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CEGL002145 Quercus muehlenbergii - Quercus macrocarpa / Andropogon gerardii Ravine Woodland
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: Chinquapin Oak - Bur Oak / Big Bluestem Ravine Woodland
Colloquial Name: Chinquapin Oak - Bur Oak Ravine Woodland
Hierarchy Level: Association
Type Concept: This chinquapin oak - bur oak woodland community is found in the central tallgrass prairie region of the United States. Stands occur in dry-mesic ravines and valleys of rivers and major streams. This wooded community is found in a landscape that is primarily prairie. The canopy is not completely closed; it is thought to range from 25-80% cover. The tree layer is dominated by Quercus muehlenbergii and Quercus macrocarpa. Cercis canadensis and Ulmus spp. are common associates. There is usually a prominent shrub layer. The two most common shrubs are Cornus drummondii and Symphoricarpos orbiculatus. Celtis occidentalis and Ulmus spp. are often in the shrub layer, especially on sites that have not been burned recently. Herbaceous dominants include Schizachyrium scoparium and Panicum virgatum. Periodic fire is necessary to maintain the relatively open, woodland character. In the absence of fire this community soon begins to succeed to other, more closed forest types.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: Discuss with Missouri and Kansas whether or not this type should be combined with ~Quercus macrocarpa / Andropogon gerardii - Hesperostipa spartea Woodland (CEGL002053)$$.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: This community has a good deal of structural variation among the different sites. The tree canopy cover is thought to vary from about 25-80%. Shrubs are almost always present (Abrams 1986). The drier sites have smaller trees, less canopy cover, and less basal area than more mesic sites. On the sites that were measured at Konza Prairie, Abrams (1986) reported that this community had an average basal area of 20.5 m2/ha. The range was 13.4-31.6 m2/ha in the nine stands he analyzed in northeastern Kansas (Groups 3 and 4 in his paper). The number of trees/ha also was highly variable. There were an average of 467 stems/ha of tree species greater than 10 cm in diameter. Eight of the stands fell within a range of 207-583 stems/ha while one had 927 stems/ha.
Floristics: This community is dominated by broad-leaved deciduous trees. Quercus muehlenbergii dominates the overstory of the driest stands with Quercus macrocarpa as a subdominant. Quercus macrocarpa becomes more important in sites where conditions are more mesic until, eventually, the community grades into a forest with relatively little Quercus muehlenbergii. Ulmus spp. and Cercis canadensis can be abundant, especially as smaller individuals, and Juniperus virginiana is uncommon. The potential of Ulmus spp. to remain as an important part of this community is in doubt because of Dutch elm disease. The two most common shrubs are Cornus drummondii and Symphoricarpos orbiculatus. Celtis occidentalis and Ulmus spp. are often in the shrub layer, especially on sites that have not been burned recently. Herbaceous dominants include Schizachyrium scoparium and Panicum virgatum.
Tree canopy cover is not completely closed in this community; it may be between 25-80%. The height of dominant trees is limited on drier sites. Shrub cover varies inversely with tree canopy cover, achieving 50-60% in some of the drier stands surveyed by Abrams (1986, 1988). The high values for shrub canopy cover may be a result of the increase in fire intervals since the 1850s. Shrub canopy fell from 59.7 to 9.5% when a woodland of this type was burned in two consecutive springs (Abrams 1988).
The composition of the canopy of this community is relatively constant, being dominated by Quercus muehlenbergii and Quercus macrocarpa (average importance values of 171.2 and 64.9, respectively, at Konza Prairie), with Cercis canadensis and Ulmus spp. in varying amounts (Abrams 1986). Morus rubra is often present but does not attain a high importance. The patterns of dominance in tree species depend on site history and environmental characteristics. Quercus muehlenbergii and Quercus macrocarpa can remain the dominants in all age classes in stands that have a fairly high fire frequency. The canopy becomes more complete as fire frequency drops. On the drier sites, Ulmus spp. and Cercis canadensis are able to reproduce preferentially in the lower light environment that occurs as the canopy begins to close over. The ability of Ulmus spp. to remain in the community depends on whether Dutch elm disease affects the stand or not. On more mesic sites, different species acquire dominant status. Quercus macrocarpa remains as a dominant. Celtis occidentalis is able to reproduce in the lower light environment and eventually comes to dominant status, with lesser amounts of Ulmus spp. and Fraxinus pennsylvanica. At this point the community has changed enough to become a different forest community.
