In-situ Iron isotope measurements and mineral compositions from ODP Hole 206-1256D and IODP Hole 335-U1256D

In-situ Fe isotope measurements have been carried out to estimate the impact of the hydrothermal metamorphic overprint on the Fe isotopic composition of Fe-Ti-oxides and Fe-sulfides of the different lithologies of the drilled rocks from IODP Hole 1256D (eastern equatorial Pacific; 15 Ma crust formed at the East Pacific Rise). Most igneous rocks normally have a very restricted range in their 56Fe/54Fe ratio. In contrast, Fe isotope compositions of hot fluids (> 300 °C) from mid-ocean-ridge spreading centers define a narrow range that is shifted to lower delta 56Fe values by 0.2 per mil - 0.5 per mil as compared to igneous rocks. Therefore, it is expected that mineral phases that contain large amounts of Fe are especially affected by the interaction with a fluid that fractionates Fe isotopes during exsolution/precipitation of those minerals. We have used a femtosecond UV-Laser ablation system to determine mineral 56Fe/54Fe ratios of selected samples with a precision of < 0.1 per mil (2 sigma level) at micrometer-scale. We have found significant variations of the delta 56Fe (IRMM-014) values in the minerals between different samples as well as within samples and mineral grains. The overall observed scale of delta 56Fe (magnetite) in 1256D rocks ranges from - 0.12 to + 0.64 per mil, and of delta 56Fe (ilmenite) from - 0.77 to + 0.01 per mil. Pyrite in the lowermost sheeted dike section is clearly distinguishable from the other investigated lithological units, having positive delta 56Fe values between + 0.29 and + 0.56 per mil, whereas pyrite in the other samples has generally negative delta 56Fe values from - 1.10 to - 0.59 permil. One key observation is that the temperature dependent inter-mineral fractionations of Fe isotopes between magnetite and ilmenite are systematically shifted towards higher values when compared to theoretically expected values, while synthesized, well equilibrated magnetite-ilmenite pairs are compatible with the theoretical predictions. Theoretical considerations including beta-factors of different aqueous Fe-chlorides and Rayleigh-type fractionations in the presence of a hydrous, chlorine-bearing fluid can explain this observation. The disagreement between observed and theoretical equilibrium fractionation, the fact that magnetite, in contrast to ilmenite shows a slight downhole trend in the delta 56Fe values, and the observation of small scale heterogeneities within single mineral grains imply that a general re-equilibration of the magnetite-ilmenite pairs is overprinted by kinetic fractionation effects, caused by the interaction of magnetite/ilmenite with hydrothermal fluids penetrating the upper oceanic crust during cooling, or incomplete re-equilibration at low temperatures. Furthermore, the observation of significant small-scale variations in the 56Fe/54Fe ratios of single minerals in this study highlights the importance of high spatial-resolution-analyses of stable isotope ratios for further investigations.

Strontium and neodymium isotope data for barite separates and pore waters, and isotope and concentration data for foraminifera and fish teeth from DSDP Leg 85 sediments

Strontium and neodymium isotopic data are reported for barite samples chemically separated from Late Miocene to Pliocene sediments from the eastern equatorial Pacific. At a site within a region of very high productivity close to the equator, 87Sr/86Sr ratios in the barite separates are indistinguishable from those of foraminifera and fish teeth from the same samples. However, at two sites north of the productivity maximum barite separates have slightly, but consistently lower (averaging 0.000062) ratios than the coexisting phases, although values still fall within the total range of published values for the contemporaneous seawater strontium isotope curve. We examine possible causes for this offset including recrystallization of the foraminifera, fish teeth or barite, the presence of non-barite contaminants, or incorporation of older, reworked deep-sea barite; the inclusion of a small amount of hydrothermal barite in the sediments seems most consistent with our data, although there are difficulties associated with adequate production and transportation of this phase. Barite is unlikely to replace calcite as a preferred tracer of seawater strontium isotopes in carbonate-rich sediments, but may prove a useful substitute in cases where calcite is rare or strongly affected by diagenesis. In contrast to the case for strontium, neodymium isotopic ratios in the barite separates are far from expected values for contemporary seawater, and appear to be dominated by an (unobserved) eolian component with high neodymium concentration and low 143Nd/144Nd. These results suggest that the true potential of barite as an indicator of paleocean neodymium isotopic ratios and REE patterns will be realized only when a more selective separation procedure is developed.

