Literatura académica sobre el tema "Trujillo (Venezuela : State)"

A new striking cloud frog of the genus Aromobates is described from the northwestern portion of the Cordillera de Merida in Venezuela. The new species is unique in several aspects, and its inclusion in Aromobates is supported by molecular analyses. This Aromobates is characterized by the presence of dark dorsolateral stripes, absence of pale dorsolateral, oblique lateral and ventrolateral stripes. Furthermore, it is the only non-aposematic Aromobates having dark to emerald green in life on dorsal surfaces and a highly ornamented pattern at both dorsal and ventral sides. This species is known from a single population in Carache (Trujillo State, Venezuela). Its population, although limited apparently to a small area, seems relatively abundant at the type locality and surroundings.

Chemical constituents of the essential oil from the leaves of Minthostachys mollis (Kunth) Griseb Vaught var. mollis collected in January 2008 at Tuñame, Trujillo State, Venezuela, were separated and identified by GCMS analysis. The essential oil was obtained by hydrodistillation and thirteen components (98.5% of the sample) were identified by comparison with the Wiley GCMS library data base. The two major components were pulegone (55.2%) and trans-menthone (31.5%). The essential oil showed a significant inhibitory effect against Gram-positive and Gram-negative bacteria, especially Bacillus subtilis and Salmonella typhi (4 μg/mL).

A new scorpion species, Tityus imei sp. nov., is described, representing the first record of the genus for the southern foothills of Sierra de Portuguesa in the western Venezuelan state of Portuguesa. The species is morphologically related to T. sanarensis, from the state of Lara, and T. boconoensis, from state of Trujillo. Tityus imei sp. nov. can be distinguished by the array of dorsal trichobothria in the pedipalp femur (d3, d4, d5) and by the following combination of female metasomal segment II characters: (i) ventral keels double and parallel up to two thirds of the segment, whereupon they converge into a single keel and separate again in the base; (ii) full, parallel ventral keels, including a well defined central keel in the second half of the segment. A molecular approach was undertaken to estimate the genetic relationship between the new species, T. sanarensis, T. boconoensis, and T. discrepans. Sequencing of a 562 bp-segment encoding sectors M6 to M11 of the cytochrome oxidase subunit I revealed that T. imei sp. nov. diverges from T. sanarensis and T. boconoensis, particularly in the polymorphic sector I4, sharing more overall sequence similarity with the northcentral Venezuelan species, T. discrepans. The new species is of potential medical importance given the presence of venom components whose mass resembles that of scorpion neurotoxins affecting voltage-sensitive sodium channels, as indicated by MALDI-TOF MS analyses.

Abstract Introduction The Mérida Andes (Venezuela) formed in the middle Miocene due to oblique convergence between the South American plate and the Maracaibo block [Audemard et al., 2002] (figs. 1A and 1B). The study area corresponds to the so-called “Barbacoas platform” [Renz, 1960], which constitutes the northeastern termination of the belt, NE of Valera (fig. 2). It is located in the northeastern part of Trujillo block [Hervouët et al., 2001], considered as an independent block separated from the main Maracaibo block along the Valera fault. According to Stéphan [1982], the N170°E-trending Caribbean compression developed in this area from late Cretaceous to Eocene. It was followed by a N105°E-trending compression older than middle Miocene, and finally by the NW-SE Andean compressional stage that lasted till now in most of the chain. However, east of El Empedrado fault, a NNE-SSW compression presently occurs that is oblique to the classical Andean stage. The tectonic evolution of the Andean stage is not well understood. The Mérida Andes are mainly composed of Precambrian and Paleozoic rocks. The northern part of the belt only comprises a complete and continuous Jurassic to Paleogene cover. This lithologic pattern is probably a consequence of the tectonic escape of the Maracaibo block, and more particularly of the smaller Trujillo block. The Mérida and Carribean belts being close to each other, the influence of the Andean deformation on the Caribbean allochthonous must be taken into account. In order to make a structural analysis at regional scale, we privileged the use of remote sensing data (Landsat, Spot and Radar images) and aerial photographs. This was complemented by structural data obtained in the field, allowing the study of geometric and chronological relationships between the tectonic structures. Lithostratigraphy of the northeastern Andes Andean formations The