Influence of hydrological connectivity on winter limnology in 1 floodplain lakes 2 of the Saskatchewan River Delta, SK

dc.contributor.authorMacKinnon, Brett D.
dc.contributor.authorSagin, Jay
dc.contributor.authorBaulch, Helen M.
dc.contributor.authorLindenschmidt, Karl-Erich
dc.contributor.authorJardine, Timothy D.
dc.date.accessioned2016-02-17T08:17:24Z
dc.date.available2016-02-17T08:17:24Z
dc.date.issued2015
dc.description.abstractGlobally, hydrological connectivity between rivers and their floodplains has been reduced by river flow management and land transformation. The Saskatchewan River Delta is North America’s largest inland delta and a hub for fish and fur production. To determine the influence of connectivity on limnology within this northern floodplain, water chemistry and stable isotopes (δ18O and δ236 H) were analyzed during the winter of 2014 in shallow lakes along a hydrological gradient. A total of five lake connectivity categories were determined by optical remote-sensing images of surface water coverage area from years of varying flood intensities. Accuracy of categories were verified by degree of 18O and 239 H enrichment within lakes. Both isotopes showed marked successional enrichment between connectivity categories with more isolated lakes exhibiting greater enrichment. Water chemistry in lakes with greater connectivity to the main channel were characterized by higher pH, dissolved oxygen, nitrates and sulfates, and lower total nitrogen, total phosphorus, and ammonium, compared to more isolated lakes. These findings illustrate how connectivity influences water chemistry in northern floodplain lakes and how it might determine the suitability of these lakes as winter refuge for fishes. Additionally, our study provides supporting evidence for the effective use of optical remote sensing imagery, an inexpensive and accessible source of data for researchers, when determining connectivity characteristics of large northern floodplain systems. Additionally, this study provides further evidence that the inundation of floodplain lakes by river water during peak discharge has an impact on the conditions within the lakes long into the winter ice-cover season. Understanding the year-round influence of river-floodplain connection is imperative for assessing potential impacts of climate change and future water regulation on such ecosystems
dc.identifier.citationMacKinnon, B. D., Sagin, J., Baulch, H. M., Lindenschmidt, K. E., & Jardine, T. D. (2015). Influence of hydrological connectivity on winter limnology in floodplain lakes of the Saskatchewan River Delta, Saskatchewan. Canadian Journal of Fisheries and Aquatic Sciences, 73(1), 140-152. https://doi.org/10.1139/cjfas-2015-0210
dc.identifier.doihttps://doi.org/10.1139/CJFAS-2015-0210
dc.identifier.urihttp://nur.nu.edu.kz/handle/123456789/1241
dc.language.isoen
dc.publisherAcademia
dc.rightsAttribution 3.0 United States
dc.sourceCanadian Journal of Fisheries and Aquatic Sciences, 73(1), pages 140-152
dc.subjectfloodplains
dc.subjectconnectivity
dc.subjectisotope
dc.subjectremote sensing
dc.subjectnutrients
dc.subjectwinter
dc.subjectdams
dc.titleInfluence of hydrological connectivity on winter limnology in 1 floodplain lakes 2 of the Saskatchewan River Delta, SK
dc.typeArticle

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