Temperatures at the last interglacial simulated by a coupled ocean-atmosphere climate model

The last interglacial (Eemian, 125,000 years ago) has generally been considered the warmest time period in the last 200,000 years and thus sometimes been used as a reference for greenhouse projections. Herein we report results from a coupled ocean-atmosphere climate model of the surface temperature response to changes in the radiative forcing at the last interglacial. Although the model generates the expected summer warming in the northern hemisphere, winter cooling of a comparable magnitude occurs over North Africa and tropical Asia. The global annual mean temperature for the Eemian run is 0.3 degrees C cooler than the control run. Validation of simulated sea surface temperatures (SSTs) against reconstructed SSTs supports this conclusion and also the assumption that the flux correction, fitted for the present state, operates satisfactorily for modest perturbations. Our results imply that contrary to conventional expectations, Eemian global temperatures may already have been reached by the mid 20th century.

Avaliação da influência do efeito de ultrassom na lixiviação de metais de placas de circuito impresso obsoletas.

Os equipamentos elétricos e eletrônicos (EEE) possuem uma grande importância na sociedade contemporânea, e estão presentes no cotidiano das pessoas de forma ubíqua. Com o aumento no consumo de EEE juntamente com a obsolescência precoce, surge um novo tipo de resíduo, chamado de Resíduos de Equipamentos Elétricos e Eletrônicos (REEE). Os REEE não devem ser descartados em aterros, pelo risco de contaminação e pelo desperdício de material. Assim, a reciclagem se faz necessária. As placas de circuito impresso (PCI) estão presentes na grande maioria do REEE e contem a maior variedade de metais, incluindo metais valiosos como Au, Ag, Pt e Cu. A complexidade torna a reciclagem destas placas muito difícil. Rotas hidrometalúrgicas tem surgido como uma alternativa mais limpa para o tratamento de PCI, em detrimento aos processos pirometalúrgicos. Nas rotas hidrometalúrgicas, os metais são extraídos pela lixiviação realizada por ácidos ou bases. O efeito ultrassônico tem sido empregado na síntese de novas substâncias e também em alguns casos no tratamento de resíduos. O processo central no uso de ultrassom é a cavitação acústica, capaz de produzir microbolhas na solução com temperatura da ordem de 5000 K e pressão de 500 atm localmente. Além disto, a implosão das bolhas de cavitação em meio heterogêneo causa um jato de solução na superfície, que pode alcançar velocidade de 100 m.s-1. Assim, esta tese tem como objetivo a investigação do efeito do ultrassom sobre PCI obsoletas. Dois efeitos foram investigados: o efeito da cominuição das PCI promovido pela cavitação e a influência da cavitação na lixiviação com ácido sulfúrico de Fe, Al e Ni. Os parâmetros investigados na cominuição foram: tipo de placa, granulometria da placa moída e potência de ultrassom. Os parâmetros de lixiviação avaliados foram: razão sólido-líquido (S/L), concentração de ácido e potência de ultrassom. Também foram realizados ensaios de lixiviação sonicados com meio oxidante. Foi feita a análise cinética para se determinar qual é o controle da reação de lixiviação.

Moneda y espacios de poder en el reino visigodo. Los tremises de El Tolmo de Minateda (Hellín, Albacete)

Los trabajos arqueológicos realizados en El Tolmo de Minateda (Hellín, Albacete) han permitido sacar a la luz los vestigios de una civitas visigoda creada a finales del siglo VI o inicios del VII. El material numismático recuperado en los niveles de uso y abandono de esta civitas está formado fundamentalmente por numerario de cobre de adscripción romana bajoimperial, y por tremises de oro de baja ley emitidos por el Estado visigodo. La contextualización estratigráfica y espacial de estas monedas ha permitido plantear diversas cuestiones referidas a la presencia y uso del numerario en época visigoda.

High-Pressure Methane Storage in Porous Materials: Are Carbon Materials in the Pole Position?

Natural gas storage on porous materials (ANG) is a promising alternative to conventional on-board compressed (CNG) or liquefied natural gas (LNG). To date, Metal–organic framework (MOF) materials have apparently been the only system published in the literature that is able to reach the new Department of Energy (DOE) value of 263 cm3 (STP: 273.15 K, 1 atm)/cm3; however, this value was obtained by using the ideal single-crystal density to calculate the volumetric capacity. Here, we prove experimentally, and for the first time, that properly designed activated carbon materials can really achieve the new DOE value while avoiding the additional drawback usually associated with MOF materials (i.e., the low mechanical stability under pressure (conforming), which is required for any practical application).