This community has a good deal of structural variation among the different sites at Konza Prairie. The tree canopy cover may vary from about 25-80%. Shrubs are almost always present (Abrams 1986). The drier sites have smaller trees, less tree canopy cover, and less basal area than more mesic sites.
Tree canopy cover is not completely closed in this community; it may be between 25-80%. The height of dominant trees is limited on drier sites. Shrub cover varies inversely with tree canopy cover, achieving 50-60% in some of the drier stands surveyed by Abrams (1986, 1988). The high values for shrub canopy cover may be a result of the increase in fire intervals since the 1850s. Shrub canopy fell from 59.7 to 9.5% when a woodland of this type was burned in two consecutive springs (Abrams 1988).
The composition of the canopy of this community is relatively constant, being dominated by Quercus muehlenbergii and Quercus macrocarpa (average importance values of 171.2 and 64.9, respectively, at Konza Prairie), with Cercis canadensis and Ulmus spp. in varying amounts (Abrams 1986). Morus rubra is often present but does not attain a high importance. The patterns of dominance in tree species depend on site history and environmental characteristics. Quercus muehlenbergii and Quercus macrocarpa can remain the dominants in all age classes in stands that have a fairly high fire frequency. The canopy becomes more complete as fire frequency drops. On the drier sites, Ulmus spp. and Cercis canadensis are able to reproduce preferentially in the lower light environment that occurs as the canopy begins to close over. The ability of Ulmus spp. to remain in the community depends on whether Dutch elm disease affects the stand or not. On more mesic sites, different species acquire dominant status. Quercus macrocarpa remains as a dominant. Celtis occidentalis is able to reproduce in the lower light environment and eventually comes to dominant status, with lesser amounts of Ulmus spp. and Fraxinus pennsylvanica. At this point the community has changed enough to become a different forest community.
This community has a good deal of structural variation among the different sites at Konza Prairie. The tree canopy cover may vary from about 25-80%. Shrubs are almost always present (Abrams 1986). The drier sites have smaller trees, less tree canopy cover, and less basal area than more mesic sites.
Dynamics: Drought and fire were common natural disturbances in this community type. Fire was very important in determining which species were able to survive and reproduce successfully. Fire killed or stunted the woody growth enough to maintain the relatively open canopy necessary for the dominant plants to reproduce successfully. The mean fire intervals for the period 1862-1983 in three stands studied by Abrams (1985) were 11.2, 12.6, and 19.7 years based on fire scars in the cross section of trees. This may be longer than the actual fire intervals because not all fires in a stand result in identifiable scars. Fire intervals prior to settlement in the Flint Hills of Konza were thought to be 2-3 years (Abrams 1985). This community is stable only with a regime of periodic fire (Abrams 1985). Most of the dominant trees in the stands studied by Abrams (1986) at Konza Prairie were 100-125 years old, indicating that they originated shortly after fire suppression began in the 1850s. These stands were likely on sites that had been prairie (Bragg and Hulbert 1976). However, these oaks were not regenerating well as the canopy began to close over. The seedling and sapling layers of unburned stands contained few oaks. On drier sites about 85% of the individuals were Cercis canadensis or Ulmus spp., most of the rest were Quercus muehlenbergii. On more mesic, lower slopes Celtis occidentalis and Ulmus spp. made up about 75% of the sapling and seedling stages. These data indicate that the more mesic sites will probably become dominated by Celtis occidentalis, while the drier sites will have some combination of Quercus muehlenbergii and Cercis canadensis. The presence of Dutch elm disease raises the question of whether Ulmus spp. can persist in this community.
