Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-25T09:02:35.561Z Has data issue: false hasContentIssue false

Quaternary Buried Paleosols: A Critical Review

Published online by Cambridge University Press:  20 January 2017

K.W.G. Valentine
Affiliation:
Agriculture Canada, Soil Research Institute, 6660 N. W. Marine Drive, Vancouver, British Columbia V6T 1X2, Canada, Department of Soil Science, University of Reading, Berkshire, England
J.B. Dalrymple
Affiliation:
Agriculture Canada, Soil Research Institute, 6660 N. W. Marine Drive, Vancouver, British Columbia V6T 1X2, Canada, Department of Soil Science, University of Reading, Berkshire, England

Abstract

A review of work on buried paleosols in the disciplines of pedology, Quaternary geology, and archaeology is presented under the headings of (1) the problems of identification, (2) techniques of study, (3) buried paleosols and Quaternary stratigraphy, (4) archaeological stratigraphy and dating, (5) layered soils, and (6) past environment from buried paleosols. It is suggested that future pedological research of interest to Quaternary studies should concentrate on clarifying what is a soil as opposed to a weathered sediment, what processes and features are peculiar to pedogenesis as opposed to diagenesis, and what are the relationships between soil-site conditions and soil characteristics.

Type
Review Article
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

American Commission on Stratigraphic Nomenclature (1961). Code of Stratigraphic Nomenclature. Bulletin of the American Association of Petroleum Geologists 45 645665.Google Scholar
Avery, B.W., Stephen, I., Brown, G., Yaalon, D.H., (1959). The origin and development of Brown Earths on Clay-with-Flints and Coombe deposits. Journal of Soil Science 10 2 177195.CrossRefGoogle Scholar
Barrière, J., (1971). Paléopédologie: utilisation des paléosols comme elements de datation des formations quaternaries. Comptes Rendus Hebdomadaires des Seances de l'Academie Sciences, Serie D, Paris 273 3 310313.Google Scholar
Beckmann, G.G., (1963). The genesis of certain Hawaiian Paleosols and their alteration after burial. Dissertation Abstracts 24 3490.Google Scholar
Berg, L., (1926). On the soil theory of the origin of Loess. Bulletin of the Geographical Institute, Leningrad No. 6.Google Scholar
Bowler, J.M., Polach, H.A., (1971). Radiocarbon analyses of soil carbonates: an evaluation from paleosols in southeastern Australia. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 97108.Google Scholar
Brewer, R., (1972). The use of macro- and micromorphological data in soil stratigraphy to elucidate surficial geology and soil genesis. Journal of the Geological Society of Australia 19 3 331344.CrossRefGoogle Scholar
Brewer, R., Crook, K.A.W., Speight, J.G., (1970). Proposal for soil-stratigraphic units in the Australian stratigraphic code. Journal of the Geological Society of Australia 17 103111.Google Scholar
Brophy, J.A., (1959). Heavy Mineral Ratios of Sangamon Weathering Profiles in Illinois. Illinois State Geological Survey Circular 273 .Google Scholar
Brunnacker, K., (1964). Böden des älteren Pleistozans bei Regensburg. Geologica Bavaria 53 148160.Google Scholar
Brunnacker, K., (1967). Fundamentals of Quaternary Soil stratigraphy in Southern Germany. Morrison, R.B., Wright, H.R. “Quaternary Soils” Proceedings of the 7th INQUA Congress Vol. 9 93102.Google Scholar
Bullock, P., Mackney, D., (1970). Micromorphology of strata in the Boyn Hill Terrace Deposits, Buckinghamshire. Osmond, D.A., Bullocks, P. Micromorphological Techniques and Applications Soil Survey Technical Monograph 2 97106Harpendon.Google Scholar
