Abstract

AbstractOngoing climate change is increasing rainfall variability in many parts of the world; in particular, the heaviest rainfall events are becoming heavier. In terrestrial ecosystems, nitrogen deposition is increasing as a result of emissions from fossil fuel burning and volatilization of nitrogen‐based fertilizers. These changes in the timing and rate of resource inputs can impact plant communities by altering competitive dynamics, succession, and community composition. In many systems, these are occurring alongside successional dynamics, making it difficult to tease apart mechanisms. Here, we resampled a nitrogen by rainfall variability manipulation experiment in a restored tallgrass prairie to examine the relative role of background community dynamics and treatment effects on plant diversity. During the treatment period, nitrogen addition and increased rainfall variability reduced diversity. Here, four and five years after the treatments were halted, we found similarly low levels of diversity across all treatments—an effect driven by dominance of a tall, fast‐growing, clonal forb, Solidago canadensis. The convergence of plots toward a low diversity state suggests that all experimental communities were gradually becoming dominated by S. canadensis, including in the absence of rainfall or nitrogen treatments. In contrast to short‐term findings from the same experiment, we conclude that our treatments accelerated succession toward a tall, clonal forb‐dominated community along an existing sere, but did not fundamentally alter longer‐term community composition—a result that was only apparent several years after the conclusion of the experiment. These findings reinforce the need to interpret the results from short‐term experimental manipulations within the context of long‐term successional change.

Highlights

  • Plant community assembly and function are influenced by a suite of anthropogenic forcings, including land-use change and disturbance, increased nitrogen (N) deposition, and concurrent changes in climate (Fujimaki et al 2009, Porter et al 2013, Perring et al 2016)

  • At the beginning of our experiment in 2012, we set out to examine how changes in resource availability might influence community dynamics of a restored tallgrass prairie that was approximately dominated by grasses and forbs (Smith et al 2016)

  • This effect persisted throughout the duration of the three-year treatment period (Smith et al 2016, Schuster and Dukes 2017)

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Summary

Introduction

Plant community assembly and function are influenced by a suite of anthropogenic forcings, including land-use change and disturbance, increased nitrogen (N) deposition, and concurrent changes in climate (Fujimaki et al 2009, Porter et al 2013, Perring et al 2016). While plant community responses to altered resource availability have been well studied (e.g., Clark and Tilman 2008, Cherwin and Knapp 2012, Borer et al 2014, Koerner and Collins 2014, Harpole et al 2016), fewer researchers have examined the conditions under which the effects of short-term manipulations last beyond the extent of the treatment period These effects alter system dynamics to send ecosystems on a trajectory of compositional and functional change that lasts beyond the cessation of a particular anthropogenic forcing (Perring et al 2016). By sampling global change experiments after the treatments end, it is possible to examine the lasting effects that human activity may have on ecosystems (Smith 2011)

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