Estudo ontogenético dos efeitos do ácido alfa-cetoisocapróico na fosforilação in vitro de filamentos intermediários de córtex cerebral de ratos

A disfunção neurológica é um sintoma comum em pacientes com Doença do Xarope do Bordo. Entretanto, os mecanismos que levam à neuropatologia dessa doença são pouco conhecidos. Neste trabalho, nós investigamos os efeitos do ácido α-cetoisocapróico (CIC) na incorporação in vitro de proteínas do tipo filamento intermediário de córtex cerebral de ratos durante o desenvolvimento. Fatias de tecido de ratos de 09, 12, 15, 17, 21 e 60 dias foram incubadas com 32P-ortofosfato na presença ou na ausência de CIC. A fração citoesquelética foi isolada e a radioatividade incorporada nas proteínas de filamento intermediário foi medida. Nós observamos que o CIC diminui a incorporação in vitro de 32P nas proteínas estudadas até 12 dias, entretanto, a fosforilação aumentou nas fatias de tecido de ratos de 17, 21 e 60 dias e nenhuma alteração ocorreu nas fatias cerebrais dos animais de 15 dias. Nós também testamos a influência do sistema glutamatérgico na incorporação in vitro de 32P nas proteínas estudadas, incubando fatias de córtex cerebral na presença de glutamato, agonistas e antagonistas glutamatérgicos. O glutamato apresentou um efeito similar ao observado para o CIC na fosforilação das proteínas de filamento intermediário durante o desenvolvimento, mas não afetou a incorporação in vitro de 32P nas proteínas estudadas nos ratos de 60 dias, sugerindo que nos animais adultos o CIC aumenta a incorporação in vitro nas proteínas estudadas por outros mecanismos. Além disso, nós observamos que os agonistas glutamatérgicos ionotrópicos NMDA, AMPA e cainato mimetizam o efeito inibitório do CIC, enquanto os agonistas metabotrópicos 1S, 3R ACPD e L-AP4 não induziram alterações na incorporação in vitro de 32P nas proteínas de filamento intermediário estudadas nos animais de 09 dias. Nos ratos de 21 dias, somente os agonistas ionotrópicos NMDA e AMPA mimetizaram o efeito estimulatório do CIC. Também observamos que quando fatias de córtex cerebral de ratos de 09 e 21 dias foram incubadas com 1mM CIC seguidas de incubação com o DL-AP5, um antagonista específico para receptores NMDA, ou com CNQX, antagonista de receptores ionotrópicos AMPA e cainato, o efeito inibitório ou estimulatório do ácido na fosforilação in vitro de ratos de 09 e 21 dias foi revertido. Estes resultados demonstram que o CIC, nas mesmas concentrações encontradas no sangue de crianças afetadas por DXB, altera o sistema de fosforilação associado com as proteínas do citoesqueleto, via sistema glutamatérgico, de maneira regulada pelo desenvolvimento. Portanto, é provável que a alteração de fosforilação das proteínas de citoesqueleto cerebral seja importante para o entendimento da patofisiologia da disfunção neuronal e das alterações estruturais observadas do SNC dos pacientes com DXB.

Citral: A monoterpene with prophylactic and therapeutic anti-nociceptive effects in experimental models of acute and chronic pain

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Relationship between Amazon biomass burning aerosols and rainfall over La Plata Basin

High aerosol loads are discharged into the atmosphere by biomass burning in Amazon and Central Brazil during the dry season. These particles can interact with clouds as cloud condensation nuclei (CCN) changing cloud microphysics and radiative properties and, thereby, affecting the radiative budget of the region. Furthermore, the biomass burning aerosols can be transported by the low level jet (LLJ) to La Plata Basin where many mesoscale convective systems (MCS) are observed during spring and summer. This work proposes to investigate whether the aerosols from biomass burning may affect the MCS in terms of rainfall over La Plata Basin during spring. Since the aerosol effect is very difficult to isolate because convective clouds are very sensitive to small environment disturbances, detailed analyses using different techniques are used. The binplot, 2D histograms and combined empirical orthogonal function (EOF) methods are used to separate certain environment conditions with the possible effects of aerosol loading. Reanalysis 2, TRMM-3B42 and AERONET data are used from 1999 up to 2012 during September-December. The results show that there are two patterns associated to rainfall-aerosol interaction in La Plata Basin: one in which the dynamic conditions are more important than aerosols to generate rain; and a second one where the aerosol particles have a role in rain formation, acting mainly to suppress rainfall over La Plata Basin.

