979 resultados para Latter lanthanides and yttrium
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In recent decades fascinating studies in developmental psychology, especially in infant research (for review see Lavelli, 2007) and recent discoveries in neuroscience (Welsh, et al, 2007; Siegel, 2001; Pally, 2007) have brought great interest to study the mode of sharing subjective experiences (affective states, intentions and attentional focus) in children and adults.It therefore appears today in the clinic is a growing consensus about the fact that the psychological disorder can be read as a deficit in intersubjective processes of affect regulation (see Benecke C. et al 2005; psychodynamic Diagnostic Manual-PDM, 2006) leading many authors to assume the centrality of affect regulation in the construction of the psychotherapeutic process of change (just to name a few Tronick, Greenberg, Stern, Sander, Fonagy, Beebe, Philippot, Rimé etc..). As previously stated, this study has led us to hypothesize that the long process of therapy is to assist with the sessions continue, a growing "emotional attunement" between the communication styles of both patient and therapist. And also to speculate that this synchronization can represent the existence of a significant positive correlation between the increased level of "emotional synchronization" and increased capacity for regulation of emotions by the patient.The research results despite the limitations of small sample showed encouraging results about the verification of the existence of an increasing degree of attunement between therapist and patient long psychotherapy sessions and also showed a good degree of positive correlation between the increase the latter construct and emotional regulation through the implicit mode of expression and nonverbal communication.
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In dieser Arbeit wurden umfangreiche laserspektroskopische Studien mit dem Zielrneines verbesserten Verständnisses höchst komplexer Spektren der Lanthanide und Aktinide durchgeführt. Einen Schwerpunkt bildete die Bestimmung bisher nicht oder mit unbefriedigender Genauigkeit bekannter erster Ionisationspotentiale für diese Elemente.rnHierzu wurden drei unterschiedliche experimentelle Methoden eingesetzt. Die Bestimmung des Ionisationspotentiales aus Rydbergserien wurde an den Beispielen Eisen, Mangan und Kobalt mit gemessenen Werten von IPFe = 63737, 6 ± 0, 2stat ± 0, 1syst cm−1, IPMn = 59959, 6 ± 0, 4 cm−1 beziehungsweise IPCo = 63564, 77 ± 0, 12 cm−1 zunächst erfolgreich erprobt. Die bestehenden Literaturwerte konnten in diesen Fällen bestätigt werden und bei Eisen und Kobalt die Genauigkeit etwa um einen Faktor drei bzw. acht verbessert werden. Im Falle der Lanthaniden und Aktiniden jedoch ist die Komplexität der Spektren derart hoch, dass Rydbergserien in einer Vielzahl weiterer Zustände beliebiger Konfiguration nicht oder kaum identifiziert werden können.rnUm dennoch das Ionisationspotential bestimmen zu können, wurde die verzögerte, gepulste Feldionisation wie auch das Verfahren der Isolated Core Excitation am Beispiel des Dysprosiums erprobt. Aus den so identifizierten Rydbergserien konnten Werte von IPFeld = 47899 ± 3 cm−1 beziehungsweise IPICE = 47900, 4 ± 1, 4 cm−1 bestimmt werden. Als komplementärer Ansatz, der auf ein möglichst reichhaltiges Spektrum in der Nähe des Ionisationspotentiales angewiesen ist, wurde zusätzlich die Sattelpunktsmethode erfolgreich eingesetzt. Das Ionisationspotential des Dysprosium wurde damit zu IPDy = 47901, 8±0, 3 cm−1 bestimmt, wobei am Samarium, dessen Ionisationspotential aus der Literatur mit höchster Genauigkeit bekannt ist, bestätigt werden konnte, dassrnauftretende systematische Fehler kleiner als 1 cm−1 sind. Das bisher sehr ungenau bekannte Ionisationspotential des Praseodyms wurde schließlich zu IPPr = 44120, 0 ± 0, 6 cm−1 gemessen. Hiermit wird der bisherige Literaturwert bei einer Verbesserung der Genauigkeit um zwei Größenordnungen um etwa 50 cm−1 nach oben korrigiert. Aus der Systematik der Ionisationspotentiale der Lanthaniden konnte schließlich das Ionisationspotential des radioaktiven Promethiums mit IPPm = 44985 ± 140 cm−1 vorhergesagt werden. Abschließend wurde die Laserresonanzionisation des Elements Protactinium demonstriertrnund das Ionisationspotential erstmals experimentell bestimmt. Ein Wert vonrn49000±110 cm−1 konnte aus dem charakteristischen Verhalten verschiedener Anregungsschemata gefolgert werden. Dieser Wert liegt etwa 1500 cm−1 höher als der bisherige Literaturwert, theoretische Vorhersagen weichen ebenfalls stark ab. Beide Abweichungen können über eine Betrachtung der Systematik der Ionisationspotentiale in der Aktinidenreihe hervorragend verstanden werden.
