UC Berkeley News


Humans and climate change: A one-two punch
A revised view of the Pleistocene extinction, which wiped out numerous ‘megafauna’ species, implicates homo sapiens and warming temperatures together

| 30 September 2004

The extinction of the giant Irish elk about 10,600 years ago appears due solely to a sudden cold snap that diminished the nutritious vegetation they needed to thrive. (Brendon Dempsey photo, courtesy Anthony Barnosky)

A Berkeley paleobiologist and his colleagues warn that Earth’s mammals could face a future as dire as their predecessors confronted 50,000 and 10,000 years ago, when a combination of climate change and human pressure resulted in the extinction of two-thirds of all large mammals on the planet.

Anthony D. Barnosky and his colleagues reached this conclusion after review of studies of the great megafauna extinctions that occurred in the late Pleistocene, when animals such as mammoths and mastodons, the saber-toothed cat, ground sloths, and native American horses and camels went extinct.

“There’s been a lot of talk about people causing the extinction of the megafauna by killing everything they saw, like a blitzkrieg,” said Barnosky. “But if you look at all the evidence, it’s clear that, while humans had a major role in these extinctions, in many cases climate change was a key part of the recipe.

“Humans and climate change were the one-two punch that drove extinction between 50,000 and 10,000 years ago — and the same thing is happening in a major way today.”

Because the global climate is changing more rapidly today than it did even in the late Pleistocene, serious consequences for many large animal species that weathered the Pleistocene extinction could be just down the road, Barnosky said. And the impact could be even greater today because of impoverished large-animal populations and appropriation of their habitat by surging populations of humans.

“Human activities today, combined with climate change, probably are going to result in inevitable extinction of many more species and unpredictable ecosystem changes,” he said.

These warnings, published in the Oct. 1 issue of Science, are based on a review of previous studies of Pleistocene animal extinctions around the world, from Australia to Europe and North America. The Pleistocene, a period starting about 1.8 million years ago, was a time of glacial comings and goings, with more than 20 cycles of cooling and warming that concluded only about 10,000 years ago, with the end of the last ice age.

In previous studies of animal remains layered in caves in the American west, Barnosky has found that during some of the last few glacial/interglacial cycles (between one million and 600,000 years ago), the number of small, medium, and large mammals in a given community remained fairly stable, though different species may have filled the various ecosystem niches. In the late Pleistocene, however, something happened to make the number of large mammals nosedive continent-wide.

The new analysis of archeological, climatic, ecological, and simulation studies shows that this happened around the world. Of more than 150 genera of megafauna — that is, animals weighing greater than 44 kilograms (97 pounds) — living on Earth 50,000 years ago, at least 97 were extinct by 10,000 years ago. If you look at localized instead of global extinctions, 121 genera disappeared from at least one continent.

Were humans the sole cause of this extinction? Barnosky and his colleagues found little evidence outside Australia for that contention, even though, at the time of large-scale extinction on that continent 40,000 to 50,000 years ago, little climate change was going on, and humans were certainly on the scene. Yet some scientists think that fires set by humans had as much to do with extinction as direct hunting. Over a few thousand years, an extended “sitzkrieg” (a phrase describing human-caused extinction by means of habitat alternation) may have led to the extinction of large mammals such as kangaroos, wombats, the marsupial lion (Thylacoleo carnifex), and the largest-ever marsupial, the 2-1/2-ton Diprotodon.

Elsewhere, human activities combined to a greater or lesser degree with climate change to lead to extinctions. In Europe and parts of Asia, mammals such as the giant Irish deer or Irish elk died out broadly toward the end of the late Pliestocene, in some areas before humans were present. Earlier, though, warm-adapted megafauna such as straight-tusked elephants (Palaeoloxodon) and hippos, which were abundant during preceding interglacials, disappeared with the coming of the last ice age, starting around 45,000 years ago and persisting up to the height of the glacial period 20,000 years ago.

“This is a very clear case of climate-caused extinction without the significant input of humans,” Barnosky said.

Similarly, in Alaska and the Yukon, the disappearances of short-faced bears (such as the grizzly-like Arctodus simus, the largest land carnivore ever to inhabit North America), mammoths, and two horse species occurred before apparent sign of human contact.

However, a second pulse of climate-caused extinctions began in Europe and Asia about 12,000 years ago as cold-adapted animals — the wooly rhino and the mammoth — died out with warming temperatures. It’s possible, Barnosky said, that the rise of Homo sapiens sapiens, with a broad variety of tools and a diverse diet, negatively impacted these animals to an extent not seen in Europe with earlier human species, such as Homo erectus and Neanderthals.

North America, in particular, is an example of humans speeding the process of climate-caused extinction, in many cases by overkill. Evidence of mammoth kills date from near the first appearance of stone spearheads made by the human Clovis civilization 11,400 years ago. Only mammoths and mastodons have been found with incontrovertible evidence that they were killed by humans in North America, though human artifacts have been found in association with extinct megafauna fossils on all continents, including Africa.

Over a period of at most 1,500 years following the appearance of Clovis-style hunters, camels and horses, rhinos and peccaries, short-faced bears and saber-toothed tigers, as well as the armadillo-like glyptodonts and the giant ground sloths (Megatheriadae), all disappeared from the North American continent.

“Humans and climate change came together at exactly the same time” to lead to these great megafauna extinctions, said Barnosky, who also sees lessons for the future in these large-mammal dieoffs.

“Humans tend to impact the bigger animals, with the smaller animals as collateral damage,” he said. “Climate change is just the opposite — it affects the little guys first and then, through them, the big guys. Today we see humans taking out the bigger animals and climate change affecting the smaller animals, so we can expect to see some pretty dramatic changes in the ecosystem.”

One major problem today is that, because of human encroachment, there are no refuges for animals that might want to relocate because of climate change.

“One thing we can do, as conservationists, is to create and connect natural areas” to allow animals to move around, Barnosky added. “Because species can no longer do this by themselves, maybe the solution is to do it for them.”