first Mesozoic deposits rest unconformably upon the marine Permian (Palmarito Fm.) [Gonzalez de Juana et al., 1980]. During the Jurassic, continental deposits of La Quinta Fm. were trapped in NE-SW grabens [Gonzalez de Juana et al., 1980] that opened due to rifting of the northern margin of the South-American plate. The first marine sediments are composed of thick sandstone layers at the bottom and limestone at the top, Barremian-Albian in age (Peñas Altas Fm). It is followed by Cenomanian-Campanian (La Luna Fm.) composed of euxinic black limestone and clay. Cretaceous ends with the Maastrichtian (Colon Fm.) composed of clay and limestone lenses with the intercalation of a white sandstone layer (Cujisal Member) [Renz, 1959; Pierce, 1960; Gonzalez de Juana et al., 1980]. Paleogene layers correspond to low depth deposits, such as the Paleocene-Eocene (Humocaro Fm.), and the upper Paleocene-early Eocene (Quebrada Arriba Fm). The Caribbean allochthonous The Caribbean series outcrop in the El Tocuyo area (fig. 3). The Barquisimeto Fm. (late Cretaceous) is composed of clay, clayey schist, marl, dark gray and black limestone, and phtanite [Bellizia, 1985; Stéphan, 1982; Lexico Estratigra-fico de Venezuela, 1997]. The Matatere Fm. (late Cretaceous-Paleocene) is composed of sandy turbidites involving sandy conglomerates. Tectonic structures of the northeastern Andes and adjacent plains The study area (figs. 3, 4) forms reliefs that can reach 3000 m. It is westerly and easterly surrounded by flat lying plains (La Pastora plain to the west ; El Tocuyo “synclinorium” [Stéphan, 1982] to the east) with elevations less than 500 m. To the north and east, it is overlain by the Lara overthrusts belonging to the Caribbean orogen. To the south, the Andean reliefs are mainly composed of Precambrian and Paleozoic rocks. This Barbacoas platform is westerly and easterly bounded by the San Pedro and Humocaro anticlines respectively, separated by the “Barbacoas synclinorium” [Renz, 1960] forming a flat-lying area. The Humocaro anticline: inversion of a Jurassic graben The 9 km width and 16 km length NE-trending Humocaro Bajo anticline is composed of a complete Meso-Cenozoic sedimentary sequence. It is overturned toward the SE (fig. 4). The Jurassic layers outcrop in the San Pedro and Humocaro Bajo anticlines whereas they are missing in the Barbacoas synclinorium, showing that the area was organized in horsts (Barbacoas) and grabens during the Jurassic. The western boundary of the Jurassic layers is not defined (El Empedrado fault?) compared to the eastern border where the layers overstep the Humocaro area. We interpret that the Humocaro anticline formed during inversion of a preexisting graben in the Andean stage. This led to formation of a wide anticline overturned outwards of the eastern graben. This is not the case of the San Pedro anticline overturned inwards of the western graben. The Barbacoas synclinorium: formation of flower structures Both the morphology and trend of the folds in the Barbacoas synclinorium (fig. 4) differ from those of the Humocaro anticline. Folds, trending ~N030°E, are narrow and well displayed on the remote sensing imagery. There are bounded by N030°E to N045°E trending left-lateral strike-slip faults juxtaposing contiguous anticlines. Numerous tectonic structures of various sizes affect these folds. In the field, we observed tension fractures striking N050°–060°E, N110°E and N150°E, an high-grade N030°–040°E deformation nearby strike-slip faults, fractures in various directions, and a field of flattened ammonites stretched in the N010°– to N030°E direction associated with a N010°E-striking cleavage. A N-S to NNE-SSW compression is well individualized (fig. 5, VE01–14, VE01–26, Ve02–30). It is responsible for left-lateral strike-slip motions along N030–045°E directed faults. Narrow anticlines, parallel to these faults, can be interpreted as flower structures. Nearby these tectonic irregularities, the compression turns from N-S to N110°E. The western area : associate pull-apart and buckling The western plain can be considered as a pull-apart basin that opened locally at the step-over of a NE-SW left-lateral fault (figs. 3, 5, VE03–12). The San Pedro anticline is parallel to and has the same length of the La Pastora plain. Since it is overturned toward the Jurassic graben (fig. 4), it cannot be related to a positive tectonic inversion. We interpret the San Pedro anticline as an extensional forced fold [Cosgrove and Ameen, 2000; Maurin and Nivière, 2000] because of (1) its position relative to the La Pastora graben; (2) the lack of internal flank; and (3) the 1500 m lowering between San Pedro and La Pastora. This deformation is associated to the NNE-SSW compressional stage (fig. 5; Ve03–12), which appears also in other areas of the northeastern Andes (figs. 5, 9). The