En mai 2019, le Canada a présenté sa soumission concernant son plateau continental étendu arctique à la Commission des limites du plateau continental. La délinéation des plateaux continentaux étendus, conformément à la Convention des Nations Unies sur le droit de la mer, résulte d’interprétations dans lesquelles s’entrelacent arguments scientifiques et juridiques à l’égard d’une situation géophysique singulière. Cet article examine la manière dont le Canada a composé avec la triple interprétation juridique, scientifique et factuelle à travers une étude articulée autour de la notion de “prolongement naturel.” Sont mis en relief les défis interprétatifs, mais aussi les opportunités que le Canada a saisies en participant au dégagement de consensus scientifiques et juridiques au soutien de la délinéation qu’il propose.

In the first millennium AD, peoples across the North American Arctic began to use and exchange metal. A group known as the Late Dorset (AD 500–1300) were the first to widely exchange metal in the Eastern Arctic. However, due to differential taphonomic processes and past excavation methods, metal objects in existing collections are rare although geographically widespread. This has led to metal being seen as a broadly exchanged but uncommon raw material among Late Dorset. This article expands the known scale of Late Dorset metal use by analyzing the blade slot thicknesses of bone and ivory objects from sites across the Eastern Arctic and comparing them to the thicknesses of associated lithic and metal endblades. These results demonstrate that Late Dorset used metal at least as frequently as stone for some activities. Given the few and geographically discrete sources, metal would have been exchanged over thousands of kilometers of fragmented Arctic landscape. The lack of similar evidence in earlier periods indicates intergroup interaction increases significantly with the Late Dorset. It is through these same vectors that knowledge and information would have flowed. Metal, consequently, represents the best material for understanding the maximum extent and intensity of their interaction networks.

One of the most persistent debates in the archaeology of the North American Arctic relates to thirteenth-century AD population distributions and movements. Around this time, the final culture of the long-lived Paleo-Inuit tradition, known as Late Dorset, was replaced by Thule Inuit, who migrated from Alaska to the Eastern Arctic. Due to the almost complete lack of evidence for direct interaction between Dorset and Thule, there are currently two contrasting models for this transitional period. The first proposes a temporal hiatus between Late Dorset and Thule during which the Eastern Arctic was unoccupied. The second proposes that Late Dorset persisted to at least the late thirteenth century and still occupied some regions of the Eastern Arctic when Thule arrived. Resolution of this question depends largely on radiocarbon dates, particularly for the poorly understood Late Dorset period. This article presents 56 new AMS radiocarbon dates from three Late Dorset sites in the Iqaluktuuq region of southeastern Victoria Island in the Central Arctic. They resolve a significant part of the debate by confirming that Dorset settlement continued in this region later than AD 1300, thus overlapping with Thule settlement in adjacent regions for decades, and perhaps as much as a century.

In 2008, four decades since Meldgaard's work at Alarniq—the type site for Dorset culture—Savelle and Dyke returned to resurvey the site. Archaeological investigations continued in 2015 and 2017 as part of the Foxe Basin Archaeological Project, when Howse conducted further surveys, excavated six semi-subterranean dwellings and two associated middens, and tested five additional features. The new site map and radiocarbon sequence have significantly changed our understanding of site use and beach-level chronology at Alarniq. The number of dwellings varies across the beach ridges, suggesting populations fluctuated throughout the site's use (2,700–800 cal BP). However, the new radiocarbon analyses also indicate that dwellings between 14.5 and 21.5 m above sea level are the same general age and that paleodemography at Alarniq is less straightforward than suggested by the number of features per beach ridge. It appears that ideal house construction location is a stronger indicator of the placement of winter houses at the site than proximity to the shoreline. We suggest this is largely related to site seasonality. These new data have significant implications for our understanding of current Dorset artifact typologies that have largely been developed using the material Meldgaard recovered at the site.