Study on the response of IFMIF fission chambers to mixed neutron-gamma fields: PH-2 experimental tests

The engineering design of fissionchambers as on-line radiation detectors for IFMIF is being performed in the framework of the IFMIF-EVEDA works. In this paper the results of the experiments performed in the BR2 reactor during the phase-2 of the foreseen validation activities are addressed. Two detectors have been tested in a mixedneutron-gamma field with high neutron fluence and gamma absorbed dose rates, comparable with the expected values in the HFTM in IFMIF. Since the neutron spectra in all BR2 channels are dominated by the thermal neutron component, the detectors have been surrounded by a cylindrical gadolinium screen to cut the thermal neutron component, in order to get a more representative test for IFMIF conditions. The integrated gamma absorbed dose was about 4 × 1010 Gy and the fast neutron fluence (E > 0.1 MeV) 4 × 1020 n/cm2. The fissionchambers were calibrated in three BR2 channels with different neutron-to-gamma ratio, and the long-term evolution of the signals was studied and compared with theoretical calculations

Seismic Hazard and Ground Motion Characterization at the Itoiz Dam (Northern Spain).

This paper presents a new hazard-consistent ground motion characterization of the Itoiz dam site, located in Northern Spain. Firstly, we propose a methodology with different approximation levels to the expected ground motion at the dam site. Secondly, we apply this methodology taking into account the particular characteristics of the site and of the dam. Hazard calculations were performed following the Probabilistic Seismic Hazard Assessment method using a logic tree, which accounts for different seismic source zonings and different ground-motion attenuation relationships. The study was done in terms of peak ground acceleration and several spectral accelerations of periods coinciding with the fundamental vibration periods of the dam. In order to estimate these ground motions we consider two different dam conditions: when the dam is empty (T = 0.1 s) and when it is filled with water to its maximum capacity (T = 0.22 s). Additionally, seismic hazard analysis is done for two return periods: 975 years, related to the project earthquake, and 4,975 years, identified with an extreme event. Soil conditions were also taken into account at the site of the dam. Through the proposed methodology we deal with different forms of characterizing ground motion at the study site. In a first step, we obtain the uniform hazard response spectra for the two return periods. In a second step, a disaggregation analysis is done in order to obtain the controlling earthquakes that can affect the dam. Subsequently, we characterize the ground motion at the dam site in terms of specific response spectra for target motions defined by the expected values SA (T) of T = 0.1 and 0.22 s for the return periods of 975 and 4,975 years, respectively. Finally, synthetic acceleration time histories for earthquake events matching the controlling parameters are generated using the discrete wave-number method and subsequently analyzed. Because of the short relative distances between the controlling earthquakes and the dam site we considered finite sources in these computations. We conclude that directivity effects should be taken into account as an important variable in this kind of studies for ground motion characteristics.

Coiled Bodies Preferentially Associate with U4, U11, and U12 Small Nuclear RNA Genes in Interphase HeLa Cells but Not with U6 and U7 Genes

Coiled bodies (CBs) are nuclear organelles involved in the metabolism of small nuclear RNAs (snRNAs) and histone messages. Their structural morphology and molecular composition have been conserved from plants to animals. CBs preferentially and specifically associate with genes that encode U1, U2, and U3 snRNAs as well as the cell cycle–regulated histone loci. A common link among these previously identified CB-associated genes is that they are either clustered or tandemly repeated in the human genome. In an effort to identify additional loci that associate with CBs, we have isolated and mapped the chromosomal locations of genomic clones corresponding to bona fide U4, U6, U7, U11, and U12 snRNA loci. Unlike the clustered U1 and U2 genes, each of these loci encode a single gene, with the exception of the U4 clone, which contains two genes. We next examined the association of these snRNA genes with CBs and found that they colocalized less frequently than their multicopy counterparts. To differentiate a lower level of preferential association from random colocalization, we developed a theoretical model of random colocalization, which yielded expected values for χ2 tests against the experimental data. Certain single-copy snRNA genes (U4, U11, and U12) but not controls were found to significantly (p < 0.000001) associate with CBs. Recent evidence indicates that the interactions between CBs and genes are mediated by nascent transcripts. Taken together, these new results suggest that CB association may be substantially augmented by the increased transcriptional capacity of clustered genes. Possible functional roles for the observed interactions of CBs with snRNA genes are discussed.