Glutamate receptors expressed in {\it Xenopus\/} oocytes: Studies in function and regulation

The amino acid glutamate is the primary excitatory neurotransmitter for the CNS and is responsible for the majority of fast synaptic transmission. Glutamate receptors have been shown to be involved in multiple forms of synaptic plasticity such as LTP, LTD, and the formation of specific synaptic connections during development. In addition to contributing to the plasticity of the CNS, glutamate receptors also are involved in, at least in part, various pathological conditions such as epilepsy, ischemic damage due to stroke, and Huntington's chorea. The regulation of glutamate receptors, particularly the ionotropic NMDA and AMPA/KA receptors is therefore of great interest. In this body of work, glutamate receptor function and regulation by kinase activity was examined using the Xenopus oocyte which is a convenient and faithful expression system for exogenous proteins. Glutamate receptor responses were measured using the two-electrode voltage clamp technique in oocytes injected with rat total forebrain RNA. NMDA elicited currents that were glycine-dependent, subject to block by Mg$\sp{2+}$ in a voltage-dependent manner and sensitive to the specific NMDA antagonist APV in a manner consistent with those types of responses found in neural tissue. Similarly, KA-evoked currents were sensitive to the specific AMPA/KA antagonist CNQX and exhibited current voltage relationships consistent with the calcium permeable type II KA receptors found in the hippocampus. There is evidence to indicate that NMDA and AMPA/KA receptors are regulated by protein kinase A (PKA). We explored this by examining the effects of activators of PKA (forskolin, 1-isobutyl-3-methylxanthine (IBMX) and 8-Br-cAMP) on NMDA and KA currents in the oocyte. In buffer where Ca$\sp{2+}$ was replaced by 2 mM Ba$\sp{2+},$ forskolin plus IBMX and 8-Br-cAMP augmented currents due to NMDA application but not KA. This augmentation was abolished by pretreating the oocytes in the kinase inhibitor K252A. The use of chloride channel blockers resulted in attenuation of this effect indicating that Ba$\sp{2+}$ influx through the NMDA channel was activating the endogenous calcium-activated chloride current and that the cAMP mediated augmentation was at the level of the chloride channel and not the NMDA channel. This was confirmed by (1) the finding that 8-Br-cAMP increased chloride currents elicited via calcium channel activation while having no effect on the calcium channels themselves and (2) the fact that lowering the Ba$\sp{2+}$ concentration to 200 $\mu$M abolished the augmentation NMDA currents by 8-Br-cAMP. Thus PKA does not appear to modulate ionotropic glutamate receptors in our preparation. Another kinase also implicated in the regulation of NMDA receptors, calcium/phospholipid-dependent protein kinase (PKC), was examined for its effects on the NMDA receptor under low Ba$\sp{2+}$ (200 $\mu$M) conditions. Phorbol esters, activators of PKC, induced a robust potentiation of NMDA currents that was blockable by the kinase inhibitor K252A. Furthermore activation of metabotropic receptors by the selective agonist trans-ACPD, also potentiated NMDA albeit more modestly. These results indicate that neither NMDA nor KA-activated glutamate receptors are modulated by PKA in Xenopus oocytes whereas NMDA receptors appear to be augmented by PKC. Furthermore, the endogenous chloride current of the oocyte was found to be responsive to Ba$\sp{2+}$ and in addition is enhanced by PKA. Both of these latter findings are novel. In conclusion, the Xenopus oocyte is a useful expression system for the analysis of ligand-gated channel activity and the regulation of those channels by phosphorylation. ^

