Did a volcanic cataclysm trigger Neanderthals’ demise?

The Campanian Ignimbrite (CI) eruption in Italy 40,000 years ago was one of the largest volcanic cataclysms in Europe, and injected a significant amount of sulfur-dioxide (SO2) into the stratosphere.

Scientists have long debated whether this eruption contributed to the final extinction of the Neanderthals, and a new study tested this hypothesis with a sophisticated climate model.

Male and female Homo neanderthalensis

The final decline of the Neanderthals

In research published in March 2015, Benjamin A Black and colleagues wrote that the CI eruption approximately coincided with the final decline of Neanderthals, as well as with dramatic territorial and cultural advances among anatomically modern humans.

Because of this, the roles of climate, hominin competition, and volcanic sulfur cooling and acid deposition have been vigorously debated as causes of Neanderthal extinction.

They point out, however, that the decline of Neanderthals in Europe began well before the CI eruption: “Radiocarbon dating has shown that at the time of the CI eruption, anatomically modern humans had already arrived in Europe, and the range of Neanderthals had steadily diminished. Work at five sites in the Mediterranean indicates that anatomically modern humans were established in these locations by then as well.”

>> Ancient skull proves modern humans long coexisted, interbred with Neanderthals

“While the precise implications of the CI eruption for cultures and livelihoods are best understood in the context of archaeological data sets,” write Black and colleagues, the results of their study quantitatively describe the magnitude and distribution of the volcanic cooling and acid deposition that ancient hominin communities experienced coincident with the final decline of the Neanderthals.

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Climate simulations of the era

In their climate simulations, Black and colleagues found that the largest temperature decreases after the eruption occurred in Eastern Europe and Asia and sidestepped the areas where the final Neanderthal populations were living (Western Europe). Therefore, the authors conclude that the eruption was probably insufficient to trigger Neanderthal extinction.

>> Neanderthal DNA is still among us



However, the abrupt cold spell that followed the eruption would still have significantly impacted day-to-day life for Neanderthals and early humans in Europe. Black and colleagues point out that temperatures in Western Europe would have decreased by an average of 2 to 4 degrees Celsius (3.6 to 7.2 degrees Fahrenheit) during the year following the eruption.

These unusual conditions, they write, may have directly influenced survival and day-to-day life for Neanderthals and anatomically-modern humans alike, and emphasize the resilience of anatomically-modern humans in the face of abrupt and adverse changes in the environment.

temperatures neanderthals



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