VIRTUAL
POSTER SESSION
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Goal Examine the species-level composition of two wet-interval floras from the Early Permian of North-Central Texas
1. Are the dominant xeric (dry) and hydric (wet) taxa different between floras? 2. How does the taxonomic diversity differ between floras? 3. What are the taphonomic differences between the two sites?
The climate fluctuated glaciers waxed and waned, but there is little resolution of the finer details of these climate swings The rock record in lower latitude ice free area (far-field) have provided more detailed resolution of glacial patterns for the Pennsylvanian (ie, cyclothems) The far-field rock record of the Permian differs greatly and does not have as great resolution; however, the paleobotanical record records intercalations of dry-adapted floras and wet-adapted floras, possibly driven by climate fluctuations related to polar ice fluctuations.
Floras from the early Permian of Texas exhibit oscillations between xeric (dry) and hydric (wet) floras
Paleosol data (Tabor and Montanez) suggests a slightly wetter interval at this point, during an overall trend from cooler/wetter to hotter/dryer
Floras were scanned using a hand lens/microscope and characterized in terms of taxonomic composition. Composition was assessed using the quadrat method of Pfefferkorn, Mustafa, and Hass (1975) Each hand sample was treated as a sampling quadrat; taxa on that quadrat were noted as present/absent, regardless of size/number of individual specimens present. Each quadrat represents both surfaces of a given hand sample Quadrat/hand-sample size was assessed roughly by making two orthogonal axis measurements in order to: Compare quadrat size to taxonomic richness Compare total surface area between the two floras
The
Floras from Cattle Tank and Farmer Tank are significantly different
Thanks to the Smithsonian Office of the Director for funding the senior author's participation in the Research Training Program and to Cindy Looy for assistance with conifers and figures. |
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Smithsonian
Institution The information presented here, as part of the Research Training Program Virtual Poster Session, represents preliminary data as the result of ten-weeks of investigation in-residence at the National Museum of Natural History. This is not an official publication nor are the finding presented here necessarily conclusive or definitive. As preliminary information, these results and/or findings should not be cited as part of conclusive work. Please contact the author if you would like further information about this research as well as the resulting scientific publication and/or presentation. |