Aaron Lopez papers, undated, 1752-1794, 1846, 1852, 1953.

Contains approximately 6800 manuscripts arranged chronologically by year for years 1752-1794. Approximately 100 are letters received or written by Lopez, his partner and father-in-law, Jacob Rodriguez Rivera, members of his family and company, and commercial agents pertaining to business activities and sailing orders for the captains of various ships. Several also refer to personal matters and acquaintances, including a series of six letters from Silas Cooke of White Hall (Middletown), R.I., to Aaron Lopez, asking his aid in returning a run-away slave (1776). The great majority of the collection consists of account records, bills of sale, orders, shipping agreements, lists of sailors on the various ships, repair records and cargo invoices. Of particular interest are a receipt for payment of a half-year's subscription to the "tzedakah" of Congregation Nefutzei Israel, Newport (1755) and several documents that reveal Lopez as a supplier of kosher meat and other religious articles to people in various parts of the colonies, Surinam, and Jamaica. Also included in this group are copies of sailing lists, documents pertaining to Lopez's naturalization which shed light upon the status of a Jew applying for citizenship in Massachusetts and a check to Lopez from the United States government for a loan made during the Revolutionary War (1779).

Surface Expression and Subunit Specific Control of Steady Protein Levels by the Kv7.2 Helix A-B Linker

12 p.

Joan Benejam i Vives (Ciutadella, 1846-1922). 'Joan Benejam i Vives (Ciutadella, 1846-1922)'.

Este material fue publicado por parte del Ayuntamiento y el Cercle Artístic de Ciutadella

Liberals and conservatives, 1846-95.

Cumple con los requisitos para OCR AS de Historia, unidad F961 Opción B y su contenido estudia el origen, el significado y la importancia de los partidos conservador y liberal en el siglo XIX, examina la historia política británica y se presta especial atención al desarrollo de las ideas y a las carreras políticas de William Gladstone y Disraeli Benjamin. Incluye una selección y definición de los temas, conceptos, acontecimientos y lugares considerados más importantes, así como breves biografías de personajes clave y consejos para los exámenes.

Tosca, de Giacomo Puccini : la génesis, la obra y su interpretación.

Se propone recoger el sonido creado por Giacomo Puccini en 'Tosca' en términos musicológicos. El análisis se centra en el proceso creativo, en la coincidencia fantástica entre acción y música, donde la novedad ocupa un papel importante tanto en su escritura orquestal como en su aportación al ámbito lírico. Una visión pormenorizada a través de su génesis (el proceso creativo), su estructura interna y externa, y por último su interpretación (cantantes, público, opiniones, literatura y cine). Se lleva a cabo un vaciado bibliográfico general referido a la historia de la ópera, de las corrientes artísticas y musicales de fines del siglo XIX y principios del siglo XX, y de los compositores contemporáneos a Giacomo Puccini. También se realiza un vaciado bibliográfico específico sobre la figura de Puccini, sus biografías, ensayos, epistolarios y programas de representación además de su obra, libretos y partituras. Se incluye también un vaciado discográfico y videográfico general de las óperas de Puccini y en concreto la de 'Tosca' con entrevistas a grandes intérpretes de los tres principales papeles: sopranos, tenores y barítonos. Se analiza el libreto y la partitura de 'Tosca' así como las diferencias y analogías entre 'La Tosca' de Victorien Sardou y 'Tosca' de Puccini. El corpus del trabajo se divide en tres apartados a modo de tres actos, donde se analizan todos los parámetros de la ópera. La asimilación de aspectos reiterativos en el catálogo compositivo pucciano y especial atención por la forma ternaria, las relaciones triangulares o efectos triples. Con 'Tosca', Puccini sintió la necesidad de consagrarse a un drama diferente, en el que el infortunio de sus personajes dejara de ser el resultado de un hado adverso, sino por el contrario, el de la ferocidad de los personajes labrando su propio destino. Busca y logra diferenciarse de lo que es común en sus dos obras inmediatamente anteriores. De la pasividad y de la inercia con que viven los personajes pretéritos se pasa al vigor desenfrenado y excesivo que excita y mueve en demasía a los personajes, maneras que les acompañan directos al infortunio. Respecto a los recursos musicales que acompañan al drama de 'Tosca', es otro método por medio del que Puccini se maneja para evitar tensión, pero añadir color armónico.