Abrams (1988) observed the effect of prescribed burns done in two consecutive springs on a relatively closed site. Before burning, only 1% of the seedlings were Quercus macrocarpa or Quercus muehlenbergii, 87% were Ulmus spp., and 6% were Celtis occidentalis. The sapling composition was very similar to that of the seedlings except that there were no oaks. The shrub cover was 59.7%. No canopy trees died as a direct result of the burns, but the shrub layer was reduced to 9.5% cover. All of the saplings were killed by the fires. Ulmus spp. and Celtis occidentalis seedlings increased, primarily as a result of basal sprouting. The oak seedlings were eliminated. Abrams (1988) hypothesized that if the area was burned frequently over several more years the fire-sensitive Ulmus spp. and Celtis occidentalis would continue to be killed, even if they avoided fires long enough to grow to be saplings. Oak seedlings could grow enough to be resistant to subsequent fires if they occurred in microsites that were not burned for a few years. If fires were frequent enough and burned all of the woody seedlings continually then the site would eventually become a prairie.
Precipitation and temperature are quite variable. The continental climate within which this community occurs is marked by hot summers and cold winters. The average temperature was 12.8°C, with a range from -2.7° to 26.6°C during the period 1951-1980 (Abrams and Knapp 1986).
Abrams (1988) observed the effect of prescribed burns done in two consecutive springs on a relatively closed site. Before burning, only 1% of the seedlings were Quercus macrocarpa or Quercus muehlenbergii, 87% were Ulmus spp., and 6% were Celtis occidentalis. The sapling composition was very similar to that of the seedlings except that there were no oaks. The shrub cover was 59.7%. No canopy trees died as a direct result of the burns, but the shrub layer was reduced to 9.5% cover. All of the saplings were killed by the fires. Ulmus spp. and Celtis occidentalis seedlings increased, primarily as a result of basal sprouting. The oak seedlings were eliminated. Abrams (1988) hypothesized that if the area was burned frequently over several more years the fire-sensitive Ulmus spp. and Celtis occidentalis would continue to be killed, even if they avoided fires long enough to grow to be saplings. Oak seedlings could grow enough to be resistant to subsequent fires if they occurred in microsites that were not burned for a few years. If fires were frequent enough and burned all of the woody seedlings continually then the site would eventually become a prairie.
Precipitation and temperature are quite variable. The continental climate within which this community occurs is marked by hot summers and cold winters. The average temperature was 12.8°C, with a range from -2.7° to 26.6°C during the period 1951-1980 (Abrams and Knapp 1986).
Environmental Description: This community occurs on moderate to steep south-facing and west-facing slopes of ravines and river valleys. The surface is not saturated or flooded by groundwater at any time during the year, but springs sometimes emerge within this woodland type. Drought is relatively common, occurring in 38% of the months from 1931-1968 (Abrams and Knapp 1986). Drought is important in this community. It excludes some species and reduces productivity in general (Bragg et al. 1993). More importantly, it leads to conditions that favor the fires necessary to maintain the woodland (Abrams and Knapp 1986). High summer temperatures, variable precipitation, moderately strong winds, and low relative humidity are all factors in the occurrence of drought in this community. The average temperature of northeastern Kansas ranged from -2.7° to 26.6°C with an average of 12.8°C for the period 1951-1980. Average rainfall was 835 mm. Most of the precipitation falls as rain in May and June. December through February are the driest months (Abrams and Knapp 1986). This community is never flooded. Springs sometimes emerge within this woodland type.
Soils of this community are deep, moderately well-drained to well-drained silts and loams. The parent material is primarily loess or glacial till. Cherty shales or limestones are the parent material in some areas of Kansas (Lauver et al. 1999). The parent material from which most soils of this community originate is glacial till or loess. In parts of the Flint Hills of eastern Kansas, shales and limestones of Permian age are at or near the surface. These rocks have an abundance of chert which increases their resistance to weathering. Residuum from these bedrocks forms the parent material in these areas (Bragg and Hulbert 1976).
Soils of this community are deep, moderately well-drained to well-drained silts and loams. The parent material is primarily loess or glacial till. Cherty shales or limestones are the parent material in some areas of Kansas (Lauver et al. 1999). The parent material from which most soils of this community originate is glacial till or loess. In parts of the Flint Hills of eastern Kansas, shales and limestones of Permian age are at or near the surface. These rocks have an abundance of chert which increases their resistance to weathering. Residuum from these bedrocks forms the parent material in these areas (Bragg and Hulbert 1976).
