Abrupt changes in climate have occurred in many locations around the globe over the last
glacial cycle, with pronounced temperature swings on timescales of decades or less in the …

More than a decade ago, ice core records from Greenland revealed that the last glacial
period was characterized by abrupt climate changes that recurred on millennial time scales …

Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …

High-resolution grain size and magnetic susceptibility records from the eastern Gulf of Cadiz
(site MD99-2339; 1170m water depth) reveal contourites formed by the Mediterranean …

基于湖北神农架青天洞一支年纹层石笋(编号: QT15) 高分辨δ 18 O 序列, 重建了29.4~ 27.4 ka
BP 亚洲夏季风演化历史. QT15 石笋δ 18 O 在约27.9 ka BP 和28.7 ka BP 显著偏负 …

The direct sea–land correlation applied to core MD99-2331 retrieved from the north-western
Iberian margin shows a two-phase pattern within Heinrich events 4, 2 and 1 in the ocean …

Rapid changes in ocean circulation and climate have been observed in marine-sediment
and ice cores over the last glacial period and deglaciation, highlighting the non-linear …

Eight-to ten-point depth profiles (from 1200 to 4800m water depth) of oxygen and carbon
isotopic values derived from benthic foraminifera, averaged over selected times in the past …

The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical
role in ocean circulation and climate change, yet its variability during the last glacial period …