The Rupicaprini originated during the Miocene in Asia and dispersed during the late Miocene-early Pliocene, the Villafranchian, and the middle Pleistocene. Rupicapra and Oreamnos spread respectively to Europe and to North America in the middle Pleistocene. The Villafranchian Procamptoceras may be considered to be the closest known form to Rupicapra's ancestor. Rupicapra evolved during the middle and late Pleistocene in west Eurasia. At the beginning of the Würm glaciation the two closely related species R. pyrenaica and R. rupicapra were in existence. The former was already geographically split into Spanish-Pyrenean and central-southern Apennines groups, while the latter species ranged from the Caucasus to the Alpine Arch. R. pyrenaica shows more conservative features and possibly differentiated directly in western Europe from older representatives of the genus that migrated to western Europe in the middle Pleistocene. The cold-adapted Alpine chamois may have differentiated in eastern Europe and then migrated west-ward because of the advent of dry climates in the east Mediterranean and Pontic regions. The Alpine chamois failed to spread to the warmer southernmost regions of Europe that became a refugium area for R. pyrenaica. This dispersal hypothesis explains the morphologic, biometric, electrophoretic, and behavioral differences among modern chamois populations.
The activity of radiotagged adult crested porcupines Hystrix cristata L., 1758, was studied in a rural hilly area of Central Italy, from July 1990 to June 1991. Three males and one female were monitored every 15 minutes for 18–24 hours/individual/week, and their activity patterns were correlated to ambient temperature, precipitation and lunar phases. Three individuals, out of the four monitored, showed a fall of activity in the beginning of the cold season, but generally porcupines appeared adapted to a wide spectrum of temperatures. The mean duration of nocturnal and crepuscular activity was 9 h 22'±42', showing little variation throughout the year. In the cold months, i.e. when nights are relatively longer, porcupines usually left their burrows after sunset and came back some hours before sunrise. In the warm season they left their burrows at sunset, or shortly before, and returned at sunrise, or shortly after. Overall diurnal activity was scarce (2 h 11' ± 1 h 30'), but in spring it increased to over 40% of the diel activity (3 h 22' ± 3 h). Moonlight avoidance was slight. Precipitation did not seem to influence the activity of porcupines.
S., 1989: Foraging behaviour of adult female Apennine chamois in relation to seasonal variation in food supply. Acta theriol., We tested the prediction that qualitative and quantitative seasonal variations of food resources influenced the foraging behaviour and efficiency of Apennine chamois, Rupicapra pyrenaica omata (Neuman, 1899). In summer, when the abundance and diversity of food resources were greater, we found a greater rate of food intake and a reduced search for food, as well as lower aggressiveness, than in the autumn. Furthermore in summer the median group size of grazing chamois was greater than in the autumn, in accordance with the availability of rich, but concentrated, food resources in the former season. No seasonal difference intime devoted to foraging was found. Apparently, the Apennine chamois maximize food intake during summer to compensate for later shortages in the colder season.
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