High prevalence anti-Trypanosoma cruzi antibodies, among blood donors in the State of Puebla, a non-endemic area of Mexico

Blood transfusion is the second most common transmission route of Chagas disease in many Latin American countries. In Mexico, the prevalence of Chagas disease and impact of transfusion of Trypanosoma cruzi-contaminated blood is not clear. We determined the seropositivity to T. cruzi in a representative random sample, of 2,140 blood donors (1,423 men and 647 women, aged 19-65 years), from a non-endemic state of almost 5 millions of inhabitants by the indirect hemagglutination (IHA) and enzyme linked immunosorbent assay (ELISA) tests using one autochthonous antigen from T. cruzi parasites, which were genetically characterized like TBAR/ME/1997/RyC-V1 (T. cruzi I) isolated from a Triatoma barberi specimen collected in the same locality. The seropositivity was up to 8.5% and 9% with IHA and ELISA tests, respectively, and up to 7.7% using both tests in common. We found high seroprevalence in a non-endemic area of Mexico, comparable to endemic countries where the disease occurs, e.g. Brazil (0.7%), Bolivia (13.7%) and Argentina (3.5%). The highest values observed in samples from urban areas, associated to continuous rural emigration and the absence of control in blood donors, suggest unsuspected high risk of transmission of T. cruzi, higher than those reported for infections by blood e.g. hepatitis (0.1%) and AIDS (0.1%) in the same region.

Bloodstream infections in late-stage acquired immunodeficiency syndrome patients evaluated by a lysis centrifugation system

Opportunistic infections, which affect acquired immunodeficiency syndrome (Aids) patients, are frequently disseminated and may cause bloodstream infections (BSI). The aim of this study was to evaluate the main causes of BSI in Aids patients with advanced stage of the disease, with special emphasis on the identification of fungemia. During a 21 months period, all patients with Aids (CD4 < 200) and febrile syndrome admitted to 3 university hospitals were systematically evaluated. For each patient presenting fever, a pair of blood cultures was collected and processed by using a commercial lysis-centrifugation system. One hundred and eleven patients (75 males) with a mean age of 36 years (median 33 years) and mean CD4 count of 64 cells/ml were included. Among the 111 patients evaluated we documented 54 episodes of BSI, including 46 patients with truly systemic infections and 8 episodes considered as contaminants. BSI were caused by gram-positive bacteria (43%), fungi (20%), gram-negative bacteria (15%), mycobacteria (15%), and mixed flora (7%). The crude mortality rate of our patients was 39%, being 50% for patients with BSI and 31% for the others. In conclusion, BSI are a common related to systemic infections on Aids patients with advanced stage of disease and is associated with a high rate of mortality.

Clinical forms of Trypanosoma cruzi infected individuals in the chronic phase of Chagas disease in Puebla, Mexico

In Mexico, despite the relatively high seroprevalence of Trypanosoma cruzi infection in humans in some areas, reported morbidity of Chagas disease is not clear. We determined clinical stage in 71 individuals seropositive to T. cruzi in the state of Puebla, Mexico, an area endemic for Chagas disease with a reported seroprevalence of 7.7%. Diagnosis of Chagas disease was made by two standardized serological tests (ELISA, IHA). Individuals were stratified according to clinical studies. All patients were submitted to EKG, barium swallow, and barium enema. Groups were identified as indeterminate form (IF) asymptomatic individuals without evidence of abnormalities (n = 34 cases); those with gastrointestinal alterations (12 patients) including symptoms of abnormal relaxation of the lower esophageal sphincter and absent peristalsis in the esophageal body, grade I megaesophagus, and/or megacolon; patients with clinical manifestations and documented changes of chronic Chagas heart disease who were subdivided as follows: mild (8 patients) - mild electrocardiographic changes of ventricular repolarization, sinus bradychardia); moderate (6 patients) - left bundle branch block, right bundle branch block associated with left anterior fascicular block); severe (8 patients) - signs of cardiomegaly, dilated cardiomyopathy); and the associated form (3 cases) that included presence of both cardiomyopathy and megaesophagus. These data highlight the importance of accurate evaluation of the prevalence and clinical course of Chagas disease in endemic and non-endemic areas of Mexico.

