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A3802 Populus deltoides ssp. wislizeni - Populus deltoides ssp. monilifera Riparian Forest Alliance

Type Concept Sentence: Vegetation within this forest alliance is characterized by Populus deltoides ssp. wislizeni- or Populus deltoides ssp. monilifera-dominated tree and shrub layers. This alliance occurs in Arizona, southeastern Utah, southwestern Colorado and New Mexico along moderately large rivers that are below 1800 m in elevation. Sites vary from point bars and other recent depositional features to alluvial terraces that may be several meters away from the channel, and several meters above the water table.


Common (Translated Scientific) Name: Rio Grande Cottonwood - Plains Cottonwood Riparian Forest Alliance

Colloquial Name: Rio Grande Cottonwood - Plains Cottonwood Riparian Forest

Hierarchy Level:  Alliance

Type Concept: Vegetation within this forest alliance is characterized by Populus deltoides ssp. wislizeni- or Populus deltoides ssp. monilifera-dominated tree layers. Canopy structure varies from a few large individuals to younger stands with high stem density. Cover may vary from sparse to dense. Other trees occasionally present include Acer negundo, Populus angustifolia, Populus x acuminata, and Salix amygdaloides. The shrub layer varies depending on the tree canopy density and other factors. Shrub associates include Artemisia tridentata ssp. tridentata, Baccharis salicifolia, Baccharis sarothroides, Ericameria nauseosa, Fallugia paradoxa, Forestiera pubescens, Gutierrezia sarothrae, Juniperus monosperma, and Juniperus scopulorum. The liana Clematis ligusticifolia may be present in some stands. The generally sparse to moderately dense herbaceous layer is dominated by graminoids, such as Distichlis spicata, Eleocharis palustris, Muhlenbergia asperifolia, and Muhlenbergia emersleyi, in relatively undisturbed stands, although introduced hay grasses are not uncommon. Forb cover is sparse except in disturbed sites, where aggressive exotic species such as Acroptilon repens or Lepidium latifolium may dominate the herbaceous stratum. This alliance occurs in Arizona, southeastern Utah, southwestern Colorado and New Mexico along moderately large rivers that are below 1800 m in elevation. Sites vary from point bars and other recent depositional features to alluvial terraces that may be several meters away from the channel, and several meters above the water table. Although this alliance is typically riparian, stands may occur at a considerable distance from rivers where water tables are relatively shallow. The alluvial soils are deep, stratified sandy loams with cobbles. Point bars within the channels are composed of fresh alluvial sands and gravels. Diagnostic of this alliance is the dominance of Populus deltoides ssp. wislizeni in the tree canopy of forests that are briefly flooded during the growing season or have relatively high water tables.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: No Data Available

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: The tree layer is dominated by tall (20-35 m in height) single-stemmed deciduous species. The canopy is overlapping, generally forming 60-100% cover. The shrub layer is also dense with up to 60% cover, and often multi-tiered, with both tall and short shrubs. The herbaceous layer is dominated by forbs with up to 20% cover. In parts of this alliance''s range, graminoid cover is primarily from introduced grass species.

Floristics: Communities within this alliance are characterized as cold-deciduous, temporarily flooded forests. The tree and shrub layers are dominated by Populus deltoides ssp. wislizeni or Populus deltoides ssp. monilifera with cover varying from 15-85% cover. Older, more mature stands will be characterized by a few large (up to 1 m diameter at breast height) trees with less canopy cover but larger basal area. Other trees occasionally present include Populus angustifolia, Populus x acuminata, Salix amygdaloides, and Salix gooddingii. In Arizona, the canopy tree may be a hybrid with Populus fremontii x Populus deltoides ssp. wislizeni. In the New Mexico stands, the understory has a shrub layer of varying cover characterized by Baccharis salicifolia (= Baccharis glutinosa), Baccharis sarothroides, Fallugia paradoxa, Forestiera pubescens (= Forestiera neomexicana), Gutierrezia sarothrae, and Juniperus monosperma. Colorado stands include scattered Artemisia tridentata ssp. tridentata and Ericameria nauseosa. The liana Clematis ligusticifolia may be present in some stands. The herbaceous layer is generally sparse to moderate, and many stands have introduced grass species. Graminoids present in relatively undisturbed stands may include Distichlis spicata, Eleocharis palustris, Muhlenbergia asperifolia, and Muhlenbergia emersleyi. Forb cover is sparse except in disturbed sites, where aggressive exotic species such as Acroptilon repens or Lepidium latifolium may dominate the herbaceous stratum.

Dynamics:  Cottonwood forests grow within an alluvial environment that is continually changing due to the ebb and flow of the river. Riparian vegetation is tolerant of, and indeed reliant on, flooding disturbance. Cottonwood communities are early-, mid- or late-seral, depending on the age class of the trees and the associated species of the stand. Mature cottonwood stands do not regenerate in place, but regenerate by germinating in different locations up or downstream. Over time, a healthy riparian area supports many stages of cottonwood communities. The process of cottonwood regeneration is well-documented. Periodic flooding events can leave sandbars of bare, mineral substrate. Cottonwood seedlings germinate and become established on newly-deposited, moist sandbars. In the absence of large floods in subsequent years, seedlings begin to trap sediment. In time, the sediment accumulates and the sandbar rises. The young forest community is then above the annual flood zone of the river channel. In this newly elevated position, with an absence of excessive browsing, fire, or agricultural conversion, this cottonwood community can grow into a mature riparian forest. At the same time, the river channel continually erodes streambanks and creates fresh, new surfaces for cottonwood establishment. This results in a dynamic patchwork of different age classes, plant associations and habitats. As cottonwoods mature, other tree species may become established. If the land surface is subject to reworking by the river, the successional processes will start over with erosion and subsequent flooding deposition. If the land surface is not subject to alluvial processes, for example on a high terrace, the cottonwoods will be replaced by upland shrub or tree species from adjacent areas.

