Ohio subset of Plant Communities of the Midwest ... - NatureServe
Ohio subset of Plant Communities of the Midwest ... - NatureServe
Ohio subset of Plant Communities of the Midwest ... - NatureServe
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Cliffs, Talus, Buttes and Badlands: Eastern Moist Acid Cliffs<br />
Sandstone <strong>Midwest</strong> Moist Cliff Sparse Vegetation<br />
Sandstone <strong>Midwest</strong> Moist Cliff Sparse Vegetation<br />
<strong>Midwest</strong> Moist Sandstone Cliff<br />
CEGL002287<br />
DESCRIPTION: Vegetation is restricted to shelves, cracks and crevices in <strong>the</strong> rock, generally averaging less than<br />
20%. In <strong>the</strong> Ozarks and Interior Low Plateau, <strong>the</strong> herbaceous layer contains <strong>the</strong> forbs Dicentra canadensis,<br />
Dodeca<strong>the</strong>on frenchii, Heuchera parviflora, Triadenum walteri (= Hypericum walteri), Mitchella repens, Mitella<br />
diphylla, among o<strong>the</strong>rs, and <strong>the</strong> ferns Athyrium filix-femina, Cystopteris bulbifera, Osmunda cinnamomea, Osmunda<br />
regalis, and Trichomanes boschianum. In <strong>the</strong> Allegheny region <strong>of</strong> <strong>Ohio</strong>, <strong>the</strong> sandstone cliffs include <strong>the</strong> forbs Agrostis<br />
perennans, Aquilegia canadensis, Mitchella repens, and Viola blanda, and <strong>the</strong> ferns Asplenium montanum,<br />
Asplenium pinnatifidum, Asplenium rhizophyllum, Asplenium trichomanes, Cystopteris fragilis, Dennstaedtia<br />
punctilobula, Dryopteris intermedia, Dryopteris marginalis, Polypodium virginianum, and <strong>the</strong> rare Asplenium bradleyi.<br />
In Minnesota and Wisconsin <strong>the</strong> moist cliffs include forbs, such as Aralia nudicaulis, Asarum canadense and Mitella<br />
diphylla, and <strong>the</strong> ferns Cystopteris bulbifera and Cystopteris fragilis. Missouri sites <strong>of</strong>ten harbor glacial relicts. The<br />
nonvascular layer is poorly described. Seepage areas in Minnesota include Sullivantia sullivantii (= Sullivantia<br />
renifolia) (also found in Missouri) and Crytogramma stelleri (White and Madany 1978, Homoya et al. 1985, Nelson<br />
1985, MNNHP 1993, Anderson 1996).<br />
Stands occur as steep to vertical rock exposures <strong>of</strong> sandstone bedrock. Aspect is variable, but stands are best<br />
developed on north- and east-facing slopes, or under sandstone overhangs (Nelson 1985, MNNHP 1993). The<br />
sandstone overhangs are amphi<strong>the</strong>atre-like cuts in sandstone cliffs. They may recede deeply enough into <strong>the</strong> cliff<br />
face that light levels are very low in <strong>the</strong> interior <strong>of</strong> <strong>the</strong> overhang. The soils beneath <strong>the</strong> overhang are typically sandy<br />
and with little vegetation. Seepage areas may also occur (Homoya et al. 1985). In Missouri, geologic formations<br />
include <strong>the</strong> St. Peter and Lamotte formations.<br />
Natural disturbances include wind and storm damage, activity by cliff-dwelling animals in <strong>the</strong> crevices, ledges and<br />
rock shelters, and <strong>the</strong> build up and collapse <strong>of</strong> ice (Nelson 1985).<br />
COMMENTS: 2, MCS. In Missouri, a descriptive name for this type could be "Mitella diphylla - Mitchella repens -<br />
Dryopteris goldiana Cliff" (Tim Nigh pers. comm. 1996), but <strong>the</strong> name would not work in Wisconsin (E. Epstein pers.<br />
comm. 1999). Also present are polypodium ferns and mosses. Differences between sandstone overhang and<br />
sandstone cliff need review. In Ontario this type is found as very small occurrences and is very rare. This type could<br />
be split into an Ozark/Interior Low Plateau sandstone cliff type and more nor<strong>the</strong>rn <strong>Midwest</strong> sandstone cliff type. Cliffs<br />
are defined as vertical exposures <strong>of</strong> rock at least 3 m tall. The distinction between open (dry) versus shaded (moist)<br />
may be more important that bedrock type, at least on a local or state level. Curtis (1959) comments that in an effort to<br />
group <strong>the</strong> Wisconsin cliff data into meaningful categories, sites were separated by rock type (dolomite, sandstone,<br />
igneous) and exposure (shaded, exposed).<br />
CONSERVATION RANK: G4G5. Although <strong>the</strong> cliffs may be relatively common, sites may lack adequate buffers above<br />
and below <strong>the</strong> cliffs.<br />
DISTRIBUTION: This moist sandstone cliff community is found throughout <strong>the</strong> central and upper midwestern United<br />
States and adjacent Canada, from <strong>Ohio</strong> and Ontario west to Minnesota, south to Kansas and east to Indiana.<br />
USFS ECOREGIONS: 212Hi:CPP, 212Ja:CPP, 212Jn:CPP, 212Kb:CCC, 221Ea:CCC, 221Ec:CCP, 221Ed:CCP, 221Ef:CCC,<br />
221Fa:CCC, 222Aa:CCC, 222Ag:CCC, 222Ak:CCC, 222Ap:CCC, 222Aq:CCC, 222Dc:CCP, 222De:CCC, 222Dh:CCC,<br />
222Di:CCP, 222Hf:CCC, 222Jc:CCC, 222Ka:CCC, 222Lc:CCC, 222Ld:CCC, 222Lf:CCC, 222Md:CCC, 222Me:CCC,<br />
251Cc:CCC, 251Ce:CCC, M221:<br />
CONSERVATION REGIONS: 36:C, 37:C, 38:C, 44:C, 45:C, 46:C, 47:C, 48:C, 49:C<br />
STATES: AR IA IL IN KS MI MN MO OH WI PROVINCES: ON<br />
MIDWEST HERITAGE SYNONYMY: IL sandstone overhang community =<br />
IN sandstone overhang =<br />
MI moist acid cliff +<br />
MN moist cliff (sou<strong>the</strong>ast section) +<br />
MO moist sandstone cliff =<br />
OH non-calcareous cliff community +<br />
WI shaded cliff (sandstone subtype) =<br />
OTHER SYNONYMY: Cliff <strong>Communities</strong> (Anderson 1996) B. Anderson also notes <strong>the</strong> sandstone overhang type.,<br />
Shaded Rock Cliffs (Curtis 1959) B<br />
USNVC HIERARCHY: OPEN CLIFF SPARSE VEGETATION ALLIANCE (VII.A.1.N.a)<br />
PLANT COMMUNITIES OF THE MIDWEST – 2001. APPENDIX: ASSOCIATION DESCRIPTIONS<br />
343