Chromosome fusions triggered by noncoding RNA

Chromosomal fusions are common in normal and cancer cells and can produce aberrant gene products that promote transformation. The mechanisms driving these fusions are poorly understood, but recurrent fusions are widespread. This suggests an underlying mechanism, and some authors have proposed a possible role for RNA in this process. The unicellular eukaryote Oxytricha trifallax displays an exorbitant capacity for natural genome editing, when it rewrites its germline genome to form a somatic epigenome. This developmental process provides a powerful model system to directly test the influence of small noncoding RNAs on chromosome fusion events during somatic differentiation. Here we show that small RNAs are capable of inducing chromosome fusions in four distinct cases (out of four tested), including one fusion of three chromosomes. We further show that these RNA-mediated chromosome fusions are heritable over multiple sexual generations and that transmission of the acquired fusion is associated with endogenous production of novel piRNA molecules that target the fused junction. We also demonstrate the capacity of a long noncoding RNA (lncRNA) to induce chromosome fusion of two distal germline loci. These results underscore the ability of short-lived, aberrant RNAs to act as drivers of chromosome fusion events that can be stably transmitted to future generations.

Climate and soil characteristics and soil arthropod abundance on Anchorage, Signy and Falkland Islands

Over a 2-year study, we investigated the effect of environmental change on the diversity and abundance of soil arthropod communities (Acari and Collembola) in the Maritime Antarctic and the Falkland Islands. Open Top Chambers (OTCs), as used extensively in the framework of the northern boreal International Tundra Experiment (ITEX), were used to increase the temperature in contrasting communities on three islands along a latitudinal temperature gradient, ranging from the Falkland Islands (51°S, mean annual temperature 7.5 °C) to Signy Island (60°S, -2.3°C) and Anchorage Island (67°S, -3.8°C). At each island an open and a closed plant community were studied: lichen vs. moss at the Antarctic sites, and grass vs. dwarf shrub at the Falkland Islands. The OTCs raised the soil surface temperature during most months of the year. During the summer the level of warming achieved was 1.7 °C at the Falkland Islands, 0.7 °C at Signy Island, and 1.1 °C at Anchorage Island. The native arthropod community diversity decreased with increasing latitude. In contrast with this pattern, Collembola abundance in the closed vegetation (dwarf shrub or moss) communities increased by at least an order of magnitude from the Falkland Islands (9.0 +/- 2 x 10**3 ind./m**2) to Signy (3.3 +/- 8.0 x 10**4 ind./m**2) and Anchorage Island (3.1 +/- 0.82 x 10**5 ind./m**2). The abundance of Acari did not show a latitudinal trend. Abundance and diversity of Acari and Collembola were unaffected by the warming treatment on the Falkland Islands and Anchorage Island. However, after two seasons of experimental warming, the total abundance of Collembola decreased (p < 0.05) in the lichen community on Signy Island as a result of the population decline of the isotomid Cryptopygus antarcticus. In the same lichen community there was also a decline (p < 0.05) of the mesostigmatid predatory mite Gamasellus racovitzai, and a significant increase in the total number of Prostigmata. Overall, our data suggest that the consequences of an experimental temperature increase of 1-2°C, comparable to the magnitude currently seen through recent climate change in the Antarctic Peninsula region, on soil arthropod communities in this region may not be similar for each location but is most likely to be small and initially slow to develop.

Establecimiento y desarrollo en el cultivo forzado de tomate : aplicación de dosis variables de fitorreguladores.

Las hormonas vegetales son capaces de controlar el desarrollo reproductivo, desde la diferenciación floral hasta los últimos estadios del desarrollo de los frutos. En particular, la etapa de fructificación y desarrollo depende del contenido endógeno de estas sustancias, y es posible manipular la iniciación del desarrollo del fruto por aplicación externa de hormonas. Previamente se evaluó el proceso de fructificación y desarrollo en el cultivo de tomate en invernadero en respuesta a la aplicación de b-NOA y AG3 en dosis fijas: se observó sensibilidad diferencial dependiendo del genotipo y tipo de regulador. El objetivo de este trabajo fue establecer dosis y momento óptimo para la aplicación de b-NOA y AG3 como formas de mejorar la fructificación y el desarrollo de frutos partenocárpicos. Como factores se consideraron tipo de regulador -b-NOA y AG3- en dosis y momentos de aplicación variables. Empleando ovarios no polinizados como sistema experimental fue posible concluir que la aplicación de 40 ppm de b-NOA a 7 días post antesis ofrece las mayores ventajas desde el punto de vista del rendimiento y menor impacto fisiológico, sin alterar el período de desarrollo de los frutos.

