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Holocene Soils and Soil-Geomorphic Relations in an Arid Region of Southern New Mexico1

Published online by Cambridge University Press:  20 January 2017

Leland H. Gile
Leland H. Gile*
Affiliation:
Soil Survey Investigations, Soil Conservation Service, Texas Tech University Lubbock, Texas 79409 USA
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Abstract

A study area in an arid region of southern New Mexico is in basin-and-range topography and includes both a river valley and a closed basin. Holocene soils occur in valley fills and low terraces between Pleistocene fans, in and near drainageways on the fan-piedmont, on ridges, and in dunes. Holocene soils suggest the character of initial development in soils that are much older and more complex, and record the beginnings of various soil horizons. Noncalcareous brown or reddish brown B horizons have formed in low-carbonate parent materials of stable sites. Incipient development of the argillic horizon and the Haplargids occurs at stable sites in very gravelly materials that are about 1–2000 yr old. The cambic horizon and Camborthids occur in adjacent low-gravel materials of the same age. The argillic horizon occurs continuously in soils of earliest Holocene, particularly in very gravelly materials. Where soils have been truncated, as in areas affected by landscape dissection, argillic and cambic horizons are usually absent and the soils are Torripsamments, Torriorthents, or Torrifluvents depending on content of sand, gravel, and organic carbon. In high-carbonate parent materials, noncalcareous, reddish brown B horizons have not formed at any time in the Holocene. Most of these soils are Torriorthents or Torrifluvents although an incipient calcic horizon has formed in some of the oldest Holocene soils; the latter are Calciorthids. Horizons of carbonate accumulation are the best and most common pedogenic indicators of soil age. Stage I carbonate horizons are a major feature of pedogenesis in the Holocene. Because of additions of carbonate from the atmosphere, carbonate horizons are morphologically similar whether they have formed in high or low-carbonate alluvium. The carbonate accumulations are illuvial.

Some Holocene deposits apparently resulted from changes in climate. Others, such as the youthful deposits of coppice dunes, apparently were caused by man's introduction of cattle and subsequent overgrazing and seed dispersal.

Type
Research Article
Information
Quaternary Research , Volume 5 , Issue 3 , September 1975 , pp. 321 - 360
Copyright
University of Washington

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Footnotes

1

Presented July 31, 1974 at the third biennial meeting of the American Quaternary Association, Madison, Wisconsin.

