308 resultados para SPR


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Studies on cultured cells have shown that agonists induce several types of G protein-coupled receptors to undergo internalization. We have investigated this phenomenon in rat striatum, using substance P (SP)-induced internalization of the SP receptor (SPR) as our model system. Within 1 min of a unilateral striatal injection of SP in the anesthetized rat, nearly 60% of the SPR-immunoreactive neurons within the injection zone display massive internalization of the SPR--i.e., 20-200 SPR+ endosomes per cell body. Within the dendrites the SPR undergoes a striking translocation from the plasma membrane to endosomes, and these dendrites also undergo a morphological reorganization, changing from a structure of rather uniform diameter to one characterized by large, swollen varicosities connected by thin fibers. In both cell bodies and dendrites the number of SPR+ endosomes returns to baseline within 60 min of SP injection. The number of neurons displaying substantial endosomal SPR internalization is dependent on the concentration of injected SP, and the SP-induced SPR internalization is inhibited by the nonpeptide neurokinin 1 receptor antagonist RP-67,580. These data demonstrate that in the central nervous system in vivo, SP induces a rapid and widespread SPR internalization in the cell bodies and dendrites and a structural reorganization of the dendrites. These results suggest that many of the observations that have been made on the internalization and recycling of G protein-coupled receptors in in vitro transfected cell systems are applicable to similar events that occur in the mammalian central nervous system in vivo.

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En Argentina, en consonancia con el resto del mundo, la Nanotecnología es considerada un área estratégica. Sin embargo, las investigaciones en Nanobiotecnología todavía constituyen un área de vacancia. El uso de nanomateriales para desarrollar plataformas bioanalíticas que permitan la construcción de biosensores ofrece múltiples ventajas y una promisoria perspectiva de aplicación en diversas áreas. En la actualidad, los laboratorios de análisis clínicos, la industria farmacéutica y alimentaria, y los laboratorios de control bromatológico y ambiental requieren de metodologías analíticas que proporcionen resultados exactos, reproducibles, rápidos, sensibles y selectivos empleando pequeños volúmenes de muestra, con un mínimo consumo de reactivos y una producción de deshechos limpia y escasa. Las investigaciones en nanobiosensores se encuentran dirigidas hacia el logro de estas metas. Uno de los grandes desafíos es lograr biosensores miniaturizados con potencialidad para el desarrollo de dispositivos de medición descentralizada (“point of care”) y la detección simultánea de multianalitos. Aún cuando se han hecho innumerables desarrollos en los casi 50 años de vida de los biosensores, todavía hay numerosos interrogantes por dilucidar. La modificación con nanomateriales juega un rol preponderante en los transductores tanto en los electroquímicos como en los plasmónicos. El uso de películas delgadas de Au para SPR modificadas con grafeno u óxido de grafeno, es un campo de una enorme potencialidad y sin embargo es muy poco explotado, por lo que reviste gran importancia. En lo referido a la capa de biorreconocimiento, se trabajará con moléculas capaces de establecer interacciones de bioafinidad, como los anticuerpos y también moléculas que son muy poco usadas en nuestro país y en Latinoamérica como ADN, aptámeros, PNA y lectinas. RESUMEN: El Objetivo general de este proyecto es desarrollar nuevas plataformas bioanalíticas para la detección de diferentes eventos de bioafinidad a partir de la integración de transductores electroquímicos (EQ) y plasmónicos con materiales nanoestructurados (nanotubos de carbono, nanoláminas de grafeno, nanoalambres metálicos); biomoléculas (ADN, “peptide nucleic acid” (PNA), aptámeros, anticuerpos, lectinas) y polímeros funcionalizados con moléculas bioactivas. Las arquitecturas supramoleculares resultantes estarán dirigidas al desarrollo de biosensores EQ y plasmónicos para la cuantificación de biomarcadores de relevancia clínica y medioambiental. Se funcionalizarán CNT, grafeno, óxido de grafeno, nanoalambres metálicos empleando homopéptidos y proteínas con alta afinidad por cationes metálicos, los que se integrarán a transductores de carbono y oro y biomoléculas de reconocimiento capaces de formar complejos de afinidad (antígeno-anticuerpo, aptámero-molécula blanco, ADN-ADN, PNA-ADN, lectinas-hidratos de carbono, ligandos-cationes metálicos y avidina-biotina). Se sintetizarán y caracterizarán nuevos monómeros y polímeros funcionalizados con moléculas bioactivas y/o grupos rédox empleando diferentes rutas sintéticas. Se desarrollarán genosensores para la detección del evento de hibridación de secuencias de interés médico (cáncer de colon y de mama, tuberculosis); aptasensores para la detección de marcadores proteicos de T. cruzi, enfermedades cardiovasculares y contaminantes catiónicos; inmunosensores para la detección de biomarcadores proteicos relacionados con enfermedades cardiovasculares y cáncer; y biosensores de afinidad con lectinas para la detección de hidratos de carbono. La caracterización de las plataformas y las señales analíticas se obtendrán empleando las siguientes técnicas: voltamperometrías cíclica, de pulso diferencial y de onda cuadrada; stripping; resonancia de plasmón superficial; espectroscopía de impedancia electroquímica; microscopías de barrido electroquímico, SEM, TEM, AFM,SNOM, espectroscopías: UV-vis, FTIR,Raman;RMN, TGA y DSC.

