Mass‐independent isotope effects and their use in understanding natural processes
Abstract In 1983, Thiemens and Heidenreich ( Science 219 , 1073) reported the discovery of a mass‐independent isotope process in oxygen. Subsequently, mass‐independent isotopic compositions were observed in meteorites, atmospheric O 2 , CO 2 , O 3 , H 2 O 2 , CO, N 2 O, and aerosol sulfate and nitra...
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crwiley:10.1560/vm6g-lwec-h5ex-39nr 2023-12-03T10:14:00+01:00 Mass‐independent isotope effects and their use in understanding natural processes Thiemens, Mark H. 2002 http://dx.doi.org/10.1560/vm6g-lwec-h5ex-39nr https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1560%2FVM6G-LWEC-H5EX-39NR https://onlinelibrary.wiley.com/doi/pdf/10.1560/VM6G-LWEC-H5EX-39NR en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Israel Journal of Chemistry volume 42, issue 1, page 43-54 ISSN 0021-2148 1869-5868 General Chemistry journal-article 2002 crwiley https://doi.org/10.1560/vm6g-lwec-h5ex-39nr 2023-11-09T13:10:40Z Abstract In 1983, Thiemens and Heidenreich ( Science 219 , 1073) reported the discovery of a mass‐independent isotope process in oxygen. Subsequently, mass‐independent isotopic compositions were observed in meteorites, atmospheric O 2 , CO 2 , O 3 , H 2 O 2 , CO, N 2 O, and aerosol sulfate and nitrate. In addition, solid samples from the Namibian Desert, Antarctic dry valleys, Miocene volcanic ash, and Death Valley varnishes all possess mass‐independent isotopic compositions that have permitted new scientific insights to be obtained. Sulfur mass‐independent isotopic anomalies in Precambrian samples have provided a completely new mechanism to track atmospheric O 2 levels and the evolution of life from ∼3.9 to 2.2 × 10 9 years ago. Measurements of mass‐independent isotopic compositions in Martian meteoritic sulfates and carbonates have also provided new information on Martian atmosphere‐regolith interactions and history. In sum, the use of mass‐independent isotopic compositions has advanced a wide range of geo‐ and cosmo‐chemical frontiers. In addition, these newly discovered effects have provided a new means to probe the chemical physics of molecular transition state theory. Article in Journal/Newspaper Antarc* Antarctic Wiley Online Library (via Crossref) Antarctic Israel Journal of Chemistry 42 1 43 54 |
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Wiley Online Library (via Crossref) |
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English |
topic |
General Chemistry |
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General Chemistry Thiemens, Mark H. Mass‐independent isotope effects and their use in understanding natural processes |
topic_facet |
General Chemistry |
description |
Abstract In 1983, Thiemens and Heidenreich ( Science 219 , 1073) reported the discovery of a mass‐independent isotope process in oxygen. Subsequently, mass‐independent isotopic compositions were observed in meteorites, atmospheric O 2 , CO 2 , O 3 , H 2 O 2 , CO, N 2 O, and aerosol sulfate and nitrate. In addition, solid samples from the Namibian Desert, Antarctic dry valleys, Miocene volcanic ash, and Death Valley varnishes all possess mass‐independent isotopic compositions that have permitted new scientific insights to be obtained. Sulfur mass‐independent isotopic anomalies in Precambrian samples have provided a completely new mechanism to track atmospheric O 2 levels and the evolution of life from ∼3.9 to 2.2 × 10 9 years ago. Measurements of mass‐independent isotopic compositions in Martian meteoritic sulfates and carbonates have also provided new information on Martian atmosphere‐regolith interactions and history. In sum, the use of mass‐independent isotopic compositions has advanced a wide range of geo‐ and cosmo‐chemical frontiers. In addition, these newly discovered effects have provided a new means to probe the chemical physics of molecular transition state theory. |
format |
Article in Journal/Newspaper |
author |
Thiemens, Mark H. |
author_facet |
Thiemens, Mark H. |
author_sort |
Thiemens, Mark H. |
title |
Mass‐independent isotope effects and their use in understanding natural processes |
title_short |
Mass‐independent isotope effects and their use in understanding natural processes |
title_full |
Mass‐independent isotope effects and their use in understanding natural processes |
title_fullStr |
Mass‐independent isotope effects and their use in understanding natural processes |
title_full_unstemmed |
Mass‐independent isotope effects and their use in understanding natural processes |
title_sort |
mass‐independent isotope effects and their use in understanding natural processes |
publisher |
Wiley |
publishDate |
2002 |
url |
http://dx.doi.org/10.1560/vm6g-lwec-h5ex-39nr https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1560%2FVM6G-LWEC-H5EX-39NR https://onlinelibrary.wiley.com/doi/pdf/10.1560/VM6G-LWEC-H5EX-39NR |
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Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Israel Journal of Chemistry volume 42, issue 1, page 43-54 ISSN 0021-2148 1869-5868 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1560/vm6g-lwec-h5ex-39nr |
container_title |
Israel Journal of Chemistry |
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42 |
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1 |
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43 |
op_container_end_page |
54 |
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1784261029885116416 |