23 resultados para Alpine grassland


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Alpine tree-line ecotones are characterized by marked changes at small spatial scales that may result in a variety of physiognomies. A set of alternative individual-based models was tested with data from four contrasting Pinus uncinata ecotones in the central Spanish Pyrenees to reveal the minimal subset of processes required for tree-line formation. A Bayesian approach combined with Markov chain Monte Carlo methods was employed to obtain the posterior distribution of model parameters, allowing the use of model selection procedures. The main features of real tree lines emerged only in models considering nonlinear responses in individual rates of growth or mortality with respect to the altitudinal gradient. Variation in tree-line physiognomy reflected mainly changes in the relative importance of these nonlinear responses, while other processes, such as dispersal limitation and facilitation, played a secondary role. Different nonlinear responses also determined the presence or absence of krummholz, in agreement with recent findings highlighting a different response of diffuse and abrupt or krummholz tree lines to climate change. The method presented here can be widely applied in individual-based simulation models and will turn model selection and evaluation in this type of models into a more transparent, effective, and efficient exercise.

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A Catalunya, la protecció i gestió de zones d’especial interès natural ha estat majoritàriament realitzada pel conjunt de les administracions públiques. Tot i així, en els últims anys han sorgit un conjunt d’iniciatives privades que a través d’acords de custòdia han passat a tenir un paper actiu en la protecció i gestió d’algunes finques amb un alt valor natural. És el cas de la finca els Cingles de l’Avenc, on s’ha dut a terme aquest treball, en la qual es pretén desenvolupar una activitat ramadera compatible amb la conservació dels valors naturals de la finca. L’objectiu principal d’aquest treball és conèixer la producció i qualitat farratgera dels diferents tipus de pastures que hi ha a la finca, i establir la càrrega ramadera que poden admetre. Aquest estudi ha tingut una durada de 3 anys i en aquest treball es presenten els resultats del 2011 i es fa l’anàlisi dels resultats dels 3 anys (2009, 2010, i 2011). L’estudi s’ha portat a terme en els 4 tipus principals de pastures que hi ha a la finca: joncedes, pastures mesòfiles, prats de dall i pastures sembrades. S’han utilitzat 11 parcel·les permanents excloses de la pastura, establertes l’any 2009, que inclouen la diversitat de tipus i zones de pastura. S’ha realitzat un mostreig de la biomassa mensual, d’abril a novembre, que ha consistit en dallar 4 quadrats de 50 x 50 cm, i s’ha calculat la producció anual. S’ha determinat la qualitat farratgera de l’herba de 4 moments de l’any: maig, juny, juliol i octubre. Després dels tres anys d’estudi hem obtingut que les pastures sembrades i els prats de dall són els més productius (1.067 g/m2.any i 1.005 g/m2.any, respectivament). La producció de les pastures mesòfiles i de les joncedes són més baixes (554 g/m2.any i 291 g/m2.any, respectivament). La qualitat farratgera de les pastures és bona a totes les comunitats, amb valors mitjans de proteïna digerible de 6,63%, de fibra bruta de 29,13%, de lignina de 7,29% i de 0,69 (ENL/1,700) unitats farratgeres. La producció anual global obtinguda a la finca durant aquests tres anys permet suportar una càrrega ramadera admissible d’unes 208 UBG (Unitats de Bestiar Gros. 1 U.B.G equival a 1 vaca a partir de 2 anys).

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This work includes the first results of some excursions to a number of representative localities of Spanish Pyrenees in the region of Jaca, mainly focused on the epiphytes of the fir and beech woods, of Scots pine and of Pinus uncinata, calcareous and siliceous alpine rocks, and also on urban tree lichens in Jaca. The result is an annotated list comprising 228 species, of which 47 are new to Spain and a hundred were not previously reported from the Spanish Pyrenees. Furthermore, it has been possible to recognize some typical examples of alpine associations and also of epiphytic associations rich in oceanic lichens, well known outside of Spain.

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The high alpine valleys in the Southem Pyrenees are characterised by a many small lakes and ponds. They occur above 2000 m and are said to have been formed by glacial erosion. The sediments in these basins should, therefore, contain s t p tigraphic information since deglaciation, at least. An interesting and may be one of the most important of these basins is Lake Llauset in the Alta Ribagorca. The Llauset basin has recently been developped for hydsopower production. In conection with the construction of the retaining wall at the 'Riegel' the sedimentary filling of the lake basin could be investigated, and the first sedimentological and stratigraphicalresults are presented.

