Immunolocalization of matrix metalloproteinases-2 and-9 during apical periodontitis development

Objective: The objective of this study was to determine the expression of matrix metalloproteinase-2 (MMP-2) and -9 (MMP-9) during apical periodontitis development. Methods: Using an experimental design of induced periapical lesions in rats and immunohistochemistry assay as investigative tool, the MMP-2 and MMP-9 expression and distribution were evaluated at 3, 7,14, 21, 30,60 and 90 days after coronary access and pulp exposure of the first left mandibular molar to the oral environment. Two blind observers scored the immunoreactivity. A semi-quantitative analysis was performed. Results: Except at day 3, MMP-2 and MMP-9 immunostaining was observed in all experimental periods. The MMP-2 (p = 0.004) and MMP-9 (p = 0.005) immunostaining was higher in the period between 7 and 21 days. They were mainly observed in cells surrounding the apical foramen and adjacent periapical areas. Cells into the hypercementosis areas were strongly stained while both osteoblasts and osteoclasts; presented discrete staining along of this study. No staining was observed on epithelial walls. At 30, 60 and 90 days, the subjacent connective tissue presented intense MMP-2 and MMP-9 immunostaining in mononuclear cells (suggestive of fibroblasts, macrophages, infiltrating neutrophils and lymphocytes). Conclusion: The results observed in this study suggest that MMP-2 and MMP-9 play a critical role in the development of inflammatory periapical lesions, probably involved in the extracellular matrix (ECM) degradation during the initial phase of the lesion development. (C) 2009 Elsevier Ltd. All rights reserved.

Histological evaluation of the effectiveness of increased apical enlargement for cleaning the apical third of curved canals

P>Objective To evaluate the influence of apical size on cleaning of the apical third of curved canals prepared with rotary instruments. Methodology Forty-four mesiobuccal canals of maxillary molars teeth were instrumented to different apical sizes (30, 0.02; 35, 0.02; 40, 0.02; 45, 0.02) using a crown-down technique. After canal preparation, the apical thirds of the roots were submitted to histological processing and examination. The specimens were analysed at 40x magnification and the images were submitted to morphometric analysis with an integration grid to evaluate the percentage of debris and uninstrumented root canal walls. The action of the instruments on the root canal walls was assessed based on the surface regularity, abrupt change on the continuity of root canal walls, and partial or total pre-dentine removal. The results were statistically compared using one-way anova with post hoc Tukey test. Pearson`s correlation was performed to identify potential correlations between values. Results The percentage of uninstrumented root canal dentine was higher when apical enlargement was performed with instruments 30, 0.02 taper (55.64 +/- 4.62%) and 35, 0.02 taper (49.03 +/- 5.70%) than with instruments 40, 0.02 taper (38.08 +/- 10.44%) and 45, 0.02 taper (32.65 +/- 8.51%) (P < 0.05). More debris were observed when apical enlargement was performed with instruments 30, 0.02 taper (34.62 +/- 9.49%) and 35, 0.02 taper (25.33 +/- 7.37%) (P < 0.05). There was a significant correlation between the amount of remaining debris and the perimeter of uninstrumented root canal dentine (r = 0.9130, P < 0.001). Conclusion No apical enlargement size allowed the root canal walls to be prepared completely. Apical third cleanliness could be predicted by instrument diameter.

Apical limit of root canal filling and its relationship with success on endodontic treatment of a mandibular molar: 11-year follow-up

Objective. This article discusses the relationship between apical limit of root canal filling and success on endodontic treatment of a mandibular molar. Study design. A mandibular right first molar with vital pulp was endodontically treated, and 3 years later periapical lesions on mesial and distal roots were detected. The canals were retreated and obturated to the same levels as in the previous treatment. Results. An 8-year radiographic follow-up showed repair of the periapical lesions on both roots. Conclusions. Results suggest that the apical limit of obturation seems to have no influence in the repair of periapical tissues in mandibular molars. (Oral Surg Oral Med Oral Pathol Oral Radiol Endod 2011; 112: e48-e50)

Microtubule integrity is essential for apical polarization and epithelial morphogenesis in the thyroid

