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Precise timing and rate of massive late Quaternary soil denudation

2003; Geological Society of America; Volume: 31; Issue: 10 Linguagem: Inglês

10.1130/g19749.1

1943-2682

M. Jennifer Cooke, Libby A. Stern, Jay L. Banner, Lawrence E. Mack, Thomas W. Stafford, Rickard S. Toomey,

earthquake and tectonic studies

Research Article| October 01, 2003 Precise timing and rate of massive late Quaternary soil denudation M. Jennifer Cooke; M. Jennifer Cooke 1Department of Geological Sciences, University of Texas, Austin, Texas 78712, USA Search for other works by this author on: GSW Google Scholar Libby A. Stern; Libby A. Stern 1Department of Geological Sciences, University of Texas, Austin, Texas 78712, USA Search for other works by this author on: GSW Google Scholar Jay L. Banner; Jay L. Banner 1Department of Geological Sciences, University of Texas, Austin, Texas 78712, USA Search for other works by this author on: GSW Google Scholar Lawrence E. Mack; Lawrence E. Mack 1Department of Geological Sciences, University of Texas, Austin, Texas 78712, USA Search for other works by this author on: GSW Google Scholar Thomas W. Stafford, Jr.; Thomas W. Stafford, Jr. 2Stafford Research Laboratories, Inc., 5401 Western Avenue, Suite C, Boulder, Colorado 80309, USA Search for other works by this author on: GSW Google Scholar Rickard S. Toomey, III Rickard S. Toomey, III 3Kartchner Caverns State Park, P.O. Box 1849, Benson, Arizona 85602, USA Search for other works by this author on: GSW Google Scholar Geology (2003) 31 (10): 853–856. https://doi.org/10.1130/G19749.1 Article history received: 16 Apr 2003 rev-recd: 07 Jul 2003 accepted: 10 Jul 2003 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation M. Jennifer Cooke, Libby A. Stern, Jay L. Banner, Lawrence E. Mack, Thomas W. Stafford, Rickard S. Toomey; Precise timing and rate of massive late Quaternary soil denudation. Geology 2003;; 31 (10): 853–856. doi: https://doi.org/10.1130/G19749.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Strontium isotopes are a unique tool to study soil-erosion dynamics. Changes in Sr isotope ratios (87Sr/86Sr) provide a record of late Quaternary landscape denudation of the Edwards Plateau of central Texas, United States. The use of Sr isotopes as a tracer for soil erosion is based on the observation that, in central Texas, the 87Sr/86Sr ratio of soil correlates with soil thickness. Plants and animals express the 87Sr/86Sr ratio of exchangeable Sr in the soil. Therefore, we use changes in Sr isotope ratios through a well-dated stratigraphic sequence of fossil plants and animals in Hall's Cave, Kerr County, Texas, as a proxy for temporal changes in soil thickness. By using this record we are able to characterize late Quaternary climate-driven soil-erosion dynamics on the Edwards Plateau. We find that continuous erosion removed at least 180 cm of soil at a constant minimum rate of 11 cm/k.y.; this continuous phase of erosion ended ca. 5 ka. The Sr isotope record of soil erosion is consistent with late Quaternary environmental change in central Texas that has been independently modeled by using local and regional climate records. However, the rate of this climate-driven soil-erosion event was an order of magnitude slower than recent soil erosion caused by human land use. These results link erosion to century- to millennial-scale climate change and are cautionary evidence that even greater landscape degradation may result from coincident climatic variability and anthropogenic influences. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.