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Draft. A draft ecological site description is either incomplete or has not undergone quality control and quality assurance review.
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R019XD052CA Moist Inland Chaparral 16-18" p.z.
Moist Inland Chaparral 16-20" p.z. is located on inland hills and is dominated by hairy-leaf ceanothus and chamise.
R019XD050CA Dry Inland Chaparral 16-20" p.z.
Dry Inland Chaparral 16-20" p.z. is located on inland hills, dominated by chamise and hairy-leaf ceanothus.
Table 1. Dominant plant species
Tree Not specified
Shrub (1) Adenostoma fasciculatum
(2) Ceanothus megacarpusHerbaceous (1) Salvia mellifera
(2) Eriogonum fasciculatumPhysiographic features
This site is located on ridges, hills and mountains with southerly slopes predominating. Slopes range from 15 to 75%, but gradients of 15 to 50% are most typical. Elevations are from 390 to 2950 feet.
Table 2. Representative physiographic features
Landforms (1) Ridge
(2) Hill
(3) Mountain
Flooding frequency None Ponding frequency None Elevation 390 – 2950 ft Slope 15 – 75 % Aspect SE, S, SW Climatic features
This site receives slightly more annual rainfall than the more coastal sites due to movement of hot and cold air masses and pressure systems influenced by the ocean and surrounding mountains. Roughly 94% of yearly precipitation falls form November through April. The driest months are June, July and August, with those months historically receiving trace amounts of rainfall. The average annual precipitation ranges from 18 to 24 inches. The mean annual air temperature ranges from 60 to 64 degrees F.
There are no reliable climate stations for this specific ecological site. The two stations listed (Oxnard and Los Angeles Civic Center) are on the extreme northwest and southwest of the area.
Table 3 Representative climatic features
Frost-free period (average) 350 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
This site is not influenced by wetland or riparian water features.
Soil features
This ecological site is associated with the Talepop, Sumiwawa, and Hipuk soil series. These soils are all shallow, well to excessively drained soils, derived from colluvium and residuum from soft sandtone or fractured meta-volcanic rock (Talepop). The Talepop soil has a gravelly loam surface and subsurface texture. Highly fractured meta-volcanic rock is encountered between 5 and 14 inches. This bedrock has fractures 1 to 3 inches apart, and with about 10 to 15 percent soil in fractures with a few roots. The Sumiwawa soil has a gravelly loamy sand surface and subsurface texture to 9.5 inches. From 9.5 to 13 inches is a loamy sand, with soft sandtstone bedrock between 13 to 22 inches. Below 22 inches is hard sandtone bedrock. The Hipuk soil has gravelly sandy loam surface texture in the upper inch, with a
sandy loam texture from 1 to 4 inches. Between 4 and 8 inches is a sandy clay loam, and from 8 to 18 inches is a gravelly sandy clay loam. Fractured sandstone bedrock is encountered between 18 to 24 inches, and hard sandstone bedrock is below 24 inches.
The Talepop soils are classified as Loamy, mixed, superactive, thermic, shallow Typic Argixerolls, the Sumiwawa soils are Mixed, thermic, shallow Typic Xeropsamments, and the Hipuk soils are Loamy, mixed, superactive, thermic, shallow Typic Haploxeralfs.
