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Volume 27, Issue 5 p. 1529-1540
Article

Lake nutrient stoichiometry is less predictable than nutrient concentrations at regional and sub-continental scales

Sarah M. Collins

Corresponding Author

Sarah M. Collins

Department of Fisheries and Wildlife, Michigan State University, 13 Natural Resources, East Lansing, Michigan, 48824 USA

Center for Limnology, University of Wisconsin, 680 North Park Street, Madison, Wisconsin, 53706 USA

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Samantha K. Oliver

Samantha K. Oliver

Center for Limnology, University of Wisconsin, 680 North Park Street, Madison, Wisconsin, 53706 USA

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Jean-Francois Lapierre

Jean-Francois Lapierre

Département de Sciences Biologiques, Université de Montreal, Pavillon Marie-Victorin, CP 6128, succursale Centre-ville, Montréal, Quebec, H3C 3J7 Canada

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Emily H. Stanley

Emily H. Stanley

Center for Limnology, University of Wisconsin, 680 North Park Street, Madison, Wisconsin, 53706 USA

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John R. Jones

John R. Jones

School of Natural Resources, University of Missouri, 302 Anheuser-Busch Natural Resources Building, Columbia, Missouri, 65211 USA

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Tyler Wagner

Tyler Wagner

U.S. Geological Survey, Pennsylvania Cooperative Fish and Wildlife Unit, The Pennsylvania State University, 402 Forest Resources Building, University Park, Pennsylvania, 16802 USA

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Patricia A. Soranno

Patricia A. Soranno

Department of Fisheries and Wildlife, Michigan State University, 13 Natural Resources, East Lansing, Michigan, 48824 USA

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First published: 31 March 2017
Citations: 41
Corresponding Editor: Christer Nilsson.

Abstract

Production in many ecosystems is co-limited by multiple elements. While a known suite of drivers associated with nutrient sources, nutrient transport, and internal processing controls concentrations of phosphorus (P) and nitrogen (N) in lakes, much less is known about whether the drivers of single nutrient concentrations can also explain spatial or temporal variation in lake N:P stoichiometry. Predicting stoichiometry might be more complex than predicting concentrations of individual elements because some drivers have similar relationships with N and P, leading to a weak relationship with their ratio. Further, the dominant controls on elemental concentrations likely vary across regions, resulting in context dependent relationships between drivers, lake nutrients and their ratios. Here, we examine whether known drivers of N and P concentrations can explain variation in N:P stoichiometry, and whether explaining variation in stoichiometry differs across regions. We examined drivers of N:P in ~2,700 lakes at a sub-continental scale and two large regions nested within the sub-continental study area that have contrasting ecological context, including differences in the dominant type of land cover (agriculture vs. forest). At the sub-continental scale, lake nutrient concentrations were correlated with nutrient loading and lake internal processing, but stoichiometry was only weakly correlated to drivers of lake nutrients. At the regional scale, drivers that explained variation in nutrients and stoichiometry differed between regions. In the Midwestern U.S. region, dominated by agricultural land use, lake depth and the percentage of row crop agriculture were strong predictors of stoichiometry because only phosphorus was related to lake depth and only nitrogen was related to the percentage of row crop agriculture. In contrast, all drivers were related to N and P in similar ways in the Northeastern U.S. region, leading to weak relationships between drivers and stoichiometry. Our results suggest ecological context mediates controls on lake nutrients and stoichiometry. Predicting stoichiometry was generally more difficult than predicting nutrient concentrations, but human activity may decouple N and P, leading to better prediction of N:P stoichiometry in regions with high anthropogenic activity.