During the Mesozoic (242–66 million years ago), terrestrial regions underwent a massive shift in their size, position and connectivity. At the beginning of the era, the land masses were joined into a
N is the number of data points in the data set; M is the number of specimens from which the data were obtained. Type indicates the kind of data set: whole bone (W) or longitudinal (L). See Table S6 fo
Biome distributions for Beringia were simulated for the Late Quaternary periods by employing a global equilibrium biogeochemistry-biogeography model, BIOME4. This model was driven by the same numerica
The dataset is to describe the habitat structure and bioenergetic characteristics of woolly mammoths (Mammuthus primigenius) in North America during the last deglaciation between 15 and 10 ka. The ha