10Be and 14C in the earth system ...
In a very short period of time, 10Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10Be ice-...
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Online Access: | https://dx.doi.org/10.48350/158601 https://boris-portal.unibe.ch/handle/20.500.12422/43246 |
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ftdatacite:10.48350/158601 2024-10-20T14:09:24+00:00 10Be and 14C in the earth system ... Oeschger, H. Beer, J. Andrée, M. 1987 https://dx.doi.org/10.48350/158601 https://boris-portal.unibe.ch/handle/20.500.12422/43246 en eng University of Bern Text JournalArticle ScholarlyArticle article-journal 1987 ftdatacite https://doi.org/10.48350/158601 2024-10-01T11:43:06Z In a very short period of time, 10Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10Be ice-core (from the past 10 ka) and ocean-sediment profiles (geomagnetic reversals); (c) climatic effects reflected in 10Be profiles in loess and polar ice cores (10Be behaviour in atmosphere); (d) comparison of 10Be and 14C variations (tree rings) from carbon-cycle models and inform ation on ocean circulation history from 14C m easurements on benthic and planktonic Foram inifera in ocean sediments. An overview on work in collaboration with the Zurich AMS facility (with Professor W. Wolfli) is given. ... Article in Journal/Newspaper ice core DataCite |
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English |
description |
In a very short period of time, 10Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10Be ice-core (from the past 10 ka) and ocean-sediment profiles (geomagnetic reversals); (c) climatic effects reflected in 10Be profiles in loess and polar ice cores (10Be behaviour in atmosphere); (d) comparison of 10Be and 14C variations (tree rings) from carbon-cycle models and inform ation on ocean circulation history from 14C m easurements on benthic and planktonic Foram inifera in ocean sediments. An overview on work in collaboration with the Zurich AMS facility (with Professor W. Wolfli) is given. ... |
format |
Article in Journal/Newspaper |
author |
Oeschger, H. Beer, J. Andrée, M. |
spellingShingle |
Oeschger, H. Beer, J. Andrée, M. 10Be and 14C in the earth system ... |
author_facet |
Oeschger, H. Beer, J. Andrée, M. |
author_sort |
Oeschger, H. |
title |
10Be and 14C in the earth system ... |
title_short |
10Be and 14C in the earth system ... |
title_full |
10Be and 14C in the earth system ... |
title_fullStr |
10Be and 14C in the earth system ... |
title_full_unstemmed |
10Be and 14C in the earth system ... |
title_sort |
10be and 14c in the earth system ... |
publisher |
University of Bern |
publishDate |
1987 |
url |
https://dx.doi.org/10.48350/158601 https://boris-portal.unibe.ch/handle/20.500.12422/43246 |
genre |
ice core |
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ice core |
op_doi |
https://doi.org/10.48350/158601 |
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1813448908352782336 |