Three-dimensial patchy lattice model: Ring formation and phase separation

We investigate the structural and thermodynamic properties of a model of particles with 2 patches of type A and 10 patches of type B. Particles are placed on the sites of a face centered cubic lattice with the patches oriented along the nearest neighbor directions. The competition between the self- assembly of chains, rings, and networks on the phase diagram is investigated by carrying out a systematic investigation of this class of models, using an extension ofWertheim's theory for associating fluids and Monte Carlo numerical simulations. We varied the ratio r epsilon(AB)/epsilon(AA) of the interaction between patches A and B, epsilon(AB), and between A patches, epsilon(AA) (epsilon(BB) is set to theta) as well as the relative position of the A patches, i.e., the angle. between the (lattice) directions of the A patches. We found that both r and theta (60 degrees, 90 degrees, or 120 degrees) have a profound effect on the phase diagram. In the empty fluid regime (r < 1/2) the phase diagram is reentrant with a closed miscibility loop. The region around the lower critical point exhibits unusual structural and thermodynamic behavior determined by the presence of relatively short rings. The agreement between the results of theory and simulation is excellent for theta = 120 degrees but deteriorates as. decreases, revealing the need for new theoretical approaches to describe the structure and thermodynamics of systems dominated by small rings. (C) 2014 AIP Publishing LLC.

Generalization of Wertheim's theory for the assembly of various types of rings

We generalize Wertheim's first order perturbation theory to account for the effect in the thermodynamics of the self-assembly of rings characterized by two energy scales. The theory is applied to a lattice model of patchy particles and tested against Monte Carlo simulations on a fcc lattice. These particles have 2 patches of type A and 10 patches of type B, which may form bonds AA or AB that decrease the energy by epsilon(AA) and by epsilon(AB) = r epsilon(AA), respectively. The angle theta between the 2 A-patches on each particle is fixed at 601, 90 degrees or 120 degrees. For values of r below 1/2 and above a threshold r(th)(theta) the models exhibit a phase diagram with two critical points. Both theory and simulation predict that rth increases when theta decreases. We show that the mechanism that prevents phase separation for models with decreasing values of theta is related to the formation of loops containing AB bonds. Moreover, we show that by including the free energy of B-rings ( loops containing one AB bond), the theory describes the trends observed in the simulation results, but that for the lowest values of theta, the theoretical description deteriorates due to the increasing number of loops containing more than one AB bond.

Overexpression and purification of Treponema pallidum rubredoxin; kinetic evidence for a superoxide-mediated electron transfer with the superoxide reductase neelaredoxin

J Biol Inorg Chem (2004) 9: 839–849 DOI 10.1007/s00775-004-0584-6

One-step in situ synthesis of polyamide microcapsules with inorganic payload and their transformation into responsive thermoplastic composite materials

Well-dispersed loads of finely powdered metals, metal oxides, several carbon allotropes or nanoclays are incorporated into highly porous polyamide 6 microcapsules in controllable amounts via an original one-step in situ fabrication technique. It is based on activated anionic polymerization (AAP) of ε-caprolactam in a hydrocarbon solvent performed in the presence of the respective micro- or nanosized loads. The forming microcapsules with typical diameters of 25-50 µm entrap up to 40 wt% of load. Their melt processing produces hybrid thermoplastic composites. Mechanical, electric conductivity and magnetic response measurements show that transforming of in situ loaded microcapsules into composites by melt processing (MP) is a facile and rapid method to fabricate materials with high mechanical resistance and electro-magnetic characteristics sufficient for many industrial applications. This novel concept requires low polymerization temperatures, no functionalization or compatibilization of the loads and it is easy to scale up at industrial production levels.

Prevalencia de infección por virus hepatitis C, B y VIH en pacientes alcoholistas de la ciudad de Córdoba.

