BBC Science Focus

Slowing down climate change

- WORDS: DR HELEN PILCHER IMAGES: CHRIS LINDER, GRANT SLATER

Two men and a bunch of bison could help save our planet from climate change.

THE PERMAFROST IS DISAPPEARI­NG. AS IT THAWS, BILLIONS OF TONNES OF LONG-BURIED CARBON COULD ESCAPE INTO OUR ATMOSPHERE WITH CATACLYSMI­C CONSEQUENC­ES. BUT ONE MAN, HIS SON AND A BUNCH OF BISON HAVE A PLAN TO RESTORE THE ICE AGE ECOSYSTEM

“WE ARE RAPIDLY APPROACHIN­G THE POINT WHERE THE ARCTIC PERMAFROST WILL START THAWING. THAT WILL BE CATASTROPH­IC”

It sounds like the plot from a Hollywood blockbuste­r. Eight time zones east of Moscow, in a remote corner of Siberia accessible only by boat, two men are trying to save the world from calamitous global warming. One, Sergey Zimov, is a pony-tailed man with a ZZ Top beard and penchant for concocting grand theories and smoking roll-ups; the other is his long-suffering son, Nikita. Their plan is to create an Ice Age nature reserve full of Ice Age creatures that will act as climate change superheroe­s. Their only superpower is digestion. In a nod to the Stephen Spielberg classic, the Zimovs have decided to call their venture Pleistocen­e Park. Meanwhile, 9,000km away in a Harvard University laboratory, a bunch of scientists are working to bring back what could become the park’s star attraction – the ultimate Ice Age icon, the woolly mammoth. But time is running out and the odds are stacked against them. Can the intrepid scientists succeed before the frozen north melts?

ON THIN ICE

Scientists estimate that 1,400 billion tonnes of organic carbon lies locked up in the permafrost, the frozen subsurface layer of soil, ice and rock that covers around one-quarter of northern hemisphere land. That’s roughly twice as much carbon as exists in our atmosphere, and three times the amount found in all the world’s forests combined. Now, as our planet warms and the permafrost melts, microbes are starting to convert this organic carbon into methane and carbon dioxide. The concern is that as these greenhouse gases bleed into the atmosphere, they will accelerate the rate of global warming, leading to more melting and microbial activity. “We are rapidly approachin­g the point where the Arctic permafrost will start thawing everywhere,” says Nikita, who now manages Pleistocen­e Park. “That will be catastroph­ic but we hope that Pleistocen­e Park will make a difference.”

The Pleistocen­e is the moniker given to the last Ice Age, an interminab­le cold spell that began around 2.5 million years ago. It was a time when immense ice sheets waxed and waned over much of the northern hemisphere, locking up so much water they created cloudless blue skies. Beneath those skies were lush, open grasslands that covered much of Eurasia and North America; the so-called mammoth steppes. When Homo sapiens first set eyes on this vista, tens of thousands of years ago, it was a vibrant and biodiverse place. Immense herds of mammoth, bison, reindeer and horses roamed the plains, amidst watchful cave lions and wolves. “It was like an Arctic Serengeti,” says Nikita. “Modern humans didn’t need to worry about finding food; they needed to worry about being trampled.”

When the Pleistocen­e came to an end around 11,500 years ago, it all disappeare­d. Many of the biggest animals, including mammoths, woolly rhinos and cave lions went the way of the dodo, and the grasslands were replaced with an unkempt ragbag of scruffy tundra and scrawny saplings. Now the remains of that Ice Age ecosystem lie trapped in the permafrost.

Thirty years ago, most scientists thought this transition was driven by climate change. As the Ice Age drew to a close, warming caused the pastures and animals to die. Then Sergey put forward a new theory, which he outlined in a Soviet journal in 1988.

PARK LIFE

It’s well known that animals provide ecological services to the environmen­t in which they live. According to

Sergey, during the Pleistocen­e, big herbivores would have kept weeds and forests at bay, and returned nutrients to the ground via their droppings. In summer, they helped send the Sun’s warming radiation away from the planet by maintainin­g grassland, which is more reflective than closed woodland. In winter, the herbivores broke up the snow and helped keep the ground frozen by exposing it to the bitter Arctic air. If the big grazers could be returned, he mused, they should be able to convert the mossy tundra back to productive grassland and help keep the permafrost frozen.

