Oeschger, H.; Beer, J.; Andrée, M. (1987). 10Be and 14C in the earth system. Philosophical transactions of the Royal Society. Series A - mathematical, physical and engineering sciences, 323(1569), pp. 45-56. Royal Society of London 10.1098/rsta.1987.0071
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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.
Item Type: |
Journal Article (Original Article) |
|---|---|
Division/Institute: |
08 Faculty of Science > Physics Institute > Climate and Environmental Physics |
Subjects: |
500 Science > 530 Physics |
ISSN: |
1364-503X |
Publisher: |
Royal Society of London |
Language: |
English |
Submitter: |
BORIS Import 2 |
Date Deposited: |
11 Oct 2021 12:15 |
Last Modified: |
13 Oct 2021 07:12 |
Publisher DOI: |
10.1098/rsta.1987.0071 |
BORIS DOI: |
10.48350/158601 |
URI: |
https://boris.unibe.ch/id/eprint/158601 |
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