77 research outputs found

    Permanence and changes in pastoral farming in the Southern Alps

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    The Southern Alps, where sheep farming is highly prevalent, is specific to the mountains of the Mediterranean region and, consequently, is in sharp contrast with the Northern Alps. The age-old practice of pastoralism that has shaped the landscapes and human societies has existed for thousands of years, questioning the emergence of the concept of naturality linked to this region. Nevertheless, the perception of the durability of an activity seen as traditional should not obscure the extent of changes that have had an impact on it in the past. In light of this, there is much to learn from the comparison between the major upheaval that affected pastoral farming at the end of the 19th century, and the current process of change whose outcome is not yet known. In both cases, changes in public policies and markets, as well as the emergence of new environmental stakes have determined or are in the processes of determining the future of pastoral farming. Faced with society’s increasingly specific but sometimes contradictory expectations, the types of livestock farming widely used in pastoral areas thus appear to be the best adapted to propose "natural" and local products, but the most vulnerable as well in view of the establishment of a large population of wolves. This contradiction is indicative of the shock of values between two societal projects for abandoned land, the first, heir to a rural tradition that is responsible for maintaining a human presence in the mountains, and the second, the vector of a “naturality” based on the reconstitution of ecological pyramids

    Dog predation over flocks of sheep in the Luberon area

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    Le Parc naturel rĂ©gional du Luberon a toujours soutenu l’élevage pastoral en tant qu’outil majeur de gestion de la biodiversitĂ© sur son territoire. L’inquiĂ©tude exprimĂ©e par les Ă©leveurs face Ă  l’éventualitĂ© de l’arrivĂ©e de loups a amenĂ© le PNRL, en collaboration avec le CERPAM, Ă  rĂ©aliser une enquĂȘte sur la prĂ©dation due aux chiens, afin de constituer un Ă©tat des lieux prĂ©alable sur le sujet. Une enquĂȘte exhaustive a Ă©tĂ© menĂ©e auprĂšs des Ă©leveurs sur l’ensemble du territoire du Luberon, afin de recenser les attaques de chiens et de comprendre les conditions de cette prĂ©dation. Les rĂ©sultats montrent une faible frĂ©quence d’attaques et un faible taux de prĂ©dation par les chiens dans cette rĂ©gion oĂč le cheptel ovin est important. Quelques sĂ©quences d’attaques concentrent la majoritĂ© des dommages. L’essentiel des problĂšmes est liĂ© Ă  la divagation de chiens du voisinage, trĂšs rarement Ă  des chiens rĂ©ellement « errants ». Enfin, les attaques de chiens n’ont rien de discret, ces derniers sont repĂ©rĂ©s visuellement dans 85% des Ă©pisodes de prĂ©dation. Les rĂ©sultats ont Ă©tĂ© comparĂ©s Ă  d’autres Ă©tudes menĂ©es dans d’autres rĂ©gions. La prĂ©dation due aux chiens est faible dans un autre massif des Alpes du Sud, mais plus forte dans les rĂ©gions oĂč le poids Ă©conomique de l’élevage ovin est rĂ©siduel. L’ambition du gestionnaire, au travers de cette Ă©tude, est d’amĂ©liorer la sensibilisation de tous les acteurs concernĂ©s pour limiter la divagation des chiens (rĂ©sidents, touristes, communes, chasseurs) mais aussi de se donner les moyens de gĂ©rer avec la plus grande transparence l’éventualitĂ© du retour des loups sur ce territoire.The pastoral breeding has always been supported by the Regional Natural Park of the Luberon as the tool for biodiversity maintenance. The sheep breeders anxiety of potential wolves predation has led the PNRL, in collaboration with the CERPAM (a technical breeders’ organization), to realise a study of the predation of dog origin, in order to define the state of the situation. An exhaustive inquiry of dogs attack has been carried on over the whole Luberon area breeders to count and to understand the conditions of this phenomenon. The results display a weak frequency of attacks of predation by the dogs in this region of important sheep concentration. Some attack events are concentrating the majority of the damage. The principal problem is neighbourhood dog wandering, and rarely from stray dogs. These dogs attacks are not discrete because for 85% of them, they were visually noticed. The results were then compared to other studies from different regions. This predation is also weak in an other area of the South Alps but is found more frequent in the regions with a limited sheep farming. The ambition of the Park of the Luberon with this study is to improve the sensibilisation of the territory actors in order to reduce this dog wandering but also, to have the necessary knowledge and conditions to face with clearness a potential wolf attack

    The « rare and sensitive biotopes » agro-environmental measure in the Luberon regional natural park : assesment for the territory and for breeding practices

