Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins

Abstract This paper presents the first detailed record of Paleoeskimo occupation history of Foxe Basin, Nunavut, Arctic Canada, the traditional Paleoeskimo “core area.” Rather than continuous, stable occupations from approximately 4000–1000 B.P. traditionally assumed for the core area, the region ha...

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Published in:American Antiquity
Main Authors: Savelle, James M., Dyke, Arthur S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2014
Subjects:
Online Access:http://dx.doi.org/10.7183/0002-7316.79.2.249
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0002731600002547
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spelling crcambridgeupr:10.7183/0002-7316.79.2.249 2024-06-23T07:49:34+00:00 Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins Savelle, James M. Dyke, Arthur S. 2014 http://dx.doi.org/10.7183/0002-7316.79.2.249 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0002731600002547 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms American Antiquity volume 79, issue 2, page 249-276 ISSN 0002-7316 2325-5064 journal-article 2014 crcambridgeupr https://doi.org/10.7183/0002-7316.79.2.249 2024-05-29T08:09:54Z Abstract This paper presents the first detailed record of Paleoeskimo occupation history of Foxe Basin, Nunavut, Arctic Canada, the traditional Paleoeskimo “core area.” Rather than continuous, stable occupations from approximately 4000–1000 B.P. traditionally assumed for the core area, the region has undergone a series of demographic oscillations, including several instances of abandonment of key areas, most notably Igloolik. The Foxe Basin demographic trends are reminiscent of Paleoeskimo “boom and bust” cycles recognized elsewhere, but show no consistent chronological pattern either within Foxe Basin or inter-regionally. Equally important, our results bear on the critical question of the Pre-Dorset to Dorset transition. Rather than having been a gradual in situ process centered within the core area, the demographic patterns, including the abrupt and widespread appearance of semi-subterranean dwellings during earliest Dorset, are consistent with newly arrived populations from outside of Foxe Basin. While there is no obvious “parent” culture to Dorset within the Eastern Arctic, it is suggested that a Western Arctic origin, specifically Norton Culture, invoking to some extent Jorgen Meldgaard’s “smell of the forest”, may have played a significant role. Article in Journal/Newspaper Arctic Foxe Basin Igloolik Nunavut Cambridge University Press Arctic Canada Foxe Basin ENVELOPE(-77.918,-77.918,65.931,65.931) Igloolik ENVELOPE(-81.800,-81.800,69.378,69.378) Nunavut American Antiquity 79 2 249 276
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract This paper presents the first detailed record of Paleoeskimo occupation history of Foxe Basin, Nunavut, Arctic Canada, the traditional Paleoeskimo “core area.” Rather than continuous, stable occupations from approximately 4000–1000 B.P. traditionally assumed for the core area, the region has undergone a series of demographic oscillations, including several instances of abandonment of key areas, most notably Igloolik. The Foxe Basin demographic trends are reminiscent of Paleoeskimo “boom and bust” cycles recognized elsewhere, but show no consistent chronological pattern either within Foxe Basin or inter-regionally. Equally important, our results bear on the critical question of the Pre-Dorset to Dorset transition. Rather than having been a gradual in situ process centered within the core area, the demographic patterns, including the abrupt and widespread appearance of semi-subterranean dwellings during earliest Dorset, are consistent with newly arrived populations from outside of Foxe Basin. While there is no obvious “parent” culture to Dorset within the Eastern Arctic, it is suggested that a Western Arctic origin, specifically Norton Culture, invoking to some extent Jorgen Meldgaard’s “smell of the forest”, may have played a significant role.
format Article in Journal/Newspaper
author Savelle, James M.
Dyke, Arthur S.
spellingShingle Savelle, James M.
Dyke, Arthur S.
Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
author_facet Savelle, James M.
Dyke, Arthur S.
author_sort Savelle, James M.
title Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
title_short Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
title_full Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
title_fullStr Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
title_full_unstemmed Paleoeskimo Occupation History of Foxe Basin, Arctic Canada: Implications for the Core Area Model and Dorset Origins
title_sort paleoeskimo occupation history of foxe basin, arctic canada: implications for the core area model and dorset origins
publisher Cambridge University Press (CUP)
publishDate 2014
url http://dx.doi.org/10.7183/0002-7316.79.2.249
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0002731600002547
long_lat ENVELOPE(-77.918,-77.918,65.931,65.931)
ENVELOPE(-81.800,-81.800,69.378,69.378)
geographic Arctic
Canada
Foxe Basin
Igloolik
Nunavut
geographic_facet Arctic
Canada
Foxe Basin
Igloolik
Nunavut
genre Arctic
Foxe Basin
Igloolik
Nunavut
genre_facet Arctic
Foxe Basin
Igloolik
Nunavut
op_source American Antiquity
volume 79, issue 2, page 249-276
ISSN 0002-7316 2325-5064
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.7183/0002-7316.79.2.249
container_title American Antiquity
container_volume 79
container_issue 2
container_start_page 249
op_container_end_page 276
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