The "wrack line" forms at the uppermost tide line of the marine intertidal gravel/sand beach. Here marine algae, eelgrass, shells, and other debris, are deposited at high tide. Since plants and seaweeds cannot grow in the unstable wash zone of the beach, numerous shorebirds and other animals rely on the wrack line as a food source.
There are an estimated 1000 miles of marine intertidal gravel/sand beach on Long Island covering about 10,000 to 16,000 acres; there may be more than 30 to 50 extant occurrences statewide. The several documented occurrences of this community have good viability and are protected on public or private conservation land. The community is restricted to the ocean shoreline of the Coastal Lowlands ecozone in Suffolk, Richmond, Queens, Kings, and Nassau Counties. Although the number of marine intertidal gravel/sand beaches may have increased slightly when formerly long, continuous examples were fragmented by development, the overall trend for the community is declining as a result of coastal development and recreational overuse. Sea level rise may result in permanent flooding of some occurrences, especially in areas where barriers prevent the migration of beaches inland.
The number and acreage of marine intertidal gravel/sand beaches have likely remained stable in recent decades, because most beach development occurs above mean high tide in the maritime beach and dune areas. However, beach viability/ecological integrity is suspected to be slowly declining, primarily due to anthropogenic alterations (both physical and hydrological) to beach/dune/swale dynamics and coastal development (e.g., fragmentation, shoreline hardening, road construction, and community destruction).
Although the number of marine intertidal gravel/sand beaches in New York may have increased from historical numbers when formerly long, continuous examples were fragmented by development into numerous large and small stretches of beach, their aerial extent and viability are suspected to have declined substantially over the long-term. These declines are likely correlated with coastal development and associated changes in connectivity, hydrology, water quality, and natural processes.
Maintain dynamic beach and dune processes, prevent recreational overuse (driving on the beach is particularly destructive) and encourage the public to carry away all of their trash. Ensure connectivity landward to maritime beaches and dunes, and offshore toward the open ocean that allows plants and animals to freely move between these habitats. Remove shoreline armoring to increase overland sediment input; improve water quality by reducing or eliminating sewer and stormwater discharge and pesticide application; restore tidal regime by removing culverts, dikes, and impoundments, plugging ditches, and replacing static flow restriction devices with those that are calibrated for local tidal hydrology.
Threats to marine intertidal gravel/sand beaches in New York include driving on the beach at low tide (ATVs and four-wheel drive vehicles), fragmentation by development, barriers to connectivity between the open ocean and the beach/dune system, trampling, increased horseback riding, and trash. Processes that create and maintain these beaches have been disrupted by hydrologic alterations to tidal dynamics, fragmentation, shoreline hardening, altered sediment budgets, and management practices like beach replenishment. Sea level rise may result in permanent flooding of some occurrences, especially in areas where barriers prevent the migration of beaches inland.
Maintain dynamic beach and dune processes, prevent recreational overuse (driving on the beach at low tide is particularly destructive) and encourage the public to carry away all of their trash. Ocean-derived trash may be deposited in the wrackline at some locations. Ensure connectivity between maritime dunes, maritime beaches, and the open ocean to allow seed dispersal and to enable species to freely move between habitats during nesting season. Remove shoreline armoring to increase overland sediment input; improve water quality by reducing or eliminating sewer and stormwater discharge and pesticide application; restore tidal regime by removing culverts, dikes, and impoundments, plugging ditches, and replacing static flow restriction devices with those that are calibrated for local tidal hydrology.
Minimize or eliminate hardened shoreline and avoid dumping dredge spoil onto marine intertidal beaches. This community is best protected as part of a larger ocean shoreline ecosystem. Protected areas should encompass nearshore marine communities, such as marine rocky intertidal and marine eelgrass meadows if present, as well as onshore maritime communities, such as maritime beach, dunes, and bluffs if present. Connectivity should be maintained in both directions, on- and offshore. Connectivity between these habitats is important not only for nutrient flow and seed dispersal, but also for animals that move between them seasonally. Similarly, fragmentation of linear beaches should be avoided. Bisecting roads and developments significantly disrupt biota and alter physical beach processes.
Surveys and documentation of additional occurrences are needed, as are data on rare and characteristic animals, especially benthic invertebrates.
