GSA Annual Meeting in Phoenix, Arizona, USA - 2019

Paper No. 15-5
Presentation Time: 9:05 AM


LUKENS, William E.1, FOX, David L.2, SNELL, Kathryn E.3, WIEST, Logan A.4, LAYZELL, Anthony L.5, UNO, Kevin T.6, POLISSAR, Pratigya J.6, MARTIN, Robert A.7, FOX-DOBBS, Kena8 and PELÁEZ-CAMPOMANES, Pablo9, (1)Department of Geology and Environmental Science, James Madison University, Harrisonburg, VA 22807, (2)Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, (3)Department of Geological Sciences, University of Colorado Boulder, Boulder, CO 80309, (4)Department of Geosciences, Mansfield University of Pennsylvania, Mansfield, PA 16933, (5)Kansas Geological Survey, University of Kansas, 1930 Constant Ave, Lawrence, KS 66047, (6)Biology and Paleoenvironment, Lamont Doherty Earth Observatory, 61 Route 9W, PO Box 1000, Palisades, NY 10964-8000, (7)Department of Biology, Murray State University, Murray, KY 42071, (8)Department of Geology, University of Puget Sound, 1500 N Warner St, Tacoma, WA 98416, (9)Paleobiology, National Museum of Natural History, Madrid, 28006, Spain

Terrestrial paleoenvironmental reconstructions from the Pliocene Epoch (5.3-2.6 Ma) are rare from the North American continental interior, but are important because they provide insight into the evolutionary context of modern landscapes and ecological systems. Pliocene marine records indicate that global climate was warmer and atmospheric pCO2 was higher than pre-industrial conditions and potentially analogous to future warming scenarios. In this study, we investigate sedimentary environments and paleoclimate conditions from the Meade Basin of southwest Kansas, a moderately sized basin formed from dissolution and withdrawal of deep evaporites. Pliocene intervals of the Meade Basin have yielded classic faunal assemblages representing the early to middle Blancan North American Land Mammal Age (~ 4.5-3.2 Ma). We reconstruct paleoenvironments using lithofacies analysis, paleopedology, and ichnology. The stratigraphic interval we examined is bounded by large-scale, fluvial trunk channels with SSW paleocurrent trends—tangential to modern drainages—likely due to local halotectonic subsidence during the Neogene. The stratigraphic interval between these fluvially dominated phases consists of palustrine landscapes with temporally and laterally variable subaqueous and subaerial facies. Paleosols are abundant; however, most pedotypes are poorly to variably drained, and so their elemental compositions do not reflect local climate state. The few mature, oxidized, and relatively well-drained paleosols observed contain elemental signatures consistent with sub-humid climate conditions. Frequent and recursive ponding events are discerned through the tiering of burrows (Camborygma isp.) similar to those produced by modern crayfish. The drivers of these flooding events are most likely episodic halotectonic subsidence and groundwater discharge, though influence from intervals of relatively wetter climate cannot be ruled out. By the late middle Pliocene, landscapes returned to fluvially dominated environments as sedimentation began to outpace accommodation. Our results collectively indicate that climate was likely wetter than modern conditions in the early to middle Pliocene in the western Great Plains, contrary to forecasts for the region under current pCO2-driven warming.