3,574 research outputs found

    The Betic Ophiolites and the Mesozoic Evolution of the Western Tethys

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    The Betic Ophiolites consist of numerous tectonic slices, metric to kilometric in size, of eclogitized mafic and ultramafic rocks associated to oceanic metasediments, deriving from the Betic oceanic domain. The outcrop of these ophiolites is aligned along 250 km in the Mulhacen Complex of the Nevado-Filabride Domain, located at the center-eastern zone of the Betic Cordillera (SE Spain). According to petrological/geochemical inferences and SHRIMP (Sensitive High Resolution Ion Micro-Probe) dating of igneous zircons, the Betic oceanic lithosphere originated along an ultra-slow mid-ocean ridge, after rifting, thinning and breakup of the preexisting continental crust. The Betic oceanic sector, located at the westernmost end of the Tethys Ocean, developed from the Lower to Middle Jurassic (185-170 Ma), just at the beginning of the Pangaea break-up between the Iberia-European and the Africa-Adrian plates. Subsequently, the oceanic spreading migrated northeastward to form the Ligurian and Alpine Tethys oceans, from 165 to 140 Ma. Breakup and oceanization isolated continental remnants, known as the Mesomediterranean Terrane, which were deformed and affected by the Upper Cretaceous-Paleocene Eo-Alpine high-pressure metamorphic event, due to the intra-oceanic subduction of the Jurassic oceanic lithosphere and the related continental margins. This process was followed by the partial exhumation of the subducted oceanic rocks onto their continental margins, forming the Betic and Alpine Ophiolites. Subsequently, along the Upper Oligocene and Miocene, the deformed and metamorphosed Mesomediterranean Terrane was dismembered into different continental blocks collectively known as AlKaPeCa microplate (Alboran, Kabylian, Peloritan and Calabrian). In particular, the Alboran block was displaced toward the SW to occupy its current setting between the Iberian and African plates, due to the Neogene opening of the Algero-Provencal Basin. During this translation, the different domains of the Alboran microplate, forming the Internal Zones of the Betic and Rifean Cordilleras, collided with the External Zones representing the Iberian and African margins and, together with them, underwent the later alpine deformation and metamorphism, characterized by local differences of P-T (Pressure-Temperature) conditions. These Neogene metamorphic processes, known as Meso-Alpine and Neo-Alpine events, developed in the Nevado-Filabride Domain under Ab-Ep amphibolite and greenschists facies conditions, respectively, causing retrogradation and intensive deformation of the Eo-Alpine eclogites.This research was funded by Project CGL2009-12369 of the Spanish Ministry of Science and Innovation, co-financed with FEDER funds, and by Research Group RNM 333 of Junta de AndalucĂ­a (Spain)

    Status in Diffuse Large B Cell Lymphoma not otherwise specified: A single center study from Argentina

