Multiple Severe Volcanic Eruptions Between 536 and 540 AD Triggered a Long Lasting Cold Event

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The mechanism is well understood. Large explosive volcanic eruptions inject sulfur dioxide into the stratosphere, where it forms sulfate aerosols that reflect incoming solar radiation back into space. The result is a measurable reduction in sunlight reaching the Earth's surface - and with it, a collapse in agricultural productivity that cascades through every civilisation dependent on it.
Between 536 and 540 AD, multiple severe eruptions produced exactly this effect at a scale not seen in the preceding millennia. The cold event that followed is not speculative. It is recorded across independent data streams simultaneously - dendrochronology showing stunted tree ring growth, ice core records preserving the volcanic sulfate layers, and historical sources from cultures across the Northern Hemisphere describing crop failures, famine, and societal breakdown. Randall Carlson connects this directly to the broader pattern he has spent decades documenting: abrupt climatic disruption as one of the primary drivers of civilisation collapse, population decline, and the reorganisation of material culture across the ancient world. The 530s AD are among the clearest and best evidenced examples in the historical record.

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