Thermal conductivity at DSDP Leg 60 Holes

A total of 1547 thermal conductivity values were determined by both the NP (needle probe method) and the QTM (quick thermal conductivity meter) on 1319 samples recovered during DSDP Leg 60. The NP method is primarily for the measurement of soft sedimentary samples, and the result is free from the effect of porewater evaporation. Measurement by the QTM method is faster and is applicable to all types of samples-namely, sediments (soft, semilithified, and lithified) and basement rocks. Data from the deep holes at Sites 453, 458, and 459 show that the thermal conductivity increases with depth, the rate of increase ranging from (0.18 mcal/cm s °C)/100 m at Site 459 to (0.72 mcal/cm s °C)/100 m at Site 456. A positive correlation between the sedimentary accumulation rate and the rate of thermal conductivity increase with depth indicates that both compaction and lithification are important factors. Drilled pillow basalts show nearly uniform thermal conductivity. At She 454 the thermal conductivity of one basaltic flow unit was higher near the center of the unit and lower toward the margin, reflecting variable vesicularity. Hydrothermally altered basalts at Site 456 showed higher thermal conductivity than fresh basalt because secondary calcite, quartz, and pyrite are generally more thermally conductive than fresh basalt. The average thermal conductivity in the top 50 meters of sediments correlates inversely with water depth because of dissolution of calcite, a mineral with high thermal conductivity, from the sediments as the water depth exceeds the lysocline and the carbonate compensation depth. Differences between the Mariana Trench data and the Mariana Basin and Trough data may reflect different abundances of terrigenous material in the sediment. There are remarkable correlations between thermal conductivity and other physical properties. The relationship between thermal conductivity and compressional wave velocity can be used to infer the ocean crustal thermal conductivity from the seismic velocity structure.

Horizontal profiles of longwave and shortwave radiation components over sea ice near Barrow, Alaska during the 2011 melt

An integrated instrument package for measuring and understanding the surface radiation budget of sea ice is presented, along with results from its first deployment. The setup simultaneously measures broadband fluxes of upwelling and downwelling terrestrial and solar radiation (four components separately), spectral fluxes of incident and reflected solar radiation, and supporting data such as air temperature and humidity, surface temperature, and location (GPS), in addition to photographing the sky and observed surface during each measurement. The instruments are mounted on a small sled, allowing measurements of the radiation budget to be made at many locations in the study area to see the effect of small-scale surface processes on the large-scale radiation budget. Such observations have many applications, from calibration and validation of remote sensing products to improving our understanding of surface processes that affect atmosphere-snow-ice interactions and drive feedbacks, ultimately leading to the potential to improve climate modelling of ice-covered regions of the ocean. The photographs, spectral data, and other observations allow for improved analysis of the broadband data. An example of this is shown by using the observations made during a partly cloudy day, which show erratic variations due to passing clouds, and creating a careful estimate of what the radiation budget along the observed line would have been under uniform sky conditions, clear or overcast. Other data from the setup's first deployment, in June 2011 on fast ice near Point Barrow, Alaska, are also shown; these illustrate the rapid changes of the radiation budget during a cold period that led to refreezing and new snow well into the melt season.

