The few remaining oak woods in southern Wisconsin which have escaped disturbance by fire, grazing, or extensive cutting present an unusual opportunity for studies of successional relationships. Although maple-basswood (Acer saccharum-Tilia americana) is the climatic climax community for the westward extension of the central deciduous forest (Braun, '47), it has been noted that Indians using fires as hunting adjuncts successfully maintained a number of large areas in oak-opening and prairie disclimax until a century ago (Cottam, '49). A study of the records of the original land survey conducted in 1832-'35 has shown that most of Dane County was either oak-opening, prairie, or marsh (Ellarson, '48). Three small terminal maple forests existed in areas protected by lakes from fire driven by the prevailing southwest winds. Settlement of the region resulted both in the clearing for agricultural purposes of a major proportion of the area occupied by oak-opening and in a cessation of fire. The few remaining uncleared areas have developed into close-canopied oak forests of varying composition (Curtis and McIntosh, '51) . The stand of oak which comprises the subject of this study is located in Sections 7 and 8, T-9-N, R-8-E, in northwestern Dane County, Wis. The entire oak woods occupies roughly a half square mile and falls within a region which, at the time of the original land survey, was oak-opening (Ellarson, '48). The topography of the area is gently to moderately rolling, a result of glaciation. Nine miles to the west is a terminal moraine which marks the edge of glaciation and the beginning of the Wisconsin Driftless Area. It is believed by some investigators that after retreat of the glacier, maple and basswood spread throughout the region from a Pleistocene refuge in the Driftless Area (Braun, '47). The soil is Miami silt loam. The oak woods was studied with particular attention to several distinct areas occupied by red maple (Acer rubrum). The author would Jike to take this opportunity to express his gratitude for the constant interest and assistance provided by Prof. John T. Curtis from the time of initiation of the project to its completion. Method.-Visual inspection of the woods, particularly during fall when leaf colors are brilliant, conveys the definite impression that red maples are coming into the understory in at least five strikingly demarked areas. At -the center of each of these areas, one or more red maple trees of considerable size are to be found, and beneath these trees and for a distance around them the herbaceous and shrubby vegetation is nearly absent or extremely thin.
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