Ecology of Red Maple Swamps in the Glaciated Northeast: A ...
Ecology of Red Maple Swamps in the Glaciated Northeast: A ...
Ecology of Red Maple Swamps in the Glaciated Northeast: A ...
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Fig. 8.4. Electric utility l<strong>in</strong>es pass<strong>in</strong>g through a former red maple swamp. Forested swamp flanks <strong>the</strong><br />
pwerl<strong>in</strong>e on ei<strong>the</strong>r side while shrub swamp dom<strong>in</strong>ates <strong>the</strong> right-<strong>of</strong>-way.<br />
agricultural purposes. In nor<strong>the</strong>astern Connecticut,<br />
red maple swamps were sometimes clear-cut<br />
for fuelwood dur<strong>in</strong>g <strong>the</strong> first half <strong>of</strong> <strong>the</strong> twentieth<br />
century (Grace 1972).<br />
Clear<strong>in</strong>g <strong>of</strong> forested wetland for utility rights-<strong>of</strong>way<br />
is a major form <strong>of</strong> alteration that is grow<strong>in</strong>g <strong>in</strong><br />
importance throughout <strong>the</strong> Nor<strong>the</strong>ast (Fig. 8.4). In<br />
a sample <strong>of</strong> 100 Vermont wetlands surveyed <strong>in</strong><br />
1974,14% had been affected by transmission l<strong>in</strong>es<br />
(Wanner 1979). The impacts <strong>of</strong> cutt<strong>in</strong>g usually are<br />
compounded by wetland fa<strong>in</strong>g for <strong>the</strong> construction<br />
<strong>of</strong> power l<strong>in</strong>e ma<strong>in</strong>tenanm roads.<br />
The degree <strong>of</strong> impact <strong>of</strong> timber removal on<br />
wetland functions and values depends on <strong>the</strong> <strong>in</strong>tensity<br />
<strong>of</strong> cutt<strong>in</strong>g. Clear-cuts radically alter habitat<br />
values and may result <strong>in</strong> slightly higher water<br />
levels dur<strong>in</strong>g <strong>the</strong> summer because <strong>of</strong> reduced transpiration<br />
losses; selective cutt<strong>in</strong>g may have far<br />
less impact. Timber harvest<strong>in</strong>g for wood products<br />
is not currently a major form <strong>of</strong> alteration <strong>in</strong> red<br />
maple swamps, but <strong>in</strong>creas<strong>in</strong>g energy costs and<br />
elim<strong>in</strong>ation <strong>of</strong> upland forests by urbanization may<br />
heighten <strong>the</strong> importance <strong>of</strong> this activity <strong>in</strong> <strong>the</strong><br />
future.<br />
Water Level Manipulation<br />
Human-<strong>in</strong>duced changes <strong>in</strong> <strong>the</strong> water regime <strong>of</strong><br />
a red maple swamp may have major impacts on <strong>the</strong><br />
floristic composition and structure <strong>of</strong> <strong>the</strong> plant community,<br />
its habitat values, and its scenic and recreational<br />
values. Prior to <strong>the</strong> passage <strong>of</strong> wetland<br />
protection regulations, changes <strong>in</strong> wetland water<br />
regimes were a common consequence <strong>of</strong> highway<br />
construction. Culverts that were <strong>in</strong>wmt1y designed,<br />
improperly <strong>in</strong>stalled, or omitted altoge<strong>the</strong>r<br />
fkequently resulted <strong>in</strong> impoundment <strong>of</strong> water on<br />
<strong>the</strong> upstream side <strong>of</strong> <strong>the</strong> road and a reduction <strong>in</strong><br />
surface-water flow to <strong>the</strong> downstream side. Such<br />
impoundment commonly converted red maple<br />
swamps to marshes or shrub swamps. These impacts<br />
are less common today where wetland regulations<br />
are strictly enforced; however, sediment accumulation<br />
<strong>in</strong> culverts under roads may cause<br />
gradual changes <strong>in</strong> wah~egimes <strong>the</strong> same<br />
ultimate result (Golet and Parkhurst 1981). Nearly<br />
Wh <strong>of</strong> <strong>the</strong> human-<strong>in</strong>duced changes <strong>in</strong> <strong>in</strong>land wetlands<br />
<strong>of</strong> South K<strong>in</strong>gstown, R.I., between 1939 and<br />
1972 were retrogressive; raised water levels were<br />
<strong>the</strong> eause <strong>in</strong> most cases.<br />
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