Four whole-istic aspects of schistosome granuloma biology: fractal arrangement, internal regulation, autopoietic component and closure

This paper centers on some whole-istic organizational and functional aspects of hepatic Schistosoma mansoni granuloma, which is an extremely complex system. First, it structurally develops a collagenic topology, originated bidirectionally from an inward and outward assembly of growth units. Inward growth appears to be originated from myofibroblasts derived from small portal vessel around intravascular entrapped eggs, while outward growth arises from hepatic stellate cells. The auto-assembly of the growth units defines the three-dimensional scaffold of the schistosome granulomas. The granuloma surface irregularity and its border presented fractal dimension equal to 1.58. Second, it is internally regulated by intricate networks of immuneneuroendocrine stimuli orchestrated by leptin and leptin receptors, substance P and Vasoactive intestinal peptide. Third, it can reach the population of ± 40,000 cells and presents an autopoietic component evidenced by internal proliferation (Ki-67+ Cells), and by expression of c-Kit+ Cells, leptin and leptin receptor (Ob-R), granulocyte-colony stimulating factor (G-CSF-R), and erythropoietin (Epo-R) receptors. Fourth, the granulomas cells are intimately connected by pan-cadherins, occludin and connexin-43, building a state of closing (granuloma closure). In conclusion, the granuloma is characterized by transitory stages in such a way that its organized structure emerges as a global property which is greater than the sum of actions of its individual cells and extracellular matrix components.

Metallothionein-1 and nitric oxide expression are inversely correlated in a murine model of Chagas disease

Chagas disease, caused by Trypanosoma cruzi, represents an endemic among Latin America countries. The participation of free radicals, especially nitric oxide (NO), has been demonstrated in the pathophysiology of seropositive individuals with T. cruzi. In Chagas disease, increased NO contributes to the development of cardiomyopathy and megacolon. Metallothioneins (MTs) are efficient free radicals scavengers of NO in vitro and in vivo. Here, we developed a murine model of the chronic phase of Chagas disease using endemic T. cruzi RyCH1 in BALB/c mice, which were divided into four groups: infected non-treated (Inf), infected N-monomethyl-L-arginine treated (Inf L-NAME), non-infected L-NAME treated and non-infected vehicle-treated. We determined blood parasitaemia and NO levels, the extent of parasite nests in tissues and liver MT-I expression levels. It was observed that NO levels were increasing in Inf mice in a time-dependent manner. Inf L-NAME mice had fewer T. cruzi nests in cardiac and skeletal muscle with decreased blood NO levels at day 135 post infection. This affect was negatively correlated with an increase of MT-I expression (r = -0.8462, p < 0.0001). In conclusion, we determined that in Chagas disease, an unknown inhibitory mechanism reduces MT-I expression, allowing augmented NO levels.

Sr, C and O isotope systematics in the Pucara Basin, central Peru - Comparison between Mississippi Valley-type deposits and barren areas

