Print Report

CEGL002292 Central Midwest-Interior Limestone - Dolostone Moist Cliff Vegetation

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Central Midwest-Interior Limestone - Dolostone Moist Cliff Vegetation

Colloquial Name: Central Midwest-Interior Moist Limestone - Dolostone Cliff

Hierarchy Level:  Association

Type Concept: This limestone - dolostone moist cliff community occurs in localized areas throughout the central midwestern-interior United States and southern Ontario, Canada. The cliffs are often very steep and found along rivers and strongly dissected hills. The aspect is typically northern and east, but is variable. Soils are generally absent, except on ledges or shelves. The cliff is moist due to seepage or shading due to aspect. The vegetation is generally quite sparse (<25% cover). Trees, when present, are scattered. Shrubs, herbs, and nonvascular species are more often present. Characteristic trees include Acer saccharum. Characteristic shrubs include Hydrangea arborescens and Staphylea trifolia. Common ferns include Adiantum pedatum, Asplenium rhizophyllum, and Cystopteris bulbifera, as well as Asplenium ruta-muraria and Asplenium resiliens. Other herbs include Aquilegia canadensis, Chenopodium simplex, Lysimachia quadriflora, Parnassia grandifolia, Pilea pumila, Selaginella apoda, Solidago caesia, and Solidago flexicaulis. Mosses, liverworts and lichens are also present.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This moist cliff type is apparently less common across the region than ~Central Midwest-Interior Limestone - Dolostone Dry Cliff Sparse Vegetation (CEGL002291)$$. Definitions of cliff types remain problematic. Curtis (1959) in Wisconsin suggested that substrate was of secondary importance compared to moisture (shading versus open) in determining floristic patterns. Furthermore some cliffs are a combination of layers of sandstone, shale and limestone or dolostone, making classification problematic. Tim Nigh (pers. comm. 1996) has suggested that the Missouri type could be named "Hydrangea arborescens - Adiantum capillus-veneris - Cystopteris bulbifera - Parnassia grandifolia Alkaline Cliff." This type should also be compared with ~Cystopteris bulbifera - (Asplenium rhizophyllum) Cliff Sparse Vegetation (CEGL004394)$$ in the Southeast. Ozark and southern Illinois and Indiana cliffs may be better placed into a Southeastern/Interior Low Plateau type, separate from a Midwest type, based on such species as Asplenium ruta-muraria and Asplenium resiliens. In southeastern Indiana, other rare calciphitic species include Carex eburnea, Heuchera villosa, Phlox bifida ssp. stellaria, Hylotelephium telephioides, and Sullivantia sullivantii. Limestone cliffs along the Niagara Escarpment in central Ontario/Bruce Peninsula may be different from those in southern Ontario (W. Bakowsky pers. comm. 1998) and from other Great Lakes Limestone cliffs. More northern examples of these cliffs in the Great Lakes region may also contain ~Thuja occidentalis Cliff Woodland (CEGL002451)$$, which may overlap in concept with this type.

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

Physiognomy and Structure: No Data Available

Floristics: The vegetation is generally quite sparse (<25% cover). Trees, when present, are scattered. Shrubs, herbs, and nonvascular species are more often present. Characteristic trees include Acer saccharum. Characteristic shrubs include Hydrangea arborescens and Staphylea trifolia. Common ferns include Adiantum pedatum, Asplenium rhizophyllum (= Camptosorus rhizophyllus), and Cystopteris bulbifera, as well as Asplenium ruta-muraria and Asplenium resiliens in the southern part of the range. Other herbs include Aquilegia canadensis, Chenopodium simplex, Lysimachia quadriflora, Parnassia grandifolia, Pilea pumila, Selaginella apoda, Solidago caesia, and Solidago flexicaulis. Mosses, liverworts and lichens are also present (Curtis 1959, White and Madany 1978, Homoya et al. 1985, Nelson 1985). In Wisconsin, seepage areas include Primula mistassinica and Campanula rotundifolia. In Oklahoma, the type occurs in the Arbuckle Mountains. The vegetation is sparse, but includes Boehmeria cylindrica, Pellaea atropurpurea, Asplenium platyneuron, and Urtica chamaedryoides.

Dynamics:  Disturbances include wind and icestorm damage (Nelson 1985).

Environmental Description:  The cliffs are often very steep and found along rivers and strongly dissected hills. The aspect is typically north and east, but is variable. Soils are generally absent, except on ledges or shelves. The cliff is moist due to seepage or shading due to aspect (Nelson 1985).

Geographic Range: This limestone - dolostone cliff community occurs in localized areas throughout the central midwestern and interior regions of the United States and southern Ontario, Canada, ranging from Ohio and southern Ontario west to Iowa, south to Oklahoma and Arkansas, and east to Tennessee.

Nations: CA,US

States/Provinces:  IA, IL, IN, KS, KY, MI, MN, MO, OH, ON, TN, WI




Confidence Level: Low - Poorly Documented

Confidence Level Comments: No Data Available

Grank: G4G5

Greasons: No Data Available


Concept Lineage: Dripping cliffs are included as variants of moist cliffs.

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Limestone - Dolostone Midwest Moist Cliff Sparse Vegetation (Faber-Langendoen 2001)
< Shaded Cliff (Curtis 1959)

Concept Author(s): D. Faber-Langendoen (2001)

Author of Description: D. Faber-Langendoen

Acknowledgements: No Data Available

Version Date: 02-27-17

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