Future research on marine intertidal gravel/sand beaches should include monitoring community response to sea level rise, sediment starvation, and permanent flooding and studying nutrient exchange processes and relationships to adjacent maritime communities above high tide.
This community is restricted to the ocean shoreline with sand or gravel substrate of the Coastal Lowlands ecozone in Suffolk, Richmond, Queens, Kings, and Nassau Counties
This community ranges along the Atlantic Coast from southern Maine to North Carolina.
The marine intertidal gravel/sand beach is a community washed by rough, high-energy waves, with sand or gravel substrates that are well-drained at low tide. These areas are subject to high fluctuations in salinity and moisture, but generally the sand is noticeably wetter than the adjacent maritime beach sand. A relatively low diversity community, it is perhaps best characterized by the benthic invertebrate fauna including polychaetes (Spiophanes bombyx, Pygospio elegans, Clymenella torquata, Scoloplos fragilis, Nephtys incisa), amphipods (Protohaustorius deichmannae, Acantho¬haustorius millsi), and mole crabs (Emerita spp.). This community provides feeding grounds for migrant shorebirds, such as sanderling (Calidris alba) and semipalmated plover (Charadrius semipalmatus), and breeding shorebirds, such as piping plover (Charadrius melodus).
These areas are subject to high fluctuations in salinity and moisture, but generally the sand is noticeably wetter than the adjacent maritime beach sand and located below the wrack line.
Known examples of this community have been found at elevations between -2 feet and 35 feet.
Marine intertidal gravel/sand beaches are scenic year-round! Enjoy a visit in the middle of the summer when the ocean is warm for swimming.
amphipod (Acantho¬haustorius millsi)
amphipod (Protohaustorius deichmannae)
mole crabs (Emerita spp.).
polychaete (Clymenella torquata)
polychaete (Nephtys incisa)
polychaete (Pygospio elegans)
polychaete (Scoloplos fragilis)
polychaete (Spiophanes bombyx)
This figure helps visualize the structure and "look" or "feel" of a typical Marine Intertidal Gravel/Sand Beach. Each bar represents the amount of "coverage" for all the species growing at that height. Because layers overlap (shrubs may grow under trees, for example), the shaded regions can add up to more than 100%.
Edinger, G. J., A. L. Feldmann, T. G. Howard, J. J. Schmid, E. Eastman, E. Largay, and L. A. Sneddon. 2008. Vegetation Classification and Mapping at Gateway National Recreation Area. Technical Report NPS/NER/NRTR—2008/107. National Park Service. Northeast Region. Philadelphia, PA.
Edinger, G. J., D. J. Evans, S. Gebauer, T. G. Howard, D. M. Hunt, and A. M. Olivero (editors). 2014. Ecological Communities of New York State. Second Edition. A revised and expanded edition of Carol Reschke’s Ecological Communities of New York State. New York Natural Heritage Program, New York State Department of Environmental Conservation, Albany, NY. https://www.nynhp.org/ecological-communities/
Edinger, G. J., E. S. Runnells, and T. G. Howard. 2019. Montauk Point, Marine Rocky Intertidal Monitoring, Year One 2018 Baseline Results. New York Natural Heritage Program, Albany, NY.
Edinger, Gregory J., D.J. Evans, Shane Gebauer, Timothy G. Howard, David M. Hunt, and Adele M. Olivero (editors). 2002. Ecological Communities of New York State. Second Edition. A revised and expanded edition of Carol Reschke's Ecological Communities of New York State. (Draft for review). New York Natural Heritage Program, New York State Department of Environmental Conservation. Albany, NY. 136 pp.
New York Natural Heritage Program. 2022. New York Natural Heritage Program Databases. Albany, NY.
Reschke, Carol. 1990. Ecological communities of New York State. New York Natural Heritage Program, New York State Department of Environmental Conservation. Latham, NY. 96 pp. plus xi.
This guide was authored by: Gregory J. Edinger
Information for this guide was last updated on: May 5, 2021
Please cite this page as:
New York Natural Heritage Program. 2022. Online Conservation Guide for Marine intertidal gravel/sand beach. Available from: https://guides.nynhp.org/marine-intertidal-gravelsand-beach/. Accessed January 16, 2022.