Numerical simulations of magma chamber dynamics at Campi Flegrei, and associated seismicity, deformation and gravity changes

Understanding the complex relationships between quantities measured by volcanic monitoring network and shallow magma processes is a crucial headway for the comprehension of volcanic processes and a more realistic evaluation of the associated hazard. This question is very relevant at Campi Flegrei, a volcanic quiescent caldera immediately north-west of Napoli (Italy). The system activity shows a high fumarole release and periodic ground slow movement (bradyseism) with high seismicity. This activity, with the high people density and the presence of military and industrial buildings, makes Campi Flegrei one of the areas with higher volcanic hazard in the world. In such a context my thesis has been focused on magma dynamics due to the refilling of shallow magma chambers, and on the geophysical signals detectable by seismic, deformative and gravimetric monitoring networks that are associated with this phenomenologies. Indeed, the refilling of magma chambers is a process frequently occurring just before a volcanic eruption; therefore, the faculty of identifying this dynamics by means of recorded signal analysis is important to evaluate the short term volcanic hazard. The space-time evolution of dynamics due to injection of new magma in the magma chamber has been studied performing numerical simulations with, and implementing additional features in, the code GALES (Longo et al., 2006), recently developed and still on the upgrade at the Istituto Nazionale di Geofisica e Vulcanologia in Pisa (Italy). GALES is a finite element code based on a physico-mathematical two dimensional, transient model able to treat fluids as multiphase homogeneous mixtures, compressible to incompressible. The fundamental equations of mass, momentum and energy balance are discretised both in time and space using the Galerkin Least-Squares and discontinuity-capturing stabilisation technique. The physical properties of the mixture are computed as a function of local conditions of magma composition, pressure and temperature.The model features enable to study a broad range of phenomenologies characterizing pre and sin-eruptive magma dynamics in a wide domain from the volcanic crater to deep magma feeding zones. The study of displacement field associated with the simulated fluid dynamics has been carried out with a numerical code developed by the Geophysical group at the University College Dublin (O’Brien and Bean, 2004b), with whom we started a very profitable collaboration. In this code, the seismic wave propagation in heterogeneous media with free surface (e.g. the Earth’s surface) is simulated using a discrete elastic lattice where particle interactions are controlled by the Hooke’s law. This method allows to consider medium heterogeneities and complex topography. The initial and boundary conditions for the simulations have been defined within a coordinate project (INGV-DPC 2004-06 V3_2 “Research on active volcanoes, precursors, scenarios, hazard and risk - Campi Flegrei”), to which this thesis contributes, and many researchers experienced on Campi Flegrei in volcanological, seismic, petrological, geochemical fields, etc. collaborate. Numerical simulations of magma and rock dynamis have been coupled as described in the thesis. The first part of the thesis consists of a parametric study aimed at understanding the eect of the presence in magma of carbon dioxide in magma in the convection dynamics. Indeed, the presence of this volatile was relevant in many Campi Flegrei eruptions, including some eruptions commonly considered as reference for a future activity of this volcano. A set of simulations considering an elliptical magma chamber, compositionally uniform, refilled from below by a magma with volatile content equal or dierent from that of the resident magma has been performed. To do this, a multicomponent non-ideal magma saturation model (Papale et al., 2006) that considers the simultaneous presence of CO2 and H2O, has been implemented in GALES. Results show that the presence of CO2 in the incoming magma increases its buoyancy force promoting convection ad mixing. The simulated dynamics produce pressure transients with frequency and amplitude in the sensitivity range of modern geophysical monitoring networks such as the one installed at Campi Flegrei . In the second part, simulations more related with the Campi Flegrei volcanic system have been performed. The simulated system has been defined on the basis of conditions consistent with the bulk of knowledge of Campi Flegrei and in particular of the Agnano-Monte Spina eruption (4100 B.P.), commonly considered as reference for a future high intensity eruption in this area. The magmatic system has been modelled as a long dyke refilling a small shallow magma chamber; magmas with trachytic and phonolitic composition and variable volatile content of H2O and CO2 have been considered. The simulations have been carried out changing the condition of magma injection, the system configuration (magma chamber geometry, dyke size) and the resident and refilling magma composition and volatile content, in order to study the influence of these factors on the simulated dynamics. Simulation results allow to follow each step of the gas-rich magma ascent in the denser magma, highlighting the details of magma convection and mixing. In particular, the presence of more CO2 in the deep magma results in more ecient and faster dynamics. Through this simulations the variation of the gravimetric field has been determined. Afterward, the space-time distribution of stress resulting from numerical simulations have been used as boundary conditions for the simulations of the displacement field imposed by the magmatic dynamics on rocks. The properties of the simulated domain (rock density, P and S wave velocities) have been based on data from literature on active and passive tomographic experiments, obtained through a collaboration with A. Zollo at the Dept. of Physics of the Federici II Univeristy in Napoli. The elasto-dynamics simulations allow to determine the variations of the space-time distribution of deformation and the seismic signal associated with the studied magmatic dynamics. In particular, results show that these dynamics induce deformations similar to those measured at Campi Flegrei and seismic signals with energies concentrated on the typical frequency bands observed in volcanic areas. The present work shows that an approach based on the solution of equations describing the physics of processes within a magmatic fluid and the surrounding rock system is able to recognise and describe the relationships between geophysical signals detectable on the surface and deep magma dynamics. Therefore, the results suggest that the combined study of geophysical data and informations from numerical simulations can allow in a near future a more ecient evaluation of the short term volcanic hazard.