La Hepatitis C y B, junto al alcoholismo, continúan siendo un verdadero problema de Salud Pública. Sin embargo, actualmente no existen datos locales que nos permitan estimar la prevalencia de infección por virus hepatotropos en pacientes alcoholistas, sus genotipos, distrubución geográfica, ni su asociación con determinado tipo de alcoholismo. Además, la co-infección del virus de la inmunodeficiencia humana (VIH) con los virus de hepatitis supone un impacto muy importante desde el punto de vista sanitario y estadístico en nuestro país, ya que alrededor del 50 por ciento de los pacientes VIH positivos presentan dicha coinfección. Es así que, por ser de interés sanitario y por compartir vías de transmisión con el virus de hepatitis B y C, nos parece adecuado estudiar también la presencia de VIH-1 en esta población. Nuestro centro de atención pública (IPAD), atiende a pacientes con trastornos por el consumo de sustancias; deshabitúa y rehabilita alcoholistas y a otros trastornos por consumo. Dichos pacientes, que viven en la ciudad capital, serán evaluados serológicamente para la detección de virus hepatotropos C-B y el VIH. Considerando que en nuestra institución se atiende a un 70 % de Alcoholistas Puros (con un promedio de 7 pacientes nuevos por día), nos resulta importante pesquisar la prevalencia de Virus C, B y VIH en nuestra población de alcoholistas. Toda esta problemática, es la propuesta de mi tesis doctoral. Hipótesis: estimamos encontrar en nuestra población de estudio cifras superiores a la prevalencia de estos virus publicada en bancos de sangre, lo cual se toma como referencia. Objetivos: -Conocer la prevalencia de infección por Virus de Hepatitis C, B y VIH-1 en pacientes alcoholistas de la ciudad de Córdoba, determinar si existe asociación de estos virus con algún tipo de alcoholismo, e identificar genotipos prevalentes y su distribución geográfica en Córdoba. Se incluirán en forma prospectiva y aleatorea, pacientes que concurren por primera vez, de ambos sexos, mayores de 21 años, alcoholistas puros (Gama-Delta-Epsilon de Jellinek). Se confeccionará una ficha, previo consentimiento informado, que permitirá categorizar al "tipo de bebedor". Se les realizará Serología para HCV, Ag HBs (en caso de reactividad se adicionará el Anti HBcore) y VIH. En caso de la positividad serológica, se procederá al frisado de los mismos, para la Genotipificación correspondiente. La recolección, captura y procesamiento de los datos se realizarán en una planilla o ficha. Luego se reubicarán en una base electrónica de datos y se harán los análisis estadísticos de los mismos. Resultados esperados: estimamos encontrar, coincidiendo con la bibliografía, un aumento en la prevalencia de estos virus. Creemos que pueden existir diferencias en los distintos tipos de alcoholismo debido a las diversas situaciones de riesgo a las que se exponen (más exposición en el Gama de Jellineck). Por esto esperamos encontrar un aumento en la prevalencia del Virus C, especialmente en el tipo consuetudinario (delta de Jellineck) por los trastornos nutritivos derivados del modo de consumo. Posiblemente esto pueda ser la llave de otros estudios que puedan esclarecer una vía de transmisión desconocida para este virus. De la misma manera, identificar los distintos genotipos existentes en nuestra ciudad y su distribución, y que como sabemos tiene implicancia en la evolución, y en los costos por el tiempo de tratamiento. Esta información será un aporte para programar medidas de vigilancia epidemiológica adecuada, elaborar estrategias preventivas además de aplicar el tratamiento correspondiente a los pacientes infectados que se detecten como tal durante el desarrollo del proyecto.

