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High biodegradability of riverine dissolved organic carbon in late winter in Hudson Bay, Canada

Bibliographic Data

ID19569163
AuthorsZ V Kazmiruk, Zakhar Kazmiruk (0000-0001-8684-7672, University of Manitoba), David Capelle (0000-0002-6802-5728, University of Manitoba), D W Capelle, Christina Michelle Kamula (University of Manitoba), Søren Rysgaard (0000-0003-1726-2958, Aarhus University), Tim Papakyriakou (0000-0002-2019-9104, University of Manitoba), Zou Zou A Kuzyk (0000-0002-6891-6125, University of Manitoba), Z A Kuzyk
Year2021
Volume9
Issue1
Publication date2021-05-26
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2020.00123
OpenAlexW3162275194
LanguageEN
Citations received1
References cited60

Hudson Bay, at the southern margin of the Arctic Ocean, receives nearly one-third of Canada’s river discharge and approximately 5.5 Tg of riverine dissolved organic carbon (DOC) annually. Riverine DOC fluxes to Hudson Bay are expected to increase with climate change, but how this increase will influence the biogeochemistry of the coastal waters is largely unknown. In particular, the fate of riverine DOC that enters Hudson Bay during the dark, frozen winter period (roughly January to April) is poorly known despite high discharge from the large, regulated rivers of Hudson and James Bays at that time. Few studies have assessed the degradability of riverine DOC transported in winter anywhere across the Arctic, leaving unanswered questions regarding the impact of riverine DOC on the Arctic carbon budget, CO2 fluxes, and local food webs. Here, we assessed the biodegradability of DOC in riverine and coastal waters of southern Hudson Bay in late winter using 45-day incubation experiments. We found 24%–60% of the DOC in the rivers and on average 21% of the DOC in the immediate coastal waters to be biodegradable. Differences in biodegradability appeared to depend on properties of the rivers/watersheds and physical and biochemical processes in the aquatic environments. DOC biodegradability correlated strongly with DOC concentration, which was higher during winter than summer in all studied rivers and higher in the Nelson and Hayes Rivers, draining the Hudson Bay Lowlands than in most previously studied large rivers of the Arctic watershed. The Nelson River, regulated for hydropower production, had the highest winter DOC concentrations and most degradable DOC. The high biodegradability of Hudson Bay riverine DOC in late winter and high concentrations and fluxes of riverine DOC at that time imply strong leverage for future increases in DOC fluxes to impact the carbon cycle of these coastal waters

Arctic · Bay · Biogeochemistry · Discharge · Dissolved organic carbon · Drainage basin · Geography · Total organic carbon · Arctic and Antarctic ice dynamics · Climate change and permafrost · Environmental Science · Marine and coastal ecosystems · Ecology · Geology · Oceanography

  • Nutrient inputs from subarctic rivers into Hudson Bay

    Open Access•Janghan Lee, Andrew Tefs et al.•Elementa Science of the…•2023

Unique citing works1
Citations per year0.33
Citation span2023 - 2023 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae