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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Community S tructare<br />
<strong>Red</strong> maple swamps conta<strong>in</strong> as many as five<br />
dist<strong>in</strong>ct vegetation life-form layers: trees, sapl<strong>in</strong>gs,<br />
shrubs, herbs, and ground cover (Fig. 3.6). In this<br />
report,, trees axe considered to be woody plants at<br />
least 6 m tall (after Coward<strong>in</strong> et al. 1979), while<br />
sapl<strong>in</strong>gs are woody plants <strong>of</strong> tree form that are<br />
shorter than 6 m. In mature red mapIe swamps<br />
(i.e., those at least 40-50 years <strong>of</strong> age), <strong>the</strong> tree<br />
canopy typically forms a layer about 8 to 15 m<br />
above <strong>the</strong> forest floor. Sapl<strong>in</strong>g crow~ls axe most<br />
evident at a height <strong>of</strong> 3 to 6 m above <strong>the</strong> ground;<br />
however, at most sites, <strong>the</strong> sapl<strong>in</strong>g layer is <strong>the</strong> most<br />
paorly developed. The shrub layer <strong>in</strong>cludes woody<br />
plants that are us\lally less than 3 m tall. Shrub<br />
foliage is commonly dense and <strong>of</strong>ten extends to<br />
with<strong>in</strong> a mebr <strong>of</strong> <strong>the</strong> ground. The herb layer consists<br />
<strong>of</strong> nonwaody erect plants such as ferns,<br />
grasses, sedges, and broad-leaved herbs that are<br />
nomalIy less than 1.5 In tall. Bryophytes, clubnlusses<br />
(Ly@opOd<strong>in</strong>ceae), trail<strong>in</strong>g shrubs (e.g.,<br />
IZub~s hispidus, GiultFzria pmurntwns), and<br />
o<strong>the</strong>r law-grow<strong>in</strong>g plants fornr <strong>the</strong> ground cover<br />
layer. V<strong>in</strong>ee such as penbriers (Smiht spp.),<br />
Virg<strong>in</strong>ia creeper (Pnrth~noeissus quirzquefolia),<br />
and poisox~ ivy CbxWdro~z<br />
mdimns) also are<br />
a eonspicuou~ component <strong>of</strong> many red maple<br />
swanxps. he,<br />
shrub, and herb strata predom<strong>in</strong>ate<br />
<strong>in</strong> nm~t red maplo ewmlps, arid we will emphasize<br />
<strong>the</strong>se life forms <strong>in</strong> this report.<br />
'I'hc followixlg pamgraptls prrsent a description<br />
<strong>of</strong> pltnit community struct,\irc. <strong>in</strong> nor<strong>the</strong>astern red<br />
maple swamps. Studies on this topic have been few;<br />
most have been wnducted <strong>in</strong> sou<strong>the</strong>rn New England,<br />
New York, or New Jersey. While some <strong>of</strong> <strong>the</strong><br />
New Jersey sites lie outside <strong>the</strong> glaciated Nor<strong>the</strong>ast,<br />
Uley are <strong>in</strong>cluded hem because <strong>of</strong> <strong>the</strong>ir obvious<br />
similarity, both structurally and floristically, to<br />
swamps far<strong>the</strong>r north. Quantitative data from <strong>the</strong><br />
studies cited <strong>in</strong> this section <strong>of</strong>ten cannot be compared<br />
directIy because <strong>of</strong> differ<strong>in</strong>g def<strong>in</strong>itions <strong>of</strong> <strong>the</strong><br />
life forms sampled. Variations among sites <strong>in</strong> stand<br />
age, orig<strong>in</strong> (sprout vs. seedl<strong>in</strong>g), and environmental<br />
conditions such as water regime also confound comparisons<br />
among studies. Never<strong>the</strong>less, <strong>the</strong> follow<strong>in</strong>g<br />
data provide a general picture <strong>of</strong> community<br />
structure <strong>in</strong> severai areas <strong>of</strong> <strong>the</strong> Nor<strong>the</strong>ast.<br />
Tree Layer<br />
Forested wetlands <strong>in</strong> <strong>the</strong> United States are generally<br />
characterized by high stem density, high<br />
basal area, and tree heights <strong>in</strong> excess <strong>of</strong> 10 m<br />
(Brown et d. 1979). Trees <strong>in</strong> nor<strong>the</strong>rn swarrlps<br />
(235' N latitude) tend to be shorter and to have<br />
lower basal areas than trees <strong>in</strong> sou<strong>the</strong>rn swamps,<br />
A review <strong>of</strong> structural data from mature nor<strong>the</strong>astern<br />
red maple swamps Fable 3.1) suggests<br />
that tree heights are comparable to those from<br />
o<strong>the</strong>r temperate, nonfloodpla<strong>in</strong> wetland forests<br />
(Brown et d. 1979), but tree density and basal area<br />
are co1*111lonly below average.<br />
Eieighta <strong>of</strong> red maple stands 30-100 years <strong>of</strong> age<br />
span a relatively narrow range. Stand heights reported<br />
from sou<strong>the</strong>rn New England and nor<strong>the</strong>ni<br />
I<br />
Fig. 3.6. Structural pr<strong>of</strong>ile <strong>of</strong> a seasonally flooded red maple swamp. Illustrated are tree (>6 m), sapl<strong>in</strong>g (3-6 m),<br />
(