Genome-wide association studies reveal genomic windows and candidate genes related to fat deposition in chickens.

2016

Identification of CNVs on the genome of Brazilian chicken lines.

2016

Reserva de fluxo coronariano na anemia falciforme

FUNDAMENTO: Pacientes com anemia falciforme (FAL) apresentam freqüentemente episódios de dor precordial, possuem alterações eletrocardiográficas em repouso e exibem alterações da estrutura e das funções cardíacas. OBJETIVO: Avaliar o efeito dos episódios repetitivos de vaso-oclusão sobre a microcirculação coronariana. MÉTODOS: Pacientes estáveis com FAL (n = 10, cinco mulheres, 24,4 + 5,4 anos) foram submetidos a medida das velocidades de fluxo coronariano e da reserva de fluxo coronariano (RFC) na artéria coronária descendente anterior por meio de ecocardiografia transesofágica em estado basal e após hiperemia máxima, obtida com adenosina intravenosa. Esses pacientes foram comparados a pacientes com traço falciforme (TRA, n = 10, cinco mulheres, 27,7 + 3,2 anos), anemia ferropriva (FER, n = 8, oito mulheres, 26,6 + 5,2 anos) e grupo controle (NOR, n = 10, cinco mulheres, 26,3 + 6,3 anos). RESULTADOS: O grupo FAL apresentou aumento das velocidades de fluxo coronariano diastólico (p < 0,01) em estado basal e durante hiperemia máxima (67,3 + 14,0 cm/s e 198,2 + 37,9 cm/s, respectivamente), quando comparado aos três outros grupos (TRA, 34,4 + 11,9 cm/s e 114,7 + 36,4 cm/s; FER, 42,4 + 10,4 cm/s e 141,0 + 18,7 cm/s e NOR, 38,1 + 10,0 cm/s e 126,8 + 24,6 cm/s). Entretanto, a RFC foi normal no grupo FAL (3,0 + 0,7) e comparável (p = 0,70) aos demais grupos (TRA, 3,4 + 0,8; FER, 3,5 + 1,2 e NOR, 3,4 + 0,8). CONCLUSÃO: Apesar de maiores velocidades de fluxo coronariano já em estado basal e também durante hiperemia máxima, a RFC é normal na FAL, o que sugere integridade da microcirculação coronariana. Os episódios de vaso-oclusão não são responsáveis pelos achados cardiológicos da doença.

Flora of Guatemala : families Leguminosae, Geraniaceae, Oxalidaceae, Tropaeolaceae, Linaceae, Erythroxylaceae, Zygophyllaceae, Rutaceae, Simaroubaceae, Burseraceae, Meliaceae, and Malpighiaceae / by Paul C. Standley and Julian A. Steyermark.

v.24:pt.5(1946)

Eight new bats of the genus Rhinolophus.

v.24:no.5(1939)

Quantifying consistency of Event Related Potentials across subjects based on single-trial topographic analysis

Introduction: Non-invasive brain imaging techniques often contrast experimental conditions across a cohort of participants, obfuscating distinctions in individual performance and brain mechanisms that are better characterised by the inter-trial variability. To overcome such limitations, we developed topographic analysis methods for single-trial EEG data [1]. So far this was typically based on time-frequency analysis of single-electrode data or single independent components. The method's efficacy is demonstrated for event-related responses to environmental sounds, hitherto studied at an average event-related potential (ERP) level. Methods: Nine healthy subjects participated to the experiment. Auditory meaningful sounds of common objects were used for a target detection task [2]. On each block, subjects were asked to discriminate target sounds, which were living or man-made auditory objects. Continuous 64-channel EEG was acquired during the task. Two datasets were considered for each subject including single-trial of the two conditions, living and man-made. The analysis comprised two steps. In the first part, a mixture of Gaussians analysis [3] provided representative topographies for each subject. In the second step, conditional probabilities for each Gaussian provided statistical inference on the structure of these topographies across trials, time, and experimental conditions. Similar analysis was conducted at group-level. Results: Results show that the occurrence of each map is structured in time and consistent across trials both at the single-subject and at group level. Conducting separate analyses of ERPs at single-subject and group levels, we could quantify the consistency of identified topographies and their time course of activation within and across participants as well as experimental conditions. A general agreement was found with previous analysis at average ERP level. Conclusions: This novel approach to single-trial analysis promises to have impact on several domains. In clinical research, it gives the possibility to statistically evaluate single-subject data, an essential tool for analysing patients with specific deficits and impairments and their deviation from normative standards. In cognitive neuroscience, it provides a novel tool for understanding behaviour and brain activity interdependencies at both single-subject and at group levels. In basic neurophysiology, it provides a new representation of ERPs and promises to cast light on the mechanisms of its generation and inter-individual variability.

