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Middle-Holocene mobilization of aeolian sand in western upper Michigan and the potential relationship with climate and fire

Bibliographic Data

ID12267258
AuthorsAlan F Arbogast (0000-0001-6289-1732, Michigan State University, corresponding author), Susan C Packman (University of Wales)
Year2004
Volume14
Issue3
Pages464-471
Publication date2004-04-01
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1191/0959683604hl723rr
OpenAlexW2108651535
LanguageEN
Citations received8
References cited44

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

Aeolian processes · Geography · Geomorphology · Holocene · Physical geography · Thermoluminescence dating · Aeolian processes and effects · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology

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Citations per year0.38
Citation span2005 - 2025 (21)
Highly citedNo

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