An assemblage of fossil plant spores from the Middle Devonian of New York state (approx. 375,000,000 years old) was extracted using standard palynological techniques. Little is
known of the fine structure of spores of this geologic age since none have been examined with the TEM. Any information gathered will ultimately contribute to the understanding of plant diversity in this time of active plant evolution.
Description
Color poster with text and images (Spring 2009)
Sponsor(s)
University of Wisconsin--Eau Claire Office of Research and Sponsored Programs.