Exploring nu signals in dark matter detectors

We investigate standard and non-standard solar neutrino signals in direct dark matter detection experiments. It is well known that even without new physics, scattering of solar neutrinos on nuclei or electrons is an irreducible background for direct dark matter searches, once these experiments reach the ton scale. Here, we entertain the possibility that neutrino interactions are enhanced by new physics, such as new light force carriers (for instance a "dark photon") or neutrino magnetic moments. We consider models with only the three standard neutrino flavors, as well as scenarios with extra sterile neutrinos. We find that low-energy neutrino-electron and neutrino-nucleus scattering rates can be enhanced by several orders of magnitude, potentially enough to explain the event excesses observed in CoGeNT and CRESST. We also investigate temporal modulation in these neutrino signals, which can arise from geometric effects, oscillation physics, non-standard neutrino energy loss, and direction-dependent detection efficiencies. We emphasize that, in addition to providing potential explanations for existing signals, models featuring new physics in the neutrino sector can also be very relevant to future dark matter searches, where, on the one hand, they can be probed and constrained, but on the other hand, their signatures could also be confused with dark matter signals.

Global gene expression profiling of oral cavity cancers suggests molecular heterogeneity within anatomic subsites

Abstract Background Oral squamous cell carcinoma (OSCC) is a frequent neoplasm, which is usually aggressive and has unpredictable biological behavior and unfavorable prognosis. The comprehension of the molecular basis of this variability should lead to the development of targeted therapies as well as to improvements in specificity and sensitivity of diagnosis. Results Samples of primary OSCCs and their corresponding surgical margins were obtained from male patients during surgery and their gene expression profiles were screened using whole-genome microarray technology. Hierarchical clustering and Principal Components Analysis were used for data visualization and One-way Analysis of Variance was used to identify differentially expressed genes. Samples clustered mostly according to disease subsite, suggesting molecular heterogeneity within tumor stages. In order to corroborate our results, two publicly available datasets of microarray experiments were assessed. We found significant molecular differences between OSCC anatomic subsites concerning groups of genes presently or potentially important for drug development, including mRNA processing, cytoskeleton organization and biogenesis, metabolic process, cell cycle and apoptosis. Conclusion Our results corroborate literature data on molecular heterogeneity of OSCCs. Differences between disease subsites and among samples belonging to the same TNM class highlight the importance of gene expression-based classification and challenge the development of targeted therapies.

Functional characterisation of the non-essential protein kinases and phosphatases regulating Aspergillus nidulans hydrolytic enzyme production

Abstract Background Despite recent advances in the understanding of lignocellulolytic enzyme regulation, less is known about how different carbon sources are sensed and the signaling cascades that result in the adaptation of cellular metabolism and hydrolase secretion. Therefore, the role played by non-essential protein kinases (NPK) and phosphatases (NPP) in the sensing of carbon and/or energetic status was investigated in the model filamentous fungus Aspergillus nidulans. Results Eleven NPKs and seven NPPs were identified as being involved in cellulase, and in some cases also hemicellulase, production in A. nidulans. The regulation of CreA-mediated carbon catabolite repression (CCR) in the parental strain was determined by fluorescence microscopy, utilising a CreA: GFP fusion protein. The sensing of phosphorylated glucose, via the RAS signalling pathway induced CreA repression, while carbon starvation resulted in derepression. Growth on cellulose represented carbon starvation and derepressing conditions. The involvement of the identified NPKs in the regulation of cellulose-induced responses and CreA derepression was assessed by genome-wide transcriptomics (GEO accession 47810). CreA:GFP localisation and the restoration of endocellulase activity via the introduction of the ∆creA mutation, was assessed in the NPK-deficient backgrounds. The absence of either the schA or snfA kinase dramatically reduced cellulose-induced transcriptional responses, including the expression of hydrolytic enzymes and transporters. The mechanism by which these two NPKs controlled gene transcription was identified, as the NPK-deficient mutants were not able to unlock CreA-mediated carbon catabolite repression under derepressing conditions, such as carbon starvation or growth on cellulose. Conclusions Collectively, this study identified multiple kinases and phosphatases involved in the sensing of carbon and/or energetic status, while demonstrating the overlapping, synergistic roles of schA and snfA in the regulation of CreA derepression and hydrolytic enzyme production in A. nidulans. The importance of a carbon starvation-induced signal for CreA derepression, permitting transcriptional activator binding, appeared paramount for hydrolase secretion.

