ATP activates ataxia-telangiectasia mutated (ATM) in vitro - Importance of autophosphorylation

Ataxia-telangiectasia Mutated (ATM), mutated in the human disorder ataxia-telangiectasia, is rapidly activated by DNA double strand breaks. The mechanism of activation remains unresolved, and it is uncertain whether autophosphorylation contributes to activation. We describe an in vitro immunoprecipitation system demonstrating activation of ATM kinase from unirradiated extracts by preincubation with ATP. Activation is both time- and ATP concentration-dependent, other nucleotides fail to activate ATM, and DNA is not required. ATP activation is specific for ATM since it is not observed with kinase-dead ATM, it requires Mn2+, and it is inhibited by wortmannin. Exposure of activated ATM to phosphatase abrogates activity, and repeat cycles of ATP and phosphatase treatment reveal a requirement for autophosphorylation in the activation process. Phosphopeptide mapping revealed similarities between the patterns of autophosphorylation for irradiated and ATP-treated ATM. Caffeine inhibited ATM kinase activity for substrates but did not interfere with ATM autophosphorylation. ATP failed to activate either A-T and rad3-related protein (ATR) or DNA-dependent protein kinase under these conditions, supporting the specificity for ATM. These data demonstrate that ATP can specifically induce activation of ATM by a mechanism involving autophosphorylation. The relationship of this activation to DNA damage activation remains unclear but represents a useful model for understanding in vivo activation.

Stratification of the earth beneath the Azores from P and S receiver functions

Seismic recordings of IRIS/IDA/GSN station CMLA and of several temporary stations in the Azores archipelago are processed with P and S receiver function (PRF and SRF) techniques. Contrary to regional seismic tomography these methods provide estimates of the absolute velocities and of the Vp/Vs ratio up to a depth of similar to 300 km. Joint inversion of PRFs and SRFs for a few data sets consistently reveals a division of the subsurface medium into four zones with a distinctly different Vp/Vs ratio: the crust similar to 20 km thick with a ratio of similar to 1.9 in the lower crust, the high-Vs mantle lid with a strongly reduced VpNs velocity ratio relative to the standard 1.8, the low-velocity zone (LVZ) with a velocity ratio of similar to 2.0, and the underlying upper-mantle layer with a standard velocity ratio. Our estimates of crustal thickness greatly exceed previous estimates (similar to 10 km). The base of the high-Vs lid (the Gutenberg discontinuity) is at a depth of-SO km. The LVZ with a reduction of S velocity of similar to 15% relative to the standard (IASP91) model is terminated at a depth of similar to 200 km. The average thickness of the mantle transition zone (TZ) is evaluated from the time difference between the S410p and SKS660p, seismic phases that are robustly detected in the S and SKS receiver functions. This thickness is practically similar to the standard IASP91 value of 250 km. and is characteristic of a large region of the North Atlantic outside the Azores plateau. Our data are indicative of a reduction of the S-wave velocity of several percent relative to the standard velocity in a depth interval from 460 to 500 km. This reduction is found in the nearest vicinities of the Azores, in the region sampled by the PRFs, but, as evidenced by SRFs, it is missing at a distance of a few hundred kilometers from the islands. We speculate that this anomaly may correspond to the source of a plume which generated the Azores hotspot. Previously, a low S velocity in this depth range was found with SRF techniques beneath a few other hotspots.

Cape Verde hotspot from the upper crust to the top of the lower mantle

We investigate the crust, upper mantle and mantle transition zone of the Cape Verde hotspot by using seismic P and S receiver functions from several tens of local seismograph stations. We find a strong discontinuity at a depth of similar to 10 km underlain by a similar to 15-km thick layer with a high (similar to 1.9) Vp/Vs velocity ratio. We interpret this discontinuity and the underlying layer as the fossil Moho, inherited from the pre-hotspot era, and the plume-related magmatic underplate. Our uppermost-mantle models are very different from those previously obtained for this region: our S velocity is much lower and there are no indications of low densities. Contrary to previously published arguments for the standard transition zone thickness our data indicate that this thickness under the Cape Verde islands is up to similar to 30 km less than in the ambient mantle. This reduction is a combined effect of a depression of the 410-km discontinuity and an uplift of the 660-km discontinuity. The uplift is in contrast to laboratory data and some seismic data on a negligible dependence of depth of the 660-km discontinuity on temperature in hotspots. A large negative pressure-temperature slope which is suggested by our data implies that the 660-km discontinuity may resist passage of the plume. Our data reveal beneath the islands a reduction of S velocity of a few percent between 470-km and 510-km depths. The low velocity layer in the upper transition zone under the Cape Verde archipelago is very similar to that previously found under the Azores and a few other hotspots. In the literature there are reports on a regional 520-km discontinuity, the impedance of which is too large to be explained by the known phase transitions. Our observations suggest that the 520-km discontinuity may present the base of the low-velocity layer in the transition zone. (C) 2011 Elsevier B.V. All rights reserved.

