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Bipolar impact and phasing of Heinrich-type climate variability - Nature
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During the last ice age, the Laurentide Ice Sheet exhibited extreme iceberg discharge events that are recorded in North Atlantic sediments1. These Heinrich events have far-reaching climate impacts, including widespread disruptions to hydrological and biogeochemical cycles2–4. They occurred during Heinrich stadials—cold periods with strongly weakened Atlantic overturning circulation5–7.
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