Avaliação das características do líquido ruminal associada à termografia digital e atividade pedométria em vacas holandesas

Pós-graduação em Medicina Veterinária - FMVZ

Preventive diagnosis of dairy cow lameness

This research aimed to develop a Fuzzy inference based on expert system to help preventing lameness in dairy cattle. Hoof length, nutritional parameters and floor material properties (roughness) were used to build the Fuzzy inference system. The expert system architecture was defined using Unified Modelling Language (UML). Data were collected in a commercial dairy herd using two different subgroups (H-1 and H-2), in order to validate the Fuzzy inference functions. The numbers of True Positive (TP), False Positive (FP), True Negative (TN), and False Negative (FN) responses were used to build the classifier system up, after an established gold standard comparison. A Lesion Incidence Possibility (LIP) developed function indicates the chances of a cow becoming lame. The obtained lameness percentage in H-1 and H-2 was 8.40% and 1.77%, respectively. The system estimated a Lesion Incidence Possibility (LIP) of 5.00% and 2.00% in H-1 and H-2, respectively. The system simulation presented 3.40% difference from real cattle lameness data for H-1, while for H-2, it was 0.23%; indicating the system efficiency in decision-making.

Aspectos morfológicos da veia efálica na trombose aguda experimental e na aplicação de cateter de Fogarty em equinos

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Borreliosis in horses: epidemiology, experimental infection and therapeutic

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

Acidose láctica ruminal aguda induzida experimentalmente em ovinos: estudo clínico e laboratorial

Pós-graduação em Medicina Veterinária - FCAV

Element contents, sulfur and oxygen isotopes, and molecular biomarkers of phosphatic crust samples from the Chimbote Platform of the shelf off Peru

Authigenic phosphatic laminites enclosed in phosphorite crusts from the shelf off Peru (10°01' S and 10°24' S) consist of carbonate fluorapatite layers, which contain abundant sulfide minerals including pyrite (FeS2) and sphalerite (ZnS). Low d34Spyrite values (average -28.8 per mill) agree with bacterial sulfate reduction and subsequent pyrite formation. Stable sulfur isotopic compositions of sulfate bound in carbonate fluorapatite are lower than that of sulfate from ambient sea water, suggesting bacterial reoxidation of sulfide by sulfide-oxidizing bacteria. The release of phosphorus and subsequent formation of the autochthonous phosphatic laminites are apparently caused by the activity of sulfate-reducing bacteria and associated sulfide-oxidizing bacteria. Following an extraction-phosphorite dissolution-extraction procedure, molecular fossils of sulfate-reducing bacteria (mono-O-alkyl glycerol ethers, di-O-alkyl glycerol ethers, as well as the short-chain branched fatty acids i/ai-C15:0, i/ai-C17:0 and 10MeC16:0) are found to be among the most abundant compounds. The fact that these molecular fossils of sulfate-reducing bacteria are distinctly more abundant after dissolution of the phosphatic laminite reveals that the lipids are tightly bound to the mineral lattice of carbonate fluorapatite. Moreover, compared with the autochthonous laminite, molecular fossils of sulfate-reducing bacteria are: (1) significantly less abundant and (2) not as tightly bound to the mineral lattice in the other, allochthonous facies of the Peruvian crusts consisting of phosphatic coated grains. These observations confirm the importance of sulfate-reducing bacteria in the formation of the phosphatic laminite. Model calculations highlight that organic matter degradation by sulfate-reducing bacteria has the potential to liberate sufficient phosphorus for phosphogenesis.

Geochemistry of phosphatic crusts from the shelf off Peru

Authigenic phosphorite crusts from the shelf off Peru (9°40°S to 13°30°S) consist of a facies with phosphatic coated grains covered by younger phosphatic laminite. The crusts are composed of carbonate fluorapatite, which probably formed via an amorphous precursor close to the sediment water interface as indicated by low F/P2O5 ratios, Sr and Ca isotopes, as well as rare earth element patterns agreeing with seawater-dominated fluids. Small negative Ce anomalies and U enrichment in the laminite suggest suboxic conditions close to the sediment-water interface during its formation. Increased contents of chalcophilic elements and abundant sulfide minerals in the facies with phosphatic coated grains as well as in the laminite denote sulfate reduction and, consequently, point to episodical development of anoxic conditions during phosphogenesis. The Peruvian phosphorites formed episodically over an extended period of time lasting from Middle Miocene to Pleistocene. Individual phosphatic coated grains show a succession of phosphatic layers with varying contents of organic matter and sulfide-rich phosphatic layers. Coated grains supposedly formed as a result of episodic suspension caused by high turbulence and shifting redox conditions. Episodic anoxia in the pore water induced pyritization in the outermost carbonate fluorapatite layer. Phosphatic coated grains were later transported to the place of crust formation, where subsequent laminite formation was favored under lower energy conditions. A similar succession of phosphatic layers with varying contents of organic matter and sulfide-rich layers in the laminite suggests a formation mechanism analogous to that of individual coated grains.

Aspectos do desenvolvimento morfológico, morfométrico e ultraestrutural do aparelho ungueal do cavalo Baixadeiro

O cavalo Baixadeiro é encontrado na Baixada Maranhense, região caracterizada por planície, podendo permanecer alagada por até seis meses. Ainda que diante destas condições, o cavalo Baixadeiro pode viver sem apresentar doenças da úngula, tais como, a laminite. Assim, propôs-se identificar elementos morfológicos da úngula desta raça específica de cavalo com o intuito de explicar tal resistência à umidade. Foram utilizadas amostras de úngula provenientes de 4 cavalos Baixadeiros (N=16) e de 4 cavalos Puro Sangue Inglês (N=16). Todas as úngulas foram analisadas por macroscopia, morfometria e por microscopia eletrônica de varredura e de luz. Macroscopicamente, a úngula do cavalo Baixadeiro era cuneiforme, com comprimento médio de 10.22 ± 1.3 cm, largura de 9.83 ± 1.01 cm e comprimento da parede medial de 5.67 ± 0.76 cm. A úngula do cavalo Puro Sangue Inglês teve um comprimento médio de 13.47 ± 0.8 cm, largura de 12.54 ± 0.49 cm e comprimento da parede medial de 7.77 ± 0.54 cm. Na microscopia de luz da camada interna, o tecido que conecta as lamelas epidérmicas primárias às secundárias e ao estrato médio foi visualmente mais espesso no Baixadeiro. Além disso, a região distal das lamelas era mais compacta do que as da região proximal, enquanto que no Puro Sangue Inglês não foram observadas diferenças. Na microscopia eletrônica de varredura, o espaço intertubular do estrato médio foi visualmente maior. A partir desta arquitetura nós sugerimos que existe maior adesão da cápsula da úngula à falange distal no cavalo Baixadeiro, provavelmente diminuindo a incidência de rotação da falange distal e, consequentemente, diminuindo a laminite