PREVALENCIA DE INFECCION POR VIRUS HEPATITIS C, B Y VIH EN PACIENTES ALCOHOLISTAS DE LA CIUDAD DE CORDOBA

La Hepatitis C y B, junto al alcoholismo, continúan siendo un verdadero problema de Salud Pública. Sin embargo, actualmente no existen datos locales que nos permitan estimar la prevalencia de infección por virus hepatotropos en pacientes alcoholistas, sus genotipos, distrubución geográfica, ni su asociación con determinado tipo de alcoholismo. Además, la co-infección del virus de la inmunodeficiencia humana (VIH) con los virus de hepatitis supone un impacto muy importante desde el punto de vista sanitario y estadístico en nuestro país, ya que alrededor del 50 por ciento de los pacientes VIH positivos presentan dicha coinfección. Es así que, por ser de interés sanitario y por compartir vías de transmisión con el virus de hepatitis B y C, nos parece adecuado estudiar también la presencia de VIH-1 en esta población. Nuestro centro de atención pública (IPAD), atiende a pacientes con trastornos por el consumo de sustancias; deshabitúa y rehabilita alcoholistas y a otros trastornos por consumo. Dichos pacientes, que viven en la ciudad capital, serán evaluados serológicamente para la detección de virus hepatotropos C-B y el VIH. Considerando que en nuestra institución se atiende a un 70 % de Alcoholistas Puros (con un promedio de 7 pacientes nuevos por día), nos resulta importante pesquisar la prevalencia de Virus C, B y VIH en nuestra población de alcoholistas. Toda esta problemática, es la propuesta de mi tesis doctoral. Hipótesis: estimamos encontrar en nuestra población de estudio cifras superiores a la prevalencia de estos virus publicada en bancos de sangre, lo cual se toma como referencia. Objetivos: -Conocer la prevalencia de infección por Virus de Hepatitis C, B y VIH-1 en pacientes alcoholistas de la ciudad de Córdoba, determinar si existe asociación de estos virus con algún tipo de alcoholismo, e identificar genotipos prevalentes y su distribución geográfica en Córdoba. Se incluirán en forma prospectiva y aleatorea, pacientes que concurren por primera vez, de ambos sexos, mayores de 21 años, alcoholistas puros (Gama-Delta-Epsilon de Jellinek). Se confeccionará una ficha, previo consentimiento informado, que permitirá categorizar al "tipo de bebedor". Se les realizará Serología para HCV, Ag HBs (en caso de reactividad se adicionará el Anti HBcore) y VIH. En caso de la positividad serológica, se procederá al frisado de los mismos, para la Genotipificación correspondiente. La recolección, captura y procesamiento de los datos se realizarán en una planilla o ficha. Luego se reubicarán en una base electrónica de datos y se harán los análisis estadísticos de los mismos. Resultados esperados: estimamos encontrar, coincidiendo con la bibliografía, un aumento en la prevalencia de estos virus. Creemos que pueden existir diferencias en los distintos tipos de alcoholismo debido a las diversas situaciones de riesgo a las que se exponen (más exposición en el Gama de Jellineck). Por esto esperamos encontrar un aumento en la prevalencia del Virus C, especialmente en el tipo consuetudinario (delta de Jellineck) por los trastornos nutritivos derivados del modo de consumo. Posiblemente esto pueda ser la llave de otros estudios que puedan esclarecer una vía de transmisión desconocida para este virus. De la misma manera, identificar los distintos genotipos existentes en nuestra ciudad y su distribución, y que como sabemos tiene implicancia en la evolución, y en los costos por el tiempo de tratamiento. Esta información será un aporte para programar medidas de vigilancia epidemiológica adecuada, elaborar estrategias preventivas además de aplicar el tratamiento correspondiente a los pacientes infectados que se detecten como tal durante el desarrollo del proyecto.

Helmintos parasitos de Nectomys squamipes (Brants) do município de Sumidouro, RJ

Os helmintos encontrados em setenta e uma necrópsias de Nectomys squamipes, capturados no Município de Sumidouro, Estado do Rio de janeiro, São analisados qualitativamente e quantitativamente. Foram estudadas as seguintes espécies: Pseudechinostomum caballeroi, Raillietina sp., Hassalstrongylus epsilon, Syphacia venteli, Aspidodera raillieti, Physaloptera getula e Litomosoides carinii.

IgG Anti-IgE Autoantibodies in Visceral Leishmaniasis

Procedures for IgG depletion in visceral leishmaniasis (VL) and schistosomiasis sera using Sepharose-protein G beads also deplete IgE. In this study, the presence of IgG anti-IgE autoantibodies in sera from patients with VL (n = 10), and hepatic-intestinal schistosomiasis (n = 10) and from healthy individuals (n = 10) was investigated. A sandwich ELISA using goat IgG anti-human IgE to capture serum IgE and goat anti-human IgG peroxidase conjugate to demonstrate the binding of IgG to the IgE captured was performed. VL sera had higher titers (p < 0.05) of IgG anti-IgE autoantibodies (OD = 2.01 ± 0.43) than sera from healthy individuals (OD = 1.35 ± 0.16) or persons infected with Schistosoma mansoni (OD = 1.34 ± 0.18). The immunoblotting carried out with eluates from Sepharose-protein G beads used to deplete IgG from these sera and goat anti-human IgE peroxidase conjugate, showed a similar pattern of bands, predominating the 75 kDa epsilon-heavy chain and also polypeptides resulting from physiological enzymatic digestion of IgE. A frequent additional band immediately above 75 kDa was observed only in VL sera.

