ANALYZING THE RELATIONSHIP BETWEEN SEA LEVEL, GEOGRAPHIC RANGE, AND INVASION EVENTS IN CINCINNATIAN (LATE ORDOVICIAN ) BRACHIOPODS USING GIS
Species ranges were reconstructed both spatially and temporally (following the sequence stratigraphic framework of Holland [1993]) using a Geographic Information System to quantitatively derive the geographic area of species ranges and describe lateral migration patterns in response to regional sea-level fluctuation. Geographic extent of species' ranges across multiple time slices enabled analysis of habitat tracking patterns, which were examined through time-slice animations, as well as their close link to sea-level through statistical analyses.
Statistical tests support the link between species' geographic ranges and regional sea-level fluctuation; geographic range expands as water depth increases with relative sea-level rise. Species also track preferred habitats by lateral migration along the carbonate-siliciclastic ramp in response to sea-level change. Individual species, as well as much of the total population within each chronostratigraphic time-slice, display congruent patterns of movement throughout the Cincinnati Arch. The Richmondian Invasion, an influx of species into the Cincinnati Arch, resulted in regional extinction and the eventual replacement of many native species with immigrant taxa. Statistical analyses indicate that the native species which persisted into the Richmondian were only those with large geographic ranges. This suggests species with larger ranges, typically generalists, were best able to compete in the new invasive regime.