencia de plantas enfermas por pudrición radical y del tallo. Los resultados indican, que en la fase de semillero el Agua hirviendo fue el mejor tratamiento por ejercer buen efecto sobre patógenos del suelo en ambas variedades, en cambio Cal (460 g) y Ceniza (115 g) realizaron mejor efecto en la variedad VF-134, seguido por Mezcla de cal y ceniza, que resultó muy efectivo en el manejo de patógenos en la variedad UC-82. En fase de campo la mezcla de cal y ceniza fue el mejor tratamiento por ejercer buen control sobre la incidencia de pudrición radical y del tallo.

Estudio de medios de cultivos, explantes, frascos y sustratos en cladodio de pitahaya (Hylocereus undatus Britton et Rose) cv. chocoya de Nicaragua en fase de micropropagacion

Se estudiaron las fases de multiplicación, enraizamiento, aclimatización y el trasplante en el cultivo de pitahaya ( Hylocereus undatus Britton et Rose ) cultivar Chocoya . El ensayo se desarrolló en 4 fases: Fase 1: Multiplicación. 1a) Efecto de 9 medios de cultivo (dosis de BAP y sacarosa) y tipo de explantes (apical, central y basal). 1b) Efecto en crecimiento de tres tipos de explantes (apical, central y basal), número de explantes (5, 6 y 7 explantes/frasco) y volumen del frasco (220 y 430 ml). Fase 2: Enraizamiento. Efect o de 9 medios de cultivo , consistencia de medios de cultivo (líquida y semisólida) con explantes centrales. Fase 3: Aclimatización. Establecimiento de plántulas provenientes de la fase de enraizamiento con do s tipos de sustrato (compost y lombrihumus). Fase 4: Trasplante. Trasplante al campo de plantas provenientes de la fase de aclimatización segmentando el cladodio en 3 partes. Los ensayos fueron esta blecidos sobre diseños factoriales apropiados, y se utilizó Duncan - Waller ( Pr =0.05) como criterio de separación de promedios en las variables de cladodios, raíces, sobrevivencia, número de brotes, entre otras. En los medios de cultivo que contenían 1 mg l - 1 de BAP con 30 ó 40 g/l de sacarosa, resultó mejor el número de brotes emitidos por segmentos apicales de la vaina. En los tratamientos segmento central en frasco de 220 ml y 430 ml y segmento apical en frasco de 430 ml, el número de brotes fue mayor en t odos ellos con 5 y 6 tejidos por frasco. El promedio de raíces por cladodio fue de 3.32 en el medio de cultivo que contenía 30g/l de sacarosa, sin adición de AIA y de consistencia sólida. La aclimatación en el sustrato compost el promedio de longitud, núme ro de raíces y el porcentaje de sobrevivencia fue mejor cuando las plantas habían enraizado previamente en un medio de cultivo con 0.5 mg l - 1 de AIA y 60 g/l de sacarosa y en sustrato de lombrihumus la aclimatación fue mejor con plantas previamente enraizad as en el medio de cultivo con 0.5 mg/l de AIA y 30 g/l de sacarosa. En el trasplante, el segmento apical de la vaina presentó una mayor longitud (14.56 cm), la longitud de los brotes axilares fue superior en los segmentos centrales (2.46 cm). En todos los tratamientos no hubo muerte de los cladodios enraizados

Proceso sobre rato y no consumado : fase inicial diocesana

Resumen: El proceso para conceder la gracia apostólica de la dispensa del matrimonio rato y no consumado tiene una fase diocesana. La misma ha sido presentada por el autor en forma de taller práctico y forma parte del curso práctico Procesos matrimoniales, hoy, dictado por la Rota Romana en su visita a la Facultad de Derecho Canónico en Buenos Aires.

Evaluación del comportamiento de dos especies forrajeras Marango (Moringa oleifera Lam.) y Leucaena (Leucaena leucocephala De Witt) en la fase de vivero en la Universidad Nacional Agraria, Managua

Con el objetivo de caracterizar el comportamiento inicial de Moringa oleifera y profundizar en las ventajas de esta especie, en comparación con otra forrajera de rápido crecimiento (Leucaena leucocephala); se llevo a cabo en el vivero de la Facultad de Recursos Naturales un ensayo con diseño completamente aleatorio con dos tratamientos, y 20 repeticiones. Se realizó un conteo diario de germinación por un periodo de tres semanas (21 días); mientras patrones de crecimiento fueron determinados a partir de evaluaciones semanales de diámetro basal y raíz, longitud de tallo y raíz, y numero de raíces secundarias; así como producción de biomasa expresada en peso seco y peso fresco de la parte área y radicular, de una muestra de 8 plantas destruidas semanalmente. Los resultados muestran ventajas de la especie M. oleifera para la mayoría de variables; solo superado en el número de raíces secundarias de L .leucocephala. Los valores relacionados a la calidad o potencial de establecimiento sugieren pocos problemas de establecimiento en campo para las especies M. oleifera y L. leucocephala como producto del rápido crecimiento, y aun con la desigual proporción en la relación tallo-raíz, y biomasa.