South-Central Section - 51st Annual Meeting - 2017

Paper No. 2-10
Presentation Time: 11:20 AM

AN ICHNOLOGICAL PROXY FOR THE RESPONSE AND RECOVERY OF SOIL FAUNA ACROSS THE K-PG EXTINCTION INVERVAL: BIG BEND NATIONAL PARK


WIEST, Logan A.1, LUKENS, William E.1, DRIESE, Steven G.1, TUBBS, Jack D.2, LETOURMY, Yohan1 and LESLIE, Caitlin E.1, (1)Terrestrial Paleoclimatology Research Group, Department of Geosciences, Baylor University, One Bear Place #97354, Baylor University, Waco, TX 76798-7354, (2)Department of Statistical Science, Baylor University, Waco, TX 76798, Logan_Wiest@baylor.edu

We present the results of an ichnological proxy for ecosystem stress applied to a continental Cretaceous-Paleogene (K-Pg) mass-extinction interval at Big Bend National Park, which reveals an ecological perturbation that is otherwise not apparent in the lithology or traditional paleontology. The trace-fossil record of soil-dwelling organisms within alluvial deposits and associated paleosols from the Dawson Creek section contains Planolites, Celliforma, Skolithos and Naktodemasis (adhesive meniscate burrows; AMB), however our quantitative efforts focused on AMB (n=801) due to the pervasiveness of this trace throughout the study interval. Previous studies demonstrate AMB were likely generated by burrower bugs or cicada nymphs. As a proxy for the body size of the tracemaker, our dataset indicates that a smaller burrow diameter is statistically (α < 0.05) correlated with poor drainage (mean = 6.4±0.2 mm) in comparison to moderately (7.1±0.2 mm) or well-drained conditions (7.1±0.1 mm) within paleosols (n=15). Soil order also has a correlation to body size within the soil-dwelling community - Entisols contain smaller-diameter burrows (6.5±0.1 mm) than Inceptisols (7.2±0.1 mm) or Vertisols (7.1±0.2 mm). Whereas the precise stratigraphic placement of the K-Pg boundary is unknown at Big Bend due to the lack of diagnostic geochemical indicators and sparsity of age-specific body fossils, a previous approximation of the position based on a combination of absolute ages and rates of pedogenesis has tentatively placed the boundary at 5 m above a channel sandstone containing the highest dinosaur remains and 26 m below a Pg assemblage. Our dataset reveals an abrupt decrease in AMB diameter (5.6±0.3 mm) within a paleosol (referred to as P22) immediately superjacent to the highest dinosaur remains. P22 is a well-drained Vertisol, therefore the anomalous shift cannot be attributed to drainage or paleosol order. Furthermore, AMB diameters remain smaller on average above P22 (6.6±0.1 mm) in comparison to the burrows constructed during the interval known to be Cretaceous in age (7.3±0.1 mm). We interpret the trace fossils in P22 to signify the post-extinction recovery community and propose that the stratigraphic position of the K-Pg boundary in Big Bend is represented by the dinosaur-bearing channel sandstone subjacent to P22.