Intensive Virginia Division of Natural Heritage, see http://www.dcr.virginia.gov/natural_heritage/documents/nh_plotform_instructions.pdf
Overall Taxon Cover Values are Automatically Calculated?
no
Plot Quality Fields:
Plot Validation Level
(2) classification plot: sufficient for inclusion in a classification revision
Overall Plot Vegetation Fields:
Field Height
1
m
Field Cover
75
%
Nonvascular Cover
15
%
Misc Fields:
Observation Narrative
Plot captures fairly diverse, graminoid-dominated vegetation on east end of Buffalo Mountain summit. This community is distinct from more sparsely vegetated bedrock pavement barren characterized by Minuartia groenlandica and Paronychia argyrocoma. Shrub stature and cover are considerably less here than on west slope just below summit, where this community type is more extensive. Rhynchospora globularis is especially striking in this stand, and Scleria triglomerata, Hypoxis hirsuta, and Muhlenbergia capillaris are among the other graminoids more abundant in this stand than in that on the west slope (see plots BUFF008P and BUFF008D). Seasonal runoff, which Tom Rawinski highlighted in the other stand, probably contributes to more widespread mesic conditions here, but equally important are accumulation of soil and high cover of bunch grasses. Soils on the summit are substantially more deficient in base cations and have much aluminum concentrations than those of lower elevations at Buffalo Mountain, which could reflect the effects of chronic acid precipitation.
Very dark brown, nearly black, silty loam, apparently high in organic matter; rocks and tiny mineral fragments abound; soil collected from only one point to minimize disturbance
Disturbance Data:
Disturbance Type
Disturbance Intensity
Disturbance Comment
unknown
Soil chemistry data (chiefly concentrations of base cations and Al) suggest chronic acidification of soil as a result of acid precipitation.