Stability of fractional order systems

The theory and applications of fractional calculus (FC) had a considerable progress during the last years. Dynamical systems and control are one of the most active areas, and several authors focused on the stability of fractional order systems. Nevertheless, due to the multitude of efforts in a short period of time, contributions are scattered along the literature, and it becomes difficult for researchers to have a complete and systematic picture of the present day knowledge. This paper is an attempt to overcome this situation by reviewing the state of the art and putting this topic in a systematic form. While the problem is formulated with rigour, from the mathematical point of view, the exposition intends to be easy to read by the applied researchers. Different types of systems are considered, namely, linear/nonlinear, positive, with delay, distributed, and continuous/discrete. Several possible routes of future progress that emerge are also tackled.

Mantle beneath the Gibraltar Arc from receiver functions

P and S receiver functions (PRF and SRF) from 19 seismograph stations in the Gibraltar Arc and the Iberian Massif reveal new details of the regional deep structure. Within the high-velocity mantle body below southern Spain the 660-km discontinuity is depressed by at least 20 km. The Ps phase from the 410-km discontinuity is missing at most stations in the Gibraltar Arc. A thin (similar to 50 km) low-S-velocity layer atop the 410-km discontinuity is found under the Atlantic margin. At most stations the S410p phase in the SRFs arrives 1.0-2.5 s earlier than predicted by IASP91 model, but, for the propagation paths through the upper mantle below southern Spain, the arrivals of S410p are delayed by up to +1.5 s. The early arrivals can be explained by elevated Vp/Vs ratio in the upper mantle or by a depressed 410-km discontinuity. The positive residuals are indicative of a low (similar to 1.7 versus similar to 1.8 in IASP91) Vp/Vs ratio. Previously, the low ratio was found in depleted lithosphere of Precambrian cratons. From simultaneous inversion of the PRFs and SRFs we recognize two types of the mantle: 'continental' and 'oceanic'. In the 'continental' upper mantle the S-wave velocity in the high-velocity lid is 4.4-4.5 km s(-1), the S-velocity contrast between the lid and the underlying mantle is often near the limit of resolution (0.1 km s(-1)), and the bottom of the lid is at a depth reaching 90 100 km. In the 'oceanic' domain, the S-wave velocities in the lid and the underlying mantle are typically 4.2-4.3 and similar to 4.0 km s(-1), respectively. The bottom of the lid is at a shallow depth (around 50 km), and at some locations the lid is replaced by a low S-wave velocity layer. The narrow S-N-oriented band of earthquakes at depths from 70 to 120 km in the Alboran Sea is in the 'continental' domain, near the boundary between the 'continental' and 'oceanic' domains, and the intermediate seismicity may be an effect of ongoing destruction of the continental lithosphere.

Systematic identification of genomic markers of drug sensitivity in cancer cells.

Clinical responses to anticancer therapies are often restricted to a subset of patients. In some cases, mutated cancer genes are potent biomarkers for responses to targeted agents. Here, to uncover new biomarkers of sensitivity and resistance to cancer therapeutics, we screened a panel of several hundred cancer cell lines--which represent much of the tissue-type and genetic diversity of human cancers--with 130 drugs under clinical and preclinical investigation. In aggregate, we found that mutated cancer genes were associated with cellular response to most currently available cancer drugs. Classic oncogene addiction paradigms were modified by additional tissue-specific or expression biomarkers, and some frequently mutated genes were associated with sensitivity to a broad range of therapeutic agents. Unexpected relationships were revealed, including the marked sensitivity of Ewing's sarcoma cells harbouring the EWS (also known as EWSR1)-FLI1 gene translocation to poly(ADP-ribose) polymerase (PARP) inhibitors. By linking drug activity to the functional complexity of cancer genomes, systematic pharmacogenomic profiling in cancer cell lines provides a powerful biomarker discovery platform to guide rational cancer therapeutic strategies.