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The human DMD locus encodes dystrophin protein. Absence or reduced levels of dystrophin (DMD or BMD phenotype, respectively) lead to progressive muscle wasting. Little is known about the complex coordination of dystrophin expression and its transcriptional regulation is a field of intense interest. In this work we found that DMD locus harbours multiple long non coding RNAs which orchestrate and control transcription of muscle dystrophin mRNA isoforms. These lncRNAs are tissue-specific and highly expressed during myogenesis, suggesting a possible role in tissue-specific expression of DMD gene isoforms. Their forced ectopic expression in human muscle and neuronal cells leads to a specific and negative regulation of endogenous dystrophin full lenght isoforms. An intriguing aspect regarding the transcription of the DMD locus is the gene size (2.4Mb). The mechanism that ensures the complete synthesis of the primary transcript and the coordinated splicing of 79 exons is still completely unknown. By ChIP-on-chip analyses, we discovered novel regions never been involved before in the transcription regulation of the DMD locus. Specifically, we observed enrichments for Pol II, P-Ser2, P-Ser5, Ac-H3 and 2Me-H3K4 in an intronic region of 3Kb (approximately 21Kb) downstream of the end of DMD exon 52 and in a region of 4Kb spanning the DMD exon 62. Interestingly, this latter region and the TSS of Dp71 are strongly marked by 3Me-H3K36, an histone modification associated with the regulation of splicing process. Furthermore, we also observed strong presence of open chromatin marks (Ac-H3 and 2Me-H3K4) around intron 34 and the exon 45 without presence of RNA pol II. We speculate that these two regions may exert an enhancer-like function on Dp427m promoter, although further investigations are necessary. Finally, we investigated the nuclear-cytoplasmic compartmentalization of the muscular dystrophin mRNA and, specifically, we verified whether the exon skipping therapy could influence its cellular distribution.
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Ophioluxin, a potent platelet agonist, was purified from the venom of Ophiophagus hannah (King cobra). Under nonreducing conditions it has a mass of 85 kDa, similar to convulxin, and on reduction gives two subunits with masses of 16 and 17 kDa, slightly larger than those of convulxin. The N-terminal sequences of both subunits are very similar to those of convulxin and other C-type lectins. Ophioluxin induces a pattern of tyrosine-phosphorylated proteins in platelets like that caused by convulxin, when using appropriate concentrations based on aggregation response, because it is about 2-4 times more powerful as agonist than the latter. Ophioluxin and convulxin induce [Ca(2+)](i) elevation both in platelets and in Dami megakaryocytic cells, and each of these C-type lectins desensitizes responses to the other. Convulxin agglutinates fixed platelets at 2 microg/ml, whereas ophioluxin does not, even at 80 microg/ml. Ophioluxin resembles convulxin more than echicetin or alboaggregin B because polyclonal anti-ophioluxin antibodies recognize both ophioluxin and convulxin, but not echicetin, and platelets adhere to and spread on ophioluxin- or convulxin-precoated surfaces in the same way that is clearly different from their behavior on an alboaggregin B surface. Immobilized ophioluxin was used to isolate the glycoprotein VI-Fcgamma complex from resting platelets, which also contained Fyn, Lyn, Syk, LAT, and SLP76. Ophioluxin is the first multiheterodimeric, convulxin-like snake C-type lectin, as well as the first platelet agonist, to be described from the Elapidae snake family.
