4.5 Article

Spatial and Temporal Variability of Nutrient Dynamics and Ecosystem Metabolism in a Hyper-eutrophic Reservoir Differ Between a Wet and Dry Year

Journal

ECOSYSTEMS
Volume 24, Issue 1, Pages 68-88

Publisher

SPRINGER
DOI: 10.1007/s10021-020-00505-8

Keywords

Environmental variability; Storm; Ecosystem metabolism; Carbon; Nitrogen; Phosphorus

Categories

Funding

  1. MU Academic Challenge program
  2. National Science Foundation Long-Term Research in Environmental Biology (LTREB) [DEB-1255159]

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Climate change plays a significant role in altering hydrologic regimes and impacting aquatic ecosystems. This study found that lakes exhibit resilience to changes in hydrologic variability, with marked differences in watershed discharge and nutrient loading producing relatively small differences in lake metrics. Discrete storm events have strong yet ephemeral effects on lake biogeochemistry and ecosystem metabolism, particularly near stream inlets where increases in limiting nutrients are observed.
Climate change alters hydrologic regimes, including their variability. Effects will be pronounced in aquatic ecosystems, where resource subsidies (e.g., nutrients, carbon) drive key ecosystem processes. However, we know little about how changing hydrologic regimes will modulate the spatiotemporal dynamics of lake biogeochemistry and ecosystem metabolism. To address this, we quantified ecosystem metabolism and nutrient dynamicsat high spatial resolution in Acton Lake, a hyper-eutrophic reservoir in the Midwestern US. We captured two consecutive growing seasons with markedly different watershed discharge and nutrient loading. Temporal variability often exceeded spatial variability in both wet and dry years. However, relative spatial variability was higher in the dry year, suggesting that internal processes are more important in structuring spatial dynamics in dry years. Strikingly, marked differences in watershed discharge and nutrient loading between years produced relatively small differences in many lake metrics, suggesting resilience to hydrologic variability. We found little difference in gross primary productivity between wet and dry years, but ecosystem respiration was higher in the wet year, shifting net ecosystem production below zero. Discrete storm events produced strong, yet ephemeral and spatially explicit effects, reflective of the balance of stream input and discharge over the dam. Increases in limiting nutrients were restricted to near stream inlets and returned to pre-storm baseline within days. Ecosystem metabolism was suppressed during storm events, likely due to biomass flushing. Understanding how changing hydrologic regimes will mediate spatiotemporal dynamics of ecosystem metrics is paramount to preserving the ecological integrity and ecosystem services of lakes under future climates.

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