Evaluating Restoration Baselines for Historically Fire-Protected Woodlands within a Northeastern Illinois Prairie Peninsula Landscape

2014 ◽  
Vol 34 (2) ◽  
pp. 166-177 ◽  
Author(s):  
R.T. Fahey ◽  
D.A. Maurer ◽  
M.L. Bowles ◽  
J. McBride
Keyword(s):  
1977 ◽  
Vol 55 (5) ◽  
pp. 593-605 ◽  
Author(s):  
T. M. Roberts ◽  
T. Robson ◽  
P. M. Catling

Plants of the prairie peninsula have persisted in southwestern Ontario in localized areas where a high water table in spring, severe drought in midsummer, and intermittent burning have limited forest encroachment. Unlike these relicts of the postglacial xerothermic period, a community of prairie species on a railway embankment at West Hill (Toronto) has developed within the last 100 years. It is postulated that the persistence of these prairie species in the face of intense competition by seedlings from the surrounding fields is due largely to their adaptation to the seasonal fluctuation of moisture availability, nutrient deficiency, and periodic disturbance at this site. Mortality of invading seedlings was due to extrinsic environmental stresses rather than competition for limited resources during the period of active growth. The perennial Liatris spicata was able to dominate part of the habitat as a result of rapid growth of adults and seedlings before drought, low requirement for nutrients and effective mobilization from the corm in spring, and resorption before senescence. Experimental trials suggest that accumulation of litter, improving the moisture-retention and nutrient availability of the substrate, will lead eventually to elimination of Liatris and the other disjunct species. The case for preserving this community and other wet-mesic prairies in southwestern Ontario is outlined. However, it is clear that the current practice of 'conservation by complete protection' should be replaced by a management policy of periodic burning or mowing.


1983 ◽  
Vol 4 (2) ◽  
pp. 153-166 ◽  
Author(s):  
Chelvadurai Manogaran
Keyword(s):  

1979 ◽  
Vol 140 (2) ◽  
pp. 232-240 ◽  
Author(s):  
Cassandra S. Rodgers ◽  
Roger C. Anderson

1974 ◽  
Vol 4 (4) ◽  
pp. 487-495 ◽  
Author(s):  
Robert V. Ruhe

In midwestern United States the most important widespread environmental event during the Holocene about 8000 y.a. was the establishment of an effective precipitation pattern that in part defines the Prairie Peninsula. The pattern occupies a region that is dominated by dry westerly air for 6–9 mo during normal years and for 9–12 mo during drought years. Regional soil geography correlates readily with zones of precipitation effectiveness with Brunizem (Udolls) conforming to the moist, subhumid zone, Chernozem (Boralls, Udolls) relating to the dry, subhumid zone, and Chestnut and Brown soils (Ustolls) fitting the semiarid zone. During the past few thousand years, a climatic reversal has caused encroachment of forest on prairie resulting in the formation of transitional or intergrade soils.In local areas the Holocene is expressed on the land surface by the soil geomorphic unit which is the repetitive occurrence of a sequence of soils on the erosional surface of a hillslope and on the correlative depositional body at the foot and toe of the slope. This unit embraces time, lithology, landscape, and soils and provides a means for mapping the Holocene on the countryside.


2012 ◽  
Vol 39 (1-6) ◽  
pp. 297-322
Author(s):  
Lauren E. Brown ◽  
Christopher A. Phillips

The examination of 387 preserved red-bellied snakes, Storeria occipitomaculata, from 18 museums and collections, literature records, and unpublished records revealed distributional records throughout much of Illinois, in contrast to earlier studies which found a more limited distribution. Seventy-one records of habitat types from museum records, field notes, and literature indicated that the species occupies woodlands but is not primarily forest adapted. It also inhabits prairie and prairielike habitats in Illinois. The common occurrence of this species in this type of habitat has not heretofore been reported elsewhere in the range of the snake. Our findings do not support an older zoogeographic theory that assumed the snake was nonadapted for prairie and thus excluded from the Prairie Peninsula. We propose that the species was able to occupy the area near the ice rim of the Wisconsin Episode glaciation, and followed the glaciation as it retreated because of the snake’s cold tolerance, ability to inhabit northern prairies and coniferous forests, vivipary which allows thermoregulation by gravid females, and the relatively temperate climate along the glacial rim. Within recent times, it seems likely that the snake was extirpated throughout much of the former prairie by destructive changes associated with agriculture.


1977 ◽  
Vol 8 (3) ◽  
pp. 307-323 ◽  
Author(s):  
James E. King ◽  
William H. Allen

Pollen preserved in a peat deposit from a large swamp, the Old Field in the Mississippi River Valley near Advance, Missouri, records radiocarbon-dated vegetation changes between 9000 and about 3000 years ago. The principal feature of both the percentage and influx pollen diagrams is the replacement of arboreal pollen, primarily Quercus, Fraxinus, and Cephalanthus, with Gramineae and NAP between 8700 and 5000 years BP. This vegetation shift is interpreted as reflecting a decrease in the extent of the Old Field swamp and its associated bottomland forest species along with the expansion of a grass-dominated herb community, as a result of a reduction in available ground water. The desiccation of the swamp during this period indicates a reduction in precipitation within the ground-water source area and a shift to a drier climate in the southern Midwest. The pollen suggests that the lowest water levels and driest climate in southeastern Missouri lasted from 8700 to 6500 years BP, at which time there is a partial reappearance of swamp species. Relatively dry conditions, however, continued until at least 5000 years BP. Although pollen influx data are lacking from the upper part of the profile, the relative pollen frequencies suggest an increase in trees after 5000 BP. The replacement of the arboreal vegetation by grasses and herbs between 8700 and 5000 years BP reflects the period of maximum expansion of the Prairie Peninsula in southeastern Missouri. The Old Field swamp provides the first pollen evidence that the vegetational changes along the southern border of the Prairie Peninsula were chronologically similar to those on the northern and northeastern margins.


1963 ◽  
Vol 23 (1) ◽  
pp. 3-29 ◽  
Author(s):  
Allan G. Bogue

Flaring westward from the upper valley of the Wabash lies the prairie triangle, embracing most of central and northern Illinois and almost all of Iowa. Much of this region today lies in the heart of the corn belt. Its economic history is a story of practical experimentation, adaptation, and change as its restless settlers endeavored after 1820 to unlock its wealth. To do so, the prairie pioneers had to adapt techniques and crops to the novel environment of an almost treeless grassland at a time when both technology and markets were undergoing revolutionary change. In 1830 the farm-makers had hardly begun their task; by the 1890's the land was tamed, the corn belt a fact, its farmers on the threshold of a golden age.


Ecology ◽  
2006 ◽  
Vol 87 (10) ◽  
pp. 2523-2536 ◽  
Author(s):  
David M. Nelson ◽  
Feng Sheng Hu ◽  
Eric C. Grimm ◽  
B. Brandon Curry ◽  
Jennifer E. Slate
Keyword(s):  

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