Hominin History / Articles / Human bottlenecks
Human Evolution 101

Did Humans Nearly Go Extinct?

Two famous claims say our ancestors came close to vanishing: once after a supervolcano, and once for over 100,000 years. One has largely collapsed. The other is still being fought over.

The short answer

The idea that the Toba supereruption about 74,000 years ago nearly wiped out Homo sapiens is now poorly supported: archaeological sites in India, South Africa and Ethiopia show people carried on through it. A separate 2023 genetic study proposed that our ancestors fell to roughly 1,280 breeding individuals between about 930,000 and 813,000 years ago. That result is real science but contested, because other methods do not detect it.

Humans are strikingly similar to one another genetically. Two chimpanzees from neighbouring forests in central Africa can differ more than two people from opposite sides of the planet. For decades, that low diversity has invited a dramatic explanation: at some point, our ancestors were reduced to a very small population and squeezed through a bottleneck.

Two candidate catastrophes have dominated the debate. One is a supervolcano. The other is a long, slow crisis nearly a million years ago. Here is how each claim holds up.

FeatureToba catastrophe hypothesisEarly Pleistocene bottleneck
When~74,000 years ago~930,000–813,000 years ago
WhoHomo sapiens (and others)The shared ancestors of sapiens, Neanderthals and Denisovans
Proposed causeVolcanic winter after the Toba eruptionClimate shifts of the Mid-Pleistocene Transition
Claimed sizeA few thousand to ~10,000 people~1,280 breeding individuals for ~117,000 years
Main evidenceLow genetic diversity; eruption scaleFitCoal analysis of 3,154 modern genomes
Status todayLargely rejectedActively debated

Toba: the biggest eruption in two million years

About 74,000 years ago, the Toba volcano on Sumatra erupted with a force unmatched in the last two million years. It ejected on the order of 2,800 cubic kilometres of material — thousands of times more than Mount St Helens in 1980. Lake Toba, 100 kilometres long, fills the collapsed caldera today. Ash fell as far away as India, where layers several metres thick survive, and fine glass shards reached southern Africa.

In 1998 the anthropologist Stanley Ambrose connected the eruption to the genetic evidence. His Toba catastrophe hypothesis proposed that years of volcanic winter and a millennium of cold killed most humans, leaving perhaps a few thousand to 10,000 survivors, and that later human populations diversified rapidly from this remnant.

Why the Toba catastrophe has faded

The hypothesis made a testable prediction: if you find the Toba ash layer at an archaeological site, human activity should crash above it. When archaeologists found such sites, it didn’t.

Jwalapuram, India

Michael Petraglia’s team found stone tools directly below and above the Toba ash in southern India, made in similar ways on both sides. Whoever lived there came through the eruption, at least locally.

Pinnacle Point, South Africa

In 2018, Eugene Smith and colleagues identified microscopic Toba glass shards in sediments at Pinnacle Point 5-6 on the south coast of South Africa, 9,000 kilometres from the volcano. The human occupation not only continued through the eruption layer; it intensified.

Shinfa-Metema 1, Ethiopia

In 2024, John Kappelman’s team found Toba shards at a riverside site in northwest Ethiopia. People there seem to have adapted to drier conditions after the eruption by fishing in shrinking seasonal pools and following rivers — “blue highways” that may even have helped carry people out of Africa.

Lake Malawi

Sediment cores from Lake Malawi, which trap Toba ash, show no major cooling or vegetation collapse in East Africa after the eruption.

Toba was a genuine global event. It simply does not appear to have been an extinction-level one for our species.

The genetic side of the argument

Part of Toba’s original appeal came from a misunderstood number. Geneticists often estimate human effective population size at around 10,000. That does not mean only 10,000 people were alive. Effective size is a long-term average that reflects how much genetic variation a population keeps; a species spread across a continent in many small, loosely connected groups can have millions of individuals over time and still have a low effective size.

So low diversity is evidence of a smallish, structured ancestral population over a long time — not necessarily of one sudden near-extinction event.

The 900,000-year-old bottleneck

In 2023 Wangjie Hu, Haipeng Li and colleagues published a far more startling claim in Science. Using a new method called FitCoal, which reconstructs past population sizes from patterns of variation in modern genomes, they analysed 3,154 genomes from 50 populations. They concluded that our ancestors crashed from around 100,000 breeding individuals to about 1,280, starting roughly 930,000 years ago, and stayed at that level for some 117,000 years.

The timing is intriguing. It overlaps the Mid-Pleistocene Transition, when glacial cycles lengthened and intensified, and it coincides with a notable gap in the African and Eurasian hominin fossil record. The authors also suggested the squeeze might relate to the fusion of two ancestral chromosomes into human chromosome 2, and to the origin of the lineage that later split into Neanderthals, Denisovans and us.

Why many geneticists are unconvinced

Several independent teams have pushed back:

The claim has not been refuted, but it has not been confirmed either. The honest position is that it is a serious hypothesis with serious objections.

The bottlenecks we are sure of

Real, well-documented bottlenecks exist, just on a smaller scale. The small groups that left Africa roughly 60,000–50,000 years ago carried only part of Africa’s variation, which is why African populations remain the most genetically diverse on Earth. The first people into the Americas passed through a further founder bottleneck. And late Neanderthals had extremely low diversity, with long runs of identical DNA in some individuals — a sign of small, inbred groups on a path to extinction.

What it means

Our species may never have come within a whisker of vanishing in a single catastrophe. The more likely story is quieter: a population that was small, scattered and patchily connected for hundreds of thousands of years, surviving climate swings through flexibility rather than luck. That is less cinematic than a supervolcano — and arguably more impressive.

Follow how a small African population spread across the world on the migration map.

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Frequently asked questions

Did the Toba eruption nearly wipe out humans?

Probably not. Archaeological sites in India, South Africa and Ethiopia that contain Toba ash show human activity continuing, and sometimes increasing, after the eruption about 74,000 years ago.

What is a genetic bottleneck?

A bottleneck is a sharp reduction in population size that removes much of a species' genetic variation. The survivors' descendants carry only the diversity that passed through the squeeze.

Were humans reduced to 1,280 people?

A 2023 study using a method called FitCoal proposed that our ancestors fell to about 1,280 breeding individuals from roughly 930,000 to 813,000 years ago. Other methods do not detect this, and the result remains contested.

Why do humans have low genetic diversity?

Our ancestors had a relatively small long-term effective population size, and the groups that left Africa carried only a subset of African variation. Low diversity does not require a single near-extinction event.

How big was the Toba eruption?

It was the largest known eruption of the last two million years, ejecting roughly 2,800 cubic kilometres of material and spreading ash from India to southern Africa.

Sources & further reading
  1. Ambrose, S. H. (1998). 'Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans.' Journal of Human Evolution 34.
  2. Smith, E. I. et al. (2018). 'Humans thrived in South Africa through the Toba eruption about 74,000 years ago.' Nature 555. nature.com
  3. Kappelman, J. et al. (2024). 'Adaptive foraging behaviours in the Horn of Africa during Toba supereruption.' Nature 628. nature.com
  4. Hu, W. et al. (2023). 'Genomic inference of a severe human bottleneck during the Early to Middle Pleistocene transition.' Science 381. science.org
  5. Petraglia, M. et al. (2007). 'Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption.' Science 317.