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Add/Drop	Name	Reference	Plots↓	Description
Comm #8551	CEGL000558 » more details accession code: VB.CC.3168.CEGL000558 NOT CURRENTLY ACCEPTED	EcoArt 2002	0
Comm #8552	CEGL000560 » more details accession code: VB.CC.3170.CEGL000560 NOT CURRENTLY ACCEPTED	EcoArt 2002	0
Comm #8553	III.A.1.N.b » more details accession code: VB.CC.678.IIIA1NB	EcoArt 2002	0
Comm #8554	Alnus (incana, viridis ssp. sinuata) / Lysichiton americanus - Oenanthe sarmentosa Shrubland » more details accession code: VB.CC.19920.ALNUSINCANAVIRI	Western Ecology Working Group of...	0	This wetland association occurs only in a limited area of the central Puget Lowlands of Washington. It occurs along low-gradient or partially impounded stream systems or in impounded wetlands. Sites are seasonally flooded to permanently flooded with significant water-level fluctuation. Soils are composed of peat and muck. The deciduous tall-shrub canopy is dominated by either Alnus incana or Alnus viridis ssp. sinuata, apparently the latter more frequently. Other tall shrubs usually present are Salix spp. and Frangula purshiana, either of which can be locally codominant. The understory is usually codominated by Lysichiton americanus and one or more of the following graminoids: Carex utriculata, Carex aquatilis var. dives, Carex obnupta, Carex cusickii, and Calamagrostis canadensis. Oenanthe sarmentosa is almost always present. The combination of dominance of Alnus incana or Alnus viridis ssp. sinuata in the canopy with Lysichiton americanus and Oenanthe sarmentosa appears to be diagnostic.
Comm #8555	CEGL002063 » more details accession code: VB.CC.4608.CEGL002063 NOT CURRENTLY ACCEPTED	EcoArt 2002	0
Comm #8556	CEGL002065 » more details accession code: VB.CC.4609.CEGL002065 NOT CURRENTLY ACCEPTED	EcoArt 2002	0
Comm #8557	A.1084 » more details accession code: VB.CC.854.A1084 NOT CURRENTLY ACCEPTED	EcoArt 2002	0	Stands included in this alliance occur in alpine areas in the Washington Cascade Mountains. Elevations range from 1920-2135 m. This vegetation is found on depressions to gentle slopes with any aspect. Sites are moist areas that receive moisture from surrounding higher ground from melting snowdrifts or small streams. Some stands were found on the base of a lobe of soil formed by solifluction. Soils are poorly drained and derived from thick accumulations of pumice parent material. Mean bare ground was about 13%. Stands typically have a dense evergreen dwarf-shrub layer that is dominated by ~Phyllodoce glanduliflora$. The herbaceous layer is moderately dense to dense, and is codominated by the perennial forbs ~Oreostemma alpigenum (= Aster alpigenus), Lupinus sellulus var. lobbii$, and the perennial graminoid ~Carex spectabilis$. Other consistent species include ~Cassiope mertensiana, Potentilla flabellifolia$, and ~Antennaria lanata$. This is a relatively species-poor community.
Comm #8558	CEGL000431 » more details accession code: VB.CC.3045.CEGL000431 NOT CURRENTLY ACCEPTED	EcoArt 2002	0
Comm #8559	Chamaedaphne calyculata / Carex oligosperma / Sphagnum spp. Dwarf-shrubland » more details accession code: VB.CC.19102.CHAMAEDAPHNECAL	Midwestern Ecology Working Group...	0	This intermittent wetland shrub community is found near the western and central Great Lakes along lakeshores or in depressions. It usually occurs on sandy glacial lakeplains and outwash plains. Soils range from loamy sand and peaty sand to peaty muck and are strongly acid to very strongly acid. The water level fluctuates seasonally and from year to year. This wetland is dominated by herbs, or by herbs and shrubs. Chamaedaphne calyculata is a short shrub which is present in this community. Herbaceous species present include Carex oligosperma and Juncus spp., and in some places, Calamagrostis canadensis, Calamagrostis stricta, Eleocharis olivacea, Eleocharis robbinsii, and Phalaris arundinacea. The nonvascular layer contains some Sphagnum spp.
Comm #8560	CEGL001333 » more details accession code: VB.CC.3919.CEGL001333 NOT CURRENTLY ACCEPTED	EcoArt 2002	0