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Draft. A draft ecological site description is either incomplete or has not undergone quality control and quality assurance review.
Associated sites
F015XI200CA Blue Oak Woodland (DRAFT) 17-19" p.z.
Quercus douglasii/Nassella pulchra-Koelaria macrantha - R015XI101CA grades into this site in areas where soil moisture is more readily available and soils are more stable and well developed.
R015XI100CA Hills, south-facing 17-19" p.z.
Hills, south-facing 17-19" p.z. - R015XI101CA grades into this site as the slopes become less protected from sun exposure. Soil moisture and water availability is lower and temperatures are warmer.
R015XI105CA Footslopes and backslopes 17-19" p.z.
Footslopes and backslopes 17-19" p.z. - R015XI101CA grades into this site on north-facing footslopes and backslopes where soil moisture and temperatures are cooler.
Table 1. Dominant plant species
Tree Not specified
Shrub (1) Arctostaphylos glauca
(2) Arctostaphylos pungensHerbaceous (1) Nassella lepida
(2) Poa secundaPhysiographic features
This ecological site is found on hills with slopes ranging from 2 to 70% at elevations from 984 to 3362 feet, and is found primarily on north-facing slopes.
Table 2. Representative physiographic features
Landforms (1) Hill
Elevation 984 – 3362 ft Slope 2 – 75 % Aspect N, NE, NW Climatic features
The average annual precipitation in MLRA 15 is from 6 to 20 inches (150 to 510 millimeters) in the area south of San Francisco, and snowfall is rare. The north half of this area can be divided into two rainfall and snowfall zones. The southern half north of San Francisco has an average annual precipitation from 18 to 40 inches (460 to 1,015 millimeters) and snowfall is rare. In the north half, average annual precipitation is from 40 to 79 inches per year (1,015 to 2,010 millimeters) and snowfall is common. Precipitation is evenly distributed throughout fall, winter, and spring but is very low in summer. Coastal areas receive some moisture from fog in summer. Most of the rainfall occurs as low to moderate intensity, Pacific frontal storms during the winter from October to May. The average annual temperature is from 51 to 66 degrees F (10 to 19 degrees C), decreasing from south to north. The average frost-free period is 275 days (180 to 365 days), decreasing with elevation and from south to north.
At Pinnacles National Monument, the average annual precipitation is 17 inches with a range between 17 and 19 inches, mostly from rain in the winter months from November through April. The average annual air temperature is between 59 and 61 degrees Fahrenheit, and the frost-free period (>32F) is 190 to 210 days.
NOTE: Data collected for monthly precipitation and temperatures is only from one climate station.Table 3 Representative climatic features
Frost-free period (average) 210 days Freeze-free period (average) 0 days Precipitation total (average) 20 in BarLineFigure 1. Monthly precipitation range
BarLineFigure 2. Monthly average minimum and maximum temperature
">Influencing water features
Water features are not a part of this ecological site.
Soil features
The soils for this ecological site are derived from residuum weathered from rhyolite (Chalone and Highpeaks), acidic volcanic breccia (Chalone and Highpeaks), and/or granite (Backdoor - north-facing).
Rhyolitic breccia makes up a significant proportion of the soil parent materials for this site, which includes the Pinnacles rock formations from which the park derives its name. Breccia consists of welded fragments of hard, fine-grained, acidic volcanic rock and is typically low in plant nutrients. The Highpeaks series is a shallow soil on steep to very steep convex hillslopes where they are often shaded, conserving moisture; however, the water storage capacity of these soils is very low. The Chalone soils are also derived from rhyolitic breccia but are moderately deep to bedrock. Because the breccia is highly resistant to weathering, pedogenic clay accumulations is slow to occur, resulting in soils that have slightly decomposed plant materials on the surface, a thin darkened gravelly sandy loam mineral surface horizon, and a pale extremely gravelly sandy clay loam subsoil over hard bedrock. When these soils are saturated, most storm water runs off resulting in erosion which keeps the Highpeaks soil shallow and the surface horizon of the Chalone soil thin. However, unlike the soils found under chamise chaparral, these soils have slightly higher soil fertility and organic matter, primarily due to their northerly aspects that cause lower evapotranspiration rates and a thicker litter layer provided by a larger variety of chaparral species.
