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 Dry Alkaline Cliffs<br />
Limestone - Dolostone <strong>Midwest</strong> Dry Cliff Sparse Vegetation<br />
Limestone - Dolostone <strong>Midwest</strong> Dry Cliff Sparse Vegetation<br />
<strong>Midwest</strong> Dry Limestone - Dolostone Cliff<br />
CEGL002291<br />
DESCRIPTION: Vegetation is restricted to shelves, cracks and crevices in <strong>the</strong> rock, generally averaging less than<br />
20%, and typically consisting <strong>of</strong> vines and ferns. In <strong>the</strong> Ozarks and Interior Plateau region, ferns include Cheilan<strong>the</strong>s<br />
feei, Argyrochosma dealbata (= Notholaena dealbata), Pellaea atropurpurea, and Pellaea glabella. Herbaceous forbs<br />
and graminoids include Aquilegia canadensis, Hedyotis nigricans (= Houstonia nigricans), Mentzelia oligosperma,<br />
Muhlenbergia cuspidata, Sedum pulchellum, and Solidago rugosa ssp. aspera (= Solidago drummondii). Lichens<br />
include Dermatocarpon lachneum, Lecanora muralis and Psora russellii. In <strong>Ohio</strong>, stands contain <strong>the</strong> ferns Pellaea<br />
atropurpurea and Pellaea glabella, and <strong>the</strong> forbs Aquilegia canadensis, Arabis laevigata, Heuchera americana,<br />
Hydrangea arborescens, and Sedum ternatum. Scattered woody plants across <strong>the</strong> range include Celastrus<br />
scandens, Juniperus virginiana, Par<strong>the</strong>nocissus quinquefolia, Physocarpus opulifolius, Quercus prinus (southward),<br />
and Toxicodendron radicans (= Rhus radicans), and far<strong>the</strong>r north, Taxus canadensis, Thuja occidentalis, and Tsuga<br />
canadensis (Curtis 1959, Nelson 1985, MNNHP 1993, Anderson 1996).<br />
Stands occur as steep to vertical rock exposures <strong>of</strong> limestone bedrock. Aspect is variable, but stands are best<br />
developed on south- and west-facing slopes. Soils are ei<strong>the</strong>r absent or, along ledges and shelves, very shallow. The<br />
cliffs drain very rapidly, and can become very dry in summer (Nelson 1985).<br />
Natural disturbances include drought stress, wind and storm damage, and disturbances from cliff-dwelling animals,<br />
particularly in <strong>the</strong> crevices, ledges and rock shelters (Nelson 1985).<br />
COMMENTS: 2, MCS. Definitions <strong>of</strong> cliff types remain problematic. A minimum height <strong>of</strong> 3 m may be practical. Curtis<br />
(1959) in Wisconsin suggested that substrate was <strong>of</strong> secondary importance compared to moisture (shading vs. open)<br />
in determining floristic patterns. Fur<strong>the</strong>rmore some cliffs are a combination <strong>of</strong> layers <strong>of</strong> sandstone, shale and<br />
limestone or dolostone, making classification problematic. The combination <strong>of</strong> moisture and substrate is retained<br />
here, but a more systematic rangewide comparison <strong>of</strong> cliff floras is needed. Tim Nigh (pers. comm. 1996) has<br />
suggested that <strong>the</strong> Missouri type could be named "Aquilegia canadensis - Solidago rugosa ssp. aspera (= Solidago<br />
drummondii) - Pellaea atropurpurea Cliff." Ozark, sou<strong>the</strong>rn Illinois and Indiana cliffs may be better placed into a<br />
Sou<strong>the</strong>astern/Interior Low Plateau type, separate from an upper <strong>Midwest</strong> type. Limestone cliffs along <strong>the</strong> Niagara<br />
Escarpment in central Ontario/Bruce Peninsula may be different from those in sou<strong>the</strong>rn Ontario (Wasyl Bakowsky<br />
pers. comm. 1998) and from o<strong>the</strong>r Great Lakes Limestone cliffs. A series <strong>of</strong> studies in Ontario's cliffs have led to<br />
surprising biological discoveries, including a rich snail fauna, unusual cyanobacteria, and old growth Thuja<br />
occidentalis stands on <strong>the</strong> cliffs (Larson and Kelly 1991, Larson, Mat<strong>the</strong>s and Kelly 1999, Larson et al. 1999). Chalk<br />
breaks in west-central Kansas along <strong>the</strong> Smoky Hill River and associated terrain are cliff-like and probably need to be<br />
separated from <strong>the</strong> eastern cliffs (Lauver pers. comm. 1998).<br />
CONSERVATION RANK: G4G5. In Missouri many sites have been quarried (M. Leahy pers. comm. 1999). This issue<br />
should be examined range-wide. O<strong>the</strong>r sites lack adequate buffers above and below <strong>the</strong> cliffs. Finally, rock-climbing<br />
can be disruptive to vegetation (Larson et al. 1999).<br />
DISTRIBUTION: This limestone/dolostone cliff community type is found throughout <strong>the</strong> midwestern United States and<br />
adjacent Canada, from <strong>Ohio</strong> and Ontario, west to Minnesota, south to Kansas, and possibly Arkansas, and east to<br />
Indiana.<br />
USFS ECOREGIONS: 212Jn:CCC, 222Ac:CCC, 222Ad:CCC, 222Ae:CCC, 222Af:CCC, 222Ag:CCC, 222Ah:CCC, 222Ak:CCC,<br />
222Am:CCC, 222Ap:CCC, 222Aq:CCC, 222Df:CCC, 222Di:CCP, 222Ek:CCC, 222Fd:CCC, 222Fe:CCC, 222Hc:CCC,<br />
222Hf:CCP, 222Lc:CCC, 222Lf:CCC, 222Md:CCC, 251Ce:CCC<br />
CONSERVATION REGIONS: 36:C, 37:C, 38:C, 44:C, 45:C, 46:C, 48:C<br />
STATES: IA IL IN KS MI MN MO OH PROVINCES: ON<br />
MIDWEST HERITAGE SYNONYMY: IL<br />
limestone cliff community; dolomite cliff community I<br />
IN limestone cliff +<br />
MI dry non-acid cliff +<br />
MN dry cliff (sou<strong>the</strong>ast section) +<br />
MO dry limestone/dolomite cliff =<br />
OH calcareous cliff community +<br />
OTHER SYNONYMY: Exposed Rock Cliffs (Curtis 1959) B, Cliff <strong>Communities</strong> (Anderson 1996) 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 />
335