A combined Sr, O and C isotope study has been carried out in the Pucara basin, central Peru, to compare local isotopic trends of the San Vicente and Shalipayco Zn-Pb Mississippi Valley-type (MVT) deposits with regional geochemical patterns of the sedimentary host basin. Gypsum, limestone and regional replacement dolomite yield Sr-87/Sr-86 ratios that fall within or slightly below the published range of seawater Sr-87/Sr-86 values for the Lower Jurassic and the Upper Triassic. Our data indicate that the Sr isotopic composition of seawater between the Hettangian and the Toarcian may extend to lower Sr-87/Sr-86 ratios than previously published values. An Sr-87-enrichment is noted in (1) carbonate rocks from the lowermost part of the Pucara basin, and (2) different carbonate generations at the MVT deposits. This indicates that host rocks at MVT deposits and in the lowermost part of the carbonate sequence interacted with Sr-87-enriched fluids. The fluids acquired their radiogenic nature by interaction with lithologies underlying the carbonate rocks of the Pucara basin. The San Ramon granite, similar Permo-Triassic intrusions and their elastic derivatives in the Mitu Group are likely sources of radiogenic Sr-87. The Brazilian shield and its erosion products are an additional potential source of radiogenic Sr-87. Volcanic rocks of the Mitu Group are not a significant source for radiogenic Sr-87; however, molasse-type sedimentary rocks and volcaniclastic rocks cannot be ruled out as a possible source of radiogenic Sr-87. The marked enrichment in Sr-87 of carbonates toward the lower part of the Pucara Group is accompanied by only a slight decrease in delta(18)O values and essentially no change in delta(13)C values, whereas replacement dolomite and sparry carbonates at the MVT deposits display a coherent trend of progressive Sr-87-enrichment, and O-18- and C-13-depletion. The depletion in O-18 in carbonates from the MVT deposits are likely related to a temperature increase, possibly coupled with a O-18-enrichment of the ore-forming fluids. Progressively lower delta(13)C values throughout the paragenetic sequence at the MVT deposits are interpreted as a gradually more important contribution from organically derived carbon. Quantitative calculations show that a single fluid-rock interaction model satisfactorily reproduces the marked Sr-87-enrichment and the slight decrease in delta(18)O values in carbonate rocks from the lower part of the Pucara Group. By contrast, the isotopic covariation trends of the MVT deposits are better reproduced by a model combining fluid mixing and fluid-rock interaction. The modelled ore-bearing fluids have a range of compositions between a hot, saline, radiogenic brine that had interacted with lithologies underlying the Pucara sequence and cooler, dilute brines possibly representing local fluids within the Pucara sequence. The composition of the local fluids varies according to the nature of the lithologies present in the neighborhood of the different MVT deposits. The proportion of the radiogenic fluid in the modelled fluid mixtures interacting with the carbonate host rocks at the MVT deposits decreases as one moves up in the stratigraphic sequence of the Pucara Group.

Modification of the Perrine-Baum diagram to improve the calculation of high voltage electric lines

Through the history of Electrical Engineering education, vectorial and phasorial diagrams have been used as a fundamental learning tool. At present, computational power has replaced them by long data lists, the result of solving equation systems by means of numerical methods. In this sense, diagrams have been shifted to an academic background and although theoretically explained, they are not used in a practical way within specific examples. This fact may be against the understanding of the complex behavior of the electrical power systems by students. This article proposes a modification of the classical Perrine-Baum diagram construction to allowing both a more practical representation and a better understanding of the behavior of a high-voltage electric line under different levels of load. This modification allows, at the same time, the forecast of the obsolescence of this behavior and line’s loading capacity. Complementary, we evaluate the impact of this tool in the learning process showing comparative undergraduate results during three academic years

Genetic characterization of the ABO blood group in Neandertals

Background: The high polymorphism rate in the human ABO blood group gene seems to be related to susceptibility to different pathogens. It has been estimated that all genetic variation underlying the human ABO alleles appeared along the human lineage, after the divergence from the chimpanzee lineage. A paleogenetic analysis of the ABO blood group gene in Neandertals allows us to directly test for the presence of the ABO alleles in these extinct humans. Results: We have analysed two male Neandertals that were retrieved under controlled conditions at the El Sidron site in Asturias (Spain) and that appeared to be almost free of modern human DNA contamination. We find a human specific diagnostic deletion for blood group O (O01 haplotype) in both Neandertal individuals. Conclusion: These results suggest that the genetic change responsible for the O blood group in humans predates the human and Neandertal divergence. A potential selective event associated with the emergence of the O allele may have therefore occurred after humans separated from their common ancestor with chimpanzees and before the human-Neandertal population divergence.