Granite, although it underlies most of the monument, is only expressed in certain areas of the Monument because of the presence of other overlying materials. Granite is exposed primarily along the southern part of Chalone Creek and at the west entrance to the Monument. The Backdoor series (north-facing) is a moderately deep soil on very steep north-facing hills where they are also often shaded, conserving moisture and reducing evapotranspiration rates. Because the Backdoor series is composed of granite, a coarse-grained, acidic intrusive igneous rock, the soils weather to a deep profile with low nutrient status. These soils allow winter rainfall to percolate through the profile, transporting clay particles into the subsurface horizons and increasing soil moisture levels throughout the root zone. These processes result in a soil that has a dark loam surface (due to substantial litter accumulations and decomposition) over a gravelly clay loam subsoil which in turn overlies extremely gravelly loamy coarse sand underlying material to a depth of more than 60 inches.
This ecological site occurs on the following soil components in the Pinnacles National Monument soil survey.
SSA MU Symbol Component name
CA069 105 Chalone
CA069 109 Highpeaks
CA069 111 Backdoor
CA069 127 Chalone
CA069 138 Highpeaks
CA069 138 Chalone
CA069 139 Highpeaks
CA069 139 Chalone
CA069 155 Chalone
CA069 156 ChaloneTable 4. Representative soil features
Surface texture (1) Gravelly loam
(2) Sandy loam
(3) Very gravelly loamy coarse sand
Family particle size (1) Sandy
Drainage class Well drained Permeability class Moderately slow to moderate Soil depth 8 – 80 in Surface fragment cover <=3" 0 – 55 % Surface fragment cover >3" 3 – 45 % Available water capacity
(0-40in)0.8 – 4.6 in Electrical conductivity
(0-40in)0 – 2 mmhos/cm Sodium adsorption ratio
(0-40in)0 – 2 Soil reaction (1:1 water)
(0-40in)5 – 7.7 Subsurface fragment volume <=3"
(Depth not specified)5 – 80 % Subsurface fragment volume >3"
(Depth not specified)5 – 25 % Ecological dynamics
Before European settlement, the natural plant communities for this ecological site ranged from manzanita-dominated chaparral to scrub oak-dominated chaparral with sparse understories of native perennial and annual grasses and forbs (also commonly known as mixed chaparral) to a mixed chaparral-grassland dominated community (post-fire). The reference state for this ecological site is similar to its pre-European state; however the density of the chaparral species may be different due to fire suppression and the understory species are now commonly dominated by annual grasses and forbs. Primary species include oats (Avena spp.), bromes (Bromus spp.), annual fescues (Vulpia spp.), miner’s lettuce (Claytonia spp.), shooting-star (Dodecethon spp.), catsear (Hypochaeris spp.), clarkia (Clarkia spp.) and lotus (Lotus spp.). These two plant communities can be found all through this ecological site, however the manzanita-dominated plant community is more prevalent and visible throughout Pinnacles National Monument.
The reference state for this ecological site is a numerous mixture of common chaparral species, however the dominant species include bigberry manzanita (Arctostaphylos glauca), pointleaf manzanita (Arctostaphylos pungens), buckbrush (Ceanothus cuneatus), toyon (Heteromeles arbutifolia), scrub oak (Quercus berberdifolia), and the shrubby interior live oak (Quercus wislizeni var. frutescens), with lesser dominants including birchleaf mountain mahogany (Cercocarpus betuloides var. betuloides), coffeeberry (Rhamnus ilicifolia), hollyleaf cherry (Prunus ilicifolia), California ash (Fraxinus dipetala), gooseberry and current (Ribes spp.), chamise (Adenostoma fasciculatum), California buckwheat (Eriogonum fasciculatum), man-root (Marah fabaceus), foothill pine (Pinus sabiniana) and an understory composed of native and annual grasses and forbs. Other species that can be found throughout this ecological site include; poison oak (Toxicodendron diversilobum), California buckeye (Aesculus californica), monkeyflower (Mimulus spp.), penstemon (Penstemon spp.), honeysuckle (Lonicera spp.), dodder (Cuscuta spp.), phacelias (Phacelia spp.), wooly bluecurls (Trichostema lanatum), larkspur (Delphinium spp.), bedstraw (Galium spp.), catsears (Hypochaeris spp.), bluegrass (Poa spp.), foothill needlegrass (Nassella lepida), silver hairgrass (Aira caryophyllea), ripgut brome (Bromus diandrus), soft brome (Bromus hordeaceus), oats (Avena spp.), rabbitfootgrass (Polypogon monspeliensis), rat-tail fescue (Vulpia myuros), and goldback fern (Pentagramma triangularis).
