Show simple item record

Files in this item

FilesSizeFormatView

There are no files associated with this item.

Item metadata

dc.contributor.advisorBurke, Andrea
dc.contributor.advisorRae, James William Buchanan
dc.contributor.authorCrumpton-Banks, Jessica Georgina Magdalen
dc.coverage.spatialvi, 238 p.en_US
dc.date.accessioned2020-07-31T11:45:48Z
dc.date.available2020-07-31T11:45:48Z
dc.date.issued2020-12-01
dc.identifier.urihttp://hdl.handle.net/10023/20385
dc.description.abstractThe Southern Ocean is widely thought to play an important role in atmospheric CO₂ change over glacial-interglacial cycles. It has been suggested that as the region that ventilates the majority of the world’s carbon-rich deep waters today, reduced exchange between deep waters and the atmosphere in the Southern Ocean acted to draw down CO₂ over glacial timescales. However, direct evidence of the Southern Ocean’s role in glacial CO₂ drawdown has been lacking thus far. Here I apply the boron-isotope pH-proxy to foraminifera from the Antarctic Zone sediment core PS1506 over the last glacial cycle. The low boron concentrations in these polar foraminifera makes these samples particularly sensitive to boron blank and so a close examination of the sources of blank, and an assessment of the precision of blank measurements, has been made. The ratios of trace elements to calcium in foraminiferal shells are widely applied as proxies for palaeoenvironmental parameters such as temperature. As Southern Ocean carbonate sediments are particularly prone to dissolution, which can affect trace element concentrations, an assessment of dissolution has been made. Firstly, dissolution experiments were conducted to constrain the impact of dissolution in a controlled setting, and secondly, shell mass and trace elements were evaluated for the downcore record. Imaging reveals similar etching textures in both experimentally dissolved samples and deglacial intervals, when shell mass is also low and several trace elements exhibit an excursion to lower values. Boron isotope data for PS1506 show that during the penultimate interglacial, surface water pH was low. At the onset of atmospheric CO₂ drawdown, pH increased, indicating low CO₂ surface waters. This is consistent with the signature predicted for a more stratified Southern Ocean, and is evidence that stratification in the Antarctic Zone acted to contribute to CO₂ drawdown early in the transition to a glacial state.en_US
dc.description.sponsorship"This work was supported by the Natural Environmental Research Council [grant number NE/L002590/1]." -- Fundingen
dc.language.isoenen_US
dc.publisherUniversity of St Andrewsen
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectPalaeoceanographyen_US
dc.subjectSouthern Oceanen_US
dc.subjectForaminiferaen_US
dc.subjectCO₂en_US
dc.subjectGlacial-interglacialen_US
dc.subjectBoron isotopesen_US
dc.subjectClimateen_US
dc.titleGeochemical reconstructions of Southern Ocean pH and temperature over the last glacial cycleen_US
dc.typeThesisen_US
dc.contributor.sponsorNatural Environment Research Council (NERC)en_US
dc.type.qualificationlevelDoctoralen_US
dc.type.qualificationnamePhD Doctor of Philosophyen_US
dc.publisher.institutionThe University of St Andrewsen_US
dc.rights.embargodate2022-06-26
dc.rights.embargoreasonThesis restricted in accordance with University regulations. Electronic copy restricted until 26th June 2022en


The following license files are associated with this item:

    This item appears in the following Collection(s)

    Show simple item record

    Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
    Except where otherwise noted within the work, this item's license for re-use is described as Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International