This ecological site has been correlated with the following mapinits and soil components within the Santa Monica Mountain Soil Survey Area (CA692):
Map unit Component Percent
175 Talepop 15
176 Talepop 15
177 Talepop 15
178 Talepop 35
230 Talepop 15
231 Talepop 50
302 Sumiwawa 15
303 Sumiwawa 15
470 Hipuk 30
470 Sumiwawa 40
472 Hipuk 15
472 Sumiwawa 30
Table 4. Representative soil features
Surface texture (1) Gravelly loam
(2) Gravelly loamy sand
(3) Gravelly sandy loam
Family particle size (1) Loamy
Drainage class Well drained to somewhat excessively drained Permeability class Moderately slow to rapid Soil depth 4 – 40 in Surface fragment cover <=3" 5 – 40 % Surface fragment cover >3" 2 – 10 % Available water capacity
(0-40in)0.47 – 2.45 in Soil reaction (1:1 water)
(0-40in)5.6 – 7.3 Subsurface fragment volume <=3"
(Depth not specified)10 – 35 % Subsurface fragment volume >3"
(Depth not specified)2 – 30 % Ecological dynamics
This ecological site is dominated by chamise (Adenostoma fasciculatum), with black sage (Salvia mellifera), bigpod ceanothus (Ceanothus megacarpus), and Eastern Mojave buckwheat (Eriogonum fasciculatum). Chamise is commonly found on the driest zone within the chaparral communities on shallow soils and southern exposures. This site is found with the Dry Chaparral Ecological Site (R020XD038CA). The Dry Chaparral Ecological Site is dominated by redshank (Adenostoma sparsifolium) and bigpod ceanothus (Ceanothus megacarpus), and has deeper soils.
This mixed chaparral community is comprised of dense stands of shrubs that are all structurally similar, with 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.
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. Some reports suggest that chaparral species have different rooting depths, which allow them to utilize different zones within the soil to reduce competition. Chamise generally develops several deep tap roots, which are able to penetrate 10 to 12 feet into fractured bedrock. It also produces lateral roots from the lignotuber (McMurray, 1990). It is also possible that mycorrhizal associations may enhance the ability of chamise to reach water and mineral nutrients.
The successional patterns of chaparral are initiated by fire. The time between fires plays an important role in the chaparral system. Old growth chaparral is a natural and healthy community, but it is becoming rare due to an increased fire frequency (Halsey, 2005). Until recently it was commonly perceived that chaparral needs to burn in order to maintain its vigor and heath. Many chaparral shrub species can live for more than 100 years without becoming decadent, and with out affecting their ability to regenerate after a fire (Keeley et al, 2005). Chaparral can develop into extremely dense, sometimes impenetrable stands of dead branches and heavy litter, however these shrub can self thin over time. Fire can be detrimental to chaparral communities if it becomes too frequent; however with longer fire intervals fire is beneficial. When fire burns through chaparral it recharges 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. Chamise (Adenostoma fasciculatum) and bigpod ceanothus (Ceanothus megacarpus) produce large amounts of seed that accumulate over the years and lie dormant in the soil until a fire stratifies the seed coat for germination. Bigpod ceanothus is an obligate seeder while chamise (Adenostoma fasciculatum) resprouts vigorously after fire. Black sage is smaller shrub or sub shrub. It can resprout after low intensity fires, but it often killed by high intensity fires associated with this chaparral community. Black sage stores dormant seeds in the soil, which need light and charred wood leachate in order to germinate. Black sage may produce allelopathic compounds that may inhibit growth of other plants (McMurray, 1990). The other common shrub associated with this site is Eastern Mojave buckwheat (Eriogonum fasciculatum). This buckwheat is a large sub-shrub or small shrub, and it is intermixed with and looks somewhat similar to chamise. It does not resprout well after fire, but reproduces from seed (Montalvo). 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 that was probably greater than 70 years, with lightning being the primary ignition source (Keeley and Fotheringham 2001). Fire intervals may have been up to 200 years along the coast, but have generally increased to 40-50 year intervals with the increase in human caused fires.
The chaparral in this area grows mostly in spring from Feb to June, becoming mostly dormant in the summer months. During the summer months they are more susceptible to fire.
State and transition model
Custom diagramStandard diagram
Figure 3. Shallow Chaparral Model
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 3 submodel, plant communities
State 4 submodel, plant communities
State 5 submodel, plant communities
State 1
1.1 Chamise ChaparralCommunity 1.1
1.1 Chamise ChaparralThis chaparral community is dominated by chamise (Adenostoma fasciculatum). Other common plants are bigpod ceanothus (Ceanothus megacarpus), California brittlebush (Encelia californica), Eastern Mojave buckwheat (Eriogonum fasciculatum), purple needlegrass (Nassella pulchra), sugar sumac (Rhus ovata), San Luis purple sage (Salvia leucophylla), black sage (Salvia mellifera), and chaparral yucca (Yucca whipplei).
