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Age calibration of carbonate rind thickness in late pleistocene soils for surficial deposit age estimation, Southwest USA

Published online by Cambridge University Press:  20 January 2017

Lee Amoroso
Lee Amoroso*
Affiliation:
U.S. Geological Survey, 2255 North Gemini Drive, Flagstaff, AZ 86001, USA
*
*Fax: +1 928 556 7169.Email Address:[email protected]
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Abstract

Carbonate rinds have been used for cross-correlation of landforms as well as a quantitative indicator of soil age. Using the measured rind thickness of clasts found within a deposit, whose age has been independently determined, allows the construction of a calibrated surface-age proxy. Measurements were taken at sites within the Mojave Desert, the northwestern Sonoran Desert, the southern Great Basin, and the western Colorado Plateau. These sites are all within about 300 km of the intersection of the borders of the states of California, Arizona, and Nevada. In the study area, elevation varied from 200 to 1200 m, MAP was from 95 to 195 mm, and MAT was from 18.4° to 23.3°C. The calibrated proxy, while not accounting for the effects of parent material or climate on rind development, does show a strong correlation (R2 = 0.74, P < 0.05) between carbonate rind thickness and surface age for deposits of late to middle Pleistocene age. The calibrated chronosequence, rind thickness = 0.0889 + 0.0079 [surface age]), is in general valid over a large region of southwestern United States. This statistical relation suggests that parent material, climate, and elevation may not be as strong a control on carbonate accumulation as is age for younger soils.

Keywords

Carbonate rindsRock coatingsSurface ageChronosequenceCarbonate cutan
Type
Short Paper
Information
Quaternary Research , Volume 65 , Issue 1 , January 2006 , pp. 172 - 178
Copyright
University of Washington