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Essential biological processes are governed by organized, dynamic interactions between multiple biomolecular systems. Complexes are thus formed to enable the biological function and get dissembled as the process is completed. Examples of such processes include the translation of the messenger RNA into protein by the ribosome, the folding of proteins by chaperonins or the entry of viruses in host cells. Understanding these fundamental processes by characterizing the molecular mechanisms that enable then, would allow the (better) design of therapies and drugs. Such molecular mechanisms may be revealed trough the structural elucidation of the biomolecular assemblies at the core of these processes. Various experimental techniques may be applied to investigate the molecular architecture of biomolecular assemblies. High-resolution techniques, such as X-ray crystallography, may solve the atomic structure of the system, but are typically constrained to biomolecules of reduced flexibility and dimensions. In particular, X-ray crystallography requires the sample to form a three dimensional (3D) crystal lattice which is technically di‑cult, if not impossible, to obtain, especially for large, dynamic systems. Often these techniques solve the structure of the different constituent components within the assembly, but encounter difficulties when investigating the entire system. On the other hand, imaging techniques, such as cryo-electron microscopy (cryo-EM), are able to depict large systems in near-native environment, without requiring the formation of crystals. The structures solved by cryo-EM cover a wide range of resolutions, from very low level of detail where only the overall shape of the system is visible, to high-resolution that approach, but not yet reach, atomic level of detail. In this dissertation, several modeling methods are introduced to either integrate cryo-EM datasets with structural data from X-ray crystallography, or to directly interpret the cryo-EM reconstruction. Such computational techniques were developed with the goal of creating an atomic model for the cryo-EM data. The low-resolution reconstructions lack the level of detail to permit a direct atomic interpretation, i.e. one cannot reliably locate the atoms or amino-acid residues within the structure obtained by cryo-EM. Thereby one needs to consider additional information, for example, structural data from other sources such as X-ray crystallography, in order to enable such a high-resolution interpretation. Modeling techniques are thus developed to integrate the structural data from the different biophysical sources, examples including the work described in the manuscript I and II of this dissertation. At intermediate and high-resolution, cryo-EM reconstructions depict consistent 3D folds such as tubular features which in general correspond to alpha-helices. Such features can be annotated and later on used to build the atomic model of the system, see manuscript III as alternative. Three manuscripts are presented as part of the PhD dissertation, each introducing a computational technique that facilitates the interpretation of cryo-EM reconstructions. The first manuscript is an application paper that describes a heuristics to generate the atomic model for the protein envelope of the Rift Valley fever virus. The second manuscript introduces the evolutionary tabu search strategies to enable the integration of multiple component atomic structures with the cryo-EM map of their assembly. Finally, the third manuscript develops further the latter technique and apply it to annotate consistent 3D patterns in intermediate-resolution cryo-EM reconstructions. The first manuscript, titled An assembly model for Rift Valley fever virus, was submitted for publication in the Journal of Molecular Biology. The cryo-EM structure of the Rift Valley fever virus was previously solved at 27Å-resolution by Dr. Freiberg and collaborators. Such reconstruction shows the overall shape of the virus envelope, yet the reduced level of detail prevents the direct atomic interpretation. High-resolution structures are not yet available for the entire virus nor for the two different component glycoproteins that form its envelope. However, homology models may be generated for these glycoproteins based on similar structures that are available at atomic resolutions. The manuscript presents the steps required to identify an atomic model of the entire virus envelope, based on the low-resolution cryo-EM map of the envelope and the homology models of the two glycoproteins. Starting with the results of the exhaustive search to place the two glycoproteins, the model is built iterative by running multiple multi-body refinements to hierarchically generate models for the different regions of the envelope. The generated atomic model is supported by prior knowledge regarding virus biology and contains valuable information about the molecular architecture of the system. It provides the basis for further investigations seeking to reveal different processes in which the virus is involved such as assembly or fusion. The second