Sensing the "LUV" with HST+COS in Cycle 20 and beyond

New Cosmic Origins Spectrograph (COS) observing modes have extended the Hubble Space Telescope's spectral range to wavelengths between 900-1150 Å. However, the G140L/1280 and the Cycle 19 available G130M central wavelengths (1055 and 1096) that sample below 1150 Å were only available at focus positions which provided low-resolution (R<3,000). For HST Cycle 20, we introduced a new G130M/1222 central wavelength that covers 1065-1365 Å with R>10,000 everywhere, but optimized for 15000 from 1080-1200 Å. This mode places geo-coronal Lyα between the COS FUV detector segments to minimize detector gain sag. Also for Cycle 20, the resolution of the G130M/1055 and 1096 modes will be increased by a factor of 3-4 by optimizing the focus positions for these modes. This will give HST approximately the effective area of FUSE over the FUSE bandpass at 10,000. Here we present the current calibration status of the COS G130M/1055, 1096, and 1222 central wavelength settings at the original and second FUV lifetime positions with an emphasis on observing over the "Lyman UV", or "LUV", 912-1216 Å.

Estudios tafonómicos en foraminíferos bentónicos como proxy de hidrodinámica y sedimentología en el gradiente Río de La Plata – Océano Atlántico Sur Occidental

Los foraminíferos bentónicos representan un excelente proxy geológico, ya que sus caparazones son incorporados en el sedimento y pasan a comportarse como granos sedimentares durante los eventos de transporte y erosión, permitiendo así, el registro de condiciones y eventos que ocurren en los océanos. De este modo, son usados para describir patrones de hidrodinámica y evaluar índices de deposición, erosión y retrabajamiento del sedimento en los ambientes marinos. Concretamente, las regiones costeras representan zonas de alta complejidad ambiental, debido a que en ellas se da la mezcla de agua tanto de origen continental como marino, y a su vez, al efecto de la descarga fluvial que aporta material particulado del continente para el océano. El Río de la Plata (RdLP) representa el cuarto mayor estuario del mundo y el segundo del continente americano, lo cual convierte al sistema RdLP-Océano Atlántico en un complejo gradiente estuarino de interés en estudios sedimentológicos con posteriores aplicaciones paleo-climáticas y paleo-ecológicas del Cuaternario Superior. En el presente estudio, se registra a partir de las asociaciones muertas, para la región del estuario entrada de agua marina hasta la zona del frente termohalino. Dichas asociaciones se caracterizaron por especies típicas de plataforma y aguas frías. La región marina del RdlP registró los mayores porcentajes de abrasión y fragmentación de caparazones, indicando una zona de alta energía. Por otro lado, en la región más oceánica las asociaciones muertas reflejaron un transporte en dirección norte, influenciado por la pluma del RdlP. Cabe resaltar la presencia en esta región de una isla barrera, vestigio de una paleo-costa producto de una regresión Holocénica. Este local se caracterizó por un aumento de la abrasión y fragmentación mostrando la gran hidrodinámica presente. En todos los casos existió correlación entre las señales tafonómicas y los datos geo-químicos (sedimentología, pH, oxígeno disuelto, carbono orgánico y nitrógeno total)

Estudios tafonómicos en foraminíferos bentónicos como proxy de hidrodinámica y sedimentología en el gradiente Río de La Plata – Océano Atlántico Sur Occidental

Los foraminíferos bentónicos representan un excelente proxy geológico, ya que sus caparazones son incorporados en el sedimento y pasan a comportarse como granos sedimentares durante los eventos de transporte y erosión, permitiendo así, el registro de condiciones y eventos que ocurren en los océanos. De este modo, son usados para describir patrones de hidrodinámica y evaluar índices de deposición, erosión y retrabajamiento del sedimento en los ambientes marinos. Concretamente, las regiones costeras representan zonas de alta complejidad ambiental, debido a que en ellas se da la mezcla de agua tanto de origen continental como marino, y a su vez, al efecto de la descarga fluvial que aporta material particulado del continente para el océano. El Río de la Plata (RdLP) representa el cuarto mayor estuario del mundo y el segundo del continente americano, lo cual convierte al sistema RdLP-Océano Atlántico en un complejo gradiente estuarino de interés en estudios sedimentológicos con posteriores aplicaciones paleo-climáticas y paleo-ecológicas del Cuaternario Superior. En el presente estudio, se registra a partir de las asociaciones muertas, para la región del estuario entrada de agua marina hasta la zona del frente termohalino. Dichas asociaciones se caracterizaron por especies típicas de plataforma y aguas frías. La región marina del RdlP registró los mayores porcentajes de abrasión y fragmentación de caparazones, indicando una zona de alta energía. Por otro lado, en la región más oceánica las asociaciones muertas reflejaron un transporte en dirección norte, influenciado por la pluma del RdlP. Cabe resaltar la presencia en esta región de una isla barrera, vestigio de una paleo-costa producto de una regresión Holocénica. Este local se caracterizó por un aumento de la abrasión y fragmentación mostrando la gran hidrodinámica presente. En todos los casos existió correlación entre las señales tafonómicas y los datos geo-químicos (sedimentología, pH, oxígeno disuelto, carbono orgánico y nitrógeno total).