Sequence analysis of the cis-regulatory regions of the bithorax complex of Drosophila.

The bithorax complex (BX-C) of Drosophila, one of two complexes that act as master regulators of the body plan of the fly, has now been entirely sequenced and comprises approximately 315,000 bp, only 1.4% of which codes for protein. Analysis of this sequence reveals significantly overrepresented DNA motifs of unknown, as well as known, functions in the non-protein-coding portion of the sequence. The following types of motifs in that portion are analyzed: (i) concatamers of mono-, di-, and trinucleotides; (ii) tightly clustered hexanucleotides (spaced < or = 5 bases apart); (iii) direct and reverse repeats longer than 20 bp; and (iv) a number of motifs known from biochemical studies to play a role in the regulation of the BX-C. The hexanucleotide AGATAC is remarkably overrepresented and is surmised to play a role in chromosome pairing. The positions of sites of highly overrepresented motifs are plotted for those that occur at more than five sites in the sequence, when < 0.5 case is expected. Expected values are based on a third-order Markov chain, which is the optimal order for representing the BXCALL sequence.

Avaliação do volume e índices vasculares placentários pela ultrassonografia tridimensional em gestações com restrição grave de crescimento fetal

INTRODUÇÃO: A restrição de crescimento fetal (RCF) representa uma das principais complicações da gravidez e está associada a elevadas taxas de morbimortalidade perinatal. A frequência de desfechos desfavoráveis neonatais está diretamente relacionada à gravidade da RCF, sendo que os casos de pior evolução estão relacionados com peso abaixo do percentil 3. O mecanismo do crescimento fetal não está totalmente esclarecido, mas resulta da interação entre potencial genético de crescimento e fatores placentários, maternos e ambientais. Dentre os fatores etiológicos, o desenvolvimento anormal da placenta e a diminuição da perfusão uteroplacentária são as principais causas de RCF. Este estudo teve por objetivo avaliar volume e índices de vascularização placentários, por meio da ultrassonografia tridimensional (US3D), em gestações com RCF grave, e as correlações dos parâmetros placentários com valores de normalidade e dopplervelocimetria materno-fetal. MÉTODOS: Foram avaliadas 27 gestantes cujos fetos apresentavam peso estimado abaixo do percentil 3 para a idade gestacional. Por meio da US3D, utilizando-se a técnica VOCAL, foram mensurados o volume placentário (VP) e os índices vasculares: índice de vascularização (IV), índice de fluxo (IF) e índice de vascularização e fluxo (IVF). Os dados foram comparados com a curva de normalidade para a idade gestacional e peso fetal descrita por De Paula e cols. (2008, 2009). Desde que os volumes placentários variam durante a gravidez, os valores observados foram comparados com os valores esperados para a idade gestacional e peso fetal. Foram criados os índices volume observado/ esperado para a idade gestacional (Vo/e IG) e volume placentário observado/ esperado para o peso fetal (Vo/e PF). Os parâmetros placentários foram correlacionados com índice de pulsatilidade (IP) médio de (AUt) e IP de artéria umbilical (AU), e avaliados segundo a presença de incisura protodiastólica bilateral em AUt. RESULTADOS: Quando comparadas à curva de normalidade, as placentas de gestação com RCF grave apresentaram VP, IV, IF e IVF significativamente menores (p < 0,0001 para todos os parâmetros). Houve correlação inversa estatisticamente significante da média do PI de AUt com o Vo/e IG (r= -0,461, p= 0,018), IV (r= -0,401, p= 0,042) e IVF (r= -0,421, p= 0,048). No grupo de gestantes que apresentavam incisura protodiastólica bilateral de artérias uterinas, Vo/e IG (p= 0,014), Vo/e PF (p= 0,02) e IV (p= 0,044) foram significativamente mais baixos. Nenhum dos parâmetros placentários apresentou correlação significativa com IP de AU. CONCLUSÕES: Observou-se que o volume e os índices de vascularização placentários apresentam-se diminuídos nos fetos com RCF grave. IP médio de AUT apresenta correlação negativa com Vo/e IG, IV e IVF, e Vo/e IG, Vo/e PF e IV apresentaram-se reduzidos nos casos de incisura bilateral. Não houve correlação significativa dos parâmetros placentários com IP de AU