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Des programmes de recherche pluridisciplinaires sur l’occupation du sol et le pastoralisme de la Préhistoire au Moyen Âge dans le sud du massif alpin sont menés, depuis 1998, sur les massifs du Haut Champsaur, de Freissinières et de l’Argentièrois (Hautes-Alpes). Des dix phases d’occupation et d'activité agropastorale mises en évidence (prospections pédestres et fouilles), entre 1600 et 2700 m d’altitude, trois se distinguent: la fin du Néolithique, l’âge du Bronze et la période médiévale. Au travers des premières données archéologiques et environnementales, cet article présente, depuis le milieu du IIIe millénaire au début du Ier millénaire, les grandes caractéristiques de l’occupation du sol mais aussi l’originalité et l’importance de l’activité humaine dans cette zone alpine. La fin du Néolithique et l’âge du Bronze correspondent à une multiplication des gisements archéologiques marquant de façon évidente une rupture dans la gestion de l'espace montagnard. Les paysages sont largement façonnés par les activités humaines et l’entretien des terres cultivées, des prairies et des alpages, paraît continu. À la lumière des données de terrain, l’une des évolutions qui apparaît sur les sites d’altitude durant cette période concerne l’apparition de structures pastorales bâties entre 2 067 et 2 303 m d’altitude (datation 14C).

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Background: Myotragus balearicus was an endemic bovid from the Balearic Islands (Western Mediterranean) that became extinct around 6,000-4,000 years ago. The Myotragus evolutionary lineage became isolated in the islands most probably at the end of the Messinian crisis, when the desiccation of the Mediterranean ended, in a geological date established at 5.35 Mya. Thus, the sequences of Myotragus could be very valuable for calibrating the mammalian mitochondrial DNA clock and, in particular, the tree of the Caprinae subfamily, to which Myotragus belongs. Results: We have retrieved the complete mitochondrial cytochrome b gene (1,143 base pairs), plus fragments of the mitochondrial 12S gene and the nuclear 28S rDNA multi-copy gene from a well preserved Myotragus subfossil bone. The best resolved phylogenetic trees, obtained with the cytochrome b gene, placed Myotragus in a position basal to the Ovis group. Using the calibration provided by the isolation of Balearic Islands, we calculated that the initial radiation of caprines can be dated at 6.2 ± 0.4 Mya. In addition, alpine and southern chamois, considered until recently the same species, split around 1.6 ± 0.3 Mya, indicating that the two chamois species have been separated much longer than previously thought. Conclusion: Since there are almost no extant endemic mammals in Mediterranean islands, the sequence of the extinct Balearic endemic Myotragus has been crucial for allowing us to use the Messinian crisis calibration point for dating the caprines phylogenetic tree.

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The general objective of the international MEDiterranean EXperiment (MEDEX) was the better understanding and forecasting of cyclones that produce high impact weather in the Mediterranean. This paper reviews the motivation and foundation of MEDEX, the gestation, history and organisation of the project, as well as the main products and scientific achievements obtained from it. MEDEX obtained the approval of World Meteorological Organisation (WMO) and can be considered as framed within other WMO actions, such as the ALPine EXperiment (ALPEX), the Mediterranean Cyclones Study Project (MCP) and, to a certain extent, THe Observing System Research and Predictability EXperiment (THORPEX) and the HYdrological cycle in Mediterranean EXperiment (HyMeX). Through two phases (2000 2005 and 2006 2010), MEDEX has produced a specific database, with information about cyclones and severe or high impact weather events, several main reports and a specific data targeting system field campaign (DTS-MEDEX-2009). The scientific achievements are significant in fields like climatology, dynamical understanding of the physical processes and social impact of cyclones, as well as in aspects related to the location of sensitive zones for individual cases, the climatology of sensitivity zones and the improvement of the forecasts through innovative methods like mesoscale ensemble prediction systems.

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In the mid-20th century, the southern parts of the Madres and Mont Coronat massif (Eastern Pyrenees, France) were characterized by a Mediterranean landscape shaped by human activity. Long-term use of these mountains for crops, livestock, and forestry led to an increase in grassland areas at the expense of forest. However, socioeconomic transformation (abandonment of agriculture and a decrease in the rural population) in recent decades has caused profound changes in this massif. Interpretation of aerial photographs (1953, 1969, 1988, and 2000) made it possible to detect and analyze the changes produced in the study area (6787 ha) during this period. In 1953 most of the massif landscape consisted of grasslands (38%) and open forests (18%), with some areas of dense forest (15%). By 2000, dense forest cover had doubled in size (31%), and grassland had decreased considerably (by 73% of the initial area). Since 1953, the study area has become more homogeneous, with a few local exceptions. The results of this study suggest that socioeconomic factors might be the main cause of landscape transformations in this period of approximately 50 years.