The salinity of coastal salt ponds can change over time. Lakes or ponds are formed when sandspits close off a lagoon or bay of the ocean. During storm surges these sandspits can be destroyed and the pond is again connected to the ocean. The water is typically brackish with varying degrees of salinity depending on the amount of freshwater inflow and if the pond has recently been connected to the ocean salt water. The plant and animal life in these ponds can change drastically depending on the salinity of the water. These ponds can be the nurseries for many species of fish and shellfish. They are also a favorite stopping point for all types of migratory birds.
This community only occurs on the coastal plain of New York. There are very few, small (low acreage) occurrences currently mapped. Many documented occurrences have good viability and are protected while others are threatened by coastal development. The current trend for this community is probably stable for occurrences on public land, or declining slightly elsewhere due to moderate threats related to development pressure or alteration to the natural hydrology. This community has declined moderately to substantially from historical numbers likely correlated with an increase in residential and commercial development.
The number and acreage of coastal salt ponds in New York have probably declined in recent decades due to human impacts on the hydrology including ditching, draining, impoundments, and artificial connections to the ocean. The inlets to some of the larger ponds are kept open by dredging to allow boat passage between marinas that were built on the pond and the ocean thereby disrupting the natural processes of the opening and closing of ponds to the ocean.
The numbers and acreage of coastal salt ponds have probably declined steadily from their historical range. It is estimated that there were approximately 2000 acres in New York. Currently, a little over 200 acres are mapped. The decline probably coincided with settlement of the area and a steady increase in residential and commercial development.
The coastal salt pond community is threatened by coastal development and alterations to hydrology or tidal regimes including ditching, dredging, and the construction of artificial connections to the ocean. The inlets of larger salt ponds are kept open by regular dredging to allow boat traffic. The natural opening and closing of the connection to the ocean caused by storms is disrupted. Shorelines are also artificially hardened to prevent the natural movement of sand. There are also threats to water quality including oil spills from holding tanks on adjacent uplands. Other threats include an increase in recreational development, trash, the presence of exotic species including mute swans, and the spread of invasive plant species such as common reed (Phragmites australis).
Coastal plain ponds are susceptible to alterations by a number of different factors. Management considerations of these ponds on Long Island needs to include: preventing off-road vehicle use and limiting trails; improving the integrity of the pond margins; maintaining or improving water quality; removing invasive species including mute swans and common reed (Phragmites australis); maintaining intact upland landscapes and maintaining the natural hydrology including avoiding mosquito ditching and artificial connections to the ocean.
Strive to minimize or eliminate alterations to hydrology. In particular, strive to maintain the natural processes that originally formed the ponds. These ponds were formed and are maintained when sandspits close off a lagoon or bay of the ocean forming a pond or lake. During storm surges, these sandspits can be destroyed and the pond is once again connected to the ocean. The artificial dredging to maintain a permanent connection to the ocean disrupts this process. In addition, hardened (stabilized) shorelines prevent the natural movement of sand by wind and water that is instrumental in the formation and maintenance of this natural community. Connectivity to other coastal natural communities should be maintained. Connectivity between these habitats is important not only for nutrient flow and seed dispersal, but also for animals that move between them seasonally. Development of site conservation plans that identify threats and their sources and provide management and protection recommendations would ensure the long-term viability of coastal salt ponds.
Inventory needs for coastal salt ponds include: conduct surveys for additional sites; improve maps; refine species identifications; improve composition and structure descriptions for each association; and determine long-term variation of tidal overwash rate, salinity, temperature, water surface elevation, and trophic state.
Research is needed to fill information gaps about coastal salt ponds, especially to advance our understanding of their classification. Research is also needed to document the two community microhabitats that are typically encountered within one pond complex: 1) the "pond" or aquatic portion of the complex and 2) the "shore" or the non-aquatic part of the complex. These two microhabitats are likely to warrant separate communities and may be distinguished in a future version of the state community classification: the former retaining the name "coastal salt pond," the latter designated as a "coastal salt pond shore."
Coastal salt ponds are limited to the coastal plain (lowlands) of New York. Their original range probably included all of Long Island. Currently, most are found in eastern Suffolk County.