manuscript was recently published in the of Journal of Structural Biology (doi:10.1016/j.jsb.2009.12.028) under the title Evolutionary tabu search strategies for the simultaneous registration of multiple atomic structures in cryo-EM reconstructions. This manuscript introduces the evolutionary tabu search strategies applied to enable a multi-body registration. This technique is a hybrid approach that combines a genetic algorithm with a tabu search strategy to promote the proper exploration of the high-dimensional search space. Similar to the Rift Valley fever virus, it is common that the structure of a large multi-component assembly is available at low-resolution from cryo-EM, while high-resolution structures are solved for the different components but lack for the entire system. Evolutionary tabu search strategies enable the building of an atomic model for the entire system by considering simultaneously the different components. Such registration indirectly introduces spatial constrains as all components need to be placed within the assembly, enabling the proper docked in the low-resolution map of the entire assembly. Along with the method description, the manuscript covers the validation, presenting the benefit of the technique in both synthetic and experimental test cases. Such approach successfully docked multiple components up to resolutions of 40Å. The third manuscript is entitled Evolutionary Bidirectional Expansion for the Annotation of Alpha Helices in Electron Cryo-Microscopy Reconstructions and was submitted for publication in the Journal of Structural Biology. The modeling approach described in this manuscript applies the evolutionary tabu search strategies in combination with the bidirectional expansion to annotate secondary structure elements in intermediate resolution cryo-EM reconstructions. In particular, secondary structure elements such as alpha helices show consistent patterns in cryo-EM data, and are visible as rod-like patterns of high density. The evolutionary tabu search strategy is applied to identify the placement of the different alpha helices, while the bidirectional expansion characterizes their length and curvature. The manuscript presents the validation of the approach at resolutions ranging between 6 and 14Å, a level of detail where alpha helices are visible. Up to resolution of 12 Å, the method measures sensitivities between 70-100% as estimated in experimental test cases, i.e. 70-100% of the alpha-helices were correctly predicted in an automatic manner in the experimental data. The three manuscripts presented in this PhD dissertation cover different computation methods for the integration and interpretation of cryo-EM reconstructions. The methods were developed in the molecular modeling software Sculptor (http://sculptor.biomachina.org) and are available for the scientific community interested in the multi-resolution modeling of cryo-EM data. The work spans a wide range of resolution covering multi-body refinement and registration at low-resolution along with annotation of consistent patterns at high-resolution. Such methods are essential for the modeling of cryo-EM data, and may be applied in other fields where similar spatial problems are encountered, such as medical imaging.
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Layered Fe-Mn crusts from the off-axis region of the first segment of the Central Indian Ridge north of the Rodrigues Triple Junction were studied geochemically and mineralogically. Vernadite (delta-MnO2) is the main mineral oxide phase. 230Thxs and Co concentrations suggest high growth rates of up to 29 mm/Myr and a maximum age of the basal crust layer of 1 Ma. Whereas most of the major and minor elements show concentrations which are typical of hydrogenetic formation, Co, Pb, Ni and Ti concentrations are strikingly lower. Concentrations and distribution of the strictly trivalent rare-earths and yttrium (REY) are typical of hydrogenetic ferromanganese oxide precipitates, but in marked contrast, the crusts are characterized by negative CeSN (shale normalized) anomalies and (Ce/Pr)SN ratios less than unity. Profiles through the crusts reveal only minor variations of the REY distribution and (Ce/Pr)SN ratios range from 0.45 to 0.68 (compared to ratios of up to 2 for typical hydrogenetic crusts from the Central Indian Basin). The apparent bulk partition coefficients between the crusts and seawater suggest that for the strictly trivalent REY the adsorption-desorption equilibrium has been reached. Positive Ce anomalies in the partition coefficient patterns reveal preferential uptake of Ce, but to a lesser extent than in normal hydrogenetic crusts. A new parameter (excess Ce, Cexs) to quantify the degree of decoupling of Ce from REY(III) is established on the basis of partition coefficients. Cexs/Cebulk ratios suggest that the CIR crusts formed by precipitation of Fe-Mn oxides from a hydrothermal plume and that in hydrothermal plumes and normal seawater the enrichment of Ce results from the same oxidative sorption process. The growth rates, calculated with 230Thxs data as well as with the Co formula, are inversely related to Cexs.
