Características evolutivas do Cysticercus cellulosae no encéfalo e no coração humanos

O presente estudo teve como objetivos avaliar a prevalência de cisticercose, classificar as etapas evolutivas dos cisticercos encontrados nos encéfalos e corações humanos, diferenciá-las de acordo com os aspectos macro e microscópicos dos processos patológicos gerais e comparar os processos encontrados nos encéfalos e corações. Foram revisados protocolos de autópsias realizadas no Hospital Escola da Faculdade de Medicina do Triângulo Mineiro, Uberaba, MG, Brasil, no período de 1970 a 2000. Verificou-se a prevalência da cisticercose em 71 casos, sendo 18 (25,4%) de cisticercose cardíaca e 53 (74,6%) de encefálica. Foram analisados 19 cisticercos, sendo 9 de encéfalos e 10 de corações. Os cisticercos foram classificados, de acordo com sua fase evolutiva, em etapas: vesicular, vesicular coloidal, granular nodular e nodular calcificada, com similaridade entre os diagnósticos macro e microscópico. Entre os processos patológicos destacaram-se a beta-fibrilose e a fibroelastose endocárdica. Adicionalmente, demonstrou-se que a classificação pode ser aplicada tanto na cisticercose encefálica como na cardíaca.

Estudo pré-natal da hiper-refringência endocárdica fetal e sua relação com toxoplasmose materna

OBJETIVO: Estudar, comparativamente, um grupo de fetos de mães com toxoplasmose aguda ou recente e um grupo sem doença sistêmica, analisando-se a presença de alterações da refringência endocárdica. MÉTODOS: Avaliados 91 fetos cujas mães tinham diagnóstico de toxoplasmose aguda ou recente, detectados por soroconversão ou presença de títulos elevados de IgM e IgG, confirmados através do teste de captura e comparados com um grupo controle constituído de 182 fetos, selecionados a partir de uma população de baixo risco, participante de um programa de rastreamento de cardiopatias pré-natais. RESULTADOS: Não houve diferença significativa entre as idades médias gestacionais (29,2±4,6 semanas; 29,2±4,6 semanas) e maternas (25,7±6,7 anos; 26±5,4 anos) nos dois grupos. Áreas de hiperecogenicidade endocárdica observadas em 69 fetos com toxoplasmose materna (75,8%) e em apenas 6 fetos do grupo controle (3,3%) (p<0,001). Em 52 dos casos do grupo de estudo (75,4%) a hiper-refringência endocárdica era difusa e em 17 (24,3%), focal. No grupo controle, uma distribuição focal foi observada em 5 fetos (83,3%). CONCLUSÃO: A imagem ecocardiográfica pré-natal de hiper-refringência endocárdica focal ou difusa é mais prevalente em gestações com toxoplasmose materna do que naquelas normais, existindo associação entre a presença de hiperecogenicidade endocárdica fetal e doença materna.

Avaliação da expressão de metaloproteinases, TIMP-1 e da esclerose vascular nas endometrites crônicas das éguas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Abundance of plant macrofossils, mollusca and ostracoda in sediments obtained near Tessin, north Germany

A depression filled with Late Glacial and Holocene sediments was excavated during the geological exploration and recovery of a dump area near Tessin close to Rostock, and initiated the studies of the present paper. Pebble analysis of three exposed or respectively drilled till horizons as well as pollenanalytical, carpological and faunistical studies carried out allow the stratigraphical subdivision of the Quaternary sequence of the dump area. The basal till was probably the result of dead ice decay, and was lithostratigraphically assigned to the Pomerian Stage (qw2). The palynological results of boreholes RKS 19/93 and A/92 reveal pre-Allerod and other sediments instead of the expected interweichselian deposits. Based on the palynological and carpological findings, we correlated the beginning of the late glacial development in the locality with the end of the Meiendorf-lnterstadial sensu Menke in Bock et al. (1985, doi:10.3285/eg.35.1.18). The limnic-telmatic sedimentation could be observed pollen floristically probably starting with the Meiendorf-lnterstadial (Hippophae-Betula nana-phase) followed by the Bolling-(Betula nana-B. alba s.l.-Artemisia-Helianthemum-Poaceae-phase) and the Allerad-lnterstadial [Betula alba s.l.-(Pinus)-Cyperaceae-phase] lasting up to the Younger Dryas (Juniperus-Artemisia-Poaceae-phase). Sedimentation closed during the Younger Dryas with the accumulation of fine sands. It was reactivated later during the Holocene due to the anthropogene influence (Older and Younger Subatlantic, dampness of the depression by clearing).

