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Updated: Feb 7, 2026

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Contrasting decadal-scale changes in elevation and vegetation in two Long Island Sound salt marshes
J C Carey1, K B Raposa2, C Wigand3
1The Ecosystems Center, Marine Biological Laboratory. Woods Hole, Massachusetts.
Summary
Salt marshes in the Northeastern US are experiencing varied responses to sea level rise. Some marshes are not keeping pace, while others are adapting, highlighting regional differences in marsh resilience.
Area of Science:
- Coastal ecology
- Geomorphology
- Environmental science
Background:
- Northeastern US salt marshes face co-stressors like sea level rise, nutrient enrichment, and low sediment supply.
- Understanding marsh surface elevation response is critical for predicting coastal ecosystem stability.
Purpose of the Study:
- To evaluate how salt marsh surface elevations respond to relative sea level rise (RSLR) and other co-stressors.
- To compare elevation changes and vegetation patterns in two distinct salt marshes.
Main Methods:
- Utilized surface elevation tables (SETs) and surface elevation pins to measure marsh surface elevation changes.
- Analyzed long-term historical vegetation data alongside elevation measurements.
- Compared marsh elevation gain rates with local rates of RSLR.
Main Results:
- Barn Island marsh is not keeping pace with RSLR (2.3 mm yr⁻¹), while Mamacoke Marsh shows increased elevation gain (4.2 mm yr⁻¹) to keep pace.
- Vegetation patterns at Barn Island shifted towards lower-elevation species, indicating stress.
- Mamacoke Marsh vegetation showed minimal change, suggesting greater stability.
Conclusions:
- Marsh elevation dynamics and vegetation responses to RSLR vary significantly, even within close proximity.
- Differences in sediment availability, salinity, and elevation capital likely drive contrasting marsh resilience.
- Findings emphasize that not all salt marshes in the region may respond uniformly to accelerated RSLR.
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