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Seminar Series - Spring 2008
Next Seminar:
Monday, 28 April 2008, 11:00 A.M. Illinois State Geological Survey, 101 Natural Resources Building Application of Predictive Biomantle Principles to Resolving Enigmatic Topographic-Landform-Soil Issues: The Case of Mima Mounds Donald L. Johnson,1 presenting, Diana N. Johnson,2 Hong Wang,3 Keith C. Hackley,3 Richard A. Cahill,3 and Jennifer Burnham4 Abstract"Probably no landform of similar size [Mima mounds] has occupied such a conspicuous place in geological controversy.5 A recent article in Nature10 leads with the question: "Do biota affect landscape form and evolution?" Although that paper focused largely on the quantitative role of biota in mediating fluvial transport, the question posed in the article, and its title ("The search for a topographical signature of life") have broad and intriguing implications. The search for topographical and other signatures of life is a theme that, until recently, has been largely absent in the broad arena of Earth, biological, and environmental sciences. But new searches and researches are advancing the theme, with fruitful and useful discoveries being made. This talk summarizes our research along these lines. We demonstrate how biomantle principles applied to both field observations and laboratory data (particle size, pH, organic matter, C-14 analyses/ measurements) do in fact reveal unequivocal topographic and landform signatures of life. We further demonstrate how these predictive principles aid in resolving long-standing cross-disciplinary issues, for example the origin of Mima mounds (pimple mounds, prairie mounds, etc.). Our primary Mima mound work was at Mima Prairie near Olympia in Washington State, and at Diamond Grove Prairie near Joplin in Missouri. Supplemental researches and observations were made at multiple Mima moundfields across western North America over a multi-decadal timeframe. Moundfields were visited and revisited, examined and reexamined, some multiple times, in several cases annually over many years. New moundfields were predictively discovered. The sum of our collective research strongly indicates that Mima mounds are point-centered, locally thickened biomantles produced predominantly through bioturbation by small vertebrates. The process mainly involves repeated biotransfers and biosorting by the supremely fossorial members of Geomyidae. (The Dalquest-Scheffer-Cox model of nest-centered centripetal burrowing by these animals is supported.) An unexpected bonus of our Mima mound research was to shed bright genetic light on another equally long standing and contentious landscape issue; the bioturbational origin of stone lines (stonelayers) in soils.
1 Dept. Geography, University of Illinois, Urbana, IL
61801 USA, dljohns@uiuc.edu
Other Seminars and Colloquia of interest on the UIUC Campus
Department of Geology
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