Políticas de encaminamiento tolerantes a fallos

El uso intensivo y prolongado de computadores de altas prestaciones para ejecutar aplicaciones computacionalmente intensivas, sumado al elevado número de elementos que los componen, incrementan drásticamente la probabilidad de ocurrencia de fallos durante su funcionamiento. El objetivo del trabajo es resolver el problema de tolerancia a fallos para redes de interconexión de altas prestaciones, partiendo del diseño de polí­ticas de encaminamiento tolerantes a fallos. Buscamos resolver una determinada cantidad de fallos de enlaces y nodos, considerando sus factores de impacto y probabilidad de aparición. Para ello aprovechamos la redundancia de caminos de comunicación existentes, partiendo desde enfoques de encaminamiento adaptativos capaces de cumplir con las cuatro fases de la tolerancia a fallos: detección del error, contención del daño, recuperación del error, y tratamiento del fallo y continuidad del servicio. La experimentación muestra una degradación de prestaciones menor al 5%. En el futuro, se tratará la pérdida de información en tránsito.

15

Developing a predictive understanding of subsurface flow and transport is complicated by the disparity of scales across which controlling hydrological properties and processes span. Conventional techniques for characterizing hydrogeological properties (such as pumping, slug, and flowmeter tests) typically rely on borehole access to the subsurface. Because their spatial extent is commonly limited to the vicinity near the wellbores, these methods often cannot provide sufficient information to describe key controls on subsurface flow and transport. The field of hydrogeophysics has evolved in recent years to explore the potential that geophysical methods hold for improving the quantification of subsurface properties and processes relevant for hydrological investigations. This chapter is intended to familiarize hydrogeologists and water-resource professionals with the state of the art as well as existing challenges associated with hydrogeophysics. We provide a review of the key components of hydrogeophysical studies, which include: geophysical methods commonly used for shallow subsurface characterization; petrophysical relationships used to link the geophysical properties to hydrological properties and state variables; and estimation or inversion methods used to integrate hydrological and geophysical measurements in a consistent manner. We demonstrate the use of these different geophysical methods, petrophysical relationships, and estimation approaches through several field-scale case studies. Among other applications, the case studies illustrate the use of hydrogeophysical approaches to quantify subsurface architecture that influence flow (such as hydrostratigraphy and preferential pathways); delineate anomalous subsurface fluid bodies (such as contaminant plumes); monitor hydrological processes (such as infiltration, freshwater-seawater interface dynamics, and flow through fractures); and estimate hydrological properties (such as hydraulic conductivity) and state variables (such as water content). The case studies have been chosen to illustrate how hydrogeophysical approaches can yield insights about complex subsurface hydrological processes, provide input that improves flow and transport predictions, and provide quantitative information over field-relevant spatial scales. The chapter concludes by describing existing hydrogeophysical challenges and associated research needs. In particular, we identify the area of quantitative watershed hydrogeophysics as a frontier area, where significant effort is required to advance the estimation of hydrological properties and processes (and their uncertainties) over spatial scales relevant to the management of water resources and contaminants.

Paper del sulfur d'hidrogen com a neurotransmissor a nivell dels sistema nerviòs entèric

Al llarg dels últims anys l’òxid nítric (NO) i el monòxid de carboni (CO) han estat investigats com dos neurotransmissors gasosos del tracte gastrointestinal. Algunes dades demostren que el sulfur d’hidrogen (H2S) podria ser el tercer neurotransmissor gasos a nivell central i perifèric. Objectiu: valorar si el H2S compleix els requisits per ser considerat com el tercer neurotransmissor gasos a nivell del sistema nerviós entèric. Mètodes: la motilitat espontània de preparacions de múscul llis circular de mostres de còlon sigma humà i còlon mig de rata es van determinar in vitro mitjançant la tècnica de banys d’òrgans. El hidrogensulfur de sodi (NaHS) va ser utilitzat com donador de H2S. Resultats: 1- El NaHS va inhibir de forma concentració depenent la motilitat espontània en presència de bloqueig neural amb Tetrodotoxina (TTX 1 μM) (IC50 101±18 μM rata n=10; 329±86 μM humà n=18). 2- Aquesta relaxació es va veure reduïda per ODQ 10 μM, un inhibidor de la guanilat ciclasa, en còlon mig de rata (n=5). En humà a més de ser reduïda per ODQ 10μM (n=6), també ho va ser per SQ 22,536 100 μM (n=10), un inhibidor de l’adenilat ciclasa, i per L-NNA 1 mM (n=8), un inhibidor de la sintesi de NO. 3- En còlon de rata la incubació amb D,L-Propargilglicina 2 mM (PAG), un inhibidor de la síntesi de H2S, va incrementar la motilitat tant en situació control (10,05±2,06 vs 17,46±3,37 g•min-1 AUC, P&0,001, n=10) com en presència de TTX 1μM (14,45±7,28 vs 21,67±10,05 g•min-1 AUC, P&0,01, n=7). Conclusió: el H2S compleix part dels criteris per ser considerat un neurotransmissor gasos inhibitori en el tracte gastrointestinal: la inhibició de la seva síntesi incrementa la motilitat intestinal i la seva addició exògena produeix relaxació de la musculatura llisa intestinal.

