Southern New Zealand is a cool-temperate insular region, first coloniz
ed about 800 BP by hunter-gatherers, Archaeological data, particularly
from the site at Shag River Mouth, show that small villages, establis
hed early in the settlement sequence, were occupied only briefly and t
hat by about 400 BP village habitation had ceased. Ethnographic observ
ations and some archaeological evidence show that villages were re-est
ablished late in the sequence, by about 200 BP. It is argued that thes
e phases of sedentary settlement largely reflect different responses t
o relative scarcity of resources. In the early phase, transient villag
es were established close to rich resource clumps, notably of seals an
d moas, and these were depleted serially until that settlement mode wa
s no longer practical. In the later phase, villages were sustained by
long-distance movement of dispersed resources, in a system facilitated
by new socio-political conditions.