Metal-free catalysts derived from lignin for efficient wet peroxide oxidation

In this work, a wheat and hemp lignin (Sarkanda, Granit S.A.) has been used as raw material for the development of metal-free activated carbons. These materials were tested in the catalytic wet peroxide oxidation (CWPO) of 4-nitrophenol (4-NP; 5 g L-1) during 24 h experiments conducted at relatively mild operating conditions (p = 1 atm, t = 50 °C, pH = 3, catalyst load = 2.5 g L-1 and [H2O2]0 = 17.8 g L-1). First, the lignin was carbonized under N2 atmosphere followed by the activation of the obtained non-porous carbon (LG) under air atmosphere at different temperatures (150 to 350 ºC), leading to the generation of significant porosity.

Biochemical and functional characterization of the tumor suppressors BRCA1 and BAP1

L’ubiquitination est une modification post-traductionnelle qui joue un rôle majeur dans la régulation d’une multitude de processus cellulaires. Dans cette thèse, je discuterai de la caractérisation de deux protéines, BRCA1 et BAP1, soit deux suppresseurs de tumeurs fonctionnellement reliés. BRCA1, une ubiquitine ligase qui catalyse la liaison de l’ubiquitine à une protéine cible, est mutée dans les cancers du sein et de l'ovaire. Il est bien établi que cette protéine aide à maintenir la stabilité génomique suite à un bris double brin de l’ADN (BDB), et ce, à l’aide d’un mécanisme de réparation bien caractérisé appelé recombinaison homologue. Cependant, les mécanismes de régulation de BRCA1 suite à des stresses génotoxiques n’impliquant pas directement un BDB ne sont pas pleinement élucidés. Nous avons démontré que BRCA1 est régulée par dégradation protéasomale suite à une exposition des cellules à deux agents génotoxiques reconnus pour ne pas directement générer des BDBs, soit les rayons UV, qui provoquent la distorsion de l’hélice d’ADN, et le méthyle méthanesulfonate (MMS), qui entraîne l’alkylation de l’ADN. La dégradation de BRCA1 est réversible et indépendante des kinases associées à la voie des PI3 kinase, soit ATM, ATR et DNA-PK, protéines qui sont rapidement activées par les dommages à l’ADN. Nous proposons que la dégradation de BRCA1 prévienne son recrutement intempestif, ainsi que celui des facteurs qui lui sont associés, à des sites de dommages d’ADN qui ne sont pas des BDBs, et que cette régulation coordonne la réparation de l’ADN. L’enzyme de déubiquitination BAP1 a initialement été identifiée comme une protéine capable d’interagir avec BRCA1 et de réguler sa fonction. Elle est également connue pour sa capacité à se lier avec les protéines du groupe Polycomb, ASXL1 et ASXL2. Cependant, l’importance de ces interactions n’a toujours pas été établie. Nous avons démontré que BAP1 forme deux complexes protéiques mutuellement exclusifs avec ASXL1 et ASXL2. Ces interactions sont critiques pour la liaison de BAP1 à l’ubiquitine ainsi que pour la stimulation de son activité enzymatique envers l’histone H2A. Nous avons également identifié des mutations de BAP1 dérivées de cancers qui empêchent à la fois son interaction avec ASXL1 et AXSL2, et son activité de déubiquitinase, ce qui fournit un lien mécanistique direct entre la déubiquitination de H2A et la tumorigenèse. Élucider les mécanismes de régulation de BRCA1 et BAP1 menera à une meilleure compréhension de leurs rôles de suppresseurs de tumeurs, permettant ainsi d’établir de nouvelles stratégies de diagnostic et traitement du cancer.