Butler, B.E., (1958). Depositional Systems of the Riverine Plain in Relation to Soils. CSIRO Soil Publication 10 .Google Scholar
Campbell, C.A., Paul, E.A., Rennie, D.A., McCallum, K.J., (1967). Applicability of the carbon dating method of analysis to soil humus studies. Soil Science 104 217224.Google Scholar
Chandler, R.F., (1942). The time required for podzol profile formation as evidenced by the Mendenhall glacial deposits near Juneau, Alaska. Soil Science Society of America Proceedings 7 454459.CrossRefGoogle Scholar
Churchward, H.M., (1961). Soil Studies at Swan Hill, Victoria, Australia 1. Soil layering. Journal of Soil Science 12 1 7386.Google Scholar
Cornwall, I.W., (1953). Soil Science and Archaeology with illustrations from some British Bronze Age monuments. Proceedings of the Prehistoric Society 19 129147.CrossRefGoogle Scholar
Dalrymple, J.B., (1958). The application of soil micromorphology to fossil soils and other deposits from archaeological sites. Journal of Soil Science 9 2 199209.CrossRefGoogle Scholar
Dalrymple, J.B., (1964). The application of soil micromorphology to the recognition and interpretation of fossil soils in volcanic ash deposits from the North Island, New Zealand. “Soil Micromorphology”, Proceedings of the II International Working Meeting on Soil Micromorphology Arnhem. 339349.Google Scholar
Dalrymple, J.B., (1967). A study of paleosols in volcanic ash-fall deposits from northern North Island, New Zealand, and the evaluation of soil micromorphology for establishing their stratigraphic correlation. Morrison, R.B., Wright, H.E. “Quaternary Soils”, Proceedings of the 7th INQUA Congress Vol. 9 104122.Google Scholar
Dimbleby, G.W., (1952). The historical status of moorland in northeast Yorkshire. New Phytologist 56 1228.Google Scholar
Domaar, J.F., (1967). Infrared spectra of humic acids from soils formed under grass or trees. Geoderma 1 3745.CrossRefGoogle Scholar
Dormaar, J.F., Lutwick, L.E., (1969). Infrared spectra of humic acids and opal phytoliths as indicators of paleosols. Canadian Journal of Soil Science 49 1 2937.Google Scholar
Evans, J.G., Valentine, K.W.G., (1974). Ecological changes induced by Prehistoric man at Pitstone, Buckinghamshire. Journal of Archaeological Science 1 343351.CrossRefGoogle Scholar
Federoff, N., (1969). Caractères micromorphologiques des pédogèneses quaternaries en France. Etudes sur le Quaternaire, VIIIe Congress INQUA, Paris Vol. 1 341349.Google Scholar
Ferguson, C.W., (1968). Bristlecone pine: Science and esthetics. Science 159 839846.CrossRefGoogle ScholarPubMed
Fink, J., (1954). Die fossilen Böden im österreichischen löss. Quatar 6 85108.Google Scholar
Frye, J.C., Leonard, A.B., (1949). Pleistocene stratigraphic sequence in northeastern Kansas. American Journal of Science 247 883899.Google Scholar
Frye, J.C., Shaffer, P.R., Willman, H.B., Ekblaw, G.E., (1960). Accretion Gley and the gumbotil dilemma. American Journal of Science 258 185190.Google Scholar
Gerasimov, I.P., (1971). Nature and originality of paleosols. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 1527.Google Scholar
Gerasimov, I.P., (1973). Chernozems, buried soils, and Loesses of the Russian Plain: their age and genesis. Soil Science 116 3 202210.Google Scholar
Gile, L.H., Hawley, J.W., (1966). Periodic sedimentation and soil formation on an alluvial-fan piedmont in southern New Mexico. Soil Science Society of America Proceedings 30 261268.Google Scholar