Focused time-lapse inversion of radio and audio magnetotelluric data

Geoelectrical techniques are widely used to monitor groundwater processes, while surprisingly few studies have considered audio (AMT) and radio (RMT) magnetotellurics for such purposes. In this numerical investigation, we analyze to what extent inversion results based on AMT and RMT monitoring data can be improved by (1) time-lapse difference inversion; (2) incorporation of statistical information about the expected model update (i.e., the model regularization is based on a geostatistical model); (3) using alternative model norms to quantify temporal changes (i.e., approximations of l(1) and Cauchy norms using iteratively reweighted least-squares), (4) constraining model updates to predefined ranges (i.e., using Lagrange Multipliers to only allow either increases or decreases of electrical resistivity with respect to background conditions). To do so, we consider a simple illustrative model and a more realistic test case related to seawater intrusion. The results are encouraging and show significant improvements when using time-lapse difference inversion with non l(2) model norms. Artifacts that may arise when imposing compactness of regions with temporal changes can be suppressed through inequality constraints to yield models without oscillations outside the true region of temporal changes. Based on these results, we recommend approximate l(1)-norm solutions as they can resolve both sharp and smooth interfaces within the same model. (C) 2012 Elsevier B.V. All rights reserved.

Comunidade política, imigração e coesão social: o caso português

This work contributes to an understanding of how the existence of multiple ethnic- cultural belongings in the political community concurs with the maintenance of a socially cohesive and politically united community. Considering the immigration reality in Portugal, we tried to identify the bonds that link immigrants to the political community and how those bonds can be mobilized to integrate immigrants in a common living project inside the national territory. Methodologically, this investigation is based in a qualitative and quantitative analysis of the policies and measures applied in Portugal in the immigration sphere, as well as the results of the empirical work we carried out with two immigration groups (Brazilians and Cape Verdeans) living in Lisbon’s metropolitan area, and the answers to a survey we sent to immigrant associations. The results of this research revealed the existence of a certain political ambivalence concerning the immigrant integration process, which expresses itself to a certain degree in the way national citizens and immigrants appraise the immigrant contribution to Portuguese society. The prevailing and blurred idea states that immigration expenses don’t make up for the benefits, and that is likely to influence the mutual relationship established between the two. Despite the existence of objective situations of social and economic disparity and despite a feeling of discrimination shared between immigrants, it is possible to identify a progressive citizenship universalization and the formal acceptance of immigrant religious and cultural traditions, even though the Portuguese parliament does not reflect such diversity. Thus, we perceive the possibility of warranting specific ethnic and cultural minority rights without the ethnicization or culturalization of political representation, and the general standards that serve as a backbone to the national political community might be enough to warrant that protection. Notwithstanding, some signs suggest that immigrant access to public sphere might not be easy, and this might have repercussions in the visibility and in the public discussion of demands, with outcomes on the type of integration policies Portugal applies.

Caracterização etnopedológica de Planossolos utilizados em cerâmica artesanal no Agreste Paraibano

Técnicas adaptadas da etnociência clássica foram utilizadas para descrever e avaliar os conhecimentos de um grupo de artesãos camponeses do Agreste Paraibano sobre alguns solos que eles usam como recurso cerâmico. Cinco perfis de solo foram descritos por agrônomos-pesquisadores (abordagem eticista) e por camponeses (abordagem emicista), em locais onde a população local extrai material para cerâmica. Amostras coletadas em ambas as abordagens foram usadas para caracterização morfológica e analítica desses solos. Os camponeses pesquisados foram capazes de distinguir, identificar e nomear diversos materiais de solo, arranjados em estratos ao longo dos perfis de solo, de modo comparável ao arranjo dos horizontes pedogenéticos. A visão, o tato e o paladar foram empregados pelos artesãos na avaliação da qualidade do solo para cerâmica. Quatro perfis descritos junto às fontes de material cerâmico foram classificados como Planossolo Nátrico e um como Planossolo Háplico. A realização de pesquisas etnopedológicas em diferentes contextos sociais e pedológicos pode contribuir para o avanço da ciência do solo, sendo também uma oportunidade para melhor compreender as formas camponesas de conhecimento e manejo de solos.