Anàlisi de l'obra cinematogràfica de quatre documentalistes russos o de repúbliques ex-soviètiques : la relació amb les noves tendències del documental i el llegat soviètic

El treball de recerca té com a principal objectiu l'estudi del cinema documental rus contemporani a través de l'obra cinematogràfica d'Alexander Sokurov, Sergei Dvortsevoi, Sergei Loznitsa i Victor Kossakovski. En un primer moment la investigació s'havia encaminat en un estudi comparatiu sobre les noves tendències del documental i els models de realisme proposats des de la Rússia post-comunista. El treball s'ha realitzat a partir de tres vies d'investigació. La primera ha consistit en una exhaustiva recerca bibliogràfica sobre cinema documental i cinema soviètic. La segona s'ha plantejat a partir d'un anàlisi acurat de les diverses pel•lícules. Finalment, la tercera via s'ha desenvolupat a partir d'un treball de camp realitzat durant una estada a Rússia, un període en el qual va ser possible entrevistar dos dels cineastes protagonistes de l'estudi, Sergei Dvortsevoi i Victor Kossakovski, així com el crític de cinema Andrei Xemijakin. També va ser fonamental l'assistència a la taula rodona i la master class impartida per Sergei Loznitsa en el marc del desè aniversari del Màster en Teoria i Pràctica de Documental Creatiu de la Universitat Autònoma de Barcelona. Tot i que es poden traçar vincles entre el treball dels quatre cineastes escollits i algunes de les pràctiques contemporànies en l'àmbit de la no-ficció, com pot ser l'experiència de Sergei Loznitsa en el terreny del found-footage, o els documentals experimentals de caràcter assagístic d'Alexander Sokurov, així com la tendència observacional i el pas al cinema de ficció de Segei Dvortsevoi, o l'ús de la tecnologia digital en les últimes pel•lícules de Victor Kossakovski. Tot i aquestes aproximacions, es pot afirmar que el model de realisme proposat per aquests cineastes troba el seu autèntic llegat en el cinema soviètic. Una herència que comença amb el cinema de Dziga Vertov –pioner del documental artístic i revolucionari- i acaba en el d'Artavadz Pelechian.

Insect trypanosomatids: the need to know more

Of ten recognized trypanosomatid genera, only two -- pathogenic Trypanosoma and Leishmania -- have been actively investigated for any length of time while the plant flagellates -- Phytomonas -- have recently begun to attract attention due to their role as agricultural parasites. The remaining genera that comprise parasites associated with insects have been largely neglected except for two or three containing popular isolates. This publication reviews current knowledge of trypanosomatids from insects.

Phylogeny of the kinetoplastida: taxonomic problems and insights into the evolution of parasitism

To further investigate phylogeny of kinetoplastid protozoa, the sequences of small subunit (18S) ribosomal RNA of nine bodonid isolates and ten isolates of insect trypanosomatids have been determined. The root of the kinetoplastid tree was attached to the branch of Bodo designis and/or Cruzella marina. The suborder Trypanosomatina appeared as a monophyletic group, while the suborder Bodonina was paraphyletic. Among bodonid lineages, parasitic organisms were intermingled with free-living ones, implying multiple transitions to parasitism and supporting the `vertebrate-first hypothesis'. The tree indicated that the genera Cryptobia and Bodo are artificial taxa. Separation of fish cryptobias and Trypanoplasma borreli as different genera was not supported. In trypanosomatids, the genera Leptomonas and Blastocrithidia were polyphyletic, similar to the genera Herpetomonas and Crithidia and in contrast to the monophyletic genera Trypanosoma and Phytomonas. This analysis has shown that the morphological classification of kinetoplastids does not in general reflect their genetic affinities and needs a revision.

Anàlisi de l'obra cinematogràfica de quatre documentalistes russos o de repúbliques ex-soviètiques: la relació amb les noves tendències del documental i el llegat soviètic.

