Selección y estimación de parámetros genéticos en bovinos lecheros

La estimación de parámetros genéticos en bovinos lecheros requiere ajustar modelos estadísticos para datos longitudinales (modelos de regresión aleatoria y/o medidas repetidas). Es esencial en regresión aleatoria determinar el orden correcto de los polinomios que describen los coeficientes aleatorios en el tiempo. Tradicionalmente, esta tarea se desarrolló empleando criterios de selección como AIC o BIC, que no siempre logran dilucidar claramente el modelo apropiado. Esta tesis introduce el criterio PAL para la selección del orden del polinomio en modelos de regresión aleatoria, empleando una penalización adaptativa de la función de verosimilitud. Comparativamente, PAL presentó un desempeño superior a AIC y BIC, y su aplicación a datos de producción produjo un modelo parsimonioso, con buena bondad de ajuste y habilidad de predicción. Se abordó además el problema de estimar parámetros genéticos bajo un modelo de medidas repetidas para caracteres que muestran distribución asimétrica. Para evitar desvíos del supuesto de normalidad de los errores, se presentó un modelo alternativo basado en asumir una distribución Normal asimétrica. Se implementó un enfoque bayesiano con muestreo de Gibbs en datos de intervalos entre partos. Incluyendo un parámetro adicional, se obtuvieron estimaciones más precisas de los parámetros genéticos. Estos desarrollos metodológicos estuvieron motivados por los desafíos que enfrenta actualmente el programa de mejoramiento genético de la raza Holstein en Colombia. Entre ellos, figura también el impacto de introducir toros extranjeros provenientes del programa de selección genómica norteamericana. En este marco, se estimó el progreso genético esperado en la población comercial colombiana. Los cálculos reflejaron que utilizar toros genómicos jóvenes se traducirá en una respuesta genética acelerada y en una disminución de la diferencia genética entre el hato comercial y el núcleo del cual provienen.

Mineralogy and geochemistry of Holocene sediments from the North Atlantic

Bulk mineralogy, Sm, Nd and Pb elemental and isotopic compositions of the clay-size fraction of Holocene sediments were analyzed in three deep North Atlantic cores to trace the particle provenance. The aims of the present paper are to identify the origin of the particles driven by deep currents and to reconstruct deep circulation changes over the Holocene in the North Atlantic. The three cores are retrieved in fracture zones; two of them are located in the Island Basin along the gyre of North Atlantic Deep Water, and the third core is located off the present deep circulation gyre in the Labrador Sea. Whereas sedimentary supplies in the Labrador Sea were constantly derived from proximal sources, the geochemical mixing trends in the Iceland Basin samples indicate pronounced changes in the relative contribution of continental margin inputs over the past 6 kyr. Supplies from western European margin that sharply increased at 6 kyr were progressively diluted by a larger contribution of Scandinavian margins over the last 3 kyr. Changes in composition of the particles imply significant reorganization of paleocirculation of the deep North Atlantic components in the eastern basins: mainly reorganizations for both Iceland-Scotland Overflow Water and Norwegian Sea Overflow Water. Moreover the unusual Pb isotopic composition of the oldest sediments from the southern Iceland Basin indicates that distal supplies from Greenland margin were driven into the Iceland Basin, supporting a deep connection between Labrador Sea and Iceland Basin through the Charlie Gibbs Fracture Zone prior the Holocene Transition period.

Soil carbon in the Jena Experiment (all blocks Main Experiment up to 30cm depth, year 2006)

This data set contains soil carbon measurements (Organic carbon, inorganic carbon, and total carbon; all measured in dried soil samples) from the main experiment plots of a large grassland biodiversity experiment (the Jena Experiment; see further details below). In the main experiment, 82 grassland plots of 20 x 20 m were established from a pool of 60 species belonging to four functional groups (grasses, legumes, tall and small herbs). In May 2002, varying numbers of plant species from this species pool were sown into the plots to create a gradient of plant species richness (1, 2, 4, 8, 16 and 60 species) and functional richness (1, 2, 3, 4 functional groups). Plots were maintained by bi-annual weeding and mowing. Soil sampling and analysis: Stratified soil sampling was performed in April 2006 to a depth of 30 cm. Three samples per plot were taken using a split tube sampler with an inner diameter of 4.8 cm (Eijkelkamp Agrisearch Equipment, Giesbeek, the Netherlands). Sampling locations were less than 30 cm apart from sampling locations in 2002. Soil samples were segmented into 5 cm depth segments in the field (resulting in six depth layers) and made into composite samples per depth. Subsequently, samples were dried at 40°C. All soil samples were passed through a sieve with a mesh size of 2 mm. Because of much higher proportions of roots in the soil, samples in years after 2002 were further sieved to 1 mm according to common root removal methods. No additional mineral particles were removed by this procedure. Total carbon concentration was analyzed on ball-milled subsamples (time 4 min, frequency 30 s**-1) by an elemental analyzer at 1150°C (Elementaranalysator vario Max CN; Elementar Analysensysteme GmbH, Hanau, Germany). We measured inorganic carbon concentration by elemental analysis at 1150°C after removal of organic carbon for 16 h at 450°C in a muffle furnace. Organic carbon concentration was calculated as the difference between both measurements of total and inorganic carbon.