allochthonous deformation West of El Tocuyo (figs. 3, 6), the Caribbean allochthonous, Upper Cretaceous in age (Barquisimeto Fm.), associated to the Paleocene-Eocene Morán Fm. is juxtaposed to the Andean autochthonous along vertical or sub-horizontal faults (fig. 6, 7). The Andean series are composed of the Peñas Altas and La Luna Fms. The Morán Fm. is highly folded comparatively to the underlying Cretaceous deposits. Moreover, since the intermediate deposits (Colon, Humocaro and Quebrada Arriba Fms.) do not outcrop, we interpret that the Morán Fm. is allochthonous in this area. To the south, in the Humocaro area, the Morán Fm. is slightly deformed and rests conformably upon the Quebrada Arriba Fm., showing that it is autochthonous in this southern area. In the El Tocuyo area, the Barquisimeto Fm. is represented as olistolites involved in the Morán Fm. (fig. 7B). In the Barquisimeto Fm., we observed N070°E- to N140°E-trending folds (fig. 8) with sub-horizontal axes that formed during the emplacement of the Caribbean overthrusts. These folds were reactivated during the Andean stage into recumbent folds trending N175°E to N050°E. In both the Barquisimeto and Morán Fms., we observed N000°– to N035°E-trending folds that can be sorted into two units corresponding (1) to sub-horizontal axes (plunges from 5°to 30°to the north) associated to a fracture or crenulation cleavage; and (2) to upright (45°to 64°to the north) axes. High-grade deformation develops at the bottom of the sedimentary units, showing that folding is related to ESE-ward displacement of these two formations. The upright fold axes, only observed on the borders of the El Tocuyo plain, characterize strike-slip motion of sub-meridian faults bounding this basin. Flat lying plains develop east and west of the northeastern Andes (figs. 3, 6, 7) and constitute an abrupt change in the topography. Our analysis of satellite imagery complemented by field observations show that the El Tocuyo plain (fig. 6) may be interpreted as a pull-apart basin that initiated along a left-lateral fault relay trending N000°E. The synclinal-like morphology of the basin results from the progressive breaking of the western fault, that locally buckles before vanishing in the south (fig. 7). This geometry greatly resembles to that of extensional forced folds initiating at the borders of grabens. Here, this deformation is associated to the NW-SE compressionnal Andean stage (fig. 9, VE01–49, VE02–54). Conclusions The northeastern part of the Mérida Andes recorded several tectonic stages that can be described as follows: – (1) the Jurassic rifting, corresponding to the formation of NE-trending grabens filled by La Quinta Fm.; – (2) the Caribbean orogen (upper Cretaceous-early Oligocene) associated with the emplacement of Caribbean overthrusts. The front of some units (Barquisimeto Fm.) can be partly involved into the Paleocene-Eocene Morán Fm. This stage is characterized by N070°E- to N150°E-trending folds; – (3) an ESE-WNW compression older than the middle Miocene, that may correspond to the N105°E-trending stage of Stéphan [1982], and related to ESE-ward displacement of the Morán Fm. and the Caribbean units; – (4) the NW- to NNW-directed Andean compression lasting from middle Miocene onwards. It is responsible for the formation of NE-SW folds, sometimes related to reactivation of the Jurassic grabens (Humocaro anticline); – (5) a NNE-SSW compression, younger than the Andean compression, and responsible for N-S right-lateral strike-slip faulting and NE-SW left-lateral strike-slip faulting. Relays along strike-slip faults locally created transtensional or transpressional areas, which localized flower structures (Barbacoas area for instance) and pull-apart basins (La Pastora) respectively. Important lowering along the pull-apart basins created the buckling of the sedimentary cover responsible for the formation of extensional forced folds. Near NE-SW strike-slip faults, the stress turns anti-clockwise to strike N100°E. North of the Boconó fault and east of the Valera fault, the Trujillo block [Hervouët et al., 2001] is composed of several compartments separated by sub-meridian left-lateral strike-slip faults. Our analysis of satellite imagery, structural observations in the field and slip vectors derived from focal mechanisms of earthquakes [Dhont et al., 2002; 2004] show that the Trujillo block tectonically escapes towards the north or north-east. However, between El Empedrado fault and Bocono fault, in front of the Carribean overthrusts, numerous focal mechanisms of earthquakes and structural observations in the field indicate that the Andean compressional stage is relieved by a NNE-SSW compression. North of the Trujillo block, the Caribbean overthrusts act as a barrier for the escape of this triangular block towards the north-east (fig. 1C).

