10 Be and 14 C in the Earth system

In a very short period of time, 10 Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10 Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10 Be i...

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Published in:Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 1987
Subjects:
ice core
Online Access:http://dx.doi.org/10.1098/rsta.1987.0071
https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1987.0071
id crroyalsociety:10.1098/rsta.1987.0071
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spelling crroyalsociety:10.1098/rsta.1987.0071 2024-06-02T08:08:07+00:00 10 Be and 14 C in the Earth system 1987 http://dx.doi.org/10.1098/rsta.1987.0071 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1987.0071 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences volume 323, issue 1569, page 45-56 ISSN 0080-4614 2054-0272 journal-article 1987 crroyalsociety https://doi.org/10.1098/rsta.1987.0071 2024-05-07T14:16:23Z In a very short period of time, 10 Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10 Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10 Be ice-core (from the past 10 ka) and ocean-sediment profiles (geomagnetic reversals); (c) climatic effects reflected in 10 Be profiles in loess and polar ice cores ( 10 Be behaviour in atmosphere); (d) comparison of 10 Be and 14 C variations (tree rings) from carbon-cycle models and inform ation on ocean circulation history from 14 C 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 The Royal Society Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences 323 1569 45 56
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description In a very short period of time, 10 Be data have significantly improved our knowledge in various fields of Earth and planetary sciences. Examples are: (a) solar modulation of isotope production, revealed in 10 Be ice-core profiles; (b)geomagnetic m odulation of isotope production, revealed in 10 Be ice-core (from the past 10 ka) and ocean-sediment profiles (geomagnetic reversals); (c) climatic effects reflected in 10 Be profiles in loess and polar ice cores ( 10 Be behaviour in atmosphere); (d) comparison of 10 Be and 14 C variations (tree rings) from carbon-cycle models and inform ation on ocean circulation history from 14 C 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
title 10 Be and 14 C in the Earth system
spellingShingle 10 Be and 14 C in the Earth system
title_short 10 Be and 14 C in the Earth system
title_full 10 Be and 14 C in the Earth system
title_fullStr 10 Be and 14 C in the Earth system
title_full_unstemmed 10 Be and 14 C in the Earth system
title_sort 10 be and 14 c in the earth system
publisher The Royal Society
publishDate 1987
url http://dx.doi.org/10.1098/rsta.1987.0071
https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1987.0071
genre ice core
genre_facet ice core
op_source Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
volume 323, issue 1569, page 45-56
ISSN 0080-4614 2054-0272
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rsta.1987.0071
container_title Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
container_volume 323
container_issue 1569
container_start_page 45
op_container_end_page 56
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