Print Report
A3575 Juniperus monosperma Wooded Grassland Alliance
Type Concept Sentence: This juniper woodland and savanna alliance is characterized by an open to moderately dense, short (<15 m) tree canopy and is strongly dominated by Juniperus monosperma or Juniperus scopulorum at higher elevations with an understory dominated by an open to dense layer of perennial grasses and lacking significant cover of shrubs. It occurs on warm, dry mountains and foothills in southern Colorado east of the Continental Divide and in mountains and plateaus of northern and central New Mexico, extending east on breaks in the southeastern Great Plains.
Common (Translated Scientific) Name: One-seed Juniper Wooded Grassland Alliance
Colloquial Name: One-seed Juniper Wooded Grassland
Hierarchy Level: Alliance
Type Concept: This woodland and savanna alliance is characterized by diagnostic tree species Juniperus monosperma that forms a very open to moderately dense tree layer. At higher elevations and relatively mesic sites, such as along drainages, Juniperus scopulorum may be present and sometimes dominant. In southern transitional areas with ~Madrean Pinyon - Juniper Woodland Group (G200)$$ in central New Mexico, Juniperus deppeana may be present but not dominant. Other conifers, including Pinus edulis, are absent or accidental with very low cover. Scattered shrubs and dwarf-shrubs may be present but do not form a layer. The understory is characterized by an moderate to dense herbaceous layer composed of grasses often with diverse, but low cover of forbs. Characteristic species may include Achnatherum hymenoides, Achnatherum nelsonii, Achnatherum scribneri, Andropogon hallii, Achnatherum hymenoides, Bouteloua eriopoda, Bouteloua gracilis, Bouteloua hirsuta, Hesperostipa comata, Hesperostipa neomexicana, Pleuraphis jamesii, and Schizachyrium scoparium. This alliance occurs on warm, dry mountains and foothills in southern Colorado east of the Continental Divide and in mountains and plateaus of northern and central New Mexico, extending east on breaks in the southeastern Great Plains. Stands occur on nearly level surfaces to steep, rocky slopes in canyons, on hillsides, and on mesatops, but also occur on stream terraces and on deep sands. Elevations range from 1200-2100 m. Aspect does not seem important except in elevational extremes for a given latitude. Sites are typically dry with shallow, rocky, calcareous, alkaline soils. Soil textures range from sandy loam to clay soils typically derived from limestone, sandstone or shale.
Diagnostic Characteristics: This woodland alliance is found in foothills in southern Colorado east of the Continental Divide and in mountains and plateaus of northern and central New Mexico, extending east on breaks in the southeastern Great Plains. These woodlands are characterized by diagnostic tree species Juniperus monosperma that forms an open to dense tree layer. At higher elevations and relatively mesic sites, Juniperus scopulorum may be present and sometimes dominant. In southern transitional areas with ~Madrean Pinyon-Juniper Woodland Group (G200)$$ in central New Mexico, Juniperus deppeana may be present but not dominant. Other conifers, including Pinus edulis, are absent or accidental with very low cover. The understory is characterized by a moderate to dense herbaceous layer composed of grasses often with a diverse but low cover of forbs.
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: In northwestern New Mexico, the distributional ranges of Juniperus monosperma and Juniperus osteosperma overlap. This alliance does not occur within the range of Juniperus osteosperma in this transition zone from the southern Rocky Mountain juniper woodland and savanna alliances to the Colorado Plateau juniper woodland and savanna alliances.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: Vegetation included in this alliance has a sparse to moderately dense (5-45% cover) tree canopy that is typically 2-10 m tall. Stands are solely dominated by scale-leaved evergreen trees. Broad-leaved and needle-leaved evergreen trees may be present but have low cover (<5%). A sparse to moderate layer that is dominated by perennial graminoids is usually present. Perennial forbs may be scattered. Annual forbs and grasses may be seasonally present. Scattered shrubs may be present with low cover (<10%) and less cover than the herbaceous layer. Cacti and stem succulents are often present.
