Late Wisconsinan Wood and Other Tree Remains in the Presumpscot Formation, Portland Maine

Authors

  • Fay Hyland Department of Botany and Plant Pathology, University of Maine, Orono, Maine 04473
  • Woodrow B. Thompson Maine Geological Survey, Department of Conservation, Augusta, Maine 04333
  • Robert Stuckenrath, Jr. Radiation Biology Laboratory, Smithsonian Institution, Rockville, Maryland 20852

DOI:

https://doi.org/10.4138/1966

Abstract

Well preserved tree remains have been discovered in glaciomarine clay of the Late Wisconsinan Presumpscot Formation at Portland, Maine. Logs, branches, cones, and needles occurred, just above the contact between the clay and underlying gravel deposit. They were the first tree remains to be found in the Presumpscot Formation. The radiocarbon ages of the logs vary considerably, but their true age is believed to be between 12,000 and 12,500 years. Specimens from the Portland locality are described in detail in the present study. The logs and needles have been identified as spruce, and the associated cones indicate that the species is white spruce, (Picea glauca (Moench) Voss). The concentration and degree of preservation of the remains suggest a local source - possibly the nearby hills that were above sea level in late-glacial time. The occurrence of the spruce logs in Portland also indicates that trees may have colonized southwestern coastal Maine very soon after the retreat of Late Wisconsinan glacial ice from this area.

Downloads

Published

1978-12-01

How to Cite

Hyland, F., Thompson, W. B., & Stuckenrath, Jr., R. (1978). Late Wisconsinan Wood and Other Tree Remains in the Presumpscot Formation, Portland Maine. Atlantic Geoscience, 14(3). https://doi.org/10.4138/1966

Issue

Vol. 14 No. 3 (1978)

Section

Reports

License

All material contained in Atlantic Geology is copyrighted by the journal. Permission to photocopy for internal or personal use or for the internal or personal use of specific clients is granted by Atlantic Geology to libraries and other users registered with the Copyright Clearance Center (CCC), provided that the stated fee per copy is paid directly to the CCC, 21 Congress Street, Salem, Massachusetts 01970 USA. Other requests should be addressed to one of the journal editors, or sent to Atlantic Geology, Box 116, Acadia University, Wolfville, NS, Canada B4P 2R6. Permission to use a single graphic for which Atlantic Geology owns copyright is considered “fair dealing” under the Canadian Copyright Act and “fair use” by the journal, and no other permission need be granted, subject to the image being appropriately cited in all reproductions. The same fair dealing/fair use policy applies to sections of text up to 100 words in length.