494 resultados para Felis-catus


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Os Autores analisaram soros de 47 Cannis familiaris, de 9 Felis cattus, de 64 Didelphis marsupialis aurita, de 9 Dasypus novemcinctus, de 4 Cabassous tatouay e de 29 Rattus rattus, através da reação de imunofluorescência indireta, para pesquisar a presença de anticorpos anti Toxoplasma gondii. Estes foram encontrados apenas em C. familiaris (63,8%) e em D. m. aurita (4,7%). Frente aos resultados obtidos, os Autores sugerem que novas pesquisas nesta área sejam realizadas, para que se conheça melhor a importância epidemiológica de várias espécies animais na disseminação da toxoplasmose.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Coccidiosis is one of the most common parasitic diseases in dogs and cats in all the world. The aim of this study was to determine the occurrence of this parasitosis in dog and cat population at the Municipality of Andradina in the State of São Paulo, from 2007 to 2009. Fecal samples from 97 cats and 93 dogs were analyzed by using the techniques of flotation in saturated sodium chloride and spontaneous sedimentation. The species were classified according to morphology of the oocysts. Cystoisospora fecal oocyst found in 71.1% (69/97) of the cats, and simple infection by C. rivolta and C. felis occurred respectively in 41.0% (16/39) and 20.5% (8/39) animals, with P ≥ 0.2319. In 39.7%(37/93) of the dogs was found positive for Cystoisospora spp. And the species C. canis identified in the largest proportion (63.9%) with P = 0.0005. From the results, we conclude that dogs and cats had high incidence of infection Cystoisospora, being C. canis and C. rivolta most observed species, respectively.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Pós-graduação em Medicina Veterinária - FMVZ

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Table of Contents: Piroplasmosis Hits Missouri Horses Cytauxzoon felis in Wild Felids SCIF & Mossy Oak Fund HD Research Hardware Disease in a Key Deer Wildlife Poisoning in Kansas Swine Brucellosis Infects Hog Hunters SCWDS Personnel Changes NWHC Has New Director New USDI Publication on Bats Recent SCWDS Publications Available

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Die Hauskatze (F. s. catus) ist eines der beliebtesten Haustiere in Deutschland. Das enge Zusammenleben mit dem Menschen bedingt die Übertragung von Haaren auf Gegenstände oder andere Personen, sodass diese Spuren für eine forensische Untersuchung von größter Bedeutung sind. Da in Haaren mit einer sehr geringen Menge an Kern-DNA gerechnet werden muss und diese sich zudem in einem degradierten Zustand befindet, wurden die zur Individualisierung ausgewählten Tetranukleotid-STR-Markersysteme dahingehend optimiert. Die Optimierung umfasste neben der Reduktion der Produktgrößenbereiche auch die Anpassung der PCR-Profile. Die Sequenzierung und Beschreibung der Repeatmotive aller Marker führte überwiegend zu einer von der Literatur abweichenden Darstellung. Anhand der Sequenzanalyse erfolgte die Einteilung der Marker in STR-Klassen sowie die Einführung einer markerspezifischen Nomenklatur. Diese spiegelt sich vor allem in den erstellten Allelleitern wider, die zum Abgleich der amplifizierten Produkte eines jeden Markersystems eingesetzt werden. Die Allelleitern dienen als interne Laborreferenz und können als Standard für den Datenaustausch zwischen unterschiedlichen Laboren genutzt werden. Mittels 14 speziell angepassten Markersystemen und dem geschlechtsspezifischen Marker Amelogenin kann praktisch eine Individualisierung für F. s. catus durchgeführt werden. rnSind über die Kern-DNA keine oder nur unzureichende Ergebnisse zu erhalten, kann alternativ auf die Untersuchung der mitochondrialen DNA zurückgegriffen werden. Neben Systemen, die einen Aufschluss zum Artnachweis erbringen, stehen in der Kontrollregion von F. s. catus weitere Systeme für eine Differenzierung in Haplotypen zur Verfügung. Trotz der maternalen Vererbung der mtDNA und der dadurch nicht zu realisierenden Individualisierung liefert diese Einteilung einen hohen Anteil an einzigartigen Haplotypen, die in der untersuchten Stichprobe nur durch je ein Individuum repräsentiert wurden. Die Aufspaltung in Haplotypen liefert einen Aussagewert, mit dem gegebenenfalls ein Ausschluss zwischen Spur und Vergleich getroffen werden kann.rnBeide Analyseverfahren, sei es auf Ebene der Kern- oder mitochondrialen DNA, bieten eine Möglichkeit den größtmöglichsten Informationsgehalt aus einer Spur zu erhalten. Im forensischen Bereich steht somit erstmals ein komplett standardisiertes Verfahren zur Untersuchung von Spuren der Hauskatze zur Verfügung. Dieses reicht von der Artbestimmung einer Spur bis zur praktisch individuellen Zuordnung.