Glinka, K.D., (1927). The Great Soil Groups of the World and Their Development. C. F. Marbut, Trans. Ann Arbor, Mich..Google Scholar
Godwin, H., (1954). Recurrence-surfaces. Danmarks Geologiske Undersogeise II Raekke 80 2230.Google Scholar
Goh, K.M., (1972). Amino acid levels as indicators of paleosols in New Zealand soil profiles. Geoderma 7 3347.CrossRefGoogle Scholar
Hardcastle, J., (1889). Origin of the loess Deposit of the Timaru Plateau. Transactions of the New Zealand Institute 22 406414.Google Scholar
Havinga, A.J., (1963). A Palynological investigation of soil profiles developed in cover sand. Mededelingen van de Landbouwhogeschool te Wageningen, Nederland 63 1 193.Google Scholar
Hunt, C.B., Sokoloff, V.P., (1950). Pre-Wisconsin Soil in the Rocky Mountain Regin, A Progress Report. United States Geological Survey Professional Paper 221-G 109123.Google Scholar
Kay, G.F., (1916a). Some features of the Kansan Drift in southern Iowa. Geological Society of America Bulletin 27 115117.Google Scholar
Kay, G.F., (1916b). Gumbotil, a new term in Pleistocene geology. Science 44 637638.Google Scholar
Kay, G.F., Apfel, E.T., (1929). The pre-Illinoian Pleistocene geology of Iowa. Iowa Geological Survey 34 1304.Google Scholar
Kerney, M.P., (1963). Late-glacial deposits on the Chalk of southeast England. Philosphical Transactions of the Royal Society of London, Series B 246 203254.Google Scholar
Kobayashi, K., (1965). Late Quaternary chronology of Japan. Earth Science, Japan 79 117.Google Scholar
Kobayashi, K., Shimizu, M., (1962). Pleistocene Tephras in the Northern Part of the Ina Valley, Central Japan. Journal of the Faculty of Liberal Arts and Science, Shinsu University 12 2 2045.Google Scholar
Leighton, M.M., (1923). The differentiation of the Drift Sheets of northwestern Illinois. Journal of Geology 21 4 265281.CrossRefGoogle Scholar
Leighton, M.M., MacClintock, P., (1930). Weathered zones of drift sheets of Illinois. Journal of Geology 38 1 2853.CrossRefGoogle Scholar
Leighton, M.M., MacClintock, P., (1962). The weathered mantle of glacial tills beneath original surfaces in north-central United States. Journal of Geology 70 267293.Google Scholar
Leverett, F., (1898). The weathered zone (Yarmouth) between the Illinoian and Kansas till sheets. Journal of Geology 6 238243.Google Scholar
Markov, K.K., Lazukov, G.I., Nikolayv, V.A., (1965) The Quaternary Period Vol. II Moscow University (in Russian).Google Scholar
Matsui, T., (1967). An application of soil stratigraphy to the Quaternary Geology and landscape development of Kyushu, Japan. Morrison, R.B., Wright, H.E. “Quaternary Soils”, Proceedings of the 7th INQUA Congress Vol. 9 205219.Google Scholar
Matsui, T., Saito, K., Yano, Y., (1970). A Comparative Clay Mineralogy of Relict and Fossil Red Soils with Overlying Pyroclastics around Chikugo Plain. Miscellaneous Report 73 Research Institute for Natural Resources Tokyo 3759.Google Scholar
Meade, R.H., (1960). Compaction and development of preferred orientation in clayey sediments. Dissertation Abstracts 21 VI 3421.Google Scholar
Mermut, A., Pape, Th., (1971). Micromorphology of two soils from Turkey, with special reference to in situ formation of clay cutans. Geoderma 5 271281.Google Scholar
Morozova, T.D., (1932). Fossils soils of the Valdry interstadia. Academiia Nauk SSSR Doklady, Earth Science Sections 143 16.Google Scholar
Morozova, T.D., (1963). Ancient soil profiles and their geographical extension in different epochs of soil formation in the upper pleistocene (a study of soils buried in loesses of the Central Part of the Russian Plain). Soil Proceedings of the Russian Academy of Science 12 2637.Google Scholar