Late Jurassic oceanic crust and Upper Cretaceous Caribbean plateau picritic basalts exposed in the Duarte igneous complex, Hispaniola

Four distinct rock units have been recognized near El Aguacate, in the Janico-Juncalito-La Vega area of the Duarte complex (Dominican Republic): (1) serpentinites crosscut by numerous diabasic dikes, (2) basalts interbedded with Late Jurassic ribbon cherts, (3) picrites and ankaramites relatively enriched in incompatible trace elements, and (4) amphibolites and gneissic amphibolites chemically similar to Oceanic Plateau Basalts. Similar Ar-Ar ages of late magmatic amphibole from a picrite, and hornblende from an amphibolite (86.1 +/- 1.3 Ma and 86.7 +/- 1.6 Ma, respectively), suggest that the Duarte picrites are contemporaneous with the Deep Sea Drilling Program Leg 15 and Ocean Drilling Program Leg 126 basalts drilled from the Caribbean oceanic plateau. These basalts are associated with sediments containing Late Cretaceous faunas. Sr, Nd, and Pb data show that enriched picrites and amphibolites are isotopically similar to mafic lavas from previously described Caribbean plateau and Galapagos hotspot basalts. Major element, trace element, and lead isotopic features of Late Jurassic basalts and diabases are consistent with those of normal oceanic crust basalt. However, these basalts differ from typical N-MORB because they have lower epsilon Nd ratios that plot within the range of Ocean Island Basalts. These rocks appear to represent remnants of the Caribbean Jurassic oceanic crust formed from an oceanic ridge possibly close to a hotspot. Later, they were tectonically juxtaposed with Late Cretaceous slices of the Caribbean-Colombian plateau.

Enriched basaltic andesites from mid-crustal fractional crystallization, recharge, and assimilation (Pilavo Volcano, Western Cordillera of Ecuador)

The origin of andesite is an important issue in petrology because andesite is the main eruptive product at convergent margins, corresponds to the average crustal composition and is often associated with major Cu-Au mineralization. In this study we present petrographic, mineralogical, geochemical and isotopic data for basaltic andesites of the latest Pleistocene Pilavo volcano, one of the most frontal volcanoes of the Ecuadorian Quaternary arc, situated upon thick (30-50 km) mafic crust composed of accreted Cretaceous oceanic plateau rocks and overlying mafic to intermediate Late Cretaceous-Late Tertiary magmatic arcs. The Pilavo rocks are basaltic andesites (54-57 center dot 5 wt % SiO(2)) with a tholeiitic affinity as opposed to the typical calc-alkaline high-silica andesites and dacites (SiO(2) 59-66 wt %) of other frontal arc volcanoes of Ecuador (e.g. Pichincha, Pululahua). They have much higher incompatible element contents (e.g. Sr 650-1350 ppm, Ba 650-1800 ppm, Zr 100-225 ppm, Th 5-25 ppm, La 15-65 ppm) and Th/La ratios (0 center dot 28-0 center dot 36) than Pichincha and Pululahua, and more primitive Sr ((87)Sr/(86)Sr similar to 0 center dot 7038-0 center dot 7039) and Nd (epsilon(Nd) similar to +5 center dot 5 to +6 center dot 1) isotopic signatures. Pilavo andesites have geochemical affinities with modern and recent high-MgO andesites (e.g. low-silica adakites, Setouchi sanukites) and, especially, with Archean sanukitoids, for both of which incompatible element enrichments are believed to result from interactions of slab melts with peridotitic mantle. Petrographic, mineral chemistry, bulk-rock geochemical and isotopic data indicate that the Pilavo magmatic rocks have evolved through three main stages: (1) generation of a basaltic magma in the mantle wedge region by flux melting induced by slab-derived fluids (aqueous, supercritical or melts); (2) high-pressure differentiation of the basaltic melt (at the mantle-crust boundary or at lower crustal levels) through sustained fractionation of olivine and clinopyroxene, leading to hydrous, high-alumina basaltic andesite melts with a tholeiitic affinity, enriched in incompatible elements and strongly impoverished in Ni and Cr; (3) establishment of one or more mid-crustal magma storage reservoirs in which the magmas evolved through dominant amphibole and clinopyroxene (but no plagioclase) fractionation accompanied by assimilation of the modified plutonic roots of the arc and recharge by incoming batches of more primitive magma from depth. The latter process has resulted in strongly increasing incompatible element concentrations in the Pilavo basaltic andesites, coupled with slightly increasing crustal isotopic signatures and a shift towards a more calc-alkaline affinity. Our data show that, although ultimately originating from the slab, incompatible element abundances in arc andesites with primitive isotopic signatures can be significantly enhanced by intra-crustal processes within a thick juvenile mafic crust, thus providing an additional process for the generation of enriched andesites.

