Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...

The boron isotope proxy is a valuable tool for reconstructing ocean pH and atmospheric CO₂ in Earth’s history. Its use on foraminifera in deep sea sediment cores has helped shape our understanding of Cenozoic carbon cycling and climate change, yet most of the extreme examples of biotic and climatic...

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Main Author: Trudgill, Molly Diana
Format: Article in Journal/Newspaper
Language:English
Published: The University of St Andrews 2023
Subjects:
Online Access:https://dx.doi.org/10.17630/sta/327
https://research-repository.st-andrews.ac.uk/handle/10023/27101
id ftdatacite:10.17630/sta/327
record_format openpolar
spelling ftdatacite:10.17630/sta/327 2023-05-15T17:51:16+02:00 Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ... Trudgill, Molly Diana 2023 https://dx.doi.org/10.17630/sta/327 https://research-repository.st-andrews.ac.uk/handle/10023/27101 en eng The University of St Andrews Thesis restricted in accordance with University regulations. Restricted until 12th January 2028 2028-01-12 Creative Commons Attribution Non Commercial No Derivatives 4.0 International Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 Boron isotopes Ocean pH CO₂ Mass extinction events Paleoclimate Ocean acidification QC884.T8 Paleoclimatology Boron--Isotopes Atmospheric carbon dioxide article CreativeWork 2023 ftdatacite https://doi.org/10.17630/sta/327 2023-04-03T13:22:20Z The boron isotope proxy is a valuable tool for reconstructing ocean pH and atmospheric CO₂ in Earth’s history. Its use on foraminifera in deep sea sediment cores has helped shape our understanding of Cenozoic carbon cycling and climate change, yet most of the extreme examples of biotic and climatic change are in the geological record, where the proxy has seen limited use. The boron isotope proxy’s widespread usage is also hindered by the challenges involved in traditional methods for measuring it: gravity microcolumns require exacting laboratory conditions and are time intensive. Older samples may have more variable matrices which can also be a problem for a gravity column. In order to expand the boron isotope proxy into a wider variety of matrices, Chapter 3 presents a new batch method for the purification of boron from its sample matrix. Together with methodological improvements for measurement by MC-ICPMS discussed in Chapter 2, these developments allow for measurement of a wide variety of samples with ... Article in Journal/Newspaper Ocean acidification DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Boron isotopes
Ocean pH
CO₂
Mass extinction events
Paleoclimate
Ocean acidification
QC884.T8
Paleoclimatology
Boron--Isotopes
Atmospheric carbon dioxide
spellingShingle Boron isotopes
Ocean pH
CO₂
Mass extinction events
Paleoclimate
Ocean acidification
QC884.T8
Paleoclimatology
Boron--Isotopes
Atmospheric carbon dioxide
Trudgill, Molly Diana
Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
topic_facet Boron isotopes
Ocean pH
CO₂
Mass extinction events
Paleoclimate
Ocean acidification
QC884.T8
Paleoclimatology
Boron--Isotopes
Atmospheric carbon dioxide
description The boron isotope proxy is a valuable tool for reconstructing ocean pH and atmospheric CO₂ in Earth’s history. Its use on foraminifera in deep sea sediment cores has helped shape our understanding of Cenozoic carbon cycling and climate change, yet most of the extreme examples of biotic and climatic change are in the geological record, where the proxy has seen limited use. The boron isotope proxy’s widespread usage is also hindered by the challenges involved in traditional methods for measuring it: gravity microcolumns require exacting laboratory conditions and are time intensive. Older samples may have more variable matrices which can also be a problem for a gravity column. In order to expand the boron isotope proxy into a wider variety of matrices, Chapter 3 presents a new batch method for the purification of boron from its sample matrix. Together with methodological improvements for measurement by MC-ICPMS discussed in Chapter 2, these developments allow for measurement of a wide variety of samples with ...
format Article in Journal/Newspaper
author Trudgill, Molly Diana
author_facet Trudgill, Molly Diana
author_sort Trudgill, Molly Diana
title Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
title_short Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
title_full Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
title_fullStr Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
title_full_unstemmed Boron based geochemical reconstructions of ocean pH and atmospheric CO₂ in the geological record ...
title_sort boron based geochemical reconstructions of ocean ph and atmospheric co₂ in the geological record ...
publisher The University of St Andrews
publishDate 2023
url https://dx.doi.org/10.17630/sta/327
https://research-repository.st-andrews.ac.uk/handle/10023/27101
genre Ocean acidification
genre_facet Ocean acidification
op_rights Thesis restricted in accordance with University regulations. Restricted until 12th January 2028
2028-01-12
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
op_doi https://doi.org/10.17630/sta/327
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