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The State of Circumpolar Walrus Populations

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different Baffin Bay estimates, they should be treated with caution until there is better<br />

geographical coverage and improved understanding <strong>of</strong> the current summer distribution and<br />

movements <strong>of</strong> walruses in the CHA-NWG population.<br />

<strong>The</strong> biggest change in distribution <strong>of</strong> this population is in the Avanersuaq (Quaunaaq) area <strong>of</strong><br />

west Greenland, where walruses were once abundant in summer but now absent (Vibe 1950;<br />

Born et al. 1995). Freuchen (1921) and Vibe (1950) described substantial migrations <strong>of</strong> walruses<br />

northward in the spring along the west coast <strong>of</strong> Greenland and southward in the fall along the<br />

east coast <strong>of</strong> Baffin Island, but this no longer occurs (Born et al. 1995). <strong>The</strong> Baffin Bay stock is<br />

listed as Critically Endangered on the Greenland Red List (Boertmann 2007) but the recent<br />

population estimates and modelling <strong>of</strong> population dynamics (Witting and Born 2014) suggest the<br />

stock may be in better condition than this designation suggests.<br />

Canadian Central Arctic - West Greenland Population (CCA-WG)<br />

<strong>The</strong> Canadian Central Arctic - West Greenland (CCA-WG) population occupies a large area <strong>of</strong> the<br />

eastern Canadian Arctic and extends across Davis Strait to west Central Greenland (Figure 3)<br />

(Richard and Campbell 1988; Born et al. 1995; Stewart 2002, 2008; Shafer et al. 2014). It has<br />

been separated from the CHA-NWG population on the basis <strong>of</strong> apparent geographical<br />

distributions (Born et al. 1995) and genetic differences (Buchanan et al. 1998; de March et al.<br />

2002; Andersen et al. 2014; Shafer et al. 2014); and from the Canadian Low Arctic (CLA)<br />

population on the basis <strong>of</strong> geographical distributions, changes in abundance (Born et al. 1995),<br />

and lead isotope ratios (Outridge and Stewart 1999; Outridge et al. 2003). <strong>Walrus</strong>es in West<br />

Greenland and at southeastern Baffin Island, Canada, could not be distinguished from one<br />

another genetically (Andersen et al. 2014).<br />

Four management stocks have been tentatively identified within the CCA-WG population on the<br />

basis <strong>of</strong> satellite-linked radio tagging studies, observed seasonal distribution, and lead isotope<br />

ratios in the teeth (Stewart 2008; NAMMCO 2011; see also Outridge et al. 2003). <strong>The</strong>se stocks<br />

are located in Foxe Basin (Canada), north and west Hudson Bay (Canada), south and east Baffin<br />

(Canada) and West Greenland, and southern Hudson Strait-Ungava Bay-Labrador (Canada) (see<br />

D.B. Stewart et al. 2014a). Inuit elders recognize two groups <strong>of</strong> walruses in Foxe Basin on the<br />

basis <strong>of</strong> differences in the animals’ size, colour, flavour <strong>of</strong> meat and blubber, and distribution<br />

(DFO 2002). <strong>The</strong>re is exchange <strong>of</strong> animals between south and east Baffin Island and West<br />

Greenland across Davis Strait (Figure 3). Most <strong>of</strong> these stocks are likely reduced from their<br />

historical levels but no trend can be established and survey coverage is incomplete. Inuit have<br />

observed changes in walrus distribution and seasonal availability.

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