FN Archimer Export Format
PT J
TI Direct terrestrial-marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe
BT 
AF 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.
AS 1:1,2,3;2:1;3:1;4:2;5:4,5;6:1;7:5,6;8:4;9:1;10:5;11:1;12:4,5;13:10;14:7;15:8;16:9;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;
C1 Leiden Univ, Fac Archaeol, NL-2300 RA Leiden, Netherlands.
   Univ Utrecht, Fac Geosci, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands.
   Natl Ctr Human Evolut CENIEH, Burgos 09002, Spain.
   Landesamt Denkmalpflege & Archaol, D-06114 Halle, Germany.
   Forsch Bereich Altsteinzeit, Romisch German Zent Museum, D-56567 Schloss Monrepos, Neuwied, Germany.
   Johannes Gutenberg Univ Mainz, Inst Vor & Fruhgeschichte, D-55116 Mainz, Germany.
   Univ York, BioArCh Dept Chem, York YO10 5DD, N Yorkshire, England.
   Max Planck Inst Evolutionary Anthropol, Dept Human Evolut, D-04103 Leipzig, Germany.
   Univ Oslo, N-0391 Oslo, Norway.
   Univ Amsterdam, NL-1012 WX Amsterdam, Netherlands.
C2 UNIV LEIDEN, NETHERLANDS
   UNIV UTRECHT, NETHERLANDS
   CENIEH, SPAIN
   LDA LSA, GERMANY
   RGZM, GERMANY
   UNIV MAINZ, GERMANY
   UNIV YORK, UK
   MAX PLANCK INST, GERMANY
   UNIV OSLO, NORWAY
   UNIV AMSTERDAM, NETHERLANDS
IF 2.515
TC 47
UR https://archimer.ifremer.fr/doc/00228/33891/32225.pdf
   https://archimer.ifremer.fr/doc/00228/33891/32226.pdf
LA English
DT Article
CR IMAGES 1-MD101
BO Marion Dufresne
DE ;Blake Event;Eemian;Last interglacial;MIS 5e;Palaeomagnetism
AB 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.
PY 2011
PD JAN
SO Quaternary Research
SN 0033-5894
PU Academic Press Inc Elsevier Science
VL 75
IS 1
UT 000286720900022
BP 213
EP 218
DI 10.1016/j.yqres.2010.11.003
ID 33891
ER

EF