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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Urbanization<br />
In most areas <strong>of</strong> <strong>the</strong> Nor<strong>the</strong>ast, urbanization<br />
(<strong>in</strong>clud<strong>in</strong>g highway construction) is now responsible<br />
for more <strong>in</strong>land wetland losses than all o<strong>the</strong>r<br />
causes comb<strong>in</strong>ed. In major metropolitan areas, it<br />
has been <strong>the</strong> pr<strong>in</strong>cipal factor for decades. The<br />
impact <strong>of</strong> urbanization on wetlands <strong>in</strong> any geographic<br />
area usually is closely related to <strong>the</strong><br />
population density <strong>of</strong> that area. Once aga<strong>in</strong>,<br />
nor<strong>the</strong>rn New Jersey is a prime example. The<br />
Office <strong>of</strong> Technology Assessment (1984) reported<br />
that 20-50% <strong>of</strong> Troy Meadows and three large<br />
swamps (Great Piece, Little Piece, and Hatfield)<br />
<strong>in</strong> <strong>the</strong> Passaic River bas<strong>in</strong> have been destroyed as<br />
a result <strong>of</strong> highway construction and subsequent<br />
commercial, <strong>in</strong>dustrial, and residential development.<br />
The effects <strong>of</strong> urbanization are noticeable<br />
even <strong>in</strong> <strong>the</strong> most rural parts <strong>of</strong> <strong>the</strong> Nor<strong>the</strong>ast.<br />
Construction <strong>of</strong> <strong>in</strong>terstate highways has spawned<br />
a series <strong>of</strong> resort communities <strong>in</strong> areas such as<br />
<strong>the</strong> Poconos <strong>of</strong> nor<strong>the</strong>astern Pennsylvania (T<strong>in</strong>er<br />
1984), upstate New York, and <strong>the</strong> White Mounta<strong>in</strong>s<br />
<strong>of</strong> New Hampshire. Significant wetland<br />
losses have occurred <strong>in</strong> some <strong>of</strong> those areas as a<br />
result.<br />
Data ga<strong>the</strong>red <strong>in</strong> sou<strong>the</strong>rn New England trend<br />
analysis studies (Table 8.2) suggest that residential<br />
and commercial development and <strong>the</strong> development<br />
<strong>of</strong> recreational facilities such as golf<br />
courses and athletic fields frequently contribute<br />
heavily to wetland losses <strong>in</strong> rural and suburban<br />
areas undergo<strong>in</strong>g rapid population <strong>in</strong>creases.<br />
Once aga<strong>in</strong>, road construction is an <strong>in</strong>tegral part<br />
<strong>of</strong> such urbanization. In Ma<strong>in</strong>e, as <strong>in</strong> much <strong>of</strong> <strong>the</strong><br />
Nor<strong>the</strong>ast, <strong>the</strong> impacts <strong>of</strong> urbanization were historically<br />
greatest <strong>in</strong> coastal wetlands and along<br />
major rivers (Wid<strong>of</strong>f 1988). Current losses are<br />
most common <strong>in</strong> small (less than 4 ha) <strong>in</strong>land<br />
wetlands <strong>in</strong> sou<strong>the</strong>rn Ma<strong>in</strong>e where population<br />
growth has been most dramatic. Wid<strong>of</strong>f ranked<br />
residential and commercial development as <strong>the</strong><br />
s<strong>in</strong>gle most important cause <strong>of</strong> vegetated wetland<br />
loss <strong>in</strong> Ma<strong>in</strong>e; she estimated that urbanization<br />
has been responsible for nearly 4096 (more than<br />
16,000 ha) <strong>of</strong> <strong>the</strong> totaI losses.<br />
Peat Harvest<strong>in</strong>g<br />
One additional agent oi wetland deskruetion <strong>in</strong><br />
some areas <strong>of</strong> <strong>the</strong> Nor<strong>the</strong>ast is <strong>the</strong> harvest<strong>in</strong>g <strong>of</strong><br />
peat, primarily for horticultural use. Peat harvest<strong>in</strong>g<br />
is a major <strong>in</strong>dustry <strong>in</strong> states such as M<strong>in</strong>nesota<br />
and North Carol<strong>in</strong>a, but it has been practiced to<br />
