Presettlement Forests of the Unglaciated Portion of Southern Illinois
- 1 April 1981
- journal article
- research article
- Published by JSTOR in The American Midland Naturalist
- Vol. 105 (2) , 290-304
- https://doi.org/10.2307/2424747
Abstract
General Land Office survey notes of 1805-1815 were used to reconstruct the presettlement forests of southern Illinois. Witness trees were grouped into stands according to soil associations. Phytosociological attributes of absolute (D2) and relative density (D3), absolute (B2) and relative basal area (B3), percent importance .**GRAPHIC**. and mean diameter for the 32 resulting stands were estimated by applying random pairs and closest individual sampling methods. Four forest types [consisting mainly of Lirodendron tulipifera, Magnolia acuminata, Tilia heterophylla, Aesculus-octandra, Fagus grandifolia, Quercus alba and Q. velutina, Nyssa aquatica, Liquidambar styraciflua, Carya sp., Taxodium distichum, Ulmus, celtis laevigata, Fraxinus, Acer nigrum and Populus deltoides] were mapped: Mesic Oak-Hickory, Mixed Hardwoods, Lowland-Depressional and Floodplain Forests. Mesic Oak-Hickory Forest, consisting primarily of O. alba L., Q. velutina Lam. and Carya spp., occurred on soils of thin loess in the Shawnee Hills. The more mesic Mixed Hardwoods Forest occurred mainly on the thicker loess of the Thebes Hills. It was dominated by F. grandifolia Ehrh., Q. alba, Q. velutina, L. styraciflua L. and L. tulipifera L. Annually flooded inland lowlands supported a Lowland-Depressional Forest of Ulmus, Fraxinus, Quercus and Carya spp., plus Liquidambar. Floodplain Forest, dominated by P. occidentalis L., P. deltoides Bartr. and Fraxinus and Ulmus spp., occurred on the alluvial soils of the Mississippi River. This mixture of climax and successional communities was described as Western Mesophytic (after Braun, 1950). The possibility that F. grandifolia may have migrated from the South or Southwest was proposed, due to its concentration in the Thebes Hills.This publication has 15 references indexed in Scilit:
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