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En septiembre del año 2000, los gobiernos de 189 países adoptaron en Naciones Unidas un acuerdo global para combatir la desigualdad y mejorar el desarrollo humano en el mundo, con un horizonte puesto en el año 2015. Una de sus metas en este compromiso, llamado ?Los Objetivos de Desarrollo del Milenio?, consiste en reducir la pobreza extrema a la mitad. Específicamente, las autoridades de la República Argentina acordaron ?erradicar la indigencia y el hambre? entre 1990 y 2015, con una meta adicional consistente en ?reducir la pobreza a menos del 20 ?. En tiempos de grandes diferencias entre las estadísticas oficiales ?que están indicando mejores condiciones de vida en estos últimos años??y los informes de la oposición, de las consultoras privadas y de la Iglesia ?los cuales exhiben una posición contraria?, se desprende que la preocupación por erradicar el hambre está implícitamente presente en todos los sectores. Dada la cercanía de la fecha establecida como límite, se considera de interés la posibilidad de construir un nuevo instrumento de medición: un indicador del hambre para el próximo quinquenio. Por la complejidad del tema, esta propuesta innovadora presenta lineamientos básicos tendientes a la elaboración de un indicador que pueda brindar un seguimiento del fenómeno del hambre en la región, como una alternativa ante la inexistencia de estadísticas oficiales actualizadas que lo midan. Para ello se sugiere un marco teórico inexistente, hasta donde se conoce, obligando a definir aspectos conceptuales de variables relevantes. Tener un conocimiento más riguroso sobre los hogares argentinos que padecen el flagelo del hambre y poder identificarlos permitirá una mejor distribución de los recursos y procurar, a no muy largo plazo, que ningún habitante se encuentre en situación de pobreza extrema
Resumo:
En septiembre del año 2000, los gobiernos de 189 países adoptaron en Naciones Unidas un acuerdo global para combatir la desigualdad y mejorar el desarrollo humano en el mundo, con un horizonte puesto en el año 2015. Una de sus metas en este compromiso, llamado ?Los Objetivos de Desarrollo del Milenio?, consiste en reducir la pobreza extrema a la mitad. Específicamente, las autoridades de la República Argentina acordaron ?erradicar la indigencia y el hambre? entre 1990 y 2015, con una meta adicional consistente en ?reducir la pobreza a menos del 20 ?. En tiempos de grandes diferencias entre las estadísticas oficiales ?que están indicando mejores condiciones de vida en estos últimos años??y los informes de la oposición, de las consultoras privadas y de la Iglesia ?los cuales exhiben una posición contraria?, se desprende que la preocupación por erradicar el hambre está implícitamente presente en todos los sectores. Dada la cercanía de la fecha establecida como límite, se considera de interés la posibilidad de construir un nuevo instrumento de medición: un indicador del hambre para el próximo quinquenio. Por la complejidad del tema, esta propuesta innovadora presenta lineamientos básicos tendientes a la elaboración de un indicador que pueda brindar un seguimiento del fenómeno del hambre en la región, como una alternativa ante la inexistencia de estadísticas oficiales actualizadas que lo midan. Para ello se sugiere un marco teórico inexistente, hasta donde se conoce, obligando a definir aspectos conceptuales de variables relevantes. Tener un conocimiento más riguroso sobre los hogares argentinos que padecen el flagelo del hambre y poder identificarlos permitirá una mejor distribución de los recursos y procurar, a no muy largo plazo, que ningún habitante se encuentre en situación de pobreza extrema
Resumo:
En septiembre del año 2000, los gobiernos de 189 países adoptaron en Naciones Unidas un acuerdo global para combatir la desigualdad y mejorar el desarrollo humano en el mundo, con un horizonte puesto en el año 2015. Una de sus metas en este compromiso, llamado ?Los Objetivos de Desarrollo del Milenio?, consiste en reducir la pobreza extrema a la mitad. Específicamente, las autoridades de la República Argentina acordaron ?erradicar la indigencia y el hambre? entre 1990 y 2015, con una meta adicional consistente en ?reducir la pobreza a menos del 20 ?. En tiempos de grandes diferencias entre las estadísticas oficiales ?que están indicando mejores condiciones