<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Santos, Sara M</style></author><author><style face="normal" font="default" size="100%">Mathias, Maria Da Luz</style></author><author><style face="normal" font="default" size="100%">Mira, António P</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The influence of local, landscape and spatial factors on the distribution of the Lusitanian and the Mediterranean pine voles in a Mediterranean landscape</style></title><secondary-title><style face="normal" font="default" size="100%">Mammalian Biology - Zeitschrift für Säugetierkunde</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">microtus duodecimcostatus</style></keyword><keyword><style  face="normal" font="default" size="100%">microtus lusitanicus</style></keyword><keyword><style  face="normal" font="default" size="100%">scale</style></keyword><keyword><style  face="normal" font="default" size="100%">Spatial effects</style></keyword><keyword><style  face="normal" font="default" size="100%">variance partitioning</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><publisher><style face="normal" font="default" size="100%">Elsevier GmbH</style></publisher><volume><style face="normal" font="default" size="100%">76</style></volume><pages><style face="normal" font="default" size="100%">133-142</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This study evaluated the relative contributions of local and landscape factors, and of spatial structure on the regional distribution of both the Lusitanian (Microtus lusitanicus Gerbe, 1879) and Mediterranean pine voles (Microtus duodecimcostatus de Selys-Longchamps, 1839) over an area of 1613 km2 within a Mediterranean landscape in central Portugal. Three sets of explanatory variables (20 local, 23 landscape, and 6 spatial) were analysed independently by means of a generalized linear model, followed by a variance partitioning procedure. Variance in the distribution patterns of M. lusitanicus and M. duodecimcostatus largely was explained by ﬁne-scale environmental factors but spatial effects also were important, especially for the distribution of M. duodecimcostatus. The close proximity of verges and the high abundance of humidity and coarse sand in the soil were the most inﬂuencing local-scale factors for the presence of M. lusitanicus; meanwhile on a larger scale, the high abundance of linear habitats was the main landscape feature determining its occurrence. Regarding the presence of M. duodecimcostatus, the close proximity of verges, high tree canopy cover and herbaceous vegetation biomass were the most inﬂuential local explanatory variables for its occurrence, while the absence of shrubs in the surrounding habitat was the main factor regulating species presence at a landscape scale. Similarities identiﬁed between the two species primarily were related to descriptors of cover, food and burrows, while differences were related to opposing spatial trends and coarse-scale descriptors.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Barbancho, A. C.</style></author><author><style face="normal" font="default" size="100%">Schnabel, S.</style></author><author><style face="normal" font="default" size="100%">Bolinches, C.</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Grandal, A. and Pages</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Effect of scale on surface runoff processes</style></title><secondary-title><style face="normal" font="default" size="100%">CADERNOS DO LABORATORIO XEOLOXICO DE LAXE 21</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">ecosystem dehesa</style></keyword><keyword><style  face="normal" font="default" size="100%">scale</style></keyword><keyword><style  face="normal" font="default" size="100%">soil erosion</style></keyword><keyword><style  face="normal" font="default" size="100%">surface runoff</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1996</style></year><pub-dates><date><style  face="normal" font="default" size="100%">1996///</style></date></pub-dates></dates><publisher><style face="normal" font="default" size="100%">EDICIOS CASTRO</style></publisher><volume><style face="normal" font="default" size="100%">21</style></volume><pages><style face="normal" font="default" size="100%">91 - 102</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">In a small catchment under the so-called dehesa landuse system, the production of surface runoff is investigated at different scales. This includes experiments with simulated rainfall at micro-plots, event-based measurements of overland flow at 17 open plots and 1 closed plot, and discharge production of the catchment and subcatchment. The runoff coefficients of the considered scales form two groups, with low values for the catchment and sub-catchment and high values for the microplots and hillslope plots. The results show that large part of runoff produced at the slopes is infiltrated afterwards at colluvial sites and the valley floors. Furthermore, they indicate the importance of studying at various scales in order to understand the hydrological processes operating in catchments.</style></abstract><notes><style face="normal" font="default" size="100%">The following values have no corresponding Zotero field:&lt;br/&gt;periodical: CADERNOS DO LABORATORIO XEOLOXICO DE LAXE 21&lt;br/&gt;pub-location: O CASTRO DE SAMOEDO, 15168 SADA, LA CORUNA, SPAIN</style></notes></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>3</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Barbancho, A C</style></author><author><style face="normal" font="default" size="100%">Schnabel, S</style></author><author><style face="normal" font="default" size="100%">Bolinches, C</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Grandal, A and Pages, L</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Effect of scale on surface runoff processes</style></title><secondary-title><style face="normal" font="default" size="100%">CADERNOS DO LABORATORIO XEOLOXICO DE LAXE 21</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">ecosystem dehesa</style></keyword><keyword><style  face="normal" font="default" size="100%">scale</style></keyword><keyword><style  face="normal" font="default" size="100%">soil erosion</style></keyword><keyword><style  face="normal" font="default" size="100%">surface runoff</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1996</style></year></dates><publisher><style face="normal" font="default" size="100%">EDICIOS CASTRO</style></publisher><pub-location><style face="normal" font="default" size="100%">O CASTRO DE SAMOEDO, 15168 SADA, LA CORUNA, SPAIN</style></pub-location><volume><style face="normal" font="default" size="100%">21</style></volume><pages><style face="normal" font="default" size="100%">91-102</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">In a small catchment under the so-called dehesa landuse system, the production of surface runoff is investigated at different scales. This includes experiments with simulated rainfall at micro-plots, event-based measurements of overland flow at 17 open plots and 1 closed plot, and discharge production of the catchment and subcatchment. The runoff coefficients of the considered scales form two groups, with low values for the catchment and sub-catchment and high values for the microplots and hillslope plots. The results show that large part of runoff produced at the slopes is infiltrated afterwards at colluvial sites and the valley floors. Furthermore, they indicate the importance of studying at various scales in order to understand the hydrological processes operating in catchments.</style></abstract></record></records></xml>