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    Dans le massif du Luberon, une Mesure agri-environnementale (MAE) a Ă©tĂ© promue pour favoriser une gestion pastorale visant Ă  prĂ©server les « biotopes rares et sensibles ». Dans ce cadre, un suivi scientifique et technique a Ă©tĂ© mis en place et cet article vise Ă  Ă©tablir un bilan de son impact sur l’élevage et sur le territoire. Ainsi, un lien a Ă©tĂ© mis en Ă©vidence entre le type d’espaces ciblĂ©s par la mesure (grands espaces « sauvages » et Ă©cartĂ©s), et les types de systĂšmes d’élevage en mesure de s’engager (gros effectifs en phase de redĂ©ploiement). La MAE n’a pas mobilisĂ© les petits Ă©levages diversifiĂ©s ni les espaces qu’ils exploitent. Les pratiques pastorales engagĂ©s dans des milieux complexes ont souvent Ă©tĂ© novatrices. La logique contractuelle imposait la recherche d’indicateurs de rĂ©ussite. Or le suivi a montrĂ© que les Ă©leveurs s’appuient sur l’hĂ©tĂ©rogĂ©nĂ©itĂ© du territoire pour mieux s’adapter aux contraintes posĂ©es par le climat mĂ©diterranĂ©en sur des surfaces pastorales peu artificialisĂ©es. La contradiction entre la dĂ©finition de mesures contractuelles Ă  la surface, forcĂ©ment standardisĂ©es, et des pratiques pastorales extensives comporte un risque de rigidification. En dĂ©finitive, l’hypothĂšse est posĂ©e selon laquelle la diversitĂ© des systĂšmes d’élevage est le meilleur gage du maintien de milieux naturels diversifiĂ©s.Within the Luberon massif, an Agro-environmental Measure (AEM) was adopted to favor a pastoral management, which aims at preserving « rare and sensitive biotopes ». Within this scope, a scientific and technical follow-up was implemented ; this article aims at assessing its impact on breeding and on the territory. In this way, a link between the type of spaces targetted by the measure (vast « wild » and spread spaces) and the breeding practice modes able to suit the measure (great numbers in phase of redeployment) was brought to the fore. The AEM has not mobilized small diversified breeders and the spaces they exploit. Pastoral practices engaged in complex environments have often been innovative. A search for success indicators was imposed by the contractual logic. The follow-up showed that breeders rest on the territory’s heterogeneity to better adapt to the constraints of the Mediterranean climate on hardly man-shaped pasture surfaces. The contradiction between the definition of standardized contractual measures for the surface and extensive pastoral practices leads to the risk of becoming too rigid. As a conclusion, it would seem that the diversity of breeding systems is the best guarantee for the maintaining of diversified natural environments

    Grassy areas on the crests of the Luberon, sentinels of the global warming - Evolution of the grazed ecosystems during thirty years, from 1982 to 2011

