Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man

The increased mercury content in a Greenland ice sheet over the last several decades suggests the dissemination of this element about the earth's atmosphere through the activities of man. The mercury content in the atmosphere appears to result primarily from the degassing of the earth's cr...

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Published in:Science
Main Authors: Weiss, Herbert V., Koide, Minoru, Goldberg, Edward D.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1971
Subjects:
Online Access:http://dx.doi.org/10.1126/science.174.4010.692
https://www.science.org/doi/pdf/10.1126/science.174.4010.692
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spelling craaas:10.1126/science.174.4010.692 2024-09-30T14:35:40+00:00 Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man Weiss, Herbert V. Koide, Minoru Goldberg, Edward D. 1971 http://dx.doi.org/10.1126/science.174.4010.692 https://www.science.org/doi/pdf/10.1126/science.174.4010.692 en eng American Association for the Advancement of Science (AAAS) Science volume 174, issue 4010, page 692-694 ISSN 0036-8075 1095-9203 journal-article 1971 craaas https://doi.org/10.1126/science.174.4010.692 2024-09-05T04:01:23Z The increased mercury content in a Greenland ice sheet over the last several decades suggests the dissemination of this element about the earth's atmosphere through the activities of man. The mercury content in the atmosphere appears to result primarily from the degassing of the earth's crust. Increased flux may come about as a result of the enhancement of this degassing process through the actions of man. Article in Journal/Newspaper Greenland Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 174 4010 692 694
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description The increased mercury content in a Greenland ice sheet over the last several decades suggests the dissemination of this element about the earth's atmosphere through the activities of man. The mercury content in the atmosphere appears to result primarily from the degassing of the earth's crust. Increased flux may come about as a result of the enhancement of this degassing process through the actions of man.
format Article in Journal/Newspaper
author Weiss, Herbert V.
Koide, Minoru
Goldberg, Edward D.
spellingShingle Weiss, Herbert V.
Koide, Minoru
Goldberg, Edward D.
Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
author_facet Weiss, Herbert V.
Koide, Minoru
Goldberg, Edward D.
author_sort Weiss, Herbert V.
title Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
title_short Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
title_full Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
title_fullStr Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
title_full_unstemmed Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man
title_sort mercury in a greenland ice sheet: evidence of recent input by man
publisher American Association for the Advancement of Science (AAAS)
publishDate 1971
url http://dx.doi.org/10.1126/science.174.4010.692
https://www.science.org/doi/pdf/10.1126/science.174.4010.692
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source Science
volume 174, issue 4010, page 692-694
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.174.4010.692
container_title Science
container_volume 174
container_issue 4010
container_start_page 692
op_container_end_page 694
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