These results are consistent with burrow survey data that provided indirect evidence of higher armadillo densities on larger landmasses.
Islands have made it on the map, but the landmasses they point to have not.
More appropriate environments would have been ponds and lakes of fresh water produced by the accumulation of precipitation on island-type landmasses.
Here we review and consider the geological evidence underlying this prevailing hypothesis of an enduring landmass.
The remaining maps are difficult to read because of the poor contrast between the blue of the sea and green used for landmasses.
Many believed that there had to be land beneath the south celestial pole to counter-balance the landmasses of the northern hemisphere.
Post-hoc contrasts between landmass categories served to identify significant differences.
Sapling recruitment on small and medium islands was only 19% and 32%, respectively, of that observed on the large landmasses that served for reference.
