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Publication Additional Information Download
Publication Type
Journal Article
Authorship
Corman J. R., Zwart J. A., Klug J., Bruesewitz D. A., de Eyto E., Klaus M., Knoll L. B., Rusak J. A., Vanni M. J., Alfonso M. B., Fernandez R. L., Yao H., Austnes K., Couture R-M., de Wit H. A., Karlsson J., Laas A.
Title
Response of lake metabolism to catchment inputs inferred using high-frequency lake and stream data from across the northern hemisphere
Year
2023
Publication Outlet
Limnology and Oceanography Volume 68, Issue 12 Pages 2617-2631
DOI
https://doi.org/10.1002/lno.12449
ISSN
0730-7268
Citation
Corman J. R., Zwart J. A., Klug J., Bruesewitz D. A., de Eyto E., Klaus M., Knoll L. B., Rusak J. A., Vanni M. J., Alfonso M. B., Fernandez R. L., Yao H., Austnes K., Couture R-M., de Wit H. A., Karlsson J., Laas A. (2023). Response of lake metabolism to catchment inputs inferred using high-frequency lake and stream data from across the northern hemisphere. Limnology and Oceanography Volume 68, Issue 12 Pages 2617-2631 https://aslopubs.onlinelibrary.wiley.com/doi/10.1002/lno.12449
Abstract
In lakes, the rates of gross primary production (GPP), ecosystem respiration (R), and net ecosystem production (NEP) are often controlled by resource availability. Herein, we explore how catchment vs. within lake predictors of metabolism compare using data from 16 lakes spanning 39°N to 64°N, a range of inflowing streams, and trophic status. For each lake, we combined stream loads of dissolved organic carbon (DOC), total nitrogen (TN), and total phosphorus (TP) with lake DOC, TN, and TP concentrations and high frequency in situ monitoring of dissolved oxygen. We found that stream load stoichiometry indicated lake stoichiometry for C : N and C : P (r2 = 0.74 and r2 = 0.84, respectively), but not for N : P (r2 = 0.04). As we found a strong positive correlation between TN and TP, we only used TP in our statistical models. For the catchment model, GPP and R were best predicted by DOC load, TP load, and load N : P (R2 = 0.85 and R2 = 0.82, respectively). For the lake model, GPP and R were best predicted by TP concentrations (R2 = 0.86 and R2 = 0.67, respectively). The inclusion of N : P in the catchment model, but not the lake model, suggests that both N and P regulate metabolism and that organisms may be responding more strongly to catchment inputs than lake resources. Our models predicted NEP poorly, though it is unclear why. Overall, our work stresses the importance of characterizing lake catchment loads to predict metabolic rates, a result that may be particularly important in catchments experiencing changing hydrologic regimes related to global environmental change.
Program Affiliations
GWF: Global Water Futures
Publication Stage
Published
Additional Information
Probably not a GWF publication
Download Links
https://doi.org/10.1002/lno.12449
https://aslopubs.onlinelibrary.wiley.com/doi/10.1002/lno.12449
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