In this study, we examined the contribution of microtubules to epithelial morphogenesis in primary thyroid cell cultures. Thyroid follicles consist of a single layer of polarized epithelial cells surrounding a closed compartment, the follicular lumen. Freshly isolated porcine thyroid cells aggregate and reorganize to form follicles when grown in primary cultures. Follicular reorganization is principally a morphogenetic process that entails the assembly of biochemically distinct apical and basolateral membrane domains, delimited by tight junctions. The establishment of cell surface polarity during folliculogenesis coincided with the polarized redistribution of microtubules, predominantly in the developing apical poles of cells. Disruption of microtubule integrity using either colchicine or nocodazole caused loss of defined apical membrane domains, tight junctions and follicular lumina. Apical membrane and tight junction markers became randomly distributed at the outer surfaces of aggregates. In contrast, the basolateral surface markers, E-cadherin and Na+,K+-ATPase, remained correctly localized at sites of cell-cell contact and at the free surfaces of cell aggregates. These findings demonstrate that microtubules play a necessary role in thyroid epithelial morphogenesis. Specifically, microtubules are essential to preserve the correct localization of apical membrane components within enclosed cellular aggregates, a situation that is also likely to pertain where lumina must be formed from solid aggregates of epithelial precursors. (C) 2001 Wiley-Liss, Inc.

Uso de alguns estimadores ridge na análise estatística de experimentos em entomologia

Inúmeros experimentos em ciências agrárias apresentam variáveis que podem dar origem a problemas de multicolinearidade. Em se tratando da aplicabilidade de modelos de regressão, o problema da multicolinearidade tem como principal consequência o inflacionamento dos erros padrão e, com isso, o valor da estatística t-student é reduzido de tal forma que interfere nos resultados inferenciais. Várias medidas são propostas, na literatura, para resolver o problema de multicolinearidade. Entretanto, o desempenho dessas medidas está sujeito ao grau de multicolinearidade que as variáveis poderão apresentar, bem como ao tamanho amostral. Frente a este problema, este trabalho tem por objetivo avaliar alguns estimadores ridge, utilizando simulação Monte Carlo, bem como, apresentar a aplicação desses estimadores em um experimento, com dados reais, na área de entomologia. Mediante esta aplicação, os resultados expressivos alcançados foram obtidos em função da eficiência dos estimadores ridge avaliados, em relação ao estimador de mínimos quadrados. Em se tratando dos resultados computacionais, concluiu-se que estimadores ridge avaliados são recomendáveis, em experimentos que considerem as variáveis com diferentes graus de multicolinearidade, para amostras maiores do que n=50.

Multi-stage evolution of a sub-aerial volcanic ridge over the last 1.3 Myr: S. Jorge Island, Azores Triple Junction

New K/Ar dating and geochemical analyses have been carried out on the WNW-ESE elongated oceanic island of S. Jorge to reconstruct the volcanic evolution of a linear ridge developed close to the Azores triple junction. We show that S. Jorge sub-aerial construction encompasses the last 1.3 Myr, a time interval far much longer than previously reported. The early development of the ridge involved a sub-aerial building phase exposed in the southeast end of the island and now constrained between 1.32 +/- 0.02 and 1.21 +/- 0.02 Ma. Basic lavas from this older stage are alkaline and enriched in incompatible elements, reflecting partial melting of an enriched mantle source. At least three differentiation cycles from alkaline basalts to mugearites are documented within this stage. The successive episodes of magma rising, storage and evolution suggest an intermittent reopening of the magma feeding system, possibly due to recurrent tensional or trans-tensional tectonic events. Present data show a gap in sub-aerial volcanism before a second main ongoing building phase starting at about 750 ka. Sub-aerial construction of the S. Jorge ridge migrated progressively towards the west, but involved several overlapping volcanic episodes constrained along the main WNW-ESE structural axis of the island. Malic magmas erupted during the second phase have been also generated by partial melting of an enriched mantle source. Trace element data suggest, however, variable and lower degrees of partial melting of a shallower mantle domain, which is interpreted as an increasing control of lithospheric deformation on the genesis and extraction of primitive melts during the last 750 kyr. The multi-stage development of the S. Jorge volcanic ridge over the last 1.3 Myr has most likely been greatly influenced by regional tectonics, controlled by deformation along the diffuse boundary between the Nubian and the Eurasian plates, and the increasing effect of sea-floor spreading at the Mid-Atlantic Ridge.

