Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-26T00:08:23.679Z Has data issue: false hasContentIssue false
  • English
  • Français

Reconstructing the Rate of Accumulation of Lake Sediment: The Effect of Sediment Focusing1

Published online by Cambridge University Press:  20 January 2017

John T. Lehman
John T. Lehman*
Affiliation:
Department of Zoology, University of Washington, Seattle, Washington 98195 USA
Get access Rights & Permissions [Opens in a new window]

Abstract

Use of accumulation rates of pollen or minerals to infer regional history is complicated by nonuniform deposition of lake sediment. Sediment focusing, direction of sediment to the deepest part of a basin, can introduce a discrepancy between changes in accumulation rates measured directly from sediment cores and actual changes in influx of sediment or pollen to a lake. This difference depends on values and temporal variation of the ratio of mean depth to maximum depth in a basin as it fills. Several models of sediment accumulation show how measurements from a single core can be transformed to yield basinwide influx rates, and how the distortion due to sediment focusing can be assessed. Basins shaped like hyperboloids or frustums may introduce much greater distortions than basins conforming to ellipsoid or sinusoid shapes.

Type
Research Article
Information
Quaternary Research , Volume 5 , Issue 4 , December 1975 , pp. 541 - 550
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.)

Footnotes

1

A contribution to the Hubbard Brook Ecosystem Study.

References

Anderson, D.V., (1961). A note on the morphology of the basins of the Great Lakes. Journal of the Fisheries Research Board of Canada 18, 273–277.CrossRefGoogle Scholar
Broecker, W.S., Walton, A., (1959). The geochemistry of C14 in fresh water systems. Geochemica et Cosmochimica Acta 16, 15–38.Google Scholar
Davis, M.B., (1968). Pollen grains in lake sediments: Redeposition caused by seasonal water circulation. Science 162, 796–799.Google Scholar
Davis, M.B., (1969). Climatic changes in southern Connecticut recorded by pollen deposition at Rogers Lake. Ecology 50, 409–422.Google Scholar
Davis, M.B., (1973). Redeposition of pollen grains in lake sediment. Limnology and Oceanography 18, 44–52.CrossRefGoogle Scholar
Davis, M.B., Deevey, E.S. Jr., (1964). Pollen accumulation rates: Estimates from late-glacial sediment of Rogers Lake. Science 145, 1293–1295.Google Scholar
Deevey, E.S. Jr., (1955). The obliteration of the hypolimnion. Memorie dell'Istituto Italiano di Idrobiologia (Supplement) 8, 9–38.Google Scholar
Deevey, E.S. Jr., Gross, M.S., Hutchinson, G.E., Kraybill, H.L., (1954). The natural C14 contents of materials from hard-water lakes. Proceedings of the National Academy of Science US 40, 285–288.Google Scholar
Gould, H.R., Budinger, T.F., (1958). Control of sedimentation and bottom configuration by convection currents, Lake Washington, Washington. Journal of Marine Research 17, 183–198.Google Scholar
Hutchinson, G.E., (1957). A Treatise on Limnology. Vol. I, Wiley New York.Google Scholar
Junge, C.O., (1966). Depth distributions for quadric surfaces and other configurations. Hrbacek, J., Hydrobiological Studies 1 Czechoslovak Academy of Sciences Prague 257–265.Google Scholar
Kerfoot, W.C., (1974). Net accumulation rates and the history of cladoceran communities. Ecology 55, 51–61.Google Scholar
Likens, G.E., Davis, M.B., (1975). Post-glacial history of Mirror Lake and its watershed in New Hampshire, U.S.A. Proceedings of the 19th Congress of the International Association for Theoretical and Applied Limnology Winnipeg(in press).Google Scholar
Mackereth, F.J.H., (1966). Some chemical observations of post-glacial lake sediments. Philosophical Transactions of the Royal Society of London Series B 250, 165–213.Google Scholar
Neumann, J., (1959). Maximum depth and average depth of lakes. Journal of the Fisheries Research Board of Canada 16, 923–927.Google Scholar
Pewé, T.L., Hopkins, D.M., Giddings, J.L., (1965). The Quaternary geology and archeology of Alaska. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States Princeton, University Press Princeton, N.J 355–374.Google Scholar
Rigg, G.B., (1958). Peat resources of Washington. Washington Department of Conservation, Division of Mines and Geology Bulletin 44, 1–272.Google Scholar
Stuiver, M., (1971). Evidence for the variation of atmospheric C14 content in the late Quaternary. Turekian, K.K., The Late Cenozoic Glacial Ages Yale University Press New Haven, Conn 57–70.Google Scholar
Wilson, I.T., Opdyke, D.F., (1941). The distribution of the chemical constituents in the accumulated sediment of Tippecanoe Lake. Investigations of Indiana Lakes and Streams 2, 16–42.Google Scholar