Pedology, geochronology, palynology and macrofossils of soil profiles in the Altdarss area, german Baltic Sea coast

A new site with Lateglacial palaeosols covered by 0.8 - 2.4 m thick aeolian sands is presented. The buried soils were subjected to multidisciplinary analyses (pedology, micromorphology, geochronology, dendrology, palynology, macrofossils). The buried soil cover comprises a catena from relatively dry ('Nano'-Podzol, Arenosol) via moist (Histic Gleysol, Gleysol) to wet conditions (Histosol). Dry soils are similar to the so-called Usselo soil, as described from sites in NW Europe and central Poland. The buried soil surface covers ca. 3.4 km**2. Pollen analyses date this surface into the late Aller0d. Due to a possible contamination by younger carbon, radiocarbon dates are too young. OSL dates indicate that the covering by aeolian sands most probably occurred during the Younger Dryas. Botanical analyses enables the reconstruction of a vegetation pattern typical for the late Allerod. Large wooden remains of pine and birch were recorded.

Pollen profiles from three former lakes in the Lake Garda area

1. Late glacial and postglacial sediments from three former lakes in the Lake Garda area (Southern Alps) were investigated. 2. The pollen diagram from Bondone (1550 m) shows an older phase rich in NAP. A younger one corresponds with the Younger Dryas time according to two radiocarbon determinations. In the Preboreal no climatic deterioration could be found. 3. At first plants, which are nowadays typical for snow-ground, pioneer and dwarf shrub associations, immigrated into the surroundings of Bondone. In Alleröd times larch and pine appeared as the first trees. At the beginning of the Preboreal dense forest existed in that region. During the Alleröd timber line was at about 1500 m. 4. In the pollen diagrams from Saltarino (194 m) and Fiavè (654 m) an oldest period rich in NAP is followed by two stadial and two interstadial phases. Tree birches and larches immigrated during the oldest interstadial phase. 5. In the case of Saltarino and Fiavè only a preliminary dating could be made. A correlation seems to be possible with diagrams published by Zoller as well as with the diagram of Bondone. Discrepances in dating, which arise then, are discussed. According to the two possibilities of dating the youngest stadial is synchronous either with the so-called Piottino stadial or the Younger Dryas time. Consequently the oldest interstadial phase of Saltarino corresponds either with the Bölling or with a pre-Bölling interstadial. The last possibility seems to be more probable. 6. In the southern part of the Lake Garda area reforestation was preceded by a long shrub phase mainly with Juniperus. At about 650 m there was a period with Pinus mugo and only with a small amount of Juniperus before reforestation. A phase with Betula nana well known from areas north of the Alps could nowhere be found. 7. In the area under study larch appeared as the first tree. Lateron it has been the most important constituent of the forests near timber line. Birch, which plays an important role as a pioneer tree in Denmark - for instance at the transition of the pollen zones III/IV - as well as in Southern Germany during Bölling time, was of less importance at the southern border of the Alps. In that area the spreading of Pinus occurred very early causing dense forests. 8. During the last stadial phase (probably Younger Dryas time) dense forests with Pinus and Larix existed at 650 m. In the lower part of the Lake Garda area, however, both thermophilous trees as Quercus and herbs frequently occurred. This leads to the conclusion that during this time tree growth was limited by dryness in lower altitudes of the border of the Southern Alps. Pinus and Juniperus, however, do not show higher values in this period, a fact which cannot yet be explained. 9. A list of plants, which were found in the sediments, is compiled. Helodium lanatum, Dictamnus albus, Mercurialis cf. ovata, Buxus, Cerinthe cf. minor, Onosma, Anthericum and Asphodelus albus are findings, which are of special interest for the history of the flora of that region.