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dc.contributor.advisorAagaard Sørensen, Steffen
dc.contributor.authorPaavilainen, Anne
dc.date.accessioned2023-06-14T05:36:46Z
dc.date.available2023-06-14T05:36:46Z
dc.date.issued2023-05-15en
dc.description.abstractThe main ambition of this thesis was to study the relationship between isotopic signature of fossil foraminifera and past methane emission at Storfjordrenna Pingos site (South of Svalbard) during the last deglaciation in context of past climatic changes. Two gravity cores, the core 1070 from the flank of the presently inactive gas hydrate pingo 5 (GHP5) and the core 1069 from the top of the GHP5, were investigated in detail. Combined benthic and planktic δ13C records, visual investigations (SEM-EDS) of the foraminiferal tests and the solid phase composition of the sediment (XRF) revealed interesting and complex methane seepage history at the presently inactive GHP5. Several paleo seepage events were found from deglaciation and Holocene deposits.en_US
dc.identifier.urihttps://hdl.handle.net/10037/29392
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universitetno
dc.publisherUiT The Arctic University of Norwayen
dc.rights.holderCopyright 2023 The Author(s)
dc.rights.urihttps://creativecommons.org/licenses/by-nc-sa/4.0en_US
dc.rightsAttribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)en_US
dc.subject.courseIDGEO-3900
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466en_US
dc.titleMultiproxy reconstruction of past methane emissions at Storfjordrenna Pingos site (South of Svalbard) during the last deglaciationen_US
dc.typeMastergradsoppgavenor
dc.typeMaster thesiseng


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Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
Med mindre det står noe annet, er denne innførselens lisens beskrevet som Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)