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Wetlands are:
areas where soils are water-saturated for a sufficient length of time
such that excess water and resulting low soil oxygen levels are princi-
pal determinants of vegetation and soil development. Wetlands will
have a relative abundance of hydrophytes in the vegetation commu-
nity and/or soils featuring “hydric” characters.
This wetland definition encompasses a wide range of ecosystems, from
semi-terrestrial fens, bogs, and swamps to semi-aquatic marshes and
shallow open water. Wetlands include a broad range of ecosystem types,
from those permanently flooded by shallow water and dominated by
aquatic organisms to forested sites with merely wet soils.
The water-saturated environment of wetlands supports a unique group
of plants called hydrophytes. These plants are adapted to grow in water-
logged soils. Excessive water and the low rate at which oxygen diffuses
under these conditions leads to a complex of critical conditions that re-
quire specialized adaptations (Daubenmire 1959). Adaptations, such as
leathery leaves (to reduce nutrient requirements and combat physiologi-
cal drought) or specialized internal air compartments (to transport
oxygen to the roots) are required for wetland plants. Obligate hy-
drophytes (such as great bulrush) are restricted to wetlands and
semi-aquatic sites. Facultative hydrophytes (such as Labrador tea and
many other members of the Heather family) occur commonly in wet-
lands but also appear on some upland sites.
Wetland soils are subhydric or hydric and have one or more of the fol-
lowing features that reflect anaerobic soil conditions:
1. Peaty organic horizons greater than 40 cm thick.
2. Non-sandy soils with blue-grey gleying within 30 cm of the surface.
3. Sandy soils with prominent mottles within 30 cm of the surface or
blue-grey matrix.
4. Hydrogen sulphide (rotten egg smell) in upper 30 cm.
From an ecological perspective, either an abundance of hydrophytes or
hydric soil conditions is generally sufficient to indicate a wetland ecosys-
tem. The boundary of the wetland is identified by changes in vegetation
structure, loss of hydrophytes, and absence of wetland soil characteris-
tics.
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