Print Report

CEGL000891 Abies concolor - Pseudotsuga menziesii / Robinia neomexicana Woodland

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: White Fir - Douglas-fir / New Mexico Locust Woodland

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: This high-elevation white fir woodland association is currently described from Grand Canyon National Park in Arizona. More survey and classification work are needed to fully characterize this type. It occurs from 2454 to 2664 m (8051-8740 feet) elevation on sideslopes, often at high levels, or on plateaus. It occurs on fairly steep slopes up to 40° (17° average) and occurs across all aspects. Soils are rapidly drained sandy loams and silt loams. This vegetation type occurs in areas which have recently burned at low to moderate severity. Codominant stands of Pinus ponderosa, Abies concolor, and Populus tremuloides characterize the tree canopy of this dry, mixed-conifer association. Abies concolor is the most frequent component of the subcanopy, and Populus tremuloides regeneration is also common. Pseudotsuga menziesii and Pinus ponderosa also occur occasionally in the subcanopy. The presence of successional or regenerating Robinia neomexicana as either a tall shrub (>2 m) or short shrub (<2 m) characterizes the shrub layer and appears to be more dominant than Populus tremuloides in areas with high volcanic ash or tuff in the substrate. The dwarf-shrub Mahonia repens is frequent at very low cover. Carex siccata is the most abundant graminoid; both Poa fendleriana and Carex rossii are frequent. Pseudostellaria jamesiana, Fragaria virginiana, and Phacelia heterophylla are the most frequent forbs. Pteridium aquilinum is fairly common.

Diagnostic Characteristics: Abies concolor and Pseudotsuga menziesii are the characteristic overstory trees. Also, Pseudotsuga menziesii regeneration is light density, while Abies concolor regeneration is abundant. The undergrowth is dominated by shrubs with 45-75% cover, Robinia neomexicana being the characteristic shrub species.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: Stuever and Hayden (1997a) identified two phases: (1) Robinia neomexicana phase which is known from the cinder cones and volcanic cinder soils in the vicinity of Springerville, Arizona. This phase has high cover of Robinia neomexicana (30-60% cover). (2) Carex siccata (= Carex foenea) phase which is known from the Jemez Caldera of northern New Mexico. This phase is characterized by the presence of Carex siccata which may have cover of up to 25%.

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

Physiognomy and Structure: No Data Available

Floristics: At Grand Canyon, codominant stands of Pinus ponderosa (up to 12% cover), Abies concolor (up to 9% cover), and Populus tremuloides (up to 15% cover) characterize the tree canopy of this dry, mixed-conifer association. Abies concolor (up to 11% cover) is the most frequent component of the subcanopy, and Populus tremuloides regeneration is also common at up to 20% cover. Pseudotsuga menziesii and Pinus ponderosa also occur occasionally in the subcanopy. The presence of successional or regenerational Robinia neomexicana characterizes the shrub layer. Robinia neomexicana is essentially always present in this community, either as a tall shrub (>2 m) or as a short shrub (<2 m). It can occur at up to 22% cover, but typically has about 11% cover. It appears to be more dominant than Populus tremuloides as a regenerational component in areas with high volcanic ash or tuff in the substrate. The dwarf-shrub Mahonia repens is frequent at very low cover. Carex siccata is the most abundant graminoid with an average of 5% cover; both Poa fendleriana and Carex rossii are frequent at about 1% cover. Pseudostellaria jamesiana, Fragaria virginiana, and Phacelia heterophylla are the most frequent forbs. Pteridium aquilinum is fairly common at about 3% cover. Seedlings of Populus tremuloides and Abies concolor occur in all 11 plots sampled. Species richness is typical for high-elevation, treed communities on the North Rim, with an average of 27 species per 400-square-meter plot.

Dynamics:  Fire history was important in the succession of this association, which may be a fire-derived or logging-stimulated seral community. Fire may kill the above-ground portion of Robinia neomexicana, but roots and rhizomes survive most fires and sucker rapidly (Pavek 1993e).

Environmental Description:  This plant association occurs on gentle slopes of cinder cones and other volcanic ash or cinder soils within elevations ranging from 2590 to 2680 m (8500-8800 feet).

At Grand Canyon, this high-elevation association occurs on the North Rim from 2454 to 2664 m (8051-8740 feet) elevation. This type tends to occur on sideslopes, often at high levels, or on plateaus. It occurs on fairly steep slopes up to 40° (17° average) and occurs across all aspects. Soils are rapidly drained sandy loams and silt loams. Stands have a high percentage of litter (typically 78%) and a relatively small percentage of wood (typically 5 to 6%) on the soil surface. This vegetation type occurs in areas which have recently burned at low to moderate severity. This association is most extensive on the eastern portion of the North Rim in the vicinity of the Saddle Mountain fire.

Geographic Range: This woodland is known from the cinder cones near Lakeside and Springerville, Arizona, and Jemez Mountains and vicinity, New Mexico. It is also found at Grand Canyon National Park in Arizona.

Nations: US

States/Provinces:  AZ, NM




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: G4Q

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Abies concolor / Robinia mexicana Habitat Type (Fitzhugh et al. 1987)
= Abies concolor / Robinia neomexicana (Stuever and Hayden 1997a) [identifies 2 phases.]

Concept Author(s): M.C. Stuever and J.S. Hayden (1997a)

Author of Description: L. Dickson and K. Christie

Acknowledgements: No Data Available

Version Date: 11-07-18

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