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Asymmetric vegetation responses to mid-Holocene aridity at the prairie–forest ecotone in south-central Minnesota

Published online by Cambridge University Press:  20 January 2017

Charles E. Umbanhowar Jr. ,
Philip Camill ,
Christoph E. Geiss  and
Rebecca Teed
Charles E. Umbanhowar Jr.*
Affiliation:
Department of Biology, St. Olaf College, 1520 St. Olaf Avenue, Northfield, MN 55057, USA
Philip Camill
Affiliation:
Department of Biology, Carleton College, One North College Street, Northfield, MN 55057, USA
Christoph E. Geiss
Affiliation:
Department of Physics, Trinity College, 300 Summit Street, Hartford, CT 06106, USA
Rebecca Teed
Affiliation:
Limnological Research Center, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, MN 55455, USA
*
⁎Corresponding author. Fax: +1 507 646 3968. E-mail address:[email protected] (C.E. Umbanhowar).
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Abstract

The mid-Holocene (ca. 8000–4000 cal yr BP) was a time of marked aridity throughout much of Minnesota, and the changes due to mid-Holocene aridity are seen as an analog for future responses to global warming. In this study, we compare the transition into (ca. 9000–7000 yr ago) and out of (ca. 5000–2500 yr ago) the mid-Holocene (MH) period at Kimble Pond and Sharkey Lake, located along the prairie forest ecotone in south-central Minnesota, using high resolution (∼ 5–36 yr) sampling of pollen, charcoal, sediment magnetic and loss-on-ignition properties. Changes in vegetation were asymmetrical with increasing aridity being marked by a pronounced shift from woodland/forest-dominated landscape to a more open mix of grassland and woodland/savanna. In contrast, at the end of the MH, grassland remained an important component of the landscape despite increasing effective moisture, and high charcoal influxes (median 2.7–4.0 vs. 0.6–1.7 mm2 cm− 2 yr− 1 at start of MH) suggest the role of fire in limiting woodland expansion. Asymmetric vegetation responses, variation among and within proxies, and the near-absence of fire today suggest caution in using changes associated with mid-Holocene aridity at the prairie forest boundary as an analog for future responses to global warming.

Keywords

ClimateEcotoneFireMid-Holocene aridityPrairie forest borderBig Woods
Type
Research Article
Information
Quaternary Research , Volume 66 , Issue 1 , July 2006 , pp. 53 - 66
Copyright
University of Washington

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