Lead concentration changes in Antarctic ice during the Wisconsin/Holocene transition

Details Lead concentration changes in Antarctic ice during the Wisconsin/Holocene transition Lead concentration changes in Antarctic ice during the Wisconsin/Holocene transition

Sep 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986natur.323..222b&link_type=abstract

Nature (ISSN 0028-0836), vol. 323, Sept. 18, 1986, p. 222-225. Research supported by the Ministere de l'Environnement, Expeditio

Computer Science

27

Antarctic Regions, Concentration (Composition), Geochemistry, Ice Environments, Lead (Metal), Primitive Earth Atmosphere, Chemical Analysis, Core Sampling, Environment Models, Pollution, Trace Elements

Scientific paper

In order to assess current global lead atmospheric pollution, it is
necessary to reconstruct the natural, pre-human atmospheric fluxes of
this toxic heavy metal. The time variations of these fluxes over the
past 27,000 years have been obtained from the analysis of an Antarctic
ice core.

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