Abstract Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing
to the ocean is important to better understand the mechanisms behind abrupt climate …

We use eighteen timescale-synchronised near-surface temperature reconstructions
spanning 10–50 thousand years before present to clarify the regional expression of …

The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …

In the light of rapidly diminishing sea ice cover in the Arctic during the present atmospheric
warming, it is imperative to study the distribution of sea ice in the past in relation to rapid …

Constraints on the timing of Atlantic meridional overturning circulation (AMOC) changes
during the last deglaciation are fundamental to understanding the climate's rapid response …

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 …

The precise reason for the differences and out-of-phase relationship between the abrupt
Dansgaard-Oeschger warmings in the Nordic seas and Greenland ice cores and the …

Marine radiocarbon dates, corrected for ocean‐atmosphere reservoir age offsets (R‐ages),
are widely used to constrain marine chronologies. R‐ages also represent the surface …

Species assemblage composition of marine microfossils offers the possibility to investigate
ecological and climatological change on time scales inaccessible using conventional …

Tephrochronology is increasingly being recognised as a key tool for the correlation of
disparate palaeoclimatic archives, underpinning chronological models and facilitating …