Diagnóstico de hemoparasitas em felídeos neotropicais provenientes de vida livre no Brasil

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

Atividade endectocida de uma nova alternativa terapêutica (S-cifenotrina, Butóxido de piperonila, D-tetrametrina e Ivermectina) em cães

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Hepatozoon spp. em carnívoros neotropicais presentes em vida livre no Parque Nacional das Emas, em Goiás, Brasil

Pós-graduação em Medicina Veterinária - FMVZ

Molecular detection of feline arthropod-borne pathogens in cats in Cuiaba, state of Mato Grosso, central-western region of Brazil

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

Tick-borne agents in domesticated and stray cats from the city of Campo Grande, state of Mato Grosso do Sul, midwestern Brazil

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

SCWDS Briefs: Volume 25, Number 2 (July 2009)

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

DNA-Analyse an tierischem Spurenmaterial - Etablierung einer Methode zur molekulargenetischen Untersuchung von Tierhaarspuren in der Fallarbeit, insbesondere der Katzen

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.

Great Barrier Reef coral element/Ca and stable isotope data and U-Th ages from IODP Expedition 325

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.

Stable oxygen isotope record and Sr/Ca ratios of corals from IODP Holes M0009D and M0023A

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.

Monthly Tahiti coral Sr/Ca and oxygen isotope data from IODP Hole 310-M0024A

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.

(Supplement Table S2) Results of 230Th/U-dating

We compared the suitability of two skeletal materials of the Atlantic brain coral Diploria strigosa for 230Th/U-dating: the commonly used bulk material comprising all skeletal elements and the denser theca wall material. Eight fossil corals of presumably Last Interglacial age from Bonaire, southern Caribbean Sea, were investigated, and several sub-samples were dated from each coral. For four corals, both the ages and the activity ratios of the bulk material and theca wall agree within uncertainty. Three corals show significantly older ages for their bulk material than for their theca wall material as well as substantially elevated 232Th content and (230Th/238U) ratios. The bulk material samples of another coral show younger ages and lower (230Th/238U) ratios than the corresponding theca wall samples. This coral also contains a considerable amount of 232Th. The application of the available open-system models developed to account for post-depositional diagenetic effects in corals shows that none of the models can successfully be applied to the Bonaire corals. The most likely explanation for this observation is that the assumptions of the models are not fulfilled by our data set. Comparison of the theca wall and bulk material data enables us to obtain information about the open-system processes that affected the corals. The corals showing apparently older ages for their bulk material were probably affected by contamination with a secondary (detrital) phase. The most likely source of the detrital material is carbonate sand. The higher (230Th/232Th) ratio of this material implies that detrital contamination would have a much stronger impact on the ages than a contaminant with a bulk Earth (230Th/232Th) ratio and that the threshold for the commonly applied 232Th reliability criterion would be much lower than the generally used value of 1 ng g^-1. The coral showing apparently younger ages for its bulk material was probably influenced by more than one diagenetic process. A potential scenario is a combination of detrital contamination and U addition by secondary pore infillings. Our results show that the dense theca wall material of D. strigosa is generally less affected by post-depositional open-system behaviour and better suited for 230Th/U-dating than the bulk material. This is also obvious from the fact that all ages of theca wall material reflect a Last Interglacial origin (~125 ka), whereas the bulk material samples are either substantially older or younger. However, for some corals, the 230Th/U-ages and activity ratios of the bulk material and the theca wall samples are similar. This shows that strictly reliable 230Th/U-ages can also be obtained from bulk material samples of exceptionally well-preserved corals. However, the bulk material samples more frequently show elevated activity ratios and ages than the corresponding theca wall samples. Our findings should be generally applicable to brain corals (Mussidae) that are found in tropical oceans worldwide and may enable reliable 230Th/U-dating of fossil corals with similar skeletal architecture, even if their bulk skeleton is altered by diagenesis. The 230Th/U-ages we consider reliable (120-130 ka), along with a recently published age of 118 ka, provide the first comprehensive dating of the elevated lower reef terrace at Bonaire (118-130 ka), which is in agreement in timing and duration with other Last Interglacial records.