Morrison, R.B., (1967). Principles of Quaternary soil stratigraphy. Morrison, R.B., Wright, H.E. “Quaternary Soils”, Proceedings of the 7th INQUA Congress 9 169.Google Scholar
Morrison, R.B., Frye, J.C., (1965). Correlations of the Middle and Late Quaternary Successions of the Lake Lahontan, Lake Bonneville, Rocky Mountain (Wasatch Range), Southern Great Plain and Eastern Midwest Areas. Nevada Bureau of Mines Report 9 .Google Scholar
Moskvitin, A.I., (1961). Comparative Stratigraphic Review of Pleistocene Sections Containing Traces of Paleolithic Man. Report of the 6th INQUA Congress, Warsaw Vol. 4 339361.Google Scholar
Mulcahy, M.J., (1961). Soil distribution in relation to landscape development. Zietschrift für Geomorphologie 3 5 211225.Google Scholar
Nikiforoff, C.C., (1943). Introduction to palaeopedology. American Journal of Science 241 194200.Google Scholar
Paepe, R., (1968). Les sols fossiles Pléistocènes de la Belgique. Pedologie 18 No. 2 176188.Google Scholar
Pěcsi, M., (1967). Horizontal and vertical distribution of the loess in Hungary. Studia Geomorphologica Carpatho-Balcanica 1319.Google Scholar
Polynov, B.B., (1927). Contribution of Russian Scientists to paleopedology. Russian Pedological Investigations, Academy of Sciences USSR 8 133.Google Scholar
Price, T.W., Blevins, R.L., Barnhisel, R.I., Bailey, H.H., (1975). Lithologic discontinuities in loessial soils of southwestern Kentucky. Soil Science Society of America Proceedings 39 9498.Google Scholar
Prosek, F., Lozek, V., (1957). Stratigraphische Ubersicht des tschechoslowakischen Quarters. Eiszeitalter und Gegenwart 8 3790.Google Scholar
Raeside, J.D., (1964). Loess deposits of the South Island, New Zealand, and the soils formed on them. New Zealand Journal of Geology and Geophysics 7 811838.CrossRefGoogle Scholar
Richmond, G.M., (1962). Quaternary stratigraphy of the La Sal Mountains, Utah. United States Geological Survey Professional Paper 324.Google Scholar
Richmond, G.M., (1970). Comparison of the Quaternary stratigraphy of the Alps and Rocky Mountains. Quaternary Research 1 328.Google Scholar
Ruellan, A., (1971). The history of soils: some problems of definition and interpretation. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 312.Google Scholar
Ruhe, R.V., (1956). Geomorphic Surfaces and the nature of soils. Soil Science 82 441455.Google Scholar
Ruhe, R.V., (1965). Quaternary paleopedology. Wright, H.E., Frey, D.G. The Quaternary of the United States Princeton University Press N.J 755764.Google Scholar
Ruhe, R.V., (1969). Quaternary Landscapes in Iowa. Iowa State University Press Ames .Google Scholar
Ruhe, R.V., Miller, G.A., Vreeken, W.J., (1971). Paleosols, Loess sedimentation and soil stratigraphy. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 4159.Google Scholar
Ruhe, R.V., Scholtes, W.H., (1956). Ages and development of soil landscapes in relation to climatic and vegetational change in Iowa. Soil Science Society of America Proceedings 20 264273.CrossRefGoogle Scholar
Runge, E.C.A., Goh, K.M., Rafter, T.A., (1973). Radiocarbon chronology and problems in its interpretation for Quaternary Loess deposits—South Canterbury, New Zealand. Soil Science Society of America Proceedings 37 742746.Google Scholar
Runge, E.C.A., Walker, T.W., Howarth, D.T., (1974). A study of Late Pleistocene Loess deposits, South Canterbury, New Zealand. 1. Forms and amounts of phosphorous compared with other techniques for identifying paleosols. Quaternary Research 4 7684.CrossRefGoogle Scholar