On the time to reach a critical number of infections in epidemic models with infective and susceptible immigrants.

In this paper we examine the time T to reach a critical number K0 of infections during an outbreak in an epidemic model with infective and susceptible immigrants. The underlying process X, which was first introduced by Ridler-Rowe (1967), is related to recurrent diseases and it appears to be analytically intractable. We present an approximating model inspired from the use of extreme values, and we derive formulae for the Laplace-Stieltjes transform of T and its moments, which are evaluated by using an iterative procedure. Numerical examples are presented to illustrate the effects of the contact and removal rates on the expected values of T and the threshold K0, when the initial time instant corresponds to an invasion time. We also study the exact reproduction number Rexact,0 and the population transmission number Rp, which are random versions of the basic reproduction number R0.

OH concentration and temperature measurements by use of near-resonant holographic interferometry

Near-resonant holographic interferometry is demonstrated to measure temperature and species concentration in a two-dimensional steady premixed air-acetylene flame. A peak temperature of (2600 +/- 100) K and a peak OH number density of (9.6 +/- 0.3) X 10(22) m(-3) are obtained, consistent with the expected values for such a flame. These values are determined by recording interferograms with a laser assumed sufficiently detuned from line center so that pressure and temperature broadening can be ignored. The results are thus obtained without making prior assumptions on the temperature or pressure of the flame beyond the existence of thermal equilibrium. (C) 2004 Optical Society of America.

Poly(methyl methacrylate) model study of optical surface quality after excimer laser photorefractive keratectomy

Purpose: To evaluate lenses produced by excimer laser ablation of poly(methyl methacrylate) (PMMA) plates. Setting: University research laboratory. Methods: Two Nidek EC-5000 scanning-slit excimer laser systems were used to ablate plane-parallel plates of PMMA. The ablated lenses were examined by focimetry, interferometry, and mechanical surface profiling. Results: The spherical optical powers of the lenses matched the expected values, but the cylindrical powers were generally lower than intended. Interferometry revealed marked irregularity in the surface of negative corrections, which often had a positive “island” at their center. Positive corrections were generally smoother. These findings were supported by the results of mechanical profiling. Contrast sensitivity measurements carried out when observing through ablated lenses whose power had been neutralized with a suitable spectacle lens of opposite sign confirmed that the surface irregularities of the ablated lenses markedly reduced contrast sensitivity over a range of spatial frequencies. Conclusion: Improvements in beam delivery systems seem desirable.

Representation of people of South Asian origin in cardiovascular outcome trials of glucose-lowering therapies in Type 2 diabetes

Aims : Our aim was to investigate the proportional representation of people of South Asian origin in cardiovascular outcome trials of glucose-lowering drugs or strategies in Type 2 diabetes, noting that these are among the most significant pieces of evidence used to formulate the guidelines on which clinical practice is largely based. Methods : We searched for cardiovascular outcome trials in Type 2 diabetes published before January 2015, and extracted data on the ethnicity of participants. These were compared against expected values for proportional representation of South Asian individuals, based on population data from the USA, from the UK, and globally. Results : Twelve studies met our inclusion criteria and, of these, eight presented a sufficiently detailed breakdown of participant ethnicity to permit numerical analysis. In general, people of South Asian origin were found to be under-represented in trials compared with UK and global expectations and over-represented compared with US expectations. Among the eight trials for which South Asian representation could be reliably estimated, seven under-represented this group relative to the 11.2% of the UK diabetes population estimated to be South Asian, with the representation in these trials ranging from 0.0% to 10.0%. Conclusions : Clinicians should exercise caution when generalizing the results of trials to their own practice, with regard to the ethnicity of individuals. Efforts should be made to improve reporting of ethnicity and improve diversity in trial recruitment, although we acknowledge that there are challenges that must be overcome to make this a reality.