Next to chamise, mixed chaparral is the most dominant and widely known plant community throughout much of California’s mid-elevational ranges. It is comprised of dense stands of shrubs that are all structurally similar with deep roots and evergreen, sclerophyllous leaves. Depending on the combined influences of disturbance, elevation, aspect and soils, the mix of species within the mixed chaparral habitat will vary. Although soil and parent material have some influence on the variety of species, microclimatic differences in soil moisture, temperature, and aspect often dictate what species will be most dominant in a given location (England 2006 and Fried et al 2004).
At Pinnacles National Monument the mixed chaparral varies primarily due to the strongly sloping north-aspects, which allow for better moisture conservation and cooler temperatures. The upper-most portions of the hills, which are generally more exposed to the sun, are dominated primarily by manzanitas, buckbrush, and chamise. These portions of the slope have higher evapotranspiration rates, lower soil moisture, and often times erode more readily, making the soils more conducive to species that are drought tolerant. Whereas at mid-slope, there is a much greater diversity of many of the species listed for this site, and in the concave depressions where water drains and temperatures stay cooler, there is a much higher dominance of toyon, birchleaf mountain mahogany, and hollyleaf cherry. As the mixed chaparral nears the bottom of the slope it grades into the hollyleaf cherry-dominated ecological site (R015XI105CA-Footslopes and backslopes 17-19” p.z.). In the canyons, the mixed chaparral will be dominated more heavily by scrub oak and the shrubby interior live oak and will begin to grade into the blue oak woodlands (F015XI200CA-Quercus douglasii/Nassella pulchra-Koelaria marcrantha 17-19” p.z.). Foothill pine is found scattered throughout this site, most often in the drainageways or fractured bedrock among the Pinnacles and rock outcroppings where water is readily available.
The primary elements that maintain this ecological site are drought and fire. Chaparral species are physiologically adapted to droughty conditions and many are also well-adapted to fire. Some of these adaptations include: extensive rooting systems (taking advantage of water near the soil surface as well as water far into the soil profile); sclerophyllous leaves; specialized stomates; the shape of the canopies (dissipates radiation by convection); the height of the shrubs (keeping the leaves away from the hot soil surface); post-fire crown sprouting; and seeds that often require high temperatures before germination (Fried et al 2004).
Along with fires and the droughty conditions, erosion also plays a significant role in maintaining this site. The site is located primarily on steep slopes with soils that are highly susceptible to surface erosion. Chaparral provides these slopes with substantial ground cover, helping dissipate raindrop impact on the soil surface as well as protecting the surface from strong winds. The extensive rooting structures of chaparral shrubs also help anchor the soils, binding soil particles and slowing the flow of subsurface water. Due to the properties of the soil, the shrubs are only able to minimize the erosion and therefore the top surface is constantly being removed and deposited downslope. This constant disturbance keeps the surface horizon thin, and weakly developed, which is most likely one of the reasons higher seral species, such as blue oak, are not found in high densities in this site.
The successional patterns of chaparral begin and end with fire. Chaparral can develop into extremely dense, sometimes impenetrable stands and many of the shrubs become senescent, requiring a fire to clear out the dead branches and heavy litter, recharge the soil’s available nitrogen and carbon, and stimulate new growth and seed germination. Most of the dominant chaparral species are able to rapidly recover and grow after a fire. Bigberry manzanita, for example, is killed by fire but is an obligate post-fire seeder, requiring high-intensity fires to crack the seedcoats; whereas toyon is relatively non-flammable and will sprout vigorously from dormant buds located on the root crown after a fire (Howard 1993 and McMurray 1990). Post-fire chaparral on north-facing slopes exhibit higher species richness, higher species turnover rates, and faster vegetation recovery in terms of biomass accumulation and return to pre-fire species composition than chaparral communities found on the drier, south-facing slopes (Guo 2001).
The historical fire regime for these mixed chaparral communities is difficult to determine prior to European settlers arrival, however there are indications of a fire-return interval somewhere between 50-100 years, with lightning being the primary ignition source (Fried et al 2004 and Keeley et al 1986).
Chaparral is important habitat for many species of birds, reptiles, rodents and mammals. Some deep-habitat dwellers rely almost entirely on chaparral for food, shelter, and reproduction sites, whereas others occupy the ecotonal zones between the chaparral and woodland, chaparral and grassland or chaparral and riparian habitats to satisfy their various needs. As the chaparral becomes more and more dense, it becomes too dense for many of these species to properly utilize the habitat and thus fires are necessary to open up the canopy, which provides better movement through the site. It also stimulates new growth of the shrubs as well as the understory herbaceous species, providing more food and shelter for a greater variety of species.State and transition model
Custom diagramStandard diagram
Figure 3. Upper, north-facing slopes
More interactive model formats are also available. View Interactive Models
More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective textEcosystem states
State 1 submodel, plant communities
State 2 submodel, plant communities
State 1
Upper slopesCommunity 1.1
Upper slopesThis plant community is the reference community for this ecological site and is dominated by Arctostaphylos glauca, A. pungens, and Ceanothus cuneatus.
