Dispersal is a major driver of the latitudinal diversity gradient of Carnivora

AimUnderstanding the relative contribution of diversification rates (speciation and extinction) and dispersal in the formation of the latitudinal diversity gradient - the decrease in species richness with increasing latitude - is a main goal of biogeography. The mammalian order Carnivora, which comprises 286 species, displays the traditional latitudinal diversity gradient seen in almost all mammalian orders. Yet the processes driving high species richness in the tropics may be fundamentally different in this group from that in other mammalian groups. Indeed, a recent study suggested that in Carnivora, unlike in all other major mammalian orders, net diversification rates are not higher in the tropics than in temperate regions. Our goal was thus to understand the reasons why there are more species of Carnivora in the tropics. LocationWorld-wide. MethodsWe reconstructed the biogeographical history of Carnivora using a time-calibrated phylogeny of the clade comprising all terrestrial species and dispersal-extinction-cladogenesis models. We also analysed a fossil dataset of carnivoran genera to examine how the latitudinal distribution of Carnivora varied through time. ResultsOur biogeographical analyses suggest that Carnivora originated in the East Palaearctic (i.e. Central Asia, China) in the early Palaeogene. Multiple independent lineages dispersed to low latitudes following three main paths: toward Africa, toward India/Southeast Asia and toward South America via the Bering Strait. These dispersal events were probably associated with local extinctions at high latitudes. Fossil data corroborate a high-latitude origin of the group, followed by late dispersal events toward lower latitudes in the Neogene. Main conclusionsUnlike most other mammalian orders, which originated and diversified at low latitudes and dispersed out of the tropics', Carnivora originated at high latitudes, and subsequently dispersed southward. Our study provides an example of combining phylogenetic and fossil data to understand the generation and maintenance of global-scale geographical variations in species richness.

Physiologie et biomécanique du ski-alpinisme

Introduction: Ski mountaineering is an increasingly popular winter sport and leisure activity. Elite athletes practice this sport with a high level of professionalism, but so far little scientific evidence was available to support their approach. The main aim of this work was to develop a specific knowledge about ski mountaineering, allowing providing specific recommendations for the practice. Methods: First we investigated energy cost (EC) and vertical energy cost (ECv). These two parameters were estimated with oxygen uptake, at different gradients (7 to 33%) and different speeds (2 to 7 km·∙h-­‐1) on treadmill with roller skis and on snow with ski mountaineering gear. Then we assessed energy expenditure (EE) during a long duration ski mountaineering event by measuring heart rate and altitude all along the race and associating them with an EE. The EE was compared with the energy intake during the race. Hydration level was estimated by comparing body weight immediately before and after the race. The energy intake during the 4 days preceding the race was estimated with food diaries and compared with the guidelines. Results/discussion: EC and ECv of ski mountaineering were very high and varied with gradient and speed. ECv decreased between 7 and 33% and with increasing speed at steep gradients. For a 5 h 51 ± 53 min race, the mean EE was 22.6 ± 2.6 MJ. The energy intake covered 20 ± 7% of the EE and was about 14% lower than the recommendations. No significant dehydration was observed. For the longest (53 km) race, we can extrapolate the EE as about 40 MJ. Before the race the energy intake and especially the carbohydrate intake were far under the guidelines (83 ± 17% and 46 ± 13% of the recommendations). Conclusions: EC and EE of ski mountaineering are very high. To minimize the EE to reach the top of a mountain and optimize the performance, the skier should choose a steep gradient and combine this steep gradient with a fast speed. The CHO intake should be increased during but, also before the race while the fluid intake seemed to be adequate. -- Introduction : Le ski-­‐alpinisme est un sport d'hiver qui s'est particulièrement développé durant les dernières décennies : de plus en plus de personnes pratiquent cette activité dans un cadre de loisirs et de plus en plus d'athlètes d'élite prennent part à des compétitions qu'ils préparent avec un haut degré de professionnalisme. Cependant, les connaissances scientifiques restent limitées et les athlètes ne disposent pas de recommandations précises et spécifiques. Le but principal de ce travail est donc de développer un savoir spécifique sur le ski-­‐alpinisme, ce qui devrait permettre d'établir des recommandations pour la pratique. Méthode : Le coût énergétique (CE) et le coût énergétique vertical (CEv) du ski-­‐alpinisme ont été calculés en mesurant la consommation d'oxygène à différentes pentes (7 à 33%) et vitesses (2 à 6.8 km·∙h-­‐1) sur tapis roulant avec des skis à roulettes et sur le terrain avec des skis de randonnée. Ensuite, la dépense énergétique (DE) d'une course de ski-­‐alpinisme de longue durée a été évaluée en mesurant la fréquence cardiaque et l'altitude en continu. La DE a été comparée à l'énergie consommée par les ravitaillements. Des carnets alimentaires ont permis d'estimer la consommation d'énergie (boissons et nourriture) pendant les 4 jours précédant la course. Résultats/discussion : Le CE du ski-­‐alpinisme est très élevé. Le CEv diminue entre 2 et 6 km·∙h-­‐1 et entre 7 et 33%. Pour une course de 5 h 51 ± 53 min (26 km), la DE était de 22.6 ± 2.6 MJ, alors que, pour le grand parcours de la Patrouille des Glaciers (53 km), elle serait d'environ 40 MJ. La consommation d'énergie, pendant le parcours de 26 km, couvrait 20 ± 7% de la DE et était inférieure de 14% aux recommandations, alors qu'aucune déshydratation significative n'était constatée. Les jours précédant la course, la consommation d'énergie et surtout d'hydrates de carbone était bien inférieure aux quantités recommandées (83 ± 17% et 46 ± 13% des recommandations). Conclusion : Le CE et la DE étaient très élevés. Pour minimiser la dépense lors d'une ascension, il faut combiner pente et vitesse élevées. La consommation d'hydrates de carbone devrait être massivement augmentée avant et pendant la course, alors que l'hydratation semble adéquate.