Central corneal thickness, intraocular pressure, and degree of myopia in an adult myopic population aged 20 to 40 years in southeast Spain: determination and relationships

Objective: To determine the values of, and study the relationships among, central corneal thickness (CCT), intraocular pressure (IOP), and degree of myopia (DM) in an adult myopic population aged 20 to 40 years in Almeria (southeast Spain). To our knowledge this is first study of this kind in this region. Methods: An observational, descriptive, cross-sectional study was done in which a sample of 310 myopic patients (620 eyes) aged 20 to 40 years was selected by gender- and age-stratified sampling, which was proportionally fixed to the size of the population strata for which a 20% prevalence of myopia, 5% epsilon, and a 95% confidence interval were hypothesized. We studied IOP, CCT, and DM and their relationships by calculating the mean, standard deviation, 95% confidence interval for the mean, median, Fisher’s asymmetry coefficient, range (maximum, minimum), and the Brown-Forsythe’s robust test for each variable (IOP, CCT, and DM). Results: In the adult myopic population of Almeria aged 20 to 40 years (mean of 29.8), the mean overall CCT was 550.12 μm. The corneas of men were thicker than those of women (P = 0.014). CCT was stable as no significant differences were seen in the 20- to 40-year-old subjects’ CCT values. The mean overall IOP was 13.60 mmHg. Men had a higher IOP than women (P = 0.002). Subjects over 30 years (13.83) had a higher IOP than those under 30 (13.38) (P = 0.04). The mean overall DM was −4.18 diopters. Men had less myopia than women (P < 0.001). Myopia was stable in the 20- to 40-year-old study population (P = 0.089). A linear relationship was found between CCT and IOP (R2 = 0.152, P ≤ 0.001). CCT influenced the IOP value by 15.2%. However no linear relationship between DM and IOP, or between CCT and DM, was found. Conclusions: CCT was found to be similar to that reported in other studies in different populations. IOP tends to increase after the age of 30 and is not accounted for by alterations in CCT values.

Central corneal thickness, intraocular pressure, and degree of myopia in an adult myopic population aged 20 to 40 years in southeast Spain: determination and relationships.

Objective: To determine the values of, and study the relationships among, central corneal thickness (CCT), intraocular pressure (IOP), and degree of myopia (DM) in an adult myopic population aged 20 to 40 years in Almeria (southeast Spain). To our knowledge this is first study of this kind in this region. Methods: An observational, descriptive, cross-sectional study was done in which a sample of 310 myopic patients (620 eyes) aged 20 to 40 years was selected by gender- and age-stratified sampling, which was proportionally fixed to the size of the population strata for which a 20% prevalence of myopia, 5% epsilon, and a 95% confidence interval were hypothesized. We studied IOP, CCT, and DM and their relationships by calculating the mean, standard deviation, 95% confidence interval for the mean, median, Fisher’s asymmetry coefficient, range (maximum, minimum), and the Brown-Forsythe’s robust test for each variable (IOP, CCT, and DM). Results: In the adult myopic population of Almeria aged 20 to 40 years (mean of 29.8), the mean overall CCT was 550.12 μm. The corneas of men were thicker than those of women (P = 0.014). CCT was stable as no significant differences were seen in the 20- to 40-year-old subjects’ CCT values. The mean overall IOP was 13.60 mmHg. Men had a higher IOP than women (P = 0.002). Subjects over 30 years (13.83) had a higher IOP than those under 30 (13.38) (P = 0.04). The mean overall DM was −4.18 diopters. Men had less myopia than women (P < 0.001). Myopia was stable in the 20- to 40-year-old study population (P = 0.089). A linear relationship was found between CCT and IOP (R2 = 0.152, P ≤ 0.001). CCT influenced the IOP value by 15.2%. However no linear relationship between DM and IOP, or between CCT and DM, was found. Conclusions: CCT was found to be similar to that reported in other studies in different populations. IOP tends to increase after the age of 30 and is not accounted for by alterations in CCT values.