Alterações morfológicas da articulação temporomandibular em pacientes odontogeriátricos

Dissertação para obtenção do grau de Mestre no Instituto Superior de Ciências da Saúde Egas Moniz

Caracterização do doente geriátrico da clínica universitária do Instituto Superior de Ciências da Saúde Egas Moniz

Dissertação para obtenção do grau de Mestre no Instituto Superior de Ciências da Saúde Egas Moniz

Prevalência e caracterização da dor orofacial nos doentes que recorrem à clínica universitária Egas Moniz

Dissertação para obtenção do grau de Mestre no Instituto Superior de Ciências da Saúde Egas Moniz

Evolution of the stable carbon isotope composition of atmospheric CO₂ over the last glacial cycle

We present new δ¹³C measurements of atmospheric CO₂ covering the last glacial/interglacial cycle, complementing previous records covering Terminations I and II. Most prominent in the new record is a significant depletion in δ¹³C(atm) of 0.5‰ occurring during marine isotope stage (MIS) 4, followed by an enrichment of the same magnitude at the beginning of MIS 3. Such a significant excursion in the record is otherwise only observed at glacial terminations, suggesting that similar processes were at play, such as changing sea surface temperatures, changes in marine biological export in the Southern Ocean (SO) due to variations in aeolian iron fluxes, changes in the Atlantic meridional overturning circulation, upwelling of deep water in the SO, and long-term trends in terrestrial carbon storage. Based on previous modeling studies, we propose constraints on some of these processes during specific time intervals. The decrease in δ¹³C(atm) at the end of MIS 4 starting approximately 64 kyr B.P. was accompanied by increasing [CO₂]. This period is also marked by a decrease in aeolian iron flux to the SO, followed by an increase in SO upwelling during Heinrich event 6, indicating that it is likely that a large amount of δ¹³C-depleted carbon was transferred to the deep oceans previously, i.e., at the onset of MIS 4. Apart from the upwelling event at the end of MIS 4 (and potentially smaller events during Heinrich events in MIS 3), upwelling of deep water in the SO remained reduced until the last glacial termination, whereupon a second pulse of isotopically light carbon was released into the atmosphere.

Helium in solubility equilibrium with quartz and porefluids in rocks - a new approach in hydrology

Quartz crystals in sandstones at depths of 1200 m–1400 m below the surface appear to reach a solubility equilibrium with the 4He-concentration in the surrounding pore- or groundwater after some time. A rather high 4Heconcentration of 4.5x10E-3 cc STP 4He/cm3 of water measured in a groundwater sample would for instance maintain a He pressure of 0.47 atm in a related volume. This value is equal within analytical error to the pressure deduced from the measured helium content of the quartz and its internal helium-accessible volume. To determine this volume, quartz crystals of 0.1 to 1 mm were separated from sandstones and exposed to a helium gas pressure of 32 atm at a temperature of 290°C for up to 2 months. By crushing, melting or isothermal heating the helium was then extracted from the helium saturated samples. Avolume on the order of 0.1% of the crystal volume is only accessible to helium atoms but not to argon atoms or water molecules. By monitoring the diffusive loss of He from the crystals at 350°C an effective diffusion constant on the order of 10E-9 cm2/s is estimated. Extrapolation to the temperature of 70°C in the sediments at a depth of 1400 m gives a typical time of about 100 000 years to reach equilibrium between helium in porewaters and the internal He-accessible volume of quartz crystals. In a geologic situation with stagnant pore- or groundwaters in sediments it therefore appears to be possible with this new method to deduce a 4He depth profile for porewaters in impermeable rocks based on their mineral record.

Petrology and geochemistry of sideromelane glass shards from Pleistocene as layers north and south of Gran Canaria

Major elements, S, F, Cl concentrations and relative proportions of S6+ to total S were analyzed with electron microprobe in sideromelane glass shards from Pleistocene volcaniclastic sediments drilled during ODP Leg 157. Glasses are moderately to strongly evolved and represent a spectrum from alkali basalt, basanite and nephelinite through hawaiite, mugearite and tephrite to phonolitic tephrite. Measured S6+/SumS (0.03±0.98) and calculated Fe2+/Fe3+ (2.5±5.8) ratios in the melt yield preeruptive redox conditions ranging from NNO-1.4 to NNO+2.1. The morphology of the glass shards, variations of S and Cl concentrations (0.010±0.127 wt% S, 0.018±0.129 wt% Cl), calculated preeruptive temperatures (1030±1200 °C) and oxygen fugacities suggest that glasses deposited even within the same ash layers have diverse origin and may have resulted from both submarine and subaerial eruptions. Most vesicle-free glasses are characterized by high concentrations of S and represent undegassed or slightly degassed submarine lavas, whereas vesiculated glasses with low concentrations of S and Cl are strongly degassed and can be ascribed to the eruptions in shallow water or on land. Sideromelane glass shards at Sites 953 are thought to have resulted from submarine eruptions northeast of Gran Canaria, glasses at Site 954 represent mostly volcaniclastic material of shallow water submarine and subaerial eruptions on Gran Canaria and Tenerife, and glasses deposited at Site 956 resulted from submarine or explosive eruptions on Tenerife.