The fire frequency and season of burn may affect the species composition. More frequent fires may favor bigpod ceaonthus. Fires in spring and summer have a higher mortality rate for chamise than in fall. This is because the carbohydrate storage in the lignotuber has been depleted due to the spring growth, and is replenished during the summer. Therefore by fall there is sufficient carbohydrate storage in the lignotubers to produce new shoots after a fire (McMurray, 1990). If fire does not burn through this area, bigpod ceanothus may start to decline in cover because it is an obligate seeder after fire. Some studies suggest that fires used to be in the summer months and would burn slowly in relatively small areas. Only occasionally would these fires last until fall and be fanned by the Santa Anna winds, which cause the fires to race across the mountains burning thousands of hectares a day (Keeley and Fotheringham, 2001).
When fire does occur in this chaparral community, it usually burns the canopy of the entire stand, following pathway 1.1a in the state and transition model, which leads to stand regeneration (Community 1.2).Figure 4. Annual production by plant type (representative values) or group (midpoint values)
State 2
1.2 Native perennial and herbaceous speciesCommunity 2.1
1.2 Native perennial and herbaceous speciesThis community is dominated by native forbs and grasses, along with resprouting shrubs and shrub seedlings. This phase is short lived because the shrubs rapidly regain dominance in a couple of years. In the first year after a fire thousands of chamise, bigpod ceanothus, black sage and Eastern Mojave buckwheat seedlings will be present. Many of these die by the second year. Chamise and black sage increase in cover from the new shoots sprouting from the surviving lignotubers.
There are several annual and perennial fire followers that may be present at this stage. Many of these species have stored dormant seeds in the soil, which will not germinate until heat from the fire, sunlight from the removal of the canopy, or nitrogen from the charred wood leachate cue germination. Some common fire followers are whisperingbells (Emmenanthe penduliflora), largeflower phacelia (Phacelia grandiflora), black sage (Salvia mellifera), yellow bleeding heart (Ehrendorferia ochroleuca formerly Dicentra ochroleuca), bush poppy (Dendromecon rigida), Coulter's snapdragon (Sairocarpus coulterianus formerly Antirrhinum coulterianum), golden eardrops (Ehrendorferia chrysantha formerly Dicentra chrysantha), western poppy (Papaver californicum), and windpoppy (Stylomecon heterophylla) (Thanos and Rundel, 1995; Dagit, 2002). Many of these fire followers are only present the first year or two after a fire.
The primary pathway for this community is 1.2a to the young chaparral community. Pathway 1.2b is uncommon, but could happen with a quick recovery of the shrubs.State 3
1.3 Young mixed chaparralCommunity 3.1
1.3 Young mixed chaparralThis community is a young mixed chaparral community still in the growth phase following a fire. The young shrubs are beginning to shade out the understory and are beginning the self thinning process. Black sage may be dominant at this time, before the chamise and bigpod ceanothus regain their height and dominance over the smaller shrubs.
The primary pathway for this community is 1.3a to continue with the growth and development of the shrub species. This phase may last from 2 to 30 years, before regaining its potential cover and composition.
If fire burns this community during this stage (initiating pathway 1.3b) it will return to the regeneration phase.State 4
State 2Community 4.1
State 2This state develops with an altered fire regime and/or with the introduction of non-native plant species. Increased fire frequencies and low intensity fires can be detrimental to chaparral and woodland regeneration. This altered state has similar plant communities to the reference state, but non-native species, particularly the annual grasses, such as oats (Avena spp.) and bromes (Bromus spp.) are present. The overall cover of the chaparral and woodland species has declined, with more openings in the canopy. Subshrubs such as black sage and buckwheats may increase in cover It is difficult to determine the effect on the chaparral species compositon during this state, but some species may be better adapted to shorter fire intervals than others.
