Controle biologico do percevejo-de-renda (Leptopharsa heveae Drake & Poor) em seringais de cultivo.

A mosca-de-renda ou percevejo-de-renda (Leptopharsa heveae - Hemiptera: Tingidae) e o mais importante inseto-praga da seringueira no Brasil. Essa praga de origem amazonica invadiu os seringais do Estado de Mato Grosso por volta de 1985 e, de 1992 a 1998, chegou aos seringais do Estado Sao Paulo e de Goias. Acredita-se que breve chegara aos Estados da Bahia, Espirito Santo e Minas Gerais. O principal agente disseminador desse inseto-praga entre estados e seringais tem sido os veiculos transportadores de coagulos e latex semiprocessado (GEB). O controle quimico dessa praga, alem de muito caro, coloca em risco os aplicadores e o meio ambiente. Em 1986, no Amazonas, o fungo Sporothrix insectorum foi constatado parasitando individuos do percevejo-de-renda. Com base nessa constatacao foram feitos alguns estudos em campo e laboratorio onde se determinaram a eficiencia biologica (capacidade do inimigo natural para infectar e destruir a praga) e a eficiencia tecnica (capacidade do inimigo natural para reduzir os danos causados na planta pela acao da praga). Os resultados desses testes evidenciaram o elevado potencial do S. insectorum para o controle do percevejode-renda. Imediatamente apos os testes, esse fungo foi enviado para os Estados de Mato Grosso, Acre, Rondonia, e mais recentemente para Sao Paulo e Goias onde vem sendo utilizado com o fungo Hirsutella verticillioides por diversos produtores e empresas. O fungo H. verticillioides, outro inimigo natural do percevejo-de-renda, isolado em 1990, na Guiana Francesa, vem sendo bem mais agressivo nos seringais da regiao Centro-Oeste e de Sao Paulo que o S. insectorum. Os resultados obtidos de avaliacoes efetuadas em alguns seringais de Goias, Mato Grosso e Sao Paulo indicam eficiencia biologica (porcentagem de insetos colonizados e fixados na folha por ambos os fungos em fevereiro), variando de 53% a 100%. Por outro lado, a eficiencia tecnica, medida pelo nivel de descoloracao da folha ou % de danos causados pela praga em fevereiro, tendo como referencia folhas nao atacadas, variou de 16% a 63%.

Evaluation of pathogenic fungi occurrence in traumatogenic structures of freshwater fish

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Adesão de Paracoccidioides brasiliensis e outros fungos anemófilos a teias de aranhas: implicações para a identificação de nichos microbianos no ambiente

The dimorphic pathogenic fungus, Paracoccidioides brasiliensis (Pb), is the etiological agent of paracoccidioidomycosis (PCM), the most important systemic mycosis in Latin America. While the yeast phase can be isolated from patients affected by paracoccidioidomycosis, dogs and naturally infected armadillos; several elements related to the ecology of the saprophytic phase of the pathogen, which is responsible for the production of infective propagules, are poorly understood, hampering the adoption of preventive measures. The demonstration of the high incidence of Pb infection in the 9- banded armadillo, Dasypus novemcinctus, has opened new perspectives for the identification of the pathogen’s habitat. At the opening of the armadillos’ burrows, spider webs are commonly found. The objective of this study was to evaluate the presence of Pb in spider webs samples related to the habitat of armadillos. Spider web samples were collected at Lageado Farm, Botucatu/SP and prepared for microscopic, molecular and mycological analyses. Microscopic analysis showed that different fungi were closely attached to spider web samples. Nested-PCR reaction showed positive amplification for Pb in 4 samples, with identity confirmed by amplicon sequencing. Fungal colonies also included members of Aspergillus, Blastobotrys, Penicillium, Candida, and Sporothrix genera, which are related to opportunistic disease and primary infections of great medical importance. In vitro adhesion tests of mycelia and yeast form of Pb to the spider webs were also performed, in order to analyze the possible physical attraction between fungal cells and the spider web protein network. The results showed a clear adherence of fungal particles to spider webs. In the current literature, there are no studies reporting adhesive properties of microorganisms to spider webs... (Complete abstract click electronic access below)

Diatom biostratigraphy and datum levels of sediments from ODP Leg 167 sites

Ocean Drilling Program Leg 167 represents the first time since 1978 that the North American Pacific margin was drilled to study ocean history. More than 7500 m of Quaternary to middle Miocene (14 Ma) sediments were recovered from 13 sites, representing the most complete stratigraphic sequence on the California margin. Diatoms are found in most samples in variable abundance and in a moderately well-preserved state throughout the sequence, and they are often dominated by robust, dissolution-resistant species. The Neogene North Pacific diatom zonation of Yanagisawa and Akiba (1998, doi:10.5575/geosoc.104.395) best divides the Miocene to Quaternary sequences, and updated ages of diatom biohorizons estimated based on the geomagnetic polarity time scale of Cande and Kent (1995, doi:10.1029/94JB03098) are slightly revised to adjust the differences between the other zonations. Most of the early middle Miocene through Pleistocene diatom datum levels that have been proven to be of stratigraphic utility in the North Pacific appear to be nearly isochronous within the level of resolution constrained by sample spacing. The assemblages are characterized by species typical of middle-to-high latitudes and regions of high surface-water productivity, predominantly by Coscinodiscus marginatus, Stephanopyxis species, Proboscia barboi, and Thalassiothrix longissima. Latest Miocene through Pliocene assemblages in the region of the California Current, however, are intermediate between those of subarctic and subtropical areas. As a result, neither the existing tropical nor the subarctic (high latitude) zonal schemes were applicable for this region. An interval of pronounced diatom dissolution detected throughout the Pliocene sequence apparently correspond to a relatively warmer paleoceanographic condition resulting in a slackening of the southward flow of the California Current.

Marine diatoms in deep sea sediments

Long-term evolution is thought to take opportunities that arise as a consequence of mass extinction (as argued, for example, by Gould, 2002) and the following biotic recovery, but there is absolutely no evidence for this being the case. However, our study shows that eutrophication by oceanic mixing also played a part in the enhancement of several evolutionary events amongst marine organisms, and these results could indicate that the rates of oceanic biodiversification may be slowed if upwelling becomes weakened by future global warming. This paper defines three distinct evolutionary events of resting spores of the marine diatom genus Chaetoceros, to reconstruct past upwelling through the analysis of several DSDP, ODP and land-based successions from the North, South and equatorial Pacific as well as the Atlantic Ocean during the past 40 million years. The Atlantic Chaetoceros Explosion (ACE) event occurred across the E/O boundary in the North Atlantic, and is characterized by resting spore diversification that occurred as a consequence of the onset of upwelling following changes in thermohaline circulation through global cooling in the early Oligocene. Pacific Chaetoceros Explosion events-1 and -2 (PACE-1 and PACE-2) are characterized by relatively higher occurrences of iron input following the Himalayan uplift and aridification at 8.5 Ma and ca. 2.5 Ma in the North Pacific region. These events not only enhanced the diversification and increased abundance of primary producers, including that of Chaetoceros, other diatoms and seaweeds, but also stimulated the evolution of zooplankton and larger predators, such as copepods and marine mammals, which ate these phytoplankton and plants. Current thinking suggests new evolutionary niches open up after a mass extinction, but our study finds that eutrophication can also stimulate evolutionary diversification. Moreover, in the opposite fashion, our results show that as thermohaline circulation abates, global warming progresses and the ocean surface becomes warmer, many marine organisms will be affected by the environmental degradation.