Floristics: This woodland and savanna alliance is characterized by diagnostic tree species Juniperus monosperma that forms a very open to moderately dense tree layer. At higher elevations and relatively mesic sites, such as along drainages, Juniperus scopulorum may be present and sometimes dominant. In southern transitional areas with ~Madrean Pinyon - Juniper Woodland Group (G200)$$ in central New Mexico, Juniperus deppeana may be present but not dominant. Other conifers, including Pinus edulis, are absent or accidental with very low cover. Scattered shrubs and dwarf-shrubs may be present but do not form a layer. The understory is characterized by an moderate to dense herbaceous layer composed of grasses often with diverse but low cover of forbs. Characteristic graminoids may include Achnatherum hymenoides, Achnatherum nelsonii, Achnatherum scribneri, Achnatherum hymenoides, Aristida spp., Bouteloua eriopoda, Bouteloua gracilis, Bouteloua hirsuta, Hesperostipa comata, Hesperostipa neomexicana, Muhlenbergia spp., Piptatheropsis micrantha (= Piptatherum micranthum), Pleuraphis jamesii, Schizachyrium scoparium, Sporobolus spp., and Andropogon hallii in rare, deep sands habitats. Many forb species can occur, but few have much cover. Commonly present forbs include species of Artemisia, Dalea, Eriogonum, Heterotheca, Hymenoxys, Mirabilis, Penstemon, Phlox, Physalis, Pediomelum (= Psoralea), and Zinnia. Annual grasses and forbs are seasonally present.
Dynamics: Juniperus monosperma is extremely drought-tolerant. It is also non-sprouting and may be killed by fire (Wright et al. 1979). The effect of fire on a stand is largely dependent on the tree height and density, fine fuel load on the ground, weather conditions, and season (Dwyer and Pieper 1967, Wright et al. 1979). Trees are more vulnerable in open stands where fires frequently occur in the spring, when the relative humidity is low, wind speeds are over 10-20 mph, and there is adequate fine fuels to carry fire (Wright et al. 1979, Fischer and Bradley 1987). Under other conditions, burns tend to be spotty with low tree mortality. Large trees are generally not killed unless fine fuels, such as tumbleweeds, have accumulated beneath the tree to provide ladder fuels for the fire to reach the crown. Closed-canopy stands rarely burn because they typically do not have enough understory or wind to carry a fire. Altered fire regimes, cutting trees for fencing, and improper grazing by livestock have significant impacts on the quality of sites. Grazing by livestock can modify the fire regime by removing the fine fuels that carry fire. Juniperus monosperma invasion into grasslands has occurred in places. Control efforts by chaining and prescribed burning have mixed results. More study is needed to understand and manage these woodlands ecologically.
Environmental Description: Stands included in this woodland alliance occur from eastern Arizona to western Texas and the Panhandle of Oklahoma and in the foothills in the southern Rocky Mountains. Stands also occur in the mountains, mesas, plateaus, piedmonts, canyons, escarpments, and other geographic breaks in the southern Great Plains. Elevations range from 1200-2100 m. Climate is semi-arid with drought not uncommon. Summers are generally hot, and winters have cold periods and occasional snows with extended periods of freezing temperatures. The mean annual precipitation ranges from 30-48 cm. Stands occur on nearly level surfaces to steep, rocky slopes in canyons, on hillsides, and on mesatops, but also occur on stream terraces and on deep sands. Aspect does not seem important except in elevational extremes for a given latitude. Low-elevation stands are restricted to the more mesic north slopes, whereas high-elevation stands occur on south aspects. Sites are typically dry with shallow, rocky, calcareous, alkaline soils. Soil textures range from sandy loam to clay soils typically derived from limestone, sandstone or shale. Other parent materials include basalt, granite, dolomite, siltstone and mixed alluvium.
Geographic Range: This woodland alliance occurs in foothills in southern Colorado east of the Continental Divide and in mountains and plateaus of northern and central New Mexico, extending east on breaks in the southeastern Great Plains.
Nations: US
States/Provinces: AZ, CO, NM, OK, TX
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.899633
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: GNR
Greasons: No Data Available
Concept Lineage: This alliance is composed of 6 herbaceous understory associations from Old Alliance II.A.4.N.a. Juniperus monosperma Woodland Alliance (A.504).
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: < Juniperus monosperma woodland alliance (Hoagland 1998a)
< Oneseed Juniper Series (Dick-Peddie 1993) [includes all the Juniperus monosperma stands]
< Oneseed Juniper Series (Dick-Peddie 1993) [includes all the Juniperus monosperma stands]
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