Larvas de simulídeos (Diptera, Simuliidae) do centro oeste, sudeste e sul do Brasil, parasitadas por microsporídeos (Protozoa) e mermitídeos (Nematoda)

A survey of simulid larval parasites was carried out in different localities of the states of Mato Grosso, Minas Gerais, São Paulo, Paraná, Santa Catarina and Rio Grande do Sul, Brazil, from February 1996 to May 1998. Prevalences for the microsporidian Polydispyrenia simulii Lutz & Splendore, 1908 were found in Morungaba and Leme, São Paulo, ranging from around 0.7 to 66.7%, depending mainly on the host simulid species. Microsporidiosis was registered in localities of São Paulo, Paraná, Santa Catarina and Rio Grande do Sul. Parasitism by Isomermis sp. (Nematoda, Mermithidae) was found in Simulium larvae from Serra do Japi, ranging from 0.8 to 45.8%, depending on the simulid species and the larval microhabitat in the stream, whether a cemented ramp in a lake outlet or the natural stream bed. Parasitism by mermithids was also found in ten localities. Mycoses caused by Coelomycidium sp. were for the first time recorded for larvae of Simulium (Chirostilbia) pertinax Kollar, 1832.

The antiquity of tuberculosis in Hungary: the skeletal evidence

The analysis of the skeletons of past human populations provides some of the best biological data regarding the history of significant diseases such as tuberculosis. The purpose of this study is to present the pathological alterations of the bones in this disease deriving from the ancient time of the territory of the Hungarian Great Plain on the basis of the earlier references and new cases. The bone changes in tuberculosis were mainly manifested in the vertebrae and less frequently in the hip, however, further alterations were observed on the surface of the endocranium and the ribs.

Spodosols pedogenesis under barreiras formation and sandbank environments in the south of Bahia

Morphologically differentiated Spodosols usually occur in the Coastal Plain of the South of Bahia and North of Espírito Santo. They are found in profiles known as "muçungas", i.e. sandy soils that accumulate water. In these areas, two kinds of Spodosols, different from those in the Restinga area, can be found: Spodosols with E albic horizon (white muçunungas) and without this horizon (black muçunungas). Eight soil profiles with spodic characteristics were collected and described in order to evaluate differences in the formation process of Barreiras and Restinga Spodosols in the South of Bahia. The soil profiles were also characterized chemically, physically and mineralogically. Additionally, texture and chemical analysis, Fe and Al extraction by sodium dithionite-citrate-bicarbonate (DBC), acid ammonium oxalate and sodium pyrophosphate, ammonium oxalate extract optic density (DOox), sulphuric acid attack, and X ray difractometry of the clay fraction were performed. In the Spodosols of the Barreiras area, fragipan was found the spodic layers. Cemented B spodic horizon were observed in the white muçunungas, and granular structure and dark color from the surface in the black muçunungas. There was no fragipan or hard spodic horizon in the Restinga Spodosol. This soil is acid, dystrophic and alic, with sandy texture and high clay percentages in the spodic horizons. The CEC, based on H + Al, is predominantly represented by the organic matter. The most representative components of the mineral phase of the clay fraction are kaolinite and possibly vermiculite traces with interlayered hydroxy. Chemical, physical, morphological and mineralogical differences were observed between the Barreiras and Restinga environments. The black and white muçunungas differ in morphologic and chemical properties only.

ALTERAÇÕES ELETROQUÍMICAS E DINÂMICA DE NUTRIENTES NA SOLUÇÃO DO SOLO EM ARROZ IRRIGADO COM LIXIVIADO INDUSTRIAL TRATADO

A utilização de efluentes industriais tratados na irrigação do arroz por alagamento pode provocar alterações eletroquímicas e aumentar o teor de nutrientes na solução do solo. Para testar essa hipótese, este trabalho teve por objetivo avaliar a dinâmica dos atributos químicos e eletroquímicos da solução do solo sob cultivo de arroz irrigado com lixiviado industrial tratado, contendo 820 mg L-1 de Na. O experimento foi conduzido em casa de vegetação, utilizando-se como unidades experimentais vasos preenchidos com 20 kg de solo, em delineamento experimental em blocos casualizados, com três repetições. Os tratamentos foram: controle (irrigação com água destilada) e quatro proporções do lixiviado (25, 50, 75 e 100 %). As coletas de solução do solo foram feitas semanalmente a partir do quarto dia após o início do alagamento (DAA) até 84 DAA. A solução do solo foi amostrada na profundidade de 10 cm e analisada para os principais nutrientes e o Na, bem como para a demanda bioquímica de oxigênio (DBO5), relação de adsorção de sódio (RAS), condutividade elétrica (CE) e potencial redox (EH). A irrigação com o lixiviado aumentou os teores de K, Ca, Mg, S, P, N-NH+4, N-NO−3 e Na, assim como os valores de RAS e CE, para valores considerados prejudiciais para as plantas. Foi observada diminuição do potencial redox na solução do solo pela irrigação com lixiviado industrial tratado. Os teores de DBO5 e o N-NH+4 diminuíram com o tempo de alagamento. Em proporções menores que 25 %, o lixiviado industrial tratado pode aumentar os teores de nutrientes em solução sem causar interferência do Na para as plantas.