El treball de recerca té com a principal objectiu l'estudi del cinema documental rus contemporani a través de l'obra cinematogràfica d'Alexander Sokurov, Sergei Dvortsevoi, Sergei Loznitsa i Victor Kossakovski. En un primer moment la investigació s'havia encaminat en un estudi comparatiu sobre les noves tendències del documental i els models de realisme proposats des de la Rússia post-comunista. El treball s'ha realitzat a partir de tres vies d'investigació. La primera ha consistit en una exhaustiva recerca bibliogràfica sobre cinema documental i cinema soviètic. La segona s'ha plantejat a partir d'un anàlisi acurat de les diverses pel•lícules. Finalment, la tercera via s'ha desenvolupat a partir d'un treball de camp realitzat durant una estada a Rússia, un període en el qual va ser possible entrevistar dos dels cineastes protagonistes de l'estudi, Sergei Dvortsevoi i Victor Kossakovski, així com el crític de cinema Andrei Xemijakin. També va ser fonamental l'assistència a la taula rodona i la master class impartida per Sergei Loznitsa en el marc del desè aniversari del Màster en Teoria i Pràctica de Documental Creatiu de la Universitat Autònoma de Barcelona. Tot i que es poden traçar vincles entre el treball dels quatre cineastes escollits i algunes de les pràctiques contemporànies en l'àmbit de la no-ficció, com pot ser l'experiència de Sergei Loznitsa en el terreny del found-footage, o els documentals experimentals de caràcter assagístic d'Alexander Sokurov, així com la tendència observacional i el pas al cinema de ficció de Segei Dvortsevoi, o l'ús de la tecnologia digital en les últimes pel•lícules de Victor Kossakovski. Tot i aquestes aproximacions, es pot afirmar que el model de realisme proposat per aquests cineastes troba el seu autèntic llegat en el cinema soviètic. Una herència que comença amb el cinema de Dziga Vertov –pioner del documental artístic i revolucionari- i acaba en el d'Artavadz Pelechian –cineasta armeni i un dels màxims representatnts del documental poètic-. El treball de recerca ha estat presentat en forma de comunicació en el congrés internacional “IMAGEing Reality: Representing the Real in Film, Television and New Media”, celebrat a Pamplona el mes d'Octubre de 2009. La comunicació s'ha redactat en format article i està pendent de publicació.

Speed of reaction-diffusion fronts in spatially heterogeneous media

The front speed problem for nonuniform reaction rate and diffusion coefficient is studied by using singular perturbation analysis, the geometric approach of Hamilton-Jacobi dynamics, and the local speed approach. Exact and perturbed expressions for the front speed are obtained in the limit of large times. For linear and fractal heterogeneities, the analytic results have been compared with numerical results exhibiting a good agreement. Finally we reach a general expression for the speed of the front in the case of smooth and weak heterogeneities

Sons de Korotkoff: desenvolvimento da pesquisa em esfigmomanometria na Escola de Enfermagem da USP

Este artigo tem como objetivos reverenciar Sergei Nicolai Korotkoff por ocasião do centenário da descoberta do método auscultatório de medida da pressão arterial na Rússia, em 1905; relatar os fatos que culminaram no desenvolvimento da esfigmomanometria no Brasil; historiar a valiosa contribuição da Escola de Enfermagem da Universidade de São Paulo (EEUSP) no desenvolvimento da pesquisa, na área da medida da pressão e analisar o produto da linha de pesquisa "Influência da Largura do Manguito na Medida da Pressão Arterial", gerada na EEUSP a partir de 1974. O artigo relata a consolidação dos achados iniciais pelos estudos que permitiram a formação dos primeiros doutores na área, que sugere a confirmação de hipóteses em estudos longitudinais.

Two complementary molecular energy decomposition schemes: the Mayer and Ziegler-Rauk methods in comparison

In the present paper we discuss and compare two different energy decomposition schemes: Mayer's Hartree-Fock energy decomposition into diatomic and monoatomic contributions [Chem. Phys. Lett. 382, 265 (2003)], and the Ziegler-Rauk dissociation energy decomposition [Inorg. Chem. 18, 1558 (1979)]. The Ziegler-Rauk scheme is based on a separation of a molecule into fragments, while Mayer's scheme can be used in the cases where a fragmentation of the system in clearly separable parts is not possible. In the Mayer scheme, the density of a free atom is deformed to give the one-atom Mulliken density that subsequently interacts to give rise to the diatomic interaction energy. We give a detailed analysis of the diatomic energy contributions in the Mayer scheme and a close look onto the one-atom Mulliken densities. The Mulliken density ρA has a single large maximum around the nuclear position of the atom A, but exhibits slightly negative values in the vicinity of neighboring atoms. The main connecting point between both analysis schemes is the electrostatic energy. Both decomposition schemes utilize the same electrostatic energy expression, but differ in how fragment densities are defined. In the Mayer scheme, the electrostatic component originates from the interaction of the Mulliken densities, while in the Ziegler-Rauk scheme, the undisturbed fragment densities interact. The values of the electrostatic energy resulting from the two schemes differ significantly but typically have the same order of magnitude. Both methods are useful and complementary since Mayer's decomposition focuses on the energy of the finally formed molecule, whereas the Ziegler-Rauk scheme describes the bond formation starting from undeformed fragment densities