Marked blue discoloration of late winter ice and water due to autumn blooms of cyanobacteria

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dc.contributor.authorHaig, Heather A.
dc.contributor.authorChegoonian, Amir M.
dc.contributor.authorDavies, John-Mark
dc.contributor.authorBateson, Deirdre
dc.contributor.authorLeavitt, Peter R.
dc.date.accessioned2023-04-26T17:46:43Z
dc.date.available2023-04-26T17:46:43Z
dc.date.issued2021-11-17
dc.description© 2021 The Author(s). Published with license by Taylor and Francis Group, LLC This is an Open Access article distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives License ((http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is properly cited, and is not altered, transformed, or built upon in any way.en_US
dc.description.abstractContinued eutrophication of inland waters by nutrient pollution can combine with unprecedented atmospheric and lake warming to create emergent environmental surprises. Here we report the first known occurrence of marked blue discoloration of ice and water in highly eutrophic prairie lakes during late winter 2021. Intense blue staining was reported first to governmental agencies by ice fishers in early March 2021, then communicated widely through social media, resulting in First Nations and public concern over potential septic field release, toxic spills, urban pollution, and agricultural mismanagement. Analysis of water from stained and reference sites using ultraviolet (UV)–visible spectrophotometry and high-performance liquid chromatography demonstrated that the blue color arose from high concentrations (∼14 mg/L) of the cyanobacterial pigment C-phycocyanin that was released after an unexpected bloom of Aphanizomenon flos-aquae in late October 2020 was frozen into littoral ice. Remote sensing using the Sentinel 3 A/B OLCI and Sentinel 2 A/B MSI satellite platforms suggested that blue staining encompassed 0.68 ± 0.24 km2 (4.25 ± 1.5% of lake surface area), persisted over 4 weeks, and was located within 50 m of the lakeshore in regions where fall blooms of cyanobacteria had been particularly dense. Although toxin levels were low (∼0.2 μg microcystin/L), high concentrations of C-phycocyanin raised public concern over eutrophication, pollution, and climate change, and resulted in rapid governmental and academic response. Given that climate change and nutrient pollution are increasing the magnitude and duration of cyanobacterial blooms, blue staining of lake ice may become widespread in eutrophic lakes subject to ice cover.en_US
dc.description.authorstatusFacultyen_US
dc.description.peerreviewyesen_US
dc.description.sponsorshipThis work was supported by the NSERC Canada Discovery Grants program, Canada Research Chairs, Canada Foundation for Innovation, the Province of Saskatchewan, and the University of Regina.en_US
dc.identifier.citationHaig, H.A., A. M. Chegoonian, J.-M. Davies, D. Bateson, and P.R. Leavitt. 2022. Marked blue discolouration of late winter ice and water due to exceptional autumnal blooms of cyanobacteria. Lake Reserv. Manag. 38: 1-15. doi.org/10.1080/10402381.2021.1992544en_US
dc.identifier.doidoi.org/10.1080/10402381.2021.1992544
dc.identifier.urihttps://hdl.handle.net/10294/15878
dc.language.isoenen_US
dc.publisherTaylor and Francis Groupen_US
dc.rightsAttribution-NonCommercial-NoDerivs 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectAphanizomenonen_US
dc.subjectC-phycocyaninen_US
dc.subjectcyanobacteriaen_US
dc.subjectfall bloomen_US
dc.subjectHPLCen_US
dc.subjectremote sensingen_US
dc.subjectSentinel 2 MSIen_US
dc.subjectSentinel 3 OLCIen_US
dc.titleMarked blue discoloration of late winter ice and water due to autumn blooms of cyanobacteriaen_US
dc.typeArticleen_US
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