Changes in mixing depth reduce phytoplankton biomass in an Arctic lake: Results from a whole-lake experiment

• Published in: Arctic, Antarctic, and Alpine Research
• Main Authors: Robert M. Northington, Jasmine E. Saros, Benjamin T. Burpee, Joan McCue
• Format: Article in Journal/Newspaper
• Language: English
• Published: Taylor & Francis Group 2019
• Subjects: phytoplankton biomass; arctic lakes; climate change; greenland; whole-lake manipulation; Environmental sciences; GE1-350; Ecology; QH540-549.5; Arctic; Greenland; Arctic Lake; Four Lakes; Antarctic and Alpine Research; Climate change; Phytoplankton
• Online Access: https://doi.org/10.1080/15230430.2019.1692412; https://doaj.org/article/b4fe2e64141b456aa8ed5201d1aae48d

Research has revealed contradictory responses of primary producers in Arctic lakes to increasing temperatures, making it unclear how future warming and climate change will alter lake productivity. We conducted a whole-lake manipulation to examine the effect of altered thermal structure on phytoplankton biomass in a lake in Greenland, one of the most rapidly warming regions of the world. Deepened lake mixing (from 4 to 8 m) in the experimental lake led to significant declines in phytoplankton biomass in the sediment traps despite warmer surface waters, indicating that changes in mixing depth may negate a positive, direct effect of warming on primary producer biomass. Light limitation (induced by deeper mixing) of phytoplankton played a greater role than temperature in structuring these Arctic lake phytoplankton communities. To put the manipulation in context, we surveyed twenty-four lakes across western Greenland to determine the strongest regional predictors of phytoplankton density. Across the landscape, lake chemistry and light attenuation in the epilimnion were the most important predictors of algal assemblages in the survey lakes. Though temperature can directly influence lake ecosystems, multiple factors will affect mixing depths of Arctic lakes, potentially leading to variable effects of warming on phytoplankton biomass and community structure.