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dc.contributor.authorMeland, Marius Yddaleng
dc.date.accessioned2006-12-19T13:14:33Z
dc.date.available2006-12-19T13:14:33Z
dc.date.issued2006-09-01eng
dc.identifier.isbn82-308-0168-1 (print version)en_US
dc.identifier.urihttps://hdl.handle.net/1956/2010
dc.description.abstractThe paleoceanography of the Nordic Seas and the northern North Atlantic during glacial and deglacial times was studied, using oxygen isotopes and Mg/Ca of foraminifera. The specific objectives are listed below: 1) Sea surface temperatures (SST) during the Last Glacial Maximum (LGM, ∼20 000 years ago) were reconstructed, using oxygen isotopes of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral). 2) The LGM climate (air temperatures, precipitation/moisture, air pressure, wind systems) was simulated, using the SSTs produced under Objective 1 as boundary conditions. 3) Mg/Ca ratios of N. pachyderma (sin.) were tested to see if they could be used to make surface/subsurface temperature estimates in the Nordic Seas for previous times. 4) Water mass exchanges between the North Atlantic and the Nordic Seas through the period 22 000 - 6000 years ago were studied. This period covers the LGM, the last deglaciation and the recent interglacial (Holocene). Benthic oxygen isotopes were used as the main proxy, supported by benthic carbon isotopes and planktonic oxygen isotopes.en_US
dc.format.extent1585302 byteseng
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dc.format.mimetypeapplication/pdfeng
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dc.language.isoengeng
dc.publisherThe University of Bergenen_US
dc.relation.haspartPaper I: Quaternary Science Reviews 24, Meland, M. Y; Jansen, E.; Elderfield, H., Constraints on SST estimates for the northern North Atlantic/Nordic Seas during the LGM, pp. 835-852. Copyright 2005 Elsevier. The published version is available at: <a href="http://dx.doi.org/10.1016/j.quascirev.2004.05.011"target=_blank>http://dx.doi.org/10.1016/j.quascirev.2004.05.011</a>en_US
dc.relation.haspartPaper II: Climate Dynamics 26, Byrkjedal Ø.; Kvamstø, N. G.; Meland, M. Y.; Jansen E.; Sensitivity of last glacial maximum climate to sea ice conditions in the Nordic Seas, pp. 473-487. Copyright 2006 Springer Verlag. Fulltext not available due to publisher restrictions. The published version is available at: <a href="http://dx.doi.org/10.1007/s00382-005-0096-2"target=_blank>http://dx.doi.org/10.1007/s00382-005-0096-2</a>en_US
dc.relation.haspartPaper III: Meland, M. Y.; Jansen, E.; Elderfield, H.; Dokken, T. M.; Olsen, A.; Bellerby, R. G. J., Mg/Ca ratios in the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in the northern North Atlantic/Nordic Seas, Geochemistry Geophysics Geosystems 7: Q06P14, 2006. Copyright 2006 The American Geophysical Union. Reproduced by permission of American Geophysical Union. The published version is available at: <a href="http://dx.doi.org/10.1029/2005GC001078"target=_blank>http://dx.doi.org/10.1029/2005GC001078</a>en_US
dc.relation.haspartPaper VI: Meland, M. Y.; Dokken, T. M.; Jansen, E.; Hevrøy, K., Water mass properties and exchange between the Nordic Seas and the northern North Atlantic during the period 22-6 ka: benthic oxygen isotope evidence. Pre-print.en_US
dc.titlePaleoceanography and paleoclimate in the Nordic Seas and the northern North Atlantic during the last 22 000 yearsen_US
dc.typeDoctoral thesis
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Faste jords fysikk: 451nob


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