Palaeomagnetic study of a subaerial volcanic ridge (Sao Jorge Island, Azores) for the past 1.3 Myr: evidence for the Cobb Mountain Subchron, volcano flank instability and tectonomagmatic implications

We present a palaeomagnetic study on 38 lava flows and 20 dykes encompassing the past 1.3 Myr on S. Jorge Island (Azores ArchipelagoNorth Atlantic Ocean). The sections sampled in the southeastern and central/western parts of the island record reversed and normal polarities, respectively. They indicate a mean palaeomagnetic pole (81.3 degrees N, 160.7 degrees E, K= 33 and A95= 3.4 degrees) with a latitude shallower than that expected from Geocentric Axial Dipole assumption, suggesting an effect of non-dipolar components of the Earth magnetic field. Virtual Geomagnetic Poles of eight flows and two dykes closely follow the contemporaneous records of the Cobb Mountain Subchron (ODP/DSDP programs) and constrain the age transition from reversed to normal polarity at ca. 1.207 +/- 0.017 Ma. Volcano flank instabilities, probably related to dyke emplacement along an NNWSSE direction, led to southwestward tilting of the lava pile towards the sea. Two spatially and temporally distinct dyke systems have been recognized on the island. The eastern is dominated by NNWSSE trending dykes emplaced before the end of the Matuyama Chron, whereas in the central/western parts the eruptive fissures oriented WNWESE controlled the westward growth of the S. Jorge Island during the Brunhes Chron. Both directions are consistent with the present-day regional stress conditions deduced from plate kinematics and tectonomorphology and suggest the emplacement of dykes along pre-existing fractures. The distinct timing and location of each dyke system likely results from a slight shift of the magmatic source.

Palaeomagnetic study of a subaerial volcanic ridge (São Jorge Island, Azores) for the cobb mountain subhron, volcano flank instability and tectonomagmatic implications

We present a palaeomagnetic study on 38 lava flows and 20 dykes encompassing the past 1.3 Myr on S. Jorge Island (Azores ArchipelagoNorth Atlantic Ocean). The sections sampled in the southeastern and central/western parts of the island record reversed and normal polarities, respectively. They indicate a mean palaeomagnetic pole (81.3 degrees N, 160.7 degrees E, K= 33 and A95= 3.4 degrees) with a latitude shallower than that expected from Geocentric Axial Dipole assumption, suggesting an effect of non-dipolar components of the Earth magnetic field. Virtual Geomagnetic Poles of eight flows and two dykes closely follow the contemporaneous records of the Cobb Mountain Subchron (ODP/DSDP programs) and constrain the age transition from reversed to normal polarity at ca. 1.207 +/- 0.017 Ma. Volcano flank instabilities, probably related to dyke emplacement along an NNWSSE direction, led to southwestward tilting of the lava pile towards the sea. Two spatially and temporally distinct dyke systems have been recognized on the island. The eastern is dominated by NNWSSE trending dykes emplaced before the end of the Matuyama Chron, whereas in the central/western parts the eruptive fissures oriented WNWESE controlled the westward growth of the S. Jorge Island during the Brunhes Chron. Both directions are consistent with the present-day regional stress conditions deduced from plate kinematics and tectonomorphology and suggest the emplacement of dykes along pre-existing fractures. The distinct timing and location of each dyke system likely results from a slight shift of the magmatic source.

The insular shelves of the Faial-Pico Ridge (Azores archipelago): a morphological record of its evolution

Shelves surrounding reefless volcanic ocean islands are formed by surf erosion of their slopes during changing sea levels. Posterosional lava flows, if abundant, can cross the coastal cliffs and fill partially or completely the accommodation space left by erosion. In this study, multibeam bathymetry, high-resolution seismic reflection profiles, and sediment samples are used to characterize the morphology of the insular shelves adjacent to Pico Island. The data show offshore fresh lava flow morphologies, as well as an irregular basement beneath shelf sedimentary bodies and reduced shelf width adjacent to older volcanic edifices in Pico. These observations suggest that these shelves have been significantly filled by volcanic progradation and can thus be classified as rejuvenated. Despite the general volcanic infilling of the shelves around Pico, most of their edges are below the depth of the Last Glacial Maximum, revealing that at least parts of the island have subsided after the shelves formed by surf erosion. Prograding lava deltas reached the shelf edge in some areas triggering small slope failures, locally decreasing the shelf width and depth of their edges. These areas can represent a significant risk for the local population; hence, their identification can be useful for hazard assessment and contribute to wiser land use planning. Shelf and subaerial geomorphology, magnetic anomalies and crustal structure data of the two islands were also interpreted to reconstruct the long-term combined onshore and offshore evolution of the Faial-Pico ridge. The subaerial emergence of this ridge is apparently older than previously thought, i.e., before approximate to 850 ka.

