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South-central Section GSA 2013 Austin. Steven G. Driese*, Lee C. Nordt, Amos V. Culbertson, Emily J. Beverly, Gary E. Stinchcomb, & Forrest Williamson (STATS) Department of Geology, Paleoclimatology Research Group One Bear Place #97354, Baylor University
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South-central Section GSA 2013 Austin Steven G. Driese*, Lee C. Nordt, Amos V. Culbertson, Emily J. Beverly, Gary E. Stinchcomb, & Forrest Williamson (STATS) Department of Geology, Paleoclimatology Research Group One Bear Place #97354, Baylor University Waco, TX 76798-7354 ; *Steven_Driese@baylor.edu Multi-Proxy Approaches to Interpreting Climate and Soil Duration in the Deep-Time Geologic Record Using Vertisols
Studies of Surface Soil and Weathering Systems as Proxy Analogs for Paleosols • Have lead to major improvements for geoscientists in interpreting climate from the fossil soil (paleosol) record using studies of surface soil systems • (a) Paleoprecipitation (MAP) • (b) Seasonality of paleoprecipitation • (c) Paleotemperature • (d) Soil drainage and maturitycharacteristics
Jenny’s (1941) Environmental Factor Model (climate, organisms, relief, parent material, and time) INPUT (cl, o, r, p, t,…) Function (f) OUTPUTf(cl, o, r, p, t,…) equals Soil (S) or soil property (s) Soils are a multi-variable system …also, climate influence on soil system is non-linear Demonstrated by Jenny (1941) and many others
Vertisols: High Shrink-Swell, High Clay-Content Soils; Abundant in Texas Coast Prairie Texas Vertisol “Climosequence”: NSF EAR-9814607 (Driese, Nordt and Mora); University of Tennessee- Knoxville, Baylor, TAMU, USDA-NRCS
Parent Material: Beaumont Fm. (>35-40 ka) alluvium: Texas Coast Prairie Lake Charles: MAP 1050-1350 mm League Series: MAP 1350-1450 mm Laewest Series: MAP 900-1050 mm Victoria Series: MAP 800-900 mm
New Vertisol MAP Proxy Nordt and Driese (2010) Geology, v. 38, p. 407-410.
Lake Brownwood Spillway, TX Culbertson (2013) M.S. Thesis, Baylor University
Upper Paleosol Interval Bssg1 Pedogenic siderite Bssg2 Culbertson(2013) Baylor Univ. M.S. Thesis
Lower Paleosol Interval Abrupt, rapid drowning Culbertson(2013) Baylor Univ. M.S. Thesis
Upper Paleosol Interval Culbertson(2013) Baylor Univ. M.S. Thesis Slow, gradual drowning
Database workflow PRISM (MAP & MAT) NED (elevation) (Gary Stinchcomb, former Baylor GEO post-doc (now @ Penn. State) + Forrest Williamson from Baylor STATS) NRCS/USDA (soils) NLCD (land cover) Paleosol Paleoclimate Model (BU-PPM v. 1.0) Database aggregation & management Paleosol literature time period morphology geochemistry, etc… researcher
New Paleoclimate Proxy – BU-PPM 1.0 Stinchcomb et al. (2013) Geochimica et Cosmochimica Acta, in review Based on 685 U.S. Soil Profiles and Partial Least Squares Regression of 11 Major Oxides
New Paleoclimate Proxy – BU-PPM 1.0 Stinchcomb et al. (2013) Geochimica et Cosmochimica Acta, in review Based on 685 U.S. Soil Profiles and Partial Least Squares Regression of 11 Major Oxides
BU-PPM1.0 results: Baylor enlarged U.S. data set vs. original Marbut (1935) soil data base used for CIA-K Stinchcomb et al. (2013) Geochimica et Cosmochimica Acta, in review
Brownwood – Paleotemperatures? Lower Paleosol Interval Upper Paleosol Interval
Young Soil vs. Dry Soil? Mass-Balance Results for TX Vertisols Soil Age (yr) MAP (mm) Ships 1000 1120 Pledger 6600 1200 Burleson 16000 1120 Lake 40000 1150 Charles Mercedes 7500 700 Older South Texas soil (Mercedes) in lower MAP resembles younger East Texas soil (Ships) in higher MAP