Geographic Range: This chinquapin oak - bur oak woodland community is found in the central tallgrass prairie region of the United States, particularly in northeastern Kansas and possibly adjacent states.
Nations: US
States/Provinces: KS
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.689586
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: G2
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.2 Cool Temperate Forest & Woodland Formation | F008 | 1.B.2 |
Division | 1.B.2.Na Eastern North American Forest & Woodland Division | D008 | 1.B.2.Na |
Macrogroup | 1.B.2.Na.4 White Oak - Bur Oak - Shagbark Hickory Forest, Woodland & Savanna Macrogroup | M012 | 1.B.2.Na.4 |
Group | 1.B.2.Na.4.b North-Central Oak - Hickory Forest & Woodland Group | G649 | 1.B.2.Na.4.b |
Alliance | A0620 Bur Oak Central Tallgrass Woodland Alliance | A0620 | 1.B.2.Na.4.b |
Association | CEGL002145 Chinquapin Oak - Bur Oak / Big Bluestem Ravine Woodland | CEGL002145 | 1.B.2.Na.4.b |
Concept Lineage: No Data Available
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: ? Celtis occidentalis - Quercus macrocarpa Type (Abrams 1986) [Abrams'' analysis of a gallery forest at Konza Prairie in northeastern Kansas found this closely related mesic forest. This allied forest community has a similar suite of species but differs in structure, species dominance patterns, and environmental parameters. The forest was dominated by Quercus macrocarpa and Celtis occidentalis, had a greater basal area/ha of trees, and less shrub cover. It is also generally on lower, gentler slopes, and has more silt content to its soils.]
= Quercus muehlenbergii - Quercus macrocarpa / Andropogon gerardii Ravine Woodland (Faber-Langendoen 2001)
= Quercus muehlenbergii - Quercus macrocarpa / Andropogon gerardii Ravine Woodland (Faber-Langendoen 2001)
- Abrams, M. D. 1985. Fire history of oak gallery forests in a northeast Kansas tallgrass prairie. The American Midland Naturalist 114(1):188-191.
- Abrams, M. D. 1986. Historical development of gallery forests in northeast Kansas. Vegetatio 65:29-37.
- Abrams, M. D. 1988. Effects of prescribed fire on woody vegetation in a gallery forest understory in northeastern Kansas. Transactions of the Kansas Academy of Science 9(3-4):63-70.
- Abrams, M. D., and A. K. Knapp. 1986. Seasonal water relations of three gallery forest hardwood species in northeast Kansas. Forest Science 32(3):687-696.
- Bragg, T. B., and L. C. Hulbert. 1976. Woody plant invasion of unburned Kansas bluestem prairie. Journal of Range Management 29(1):19-24.
- Bragg, W. K., A. K. Knapp, and J. M. Briggs. 1993. Comparative water relations of seedling and adult Quercus species during gallery forest expansion in tallgrass prairie. Forest Ecology and Management 56:29-41.
- Faber-Langendoen, D., editor. 2001. Plant communities of the Midwest: Classification in an ecological context. Association for Biodiversity Information, Arlington, VA. 61 pp. plus appendix (705 pp.).
- Lauver, C. L. 1989. Preliminary classification of the natural communities of Kansas. Unpublished report. Kansas Natural Heritage Program, Kansas Biological Survey, University of Kansas, Lawrence.
- Lauver, C. L., K. Kindscher, D. Faber-Langendoen, and R. Schneider. 1999. A classification of the natural vegetation of Kansas. The Southwestern Naturalist 44:421-443.
- Midwestern Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Minneapolis, MN.
- Weaver, J. E. 1965. Native vegetation of Nebraska. University of Nebraska Press, Lincoln. 185 pp.
- Weaver, J. E., and F. W. Albertson. 1956. Grasslands of the Great Plains: Their nature and use. Johnsen Publishing Co., Lincoln, NE. 395 pp.