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    BackgroundDiffuse large B-cell Lymphoma (DLBCL) is a heterogeneous disease. Based on Hans? algorithm, DLBCL not otherwise specified (NOS) is classified by cell-of-origin into germinal center B-cell (GCB) and non-GCB subtypes. Non-GCB ones have frequently NF-kB pathway activation and worse prognosis compared to GCB cases. MYD88 is an adaptor protein of toll-like and IL-1 receptor signalling, leading downstream NF-kB pathway activation. MYD88 L265P mutation confers the protein constitutional activation. This mutation is present in around 20% of non-GCB subtype, and rarely found in GCB subtype of DLBCL. The prognostic value of MYD88 L265P mutation in DLBCL has been matter of controversy.AimsThe aim of the study was to determine the prevalence of MYD88 L265P mutation in DLBCL NOS cases of Argentina, and compare it with previous reports in the literature.MethodsA retrospective cohort of 73 DLBCL NOS cases diagnosed in the Italian Hospital of Buenos Aires (Argentina) between 2010 and 2016 was studied. Complete clinical records, Hans? algorithm, and available material for molecular testing were inclusion criteria. Patients with prior diagnosis of low-grade lymphoma or diagnosis of immunodeficiency-associated, post-transplant, EBV+, primary mediastinal, primary testicular, primary CNS, primary effusion, leg-type or intravascular DLBCL were excluded. DNA was extracted from tissue blocks using QIAamp mini kit (Qiagen). MYD88 L265P was assessed using an in-house allele-specific probe-based Real-Time PCR assay. Positive (primary testicular DLBCL) and negative controls (tonsil) were added to each run. Every case was checked subsequently using qBiomarker MYD88 L265P Somatic Mutation Assay (Qiagen). Prevalences were expressed as percentage, confident intervals were calculated using Clopper-Pearson exact method. Kaplan Meier curves and Log-rank test were used to evaluate overall survival (OS).Results36 patients (49,31%) were female, and median age at diagnosis was 66 years (range 26-89). 33 patients (45,20%) had extranodal involvement (gastrointestinal tract: 14 cases; liver: 5 cases; bone: 4 cases; other locations: 10 cases). 44 cases (60,27%) were GCB and 29 (39,73%) were non-GCB DLBCLs. MYD88 L265P mutation was present in 2 cases (2,74% ; CI 95%: 0,33-9,55%) among all DLBCLs, including 1 GCB case (2,27% ; CI 95%: 0,06-12,02%) and 1 non-GCB case (3,45% ; CI 95%: 0,09-17.76%). There was no significant association between MYD88 L265P status, HansÂŽalgorithm subtype, sex, age or Ki67 index and OS.ConclusionIn the analyzed population, the prevalence of GCB and non-GCB subtypes among DLBCL NOS cases was similar to international reports, although we did not find significant difference between both groups regarding OS (p=0,712). MYD88 L265P mutation was found only in 2 patients (1 GCB and 1 non-GCB), accounting for 2,74% (CI 95%: 0,33-9,55%) and 2,27% (CI 95%: 0,06-12,02%) of all DLBCL NOS and non-GCB cases, respectively. Both prevalences are significantly lower than those published in 2017 by Lee et al. in a meta-analysis, where they found that MYD88 L265P is present in 16% (CI 95%: 15-18,09%) and 20,63% (CI 95%: 18,41-23%) of patients among all DLBCLs and non-GCB subtype, respectively. However, MYD88 L265P prevalence in primary SNC, testicular and leg-type DLBCLs diagnosed in our institution are similar to the literature (data not shown).Fil: Jauk, Federico. Hospital Italiano; ArgentinaFil: Kohan, Dana. Hospital Italiano; ArgentinaFil: Ortega, Leandro Ismael. Hospital Italiano; Argentina. Consejo Nacional de Investigaciones CientĂ­ficas y TĂ©cnicas; ArgentinaFil: Diaz de Arce, Heidy. Hospital Italiano; ArgentinaFil: Cristaldo, Nancy. Hospital Italiano; ArgentinaFil: RANUNCOLO, Stella Maris. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Oficina de Coordinacion Administrativa Houssay. Instituto de Medicina Traslacional E Ingenieria Biomedica. - Hospital Italiano. Instituto de Medicina Traslacional E Ingenieria Biomedica. - Instituto Universitario Hospital Italiano de Buenos Aires. Instituto de Medicina Traslacional E Ingenieria Biomedica.; ArgentinaFil: Warley, Fernando. Hospital Italiano; ArgentinaFil: Otero, Victoria. Hospital Italiano; ArgentinaFil: Garcia Rivello, Hernan Jorge. Hospital Italiano; Argentina24th Congress of the European Hematology AssociationAmsterdamHolandaEscuela Europea de HematologĂ­

    Database Models and Data Formats

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    The deliverable describes data structure and XML formats that have been investigated and defined for data representation of linguistic and semantic resources underlying the KYOTO system

    Increased Antibacterial and Antibiofilm Properties of Silver Nanoparticles Using Silver Fluoride as Precursor.