State 2
Canyon slopesCommunity 2.1
Canyon slopesScrub oak and shrubby interior live oak are more dominant on these strongly sloping areas on the north-facing canyons on the east side of Pinnacles National Monument.
Additional community tables
Table 5. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 6. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Animal community
Wildlife species found in this habitat type are also found in mixed chaparral, coastal scrub, and in the shrubs beneath many woodland and forestland types.
Over seventy species of mammals occur in these habitats, with five endemic and near-endemic species– the giant kangaroo rat (Dipodomys ingens), Heermann kangaroo rat (Dipodomys heermani), Santa Cruz kangaroo rat (Dipodomys venustus), Sonoma chipmunk (Eutamias sonomae), and the Suisun shrew (Sorex sinuosus).
Among the 100 species of birds that occur in this ecoregion, scrub jays (Aphelocoma coerulescens), acorn woodpeckers (Melanerpes formicivorus), and wrentits (Chamaea fasciata), are a few of the most characteristic species.
Army ants (Neivamyrmex spp.) and primitive bristletails, and land snails are among the ecoregion’s large number of relict and unusual invertebrate species.
Many species and communities within the ecoregion are adapted to periodic fires, indeed many species depend upon fires for regeneration. An entire guild of annual herbaceous plants that occur in chamise chaparral have seeds that lie dormant for long periods until fires trigger their germination approximately every 20-25 years.Supporting information
Inventory data references
MIXED-01 - % & lbs. MIXED-02 - % & lbs. MIXED-03 - % & lbs. CEBE-01. - %
Other references
Fried, J.S., C.L. Bolsinger, and D. Beardsley. 2004. Chaparral in Southern and Central Coastal California in the Mid-1990’s: Area, Ownership, Condition, and Change. United States Department of Agriculture, Forest Service. Resource Bulletin, PNW-RB-240.
Guo, Q. 2001. Early post-fire succession in California chaparral: Changes in diversity, density, cover and biomass. Ecological Research. 16: 471-485 pp.
Howard, J.L. 1993. Arctostaphylos glauca. In: Fire Effects Information System, [Online]. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory (Producer). Available: http://www.fs.fed.us/database/feis/ [2006, October 13].
Keeley, J.E., P.H. Zedler, C.A. Zammit, T.J. Stohlgren. 1986. Fire and demography. In: The California chaparral—paradigms reexamined. Proceedings of the symposium. Science Series 34. Los Angeles, CA: Natural History Museum of Los Angeles County: 151-153.
Keeley, J.E. and C.J. Fotheringham. 2001. Historic Fire Regime in Southern California Shrublands. Conservation Biology. 15: 1536-1548 pp.
Keeley, J.E., C.J. Fotheringham, and M. Morais. 1999. Reexamining Fire Suppression Impacts on Brushland Fire Regimes. Science. 284: 1829-1832.
Mayer, K.E. and W.F. Laudenslayer Jr. 1988. A Guide to Wildlife Habitats of California.
State of California, Resources Agency, Department of Fish and Game. Sacramento, CA. 166 pp.
McMurray, N.E. 1990. Heteromeles arbutifolia. In: Fire Effects Information System, [Online]. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory (Producer). Available: http://www.fs.fed.us/database/feis/ [2006, October 13].
McMurray, N.E. 1990. Prunus ilicifolia. In: Fire Effects Information System, [Online]. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory (Producer). Available: http://www.fs.fed.us/database/feis/ [2006, October 13].
Meentemeyer, R.K., A. Moody, and J. Franklin. 2001. Landscape-scale patterns of shrub species abundance in California chaparral: the role of topographically mediated resource gradients. Plant Ecology. 156:19-41 pp.Contributors
K. Moseley
Rangeland health reference sheet
Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.
Author(s)/participant(s) Contact for lead author Date Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
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Number and extent of rills:
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Presence of water flow patterns:
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Number and height of erosional pedestals or terracettes:
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Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
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Number of gullies and erosion associated with gullies:
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Extent of wind scoured, blowouts and/or depositional areas:
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Amount of litter movement (describe size and distance expected to travel):
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Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
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Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
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Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
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Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
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Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
Sub-dominant:
Other:
Additional:
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Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
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Average percent litter cover (%) and depth ( in):
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Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
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Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
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Perennial plant reproductive capability:
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