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Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) ArchiMer
Zhuravleva, Anastasia.
The last interglacial, MIS (Marine Isotope Stage) 5e, lasting from about ~129 to 116 ka, holds important implications for the projected global warming, as this geological interval is believed to have been significantly warmer-than-preindustrial. This thesis refines the current understanding of the MIS 5e paleoceanography in the subarctic and subtropical North Atlantic, providing new insights into ice-sheets dynamics and cross-latitudinal climatic teleconnections. For this purpose, a multi-proxy dataset comprising stable isotope compositions, foraminiferal assemblages and lithic as well as X-ray fluorescence data was produced using marine sediments from the Nordic Seas and the Bahama region. Several lines of evidence from the Nordic Seas suggest a strong...
Tipo: Text Palavras-chave: Last interglacial; MIS 5e; Greenland ice sheet; AMOC; ITCZ; Climatic variability letztes Interglazial; MIS 5e; Grönländisches Eisschild; AMOC; ITCZ; Klimatische Variabilität.
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00495/60640/64136.pdf
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Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e) ArchiMer
Irvali, Nil; Ninnemann, Ulysses S.; Galaasen, Eirik V.; Rosenthal, Yair; Kroon, Dick; Oppo, Delia W.; Kleiven, Helga F.; Darling, Kate F.; Kissel, Catherine.
At the peak of the previous interglacial period, North Atlantic and subpolar climate shared many features in common with projections of our future climate, including warmer-than-present conditions and a diminished Greenland Ice Sheet (GIS). Here we portray changes in North Atlantic hydrography linked with Greenland climate during Marine Isotope Stage (MIS) 5e using (sub)centennially sampled records of planktonic foraminiferal isotopes and assemblage counts and ice-rafted debris counts, as well as modern analog technique and Mg/Ca-based paleothermometry. We use the core MD03-2664 recovered from a high accumulation rate site (similar to 34 cm/kyr) on the Eirik sediment drift (57 degrees 26.34'N, 48 degrees 36.35'W). The results indicate that surface waters...
Tipo: Text Palavras-chave: Eirik Drift; MIS 5e; North Atlantic; Last interglacial; Multiproxy.
Ano: 2012 URL: https://archimer.ifremer.fr/doc/00139/25046/23154.pdf
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Direct terrestrial-marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe ArchiMer
Sier, Mark J.; Roebroeks, Wil; Bakels, Corrie C.; Dekkers, Mark J.; Bruehl, Enrico; De Loecker, Dimitri; Gaudzinski-windheuser, Sabine; Hesse, Norbert; Jagich, Adam; Kindler, Lutz; Kuijper, Wim J.; Laurat, Thomas; Muecher, Herman J.; Penkman, Kirsty E. H.; Richter, Daniel; Van Hinsbergen, Douwe J. J..
An interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 +/- 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e 'peak' in the marine record and the start of the last interglacial in this region.
Tipo: Text Palavras-chave: Blake Event; Eemian; Last interglacial; MIS 5e; Palaeomagnetism.
Ano: 2011 URL: https://archimer.ifremer.fr/doc/00228/33891/32225.pdf
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