4.7 Article

Net Ecosystem Production of Lakes Estimated From Hypolimnetic Organic Carbon Sinks

Journal

WATER RESOURCES RESEARCH
Volume 57, Issue 5, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020WR029473

Keywords

gross sedimentation; nitrogen; organic carbon; oxygen depletion; phosphorus; primary production; sediment accumulation

Funding

  1. Swiss National Science Foundation on Primary production under oligotrophication in lakes [200021_179123]
  2. Swiss Federal Office of the Environment (BAfU/FOEN) on Primarproduktion in Seen unter Oligotrophierung
  3. Swiss National Science Foundation (SNF) [200021_179123] Funding Source: Swiss National Science Foundation (SNF)

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This study introduces a novel concept for estimating the net ecosystem production in lakes, taking into account various factors that may interfere with the estimation process. By utilizing data from routinely available monitoring, the estimation of NEP is made more robust over the productive season. The approach also helps to verify and constrain the uncertainty of the estimates through comparison with export budgets.
This study presents a novel concept for estimating net ecosystem production (NEP), the export of organic carbon (OC) from the productive surface layer to the deep-water (hypolimnion) of 11 seasonally stratified lakes, varying in depth and trophic state. As oxygen remineralizes settling OC at a constant ratio, NEP is equivalent to the areal hypolimnetic mineralization rate (AHM) plus burial in the sediment. Two major interferences have to be considered, however. First, OC from terrestrial sources, not originating from primary production, consumes a fraction of oxidants. Second, sediment diagenetic processes of lakes in trophic transition (e.g., undergoing eutrophication or reoligotrophication) that are not in quasi-steady-state with actual fluxes of OC from the productive surface layer, bias the NEP estimation. In these cases, the flux of reduced substances diffusing from the sediment must be subtracted. This results in some overestimation for lakes with high allochthonous loads, and slight underestimation in lakes that are not in quasi-steady-state, because the actual sediment burial of autochthonous OC is small but not negligible. The presented approach requires data from routinely available monitoring and thus can be applied to historic data. The temporal integration over the productive season makes the estimation of NEP robust. Based on a historic 47 years long data record of Lake Geneva, NEP estimations (similar to 70 gC m(-2)) from AHM rates agree well with P and N export budgets from the productive surface zone, which help to verify and constrain the uncertainty of the estimates.

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