Soluble and insoluble impurities along the 950 m deep Vostok ice core (Antarctica) — Climatic implications

Author:

De Angelis M.,Legrand M.,Petit J. R.,Barkov N. I.,Korotkevitch Ye. S.,Kotlyakov V. M.

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science,Environmental Chemistry

Reference35 articles.

1. Barkov, N. I., Korotkevich, E. S., Gordienko, F. G., and Kotlyakov, V. M., 1977, The isotope analysis of ice cores from Vostok station (Antarctica), to the depth of 950 m, UGGI International Symposium on Isotopes and Impurities in Snow and Ice, Grenoble, August 1975, AIHS Pub. 118, pp. 382?387.

2. Boutron C., 1980, Respective influence of global pollution and volcanic eruptions on the past variations of the trace metals content of Antarctic snow since 1880's, J. Geophys. Res. 85, 7426?7432.

3. Briat M., Royer A., Petit J. R., and Lorius C., 1982, Late glacial input of eolian continental dust in the Dome C ice core: additional evidence from individual microparticle analysis. Ann. Glaciol. 3, 27?31.

4. Climap Project Members, 1976, Science, 191, 1131?1137.

5. Cragin, J. M., Herron, M. M., Langway, C. C., and Klouda, G., 1977, Interhemispheric comparison of changes in the composition of atmospheric precipitation during the late cenozoic era, in J. Dunbar Maxwell (ed.), Polar Oceans (Proceedings of the Polar Oceans Conference, Montreal, 1974), pp. 617?631, Arctic Institute of North America.

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