Middle-Holocene mobilization of aeolian sand in western upper Michigan and the potential relationship with climate and fire
A forested dunefield covers the Baraga Plains in western upper Michigan. The ages of five dunes, from across the dunefield, were determined by optically stimulated luminescence (OSL), employing the single-aliquot regenerative-dose (SAR) method on quartz grains. The results indicate that sand mobiliz...
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| Veröffentlicht in: | Holocene (Sevenoaks) 2004-05, Vol.14 (3), p.464-471 |
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| creator | Arbogast, Alan F. Packman, Susan C. |
| description | A forested dunefield covers the Baraga Plains in western upper Michigan. The ages of five dunes, from across the dunefield, were determined by optically stimulated luminescence (OSL), employing the single-aliquot regenerative-dose (SAR) method on quartz grains. The results indicate that sand mobilization was restricted to the middle Holocene, at around 7 ka. Four environmental variables, rapid climatic oscillations, fire, strong winds and a dry climate are invoked as a combined cause of dune formation. This study provides further evidence for the wide extent of aeolian activity in the upper Midwest of North America during the middle Holocene. |
| doi_str_mv | 10.1191/0959683604hl723rr |
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| source | SAGE Complete |
| title | Middle-Holocene mobilization of aeolian sand in western upper Michigan and the potential relationship with climate and fire |
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