Scharpenseel, H.W., (1971). Radiocarbon dating of soils—problems, troubles, hopes. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 7787.Google Scholar
Scholtes, W.H., Ruhe, R.V., Rieken, F.F., (1951). Use of morphology of buried soil profiles in the Pleistocene of Iowa. Proceedings of the Iowa Academy of Science 58 295306.Google Scholar
Schultz, C.B., Stout, T.M., (1945). Pleistocene Loess Deposits of Nebraska. American Journal of Science 243 5 231244.Google Scholar
Simmons, I.G., (1970). Environment and early man on Dartmoor, Devon, England. Proceedings of the Prehistoric Society 35 203219.Google Scholar
Simonson, R.W., (1941). Studies of buried soils formed from till in Iowa. Soil Science Society of America Proceedings 6 373381.Google Scholar
Simonson, R.W., (1954). Identification and interpretation of buried soils. American Journal of Science 252 705732.Google Scholar
Siuta, J., Motowicka-Terelak, T., (1969). The origin and systematics of ferruginous precipitates in Quaternary formations and present day soils. Biuletyn Peryglacjainy 18 209257.Google Scholar
Sorenson, C.J., (1973). Interrelationships between Soils and Climate and between Paleosols and Paleoclimates: Forest/Tundra Ecostone, North Central Canada. Univ. of Wisconsin Unpublished Ph.D. Thesis.Google Scholar
Stevenson, F.J., (1969). Pedohumus: accumulation and diagenesis during the Quaternary. Soil Science 107 6 470479.Google Scholar
Suggate, R.P., (1974). When did the Last Interglacial end?. Quaternary Research 4 246252.Google Scholar
Syers, J.K., Jackson, M.L., Berkheiser, V.E., Clayton, R.N., Rex, R.W., (1969). Eolian sediment influence on pedogenesis during the Quaternary. Soil Science 107 421427.Google Scholar
Thorp, J., (1935). Soil profile studies as an aid to understanding recent geology. Bulletin of the Geological Society of China 14 350392.Google Scholar
Thorp, J., Johnson, W.M., Reed, E.C., (1951). Some post-Pliocene buried soils of Central United States. Journal of Soil Science 2 119.Google Scholar
Twenhofel, W.H., (1926). Treatise on Sedimentation. Williams and Wilkins Baltimore .Google Scholar
Valentine, K.W.G., Dalrymple, J.B., (1975). The identification, lateral variation and chronology of two buried paleocatenas at Woodhall Spa and West Runton, England. Quaternary Research 7 551590.Google Scholar
Vogel, J.C., Zagwijn, W.H., (1967). Groningen Radiocarbon dates. VI. Radiocarbon 9 63106.CrossRefGoogle Scholar
Vucetich, C.G., Pullar, W.A., (1963). Ash beds and soils in Rotorua District. Proceedings of the New Zealand Ecological Society 10 6572.Google Scholar
Walker, P.H., (1962). Soil layers on hillslopes: a study at Nowra, N.S.W., Australia. Journal of Soil Science 13 2 167177.CrossRefGoogle Scholar
Williams, G.E., Polach, H.A., (1971). Radiocarbon dating of arid-zone calcareous paleosols. Geological Society of America Bulletin 82 30693085.Google Scholar
Working Group on the Origin and Nature of Paleosols (1971). Criteria for the Recognition and Classification of Paleosols. Yaalon, D.H. Paleopedology International Society of Soil Science and Israel Universities Press 153158.Google Scholar
Yaalon, D.H., (1971). Soil forming processes in time and space. Yaalon, D.H. Paleopedology International Society of Social Science and Israel Universities Press 2938.Google Scholar
Yehle, L.A., (1954). Soil tongues and their confusion with certain indicators of periglacial climate. American Journal of Soil Science 252 532546.Google Scholar
Zeuner, F.E., (1945). The Pleistocene Period. The Ray Society London .Google Scholar