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References

Amoroso, L., (2001). Studies in Quaternary Geology of Arizona: Active Tectonics"Relationship of Soils to Surficial Geology. Unpublished Dissertation thesis, Arizona State University, .Google Scholar
Amundson, R., Wang, Y., Chadwick, O.A., Trumbore, S., McFadden, L.D., Wells, S.G., DeNiro, M., (1994). Factors and processes governing 14C content of carbonate in desert soils. Earth and Planetary Science Letters 125, 385–405.Google Scholar
Anderson, R.S., Betancourt, J.L., Mead, J.I., Hevly, R.H., Adam, D.P., (2000). Middle- and late-Wisconsin paleobotanic and paleoclimatic records from the southern Colorado Plateau, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 155, 31–57.Google Scholar
Bender, G.L., (1982). Reference Handbook on the Deserts of North America. Greenwood Press, Westport, CT.Google Scholar
Callen, R.A., Wasson, R.J., Gillespie, R., (1983). Reliability of radiocarbon dating of pedogenic carbonate in the Australian arid zone. Sedimentary Geology 35, 1–14.Google Scholar
Chadwick, O.A., Davis, J.O., (1990). Soil-forming intervals caused by eolian sediment pulses in the Lahontan basin, northwestern Nevada. Geology 18, 243–246.2.3.CO;2>CrossRefGoogle Scholar
Colman, S.M., Dethier, D.P., (1986). An overview of rates of chemical weathering. Colman, S.M., Dethier, D.P., Rates of Chemical Weathering of Rocks and Minerals Academic Press, New York., 1–20.Google Scholar
Fenton, C.R., Webb, R.H., Pearthree, P.A., Cerling, T.E., Poreda, R.J., (2001). Displacement rates on the Toroweap and Hurricane faults: implications for Quaternary downcutting in the Grand Canyon, Arizona. Geology 29, 1035–1038.Google Scholar
Gile, L.H., Hawley, J.W., Grossman, R.B., (1981). Soils and Geomorphology in the Basin and Range Area of Southern New Mexico-Guidebook to the Desert Project. New Mexico Institute of Mining and Technology, Socorro, NM., 222 .Google Scholar
Jenny, H., (1941). Factors of Soil Formation. McGraw-Hill, New York.Google Scholar
Kneupfer, R.L.K., (1988). Estimating ages of late Quaternary stream terraces from analysis of weathering rinds and soils. Geological Society of America Bulletin 100, 1224–1236.Google Scholar
Ku, T.L., Bull, W.B., Freeman, S.T., Knauss, K.G., (1979). Th230-U234 dating of pedogenic carbonates in gravelly desert soils of Vidal Valley, Southeastern California. Geological Society of America Bulletin 90, 1063–1073.2.0.CO;2>CrossRefGoogle Scholar
Ludwig, K.R., Paces, J.B., (2002). Uranium-series dating of pedogenic silica and carbonate, Crater Flat, Nevada. Geochimica et Cosmochimica Acta 66, 487–506.Google Scholar
Machette, M.N., (1985). Calcic soils of the southwestern United States. Weide, D.L., Soils and Quaternary Geology of the Southwestern United States Geological Society of America, Boulder, CO., 1–22.Google Scholar
Mayer, L., Mcfadden, L.D., Harden, J.W., (1988). Distribution of calcium carbonate in desert soils: a model. Geology 16, 303–306.Google Scholar
McDonald, E., McFadden, L.D., (1994). Quaternary stratigraphy of the Providence Mountains piedmont and preliminary age estimates and regional stratigraphic correlations of Quaternary deposits in the Eastern Mojave Desert, California. McGill, S.F., Ross, T.M., Geological Investigations of an Active Margin: San Bernardino, California . Geological Society of America Cordilleran Section Guidebook, 27th Annual Meeting. Geological Society of America, Boulder, CO., 205–210.Google Scholar
McDonald, E., McFadden, L.D., Wells, S.G., (1995). The relative influence of climate change, desert dust, and lithologic control on soil-geomorphic processes on alluvial fans, Mojave Desert, California: summary of results. San Bernardino County Museum Association 42, 35–42.Google Scholar
McFadden, L.D., (1988). Climatic influences on rates and processes of soil development in Quaternary deposits of southern California. Reinhardt, J., Sigleo, W.R., Paleosols and Weathering through Geologic Time: Principals and Applications Geological Society of America, Boulder., 153–178.Google Scholar
McFadden, L.D., McDonald, E.V., Wells, S.G., Anderson, K., Quade, J., Forman, S.L., (1998). The vesicular layer and carbonate collars of desert soils and pavements: formation, age, and relation to climate change. Geomorphology 24, 101–145.Google Scholar
Pendall, E.G., Harden, J.W., Trumbore, S.E., Chadwick, O.A., (1994). Isotopic approach to soil carbonate dynamics and implications for paleoclimatic interpretations. Quaternary Research 42, 60–71.Google Scholar
Pustovoytov, K., (1998). Pedogenic carbonate cutans as a record of the Holocene history of relict tundra-steppes of the Upper Kolyma Valley (North-Eastern Asia). Catena 34, 185–195.Google Scholar
Pustovoytov, K., (2003). Growth rates of pedogenic carbonate coatings on coarse clasts. Quaternary International 106"107, 131–140.CrossRefGoogle Scholar
Quade, J., Forester, R.M., Whelan, J.F., (2003). Late Quaternary paleohydrologic and paleotemperature change in southern Nevada. Enzel, Y., Wells, S.G., Lancaster, N., Paleoenvironments and Paleohydrology of the Mojave and Southern Great Basin Deserts . Geological Society of America Special Paper. vol. 368, Geological Society of America, Boulder, CO., 165–188.Google Scholar
Reheis, M.C., Goodmacher, J.C., Harden, J.W., McFadden, L.D., Rockwell, T.K., Shroba, R.R., Sowers, J.M., Taylor, E.M., (1995). Quaternary soils and dust deposition in southern Nevada and California. Geological Society of America Bulletin 107, 1003–1022.Google Scholar
Schlesinger, W.H., (1985). The formation of caliche in soils of the Mojave Desert. California. Geochimica et Cosmochimica Acta 49, 57–66.Google Scholar
Sharp, W.D., Ludwig, K.R., Chadwick, O.A., Amundson, R., Glaser, L.L., (2003). Dating fluvial terraces by 230Th/U on pedogenic carbonate, Wind River Basin, Wyoming. Quaternary Research 59, 139–150.Google Scholar
Stephens, D.B., (1996). Vadose Zone Hydrology. Lewis Publishers, Boca Raton, FL.Google Scholar
Swan, A.R.H., Sandilands, M., (1995). Introduction to Geological Data Analysis. Blackwell Science, Ltd., .Google Scholar
Treadwell-Steitz, C., McFadden, L.D., (2000). Influence of parent material and grain size on carbonate coatings in gravelly soils, Palo Duro Wash, New Mexico. Geoderma 94, 1–22.Google Scholar
Van Devender, T.R, Thompson, R.S, Betancourt, J.L., (1987). Vegetation history of the deserts of southwestern North America; the nature and timing of the Late Wisconsin"Holocene transition. In:Ruddiman, W.F, Wright Jr., H.E., (Eds.), North America and Adjacent Oceans During the Last Deglaciation . Geological Society of America, The Geology of North America, v. K-3. Boulder, CO, pp. 323"352..Google Scholar
Vincent, K.R., Bull, W.B., Chadwick, O.A., (1994). Construction of a soil chronosequence using the thickness of pedogenic carbonate coatings. Journal of Geoscience Education 42, 316–324.Google Scholar
Wang, Y., Amundson, R., Trumbore, S., (1994). A model for soil 14CO2 and its implications for using 14C to date pedogenic carbonate. Geochimica et Cosmochimica Acta 58, 393–398.Google Scholar
Wells, S.G., McFadden, L.D., (1990). Preliminary results of age estimations and regional correlations of Quaternary alluvial fans within the Mojave Desert of southern California. San Bernardino County Museum Association 37, 45–53.Google Scholar
Wells, S.G., McFadden, L.D., Dohrenwend, J.C., (1987). Influence of late Quaternary climatic changes on geomorphic and pedogenic processes on a desert piedmont, eastern Mojave Desert, California. Quaternary Research 27, 130–146.Google Scholar
Weng, C., Jackson, S.T., (1999). Late Glacial and Holocene vegetation history and paleoclimate of the Kaibab Plateau, Arizona. Palaeogeography, Palaeoclimatology, Palaeoecology 153, 179–201.Google Scholar