CI[)l1:721 - Memorial University of Newfoundland DAI
CI[)l1:721 - Memorial University of Newfoundland DAI
CI[)l1:721 - Memorial University of Newfoundland DAI
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36<br />
further Meadowood sites with datable charcoal. In view <strong>of</strong> the dates that are<br />
available, it appears that Meadowood in Maine and the Maritimes emerges laler<br />
than it does to the south.<br />
Uke the Middlesex Phase, Meadowood Phase manifestations should<br />
probably be viewed as the results <strong>of</strong> diffusion, although the possibility <strong>of</strong><br />
migration should not be ruled out until more info;. :ation becomes available.<br />
The diffusion hypothesis is supported by the fact that Meadowood peoples were<br />
known for the conduct <strong>of</strong> long-distance trade (Ritchie 1980: 196; Snow 1980:<br />
267), which may account for the appearance <strong>of</strong> Meadowood traits in the Maine<br />
Maritimes region.<br />
Southern New England<br />
The hiatus for the Maine-Maritimes region's Terminal Archaic Period is not<br />
seen to the south. Evidence exists for continuous occupation to the south<br />
through the transition between the Archaic and Ceramic Periods. A brief<br />
description <strong>of</strong> the southern chronological sequence will be provided for<br />
comparison.<br />
In southern New England, there is continuous cultural development<br />
pertaining to the Susquehanna Tradition throughout the Terminal Archaic. This<br />
is defined in a series <strong>of</strong> phases, commencing with the Atlantic Phase. The<br />
Atlantic Phase dates from 4140±100 B.P. in southeastern New England<br />
(Dincauze 1972: 56). This phase terminates c. 3600 B.P., with the beginning <strong>of</strong>