Non-native species are often introduced after a fire or other disturbances such as grazing road building, or foot traffic. The non-native grasses can increase fire frequency because the grasses create an easily flammable and continuous fuel source. Frequent fire may cause a transition to state 3 (T2a) .
Once the non-native species become established it is extremely difficult to eliminate them from the area. Restoration efforts should focus on eliminating non-native species, and if possible keep the fire return interval to greater than 70 years (R2a).
State 5
State 3Community 5.1
State 3When fire repeatedly burns through a chaparral community, before the species reach maturity, the presence of the chaparral species may decline. Since most of the dormant seeds in the seed bank germinate the first year after a fire, there are very few seeds left to germinate after subsequent fires. Time without disturbance is needed for the shrubs to mature and produce seeds. Frequent fires also affect the ability for the resprouting shrubs to send up new shoots by depleting the carbohydrate storage in the root systems. In the absence of shrub seedlings and resprouting lignotubers, non-native annual grasses become dominate and self-perpetuate the frequent fire cycle. The minimal amount of time needed for the chaparral species to recover is not known, but some reports say that 20 to 40 years may be too short.
Non-native species listed by Dagit are the common non-native grasses (Avena fatua, Bromus sp., Cynodon dactylon, Festuca sp., Hordeum murinum, etc.) and mustard (Brassica nigra), followed by a variety of thistles (Centaurea melitensis, Salsola iberica, etc.).
Once the non-native species become established and the chaparral species have been eliminated it is extremely difficult to restore this area. Restoration efforts should focus on reintroducing native species, eliminating non-native species and reducing the fire frequency (R2a).Additional community tables
Table 5. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Shrub/Vine1 shrubs 830–2100 chamise ADFA Adenostoma fasciculatum 370–940 – bigpod ceanothus CEME Ceanothus megacarpus 100–250 – black sage SAME3 Salvia mellifera 100–250 – Eastern Mojave buckwheat ERFA2 Eriogonum fasciculatum 80–205 – sugar sumac RHOV Rhus ovata 55–140 – San Luis purple sage SALE3 Salvia leucophylla 45–115 – California brittlebush ENCA Encelia californica 30–70 – Grass/Grasslike2 grass 25–70 purple needlegrass NAPU4 Nassella pulchra 25–70 – Table 6. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 7. Community 3.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 8. Community 4.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 9. Community 5.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Animal community
The following birds prefer Chaparral communities for their habitat: Wrentit (Chamaea fasciata), Western Scrub-Jay (Aphelocoma californica), California Towhee (Pipilo crissalis), Spotted Towhee (Pipilo crissalis), and the California Thrasher (Toxostoma redivivum). The gig-eared woodrat (Neotoma macrotis), Red diamond rattlesnake (Crotalus exsul) and the Mt. mahogany hairstreak butterfly (Satyrium tetra) are other animals associated with chaparral (Halsey, 2005). Mule deer (Odocoileus hemionus), Rabbits, Coyote (Canis latrans), bobcat (Lynx rufus), and mountain lions (Puma concolor), also utilize chaparral for bedding, cover and/or browse. The new shoots of chamise are much more nutritious browse than the older shoots.
Recreational uses
This area is suitable for trails for hiking, biking, and horse riding as long as the slopes are not too steep. Flatter areas are suitable for campgrounds.
Wood products
The chaparral shrubs do not provide wood products in the form of lumber or true construction material. However, they could provide pulp and sawdust for things such as paper, wood pellets or biofuels. This is most likely not an economical choice at this time.
Other products
Native Americans made infusions from the bark and leaves of chamise to treat syphilis. Chamise oils were used to treat skin infections. A binding agent for arrows and baskets was made from scale insects found on chamise plants. Spanish Californians used red shank as a remedy for colds, snakebite, and tetanus (Howard, 1993 and McMurray, 1990).
