999 resultados para Michigan.


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1Recent studies demonstrated the sensitivity of northern forest ecosystems to changes in the amount and duration of snow cover at annual to decadal time scales. However, the consequences of snowfall variability remain uncertain for ecological variables operating at longer time scales, especially the distributions of forest communities. 2The Great Lakes region of North America offers a unique setting to examine the long-term effects of variable snowfall on forest communities. Lake-effect snow produces a three-fold gradient in annual snowfall over tens of kilometres, and dramatic edaphic variations occur among landform types resulting from Quaternary glaciations. We tested the hypothesis that these factors interact to control the distributions of mesic (dominated by Acer saccharum, Tsuga canadensis and Fagus grandifolia) and xeric forests (dominated by Pinus and Quercus spp.) in northern Lower Michigan. 3We compiled pre-European-settlement vegetation data and overlaid these data with records of climate, water balance and soil, onto Landtype Association polygons in a geographical information system. We then used multivariate adaptive regression splines to model the abundance of mesic vegetation in relation to environmental controls. 4Snowfall is the most predictive among five variables retained by our model, and it affects model performance 29% more than soil texture, the second most important variable. The abundance of mesic trees is high on fine-textured soils regardless of snowfall, but it increases with snowfall on coarse-textured substrates. Lake-effect snowfall also determines the species composition within mesic forests. The weighted importance of A. saccharum is significantly greater than of T. canadensis or F. grandifolia within the lake-effect snowbelt, whereas T. canadensis is more plentiful outside the snowbelt. These patterns are probably driven by the influence of snowfall on soil moisture, nutrient availability and fire return intervals. 5Our results imply that a key factor dictating the spatio-temporal patterns of forest communities in the vast region around the Great Lakes is how the lake-effect snowfall regime responds to global change. Snowfall reductions will probably cause a major decrease in the abundance of ecologically and economically important species, such as A. saccharum.

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Samples of ferromanganese nodules from several localities in Lake Michigan have been analyzed for their minor element content utilizing neutron activation techniques. The thorium and uranium levels in Lake Michigan nodules exhibit marked dissimilarities with marine nodules. The radium content of these freshwater nodules is substantially higher than the reported marine values. The concentrations of barium in the Lake Michigan nodules appear to be abnormally high. Although barium could be present as minute segregations of the mineral barite, patterns obtained using the electron microprobe suggest it is evently dispersed throughout the nodules. The average arsenic content of these freshwater nodules is at least twice as great as that reported for highly oxidized marine sediments. If all this arsenic is dissolved and released into Green Bay as a result of changing environmental conditions (eutrophication), the concentration in the water of Green Bay would be several times the maximum permissible level for drinking water.

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Frequency varies.

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Back Row: Elmer Beach, Thomas Gilmore, Hugh Borden, Henry Killilea

2nd Row: Colin Wright, Raymond Beach, Horace Prettyman, Robert Gemmel

Front Row: Richard Dott, Tom H. McNeal, Albert Moore, Henry S. Mahon, William Olcott

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back row (standing): Couch, E. Rosenthal*, Raymond Beach, John Jaycox, Henry Killilea

2nd row (seated): George C. Schemm, William Duff, John Duffy

Front Row: Banks(?), Tom H. McNeil, capt. Horace Prettyman, Dwight Goss

*President of Rugby Association

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Back Row: J. H. Duffie, George DeHaven, Fred Townsend, Ernest Sprague, William Harless, George Wood, L. McMillan

Front Row: E.W. McPherran, Royal Farrand, capt. John Duffy, James Duffy

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Back Row: mngr J.D. Armstrong, Raymond Beach, William C. Malley, Edgar W. McPherran, James Duffy, William D. Ball

2nd Row: Edward(?) DePont, S.L. Bradley, Horace Prettyman, Payne, Anson Hagle

Front Row: James Van Inwagen, Frederic L. Smith, L. McMillan

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Back Row: Capt. Edgar W. McPherran, Howard T. Abbott, James Van Inwagen, James Duffy

2nd Row: Steve Glidden, William C. Malley, Ben Boutwell, Burton Straight, mngr. Thomas Wilkinson

Front Row: G.M. Hull, David Trainer, Horace Prettyman

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Back Row: Thomas L. McKean, Clark J. Sutherland, Tom Chadbourne, David Trainer, Horace Prettyman, David McMoran

3rd Row: Sam Sherman, Lawrence Grosh, Capt. William C. Malley, mngr. George Codd, James E. Duffy

2nd Row: George Jewett

Front Row: George Dygert, George Holden, Roger Sherman