Volume changes of Jacobshavn Isbrae between 1985, 1997 and 2007

Following three decades of relative stability, Jakobshavn Isbrae, West Greenland, underwent dramatic thinning, retreat and speed-up starting in 1998. To assess the amount of ice loss, we analyzed 1985 aerial photos and derived a 40 m grid digital elevation model (DEM). We also obtained a 2007 40 m grid SPOT DEM covering the same region. Comparison of the two DEMs over an area of ~4000 km**2 revealed a total ice loss of 160 ± 4 km**3, with 107 ± 0.2 km**3 in grounded regions (0.27 mm eustatic sea-level rise) and 53 ± 4 km**3 from the disintegration of the floating tongue. Comparison of the DEMs with 1997 NASA Airborne Topographic Mapper data indicates that this ice loss essentially occurred after 1997, with +0.7 ± 5.6 km**3 between 1985 and 1997 and -160 ± 7 km**3 between 1997 and 2007. The latter is equivalent to an average specific mass balance of -3.7 ± 0.2 m/a over the study area. Previously reported thickening of the main glacier during the early 1990s was accompanied by similar-magnitude thinning outside the areas of fast flow, indicating that the land-based ice continued reacting to longer-term climate forcing.

Summary of boron isotope and Mg/Ca data

Biological productivity and carbon export in the equatorial Atlantic are thought to have been dramatically higher during the last glacial period than during the Holocene. Here we reconstruct the pH and CO2 content of surface waters from the eastern equatorial Atlantic Ocean over the past ~30 k.y. using the boron isotope composition of Globigerinoides ruber (a mixed-layer-dwelling planktic foraminifera). Our new record, combined with previously published data, indicates that during the last glacial, in contrast to today, a strong west to east gradient existed in the extent of air:sea equilibrium with respect to pCO2 (DeltapCO2), with the eastern equatorial Atlantic acting as a significant source of CO2 (+100 µatm) while the western Atlantic remained close to equilibrium (+25 µatm). This pattern suggests that a fivefold increase in the upwelling rate of deeper waters drove increased Atlantic productivity and large-scale regional cooling during the last glacial, but the higher than modern DeltapCO2 in the east indicates that export production did not keep up with enhanced upwelling of nutrients. However, the downstream decline of DeltapCO2 provides evidence that the unused nutrients from the east were eventually used for biologic carbon export, thereby effectively negating the impact of changes in upwelling on atmospheric CO2 levels. Our findings indicate that the equatorial Atlantic exerted a minimal role in contributing to lower glacial-age atmospheric CO2.

Combined effects of coral reef foraminifera Marginopora vertebralis and Heterostegina depressa in a multi-fractorial experiment

Warming and changes in ocean carbonate chemistry alter marine coastal ecosystems at an accelerating pace. The interaction between these stressors has been the subject of recent studies on reef organisms such as corals, bryozoa, molluscs, and crustose coralline algae. Here we investigated the combined effects of elevated sea surface temperatures and pCO2 on two species of photosymbiont-bearing coral reef Foraminifera: Heterostegina depressa (hosting diatoms) and Marginopora vertebralis (hosting dinoflagellates). The effects of single and combined stressors were studied by monitoring survivorship, growth, and physiological parameters, such as respiration, photochemistry (pulse amplitude modulation fluorometry and oxygen production), and chl a content. Specimens were exposed in flow-through aquaria for up to seven weeks to combinations of two pCO2 (~790 and ~490 µatm) and two temperature (28 and 31 °C) regimes. Elevated temperature had negative effects on the physiology of both species. Elevated pCO2 had negative effects on growth and apparent photosynthetic rate in H.depressa but a positive effect on effective quantum yield. With increasing pCO2, chl a content decreased in H. depressa and increased in M. vertebralis. The strongest stress responses were observed when the two stressors acted in combination. An interaction term was statistically significant in half of the measured parameters. Further exploration revealed that 75 % of these cases showed a synergistic (= larger than additive) interaction between the two stressors. These results indicate that negative physiological effects on photosymbiont-bearing coral reef Foraminifera are likely to be stronger under simultaneous acidification and temperature rise than what would be expected from the effect of each of the stressors individually.