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Characterization of the Soil Hydromorphic Conditions in a Paludified Dunefield during the Mid-Holocene Hemlock Decline near Québec City, Québec

Published online by Cambridge University Press:  20 January 2017

Najat Bhiry  and
Louise Filion
Najat Bhiry
Affiliation:
Centre d'études nordiques and Département de géographie, Université Laval, Sainte-Foy, (Québec), Canada, G1K 7P4
Louise Filion
Affiliation:
Centre d'études nordiques and Département de géographie, Université Laval, Sainte-Foy, (Québec), Canada, G1K 7P4
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Abstract

The mid-Holocene eastern hemlock [Tsuga canadensis L. (Carr.)] decline has been recently attributed to the activity of insect defoliators. N. Bihiry and L. Filion, Quaternary Research 45,312–320 (1996). In this study, soil hydromorphic conditions were investigated for the period 6800–3200 yr B.P. using micromorphological data from a peat section from a swale in a paludified dunefield in southern Québec. After a short period of plant colonization in shallow pools between 6800 and 6400 yr B.P., mesic conditions predominated in the interdune before the decline (6400–4900 yr B.P.), as evidenced by strong bioturbation and abundance of excrements from the soil fauna. During the decline, a shift from mesic to wet conditions occurred (4900–4100 yr B.P.), although xeric to mesic conditions persisted on dune ridges until at least 4200 yr B.P. Wetness culminated when beaver occupied the site (4100–3750 yr B.P.). Hemlock needles with chewing damage typical of hemlock looper (Lambdina fiscellaria) feeding were identified at levels dated 4900, 4600, and 4200 yr B.P., respectively, implying that the hemlock decline was associated with at least three defoliation events. The ca. 400-yr interval between these events likely represents the time required for this late-sucessional tree species to recover.

Type
Research Article
Information
Quaternary Research , Volume 46 , Issue 3 , November 1996 , pp. 281 - 297
Copyright
University of Washington