Early Variscan I-type pluton in the pre-Alpine basement of the Western Alps: The ca. 360 Ma Cogne diorite (NW-Italy)

Located at the internal border of the Grand-Saint-Bernard Zone, the diorite and its aureole lie on top of intensively studied Alpine eclogitic units but this pluton, poorly studied yet, has kept locally almost undeformed. The pluton intruded, at similar to 360 Ma, country-rocks mostly composed of dark shales with Na2O > K2O and minor mafic intercalations of tholeiitic basalt affinity. This association is characteristic of the Vanoise (France) basement series, where available age determinations suggest an Early Paleozoic age. Parts of the pluton, and of its hornfels aureole that is evidenced here for the first time, in the Punta Bioula section of Valsavaranche valley (NW-Italy), have been well-preserved from the Alpine deformation. Syn-emplacement hardening, dehydration-induced, probably prevented strain-enhanced Alpine recrystallization. Magmatic rock-types range continuously from subordinate mafic types at SiO2 similar to 48%, of hornblendite with cumulative or appinite affinities, to the main body of quartz diorite to quartz monzonite (SiO2 up to 62%). P-T estimates for the pluton emplacement, based on the abundance of garnet in the hornfelses, using also zircon and apatite saturation thermometry and Al-in-hornblende barometry, suggest T similar to 800-950 degrees C and minimum P in the 0.2-0.5 GPa range, with records of higher pressure conditions (up to 1-2 GPa?) in hornblendite phlogopite-cored amphibole. The high-K, Na > K, calcalkaline geochemistry is in line with a destructive plate-margin setting. Based on major element data and radiogenic isotope signature (epsilon Nd-360 Ma from -1.2 to + 0.9, Sr-87/Sr-86(360 MA) from 0.7054 to 0.7063), the parental magmas are interpreted in terms of deep-seated metabasaltic partial melts with limited contamination from shallower sources, the low radiogenic Nd-content excluding a major contribution from Vanoise tholeiites. There is no other preserved evidence for Variscan magmatism of similar age and composition in the Western Alps, but probable analogs are known in the western and northern parts of French Massif Central. Regarding the Alpine tectonics, not only the age of the pluton and its host-rocks (instead of the Permo-Carboniferous age previously believed), but also its upper mylonitic contact, suggest revisions of the Alpine nappe model. The Cogne diorite allegedly constituted the axial part of the E-verging ``pli en retour [backfold] du Valsavaranche'', a cornerstone of popular Alpine structural models: in fact, the alleged fold limbs, as attested here by field and geochemical data, do not belong to the same unit, and the backfold hypothesis is unfounded. (C) 2012 Elsevier B.V. All rights reserved.

Nd-, O-, and H-isotopic evidence for complex, closed-system fluid evolution of the peralkaline Ilimaussaq intrusion, South Greenland

Relatively homogeneous oxygen isotope compositions of amphibole, clinopyroxene, and olivine separates (+5.2 to +5.7parts per thousand relative to VSMOW) and neodymium isotope compositions (epsilon(Nd(T)) = -0.9 to -1.8 for primary magmatic minerals and epsilon(Nd(T)) = -0.1 and -0.5 for mineral separates from late-stage pegmatites and hydrothermal veins) from the alkaline to agpaitic llimaussaq intrusion, South Greenland, indicate a closed system evolution of this igneous complex and support a mantle derivation of the magma. In contrast to the homogeneous oxygen and neodymium isotopic data, deltaD values for hand-picked amphibole separates vary between -92 and -232parts per thousand and are among the most deuterium-depleted values known from igneous amphiboles. The calculated fluid phase coexisting with these amphiboles has a homogeneous oxygen isotopic composition within the normal range of magmatic waters, but extremely heterogeneous and low D/H ratios, implying a decoupling of the oxygen- and hydrogen isotope systems. Of the several possibilities that can account for such unusually low deltaD values in amphiboles (e.g., late-stage hydrothermal exchange with meteoric water, extensive magmatic degassing, contamination with organic matter, and/or effects of Fe-content and pressure on amphibole-water fractionation) the most likely explanation for the range in deltaD values is that the amphiboles have been influenced by secondary interaction and reequilibration with D-depleted fluids obtained through late-magmatic oxidation of internally generated CH(4) and/or H(2). This interpretation is consistent with the known occurrence of abundant magmatic CH(4) in the Ilimaussaq rocks and with previous studies on the isotopic compositions of the rocks and fluids. Copyright (C) 2004 Elsevier Ltd.

Minimax lower bounds for the two-armed bandit problem

We obtain minimax lower bounds on the regret for the classicaltwo--armed bandit problem. We provide a finite--sample minimax version of the well--known log $n$ asymptotic lower bound of Lai and Robbins. Also, in contrast to the log $n$ asymptotic results on the regret, we show that the minimax regret is achieved by mere random guessing under fairly mild conditions on the set of allowable configurations of the two arms. That is, we show that for {\sl every} allocation rule and for {\sl every} $n$, there is a configuration such that the regret at time $n$ is at least 1 -- $\epsilon$ times the regret of random guessing, where $\epsilon$ is any small positive constant.