Indirect costs of parasitism are shaped by variation in the type of immune challenge and food availability

Parasites can inflict indirect fitness costs to their hosts by eliciting costly immune responses. These costs depend on the type and amount of immunostimulants presented to the host immune system but also on the amount of resources available to fuel host immune responses. Here, we investigated how the relative costs of two different types of immune challenge are modulated by variation in food availability. We injected nestling tawny owls (Strix aluco) with either 10 mu g of phytohaemagglutinin (PHA) or 20 mu g of lipopolysaccharide (LPS), and subsequently raised them under two different food regimes (food-restricted vs. ad libitum). After controlling for food consumption, we found that LPS-injected nestlings lost more body mass than PHA-injected ones only when food-restricted. We also found that body mass gain of owlets fed ad libitum decreased with the intensity of the skin swelling response against LPS, but not PHA. These experimental and correlative results suggest that nestling tawny owls suffered greater immune costs when treated with LPS than PHA, and that variation in the costs of two different types of immune challenge can be exacerbated under conditions of low food availability. Our study highlights the importance of taking into consideration the interplay between host immunity and nutrition in the study of indirect costs of parasitism.

Subduction and obduction processes in the Swiss Alps

The significance of the Brianconnais domain in the Alpine orogen is reviewed in the light of data concerning its collision with the active Adriatic margin and the passive Helvetic margin. The Brianconnais which formerly belonged to the Iberian plate, was located on the northern margin of the Alpine Tethys (Liguro-Piemont ocean) since its opening in the early-Middle Jurassic. Together with the Iberian plate the Brianconnais terrane was separated from the European plate in the Late Jurassic-Early Cretaceous, following the northern Atlantic, Bay of Biscay, Valais ocean opening. This was accompanied by the onset of subduction along the northern margin of Adria and the closure of the Alpine Tethys. Stratigraphic and metamorphic data regarding this subduction and the geohistory of the Brianconnais allows the scenario of subduction-obduction processes during the Late Cretaceous-early Tertiary in the eastern and western Alps to be specified. HP-LT metamorphism record a long-lasting history of oceanic subduction-accretion, followed in the Middle Eocene by the incorporation of the Brianconnais as an exotic terrane into the accretionary prism. Middle to Late Eocene cooling ages of the Brianconnais basement and the presence of pelagic, anorogenic sedimentation lasting until the Middle Eocene on the Brianconnais preclude any sort of collision before that time between this domain and the active Adria margin or the Helvetic margin. This is confirmed by plate reconstructions constrained by magnetic anomalies in the Atlantic domain. Only a small percentage of the former Brianconnais domain was obducted, most of the crust and lithospheric roots were subducted. This applies also to domains formerly belonging to the southern Alpine Tethys margin (Austroalpine-inner Carpathian domain). It is proposed that there was a single Palaeogene subduction zone responsible for the Alpine orogen formation (from northern Spain to the East Carpathians), with the exception of a short-lived Late Cretaceous partial closure of the Valais ocean. Subduction in the western Tethyan domain originated during the closure of the Meliata ocean during the Jurassic incorporating the Austroalpine-Carpathian domain as terranes during the Cretaceous. The subduction zone propagated into the northern margin of Adria and then to the northern margin of the Iberian plate, where it gave birth to the Pyrenean-Provencal orogenic belt. This implies the absence of a separated Cretaceous subduction zone within the Austro-Carpathian Penninic ocean. Collision of Iberia with Europe forced the subduction to jump to the SE margin of Iberia in the Eocene, creating the Apenninic orogenic wedge and inverting the vergence of subduction from south- to north-directed. (C) 1998 Elsevier Science B.V. All rights reserved.