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dc.contributor.advisorRasmussen, Tine
dc.contributor.advisorZamelczyk, Kasia
dc.contributor.advisorJunttila, Juho
dc.contributor.authorBaker, May Lizabeth
dc.date.accessioned2017-09-01T05:44:51Z
dc.date.available2017-09-01T05:44:51Z
dc.date.issued2017-08-01
dc.description.abstractThe benthic foraminifera of two marine sediment cores were studied as a proxy for paleoenvironment reconstructions throughout the Late to Early Holocene. The two cores were sampled in different localities to allow a spatial comparison of changing environments in the Nordic Seas and sampled for benthic foraminiferal assemblages, grain size, IRD, sortable silts and benthic foraminifera isotopes. While attempts at correlation were made, differing sedimentation rates made this difficult. A cold period spanning ~1000 years can be seen in both sediment records, attributed to the Dark Ages Cold Period. Benthic assemblages and isotope records show only vague similarities throughout the Late Holocene, suggesting that the core environments were subject to differing climatic influences due to their different localities, with only large scale climatic events effecting both areas equallyen_US
dc.identifier.urihttps://hdl.handle.net/10037/11403
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universiteten_US
dc.publisherUiT The Arctic University of Norwayen_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2017 The Author(s)
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.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Quaternary geology, glaciology: 465en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi, glasiologi: 465en_US
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452en_US
dc.titleReconstructing the holocene. Benthic foraminifera as a proxy for the paleoceonography of the nordic seasen_US
dc.typeMaster thesisen_US
dc.typeMastergradsoppgaveen_US


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