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Time series of brightness temperatures (T(B)) from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) are examined to determine ice phenology variables on the two largest lakes of northern Canada: Great Bear Lake (GBL) and Great Slave Lake (GSL). T(B) measurements from the 18.7, 23.8, 36.5, and 89.0 GHz channels (H- and V- polarization) are compared to assess their potential for detecting freeze-onset/melt-onset and ice-on/ice-off dates on both lakes. The 18.7 GHz (H-pol) channel is found to be the most suitable for estimating these ice dates as well as the duration of the ice cover and ice-free seasons. A new algorithm is proposed using this channel and applied to map all ice phenology variables on GBL and GSL over seven ice seasons (2002-2009). Analysis of the spatio-temporal patterns of each variable at the pixel level reveals that: (1) both freeze-onset and ice-on dates occur on average about one week earlier on GBL than on GSL (Day of Year (DY) 318 and 333 for GBL; DY 328 and 343 for GSL); (2) the freeze-up process or freeze duration (freeze-onset to ice-on) takes a slightly longer amount of time on GBL than on GSL (about 1 week on average); (3) melt-onset and ice-off dates occur on average one week and approximately four weeks later, respectively, on GBL (DY 143 and 183 for GBL; DY 135 and 157 for GSL); (4) the break-up process or melt duration (melt-onset to ice-off) lasts on average about three weeks longer on GBL; and (5) ice cover duration estimated from each individual pixel is on average about three weeks longer on GBL compared to its more southern counterpart, GSL. A comparison of dates for several ice phenology variables derived from other satellite remote sensing products (e.g. NOAA Interactive Multisensor Snow and Ice Mapping System (IMS), QuikSCAT, and Canadian Ice Service Database) show that, despite its relatively coarse spatial resolution, AMSR-E 18.7 GHz provides a viable means for monitoring of ice phenology on large northern lakes.

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A multi-proxy palaeoecological investigation including pollen, plant macrofossil, radiocarbon and sedimentological analyses, was performed on a small mountain lake in the Eastern Pyrenees. This has allowed the reconstruction of: (1) the vegetation history of the area based on five pollen diagrams and eight AMS14C dates and (2) the past lake-level changes, based on plant macrofossil, lithological and pollen analysis of two stratigraphical transects correlated by pollen analysis. The palaeolake may have appeared before the Younger Dryas; the lake-level was low and the vegetation dominated by cold steppic grasslands. The lake-level rose to its highest level during the Holocene in the Middle Atlantic (at ca. 5060±45 b.p.). Postglacial forests (Quercetum mixtum and Abieto-Fagetum) developed progressively in the lower part of the valley, while dense Pinus uncinata forests rapidly invaded the surroundings of the mire and remained the dominant local vegetation until present. The observed lowering of the lake levels during the Late Atlantic and the Subboreal (from 5060 ± B.P. to 3590±40 b.p.) was related to the overgrowth of the mire. The first obvious indications of anthropogenic disturbances of the vegetation are recorded at the Atlantic/Subboreal boundary as a reduction in the forest component, which has accelerated during the last two millennia.

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Vol. 29-33 have title-page at beginning of second part of volume, covering entries in both parts; with vol. 34, title-page appears at beginning of first part of vol.

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Description based on: Vol. 2, no. 1 ; title from caption.