The quasi 16-day wave in mesospheric water vapor during boreal winter 2011/2012

This study investigates the characteristics of the quasi 16-day wave in the mesosphere during boreal winter 2011/2012 using observations of water vapor from ground-based microwave radiometers and satellite data. The ground-based microwave radiometers are located in Seoul (South Korea, 37° N), Bern (Switzerland, 47° N) and Sodankylä (Finland, 67° N). The quasi 16-day wave is observed in the mesosphere at all three locations, while the dominant period increases with latitude from 15 days at Seoul to 20 days at Sodankylä. The observed evolution of the quasi 16-day wave confirms that the wave activity is strongly decreased during a sudden stratospheric warming that occurred in mid-January 2012. Using satellite data from the Microwave Limb Sounder on the Aura satellite, we examine the zonal characteristics of the quasi 16-day wave and conclude that the observed waves above the mid-latitudinal stations Seoul and Bern are eastward-propagating s=−1 planetary waves with periods of 15 to 16 days, while the observed oscillation above the polar station Sodankylä is a standing oscillation with a period of approximately 20 days. The strongest relative wave amplitudes in water vapor during the investigated time period are approximately 15%. The wave activity varies strongly along a latitude circle. The activity of the quasi 16-day wave in mesospheric water vapor during boreal winter 2011/2012 is strongest over Northern Europe, the North Atlantic ocean and North-West Canada. The region of highest wave activity seems to be related to the position of the polar vortex. We conclude that the classic approach to characterize planetary waves zonally averaged along a latitude circle is not sufficient to explain the local observations because of the strong longitudinal dependence of the wave activity.

A climatology of the diurnal variations of stratospheric and mesospheric ozone over Bern, Switzerland

The ground-based radiometer GROMOS, stationed in Bern (47.95° N, 7.44° E), Switzerland, has a unique dataset: it obtains ozone profiles from November 1994 to present with a time resolution of 30 min and equal quality during night- and daytime. Here, we derive a monthly climatology of the daily ozone cycle from 17 yr of GROMOS observation. We present the diurnal ozone variation of the stratosphere and mesosphere. Characterizing the diurnal cycle of stratospheric ozone is important for correct trend estimates of the ozone layer derived from satellite observations. The diurnal ozone cycle from GROMOS is compared to two models: The Whole Atmosphere Community Climate Model (WACCM) and the Hamburg Model of Neutral and Ionized Atmosphere (HAMMONIA). Aura Microwave Limb Sounder (Aura/MLS) ozone data, from night- and daytime overpasses over Bern, have also been included in the comparison. Generally, observation and models show good qualitative agreement: in the lower mesosphere, daytime ozone is for both GROMOS and models around 25% less than nighttime ozone (reference is 22:30–01:30). In the stratosphere, ozone reaches its maximum in the afternoon showing values several percent larger than the midnight value. It is important that diurnal ozone variations of this order are taken into account when merging different data sets for the derivation of long-term ozone trends in the stratosphere. Further, GROMOS and models indicate a seasonal behavior of daily ozone variations in the stratosphere with a larger afternoon maximum during daytime in summer than in winter. At 0.35 hPa, observations from GROMOS and Aura/MLS show a seasonal pattern in diurnal ozone variations with larger relative amplitudes during daytime in winter (−25 ± 5%) than in summer (−18 ± 4%) (compared to mean values around midnight). For the first time, a time series of the diurnal variations in ozone is presented: 17 yr of GROMOS data show strong interannual variations in the diurnal ozone cycle for both the stratosphere and the mesosphere. There are some indications that strong temperature tides can suppress the diurnal variation of stratospheric ozone via the anticorrelation of temperature and ozone. That means the spatio-temporal variability of solar thermal tides seems to affect the diurnal cycle of stratospheric ozone.

The diurnal variation in stratospheric ozone from the MACC reanalysis, the ERA-Interim reanalysis, WACCM and Earth observations: characteristics and intercomparison

In this study we compare the diurnal variation in stratospheric ozone derived from free-running simulations of the Whole Atmosphere Community Climate Model (WACCM) and from reanalysis data of the atmospheric service MACC (Monitoring Atmospheric Composition and Climate) which both use a similar stratospheric chemistry module. We find good agreement between WACCM and the MACC reanalysis for the diurnal ozone variation in the high-latitude summer stratosphere based on photochemistry. In addition, we consult the ozone data product of the ERA-Interim reanalysis. The ERA-Interim reanalysis ozone system with its long-term ozone parametrization can not capture these diurnal variations in the upper stratosphere that are due to photochemistry. The good dynamics representations, however, reflects well dynamically induced ozone variations in the lower stratosphere. For the high-latitude winter stratosphere we describe a novel feature of diurnal variation in ozone where changes of up to 46.6% (3.3 ppmv) occur in monthly mean data. For this effect good agreement between the ERA-Interim reanalysis and the MACC reanalysis suggest quite similar diurnal advection processes of ozone. The free-running WACCM model seriously underestimates the role of diurnal advection processes at the polar vortex at the two tested resolutions. The intercomparison of the MACC reanalysis and the ERA-Interim reanalysis demonstrates how global reanalyses can benefit from a chemical representation held by a chemical transport model. The MACC reanalysis provides an unprecedented description of the dynamics and photochemistry of the diurnal variation of stratospheric ozone which is of high interest for ozone trend analysis and research on atmospheric tides. We confirm the diurnal variation in ozone at 5 hPa by observations of the Superconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) experiment and selected sites of the Network for Detection of Atmospheric Composition Change (NDACC). The latter give valuable insight even to diurnal variation of ozone in the polar winter stratosphere.

