Plant and Insect Remains from the Wisconsinan Interstadial/Stadial Transition at Wedron, North-Central Illinois

• Published in: Quaternary Research
• Main Authors: Garry, Clarke E., Schwert, Donald P., Baker, Richard G., Kemmis, Tim J., Horton, Diana G., Sullivan, Amy E.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 1990
• Subjects: Empetrum nigrum; Subarctic; Tundra
• Online Access: http://dx.doi.org/10.1016/0033-5894(90)90064-r; http://api.elsevier.com/content/article/PII:003358949090064R?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:003358949090064R?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400020718

Abstract Organic material exposed within a small swale fill in Pit 6 of the Wedron Silica Sand Co. near Wedron in LaSalle County, Illinois, includes well-preserved pollen, plant macrofossils, and insect remains. This material occurs in slackwater sediment in the lower part of the Peddicord Formation, which was deposited as existing valleys were dammed by fluvial aggradation during the initial late Wisconsinan advance of Laurentide ice into the Wedron area. Wood from the organic horizon has a radiocarbon age of 21,460 ± 470 yr B.P. (ISGS-1486). The pollen spectrum is dominated by Picea, Pinus , and Cyperaceae. Plant macrofossils comprise a mix of boreal-forest taxa, including Picea, Larix laricina , and the moss Campylium stellatum subarctic species including Betula glandulosa, Empetrum nigrum , and Selaginella selaginoides along with the predominantly arctic Vaccinium uliginosum var. alpinum, Dryas integrifolia , and Rhododendron lapponicum . The insect fauna contains the western montane ground beetle Opisthius richardsoni several arctic-subarctic ground beetles including Diacheila polita, Helophorus sibiricus , and Pterostichus (Cryobius) caribou and a diverse assemblage of insects that today inhabit the boreal forest. We interpret the biotic record to record a phase in the transition from closed boreal forest to open tundra as climatic conditions deteriorated in advance of continental glaciation.