ABSTRACTWe report preliminary results of descriptive research, with field design to identify and evaluate the use of Infor-mation and Communication Technologies (ICT) in physics laboratories of universities, public and private, in the state of Trujillo Venezuela, based pilot study center at the Universityof Los Andes, Faculty Rafael Rangel degree in Physical Educa-tion and Mathematics. Regarding the use of technology platforms, virtual environments and interactive teaching materials as an auxiliary tool in the teaching-learning process provided for students and teachers, such as software, simulators, blog, websites, forums, emails, videos, presentations, and more. We applied a survey type instrument with open and closed questionswith a numerical rating scale, questionnaires with multiple choice answers to students and teachers in physics laboratories and instrument of observation and evaluation of interactive tools used. With the obtained results confirm the relevance of the work preliminary hypothesis is generally established the reliability and validity of the data collection instruments.RESUMENSe reportan los resultados preliminares de la investigación de tipo descriptiva, con diseño de campo para identificar y evaluar el uso de las Tecnologías en Información y Comunicación (TIC) en los laboratorios de Física de las universidades, públicas y privadas, en el Estado Trujillo Venezuela, tomando como centro piloto del estudio la Universidad de Los Andes, Núcleo Rafael Rangel en la carrera de Educación Física y Matemática. En lo concerniente a la utilización de las plataformas tecnológicas, ambientes virtuales y el material didáctico interactivo como herramienta auxiliar en el proceso de enseñanza-aprendizaje dispuesto para los estudiantes y profesores, tales como software, simuladores, blog, páginas web, foros, correos electrónicos, videos, presentaciones, entre otros. Se aplicó un instrumento tipo encuesta con preguntas abiertas y cerradas con una escala de estimación numérica, cuestionarios con respuestas de elección múltiples a los estudiantes y docentes en los labo-ratorios de Física y un instrumento de observación y evaluación de las herramientas interactivas utilizadas. Con los resultados obtenidos se confirman la pertinencia de las hipótesis preliminares del trabajo general, se establece la confiabilidad y validación de los instrumentos de recolección de datos.

ABSTRACTConsidering the hypothesis that the integration of ICT in Venezuelan universities, especially to the process of teaching/ learning, curricula or teaching practices, it has not been rapid, uniform, stable and satisfying, this research wasconducted to determine the current state of progress in its incorporation through multiple channels, means and resources that constitute the higher education institutions of Trujillo state, according to a set of indicators. In this descriptive research, are explored by a design field, from the Manual for the Measurement of Information Technology and Communication in Education Institute for Statistics (2009) and according to the vision derived by Sunkel (2006), consultant to the Economic Commission for Latin America and the Caribbean (ECLAC), the following categories of indicators: (a) policy and strategy, (b) infrastructure and access, (c) Training of teachers (d) Integration into the curriculum and (e) students learning. The results indicate significant misalignments in the process, that correlate with the type of institution, the attitude and training of teachers and students, as well as deficiencies in infrastructure and technology resourcesRESUMENConsiderando la hipótesis que la integración de las TIC a las universidades venezolanas, especialmente a los procesos de enseñanza/aprendizaje, currículos o prácticas pedagógicas, no ha sido rápida, uniforme, estable y satisfactoria, se realizó esta investigación para determinar el estado actual de avance en su incorporación, mediante los múltiples cana-les, medios y recursos que las constituyen, a las instituciones de educación universitaria del estado Trujillo, de acuerdo a un conjunto de indicadores. En esta investigación de tipo descriptivo, se exploran con un diseño de campo, a partir del Manual para la Medición de las Tecnologías de la Información y la Comunicación en Educación del Instituto de Estadística de la UNESCO (2009) y de acuerdo a la visión derivada por Sunkel (2006), consultor de la Comisión Económica para América Latina y el Caribe (CEPAL), las siguientes categorías de indicadores: (a) Política y estrategia, (b) Infraestructura y acceso, (c) Capacitación de los profesores, (d) Integración en el currículum y (e) Aprendizaje de los estudiantes. Los resultados indican desajustes importantes en el proceso, que guardan correlación con el tipo de institución, la actitud y capacitación de los profesores y estudiantes, así como con las deficiencias en infraestructura y recursos tecnológicos.