Campi finiti e segnale GPS

Lo scopo della tesi è quello di studiare una delle applicazioni della teoria dei campi finiti: il segnale GPS. A questo scopo si descrivono i registri a scorrimento a retroazione lineare (linear feedback shift register, LFSR), dispositivi utili in applicazioni che richiedono la generazione molto rapida di numeri pseudo-casuali. I ricevitori GPS sfruttano il determinismo di questi dispositivi per identificare il satellite da cui proviene il segnale e per sincronizzarsi con esso. Si inizia con una breve introduzione al funzionamento del GPS, poi si studiano i campi finiti: sottocampi, estensioni di campo, gruppo moltiplicativo e costruzione attraverso la riduzione modulo un polinomio irriducibile, fattorizzazione di polinomi, formula per il numero e metodi per la determinazione di polinomi irriducibili, radici di polinomi irriducibili, coniugati, teoria di Galois (automorfismo ed orbite di Frobenius, gruppo e corrispondenza di Galois), traccia, polinomio caratteristico, formula per il numero e metodi per la determinazione di polinomi primitivi. Successivamente si introducono e si esaminano sequenze ricorrenti lineari, loro periodicità, la sequenza risposta impulsiva, il polinomio caratteristico associato ad una sequenza e la sequenza di periodo massimo. Infine, si studiano i registri a scorrimento che generano uno dei segnali GPS. In particolare si esamina la correlazione tra due sequenze. Si mostra che ogni polinomio di grado n-1 a coefficienti nel campo di Galois di ordine 2 può essere rappresentato univocamente in n bit; la somma tra polinomi può essere eseguita come XOR bit-a-bit; la moltiplicazione per piccoli coefficienti richiede al massimo uno shift ed uno XOR. Si conclude con la dimostrazione di un importante risultato: è possibile inizializzare un registro in modo tale da fargli generare una sequenza di periodo massimo poco correlata con ogni traslazione di se stessa.