Coastal groundwater discharge – an additional source of phosphorus for the oligotrophic wetlands of the Everglades

In this manuscript we define a new term we call coastal groundwater discharge (CGD), which is related to submarine groundwater discharge (SGD), but occurs when seawater intrudes inland to force brackish groundwater to discharge to the coastal wetlands. A hydrologic and geochemical investigation of both the groundwater and surface water in the southern Everglades was conducted to investigate the occurrence of CGD associated with seawater intrusion. During the wet season, the surface water chemistry remained fresh. Enhanced chloride, sodium, and calcium concentrations, indicative of brackish groundwater discharge, were observed in the surface water during the dry season. Brackish groundwaters of the southern Everglades contain 1–2.3μM concentrations of total phosphorus (TP). These concentrations exceed the expected values predicted by conservative mixing of local fresh groundwater and intruding seawater, which both have TPμM. The additional source of TP may be from seawater sediments or from the aquifer matrix as a result of water–rock interactions (such as carbonate mineral dissolution and ion exchange reactions) induced by mixing fresh groundwater with intruding seawater. We hypothesize that CGD maybe an additional source of phosphorus (a limiting nutrient) to the coastal wetlands of the southern Everglades.

Avaliação do papel dos polimorfismos em enzimas metabolizadoras e enzimas transportadoras de fármacos em neoplasias hematológicas

O cancro é um dos maiores causadores globais de mortalidade e morbilidade, ocorrendo cerca de 14 milhões de novos casos por ano e 8,2 milhões de mortes anuais com esta patologia, números que tendem a aumentar 70% nas próximas duas décadas. A característica tumoral mais nefasta é a sua capacidade de metastização para outros órgãos, um mecanismo que pode ser despoletado pela falha dos mecanismos normais de controlo de crescimento, proliferação e reparação celulares, que facilita o processo de transformação de células normais em células cancerígenas. A oncogénese processa-se em três etapas, a iniciação, a promoção e a progressão e pode ter origem em células estaminais cancerígenas, que regulam as capacidades de propagação e recidiva do tumor. As neoplasias hematológicas resultam de alterações genéticas e /ou epigenéticas que conduzem à desregulação da proliferação, ao bloqueio da diferenciação e/ou à resitência à apoptose. Para além dos fatores de risco exógenos, como agentes carcinogénicos físicos, químicos e biológicos, existem também fatores endógenos, incluindo características genéticas, que podem alterar a predisposição para o aparecimento de neoplasias, bem como influenciar a resposta à terapêutica. Uma das terapêuticas aplicadas no tratamento do cancro é a quimioterapia. Os fármacos administrados a doentes oncológicos seguem normalmente o percurso de absorção, distribuição, metabolização e eliminação. Este curso pode sofrer alterações caso as proteínas transportadoras e metabolizadoras necessárias não atuem corretamente. Para um melhor conhecimento da influência das alterações provocadas por variações nos genes que codificam proteínas transportadoras de efluxo (MDR1, MRP1), proteínas de influxo (OCTN2) e proteínas metabolizadoras (UCK2), o objetivo deste trabalho consistiu na avaliação de polimorfismos nos genes MDR1, MRP1, OCTN2 e UCK2 e da sua relação com a predisposição para o desenvolvimento de neoplasias hematológicas. Para isto, foram utilizadas amostras de 307 doentes com neoplasias hematológicas, 83 de Síndrome Mielodisplásica (SMD), 63 Leucemia Mieloide Aguda (LMA), 16 de Síndrome Mielodisplásica/Neoplasias Mieloproliferativas (SMD/NMP), 77 de Mieloma Múltiplo (MM) e 68 de Gamapatia Monoclonal de Significado Indeterminado (MGUS) e 164 de controlos não neoplásicos e/ou indivíduos saudáveis. As amostras de ADN foram extraídas do sangue periférico com protocolo adequado. De forma a determinar os genótipos correspondentes a cada amostra, realizaram-se técnicas de RFLP-PCR e ARMS-PCR. Posteriormente, calcularam-se estatisticamente as frequências alélicas e genotípicas relativas às variantes polimórficas dos genes MDR1, MRP1, OCTN2 e UCK2 e verificou-se se estavam em Equilíbrio de Hardy-Weinberg. De seguida, avaliou-se a força de associação entre as formas polimórficas e o risco de desenvolvimento de neoplasias hematológicas, através do cálculo do risco relativo por análise de regressão logística. Avaliaram-se ainda os perfis genéticos e a possível relação com o desenvolvimento e progressão da neoplasia com recurso a regressão logística e análise de Kaplan-Meier. De um modo geral as frequências alélicas e genotípicas não se revelaram alteradas comparativamente ao esperado. A análise do odds ratio associado ao polimorfismo rs1045642 do gene MDR1 revelou que o genótipo CT pode constituir um fator de risco aumentado de 1,84x para o desenvolvimento de Gamapatias Monoclonais e 2,27x para o desenvolvimento de Mieloma Múltiplo. Por outro lado, a presença de genótipos portadores do alelo T têm um efeito protetor no desenvolvimento de MM (OR=0,41). O cálculo do risco associado ao polimorfismo rs4148330 do gene MRP1 revela que o genótipo AG é um fator protetor (OR=0,50) para o desenvolvimento de LMA, assim como o alelo G (OR=0,50). Além disso, verificámos que existe uma associação de risco de desenvolver neoplasia com o polimorfismo rs2185268 do gene UCK2. De facto, a presença dos genótipos CC e AC representam um fator de risco 4,59x aumentado para o desenvolvimento de SMD/NMP. O polimorfismo rs274561 do gene OCTN2 não apresenta relação com o risco relativo de desenvolvimento neoplásico. Da avaliação da influência dos polimorfismos em estudo na sobrevivência global dos doentes, podemos assumir que a presença do genótipo GG relativo ao polimorfismo rs2185268 do gene UCK2 representa uma diminuição da sobrevivência em 11 meses. Os resultados obtidos a partir do nosso estudo permitem-nos concluir que os polimorfismos podem ser fatores relevantes na predisposição para o desenvolvimento de neoplasias hematológicas e na progressão destas doenças.