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    Les crĂȘtes du Luberon sont occupĂ©es par des pelouses mĂ©diterranĂ©o- montagnardes Ă  forte biodiversitĂ©. Ces Ă©cosystĂšmes soumis Ă  des conditions climatiques difficiles sont façonnĂ©s depuis des siĂšcles par l’action de troupeaux ovins conduits en gardiennage. Depuis quelques dĂ©cennies, ces pelouses sont menacĂ©es par la dĂ©prise pastorale, l’érosion causĂ©e par la frĂ©quentation motorisĂ©e, les dĂ©gĂąts croissants de sangliers, enfin les accidents climatiques rĂ©pĂ©tĂ©s de cette derniĂšre dĂ©cennie. Le PNRL, avec le CERPAM, l’ONF et l’appui de la recherche (INRA d’Avignon, UniversitĂ© d’Aix-Marseille) a animĂ© depuis plus de trente ans des actions de conservation de ces habitats en confortant l’élevage pastoral (rĂ©ouverture des milieux, Ă©quipements pastoraux, mesures agri-environnementales). Un bilan est dressĂ© de l’évolution des pelouses sommitales du Luberon en mobilisant divers suivis mis en place depuis 1982 pour les plus anciens, permettant de comparer pelouses pĂąturĂ©es et non pĂąturĂ©es. Cette synthĂšse concerne principalement le Grand Luberon, dans une moindre mesure le Petit Luberon. Durant cette pĂ©riode, les chargements ont fortement baissĂ© sur le Grand Luberon alors que le niveau de ressource pastorale est restĂ© stable. Cette baisse s’explique dans le cadre d’un moindre besoin de la part des Ă©leveurs du piĂ©mont utilisateurs des crĂȘtes, d’une moindre incitation agri-environnementale dans le cadre des MAET Natura 2000, enfin de pratiques de garde qui ont Ă©voluĂ© vers un pĂąturage moins « serrĂ© ». Les suivis pastoraux confirment un maintien de la ressource pastorale, mais avec l’apparition de trouĂ©es colonisĂ©es par des graminĂ©es opportunistes, rĂ©sultant sans doute de la canicule de 2003 et des sĂ©cheresses des annĂ©es suivantes. Les suivis de biodiversitĂ© effectuĂ©s dans les deux massifs montrent une Ă©volution contrastĂ©e d’un certain nombre d’espĂšces floristiques phares. Mais les baisses dominent, notamment pour Genista pulchella subsp. villarsii, Anthyllis montana, Plantago argentea, Sempervivum calcareum, Valeriana tuberosa, Ephedra nebrodensis ; les rĂ©sultats sont comparables avec et sans pĂąturage, ce qui suggĂšre fortement une cause climatique: rĂ©pĂ©tition des canicules et sĂ©cheresses entre 2003 et 2006, et/ou dĂ©but du rĂ©chauffement climatique documentĂ© dans notre rĂ©gion depuis la fin des annĂ©es 1970.Luberon’s crests are occupied by mediterraneo-mountain grassy areas with strong biodiversity. These ecosystems affected by difficult climatic conditions have been shaped for centuries by the action of guarded ovine herds. Since a few decades, these areas are threatened by the decrease of pasture, the erosion caused by motorized circulation, increasing damages of wild boars, and the repeated climatic incidents of the last decade. For more than thirty years, the PNRL, with the CERPAM and the ONF, and with the support of research centers (INRA of Avignon, University of Aix-Marseille), has developed actions to preserve these natural ecosystems by consolidating the pastoral breeding (reopening of the environment, pastoral equipments, agri-environmental measures). A balance sheet of the evolution of sommitals grassland of Luberon is drawn up by mobilizing some follow-ups set up since 1982, allowing to compare grazed and non-grazed grasslands. This synthesis concerns mainly the Grand Luberon, and to a lesser extent the Petit Luberon. During this period, loads strongly decreased on Grand Luberon, while the level of pastoral resource remained stable. This decline can be explained by a lesser need of the breeders from piedmont, using crests, by a lesser agri-environmental incitement within Natura 2000, and by practices of guarding which evolved towards a « less tight » pasture. The follow-ups confirm a preservation of the pastoral resource, but with the appearance of places colonized by opportunist grasses, resulting from the heat wave of 2003 and from the droughts of the next years. The follow-ups of biodiversity made in both massifs show a contrasted evolution for a certain number of key floral species. But many species decline, in particular Genista pulchella ssp. villarsii, Anthyllis montana, Plantago argentea, Sempervivum calcareum, Valeriana tuberosa, Ephedra nebrodensis. The results are comparable with and without pasture, and this strongly suggests a climatic cause : repetition of the heat waves and the droughts between 2003 and 2006, and\or at the beginning of the global warming informed in our region since the end of 1970s

    Pastoralisme et gestion des espaces naturels en Provence

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    The Iceland Microcontinent and a continental Greenland-Iceland-Faroe Ridge

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    The breakup of Laurasia to form the Northeast Atlantic Realm was the culmination of a long period of tectonic unrest extending back to the Late Palaeozoic. Breakup was prolonged and complex and disintegrated an inhomogeneous collage of cratons sutured by cross-cutting orogens. Volcanic rifted margins formed, which are blanketed by lavas and underlain variously by magma-inflated, extended continental crust and mafic high-velocity lower crust of ambiguous and probably partly continental provenance. New rifts formed by diachronous propagation along old zones of weakness. North of the Greenland-Iceland-Faroe Ridge the newly forming rift propagated south along the Caledonian suture. South of the Greenland-Iceland-Faroe Ridge it propagated north through the North Atlantic Craton along an axis displaced ~ 150 km to the west of the northern rift. Both propagators stalled where the confluence of the Nagssugtoqidian and Caledonian orogens formed a transverse barrier. Thereafter, the ~ 400-km-wide latitudinal zone between the stalled rift tips extended in a distributed, unstable manner along multiple axes of extension that frequently migrated or jumped laterally with shearing occurring between them in diffuse transfer zones. This style of deformation continues to the present day. It is the surface expression of underlying magma-assisted stretching of ductile mid- and lower continental crust which comprises the Icelandic-type lower crust that underlies the Greenland-Iceland-Faroe Ridge. This, and probably also one or more full-crustal-thickness microcontinents incorporated in the Ridge, are capped by surface lavas. The Greenland-Iceland-Faroe Ridge thus has a similar structure to some zones of seaward-dipping reflectors. The contemporaneous melt layer corresponds to the 3–10 km thick Icelandic-type upper crust plus magma emplaced in the ~ 10–30-km-thick Icelandic-type lower crust. This model can account for seismic and gravity data that are inconsistent with a gabbroic composition for Icelandic-type lower crust, and petrological data that show no reasonable temperature or source composition could generate the full ~ 40-km thickness of Icelandic-type crust observed. Numerical modeling confirms that extension of the continental crust can continue for many tens of Myr by lower-crustal flow from beneath the adjacent continents. Petrological estimates of the maximum potential temperature of the source of Icelandic lavas are up to 1450 °C, no more than ~ 100 °C hotter than MORB source. The geochemistry is compatible with a source comprising hydrous peridotite/pyroxenite with a component of continental mid- and lower crust. The fusible petrology, high source volatile contents, and frequent formation of new rifts can account for the true ~ 15–20 km melt thickness at the moderate temperatures observed. A continuous swathe of magma-inflated continental material beneath the 1200-km-wide Greenland-Iceland-Faroe Ridge implies that full continental breakup has not yet occurred at this latitude. Ongoing tectonic instability on the Ridge is manifest in long-term tectonic disequilibrium on the adjacent rifted margins and on the Reykjanes Ridge, where southerly migrating propagators that initiate at Iceland are associated with diachronous swathes of unusually thick oceanic crust. Magmatic volumes in the NE Atlantic Realm have likely been overestimated and the concept of a monogenetic North Atlantic Igneous Province needs to be reappraised. A model of complex, piecemeal breakup controlled by pre-existing structures that produces anomalous volcanism at barriers to rift propagation and distributes continental material in the growing oceans fits other oceanic regions including the Davis Strait and the South Atlantic and West Indian oceans

