2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 92-5
Presentation Time: 9:10 AM


LARSEN, Isaac J.1, ALMOND, Peter2, EGER, André3, STONE, John O.4, MONTGOMERY, David5 and MALCOLM, Brendon2, (1)Division of Geological and Planetary Sciences, California Institute of Technology, MC 170-25, 1200 E. California Blvd, Pasadena, CA 91125, (2)Soil and Physical Sciences Group, Lincoln Univ, Division of Soil, Plant and Ecological Sciences, PO Box 84, Canterbury, New Zealand, (3)Institute of Earth and Environmental Science, University of Potsdam, Karl-Liebknecht-Str. 24-25, 14476 Potsdam-Golm, Potsdam, 14476, Germany, (4)Department of Earth and Space Sciences and Quaternary Research Center, University of Washington, Box 351310, 070 Johnson Hall, Seattle, WA 98195, (5)Department of Earth and Space Sciences and Quaternary Research Center, University of Washington, 4000 15th Avenue NE, Box 351310, Seattle, WA 98195-1310, larseni@caltech.edu

The lack of soil production and weathering rate data from Earth’s most rapidly uplifting mountains has made it difficult to determine whether weathering rates increase or decline in response to rapid erosion. Understanding the relationship between erosion and weathering rates is critical for evaluating whether mountain uplift can influence the geological carbon cycle and climate. We measured beryllium-10 concentrations in soils from the western Southern Alps, New Zealand, which demonstrate that soil is produced from bedrock more rapidly than previously recognized, at rates from 0.1 to 2.5 mm yr-1. Weathering intensity data further indicate that soil chemical denudation rates increase proportionally with erosion rates. We also used beryllium-10 to determine catchment-scale denudation rates, which reach as high as 12 mm yr-1. Published river solute flux data suggest that catchment-scale weathering rates are comparable to the soil weathering rates, despite the much higher rates of catchment denudation. These high weathering rates suggest that soils may be a key location for denudation in tectonically-active mountains and support the view that mountains play a key role in global-scale chemical weathering.