Methane seep carbonates yield clumped isotope signatures out of equilibrium with formation temperatures

Methane cold seep systems typically exhibit extensive buildups of authigenic carbonate minerals, resulting from local increases in alkalinity driven by methane oxidation. Here, we demonstrate that modern seep authigenic carbonates exhibit anomalously low clumped isotope values (Delta(47)), as much as similar to 0.2 parts per thousand lower than expected values. In modern seeps, this range of disequilibrium translates into apparent temperatures that are always warmer than ambient temperatures, by up to 50 degrees C. We examine various mechanisms that may induce disequilibrium behaviour in modern seep carbonates, and suggest that the observed values result from several factors including kinetic isotopic effects during methane oxidation, mixing of inorganic carbon pools, pH effects and rapid precipitation. Ancient seep carbonates studied here also exhibit potential disequilibrium signals. Ultimately, these findings indicate the predominance of disequilibrium clumped isotope behaviour in modern cold seep carbonates that must be considered when characterizing environmental conditions in both modern and ancient cold seep settings.

Pré-concentração de cádmio com Saccharomyces cerevisiae e determinação em águas fluviais usando espectrometria de emissão óptica com plasma indutivamente acoplado

A preconcentration method based on the use of Saccharomyces cerevisiae as sorbent material is proposed for the determination of Cd(II) in river water. The solid phase extraction was performed in batch mode and the determination of the analyte in the solid phase was easily carried out by introducing a slurry of the yeast (0.0625 g / 2.5 mL) directly into the ICP OES. A limit of detection of 0.11 µg L-1 and a sample throughput in the range of 4 - 54 sample h-1 were obtained. Determinations of cadmium in a certified sample and in real river water samples were in excellent agreement with the expected values.