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Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf

Includes bibliographical references (leaves 82-89).

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Bibliographic Details
Main Author: Joubert, Warren R
Other Authors: Roychoudhury, Alakendra N
Format: Thesis
Language:English
Published: Department of Geological Sciences 2014
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access_status_str Open Access
author Joubert, Warren R
author2 Roychoudhury, Alakendra N
author_browse Joubert, Warren R
Roychoudhury, Alakendra N
author_facet Roychoudhury, Alakendra N
Joubert, Warren R
author_sort Joubert, Warren R
collection Thesis
description Includes bibliographical references (leaves 82-89).
format Thesis
id oai:open.uct.ac.za:11427/4204
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:41:36.780Z
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 Geological Sciences
publisherStr Department of Geological Sciences
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/4204 Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf Joubert, Warren R Roychoudhury, Alakendra N Monteiro, Pedro M S Geochemistry Includes bibliographical references (leaves 82-89). The Central Benguela inner shelf is characterised by hypoxic to anoxic sub-thermocline water conditions on a semi-permanent basis. Historical understanding of the incidence of hypoxia is that the inner shelf area off Namibia is one of the main areas of formation of low oxygen water (LOW) in the Benguela upwelling system. Local biogeochemical remineralization of organic matter mostly related to the primary production in surface waters (Chapman and Shannon, 1985) is thought to drive seasonal variability in sediment oxygen demand. New understanding of the system suggests that shelf hypoxia is driven by a remotely forced equatorial hypoxic boundary condition thought to trigger anaerobic remineralization and increased sediment fluxes of reduced metabolites (Monteiro et al., in press). The study focused on seasonal variability of sediment oxygen demand on the Namibian inner shelf and its relation to particulate organic carbon and reduced metabolite fluxes. 2014-07-30T17:26:25Z 2014-07-30T17:26:25Z 2006 Master Thesis Masters MSc http://hdl.handle.net/11427/4204 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geochemistry
Joubert, Warren R
Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
thesis_degree_str Master's
title Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
title_full Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
title_fullStr Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
title_full_unstemmed Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
title_short Seasonal variability of sediment oxygen demand and biogeochemistry on the Namibian inner shelf
title_sort seasonal variability of sediment oxygen demand and biogeochemistry on the namibian inner shelf
topic Geochemistry
url http://hdl.handle.net/11427/4204
work_keys_str_mv AT joubertwarrenr seasonalvariabilityofsedimentoxygendemandandbiogeochemistryonthenamibianinnershelf