Comparison of several wood smoke markers and source apportionment methods for wood burning particulate mass

Residential wood combustion has only recently been recognized as a major contributor to air pollution in Switzerland and in other European countries. A source apportionment method using the aethalometer light absorption parameters was applied to five winter campaigns at three sites in Switzerland: a village with high wood combustion activity in winter, an urban background site and a highway site. The particulate mass from traffic (PMtraffic) and wood burning (PMwb) emissions obtained with this model compared fairly well with results from the 14C source apportionment method. PMwb from the model was also compared to well known wood smoke markers such as anhydrosugars (levoglucosan and mannosan) and fine mode potassium, as well as to a marker recently suggested from the Aerodyne aerosol mass spectrometer (mass fragment m/z 60). Additionally the anhydrosugars were compared to the 14C results and were shown to be comparable to literature values from wood burning emission studies using different types of wood (hardwood, softwood). The levoglucosan to PMwb ratios varied much more strongly between the different campaigns (4–13%) compared to mannosan to PMwb with a range of 1–1.5%. Possible uncertainty aspects for the various methods and markers are discussed.

Trajectory mapping of middle atmospheric water vapor by a mini network of NDACC instruments

The important task to observe the global coverage of middle atmospheric trace gases like water vapor or ozone usually is accomplished by satellites. Climate and atmospheric studies rely upon the knowledge of trace gas distributions throughout the stratosphere and mesosphere. Many of these gases are currently measured from satellites, but it is not clear whether this capability will be maintained in the future. This could lead to a significant knowledge gap of the state of the atmosphere. We explore the possibilities of mapping middle atmospheric water vapor in the Northern Hemisphere by using Lagrangian trajectory calculations and water vapor profile data from a small network of five ground-based microwave radiometers. Four of them are operated within the frame of NDACC (Network for the Detection of Atmospheric Composition Change). Keeping in mind that the instruments are based on different hardware and calibration setups, a height-dependent bias of the retrieved water vapor profiles has to be expected among the microwave radiometers. In order to correct and harmonize the different data sets, the Microwave Limb Sounder (MLS) on the Aura satellite is used to serve as a kind of traveling standard. A domain-averaging TM (trajectory mapping) method is applied which simplifies the subsequent validation of the quality of the trajectory-mapped water vapor distribution towards direct satellite observations. Trajectories are calculated forwards and backwards in time for up to 10 days using 6 hourly meteorological wind analysis fields. Overall, a total of four case studies of trajectory mapping in different meteorological regimes are discussed. One of the case studies takes place during a major sudden stratospheric warming (SSW) accompanied by the polar vortex breakdown; a second takes place after the reformation of stable circulation system. TM cases close to the fall equinox and June solstice event from the year 2012 complete the study, showing the high potential of a network of ground-based remote sensing instruments to synthesize hemispheric maps of water vapor.

First continuous ground-based observations of long period oscillations in strato-/mesospheric wind profiles

Direct measurements of middle-atmospheric wind oscillations with periods between 5 and 50 days in the altitude range between mid-stratosphere (5 hPa) and upper mesosphere (0.02 hPa) have been made using a novel ground-based Doppler wind radiometer. The oscillations were not inferred from measurements of tracers, as the radiometer offers the unique capability of near-continuous horizontal wind profile measurements. Observations from four campaigns at high, mid and low latitudes with an average duration of 10 months have been analyzed. The dominant oscillation has mostly been found to lie in the extra-long period range (20–40 days), while the well-known atmospheric normal modes around 5, 10 and 16 days have also been observed. Comparisons of our results with ECMWF operational analysis model data revealed remarkably good agreement below 0.3 hPa but discrepancies above.

