Southeastern Section - 68th Annual Meeting - 2019

Paper No. 31-11
Presentation Time: 8:00 AM-12:00 PM


HONECK, Jacob W.1, TOBIN, Thomas S.1, TUITE Jr., Michael L.2, FLANNERY, David M.3, FENDLEY, Isabel4, WEAVER, Lucas N.5 and SPRAIN, Courtney J.6, (1)Geological Sciences, University of Alabama, Tuscaloosa, AL 35401, (2)Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, (3)School of Earth, Environmental and Biological Sciences, Queensland University of Technology (QUT), Brisbane, QLD 4000, Australia, (4)Department of Earth and Planetary Science, University of California, Berkeley, McCone Hall, Berkeley, CA 94720, (5)Department of Biology, University of Washington, 247 Life Sciences Building, Seattle, WA 98195, (6)Geomagnetism Laboratory, Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool, L69 7ZE, United Kingdom

A disturbance in the carbon cycle at the K-Pg boundary is inferred from an excursion in the δ13C record of both inorganic and organic carbon. In locations without evidence for impact debris or similar markers, the δ13C excursion has been successfully used to identify the location of the K-Pg boundary. In the Hell Creek region of Montana (USA), previous studies have successfully used δ13Corg curves that record an excursion associated with the K-Pg boundary for correlation within this region (Arens et al., 2014; Arens and Jahren, 2000).

To ensure the accuracy of these curves, care is taken to avoid contamination from modern sources of organic carbon, typically by digging trenches to obtain samples from below the modern weathering profile. We have noticed that despite hand trenching in this region, modern roots can still be found at depths greater than 0.75 m in apparently undisturbed material. To test the importance of sampling depth on measured δ13Corg values, we collected samples from three sections spanning the K-Pg boundary. One was obtained from a traditional hand trench, another from a deep (>1m) trench excavated using a backhoe, and a third from a sediment core. We presume that the sediment core should exhibit the least susceptibility to modern alteration, while the hand trench should be most susceptible. In addition to stratigraphic overlap, all sections were collected within 25 meters of each spatially, so variability between them should largely be explained by sampling technique.

In addition to modern contamination, the lithology of a sample may exert some control on δ13Corg values. This presents a particular challenge in the Hell Creek region because the K-Pg boundary is associated with lithological change between Cretaceous Hell Creek Formation and the overlying Paleogene Tullock Member of the Fort Union Formation. To ensure that any excursions we identify at the K-Pg boundary are not simply the result of this change, we have sampled an additional section through a longer Paleogene interval to examine the relationship between lithology and δ13Corg.

To date we have measured δ13Corg in 119 samples, from three sections and found a negative excursion of roughly 2‰ just above the K-Pg boundary, similar to previous studies. Results from an additional 170 samples will be presented at the conference.