Selenium status of cats in four regions of the world and comparison with reported incidence of hyperthyroidism in cats in those regions

Objective: To assess selenium (Se) status of cats in 4 regions of the world and to compare results for Se status with reported incidence of hyperthyroidism in cats in those regions. Animals: 50 cats (30 from 2 regions with an allegedly high incidence of hyperthyroidism and 20 from 2 regions in which the disease is less commonly reported). Procedure: Hematologic samples (heparinized whole blood, plasma, and RBC fractions) were obtained from 43 healthy euthyroid cats and 7 hyperthyroid cats. Plasma concentration of Se and activity of glutathione peroxidase (GPX) in whole blood and plasma were determined. Results: Plasma concentration of Se and GPX activity in whole blood or plasma did not differ significantly among cats from the 4 regions. However, cats had a plasma concentration of Se that was approximately 5 times the concentration reported in rats and humans. The GPX activity in whole blood or plasma in cats generally was higher than values reported in rats or humans. Conclusions and Clinical Relevance: Cats have higher Se concentrations in plasma, compared with values for other species. However, Se status alone does not appear to affect the incidence of hyperthyroidism in cats. High Se concentrations may have implications for health of cats if such concentrations are influenced by the amount of that micronutrient included in diets

Equilíbrio ácido-base e hidroeletrolítico em eqüinos com cólica Acid-base and hidroelectrolytic balance in colic horses

Foram utilizados setenta eqüinos distribuídos em três grupos experimentais, G1 (vinte eqüinos hígidos), G2 (vinte e cinco eqüinos com cólica, os quais passaram por tratamento clínico ou cirúrgico e sobreviveram) e G3 (vinte e cinco eqüinos com cólica, os quais passaram por tratamento clínico ou cirúrgico e foram a óbito ou foram sacrificados). Amostras de sangue foram obtidas em dez diferentes momentos, mediante punção da jugular, para estudo do equilíbrio ácido-base e hidroeletrolítico. Os eqüinos com cólica apresentaram diminuição (P<0,05) nos valores do pH(v), principalmente os animais do G3, a qual, associada com a diminuição da pCO2(v), cBase(v) e cHCO-3(vP), confirmou a acidose metabólica, que teve como origem a produção aumentada de lactato durante a glicólise anaeróbica decorrente da hipovolemia. Adicionalmente apresentaram hiponatremia, hipocalemia e hipercloremia. A presença e a magnitude dos desequilíbrios contribuíram substancialmente com o prognóstico dos animais com cólica.<br>Seventy horses were distributed into three experimental groups ad follows: G1, twenty healthy animals; G2, twenty-five colic horses that survived after clinical or surgical treatment; and G3, twenty-five colic horses that were sacrificed or died after clinical or surgical treatment. Blood samples were taken from the jugular vein to assess acid-base balance and water-electrolyte balance. Colic horses had lower pH(v) (P<0.05), mainly G3 animals. Acidosis was confirmed by the lower pH(v) associated with decreased pCO2(v), cBase(v) and cHCO-3(vP), which was probably due to an increased production of lactate during anaerobic glycolysis as a result from hypovolemia. Furthermore, hyponatremia, hypokalemia and hyperchloremia were detected. The presence and the extent of the imbalances contributed substantially to the prognosis of colic horses

Exploring controls of the early and stepped deglaciation on the western margin of the British Irish Ice Sheet

New optically stimulated luminescence dating and Bayesian models integrating all legacy and BRITICE-CHRONO geochronology facilitated exploration of the controls on the deglaciation of two former sectors of the British–Irish Ice Sheet, the Donegal Bay (DBIS) and Malin Sea ice-streams (MSIS). Shelf-edge glaciation occurred ~27 ka, before the global Last Glacial Maximum, and shelf-wide retreat began 26–26.5 ka at a rate of ~18.7–20.7 m a–1. MSIS grounding zone wedges and DBIS recessional moraines show episodic retreat punctuated by prolonged still-stands. By ~23–22 ka the outer shelf (~25 000 km2) was free of grounded ice. After this time, MSIS retreat was faster (~20 m a–1 vs. ~2–6 m a–1 of DBIS). Separation of Irish and Scottish ice sources occurred ~20–19.5 ka, leaving an autonomous Donegal ice dome. Inner Malin shelf deglaciation followed the submarine troughs reaching the Hebridean coast ~19 ka. DBIS retreat formed the extensive complex of moraines in outer Donegal Bay at 20.5–19 ka. DBIS retreated on land by ~17–16 ka. Isolated ice caps in Scotland and Ireland persisted until ~14.5 ka. Early retreat of this marine-terminating margin is best explained by local ice loading increasing water depths and promoting calving ice losses rather than by changes in global temperatures. Topographical controls governed the differences between the ice-stream retreat from mid-shelf to the coast