Evidence for iron‐regulated cyanobacterial predominance in oligotrophic lakes. (16th December 2013)

• Record Type: Journal Article
• Authors: Sorichetti, Ryan J.; Creed, Irena F.; Trick, Charles G.
• Is Part Of: Freshwater biology. Volume 59:Number 4(2014:Apr.)
• Page Start: 679
• Page End: 691
• Publication Date: 2013-12-16
• Subjects: Freshwater biology -- Periodicals; Biologie d'eau douce -- Périodiques; 577.605
• DOI: 10.1111/fwb.12295
• Languages: English
• ISSNs: 0046-5070

Abstract

<abstract abstract-type="main" id="fwb12295-abs-0001"> <title>Summary</title> <p> <list id="fwb12295-list-0001" list-type="order"> <list-item> <p>Cyanobacterial harmful algal blooms (cyanoHABs) are most often associated with large eutrophic lakes. In the past decade, an increase in the incidence of cyanoHABs in small oligotrophic lakes within the Laurentian Great Lakes‐St. Lawrence River Basin has been documented. We explored macro‐ and micronutrient conditions during peak phytoplankton biomass that result in high cyanobacterial densities.</p> </list-item> <list-item> <p>We hypothesised that the availability of biologically available iron (Fe) both limits the assimilation of phosphorus by competing taxa and selects for the predominance of cyanobacteria.</p> </list-item> <list-item> <p>We tested this hypothesis with a comparative study of 25 oligotrophic lakes in central Ontario, Canada. These lakes were sampled during peak phytoplankton biomass for 3 years (from 2009 to 2011) for concentrations of total phosphorus (TP), total nitrogen (TN), ammonium (<alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgg4st9d533" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math altimg="urn:x-wiley:00465070:media:fwb12295:fwb12295-math-0001" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:mi>N</mml:mi><mml:msubsup><mml:mi>H</mml:mi><mml:mn>4</mml:mn><mml:mo>+</mml:mo></mml:msubsup></mml:mrow></mml:math></alternatives>), nitrate (<alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgg4st9d4w8" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math altimg="urn:x-wiley:00465070:media:fwb12295:fwb12295-math-0002" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:mi>N</mml:mi><mml:msubsup><mml:mi>O</mml:mi><mml:mn>3</mml:mn><mml:mo>−</mml:mo></mml:msubsup></mml:mrow></mml:math></alternatives>), total dissolved Fe (TDFe) and pH for comparison with phytoplankton community biomass and composition.</p> </list-item> <list-item> <p>Correlation analyses indicated that predominance of cyanobacteria was assured at all TP levels when the availability of Fe was low. Proportionally high cyanobacterial density occurred at relatively low TP in lakes with a molar ratio of dissolved inorganic N (DIN):TP of 8:1 and a modelled ferric Fe concentration <1.0 × 10<sup>−19</sup> <sc>m</sc> at which cyanobacteria have been shown to be competitive for Fe in laboratory experiments. Regression tree analysis confirmed the minimal influence of P and N, implying that cyanobacteria thrive in low Fe environments.</p> </list-item> <list-item> <p>Our findings suggest that an increased susceptibility of oligotrophic lakes to cyanobacterial bloom formation is based on the presence of cyanobacteria that have adapted sufficiently to low Fe environments and are able to multiply rapidly when pulses of P are made available to the ecosystem. Physiologically prepared transitionary cyanobacteria do not have to compete with the eukaryotic species but rather exploit the new P and replicate faster.</p> </list-item> </list> </p> </abstract>