Wet Depressional Forest
Scenario model
Current ecosystem state
Select a state
Management practices/drivers
Select a transition or restoration pathway
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Transition T1A
Flooding or excess inundation on-site from beaver, roads, or other hydrological alterations within the watershed
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Transition T1B
Removal of tree canopy resulting in loss of evapotranspiration and elevated water levels.
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Transition T2A
Drainage of open water/diversion of water off-site.
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Restoration pathway R3A
Absence of disturbance (75+ years), removal of non-native species, and natural regeneration/plantings.
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Restoration pathway T3A
Flooding or inundation caused by beaver, roads, or other hydrological alterations within the watershed
More details -
No transition or restoration pathway between the selected states has been described
Target ecosystem state
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Description
Northern white cedar and yellow birch often find their primary rooting substrate on downed woody debris associated with these openings. Both species regenerate well on mossy, rotting wood (i.e., nurse logs) that have consistent moisture (Smith, 2008 Erdmann, 1990; Johnston, 1990). Eventually, initial rooting media from downed woody debris can leave roots exposed to air and result in poorly formed trees. Northern white cedar can also regenerate by vegetation reproduction. These stems usually are developed from fallen trees and root from branches that come in contact with moist rooting media and are extremely shade tolerant (Erdmann, 1990). Hummocks and micro depressions resulting from windthrown trees are an important component of the Reference State. This variability in microsites provides opportunity for obligate wetland species in ponded micro depressions and facultative or even some upland species on the drier hummocks.
Submodel
Description
The Flooded State develops as a result of dammed or blocked waterways. Flooding and more permanent forms of inundation (i.e., ponding) are caused by either beaver activity or development associated with road building. Only drainageway landforms are affected, and isolated depressions do not go through this state. Sites that have blocked water drainage from roads may become perpetual open water wetlands. In natural settings, the Flooded State can last for many years, but it ultimately depends on maintenance of high quality habitat conditions for beaver to proliferate. Once a site is abandoned, dams will gradually decline and ultimately drain, thereby beginning the transition to the Inundated State.
Beaver populations in North America were drastically reduced by broad scale fur trapping during the Colonial time period, into the 1800s (Mitsch and Gosselink, 2007). As a result, natural conversion of these sites to the Flooded State may be less common today than it was prior to European settlement.
Submodel
Description
Sites can transition to this state by relatively sudden and complete loss of the tree canopy, thereby losing the transpiration of water from trees that would normally occur later in the growing season to keep water tables at bay (i.e., drawdown; Slesak et al., 2014). This can happen as a result of intensive logging, forest pests, or general forest decline. Since water tables on these sites mimic annual rainfall graphs, the primary change in hydrology occurs later in the growing season, when overstory tree species would normally be causing drawdown in the Reference State. This state will likely become very common in this MLRA if the invasion of the exotic and completely destructive emerald ash borer beetle is not halted (Slesak et al., 2014; Palik et al., 2012). Plant community species composition will shift from primarily facultative wetland species to primarily obligate wetland species, such as lake sedge (Slesak et al., 2014).
Other than a few scattered trees, these sites do not seem to regenerate forests well. The probability of transitioning to the Reference State is largely unknown; it will probably require many decades to produce a closed canopy forest again. There is limited evidence that these communities succeed to a forested structure within a reasonable time frame (SNF, unpublished report b), but non-forested wetland conditions may persist for decades, and even centuries (Naiman et al., 2005; Terwilliger and Pastor, 1999). Viability of black ash seeds is only 8 years (Wright and Rauscher, 1990), so that initial seedbank is extirpated from the site. And since most sites are small and isolated, there may not be a reliable seed source nearby. The loss of important mycorrhizal relationships is also likely to impede succession to forest trees. It has been shown that long-term flooding kills symbiotic mycorrhizae; these fungi form essential relationships with tree species on most ecological sites, forested wetlands included, and recolonization following draining may be inhibited (Terwilliger and Pastor, 1999), which is likely the case on this ecological site as well. All of the aforementioned factors, in combination with extreme competition for light, nutrients, and growing space with fibrous rooted resident vegetation, make succession to a forested state very difficult.
Submodel
Mechanism
Flooding or excess inundation on-site from beaver, roads, or other hydrological alterations within the watershed.
Mechanism
Removal of tree canopy resulting in loss of transpiration and elevated water levels. Currently, alteration of natural hydrology is the most important driver of state change in this ecological site. Insect infestations such as emerald ash borer (Agrilus planipennis) or climate change will cause state change. Hydrology can be altered is by a clearcut of the forested canopy, which can significantly reduce the transpiration of water from the site, resulting in consistently higher water tables, and ultimately preclude forest regeneration (Mitsch and Gosselink, 2007; Palik et al., 2012; Erdmann et al., 1987). This process converts the site to non-forested shrub swamps or wet meadows. This can result from poor silvicultural practices, extreme wind events, or significant insect or disease outbreaks.
Mechanism
Drainage of open water/diversion of water off-site. Transition occurs following drainage of backed up water from beaver activity or road building. Initially, sites are wet meadows dominated by graminoids (i.e.. grasses, sedges, and rushes), eventually becoming invaded by wetland shrubs depending on level of ponding and soil saturation. These sites may have different soil characteristics depending on the extent and depth of sedimentation, which is largely dependent on how long the site was dammed (Naiman et al., 2005) and is also related to nearby land use and landscape-level soil geomorphology. More research is needed on how soil properties change following long term flooding from blocked hydrology and the potential for invasive species to establish in the Inundated State.
Mechanism
Succession/Time without major disturbance (75+ years), plantings, chemical/mechanical removal of invasive species
Model keys
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.