Nd-Sr isotopes in fossil fish debris from IODP Exp302

Strontium and neodymium radiogenic isotope ratios in early to middle Eocene fossil fish debris (ichthyoliths) from Lomonosov Ridge (Integrated Ocean Drilling Program Expedition 302) help constrain water mass compositions in the Eocene Arctic Ocean between 55 and 45 Ma. The inferred paleodepositional setting was a shallow, offshore marine to marginal marine environment with limited connections to surrounding ocean basins. The new data demonstrate that sources of Nd and Sr in fish debris were distinct from each other, consistent with a salinity-stratified water column above Lomonosov Ridge in the Eocene. The 87Sr/86Sr values of ichthyoliths (0.7079 - 0.7087) are more radiogenic than Eocene seawater, requiring brackish to fresh water conditions in the environment where fish metabolized Sr. The 87Sr/86Sr variations probably record changes in the overall balance of river Sr flux to the Eocene Arctic Ocean between 55 and 45 Ma and are used here to reconstruct surface water salinity values. The eNd values of ichthyoliths vary between -5.7 and -7.8, compatible with periodic (or intermittent) supply of Nd to Eocene Arctic intermediate water (AIW) from adjacent seas. Although the Norwegian-Greenland Sea and North Atlantic Ocean were the most likely sources of Eocene AIW Nd, input from the Tethys Sea (via the Turgay Strait in early Eocene time) and the North Pacific Ocean (via a proto-Bering Strait) also contributed.

Historias de vida y desencadenantes emocionales del síndrome coronario agudo : Inicio de un proyecto de investigación en el hospital El Cruce

Las enfermedades cardiovasculares son consideradas la principal causa de muerte de hombres y mujeres en todo el mundo, así como también en nuestro país. Existe en la bibliografía un número identificado de factores de riesgo que incluye el sedentarismo, el consumo de tabaco, una inadecuada dieta alimenticia, el distrés personal y laboral, la tendencia a la ira-hostilidad, la ansiedad y la depresión, los cambios sociales vinculados a los niveles socioeconómicos, y las catástrofes naturales y artificiales. Si bien estos factores de riesgo explican una condición favorable a su aparición, dando cuenta de una enfermedad arterial crónica, la presentación clínica del evento cardiovascular es habitualmente abrupta. Más de la mitad de los pacientes con infarto no son precedidos por patología previa o siquiera síntomas. La literatura científica ha estudiado la activación de los síndromes coronarios agudos, prestando un especial interés a la idea de que los comportamientos y las emociones pueden desencadenar ('gatillar") eventos cardíacos en personas susceptibles. La situación psicológica desencadenante puede ser un acontecimiento aparentemente banal si se la considera y valora de manera objetiva. Sin embargo, su importancia radica en su repercusión psicológica y en la significación que adquiere para el propio paciente en el contexto de sus vivencias actuales y pasadas. La investigación cualitativa aportada por los casos explorados a través de la corriente narrativa en medicina y psicología, y por los casos investigados mediante métodos psicoanalíticos constituyen las fuentes posibles de información acerca de los conflictos recientes vividos por los pacientes con síndrome coronario agudo. Objetivos y metodología: En el Servicio de Cardiología del Hospital de Alta Complejidad en Red 'El Cruce', de Florencio Varela, hemos comenzado a desarrollar un proyecto de investigación clínica con el propósito de evaluar en una serie de pacientes ingresados con diagnóstico confirmado de infarto agudo de miocardio o angina inestable, la prevalencia de situaciones emocionales negativas intensas estereotípicas en las horas o días previos al evento coronario. Para tal objetivo son realizadas entrevistas semidirigidas a cargo de un profesional psicólogo, a pacientes menores de 65 años de edad, en las cuales se toma en especial consideración el relato de la historia de vida reciente del paciente junto a posibles situaciones conflictivas previas que puedan acompañar el cuadro coronario agudo, la trama familiar y las personas significativas, el contexto e historia laboral, y la vida sexual del paciente. El estado de conciencia inadecuado para el interrogatorio y la existencia de eventos coronarios previos constituyen los criterios de exclusión para esta investigación. A su vez, se evaluará la correlación entre los hallazgos obtenidos en las entrevistas y una serie de test y cuestionarios reconocidos en la exploración de los factores emocionales en este tipo de pacientes: el Inventario de Hostilidad de Buss-Durkee y el score de situación de ira, la Escala de Depresión y Ansiedad Hospitalaria (HADS), el cuestionario Beck de depresión y el Cuestionario de Eventos Vitales. La reiteración en un porcentaje relevante de los casos de la identificación de la situación conflictiva estereotípica permitiría un avance significativo en esta línea de investigación fisiopatológica y psicológica, la ampliación del conocimiento relativo al síndrome coronario agudo, y facilitaría, a su vez, la elaboración de estrategias psicoterapéuticas orientadas al tratamiento y a la modificación pronóstica de la enfermedad