May 22, 2026
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0:39Now PlayingBy the early 2000s, conventional explanations for the Younger Dryas had reached a breaking point. Paleoclimatologists were correlating radiocarbon dating, varve chronologies, and dendrochronology, building a timeline of Lake Wachellian and Holocene sediments with increasing precision. Tree ring data showed rainfall patterns, thicker varves indicated heavier runoff, and the evidence was stacking up in ways that traditional models struggled to explain.
The prosaic scenarios, the safe assumptions about gradual climate shifts, were running out of explanatory power. Something dramatic had interrupted the warming trend coming out of the last ice age, and the standard mechanisms weren't adding up. The data was pointing toward a more catastrophic trigger, one that required looking beyond slow-moving Earth processes and considering external forcing mechanisms that had been largely dismissed by mainstream science.
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