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- W2020432362 abstract "New England's coastal plain ponds occupy areas of glacially deposited outwash, till, or former glacial lake beds. Generally, these ponds lie in gently sloping basins with no inlet or outlet and are intimately linked with the underlying groundwater or aquifer. Water levels rise and fall naturally with the seasons, depending on rainfall/ evaporation cycles. There are hundreds of ponds, distributed in three main areas. New England's coastal plain ponds vary significantly in physical, chemical, and biological characteristics, but are united by several dominant features. (1) With rare exceptions they are permanent bodies of water and do not dry out annually as do southern US ponds. (2) They are highly acidic and nutrient-poor. (3) Their basins are sloping, creating concentric bands of vegetation as waters recede. (4) The dominant emergent, when present, is Juncus militaris, not Panicum hemitomon as in southern US ponds. (5) Dominant plants in the drawdown zone are graminoid and herbaceous species; woody plants are absent. Forty-one Atlantic coastal plain pond plant taxa are considered rare in one or more New England states, the great majority occuring only in southeastern Massachusetts and Rhode Island. One taxon is endemic to the region: Eupatorium leucolepis var. novae-angliae; five others are nearly so. Because they hold water during the summer, New England's coastal plain ponds are attractive to recreation and housing development. During 1970–1990 large-scale impacts resulted from these activities and from recreational vehicle use and water extraction, so that few pristine ponds are left." @default.
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- W2020432362 date "1994-01-01" @default.
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- W2020432362 title "Coastal plain ponds in New England" @default.
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- W2020432362 doi "https://doi.org/10.1016/0006-3207(94)90410-3" @default.
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