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Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.

Includes bibliographical references (leaves 228-270).

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Bibliographic Details
Main Author: Thomalla, S J
Other Authors: Lucas, Mike
Format: Thesis
Language:English
Published: Department of Oceanography 2014
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access_status_str Open Access
author Thomalla, S J
author2 Lucas, Mike
author_browse Lucas, Mike
Thomalla, S J
author_facet Lucas, Mike
Thomalla, S J
author_sort Thomalla, S J
collection Thesis
description Includes bibliographical references (leaves 228-270).
format Thesis
id oai:open.uct.ac.za:11427/6452
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:35.758Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2014
publishDateRange 2014
publishDateSort 2014
publisher Department of Oceanography
publisherStr Department of Oceanography
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/6452 Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach. Thomalla, S J Lucas, Mike Turnewitsch, Robert Oceanography Includes bibliographical references (leaves 228-270). Subtropical ocean gyres are typically characterised by low carbon export into the deep ocean. However, due to their large area, even relatively small average carbon export may be globally significant. Strong correlations observed between deep-sea organic carbon, calcite and opal suggest that mineral phases may enhance the export and survival of organic matter as it sinks (the 'ballast effect'). However, the processes underlying these correlations are not well understood and remain key uncertainties in models that predict global carbon cycling. To better constrain carbon and mineral export from the surface ocean of subtropical gyres, radioactive disequilibria between 234Th and 238U were used to estimate fluxes of particulate organic carbon (POe), calcite and opal in the North and South Atlantic subtropical gyres. 2014-08-13T19:44:48Z 2014-08-13T19:44:48Z 2007 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/6452 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Oceanography
Thomalla, S J
Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
thesis_degree_str Doctoral
title Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
title_full Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
title_fullStr Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
title_full_unstemmed Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
title_short Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach.
title_sort particulate organic carbon and mineral export from the north and south atlantic gyres the 234th 238u disequilibrium approach
topic Oceanography
url http://hdl.handle.net/11427/6452
work_keys_str_mv AT thomallasj particulateorganiccarbonandmineralexportfromthenorthandsouthatlanticgyresthe234th238udisequilibriumapproach