Author : David Aaron Grimley
Publisher :
ISBN 13 :
Total Pages : 634 pages
Book Rating : 4.:/5 (379 download)
Book Synopsis Stratigraphy, Magnetic Susceptibility, and Mineralogy of Loess-paleosol Sequences in Southwestern Illinois and Eastern Missouri by : David Aaron Grimley
Download or read book Stratigraphy, Magnetic Susceptibility, and Mineralogy of Loess-paleosol Sequences in Southwestern Illinois and Eastern Missouri written by David Aaron Grimley and published by . This book was released on 1996 with total page 634 pages. Available in PDF, EPUB and Kindle. Book excerpt: Magnetic susceptibility (MS) zones, controlled by silt-size magnetite concentrations, have been delineated within oxidized, C horizon Peoria and Loveland Silts along the Illinois and Mississippi Valleys. Lower Peoria and lower Loveland Silts (MS = 55-80 $times 10sp{-5}$ SI) and Roxana Silt (MS = 60-90 $times 10sp{-5}$) have high MS probably reflecting greater contributions from Superior Lobe outwash. Middle Peoria and upper Loveland Silts (MS = 20-55 $times 10sp{-5}$) and upper Peoria Silt (MS = 40-60 $times 10sp{-5}$) have low MS, probably reflecting dilution by Lake Michigan Lobe outwash upon maximum advance of glaciers in Illinois. Feldspar/quartz and kaolinite/illite X-ray diffraction peak height ratios also increase in zones of high MS. Bulk and magnetic grain size distributions are generally uniform across MS zones at sections studied. Peoria Silt MS zones are particularly striking in loess proximal to the Illinois (Ancient Mississippi) Valley because of source area shifts caused by Mississippi River diversion at about 20.5 ka. MS zones are less pronounced along the Mississippi Valley south of St. Louis. Alteration of magnetite in gleyed loess can occur but is not thought to cause MS zones observed because minor increases in illite and dolomite in low MS zones are more consistent with a source area hypothesis. Jules and Gardena (interstadial) Geosol occur in upper portions of middle and lower Peoria Silt and are estimated to be 15-16 ka and 20-20.5 ka, respectively. Clay beds, deposited during peak glacial floods (16-20 ka), occur within middle Peoria Silt. Ultrafine magnetite and maghemite (0.01-0.1 $mu$m), authigenically formed, are responsible for high MS in upper solums of modern soils and paleosols, where they are preserved and can accumulate under oxidizing conditions. Highly substituted superparamagnetic and single domain magnetite probably forms extracellularly to bacteria in soils and later alters to maghemite. Soil firing can be locally important in causing high MS. Bt horizon thicknesses, clay content increases, feldspar weathering, and amounts of neoformed ferrimagnetics and mixed-layered kaolinite-expandables all indicate considerably greater time for development of the Yarmouth Geosol compared to the Sangamon Geosol. In the study area, Yarmouth Geosol is estimated to represent oxygen isotope stages 7-11 and the Sangamon Geosol stage 5 and portions of stage 4. Loveland Silt was probably deposited during stage 6 only. Crowley's Ridge Silt, into which Yarmouth Geosol formed, is estimated to have been deposited during stage 12. Bridgeton geosol (new) may represent stages 13-15 and Bonfils silt (new), stage 16.
