FN Archimer Export Format
PT J
TI A decadal-scale Holocene sea surface temperature record from the subpolar North Atlantic constructed using diatoms and statistics and its relation to other climate parameters
BT 
AF BERNER, K. S.
   KOC, N.
   DIVINE, D.
   GODTLIEBSEN, F.
   MOROS, M.
AS 1:1,3;2:1,3;3:1,2;4:1,2;5:4;
FF 1:;2:;3:;4:;5:;
C1 Norwegian Polar Res Inst, N-9296 Tromso, Norway.
   Univ Tromso, Dept Math & Stat, N-9037 Tromso, Norway.
   Univ Tromso, Dept Geol, N-9037 Tromso, Norway.
   Balt Sea Res Inst, D-18119 Rostock, Germany.
C2 NORWEGIAN POLAR RES INST, NORWAY
   UNIV TROMSO, NORWAY
   UNIV TROMSO, NORWAY
   BALT SEA RES INST, GERMANY
IF 3.626
TC 68
UR https://archimer.ifremer.fr/doc/00237/34843/33268.pdf
LA English
DT Article
CR IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
AB A sediment core from Reykjanes Ridge has been studied at 10- to 50-year time resolution to document variability of Holocene surface water conditions in the western North Atlantic and to evaluate effects of Holocene ice-rafting episodes. Diatom assemblages are converted to quantitative sea surface temperatures (SST) using three different transfer functions. Spectral and scale-space methods are also applied on the records to explore variability at different timescales. Diatom assemblage and SST records clearly show that decaying remnants of the Laurentide ice sheet strongly influenced early Holocene climate in the western North Atlantic. This overrode the predominance of Milankovitch forcing, which played a key role in the development of Holocene climate in the eastern North Atlantic and Nordic Seas. Superimposed on general Holocene climate change is high-frequency SST variability on the order of 1 degrees -3 degrees C. The record also documents climatic oscillations with 600- to 1000-, similar to 1500-, and 2500-year periodicities, with a time-dependent dominance of different periodicities through the Holocene; a clear change in variability occurred about 5 ka BP. The SST record also provides evidence for Holocene cooling events (HCE) that, in some cases, correlate to documented southward intrusions of ice into the North Atlantic.
PY 2008
PD MAY
SO Paleoceanography
SN 0883-8305
PU Amer Geophysical Union
VL 23
IS 2 / PA2210
UT 000256063700001
BP 1
EP 15
DI 10.1029/2006PA001339
ID 34843
ER

EF