Extreme cooling events during the last glacial, known as Heinrich Events in the North Atlantic, are a good example of how local processes change the global climate. While the impacts of Heinrich Events on the global glacial environment are well-documented in the scientific literature, their causes are still unclear. In a new study, researchers from Bremen, Kiel, Köln and São Paulo (Brazil) have now shown that an accumulation of heat in the deeper Labrador Sea caused instabilities in the Laurentide Ice Sheet, which covered much of North America at the time. The Heinrich Events were triggered as a result. The researchers demonstrated this by reconstructing past temperatures and salinities in the North Atlantic. Their results have now been published in Nature Communications.
Heinrich Events or, more accurately, Heinrich Layers, are recurrent conspicuous sediment layers, usually ten to 15 centimeters thick, with very coarse rock components that interrupt the otherwise fine-grained oceanic deposits in the North Atlantic. Discovered and described for the first time in the 1980s by geologist Hartmut Heinrich, U.S. geochemist Wally Broecker later officially named them Heinrich Layers, which has become a standard term in paleoceanography.
The presence of Heinrich Layers has been established throughout the North Atlantic, from off Iceland, southward to a line running from New York to North Africa. Such coarse rock debris could only have been transported such a great distance from its point of origin in the Hudson Bay by icebergs.






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