This coastal salt pond community occurs along the northeastern Atlantic coast from Maine to New Jersey and possibly to Maryland and Virginia. New York is in the central part of their range (NatureServe Explorer 2009).
This community occurs along the marine shoreline. Lakes or ponds are formed when sandspits close off a lagoon or bay of the ocean. During storm surges these sandspits can be destroyed and the pond is again connected to the ocean. The water is typically brackish with varying degrees of salinity depending on the amount of freshwater inflow and if the pond has recently been connected to the ocean salt water. The ponds have two microhabitats, the pond itself and the shoreline. Dominant plants and animals can change quickly depending on salinity. Typical ponds are dominated by widgeon grass and the marine red algae tubed weed. Animals in these ponds include multiple species of grass shrimp and the estuarine minnow mummichog, sheepshead minnow and various killifish. Common coastal waterbirds include great blue herons and egrets.
This community occurs along the marine shoreline. The salt ponds are formed when sandspits close off a lagoon or bay of the ocean. During storm surges these sandspits can be destroyed and the pond is again connected to the ocean. A narrow beach usually separates the pond from the ocean.
For the naturalist, some of the best times to visit are during spring and fall bird migrations. Many species of birds use the ponds as stopover points along their journeys from wintering sites in the south to breeding grounds further north. If the salt pond is big enough, the shallow and warmer waters make for good kayaking and other recreational activities in the summer months.
This New York natural community encompasses all or part of the concept of the following International Vegetation Classification (IVC) natural community associations. These are often described at finer resolution than New York's natural communities. The IVC is developed and maintained by NatureServe.
This New York natural community falls into the following ecological system(s). Ecological systems are often described at a coarser resolution than New York's natural communities and tend to represent clusters of associations found in similar environments. The ecological systems project is developed and maintained by NatureServe.
Baccharis halimifolia (groundsel-tree)
Iva frutescens (salt marsh-elder)
Baccharis halimifolia (groundsel-tree)
Eleocharis parvula (salt-loving spike-rush)
Ruppia maritima (widgeon-grass, ditch-grass)
Schoenoplectus americanus (chair-maker's bulrush)
Spartina alterniflora (smooth cord grass)
Spartina patens (salt-meadow cord grass)
Potamogeton perfoliatus (clasping-leaved pondweed)
Stuckenia pectinata (Sago pondweed)
Zannichellia palustris (horned pondweed)
This figure helps visualize the structure and "look" or "feel" of a typical Coastal Salt Pond. 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%.
Bliven, S. and A.L. Hankin (eds). 1985, Salt ponds and tidal inlets: maintenance and management considerations. Proceedings of a conference, November 19, 1983. Sponsored by Massachusetts Coastal Zone Management Office, Lloyd Center for Environmental Studies. Lloyd Center Publication # 2-85.
Conard, H.S. 1935. The plant associations of central Long Island. American Midland Naturalist 16:433-515.
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. http://www.dec.ny.gov/docs/wildlife_pdf/ecocomm2014.pdf
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.
Harlin, M.M., V.J. Masson, and R.E. Flores. 1995. Distribution and abundance of submerged aquatic vegetation in Trustom Pond, Rhode Island. Report submitted to US Fish and Wildlife Service, October 13, 1995.
NatureServe. 2009. NatureServe Explorer: An online encyclopedia of life [web application]. Version 7.1. NatureServe, Arlington, Virginia. Available http://www.natureserve.org/explorer. (Data last updated October, 2009)
New York Natural Heritage Program. 2020. 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.
Salt Ponds Coalition. 2009. Salt Ponds Coalition [web application]: Available http://www.saltpondscoalition.org/news.html. April 2009.
Thorne-Miller, B., M. M. Harlin, G. B. Thursby, M. M. Brady-Campbell, and B. A. Dworetsky. 1983. Variations in the distribution and biomass of submerged macrophytes in five coastal lagoons in Rhode Island, USA. Botanica Marina 26:231-242.
This guide was authored by: Aissa Feldmann
Information for this guide was last updated on: May 3, 2019
Please cite this page as:
New York Natural Heritage Program. 2020. Online Conservation Guide for Coastal salt pond. Available from: https://guides.nynhp.org/coastal-salt-pond/. Accessed January 19, 2020.