2005
DOI: 10.7202/010809ar
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A review of Palaeoeskimo dwelling structures in Newfoundland and Labrador

Abstract: Cet article passe en revue et résume l'information concernant les structures d'habitations paléoesquimaudes de la province de Terre-Neuve et du Labrador dans le but de produire à la fois une base de données et un instrument de recherche. Des tendances sont identifiées; certaines liées à la mobilité résidentielle.This paper reviews and summarizes information about Palaeoeskimo dwelling structures in the Province of Newfoundland and Labrador with the aim of producing a basic resource and research tool. Patterns … Show more

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Cited by 18 publications
(2 citation statements)
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“…Based on current data, the Late Dorset occupation of northwest Greenland almost certainly lasted until at least the end of the thirteenth century (Appelt and Gulløv 1999, 2009; Darwent and Foin 2010; Darwent et al 2007), potentially overlapping with the early Ruin Island phase of Thule occupations in that region (McCullough 1989). The central High Arctic (LeMoine et al 2003), Somerset Island (Damkjar 2000), western Victoria Island (Savelle et al 2012), Foxe Basin (Savelle and Dyke 2014), and northern Labrador (Desrosiers 2017; Renouf 2003) have also produced isolated dates that may point to Late Dorset populations persisting into the thirteenth century or later. The situation in Nunavik (northern Quebec) is currently unresolved, but it is also a good candidate for Late Dorset occupations with the potential for overlap with Thule (Labrèche 2015; Pinard and Gendron 2009; Plumet 1979, 1989), particularly given a new genetic analysis that may indicate some gene flow between Paleo-Inuit and Inuit in the region (Zhou et al 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Based on current data, the Late Dorset occupation of northwest Greenland almost certainly lasted until at least the end of the thirteenth century (Appelt and Gulløv 1999, 2009; Darwent and Foin 2010; Darwent et al 2007), potentially overlapping with the early Ruin Island phase of Thule occupations in that region (McCullough 1989). The central High Arctic (LeMoine et al 2003), Somerset Island (Damkjar 2000), western Victoria Island (Savelle et al 2012), Foxe Basin (Savelle and Dyke 2014), and northern Labrador (Desrosiers 2017; Renouf 2003) have also produced isolated dates that may point to Late Dorset populations persisting into the thirteenth century or later. The situation in Nunavik (northern Quebec) is currently unresolved, but it is also a good candidate for Late Dorset occupations with the potential for overlap with Thule (Labrèche 2015; Pinard and Gendron 2009; Plumet 1979, 1989), particularly given a new genetic analysis that may indicate some gene flow between Paleo-Inuit and Inuit in the region (Zhou et al 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Both groups then inhabited the exact same cold subarctic environment. The difference is that the Dorset had a specialized and seasonal harp seal subsistence economy, and were semi-sedentary as a result (Renouf, 2003), while the ancestral Beothuk were mobile generalists (Holly, 2005;Schwarz, 1994). Indeed, sedentism in itself-especially the expectation of it-is a good predictor of investment in domestic architecture (see Binford, 1990: 123-124;Kelly, 1983;Kelly et al, 2005;Kent, 1992;McGuire and Schiffer, 1983), and probably best accounts for the development of Beothuk housepits in the post-contact era (Reader, 1998: 62-63).…”
Section: Hunkering Down: Housesmentioning
confidence: 99%