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Published on: July 24, 2016
Realizing ecosystem services: wetland hydrologic function along a gradient of ecosystem condition
Daniel L McLaughlin1, Matthew J Cohen
1School of Forest Resources and Conservation, University of Florida, 319 Newins-Ziegler Hall, P.O. Box 110410, Gainesville, Florida 32611-0410, USA. mclaugd@ufl.edu
Wetland ecological condition does not always predict hydrologic function. Evapotranspiration (ET) varied with land use, benefiting intensive landscapes, while groundwater exchange provided aquifer benefits regardless of wetland condition.
Area of Science:
- Environmental Science
- Ecology
- Hydrology
Background:
- Wetlands provide critical ecosystem services, including habitat, pollutant removal, and microclimate regulation, often linked to their ecological condition.
- Regulatory assessments commonly use condition to evaluate wetland value, but the direct link between condition and all ecosystem functions, particularly hydrologic ones, is not always clear.
- Hydrologic function is crucial for many wetland services, influencing biogeochemical cycling, pollutant removal, floodwater retention, and microclimate regulation.
Purpose of the Study:
- To investigate the relationship between wetland ecological condition and hydrologic function.
- To test the hypothesis that ecological condition predicts hydrologic function, as assumed in regulatory wetland valuation.
- To assess how land use intensity influences wetland hydrologic functions and associated ecosystem services.
Main Methods:
- Assessed ecological condition using rapid and intensive methods, including Florida's official wetland assessment tool, across 11 isolated forested wetlands.
- Quantified hydrologic function by measuring hydrologic regime (water depth mean, variance, rates of change), groundwater exchange, and evapotranspiration (ET).
- Examined wetlands along a gradient of land use intensity, from minimally impacted to intensive agricultural and urban landscapes.
Main Results:
- No systematic variation in hydrologic regime (water depth dynamics) was observed across the condition gradient; reference sites exhibited a wide range of variation.
- Evapotranspiration (ET) rates were higher in intensive landscapes (urban, agriculture) due to increased leaf area, impacting microclimate regulation and carbon cycling.
- Groundwater exchange consistently reversed flow direction at all sites irrespective of condition, demonstrating a consistent buffering effect on regional aquifer levels.
Conclusions:
- Wetland ecological condition is not a reliable predictor of all hydrologic functions, challenging assumptions in current regulatory valuation methods.
- Evapotranspiration (ET) and its associated services (microclimate regulation, carbon cycling) are influenced by land use intensity, with benefits potentially amplified in developed areas.
- Isolated wetlands provide essential hydrologic services, such as aquifer buffering, regardless of their ecological condition, highlighting the value of "working wetlands" in diverse landscapes.
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