EFFECTS OF THE LATE PALEOZOIC CLIMATE TRANSITION ON SOIL ECOSYSTEMS OF THE APPALACHIAN BASIN, (MONONGAHELA AND DUNKARD GROUPS): EVIDENCE FROM ICHNOFOSSILS
A study along a 50 km long, north-south transect of multiple 30-50 m high sections of the Monongahela and Dunkard groups through southeast Ohio and West Virginia resulted in the recognition of 12 pedotypes with distinct ichnocoenoses. Ichnofossils included rhizoliths, lined and unlined burrows, plant-feeding traces, and coprolites produced by various plants, larval and adult arthropods, and vertebrates. Soil-forming environments included palustrine, levee, proximal to distal floodplain, interfluve, backswamp, marsh, and fen settings. In general, ichnocoenoses were less diverse and comprised of shallow and simple ichnofossils in poorly drained Entisols and Inceptisols of the lower part of the studied sections. Ichnocoenoses became more diverse and comprised of deeper and more complex ichnofossils in well-drained Vertisols in the middle portion of the section. Near the top of the studied section, diversity and abundance of traces decreased again, but maintained their depth in calcareous Vertisols. The ichnocoenoses indicate an upward decrease in precipitation and an increase in seasonality. In addition to this trend through time, however, the nature of the ichnocoenoses varied within each interval recording short-term oscillations in soil properties and precipitation.
Terrestrial ichnocoenoses serve as an important archive of environmental data not otherwise preserved in the sedimentary record. Analysis of these suites of ichnofossils is critical to evaluating climatic conditions in deep time and their effects on soil ecosystems.