some degree <strong>in</strong> several <strong>of</strong> <strong>the</strong> nor<strong>the</strong>astern states<br />
as well. It is an important cause <strong>of</strong> wetland loss <strong>in</strong><br />
<strong>the</strong> Poconos <strong>of</strong> nor<strong>the</strong>astern Pemylvania ('I'<strong>in</strong>er<br />
1984). In Ma<strong>in</strong>e, this <strong>in</strong>dustry peaked dur<strong>in</strong>g <strong>the</strong><br />
1930's and 1940'9, but most operations closed down<br />
for economic reasons (Wid<strong>of</strong>f 1988). Wid<strong>of</strong>f estimated<br />
that 2% (910 ha) <strong>of</strong> Ma<strong>in</strong>e's vegetated wetland<br />
loss may be due to peat harvest<strong>in</strong>g.<br />
Peat harvest<strong>in</strong>g for horticulture generally is<br />
carried out <strong>in</strong> Sphagnum bogs, which conta<strong>in</strong><br />
large quantities <strong>of</strong> poorly decomposed fibric peat.<br />
This type <strong>of</strong> peat has <strong>the</strong> highest moisture retention<br />
capacity and so is most valuable as a soil<br />
conditioner. S<strong>in</strong>ce red maple swamps have m<strong>in</strong>eral<br />
soils or well-decomposed (sapric) to moderately<br />
well-decomposed (hemic) organic soils, <strong>the</strong>y<br />
are <strong>of</strong> little value as a source <strong>of</strong> horticultural peat.<br />
Dur<strong>in</strong>g <strong>the</strong> 19'70'9, when <strong>the</strong> United States experienced<br />
a brief, but severe, shortage <strong>of</strong> fossil fuels,<br />
considerable attention was focused on <strong>the</strong> possible<br />
use <strong>of</strong> peat as a supplementary energy source. The<br />
uncerta<strong>in</strong>ty <strong>of</strong> cont<strong>in</strong>ued fossil fuel availability<br />
suggests that pressures to harvest peat from<br />
nor<strong>the</strong>astern wetlands for energy production may<br />
<strong>in</strong>crease. Sapric and hemic peats generally have<br />
higher energy value per unit <strong>of</strong> weight than fibric<br />
peat (F'arnharn 1979). For this reason, red maple<br />
swamps and o<strong>the</strong>r types <strong>of</strong> forested wetlands with<br />
organic soils may be seriously considered as potential<br />
sources <strong>of</strong> energy-produc<strong>in</strong>g peat <strong>in</strong> future<br />
years.<br />
O<strong>the</strong>r Forrns <strong>of</strong> Wetland Alteration<br />
Although direct losses clearly have <strong>the</strong> greatest<br />
impact on <strong>the</strong> wetland resource, o<strong>the</strong>r alterations<br />
beside total destruction may also significantly affect<br />
<strong>the</strong> structure and functions <strong>of</strong> wetlands and <strong>the</strong>ir<br />
value to society. The follow<strong>in</strong>g paragraphs identify<br />
some <strong>of</strong> <strong>the</strong>se additional forms <strong>of</strong> alteration.<br />
Tree Cutt<strong>in</strong>g<br />
Cutt<strong>in</strong>g <strong>of</strong> wetland trees for fuel and fence posts<br />
was common <strong>in</strong> <strong>the</strong> Nor<strong>the</strong>ast prior to <strong>the</strong> decl<strong>in</strong>e<br />
<strong>of</strong> agriculture <strong>in</strong> <strong>the</strong> late n<strong>in</strong>eteenth century. Wid<strong>of</strong>f<br />
(1988) noted that timber harvest<strong>in</strong>g is still<br />
widespread <strong>in</strong> Ma<strong>in</strong>e wetlands dur<strong>in</strong>g <strong>the</strong> w<strong>in</strong>ter.<br />
In sou<strong>the</strong>rn Rhode Island (Golet and Parkhurst<br />
1981) and <strong>in</strong> New Jersey (T<strong>in</strong>er 1985), selective<br />
cutt<strong>in</strong>g <strong>of</strong> Atlantic white cedar has converted some<br />
mixed wetland forests to predom<strong>in</strong>antly red maple.<br />
Larson et al. (1980) speculated that much <strong>of</strong><br />
<strong>the</strong> shrub swamp and shallow marsh <strong>in</strong> <strong>the</strong>ir<br />
sou<strong>the</strong>astern Massachusetts study area was formerly<br />
forested wetland that had been cleared for