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    Silver nanoparticles were produced with AgF as the starting Ag(I) salt, with pectin as the reductant and protecting agent. While the obtained nanoparticles (pAgNP-F) have the same dimensional and physicochemical properties as those already described by us and obtained from AgNO3 and pectin (pAgNP-N), the silver nanoparticles from AgF display an increased antibacterial activity against E. coli PHL628 and Staphylococcus epidermidis RP62A (S. epidermidis RP62A), both as planktonic strains and as their biofilms with respect to pAgNP-N. In particular, a comparison of the antimicrobial and antibiofilm action of pAgNP-F has been carried out with pAgNP-N, pAgNP-N and added NaF, pure AgNO3, pure AgF, AgNO3 and added NaF and pure NaNO3 and NaF salts. By also measuring the concentration of the Ag+ cation released by pAgNP-F and pAgNP-N, we were able to unravel the separate contributions of each potential antibacterial agent, observing an evident synergy between p-AgNP and the F- anion: the F- anion increases the antibacterial power of the p-AgNP solutions even when F- is just 10 ”M, a concentration at which F- alone (i.e., as its Na+ salt) is completely ineffective

    Measurement of the cosmic ray spectrum above 4×10184{\times}10^{18} eV using inclined events detected with the Pierre Auger Observatory

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    A measurement of the cosmic-ray spectrum for energies exceeding 4×10184{\times}10^{18} eV is presented, which is based on the analysis of showers with zenith angles greater than 60∘60^{\circ} detected with the Pierre Auger Observatory between 1 January 2004 and 31 December 2013. The measured spectrum confirms a flux suppression at the highest energies. Above 5.3×10185.3{\times}10^{18} eV, the "ankle", the flux can be described by a power law E−γE^{-\gamma} with index Îł=2.70±0.02 (stat)±0.1 (sys)\gamma=2.70 \pm 0.02 \,\text{(stat)} \pm 0.1\,\text{(sys)} followed by a smooth suppression region. For the energy (EsE_\text{s}) at which the spectral flux has fallen to one-half of its extrapolated value in the absence of suppression, we find Es=(5.12±0.25 (stat)−1.2+1.0 (sys))×1019E_\text{s}=(5.12\pm0.25\,\text{(stat)}^{+1.0}_{-1.2}\,\text{(sys)}){\times}10^{19} eV.Comment: Replaced with published version. Added journal reference and DO

    Energy Estimation of Cosmic Rays with the Engineering Radio Array of the Pierre Auger Observatory

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    The Auger Engineering Radio Array (AERA) is part of the Pierre Auger Observatory and is used to detect the radio emission of cosmic-ray air showers. These observations are compared to the data of the surface detector stations of the Observatory, which provide well-calibrated information on the cosmic-ray energies and arrival directions. The response of the radio stations in the 30 to 80 MHz regime has been thoroughly calibrated to enable the reconstruction of the incoming electric field. For the latter, the energy deposit per area is determined from the radio pulses at each observer position and is interpolated using a two-dimensional function that takes into account signal asymmetries due to interference between the geomagnetic and charge-excess emission components. The spatial integral over the signal distribution gives a direct measurement of the energy transferred from the primary cosmic ray into radio emission in the AERA frequency range. We measure 15.8 MeV of radiation energy for a 1 EeV air shower arriving perpendicularly to the geomagnetic field. This radiation energy -- corrected for geometrical effects -- is used as a cosmic-ray energy estimator. Performing an absolute energy calibration against the surface-detector information, we observe that this radio-energy estimator scales quadratically with the cosmic-ray energy as expected for coherent emission. We find an energy resolution of the radio reconstruction of 22% for the data set and 17% for a high-quality subset containing only events with at least five radio stations with signal.Comment: Replaced with published version. Added journal reference and DO

    Measurement of the Radiation Energy in the Radio Signal of Extensive Air Showers as a Universal Estimator of Cosmic-Ray Energy

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    We measure the energy emitted by extensive air showers in the form of radio emission in the frequency range from 30 to 80 MHz. Exploiting the accurate energy scale of the Pierre Auger Observatory, we obtain a radiation energy of 15.8 \pm 0.7 (stat) \pm 6.7 (sys) MeV for cosmic rays with an energy of 1 EeV arriving perpendicularly to a geomagnetic field of 0.24 G, scaling quadratically with the cosmic-ray energy. A comparison with predictions from state-of-the-art first-principle calculations shows agreement with our measurement. The radiation energy provides direct access to the calorimetric energy in the electromagnetic cascade of extensive air showers. Comparison with our result thus allows the direct calibration of any cosmic-ray radio detector against the well-established energy scale of the Pierre Auger Observatory.Comment: Replaced with published version. Added journal reference and DOI. Supplemental material in the ancillary file
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