Monitoring Maine's Salt Marshes

Aerial view of Little River Marsh, photo by Slade Moore & John Sowles

Why Salt Marsh Monitoring?

Salt marshes provide coastal communities with storm and flood protection, fish and wildlife habitat, recreational and commercial harvesting opportunities, and pollutant filtration. They also store carbon that would otherwise contribute to climate change, including accelerated sea level rise. Salt marshes are especially sensitive to changes in water levels because they occupy such a narrow elevation band in the space between high and low tide. Over the past 5,000 years, salt marshes responded to slowly rising oceans by accumulating sediment and plant material at a rate fast enough to build upward and keep pace with sea level rise. In recent decades, the rate of sea level rise has doubled and it's projected to increase further. Marshes in some regions are drowning, leaving scientists concerned Maine's marshes might experience the same pattern. Although efforts are underway to develop responses to the effects of accelerated sea level rise, a better understanding of the processes involved is needed to help guide Maine's response, now and in the future.

Maine's Salt Marsh Monitoring Network

Addressing so much uncertainty about how marshes will respond to sea level rise over time requires a multi-decade commitment to monitoring over a wide area.

The Maine Coastal Program and our partners have established dozens of long-term monitoring stations as the foundation of the Maine Salt Marsh Monitoring Network. An important element of our work involves the use of elevation benchmarks anchored by steel rods driven up to 80 feet deep in marsh soils for stability. Each year, we measure changes in the marsh surface elevation in relation to the benchmark. Over time, these measurements are compared to trends in the local sea level to determine if the marsh surface is keeping pace with sea level rise.

Installing steel rod in tidal marsh, and marsh mud core, photo by Kristen Puryear

We also study the processes that influence changes in marsh surface elevations. We do this by placing a layer of light grey feldspar dust in each monitoring station. Over time, sediment and organic material naturally deposit above the feldspar and we periodically record the depth of that material. If the depth is greater than the measured increase in marsh surface elevation, the marsh surface may be sinking, which is a sign of low resilience to sea level rise. At each site, we also collect data describing changes in plant communities to predict future marsh health. What we learn at these sites will help inform investment planning and other decision-making for coastal communities, marsh conservation, and habitat restoration in the coming decades.

Contributors to the Marsh Monitoring Program's Development Logos of marsh monitoring program contributor organizations

  • Backcountry Hunters & Anglers
  • Bates College
  • Bowdoin College
  • Casco Bay Estuary Partnership
  • Great Bay National Estuarine Research Reserve
  • Kennebec Estuary Land Trust
  • Maine Coast Heritage Trust
  • Maine Dept. of Inland Fisheries and Wildlife
  • Maine Geological Survey, Maine Dept. of Agriculture, Conservation, and Forestry
  • Natural Areas Program, Maine Dept. of Agriculture, Conservation, and Forestry
  • The Nature Conservancy
  • New Hampshire Department of Fish and Game
  • Stantec
  • US Fish and Wildlife Service
  • US National Oceanic and Atmospheric Administration
  • US National Park Service
  • University of Maine
  • University of New Hampshire
  • Wells National Estuarine Research Reserve
  • York Land Trust

For More Information About This Work

Contact the Marsh Monitoring Network Project Manager, Slade Moore at: smoore@bioconserve.net.