Abstract
Salt marsh survival in the face of sea-level rise (SLR) depends largely on a marsh’s ability to compensate for increased flooding by building in elevation, but the rate of elevation gain depends on processes that are not well-understood (i.e., belowground productivity, sediment accretion, and subsidence). An array of planted and unplanted pots was installed in the field to examine the effects of tidal flooding on productivity and elevation change. We found that belowground plant volume increased linearly as elevation increased for both Spartina patens and Spartina alterniflora. Even though the volume of roots increased by 400% with elevation for S. alterniflora and > 200% for S. patens, there was no relationship between belowground volume and elevation change of the original soil surface, perhaps due to the infilling of porosity by roots. However, the soil in planted treatments subsided significantly less than in unplanted controls. Measurements from Surface Elevation Tables (SETs) indicated that local high marshes have been losing elevation relative to sea level at an average rate of 2.1 mm/year. The rate of vertical gain decreased at SET locations of greater marsh elevation, and high marshes did not keep pace with SLR even when sediment supply appeared to be high (TSS = 57 ± 7 mg/L). The high marsh accretion deficit, combined with a continuing trend of reduced belowground growth with increased flooding due to SLR, suggests that S. alterniflora will replace less flood-tolerant species over time, potentially causing loss of high marsh habitat.
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Acknowledgments
We thank Cathy Wigand for her insight and guidance, Beth Watson for lending the greenhouse gas analyzer, Karen McKee for the advice during the set-up of the experiment, Chris Peter for his advice and help in the field, and the research assistants that made the study possible: Jacob Moore, Robert Lafreniere, Myrilla Hartkopf, Spencer Tate, Sarah Tierney, Molly McGovern, and John Wichert.
Funding
Permission to install the experiment and SETs was granted through the GBNERR. Funding for this research was provided by the University of New Hampshire Graduate School, the University of New Hampshire Marine Biology Program, the William Spaulding Endowment in Support of Marine Biology Research at the Jackson Estuarine Laboratory, the Society for Ecological Restoration Laderman Student Grant, and the Maine Association of Wetland Scientists, JEL contribution number 570.
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Payne, A.R., Burdick, D.M. & Moore, G.E. Potential Effects of Sea-Level Rise on Salt Marsh Elevation Dynamics in a New Hampshire Estuary. Estuaries and Coasts 42, 1405–1418 (2019). https://doi.org/10.1007/s12237-019-00589-z
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DOI: https://doi.org/10.1007/s12237-019-00589-z