Inferences concerning climatic change from a deeply frozen lake on Rundfjeld, Ellesmere Island, Arctic Canada

Author:

Blake Weston

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Aquatic Science

Reference50 articles.

1. Allan, C., C. Schiff, D. Pierson, M. English, M. Ecclestone & P. Adams, 1987. Colour Lake, Axel Heiberg Island, N.W.T., a naturally acid, high arctic lake — a data report. In P. Adams (ed.), Field Research on Axel Heiberg Island, N.W.T., Canada; Bibliographies and data reports. McGill, Axel Heiberg Is. Res. Rept., Misc. Paper No. 2: 67–189.

2. Andrée, M, H. Oeschger, U. Siegenthaler, T. Riesen, M. Moell, B. Ammann & K. Tobolski, 1986. 14C dating of plant macrofossils in lake sediment. Radiocarbon 28: 411–416.

3. Barnes, D. F., 1960. An investigation of a perenially frozen lake. Air force surveys in geophysics, Geophysics Res. Directorate, AF Cambridge Res. Laboratories, Air Force Res. Div. (ARDC), United States Air Force, Bedford, Mass. (AFCRL-TN-60–660): 134 pp.

4. Blake, W., Jr., 1972. Climatic implications of radiocarbondated driftwood in the Queen Elizabeth Islands, Arctic Canada. In Y. Vasari, H. Hyvärinen & S. Hicks (eds.), Climatic changes in Arctic areas during the last tenthousand years, Proc. of a sympsoium held in Oulanka-Kevo, Finland, 1971. Acta Universitatis Ouluensis, Ser. A, Sci. Rer. Nat. No. 3, Geol. No. 1: 77–104.

5. Blake, W. Jr., 1975. Radiocarbon age determinations and postglacial emergence at Cape Storm, southern Ellesmere Island, Arctic Canada. Geogr. Ann. 57A: 1–71.

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