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A3755 Pinus contorta Swamp Forest Alliance
Type Concept Sentence: These wetlands are dominated by Pinus contorta var. contorta (along the coastal areas) or at higher elevations (var. murrayana, var. latifolia) with or without a shrub layer where soils are poorly drained mineral with organic lenses but do not form uniformly deep peat (i.e., not a bog or fen).
Common (Translated Scientific) Name: Lodgepole Pine Swamp Forest Alliance
Colloquial Name: Lodgepole Pine Swamp Forest
Hierarchy Level: Alliance
Type Concept: These wetlands are dominated by Pinus contorta var. contorta (along the coastal areas) or at higher elevations (var. murrayana, var. latifolia) with or without a shrub layer. Soils are poorly drained sites due to topographic depressions, high water table or hardpans that impede drainage. Soils are mineral with and without organic lenses, but do not form uniformly deep peat (i.e., not a bog or fen).
Diagnostic Characteristics: Diagnostic of this lowland wetland forest alliance is the dominance of Pinus contorta in the moderately dense to dense tree canopy without significant regeneration of other tree species, and the extended flooding and high water tables during the growing season.
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: Pinus contorta swamps of coastal and montane elevations.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: This alliance is characterized by a tree canopy dominated by evergreen needle-leaved trees, with cover ranging from moderately open to closed (50-80%). There is either a dense short-shrub layer, dominated by evergreen and deciduous shrubs, or an herbaceous layer dominated by graminoids. Occasional tall deciduous shrubs occur but rarely form a stratum.
Floristics: This coniferous forest alliance is characterized by a moderately closed to closed tree canopy composed primarily of Pinus contorta. Other conifers sometimes present may include Abies grandis, Abies magnifica var. shastensis, or Tsuga mertensiana. In most stands, only Pinus contorta is successfully reproducing, and cover of mature trees of the other species is low. The short-shrub layer, if present, is usually continuous and dense. Vaccinium uliginosum is the most frequent and dominant species in such a shrub layer, but other shrubs often present include Ledum glandulosum, Vaccinium cespitosum, Dasiphora fruticosa ssp. floribunda (= Pentaphylloides floribunda), Lonicera caerulea, or Spiraea douglasii. Herbaceous species are not abundant in shrubby stands. Associate species often present can include Carex angustata, Ligusticum grayi, Fragaria spp., Thalictrum occidentale, Geum macrophyllum, Maianthemum stellatum, and Trifolium longipes. In stands with no dense short-shrub layer, the herbaceous layer is typically lush and dominated by tall graminoids such as Carex obnupta. When there are no other herbaceous species reported Sphagnum spp. can be common.
Dynamics: Pinus contorta is sensitive to all but cool surface fires. Kovalchik (1987) reports that these communities dry enough during the summer to carry fires from adjacent upland areas. Most of the shrubs and herbaceous species found in this vegetation are well-adapted to regenerating following fire, therefore, there should be little change in species composition (Kovalchik 1987). High livestock use will result in a decrease in shrub cover and an increase in introduced Poa pratensis.
Environmental Description: Stands are in forested margins of meadows, and lake or forest basins (Volland 1976, Kovalchik 1987). In all cases, the sites are flat to gentle in slope (0-7%), and microtopography can vary from concave to flat to slightly undulating or hummocky. Soils are from air-laid or alluvially deposited pumice or pumice lacustrine deposits around lake margins (Volland 1976, Kovalchik 1987). Textures are coarse, ranging from fine sandy loam to coarse sands. High seasonal water tables or flooding occurs in most stands, and water table depth can vary from near the surface year-round to over 1 m in dry seasons.
The coastal Oregon examples of this alliance are found on deflation plains of sea level coastal dune systems. In these deflation plains, wind-scour has removed dune sands until the water table is reached, and moist sands are no longer scoured. Some of these deflation plains can be up to 2 km in width. The water table is near the surface year-round, but seasonal flooding can occur during the rainy winter and spring months. Soils are poorly developed from sand deposits, with coarse textures.
The coastal Oregon examples of this alliance are found on deflation plains of sea level coastal dune systems. In these deflation plains, wind-scour has removed dune sands until the water table is reached, and moist sands are no longer scoured. Some of these deflation plains can be up to 2 km in width. The water table is near the surface year-round, but seasonal flooding can occur during the rainy winter and spring months. Soils are poorly developed from sand deposits, with coarse textures.
Geographic Range: This alliance is found along the Pacific Coast between northern California and southwestern Washington, in the Sierra Nevada of California, Coast and Cascade ranges of Oregon and on the eastern side of the Cascades in the central Oregon "Pumice Zone."
Nations: US
States/Provinces: CA, ID, OR, WA
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.899807
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: GNR
Greasons: No Data Available
Concept Lineage: A.188, in part
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: >< Pinus contorta Series (Mauk and Henderson 1984)
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