    Identification of genetic variants associated with Huntington's disease progression: a genome-wide association study

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    Background Huntington's disease is caused by a CAG repeat expansion in the huntingtin gene, HTT. Age at onset has been used as a quantitative phenotype in genetic analysis looking for Huntington's disease modifiers, but is hard to define and not always available. Therefore, we aimed to generate a novel measure of disease progression and to identify genetic markers associated with this progression measure. Methods We generated a progression score on the basis of principal component analysis of prospectively acquired longitudinal changes in motor, cognitive, and imaging measures in the 218 indivduals in the TRACK-HD cohort of Huntington's disease gene mutation carriers (data collected 2008–11). We generated a parallel progression score using data from 1773 previously genotyped participants from the European Huntington's Disease Network REGISTRY study of Huntington's disease mutation carriers (data collected 2003–13). We did a genome-wide association analyses in terms of progression for 216 TRACK-HD participants and 1773 REGISTRY participants, then a meta-analysis of these results was undertaken. Findings Longitudinal motor, cognitive, and imaging scores were correlated with each other in TRACK-HD participants, justifying use of a single, cross-domain measure of disease progression in both studies. The TRACK-HD and REGISTRY progression measures were correlated with each other (r=0·674), and with age at onset (TRACK-HD, r=0·315; REGISTRY, r=0·234). The meta-analysis of progression in TRACK-HD and REGISTRY gave a genome-wide significant signal (p=1·12 × 10−10) on chromosome 5 spanning three genes: MSH3, DHFR, and MTRNR2L2. The genes in this locus were associated with progression in TRACK-HD (MSH3 p=2·94 × 10−8 DHFR p=8·37 × 10−7 MTRNR2L2 p=2·15 × 10−9) and to a lesser extent in REGISTRY (MSH3 p=9·36 × 10−4 DHFR p=8·45 × 10−4 MTRNR2L2 p=1·20 × 10−3). The lead single nucleotide polymorphism (SNP) in TRACK-HD (rs557874766) was genome-wide significant in the meta-analysis (p=1·58 × 10−8), and encodes an aminoacid change (Pro67Ala) in MSH3. In TRACK-HD, each copy of the minor allele at this SNP was associated with a 0·4 units per year (95% CI 0·16–0·66) reduction in the rate of change of the Unified Huntington's Disease Rating Scale (UHDRS) Total Motor Score, and a reduction of 0·12 units per year (95% CI 0·06–0·18) in the rate of change of UHDRS Total Functional Capacity score. These associations remained significant after adjusting for age of onset. Interpretation The multidomain progression measure in TRACK-HD was associated with a functional variant that was genome-wide significant in our meta-analysis. The association in only 216 participants implies that the progression measure is a sensitive reflection of disease burden, that the effect size at this locus is large, or both. Knockout of Msh3 reduces somatic expansion in Huntington's disease mouse models, suggesting this mechanism as an area for future therapeutic investigation

    Ressources pastorales en Haute-Provence et modelisation de la relation vegetation/troupeau

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    SIGLEINIST T 72784 / INIST-CNRS - Institut de l'Information Scientifique et TechniqueFRFranc
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