Gelatinase B [matrix metalloproteinase (MMP)-9] and collagenases (MMP-8/-13) are upregulated in cerebrospinal fluid during aseptic and bacterial meningitis in children

We investigated the protein expression of gelatinases [matrix metalloproteinase (MMP)-2 and -9] and collagenases (MMP-8 and -13) in cerebrospinal fluid (CSF) from patients with bacterial (BM, n = 17) and aseptic (AM, n = 14) meningitis. In both, MMP-8 and -9 were increased in 100% of patients, whereas MMP-13 was detectable in 53% and 82% respectively. Three patients with clinical signs of meningitis, without CSF pleocytosis, scored positive for all three MMPs. MMP-8 appeared in two isoforms, granulocyte-type [polymorphonuclear cell (PMN)] and fibroblast/macrophage (F/M) MMP-8. Analysis of kinetic changes from serial lumbar punctures showed that these MMPs are independently regulated, and correlate only partly with CSF cytosis or levels of the endogenous inhibitor, tissue inhibitor of matrix metalloproteinase-1. In vitro, T cells, peripheral blood mononuclear cells (PBMCs) and granulocytes (PMN) release MMP-8 and -9, whereas MMP-13 could be found only in the former two cell types. Using models of exogenous (n-formyl-Met-Leu-Phe, T cell receptor cross-linking) and host-derived stimuli (interleukin-2), the kinetics and the release of the MMP-8, -9 and -13 showed strong variation between these immune cells and suggest release from preformed stocks. In addition, MMP-9 is also synthesized de novo in PBMCs and T cells. In conclusion, invading immune cells contribute only partially to MMPs in CSF during meningitis, and parenchymal cells are an equally relevant source. In this context, in patients with clinical signs of meningitis, but without CSF pleocytosis, MMPs seem to be a highly sensitive marker for intrathecal inflammation. The present data support the concept that broad-spectrum enzyme inhibition targeting gelatinases and collagenases is a potential strategy for adjunctive therapy in infectious meningitis.

Small ruminant lentivirus genotype B and E interaction: evidences on the role of Roccaverano strain on reducing proviral load of the challenging CAEV strain

Live attenuated vaccines provide the most consistent protective immunity in experimental models of lentivirus infections. In this study we tested the hypothesis that animals infected with a naturally attenuated small ruminant lentivirus field strain of genotype E may control a challenge infection with a virulent strain of the caprine arthritis encephalitis virus (CAEV-CO). Within genotype E, Roccaverano strain has been described as attenuated since decreased arthritic pathological indexes were recorded in Roccaverano-infected animals compared to animals of the same breed infected with genotype B strains. Moreover, under natural conditions, animals double-infected with genotypes B and E appear less prone to develop SRLV-related disease, leading to a putative protective role of Roccaverano strain. Here we present evidence that goats experimentally infected with the avirulent genotype E SRLV-Roccaverano strain control the proviral load of a pathogenic challenge virus (CAEV-CO strain) more efficiently than naïve animals and appear to limit the spread of histological lesions to the contralateral joints.

Recueil des travaux rédigés en mémoire du jubilé scientifique de M. Daniel Chwolson ... : 1846-1896

[Hrsg.: David Gunzburg]

CD34+ selected versus unselected autologous stem cell transplantation in patients with advanced-stage mantle cell and diffuse large B-cell lymphoma

Novel strategies aiming to increase survival rates in patients with advanced-stage mantle cell lymphoma (MCL) and relapsing diffuse large B-cell lymphoma (DLBCL) are a clinical need. High-dose chemotherapy (HDCT) with autologous stem cell transplantation (ASCT) has improved progression-free (PFS) and overall survival (OS) in MCL and relapsed DLBCL. However, the role of CD34+ cell selection before ASCT in MCL and DLBCL is unclear. We retrospectively analyzed the outcome of 62 consecutive patients with advanced-stage MCL or relapsed DLBCL undergoing ASCT with (n=31) or without (n=31) prior CD34+ selection. All patients had stage III or IV disease, with 47% having DLBCL and 53% MCL. The median duration for neutrophil and platelet recovery was 12 and 16 days in CD34+ selected patients, and 11 (P<.001) and 14 days (P=.012) in the group without selection, respectively. No differences in toxicities were observed. The 5-year PFS for CD34+ selected versus not selected patients was 67% and 39% (P=.016), and the 5-year OS was 86% and 54% (P=.007). Our data suggest that using CD34+ selected autografts for ASCT in advanced stage MCL and DLBCL is associated with longer PFS and OS without increased toxicity.