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Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.

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We present monthly resolved records of strontium/calcium (Sr/Ca) and oxygen isotope (d18O) ratios from well-preserved fossil corals drilled during the Integrated Ocean Drilling Program (IODP) Expedition 310 'Tahiti Sea Level' and reconstruct sea surface conditions in the central tropical South Pacific Ocean during two time windows of the last deglaciation. The two Tahiti corals examined here are uranium/thorium (U/Th)-dated at 12.4 and 14.2 ka, which correspond to the Younger Dryas (YD) cold reversal and the Bølling-Allerød (B-A) warming of the Northern Hemisphere, respectively. The coral Sr/Ca records indicate that annual average sea surface temperature (SST) was 2.6-3.1 °C lower at 12.4 ka and 1.0-1.6 °C lower at 14.2 ka relative to the present, with no significant changes in the amplitude of the seasonal SST cycle. These cooler conditions were accompanied by seawater d18O (d18Osw) values higher by ~0.8 per mill and ~0.6 per mill relative to the present at 12.4 and 14.2 ka, respectively, implying more saline conditions in the surface waters. Along with previously published coral Sr/Ca records from the island [Cohen and Hart (2004), Deglacial sea surface temperatures of the western tropical Pacific: A new look at old coral. Paleoceanography 19, PA4031, doi:10.1029/2004PA001084], our new Tahiti coral records suggest that a shift toward lower SST by ~1.5 °C occurred from 13.1 to 12.4 ka, which was probably associated with a shift toward higher d18Osw by ~0.2 per mill. Along with a previously published coral Sr/Ca record from Vanuatu [Corrège et al. (2004), Interdecadal variation in the extent of South Pacific tropical waters during the Younger Dyras event. Nature 428, 927-929], the Tahiti coral records provide new evidence for a pronounced cooling of the western to central tropical South Pacific during the Northern Hemisphere YD event.

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The early last glacial termination was characterized by intense North Atlantic cooling and weak overturning circulation. This interval between ~18,000 and 14,600 years ago, known as Heinrich Stadial 1, was accompanied by a disruption of global climate and has been suggested as a key factor for the termination. However, the response of interannual climate variability in the tropical Pacific (El Niño-Southern Oscillation) to Heinrich Stadial 1 is poorly understood. Here we use Sr/Ca in a fossil Tahiti coral to reconstruct tropical South Pacific sea surface temperature around 15,000 years ago at monthly resolution. Unlike today, interannual South Pacific sea surface temperature variability at typical El Niño-Southern Oscillation periods was pronounced at Tahiti. Our results indicate that the El Niño-Southern Oscillation was active during Heinrich Stadial 1, consistent with climate model simulations of enhanced El Niño-Southern Oscillation variability at that time. Furthermore, a greater El Niño-Southern Oscillation influence in the South Pacific during Heinrich Stadial 1 is suggested, resulting from a southward expansion or shift of El Niño-Southern Oscillation sea surface temperature anomalies.