Condição corporal ao parto e produção de leite sobre o desempenho reprodutivo de vacas holandesas em lactação

O objetivo, neste estudo, foi avaliar os efeitos da condição corporal ao parto e da mudança de condição corporal sobre o desempenho reprodutivo de vacas leiteiras após o parto. Para tanto, 51 vacas holandesas, de 30 dias pré-parto até 150 dias após o parto, foram distribuídas aleatoriamente de acordo com a condição corporal ao parto nas classes 1 (condição corporal maior ou igual a 3,25) e 2 (condição corporal menor ou igual a 3,0). Dentro das classes de condição corporal ao parto, os animais foram distribuídos quanto à mudança de condição corporal (Categoria 1, igual ou menor que -0,50 e Categoria 2, igual ou maior que -0,75) e à média da produção de leite ajustada para 3,5% aos 150 dias (Grupo 1 = 22,61 e Grupo 2 = 31,65 kg/dia). Não houve diferenças da condição corporal ao parto e da produção de leite ajustada para 3,5% sobre o intervalo parto primeiro estro, intervalo parto primeiro serviço, período de serviço, número de serviço / concepção e taxa de gestação aos 150 dias de lactação. Vacas que ao parto apresentaram média de escore de condição corporal de 3,40 e 2,79 tiveram semelhante desempenho reprodutivo pósparto. Em relação à produção de leite ajustada para 3,5%, vacas com produção média de 22,61 e 31,65 apresentaram similares resultados. A mudança de condição corporal não influenciou o intervalo parto primeiro serviço, o período de serviço e o número de serviço por concepção, mas apresentaram maior intervalo parto primeiro estro e menor taxa de gestação

Laser locking to the Hg-199 S-1(0)-P-3(0) clock transition with 5.4x10(-15)/root tau fractional frequency instability

With Hg-199 atoms confined in an optical lattice trap in the Lamb-Dicke regime, we obtain a spectral line at 265.6 nm for which the FWHM is similar to 15 Hz. Here we lock an ultrastable laser to this ultranarrow S-1(0) - P-3(0) clock transition and achieve a fractional frequency instability of 5.4 x 10(-15) / root tau for tau <= 400 s. The highly stable laser light used for the atom probing is derived from a 1062.6 nm fiber laser locked to an ultrastable optical cavity that exhibits a mean drift rate of -6.0 x 10(-17) s-(1) (-16.9 mHzs(-1) at 282 THz) over a six month period. A comparison between two such lasers locked to independent optical cavities shows a flicker noise limited fractional frequency instability of 4 x 10(-16) per cavity. (c) 2012 Optical Society of America

Petrogenesis of syntectonic granites emplaced at the transition from thrusting to transcurrent tectonics in post-collisional setting: Whole-rock and Sr-Nd-Pb isotope geochemistry in the Neoproterozoic Quatro Ilhas and Mariscal Granites, Southern Brazil

The Neoproterozoic post-collisional period in southern Brazil (650-580 Ma) is characterized by substantial volumes of magma emplaced along the active shear zones that compose the Southern Brazilian Shear Belt. The early-phase syntectonic magmatism (630-610 Ma) is represented by the porphyritic, high-K, metaluminous to peraluminous Quatro Ilhas Granitoids and the younger heterogranular, slightly peraluminous Mariscal Granite. Quatro II has Granitoids include three main petrographic varieties (muscovite-biotite granodiorite mbg; biotite monzogranite - bmz: and leucogranite - lcg) that, although sharing some significant geochemical characteristics, are not strictly comagmatic, as shown by chemical and Sr-Nd-Pb isotope data. The most primitive muscovite-biotite granodiorite was produced by contamination of more mafic melts (possibly with some mantle component) with peraluminous crustal melts; the biotite monzogranite, although more felsic, has higher Ca, MgO,TiO2 and Ba, and lower K2O, FeOt, Sr and Rb contents, possibly reflecting some mixing with coeval mafic magmas of tholeiitic affinity; the leucogranite may be derived from pure crustal melts. The Mariscal Granite is formed by two main granite types which occur intimately associated in the same pluton, one with higher K (5-6.5 wt.% K2O) high Rb and lower CaO, Na2O, Ba and Zr as compared to the other (3-5 wt.% of K2O). The two Mariscal Granite varieties have compositional correspondence with fine-grained granites (fgg) that occur as tabular bodies which intruded the Quatro Ilhas Granoitoids before they were fully crystallized, and are inferred to correspond to the Mariscal Granite feeders, an interpretation that is reinforced by similar U-Pb zircon crystallization ages. The initial evolution of the post-collisional magmatism, marked by the emplacement of the Quatro Ilhas Granitoids varieties, activated sources that produced mantle and crustal magmas whose emplacement was controlled both by flat-lying and transcurrent structures. The transition from thrust to transcurrent-related tectonics coincides with the increase in the proportion of crustal-derived melts. The transcurrent tectonics seems to have played an essential role in the generation of mantle-derived magmas and may have facilitated their interaction with crustal melts which seem to be to a large extent the products of reworking of orthogneiss protoliths. (C) 2012 Elsevier B.V. All rights reserved.