This New York natural community falls into the following ecological (, Rich graminoid fen The ecological integrity of the fen is dependent upon the ground water supply from the surrounding uplands. New York State Department of Environmental Conservation. 1980. In rich shrub fens, peat mosses (Sphagnum spp.) The area surrounding the preserve is buffer, part of which is being restored to native vegetation. Biodiversity Conserv. Evans, Cornus spp. (common winterberry), Larix laricina No date. Thus, road construction and development activities near this community type should strive to minimize particulate-laden run-off into this community. In 1959 a borehole was drilled at the Fen to provide drinking water for the local population, with a capacity to take 3,600m³ of water every day from the underlying aquifer. NatureServe Explorer: An online encyclopedia of life [web application]. (blue flag), Parnassia glauca If a fen is strongly groundwater influenced, traditional wetland buffers aimed at reducing surface water run-off may not sufficiently protect fen groundwater hydrology. Each bar represents the amount of A revised and expanded edition of Carol Reschke’s Ecological Communities of New York State. The deep groundwater system appears to be separated from the water in the fen’s peat layer by a clay layer that is the perching layer that the fen … The physically broadly-defined community may be widespread in areas of the United States and worldwide with calcareous peats. (poison-sumac), Cornus amomum ssp. (skunk-cabbage). maintained by NatureServe. (Draft for review). The current trend of 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. However, late summer precipitation Known examples of this community have been found at elevations between 230 feet and 770 feet. Even in fens, the water table begins to drop in late-July and August. Leopold. Linking landscape properties to local hydrogeologic gradients and plant species occurrence in minerotrophic fens of New York State, USA: A hydrogeologic setting (HGS) framework. The water level in a fen can rise and fall slightly with changes to the water table, but fens are characterized by having flowing water year around. News about Habitat Network, habitat tips, and more! floribunda), swamp fly honeysuckle (Lonicera oblongifolia), black chokeberry (Photinia melanocarpa), alder-leaf buckthorn (Rhamnus alnifolia), and poison sumac (Toxicodendron vernix). Nutrients are plenti… The nutrient rich conditions in a fen provide a diversity of plant life, which then supports a number of animal species that thrive in such highly productive habitats. A summary report prepared for the Nature Conservancy - Central/Western New York Chapter with funding from the Biodiversity Research Institute. New York Natural Heritage Program. Version 7.1. Marshes groan and gurgle wetly. (silky dogwood), Cornus sericea These were restored by blocking the flow of water in the main drainage ditch and by installing a series of channels to allow water to cross the road. Water deficiency and industrialization have led to serious water pollution in the Fen River. 1995. Lab 75:149-159. If a fen is strongly groundwater influenced, traditional wetland buffers aimed at reducing surface water run-off may not sufficiently protect fen groundwater hydrology. For example, extant bog turtle sites should be surveyed to determine the type and quality of the natural community if it is unknown. Like poison ivy and poison oak, poison sumac contains the chemical urushiol, which can cause a skin rash upon contact by sensitive people. Albany, NY. Consider how water flows around and into this wetland. Data sources can be found in Appendix 2 and additional novel approaches can be used as they become apparent. NTMWD also has water rights to, and obtains raw water from, Jim Chapman Lake (originally named Cooper Lake) on the South Sulpher River in Delta and Hopkins counties and Lake Tawakoni on the Sabine River in Rains and Van Zandt counties. So, road construction and other development activities should strive to consider: 1. how water moves through the ground, 2. the types of dissolved substances these development activities may release, and 3. how to minimize the potential for these dissolved substances to reach this natural community. State University of New York College of Environmental Science and Forestry Field forms database: Electronic field data storage and access for New York Heritage ecology, botany, and zoology. 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