de vida en estos últimos años??y los informes de la oposición, de las consultoras privadas y de la Iglesia ?los cuales exhiben una posición contraria?, se desprende que la preocupación por erradicar el hambre está implícitamente presente en todos los sectores. Dada la cercanía de la fecha establecida como límite, se considera de interés la posibilidad de construir un nuevo instrumento de medición: un indicador del hambre para el próximo quinquenio. Por la complejidad del tema, esta propuesta innovadora presenta lineamientos básicos tendientes a la elaboración de un indicador que pueda brindar un seguimiento del fenómeno del hambre en la región, como una alternativa ante la inexistencia de estadísticas oficiales actualizadas que lo midan. Para ello se sugiere un marco teórico inexistente, hasta donde se conoce, obligando a definir aspectos conceptuales de variables relevantes. Tener un conocimiento más riguroso sobre los hogares argentinos que padecen el flagelo del hambre y poder identificarlos permitirá una mejor distribución de los recursos y procurar, a no muy largo plazo, que ningún habitante se encuentre en situación de pobreza extrema
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Trace element contents in different types of recent botoom sediments of the Indian Ocean are given. Sediment samples were obtained during cruises of the P.P. Shirshov Institute of Oceanology, Moscow.
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Authigenic carbonates forming at an active methane-seep on the Makran accretionary prism mainly consist of aragonite in the form of microcrystalline, cryptocrystalline, and botryoidal phases. The d13Ccarbonate values are very negative (-49.0 to -44.0 per mill V-PDB), agreeing with microbial methane as dominant carbon source. The d18Ocarbonate values are exclusively positive (+ 3.0 to + 4.5 per mill V-PDB) and indicate precipitation in equilibrium with seawater at bottom water temperatures. The content of rare earth elements and yttrium (REE + Y) determined by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) and solution ICP-MS varies for each aragonite variety, with early microcrystalline aragonite yielding the highest, cryptocrystalline aragonite intermediate, and later botryoidal aragonite the lowest REE + Y concentrations. Shale-normalised REE + Y patterns of different types of authigenic carbonate reflect distinct pore fluid compositions during precipitation: Microcrystalline aragonite shows high contents of middle rare earth elements (MREE), reflecting REE patterns ascribed to anoxic pore water. Cryptocrystalline aragonite exhibits a seawater-like REE + Y pattern at elevated total REE + Y concentrations, indicating higher concentrations of REEs in pore waters, which were influenced by seawater. Botryoidal aragonite is characterised by seawater-like REE + Y patterns at initial growth stages followed by an increase of light rare earth elements (LREE) with advancing crystal growth, reflecting changing pore fluid composition during precipitation of this cement. Conventional sample preparation involving micro-drilling of carbonate phases and subsequent solution ICP-MS does not allow to recognise such subtle changes in the REE + Y composition of individual carbonate phases. To be able to reconstruct the evolution of pore water composition during early diagenesis, an analytical approach is required that allows to track the changing elemental composition in a paragenetic sequence as well as in individual phases. High-resolution analysis of seep carbonates from the Makran accretionary prism by LA-ICP-MS reveals that pore fluid composition not only evolved in the course of the formation of different phases, but also changed during the precipitation of individual phases.
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The book is devoted to comprehensive study of composition of sediments from the North Pacific Ocean. The sediments have been divided characterized by their lithologic and facial types, grain size composition and mineralogy. Influence of volcanism on formation of mineral and chemical composition of these sediments has been shown. Regularities of distribution of sediment accumulation rates and of a number of chemical elements on the Transpacific profile have been found. Determining role of mechanical fractionation in their localization has been shown.