Biogeographers suggest two refugial
areas where Caribou and other large mammals might have
survived when the island was covered miles deep in glacial
ice, ca 10KYA. The Grand Banks, to the southeast
of the island, are known to have been above water when sea
levels were lower due to sequestering of water in ice.
Caribou might have been forced south, and re-entered the
island from the southeast.
Alternatively, re-opening of the valley
of the St Lawrence River would have provided a
means of expansion from central North America into Quebec
and Labrador. Caribou could then have re-entered the
island from the northwest, across the narrow Strait of
Belle Isle.
The genetic analysis shows that insular
Caribou are most closely related to current populations in
Quebec and Labrador, and that the rare Clade A
(Figures 4 & 5) is found both on the island and in
Quebec. This suggests that there is ongoing gene flow
between the island and mainland, across the Strait of
Belle Isle.
Further evidence against colonization
from the southeast is that Caribou populations on the
Avalon Peninsula are genetically invariant, which
suggests a bottleneck and (or) genetic drift
affect after small numbers of animals crossed the Isthmus
of the Avalon. The presence of unbrowsed lichen (the
favorite food of caribou) on cliffs on either side of the
narrows of the Isthmus suggests little or no movement for
at least several hundred years.