References

Antevs, Ernst, (1955). Geologic-climatic dating in the West. American Antiquity 20, 317–335.CrossRefGoogle Scholar
Bryan, Kirk, (1925). Date of channel trenching (arroyo cutting) in the arid Southwest. Science 62, 338–344.Google Scholar
Buffington, Lee C., Herbel, C.H., (1965). Vegetational changes on a semidesert grassland range. Ecological Monographs 35, 139–164.CrossRefGoogle Scholar
Dunham, K.C., (1935). The Geology of the Organ Mountains with an Account of the Geology and Mineral Resources of Dona Ana County, New Mexico. New Mexico Bureau of Mines and Mineral Resources Bulletin 11, (Socorro).Google Scholar
Fairbridge, Rhodes W., (1968). Holocene, postglacial or recent epoch. The Encyclopedia of Geomorphology Reinhold Book Corporation New York.Google Scholar
Freeman, C.E., (1972). Pollen study of some Holocene alluvial deposits in Dona Ana County, Southern New Mexico. Texas Journal of Science 24, No. 2 203–219.Google Scholar
Gile, Leland H., (1966a). Coppice dunes and the Rotura soil. Soil Science Society of America Proceedings 30, 657–660.Google Scholar
Gile, Leland H., (1966b). Cambic and certain noncambic horizons in desert soils of Southern New Mexico. Soil Science Society of America Proceedings 30, 773–781.Google Scholar
Gile, L.H., Grossman, R.B., (1968). Morphology of the argillic horizon in desert soils of Southern New Mexico. Soil Science 106, 6–15.Google Scholar
Gile, L.H., Hawley, J.W., (1968). Age and comparative development of desert soils at the Gardner Spring Radiocarbon Site, New Mexico. Soil Science Society of America Proceedings 32, 709–716.CrossRefGoogle Scholar
Gile, L.H., Grossman, R.B., Hawley, J.W., (1969). Effects of landscape dissection on soils near University Park, New Mexico. Soil Science 108, 273–282.Google Scholar
Gile, L.H., Hawley, J.W., Grossman, R.B., (1970). Distribution and Genesis of Soils and Geomorphic Surfaces in a Desert Region of Southern New Mexico. Soil Science Society of America University Park, New MexicoGuidebook, Soil-Geomorphology Field Conference.Google Scholar
Gile, L.H., Peterson, F.F., Grossman, R.B., (1965). The K horizon: A master soil horizon of carbonate accumulation. Soil Science 99, 74–82.Google Scholar
Gile, L.H., Peterson, F.F., Grossman, R.B., (1966). Morphological and genetic sequences of carbonate accumulation in desert soils. Soil Science 101, 347–360.CrossRefGoogle Scholar
Hawley, J.W., (1965). Geomorphic surfaces along the Rio Grande Valley from El Paso, Texas to Caballo Reservoir, New Mexico. New Mexico Geological Society Guidebook of Southern New Mexico II, 188–198(Socorro).Google Scholar
Hawley, J.W., Kottlowski, F.E., (1969). Quaternary geology of the south-central New Mexico border region. Kottlowski, F.E., LeMone, D.V., Border Stratigraphy Symposium New Mexico Institute of Mining and Technology, State Bureau of Mines and Mineral Resources Circular 104 89–115Socorro.Google Scholar
Haynes, C.V. Jr., (1968). Geochronology of late-Quaternary alluvium. Means of Correlation of Quaternary Successions University of Utah Press Salt Lake City 591–631.Google Scholar
Hopkins, D.M., (1975). Time-stratigraphic nomenclature for the Holocene epoch. Geology 3, 10.Google Scholar
Irwin-Williams, C., Haynes, C.V., (1970). Climatic change and early population dynamics in the Southwestern United States. Quaternary Research 1, 59–71.Google Scholar
Mehringer, P.J., (1967). Pollen analysis and the alluvial chronology. The Kiva. Journal of the Arizona Archaeological and Historical Society 32, 96–101.Google Scholar
Melton, F.A., (1940). A tentative classification of sand dunes: Its application to dune history in the southern High Plains. Journal of Geology 48, 113–174.Google Scholar
Mercer, J.H., (1972). The lower boundary of the Holocene. Quaternary Research 2, 15–24.Google Scholar
Ruhe, R.V., (1964). Landscape morphology and alluvial deposits in Southern New Mexico. Annals of the Association of American Geographers 54, 147–159.CrossRefGoogle Scholar
Ruhe, R.V., (1967). Geomorphic Surfaces and Surficial Deposits in Southern New Mexico. New Mexico Bureau of Mines and Mineral Resources Memoir 18, (Socorro).Google Scholar
Soil Conservation Service(1972). Soil Survey Laboratory methods and procedures for collecting soil samples. Soil Survey Investigations Report No. 1 (Washington, D. C.).Google Scholar
Soil Survey Staff(1951). Soil Survey Manual. United States Department of Agriculture Handbook 18, (Washington, D.C.).Google Scholar
Soil Survey Staff(1962). Supplement to United States Department of Agriculture Handbook. 18, 173–188replacing.Google Scholar
Soil Survey Staff(1972). Soil Series of the United States, Puerto Rico and the Virgin Islands: Their Taxonomic Classification. Soil Conservation Service, United States Department of Agriculture Washington, D.C.Google Scholar
Soil Survey Staff. “Soil Taxonomy, a Basic System of Soil Classification For Making and Interpreting Soil Surveys.” Soil Conservation Service, United States Department of Agriculture, Washington, D. C. (In press)..Google Scholar
Walker, T.R., (1967). Formation of red beds in modern and ancient deserts. Geological Society of America Bulletin 78, 353–368.Google Scholar
York, J.C., Dick-Peddie, W.A., (1969). Vegetation changes in Southern New Mexico during the past 100 years. Arid Lands in Perspective University of Arizona Press Tucson 155–166.Google Scholar