Canadian Geographic

POLAR BLOG

A TINY SPECIES IN ANTARCTICA IS TEACHING SCIENTISTS ABOUT MONUMENTAL CHANGES

- BY JOHN BENNETT

Antarctic springtail secrets

IN THE SHADOW of the massive West Antarctic Ice Sheet, tiny creatures harbour clues to ancient environmen­tal changes at the southern end of the world — and to potential future changes around the planet. Ian Hogg, an ecologist with Polar Knowledge Canada who lives i n Cambridge Bay, Nunavut, works with a team of scientists from New Zealand and the United States to comb unexplored areas of Antarctica for informatio­n about present and past polar ecosystems. While his colleagues focus on the microscopi­c inhabitant­s of the thin Antarctic soil, such as nematodes (roundworms) and eight-legged tardigrade­s, Hogg studies the giants of this ecosystem: springtail­s. A dozen of these six-legged arthropods would fit comfortabl­y on your fingernail, but in the Lilliputia­n world of Antarctic land animals, says Hogg, “they’re the functional equivalent of elephants.” Elsewhere in the world (the snow fleas that appear on the late-winter snow in Canada are a variety of springtail), springtail­s can drift from place to place on river or ocean currents. But in Antarctica, says Hogg, they stay put: “There are areas with no open shorelines and very little in the way of running water, so many springtail population­s have been stuck right where they are for the last five million years.” “When we look at their genetics,” he explains, “we can see how long different springtail population­s have been separated from each other.” That provides the scientists with informatio­n about how long particular regions of Antarctica have been isolated and, as it is ice that separates the springtail­s, the behaviour of ice sheets. The team’s research supports geological evidence that the West Antarctic Ice Sheet — which is two kilometres thick and nearly the size of Nunavut — collapsed about five million years ago. This made it possible for some springtail population­s to mix, and their gene pools expanded. The ice sheet eventually returned, and within the last million years has collapsed and returned again, mixing and separating springtail population­s each time. Glaciologi­sts suggest that the ice sheet, which has been losing mass in recent decades because of the warming climate, may collapse again. This terrestria­l environmen­t grants ecologists a rare, uncluttere­d view of how an ecosystem operates. “Compared to the Arctic, with its higher biodiversi­ty and many varieties of animals large and small,” Hogg says, “the Antarctic systems are simple. That allows us to understand how they work and how they might respond to change in the future. Then we can take that informatio­n and apply it to more complex systems elsewhere on Earth.”

 ??  ?? DNA from springtail­s ( collected at soil-sampling sites ( near the West Antarctic Ice Sheet is helping scientists trace millions of years of environmen­tal change.
DNA from springtail­s ( collected at soil-sampling sites ( near the West Antarctic Ice Sheet is helping scientists trace millions of years of environmen­tal change.

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