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The transition from the Last Glacial Maximum to the Holocene was an internal of climate variability that was characterised by large spatial and temporal variations. Here we show that deglaciation warming in the northern Indian Ocean was initiated ca. 19 ka, which is contemporary with deglaciation warming in the Antarctica and Southern Ocean. A gradual warming occurred during the glacial/Holocene transition...
A sediment core from the north‐east North Atlantic contains high‐resolution co‐registered foraminiferal δ18O and ice‐rafted detritus (IRD) records for the last deglaciation. These reveal a distinct ice‐rafting event that occurred at the time of Greenland Interstade 1d (GI‐1d), a feature also seen in other high‐resolution cores from the North Atlantic. The occurrence of a geographically widespread...
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