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References

Allison, F.F., and Klein, C. J., (1961). Comparative rates of decomposition in soil of wood and bark particles of several softwood species. Proceedings of the Soil Science Society of America 25, 193–196.CrossRefGoogle Scholar
Altemu¨ller, H. J., (1962). Gedanken zum Aufbau des bodens und seiner begrifflichen. Erfassung, Z. Kulturtechnik 3, 323–336.Google Scholar
Babel, U., (1968). Enchytraeen-Losungsgefüge in Lo¨ss. Geoderma 2, 57– 63.CrossRefGoogle Scholar
Babel, U., (1975). Micromorphological of soil organic matter. In “Soil components” (Gieseking, H. E., Ed.), Vol. 1, pp. 369–473. Springer-Verlag, New York.Google Scholar
Bal, L., (1973). “Micromorphological Analysis of Soil. Lower Levels in the Organisation of Organic Soil materials.” Soil Survey Papers, 6, Soil Survey Institute, Wageningen.Google Scholar
Bal, L., (1982). “Zoological Ripening of Soils.” Agricultural Research Report 850, Wageningen.Google Scholar
Barber, K. E., (1981) “Peat Stratigraphy and Climatic Change. A Paleoeco-logical Test of the Theory of Cyclic Peat Bog Regeneration.” Balkema, Rotterdam.Google Scholar
Beckmann, W., and Geyger, E., (1967). Entwurf einer Ordnung der natür-lichen Hohlraun-Aggregat und Strunkturformen in Boden. In “Die Mi-cromorphometrische Bodenanalyse” (Kubiena, W. L., Ed.), pp. 163–188. Enke Verlag, Stuttgart.Google Scholar
Bhiry, N., and Filion, L., (1996a). Mid-Holocene Hemlock Decline in Eastern North America Linked with Phytophagous Insect Activity. Quaternary Research, 45, 312–320.CrossRefGoogle Scholar
Bhiry, N., and Filion, L., (1996b). Holocene plant succession in a dune-swale environment of southern Que´bec: A macrofossil analysis. Ecoscience, 3, 330–342.Google Scholar
Birks, H. J.B., and Birks, H. H., (1980). “Quaternary Palaeoecology.” Arnold, London.Google Scholar
Bold, H.C., and Wynne, M. J., (1978). “Introduction to the Algae: Structure and Reproduction.” Prentice-Hall, New Jersey.Google Scholar
Bouma, J., Fox, C.A., and Miedema, R., (1988). Micromorphology of hy-dromorphic soils: Applications for soil genesis ans land evaluation. In “Proceeding of the VIIIth International working meeting of soil micro-morphology,” pp. 257–278. San Antonio, Texas.Google Scholar
Bullock, P., Fedoroff, N., Jongerius, A., Stoops, G., and Tursina, T., (1985). “Handbook for Soil Thin Section Description.” Waine Research, Wol-verhampton.Google Scholar
Castel, I. I. Y., (1991). Micromorphology of the transition peat-Holocene drift sand deposits in the northern Netherlands. Zeitschrift für Geomor-phologie. N. F. 90, 29–43.Google Scholar
Edwards, C.A., and Health, G. W., (1963). The role of soil animals in breakdown of leaf material. In “Proceedings of the Colloquium of Soil Fauna, Soil Microflora and Their Relationships: Soil Organisms.” Oost-erbeek, Amsterdam.Google Scholar
Filion, L., (1987). Holocene Development of Parabolic Dunes in the Central St. Lawrence Lowland. Quaternary Research 28, 196–209.Google Scholar
Filion, L., and Quinty, F., (1993). Macrofossil and Tree-Ring Evidence for a Long-Term Forest Succession and Mid-Holocene Hemlock Decline. Quaternary Research 40, 89–97.CrossRefGoogle Scholar
Fox, C.A., and Tarnocai, C., (1988). The micromorphology of sedimentary peat deposit from the Pacific Temperate Wetland Region of Canada. In “Proceeding of the VIIIth International Working Meeting of Soil Micromorphology,” pp. 311–319. San Antonio, Texas.Google Scholar
Guo, Z.T., and Fedoroff, N., (1991). Paleoclimatic and stratigraphic implications of the S1 paleosol in the loess sequence in China. In “Loess, Environment and Global Change” (Liu, T. S., Ed.), pp. 187–198. Science Press, Beijing.Google Scholar
Handley, W. R. C., (1954). Mull and mor formation in relation of forest soils. Forestry Commission, Bulletin No. 23. Google Scholar
Hann, B. J., (1990). Cladocera. In “Methods in Quaternary Ecology” (Warner, B. G., Ed.), pp. 81–91. Geoscience Canada, St. John's.Google Scholar
Kemp, R.A., Derbyshire, E., Xingmin, M., Fahu, C., and Baotian, P., (1995). Pedosedimentary reconstruction of a thick loess-paleosol sequence near Lanzhou in north-central China. Quaternary Research 43, 30–45.CrossRefGoogle Scholar
Kubiena, W. L., (1938). “Micropedology.” Collegiate Press, Ames, Iowa.Google Scholar
Lee, G. B., (1983). The micromorphology of peat. In “Soil micromorphol-ogy” (Bullock, P., and Murphy, C. P., Eds.), pp. 485–501. Berkhamsted.Google Scholar
Le´vesque, M.P., and Dinel, H., (1982). Some morphological and chemical aspects of peats applied to the characterization of Histosols. Soil Science 5, 324–332.CrossRefGoogle Scholar
Miedema, R., Pape, Th., and Van De Waal, G. L., (1974). A method to impregnate wet soil samples producing high quality thin sections. Netherlands Journal of Agricultural Science 22, 37–40.Google Scholar
Puffe, D., and Grosse-Brauckman, G., (1963). Micromorphologische Unter-suchungen an Torfen. Z. Kulturtech. Flurbereinigung 4, 159–188.Google Scholar
Shoute, J. F.Th., (1984). “Vegetation Horizons and Related Phenomena. A Palaeoecological-Micromorphological Study in the Younger Holocene of the Northern Netherlands (Schildmeer area).” Dissertationes Botani-cae, Vol. 81, J. Cramer, Vaduz.Google Scholar
Smol, J.P., Cumming, B.F., Douglas, M. S.V., and Pienitz, R., (1996). Inferring past climatic change in Canada using paleolimnological techniques. Geoscience Canada 21, 113–118.Google Scholar
Van Vliet-Lanoë¨, B., (1990). Le pédocomplexe de Warmeton: où en est-on? Bilan paléopédocomplexe et micromorphologique. Quaternaire 1, 65–76.Google Scholar
Vepraskas, M. J., (1992). “Redoximorphic Features for Identifying Aquatic Conditions North.” Carolina Agricultural Research Service, Technical Bulletin No. 301, North Carolina State University, Raleigh.Google Scholar
Warner, B. G., (1990). “Methods in Quarternary Ecology.” Geological Association of Canada, St. John's, Newfoundland.Google Scholar
Wellington, W. G., (1952). Air mass climatology of Ontario north of Lake Huron and Lake Superior before outbreaks of the spruce budworm, Chori-stoneura fumiferana (Clemn.) and the forest tent caterpillar, Malacosoma disstria Hbn, (Lepidoptera, Tortricidae; Lasiocampidae). Canadian Journal of Zoology 30, 114–127.Google Scholar
Zachariae, G., (1965). Spuren tierischer Tätigkeit im Boden des Buchen-waldes. Forstwiss. Forschungen (Beihefte zum forstlichen Zentralblatt), H. 20.Google Scholar
Zachariae, G., (1967). Der Einsatz mikomorphologisher Methoden bei bode-nzoologischen Arbeiten. Geoderma 1, 175–196.CrossRefGoogle Scholar