4.2 Article

Spring distribution of ringed seals (Pusa hispida) in Eclipse Sound and Milne Inlet, Nunavut: implications for potential ice-breaking activities

Journal

ARCTIC SCIENCE
Volume 5, Issue 1, Pages 54-61

Publisher

CANADIAN SCIENCE PUBLISHING
DOI: 10.1139/as-2018-0020

Keywords

aerial survey; anthropogenic stressor; conservation; hotspot; infrared imagery

Funding

  1. Polar Continental Shelf Project (PCSP)
  2. Environment and Climate Change Canada (ECCC)
  3. World Wildlife Fund Canada (WWF)
  4. Fisheries and Oceans Canada (DFO)
  5. ArcticNet
  6. Mittimatalik Hunters and Trappers Organization of Pond Inlet, NU

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Resource development in Arctic waters is proceeding rapidly leading to increased interactions with Arctic wildlife. As sea ice extent decreases, the demand for shipping and ice-breaking operations will expand into winter and spring with greater impact on ice-dependent pinnipeds. However, knowledge of the distribution of these species, such as ringed seals (Pusa hispida (Schreber, 1775)), during spring within areas of resource development is lacking. Baffinland Iron Mines Corporation's Mary River iron ore port in southern Milne Inlet, Nunavut opened in 2015 with proposed ice-breaking activities in spring - an important period in ringed seal seasonal life-history. We conducted infrared and photographic aerial surveys in June 2016 and 2017 to overlay the proposed ice-breaking route with ringed seal hotspots (i.e., areas of higher density). We identified four areas of overlap where proposed ice-breaking would traverse through ringed seal hotspots: eastern and western Eclipse Sound (a ringed seal pupping ground identified by local knowledge), the middle of Milne Inlet, and southern Milne Inlet. We identified potential negative implications of spring ice-breaking operations on ringed seals such as displacement, separation of mothers and pups, destruction of resting and birth lairs, and vessel - seal collisions. Results are relevant to policy decision-makers who can develop mitigation strategies in the rapidly melting and developing Arctic.

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