Caracterização e classificação de cambissolos do arquipélago de Fernando de Noronha, Pernambuco

Este trabalho visou caracterizar e classificar Cambissolos de ocorrência comum no Arquipélago de Fernando de Noronha, com o objetivo de testar e contribuir para o desenvolvimento do Sistema Brasileiro de Classificação de Solos (SiBCS). Além disso, uma melhor compreensão desses solos e de sua distribuição na paisagem é de grande importância no planejamento do uso da terra, para nortear ações governamentais visando à exploração sustentável desse complexo turístico-ecológico. Com base no Mapa Detalhado de Solos do Arquipélago de Fernando de Noronha, seis perfis de Cambissolos representativos da área foram selecionados, descritos e coletados, visando à caracterização morfológica, física, química e mineralógica. Os Cambissolos foram adequadamente classificados segundo a nova versão do SiBCS, que incluiu o grande grupo "Ta eutroférrico", sugerido durante o desenvolvimento deste trabalho. Os solos do Arquipélago refletem nas suas propriedades as características marcantes do material de origem vulcânico, do clima tropical com franco domínio oceânico e do relevo. Os Cambissolos Háplicos Ta eutroférricos típicos ocupam as posições mais preservadas do planalto central da ilha principal e possuem os melhores atributos físicos e químicos para utilização agrícola ou geotécnica. Os Cambissolos Háplicos Ta eutróficos lépticos, relacionados com relevos acidentados e geralmente associados com Neossolos Litólicos e afloramentos de rocha, são solos que requerem proteção especial devido à sua alta instabilidade ao processo erosivo. Por sua vez, os Cambissolos Háplicos Sódicos vertissólicos, que ocorrem em áreas ligeiramente rebaixadas do planalto central, apresentam sérios problemas de drenagem e argilas expansivas. Quimicamente, os solos apresentam teores elevados a extremamente elevados de P extraível, de distribuição irregular tanto entre perfis como nos horizontes, o que sugere a influência de fontes distintas deste elemento.

Caracterização e classificação de Neossolos da Ilha de Fernando de Noronha (PE)

Na ilha principal do Arquipélago de Fernando de Noronha, condições peculiares de clima tropical, com franco domínio oceânico, e material de origem de natureza vulcânica contribuem para formação de solos pouco desenvolvidos, de especial interesse científico, particularmente no que tange à reestruturação do Sistema Brasileiro de Classificação de Solos (SiBCS). Com o objetivo de estudá-los, foram caracterizados morfológica, física, química e mineralogicamente e classificados sete perfis de Neossolos de ocorrência comum nesse ambiente insular, sendo dois Litólicos, um "Saprolítico", três Regolíticos e um Flúvico. Os Neossolos Litólicos apresentam contato lítico constituído por fragmentos de rocha a menos de 50 cm de profundidade. O Neossolo "Saprolítico" apresenta o contato lítico superior aos 50 cm de profundidade, porém precedido por rochas parcialmente decompostas (saprolito), que preservam ainda sua estrutura original. Os Neossolos Regolíticos estão relacionados aos depósitos sedimentares marinhos e são constituídos, predominantemente, por grãos bioclásticos carbonáticos. O Neossolo Flúvico, de origem colúvio-aluvial, apresenta camadas alternadas de materiais distintos, notoriamente, pela textura e mineralogia. Os Neossolos Litólicos foram adequadamente classificados segundo a nova versão do SiBCS (Embrapa, 2006), que inclui o subgrupo "fragmentário", sugerido durante o desenvolvimento deste trabalho. Os outros Neossolos não foram adequadamente enquadrados, ora por apresentarem características peculiares, ora pela ausência de termos mais apropriados, que melhor explicitassem suas características distintas. Sugere-se a inclusão no SiBCS da subordem dos Neossolos Saprolíticos, do grande grupo dos Neossolos Regolíticos Psamíticos, e dos subgrupos dos Neossolos Regolíticos Psamíticos bioclásticos carbonáticos e Neossolos Flúvicos Ta eutróficos bioclásticos carbonáticos.