In 1996, he set up Pleistocen­e Park to test his ideas. The reserve, which lies close to the Kolyma River in the Sakha Republic, northeaste­rn Siberia, incorporat­es 2,000 hectares of this barren tundra. With no funding, in the early days the project ran on fumes and enthusiasm. First, he acquired some stocky, semi-domesticat­ed horses from Siberian natives who used them for meat. He fed the horses with porridge oats, but without any fences, the ungrateful animals just wandered off.

Fast-forward to the present day, and the father and son team have added more than 25km of fences, 30 sheep, 30 reindeer, 9 yak, a few musk ox, some bison

“IT WAS LIKE AN ARCTIC SERENGETI. MODERN HUMANS DIDN’T NEED TO WORRY ABOUT FOOD; THEY NEEDED TO WORRY ABOUT BEING TRAMPLED”

and a couple of dozen horses, all species that lived in Siberia during Pleistocen­e times. Shrubs that were once so tall they overshadow­ed people have now been grazed to waist height or less. Tussock, a common, slow-growing weed, is giving way to meadow grass. Slowly but surely, the mammoth steppe ecosystem is beginning to return. “It’s the start of a long process,” says Nikita, “but there are encouragin­g signs.”

The ability of animals to re-sculpt landscapes is well known. There are many examples where keystone

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 ??  ?? ABOVE: Ancient bones collected from an eroding riverbank by Sergey and Nikita Zimov and students over the course of just one dayBELOW: This river, with its many side-channels, oxbows and meanders, is very representa­tive of northern Siberia
ABOVE: Ancient bones collected from an eroding riverbank by Sergey and Nikita Zimov and students over the course of just one dayBELOW: This river, with its many side-channels, oxbows and meanders, is very representa­tive of northern Siberia
 ??  ?? BELOW RIGHT: Beneath the ‘active layer’ of soil (only a metre or so deep), the ground is ice-filled soil called permafrost. This cave, which was hand-carved from the permafrost by the Zimovs and their workers, is located in Pleistocen­e Park and is used as a natural freezer to store fish
BELOW RIGHT: Beneath the ‘active layer’ of soil (only a metre or so deep), the ground is ice-filled soil called permafrost. This cave, which was hand-carved from the permafrost by the Zimovs and their workers, is located in Pleistocen­e Park and is used as a natural freezer to store fish
 ??  ?? RIGHT: The Zimovs have a herd of Yakutian horses at Pleistocen­e Park. The animals are native to Siberia and grow long coats in the winter
RIGHT: The Zimovs have a herd of Yakutian horses at Pleistocen­e Park. The animals are native to Siberia and grow long coats in the winter
 ??  ?? ABOVE: The Siberian environmen­t near Pleistocen­e Park
ABOVE: The Siberian environmen­t near Pleistocen­e Park
 ??  ?? Permafrost is made of frozen soil, rock, water and organic matter, including animal bones and plant roots from the Ice Age.As the permafrost melts, the roots of grasses that grew in the Ice Age are being devoured by hungry microbes. If oxygen is present, carbon-based sugars locked inside the roots are broken down to form carbon dioxide, but if the soils lack oxygen then methane is made. Both methane and carbon dioxide are greenhouse gases with the potential to accelerate global warming. How grasslands and grazers can help keep the permafrost frozen….In the winter, grazers trample through the snow exposing the earth to bitterly cold Arctic air. This helps keep the ground frozen and carbon locked away.In the summer, grazers promote the formation of lush, biodiverse grasslands by eating weeds, dispersing seeds and fertilisin­g the ground. They help keep forests at bay by knocking down trees and eating their bark. These grasslands reflect more sunlight than forest and scrub, causing the Arctic to absorb less heat.
Permafrost is made of frozen soil, rock, water and organic matter, including animal bones and plant roots from the Ice Age.As the permafrost melts, the roots of grasses that grew in the Ice Age are being devoured by hungry microbes. If oxygen is present, carbon-based sugars locked inside the roots are broken down to form carbon dioxide, but if the soils lack oxygen then methane is made. Both methane and carbon dioxide are greenhouse gases with the potential to accelerate global warming. How grasslands and grazers can help keep the permafrost frozen….In the winter, grazers trample through the snow exposing the earth to bitterly cold Arctic air. This helps keep the ground frozen and carbon locked away.In the summer, grazers promote the formation of lush, biodiverse grasslands by eating weeds, dispersing seeds and fertilisin­g the ground. They help keep forests at bay by knocking down trees and eating their bark. These grasslands reflect more sunlight than forest and scrub, causing the Arctic to absorb less heat.

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