Participação do receptor toll-like4 na resposta imune durante a esporotricose ecperimental

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Dicotomia Th1/Th2: papel do óxido nítrico e citocinas na esporotricose

Pós-graduação em Biociências e Biotecnologia Aplicadas à Farmácia - FCFAR

Avaliação de leveduras isoladas de áreas agrícolas como agentes no controle biológico de fitopatógenos

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Caracterização e ocorrência de bidens mosaic virus (bimv) em regiões produtoras de alface no Estado de São Paulo

Pós-graduação em Agronomia (Proteção de Plantas) - FCA

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)

Avaliação da apoptose e resposta Th17 em modelo murino de esporotricose

Pós-graduação em Biociências e Biotecnologia Aplicadas à Farmácia - FCFAR

Efeito imunomodulatório e controle da infecção fúngica do extrato de alho (Allium sativum L.) em modelo murino de esporotricose

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Analisi chimica e mineralogica di sedimenti di fondo marino del Mar Tirreno sud-orientale

A partire dal 2010 la Commissione Europea ha compilato una lista di 20 materie prime ritenute “critiche” per importanza economica e rischio di approvvigionamento, per le quali è fondamentale la ricerca di possibili fonti alternative nel territorio europeo, poiché i maggiori produttori sono tutti paesi extra-europei. Dati questi presupposti, 20 campioni di fango marino, dragati nelle adiacenze di seamounts del Tirreno sud-orientale, sono stati analizzati per mezzo di XRF, al fine di trovare arricchimenti in elementi critici quali cromo, cobalto, gallio, niobio e alcuni elementi delle Terre Rare (lantanio, cerio, neodimio, samario, ittrio). I fanghi, talvolta con frazione sabbiosa più abbondante, sono stati dapprima divisi in base al colore in fanghi marroni e grigi e fanghi di colore bianco, rosso o arancio; presentano anche inclusi di diverso tipo, quali frammenti di conchiglie, noduli neri o bruno-arancio, croste bruno-nere o bruno-arancio. Dalle analisi chimiche è risultato che campioni più ricchi in CaO hanno un contenuto minore negli elementi ricercati, al contrario dei campioni ricchi in ossidi di Si, Ti, Al, Fe. Confrontando inoltre i campioni con i valori medi di composizione della crosta terrestre superiore, essi risultano più ricchi in REY e meno in Co, Cr, Ga, Nb, mentre sono sempre più arricchiti della composizione media dei sedimenti marini. Dalle analisi mineralogiche risulta che i fanghi contengono generalmente quarzo, calcite, feldspati in piccole quantità e fillosilicati. Infine, analisi XRD e SEM-EDS sui noduli neri hanno dimostrato che si tratta di todorokite, un ossido idrato di Mn, con tenori variabili di Na, K, Ca, Mg, dalla forma globosa con microstruttura interna fibroso-raggiata. Si ritiene quindi che fanghi ricchi in CaCO3, probabilmente bioderivato, non siano l’obiettivo più adatto per la ricerca di elementi critici, mentre potrebbero esserlo fanghi più ricchi in Si, Al, Fe, K, che hanno maggiori concentrazioni di tali elementi.

Ultrasonographic features of PMEL17 ( Silver ) mutant gene-associated multiple congenital ocular anomalies (MCOA) in Comtois and Rocky Mountain horses

OBJECTIVE: (1) To describe the ultrasonographic appearance of multiple congenital ocular anomalies (MCOA) in the eyes of horses with the PMEL17 (Silver) mutant gene. (2) To compare the accuracy of B-mode ocular ultrasound to conventional direct ophthalmoscopy. ANIMALS STUDIED: Sixty-seven Comtois and 18 Rocky Mountain horses were included in the study. PROCEDURES: Horses were classified as being carriers or noncarriers of the PMEL17 mutant allele based on coat color or genetic testing. Direct ophthalmoscopy followed by standardized ultrasonographic examination was performed in all horses. RESULTS: Seventy-five of 85 horses (88.24%) carried at least one copy of the Silver mutant allele. Cornea globosa, severe iridal hypoplasia, uveal cysts, cataracts, and retinal detachment could be appreciated with ultrasound. Carrier horses had statistically significantly increased anterior chamber depth and decreased thickness of anterior uvea compared with noncarriers (P < 0.05). Uveal cysts had a wide range of location and ultrasonographic appearances. In 51/73 (69.86%) carrier horses, ultrasound detected ciliary cysts that were missed with direct ophthalmoscopy. CONCLUSIONS: In this study, ultrasonography was useful to identify uveal cysts in PMEL17 mutant carriers and to assess anterior chamber depth.

Diversity and faunal composition of benthic foraminifera in Hole 44-390A on the Blake Nose Plateau

Benthic foraminiferal assemblages are a widespread tool to understand changes in organic matter flux and bottom-water oxygenation and their relation to paleoceanographic changes in the Upper Cretaceous oceans. In this study, assemblage data (diversity, total number, and number per species and gram) from Deep Sea Drilling Project (DSDP) Site 390 (Blake Nose, western North Atlantic) were processed for the lower Maastrichtian (Globotruncana falsostuarti - Gansserina gansseri Planktic Foraminiferal Zone). These data document significant changes in nutrient flux to the sea floor as well as bottom-water oxygenation during this time interval. Parallel to the observed changes in the benthic foraminiferal assemblages the number of inoceramid shells decreases, reflecting also a significant increase in bottom-water oxygenation. We speculate, that these data could reflect the onset of a shift from warmer low-latitude to cooler high-latitude deep-water sources. This speculation will predate the major reorganization of the oceanic circulation resulting in a circulation mode similar to today at the Early/Late Maastrichtian boundary by ~1 Ma and therefore improves our understanding of Late Cretaceous paleoceanography.

Cenozoic planktonic foraminifera in the Goban Spur Region

Cenozoic planktonic foraminiferal biostratigraphy at DSDP-IPOD Leg 80 sites documents the existence of regionwide stratigraphic gaps in the Paleocene and middle Miocene. Episodes of carbonate dissolution also occurred during the Paleocene at several sites, particularly at Site 549, where destruction of foraminiferal tests may obscure evidence of an unconformity. The middle Miocene hiatus is apparent at each site where Neogene sediments were continuously cored. Upper Miocene sediments at Site 550 (the only abyssal site) are characterized by moderate to extensive dissolution of planktonic foraminifers, but they contain abundant specimens of Bolboforma that mark this stratigraphic interval (von Daniels and Spiegler, 1974, doi:10.1007/BF02986990; Roegl, 1976, doi:10.2973/dsdp.proc.35.133.1976; Murray, 1979, doi:10.2973/dsdp.proc.48.116.1979; Müller et al., 1985, doi:10.2973/dsdp.proc.80.117.1985). Although foraminiferal evidence is not conclusive, nannofossils indicate a widespread Oligocene unconformity (Müller, 1985). Several oceanographic factors, not just simple sea-level change, probably interacted to produce these regional unconformities. There are also dramatic differences in the Cenozoic sedimentary record among Leg 80 sites, indicating that each has had a distinct geologic history. The thickness of the Cenozoic section varies from 100 m at Site 551 to 471 m at Site 548. The thickness of individual chronostratigraphic units also varies, as do the number and stratigraphic position of unconformities other than those mentioned. Differences in the stratigraphic record from site to site across the continental slope result from (1) location in separate half-graben structures, (2) varying location across the developing margin, and (3) difference in position relative to the seaward edge of the enclosing half-graben. Except for turbidites, deposition at Site 550 (abyssal) was largely independent of developments on the continental slope; but it was affected by oceanographic events widespread in the North Atlantic.