XVI INQUA Congress
Paper No. 65-5
Presentation Time: 9:30 AM-9:50 AM


FREDLUND, Glen, Geography, Univ of Wisconsin Milwaukee, P.O. Box 413, Milwaukee, WI 53201, fredlund@uwm.edu, HOLLIDAY, Vance, Anthropology, The Univ of Arizona, 1009 E South Campus Drive, Building #30A, Tucson, AZ 85721-0030, and JOHNSON, Eileen, Museum of Texas Tech University, Texas Tech Univ, Museum Box 43191, Lubbock, TX 79409-3191

Pollen, phytolith, and carbon isotope records from the Southern High Plains of Texas and New Mexico provide evidence for both abrupt and gradual shifts in climate and vegetation. The inferences are based on a comparison of fossil records from 3 playa fill sequences: San Jon Site, NM, Barnes Playa, TX, and Nall Playa, TX. Data from the Lubbock Lake Site, and scattered other playa localities contribute to the body of evidence.

Full glacial vegetation was characterized by sagebrush and C3-dominated grasslands. Limited pollen evidence for spruce and other trees suggests isolated populations along fire-protected escarpments during the full glacial times. By 12,000 RCYBP grasslands composition began to shift from C3-domination towards mixed C3/C4 grassland. Higher levels of tall-grass (Panicoid) phytoliths, along with greater diatom production, occurred between 11,400 to 10,200 RCYBP. While this period generally represents more mesic conditions, suggestion of abrupt climatic changes throughout this transitional window are also present. Across this Pleistocene-Holocene transition there was a slow, steady rise in shortgrass (Chloridoid) C4 grasses culminates in the rise of the short-grass ecosystem between 8000 and 7500 BP. The record of vegetation change has important implications for bison evolution and Paleoindian adaptation during across the Pleistocene-Holocene transition.

XVI INQUA Congress
General Information for this Meeting
Session No. 65
Paleoindian Western North America: Climate and Life at the Last Glacial Termination
Reno Hilton Resort and Conference Center: Tahoe
8:00 AM-12:00 PM, Tuesday, July 29, 2003

Geological Society of America Abstracts with Programs, , p. 190

© Copyright The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.