Isotopic signatures
© 2018 Elsevier Inc. All rights reserved. Isotopes record human influence on the Earth System, providing evidence for the Anthropocene. Lead and sulfur isotopes detail pollution histories going back millennia. Carbon and nitrogen isotopes show substantial change since the Industrial Revolution, and...
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ftunivhullir:oai:hull-repository.worktribe.com:3444393 2023-05-15T17:50:53+02:00 Isotopic signatures Dean, J. R. Leng, M. J. Mackay, A. W. 2017-11-29 https://hull-repository.worktribe.com/output/3444393 https://doi.org/10.1016/B978-0-12-809665-9.10023-0 unknown Elsevier https://hull-repository.worktribe.com/output/3444393 Pagination 197-203 doi:https://doi.org/10.1016/B978-0-12-809665-9.10023-0 9780128096659; 9780128135761 doi:10.1016/B978-0-12-809665-9.10023-0 Boron Carbon Cesium Earth System Golden spike GSSP Isotope Lead Nitrogen Plutonium Radioisotope Suess effect Sulfur Specialist Research - Other Energy Environment and Sustainability Book Chapter 2017 ftunivhullir https://doi.org/10.1016/B978-0-12-809665-9.10023-0 2023-03-26T20:25:23Z © 2018 Elsevier Inc. All rights reserved. Isotopes record human influence on the Earth System, providing evidence for the Anthropocene. Lead and sulfur isotopes detail pollution histories going back millennia. Carbon and nitrogen isotopes show substantial change since the Industrial Revolution, and especially since the 1950s, related to increased fossil fuel consumption and fertilizer production. Boron isotopes record ocean acidification related to CO2 emissions. Radioisotopes, for example plutonium, have been dispersed across the Earth since the 1950s due to nuclear weapons testing and can be used as stratigraphic markers for the time that carbon and nitrogen isotopes, and non-isotope proxies, show increased human influence on the Earth System. Book Part Ocean acidification University of Hull: Repository@Hull 197 203 |
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University of Hull: Repository@Hull |
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Boron Carbon Cesium Earth System Golden spike GSSP Isotope Lead Nitrogen Plutonium Radioisotope Suess effect Sulfur Specialist Research - Other Energy Environment and Sustainability |
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Boron Carbon Cesium Earth System Golden spike GSSP Isotope Lead Nitrogen Plutonium Radioisotope Suess effect Sulfur Specialist Research - Other Energy Environment and Sustainability Dean, J. R. Leng, M. J. Mackay, A. W. Isotopic signatures |
topic_facet |
Boron Carbon Cesium Earth System Golden spike GSSP Isotope Lead Nitrogen Plutonium Radioisotope Suess effect Sulfur Specialist Research - Other Energy Environment and Sustainability |
description |
© 2018 Elsevier Inc. All rights reserved. Isotopes record human influence on the Earth System, providing evidence for the Anthropocene. Lead and sulfur isotopes detail pollution histories going back millennia. Carbon and nitrogen isotopes show substantial change since the Industrial Revolution, and especially since the 1950s, related to increased fossil fuel consumption and fertilizer production. Boron isotopes record ocean acidification related to CO2 emissions. Radioisotopes, for example plutonium, have been dispersed across the Earth since the 1950s due to nuclear weapons testing and can be used as stratigraphic markers for the time that carbon and nitrogen isotopes, and non-isotope proxies, show increased human influence on the Earth System. |
format |
Book Part |
author |
Dean, J. R. Leng, M. J. Mackay, A. W. |
author_facet |
Dean, J. R. Leng, M. J. Mackay, A. W. |
author_sort |
Dean, J. R. |
title |
Isotopic signatures |
title_short |
Isotopic signatures |
title_full |
Isotopic signatures |
title_fullStr |
Isotopic signatures |
title_full_unstemmed |
Isotopic signatures |
title_sort |
isotopic signatures |
publisher |
Elsevier |
publishDate |
2017 |
url |
https://hull-repository.worktribe.com/output/3444393 https://doi.org/10.1016/B978-0-12-809665-9.10023-0 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://hull-repository.worktribe.com/output/3444393 Pagination 197-203 doi:https://doi.org/10.1016/B978-0-12-809665-9.10023-0 9780128096659; 9780128135761 doi:10.1016/B978-0-12-809665-9.10023-0 |
op_doi |
https://doi.org/10.1016/B978-0-12-809665-9.10023-0 |
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197 |
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203 |
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1766157812047544320 |