Seasonal and interannual variability of the Queen Maud Gulf ecosystem derived from sediment trap measurements

• Published in: Limnology and Oceanography
• Main Authors: Dezutter, Thibaud, Lalande, Catherine, Darnis, Gérald, Fortier, Louis
• Other Authors: ArcticNet, Canada Foundation for Innovation, Parcs Canada, W. Garfield Weston Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2020
• Subjects: Arctic Archipelago; Canadian Arctic Archipelago; ice algae; Kitikmeot; Northwest passage; Queen Maud Gulf; Sea ice; Zooplankton; Copepods
• Online Access: http://dx.doi.org/10.1002/lno.11628; https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11628; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11628; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11628

Abstract Several years of monitoring in the northern Canadian Arctic Archipelago contrast with a lack of repeated measurements in Queen Maud Gulf. As sea ice cover declines and maritime traffic increases along the Northwest Passage, Queen Maud Gulf, including the protected national historic sites of the HMS Erebus and HMS Terror wrecks, may experience drastic environmental changes. As part of the Kitikmeot Marine Ecosystems Study, moored oceanographic devices including a sediment trap were deployed in Queen Maud Gulf over three consecutive annual cycles from October 2015 to August 2018 to study the functioning of this geographic bottleneck along the Northwest Passage. Seasonal and interannual variability in total particulate matter (TPM), particulate organic carbon (POC), and microalgal fluxes were investigated in relation to wind speed, snow depth, sea ice cover, water temperature, and current velocity. Zooplankton and meroplankton present in the sediment trap were enumerated to monitor their composition and seasonal development. Landfast ice breakup consistently occurred in early June, followed by sea ice breakup in July. The release of sea ice algae was initiated in March 2016, May 2017, and June 2018, whereas peaks in diatom fluxes occurred in August or September. Sustained abundance of pelagic copepods and meroplankton suggested an ecosystem sufficiently productive to support the year‐round development of the pelagic and benthic communities. Elevated autumn TPM and POC fluxes reflected wind‐induced mixing and resuspension in the absence of ice cover. Our results provide a baseline for evaluating the impact of environmental changes on the Queen Maud Gulf marine ecosystem.