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Michael
Nowak Dr. Scott Wing, Ph.D.
"I have learned more about science this summer than I have in the last three years of college." |
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Lateral Variation in an Early Paleogene Lignite, Williston Basin, North Dakota, USA In
light of recent evidence validating the reality of anthropogenic warming,
there is a concerted effort to understand Global Climate change and
its effect on plants and animals. In the early Paleogene, approximately
55 million years ago, there was a rapid Global warming event called
the Initial Eocene Thermal Maximum. This project is part of a larger
effort to understand floral response to rapid climate change in the
past. The most effective way to study floral trends in the past is
through dispersed fossil pollen, or palynoflora. Compared to most
megafossils (leaves and fruits), pollen preserves very well in fine-grained
sedimentary rocks. Stratigraphic sampling density is therefore much
greater. However, when there are apparent changes in the palynoflora
within a stratigraphic section, it is difficult to know whether they
represent large regional changes in the plant community, or whether
they merely represent local changes such as a windstorm, or a fire.
In an attempt to clarify this problem, this study investigates the
lateral palynofloral variation within an early Paleogene lignite.
Preliminary analysis of the data indicates significant palynofloral
variability between the samples. The Betulaceous and Taxodiaceous
taxa seem to be responsible for the majority of variation between
the samples. There also seems to be a relatively strong correlation
between the thickness of the lignite and the abundant taxa in the
sample. Samples within a thick section of the lignite tend to be dominated
by Betulaceae, and thin sections tend to be dominated by Taxodiaceae.
To understand this relationship much more data will have to be collected. This research was supported by a grant from the Bill and Jean Lane Endowment in honor of Robert Fri. |