Environmental Description:  Stands of this alliance are found primarily along riverfronts, where they develop on bare, moist soil on newly formed sandbars, front-land ridges, low streambanks, overflow areas, and well-drained flats along major streams, rivers and lake margins. Stands can also be found on abandoned fields and well-drained ridges in the first bottoms. These sites tend to be further from the main channel. Soils are formed in alluvium, are deep, medium-textured, and with adequate or excessive moisture available for vegetation during the growing season. Typically, the soil profile is highly stratified, but with distinct soil development (B) layers. Textures are predominately loose, friable sands interspersed with narrow bands of clay loams and sandy clays.

Geographic Range: This alliance occurs in Arizona, southeastern Utah, southwestern Colorado and New Mexico.

Nations: MX?,US

States/Provinces:  AZ, CO, NM, TX?, UT




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available

Type Name Database Code Classification Code
Class 1 Forest & Woodland Class C01 1
Subclass 1.B Temperate & Boreal Forest & Woodland Subclass S15 1.B
Formation 1.B.3 Temperate Flooded & Swamp Forest Formation F026 1.B.3
Division 1.B.3.Nd Western North American Interior Flooded Forest Division D013 1.B.3.Nd
Macrogroup 1.B.3.Nd.2 Interior Warm & Cool Desert Riparian Forest Macrogroup M036 1.B.3.Nd.2
Group 1.B.3.Nd.2.b Western Interior Riparian Forest & Woodland Group G797 1.B.3.Nd.2.b
Alliance A3802 Rio Grande Cottonwood - Plains Cottonwood Riparian Forest Alliance A3802 1.B.3.Nd.2.b
Association CEGL000663 Rio Grande Cottonwood / Desert-broom Flooded Forest CEGL000663 1.B.3.Nd.2.b
Association CEGL000678 Eastern Cottonwood / Scratchgrass Flooded Forest CEGL000678 1.B.3.Nd.2.b
Association CEGL002336 Rio Grande Cottonwood / Box-elder Flooded Woodland CEGL002336 1.B.3.Nd.2.b
Association CEGL002714 Rio Grande Cottonwood / Emory''s Baccharis / Alkali Sacaton Flooded Forest CEGL002714 1.B.3.Nd.2.b
Association CEGL002715 Rio Grande Cottonwood / False Quackgrass Flooded Forest CEGL002715 1.B.3.Nd.2.b
Association CEGL005964 (Rio Grande Cottonwood, Plains Cottonwood) - Goodding''s Willow Flooded Forest CEGL005964 1.B.3.Nd.2.b
Association CEGL005965 Rio Grande Cottonwood / Yerba Mansa Flooded Forest CEGL005965 1.B.3.Nd.2.b
Association CEGL005966 (Rio Grande Cottonwood, Plains Cottonwood) / Big Sagebrush Flooded Woodland CEGL005966 1.B.3.Nd.2.b
Association CEGL005967 Plains Cottonwood / Sideoats Grama Flooded Woodland CEGL005967 1.B.3.Nd.2.b
Association CEGL005968 Eastern Cottonwood / Nebraska Sedge Flooded Forest CEGL005968 1.B.3.Nd.2.b
Association CEGL005969 Eastern Cottonwood / Rubber Rabbitbrush Flooded Forest CEGL005969 1.B.3.Nd.2.b
Association CEGL005970 Eastern Cottonwood / Smooth Horsetail Flooded Forest CEGL005970 1.B.3.Nd.2.b
Association CEGL005971 (Rio Grande Cottonwood, Plains Cottonwood) / Stretchberry Flooded Forest CEGL005971 1.B.3.Nd.2.b
Association CEGL005972 Rio Grande Cottonwood / Frosted Mint Flooded Forest CEGL005972 1.B.3.Nd.2.b
Association CEGL005973 Rio Grande Cottonwood / Little Bluestem Flooded Woodland CEGL005973 1.B.3.Nd.2.b
Association CEGL005974 (Rio Grande Cottonwood, Plains Cottonwood) / Scour Flooded Woodland CEGL005974 1.B.3.Nd.2.b
Association CEGL005975 Rio Grande Cottonwood / Silver Buffaloberry Flooded Forest CEGL005975 1.B.3.Nd.2.b
Association CEGL005976 (Rio Grande Cottonwood, Plains Cottonwood) / Sparse Flooded Forest CEGL005976 1.B.3.Nd.2.b
Association CEGL005977 (Rio Grande Cottonwood, Plains Cottonwood) / Alkali Sacaton Flooded Woodland CEGL005977 1.B.3.Nd.2.b
Association CEGL005993 Rio Grande Cottonwood / Dewystem Willow Flooded Forest CEGL005993 1.B.3.Nd.2.b

Concept Lineage: A.312 ( and A.290 - carving off those associations from the west to here)

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: >< Populus-Salix wetland forest (No. 24) (Vankat 1990)
>< Cottonwood - Willow: 235 (Eyre 1980)
>< Cottonwood: 63 (Eyre 1980)
>< Eastern Broadleaf Forests: 98: Northern Floodplain Forest (Populus-Salix-Ulmus) (Küchler 1964)

Concept Author(s): G. Kittel, in Faber-Langendoen et al. (2013)

Author of Description: G. Kittel

Acknowledgements: No Data Available

Version Date: 12-18-14

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