Enhancing non-refractory aerosol apportionment from an urban industrial site through receptor modelling of complete high time-resolution aerosol mass spectra

Receptor modelling was performed on quadrupole unit mass resolution aerosol mass spectrometer (Q-AMS) sub-micron particulate matter (PM) chemical speciation measurements from Windsor, Ontario, an industrial city situated across the Detroit River from Detroit, Michigan. Aerosol and trace gas measurements were collected on board Environment Canada’s CRUISER mobile laboratory. Positive matrix factorization (PMF) was performed on the AMS full particle-phase mass spectrum (PMFFull MS) encompassing both organic and inorganic components. This approach was compared to the more common method of analysing only the organic mass spectra (PMFOrg MS). PMF of the full mass spectrum revealed that variability in the non-refractory sub-micron aerosol concentration and composition was best explained by six factors: an amine-containing factor (Amine); an ammonium sulphate and oxygenated organic aerosol containing factor (Sulphate-OA); an ammonium nitrate and oxygenated organic aerosol containing factor (Nitrate-OA); an ammonium chloride containing factor (Chloride); a hydrocarbon like organic aerosol (HOA) factor; and a moderately oxygenated organic aerosol factor (OOA). PMF of the organic mass spectrum revealed three factors of similar composition to some of those revealed through PMFFull MS: Amine, HOA and OOA. Including both the inorganic and organic mass proved to be a beneficial approach to analysing the unit mass resolution AMS data for several reasons. First, it provided a method for potentially calculating more accurate sub-micron PM mass concentrations, particularly when unusual factors are present, in this case, an Amine factor. As this method does not rely on a priori knowledge of chemical species, it circumvents the need for any adjustments to the traditional AMS species fragmentation patterns to account for atypical species, and can thus lead to more complete factor profiles. It is expected that this method would be even more useful for HR-ToF-AMS data, due to the ability to better understand the chemical nature of atypical factors from high resolution mass spectra. Second, utilizing PMF to extract factors containing inorganic species allowed for the determination of extent of neutralization, which could have implications for aerosol parameterization. Third, subtler differences in organic aerosol components were resolved through the incorporation of inorganic mass into the PMF matrix. The additional temporal features provided by the inorganic aerosol components allowed for the resolution of more types of oxygenated organic aerosol than could be reliably re-solved from PMF of organics alone. Comparison of findings from the PMFFull MS and PMFOrg MS methods showed that for the Windsor airshed, the PMFFull MS method enabled additional conclusions to be drawn in terms of aerosol sources and chemical processes. While performing PMFOrg MS can provide important distinctions between types of organic aerosol, it is shown that including inorganic species in the PMF analysis can permit further apportionment of organics for unit mass resolution AMS mass spectra.

Single particle diversity and mixing state measurements

A newly developed framework for quantifying aerosol particle diversity and mixing state based on information-theoretic entropy is applied for the first time to single particle mass spectrometry field data. Single particle mass fraction estimates for black carbon, organic aerosol, ammonium, nitrate and sulfate, derived using single particle mass spectrometer, aerosol mass spectrometer and multi-angle absorption photometer measurements are used to calculate single particle species diversity (Di). The average single particle species diversity (Dα) is then related to the species diversity of the bulk population (Dγ) to derive a mixing state index value (χ) at hourly resolution. The mixing state index is a single parameter representation of how internally/externally mixed a particle population is at a given time. The index describes a continuum, with values of 0 and 100% representing fully external and internal mixing, respectively. This framework was applied to data collected as part of the MEGAPOLI winter campaign in Paris, France, 2010. Di values are low (∼ 2) for fresh traffic and wood-burning particles that contain high mass fractions of black carbon and organic aerosol but low mass fractions of inorganic ions. Conversely, Di values are higher (∼ 4) for aged carbonaceous particles containing similar mass fractions of black carbon, organic aerosol, ammonium, nitrate and sulfate. Aerosol in Paris is estimated to be 59% internally mixed in the size range 150-1067 nm, and mixing state is dependent both upon time of day and air mass origin. Daytime primary emissions associated with vehicular traffic and wood-burning result in low χ values, while enhanced condensation of ammonium nitrate on existing particles at night leads to higher χ values. Advection of particles from continental Europe containing ammonium, nitrate and sulfate leads to increases in Dα, Dγ and χ. The mixing state index represents a useful metric by which to compare and contrast ambient particle mixing state at other locations globally.