Native Americans used the seeds from black sage by processing them into a meal to be used used for baking. The leaves and stems were used for the a mint-flavor. It is valued as a honey plant (McMurray, 1990).
Other information
Black sage is susceptible to air pollution and is therefore a good monitor of air pollution in southern California (McMurray, 1990).
Supporting information
Other references
Burk, Jack H., 1978. Seasonal and Diurnal Water Potentials in Selected Chaparral Shrubs. American Midland Naturalist, Vol. 99, No. 1 (Jan., 1978), pp. 244-248
Dagit, Rosi 2002. Post-fire Monitoring of Coast Live Oaks (Quercus agrifolia) Burned in the 1993 Old Topanga Fire. USDA Forest Service. Gen. Tech. Rep. PSW-GTR-184.
Haidinger, Tori L. and Keeley Jon E. (1993). Role of High Fire Frequency in Destruction of Mixed Chaparral. Madrono, Vol. 40, No.3, pp. 141-147, 1993.
Howard, Janet L. 1993. Adenostoma sparsifolium. 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/ [2007, October 16].
Keeley, Jon E. (2004). Impact of Antecedent Climate on Fire Regimes in Coastal California. International Journal of Wildland Fire, 2004, 13, 173-182.
Keeley Jon E. (2002). Fire Management of California Shrubland Landscapes. Environmental Management Vol. 29, No. 3, pp. 395-408.
Keeley, J.E. (2001). Fire and invasive species in Mediterranean-climate ecosystems of California. Pages 81–94 in K.E.M. Galley and T.P. Wilson (eds.). Proceedings of the Invasive Species Workshop: the Role of Fire in the Control and Spread of Invasive Species. Fire Conference 2000: the First National Congress on Fire Ecology, Prevention, and Management. Miscellaneous Publication No. 11, Tall Timbers Research Station, Tallahassee, FL.
Keeley, Jon E. (1992). Recruitment of Seedlings and Vegetative Sprouts in Unburned Chaparral. Ecology, Volume 73, Issue 4 (August, 1992), 1194-1208. The Ecological Society of America.
Keeley, Jon E. and Fotheringham C.J. (2001). Historic Fire Regime in Southern California shrublands. Conservation Biology, Volume 15, No. 6, December 2001. pp. 1536-1548.
Keeley, Jon E. and Fotheringham C.J. (1998). Mechanism of smoke-induced seed germination in a post-fire chaparral annual. Journal of Ecology, 1998, 86, 27-36. British Ecological Society.
Keeley, Jon E. and Fotheringham, C.J (?). Role of Fire in Regeneration of seed. Chapter 13. Online at: http://www.werc.usgs.gov/seki/pdfs/regeneration.pdf
Keeley, Jon E. (1992). Recruitment of Seedlings and Vegetative Sprouts in Unburned Chaparral. Ecology, Volume 73, Issue 4 (August, 1992), 1194-1208. The Ecological Society of America.
McMurray, Nancy 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/ [ 2005, June 29].
McMurray, Nancy E. 1990. Adenostoma fasciculatum. 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/ [ 2005, June 29].
McMurray, Nancy E. 1990. Salvia mellifera. 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/ [2007, November 19].
Montalvo, Arlee M., Eriogonum fasciculatum, California Buckwheat. Online at: www.fs.fed.us/global/iitf/pdf/shrubs/Eriogonum%20fasciculatum.pdf
Thanos, C. A., and Rundel, P. W. 1995. Fire-Followers in Chaparral: Nitrogenous Compounds Trigger Seed Germination. The Journal of Ecology, Vol. 83, No. 2 (Apr., 1995), pp. 207-216
Uchytil, Ronald J. 1991. Cercocarpus betuloides. 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/ [ 2005, June 29].
Contributors
Curtis Talbot, Marchel Munnecke
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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