Abstract

Phosphorus (P) is generally considered to be the main limiting nutrient to freshwater phytoplankton productivity. However, recent research is drawing attention to the importance of nitrogen (N) in freshwater eutrophication and N often constrains growth of cyanobacteria in small lakes. In this study we determined phytoplankton nutrient limitation in a large lake, Lake Erie during two growing seasons. During 2010 and 2011, nutrient enrichment bioassays (+P, +N and, +P and N) were conducted monthly from June through September with water collected in Maumee Bay (site MB18) and in the center of the western basin (site WBC). Nutrient concentrations were monitored every other week. At MB18, total P concentration was often >3 mmol/L and nitrate concentration decreased from >250 mmol/L in early summer to mmol/L in late summer. Nitrogen and P levels were about five-fold less at WBC. Bioassays indicated that phytoplankton nutrient limitation varied in summer, spatially, and even among phytoplankton groups. For site MB18, +P increased chlorophyll concentration in one of the eight bioassays, indicating that P did not typically limit production. For site WBC, +P increased chlorophyll concentration in six of the eight bioassays. As a result of very low ambient nitrate concentration (mmol/L) in late summer, +N (without P) increased chlorophyll concentration, suggesting symptoms of N-limitation. The N-fixing cyanobacterium Anabaena became dominant following N-limitation. This study highlights the need to reduce P loading to restore water quality. Furthermore, due to low nitrate concentration, the severity of the cyanobacterial blooms could be worse if not for N-limitation in western Lake Erie.

Highlights

  • Eutrophication of freshwater has become a global problem due to humans accelerating nutrient loading into lakes and rivers [1]

  • Nitrate concentration at site MB18 declined throughout the summer from high values (>250 mol/L) in early summer to values below 1 mol/L

  • In 2011 at MB18, nitrate concentration increased in late summer from concentrations below 1 mol/L to concentrations similar to early summer

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Summary

Introduction

Eutrophication of freshwater has become a global problem due to humans accelerating nutrient loading into lakes and rivers [1]. Often called blooms, are likely symptom of eutrophication due to high nutrient concentrations [2]. High phosphorus (P) concentration is considered a main factor responsible for promoting eutrophication and cyanobacterial blooms [5]. Lakes with high P concentration are likely to have high biomasses of cyanobacteria and a phytoplankton community that consists largely of cyanobacteria [6]. This knowledge led to successful P abatement programs that reduced the amount cyanobacteria in many lakes [7,8]. In lakes with sufficient P concentrations to meet phytoplankton growth demand, N is the likely nutrient to limit phytoplankton growth [12,13]

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