Uma abordagem a sistemas de crescimento celular apical: síntese de um sensor para iões citosólicos de potássio

Dissertação para obtenção do Grau de Mestre em Bioorgânica

A lesão apical em cardiopatas chagásicos crônicos: estudo necroscópico

INTRODUÇÃO: A lesão apical ventricular é típica da cardiopatia chagásica e sua presença representa risco de fenômenos tromboembólicos. O objetivo deste trabalho é avaliar a frequência de LA à necropsia de portadores de cardiopatia chagásica crônica. MÉTODOS: Análise retrospectiva de necropsias de chagásicos maiores que 17 anos. Efetuada análise estatística comparativa das variáveis clínicas e dos achados necroscópicos entre o grupo A (com lesão apical) e o grupo B (ausência de lesão apical). RESULTADOS: Estudados 51 casos: 25 no grupo A (idade média de 53 anos, 64% do sexo masculino)e 26 no B.. A LA localizava-se no ventrículo esquerdo em 80% casos. No grupo B, a média de idade foi de 56 anos e 46,1% eram do sexo masculino. A forma clínica prevalente nos dois grupos foi a miopática, mas arritmia cardíaca também esteve presente em ambos (57,9% no grupo A e 32,1% no B). Foi constatada a presença de trombos em 60% dos casos do grupo A (53,3% localizados na LA ) e 30,7% no B; CONCLUSÕES: Houve predomínio da forma miopática nos casos com LA, com média de peso cardíaco maior em relação ao B. Em ambos os grupos observamos relação diretamente proporcional entre maior peso cardíaco e presença de tromboses. Houve predomínio do número de tromboses no grupo A, mais de 50% eram localizadas na lesão, cujo diferencial clínico principal consistiu na presença maior de arritmias. A miopatia (com aumento de peso acima de 500g) foi primordial para aparecimento de tromboses.

É a cardiomiopatia hipertrófica apical vista em uma amostra na cidade do Rio de Janeiro similar à encontrada no oriente?

OBJETIVO: Investigar a existência de diferença na forma de apresentação clínica e evolutiva da cardiomiopatia hipertrófica apical (CMHA), vista em uma amostra na cidade do Rio de Janeiro e a observada no oriente, onde foi descrita. MÉTODOS: Entre 156 pacientes com cardiomiopatia hipertrófica diagnosticados em nossa instituição, foram identificados 13 (8,34%) com a forma apical, sendo estudadas as suas manifestações clínicas, os meios de diagnóstico e a sua evolução. RESULTADOS: Eram 8 homens e 5 mulheres, com idades entre 19 a 75 anos, todos da raça branca, a maioria sintomática. O eletrocardiograma revelou ondas T gigantes em precordiais em 10 pacientes (76,92%), o ecocardiograma (ECO), a presença de hipertrofia apical em todos os casos, sendo em 10 (76,92%) restrita a ponta do ventrículo esquerdo (VE), em dois (15,4%) a ponta do ventrículo direito (VD) e, em 1 (7,68%), acometendo ambos os ventrículos. A cineventriculografia confirmou os achados do ECO. A evolução variou de 6 a 264 meses (x=95,4). Ocorreram dois óbitos (15,4%) em pacientes com o comprometimento associado ao VD, devido ao aumento significativo da dimensão dos átrios, ocorrência de fibrilação atrial, insuficiência valvar mitral e/ou tricúspide e tromboembolismo. Entre os vivos, a paciente com acometimento do VD evolui com restrição diastólica, e os restantes com lesão localizada do VE , 9 estão assintomáticos em uso de propranolol (8) ou amiodarona (1) e um permanece assintomático sem medicação. CONCLUSÃO: presentação, diagnóstico e evolução, porém notamos em 3 pacientes ( 23,08%) o acometimento da ponta do VD, não descrito no oriente, mas com péssimo prognóstico evolutivo.

Cardiomiopatia hipertrófica apical associada a doença arterial coronária

Homem de 59 anos, portador de cardiomiopatia hipertrófica apical há 12 anos, apresentou agudização de quadro anginoso. Foi detectada doença arterial coronária com lesão trivascular, e indicada cirurgia de revascularização, com anastomose de artéria mamária e a colocação de duas pontes de veia safena, tendo evoluído com melhora do quadro anginoso e redução da dimensão do átrio esquerdo.

Apical aneurysm and left ventricular hypertrophy

A 59-year-old woman presented with an embolic transient ischemic attack and a history of controlled hypertension for 16 years. Both echocardiogram and MRI showed severe biventricular hypertrophy and an apical aneurysm with a thrombus. The occurrence of an apical aneurysm in the presence of cardiac hypertrophy is a rare finding and has been described in patients with hypertrophic cardiomyopathy. However, it has not been reported in patients with systemic arterial hypertension. In this patient the lack of a relationship between the severity of the hypertrophy and the levels of blood pressure, together with the presence of histologic disorganization of myocardial cardiac muscle cells by endomyocardial biopsy suggested the diagnosis of hypertrophic cardiomyopathy.