Mineralogia de um Argissolo Vermelho-Amarelo da zona úmida costeira do Estado de Pernambuco

A mineralogia do solo constitui uma excelente ferramenta para o conhecimento e a avaliação da gênese do solo e do seu comportamento físico e químico, além de ser um dos parâmetros utilizados na distinção de classes do Sistema Brasileiro de Classificação de Solos e um indicativo da reserva potencial mineral de nutrientes para as plantas. Nesse contexto, este trabalho apresenta a caracterização mineralógica das frações cascalho, areia grossa e areia fina (sob lupa binocular e microscópio petrográfico) e das frações silte e argila (difratometria de raios X) de todos os horizontes do solo, e o estudo petrográfico da rocha matriz, a partir dos quais estabelece considerações sobre a evolução mineralógica de um Argissolo Vermelho-Amarelo, típico da Zona Úmida Costeira do Estado de Pernambuco. As frações grossas ao longo de todo o Argissolo estudado são constituídas, essencialmente, por quartzo (> 95 %) anguloso a muito anguloso, o que denota a ausência de transporte de material na formação desse tipo de solo. Foram observados fragmentos de rocha (constituídos por quartzo, feldspatos e minerais opacos), feldspatos e biotita que apresentam alteração intempérica mais evidente nos horizontes mais superficiais, além de minerais opacos, como magnetita e hematita, e traços de clorita, zircão, epidotos e apatita, todos de mineralogia compatível com a rocha matriz. A fração silte é constituída por minerais do grupo das micas, dos feldspatos, do quartzo e da caulinita, além da clorita observada apenas nos horizontes mais inferiores. A fração argila mostrou a mesma mineralogia da fração silte, sendo ainda detectados minerais interestratificados nos horizontes mais inferiores. A petrografia da rocha matriz mostrou que esta é um biotita-gnaisse de granulometria média, constituído por feldspatos (plagioclásio, pertita e microclina), quartzo, biotita e, como acessórios, epidotos, zircão e minerais opacos. A análise dos resultados permite concluir que o Argissolo estudado é autóctone, bem desenvolvido e altamente intemperizado devido às condições de clima, relevo e vegetação, apresentando baixa reserva potencial mineral de nutrientes para as plantas.

Relações solo-vegetação em áreas sob processo de desertificação no município de Jataúba, PE

A degradação das terras na região semi-árida resulta de processos naturais, que podem ser induzidos ou catalisados pelo homem por meio do uso inadequado dos recursos naturais, produzindo a deterioração da cobertura vegetal, do solo e dos recursos hídricos. Visando relacionar os processos de degradação da vegetação e dos solos na zona do agreste de Pernambuco, foram caracterizados os solos e o recobrimento vegetal em doze parcelas representativas de ambientes conservados, moderadamente degradados e degradados, no município de Jataúba. Para caracterizar a vegetação, os indivíduos foram classificados em três estratos verticais ou classes de altura: 3- indivíduos com altura superior a 3,0 m (lenhosas altas), amostrados em toda a área da parcela (200 m²); 2- indivíduos com altura variando de 0,51 a 3,0 m, amostrados em subárea de 100 m² (lenhosas baixas); 1- indivíduos com altura igual ou inferior a 0,5 m, amostrados em 18 miniparcelas de 25 x 50 cm (estrato da regeneração). Os solos de cada parcela foram caracterizados morfologicamente e as amostras coletadas por horizonte para realização das análises físicas, químicas e mineralógicas. A vegetação no segundo estrato vertical apresentou significativa diminuição da densidade absoluta de acordo com a intensidade de degradação dos solos. As espécies com maiores densidades relativas foram: Neoglaziovia variegata (caroá) e Cordia leucocephala (moleque duro), no ambiente conservado; Bromelia laciniosa (macambira), Aspidosperma pyryfolium (pereiro) e Caesalpinia pyramidalis (catingueira), no ambiente moderadamente degradado, e C. pyramidalis e Sida galheirensis (malva branca), no ambiente degradado. As características dos Planossolos mais bem relacionadas com a vegetação preservada foram: os maiores conteúdos de cascalho nos horizontes superficiais, a maior espessura dos horizontes A + E e os teores mais elevados de CO. A ocorrência de encrostamento superficial e erosão e os elevados teores de Na trocável foram observados mais intensamente nos ambientes degradados, sendo mais severos onde a vegetação se encontrava mais esparsa.