March to extinction?

March to extinction?

Penguin Ecosystem

March to extinction?

Cape Royds, home to the southernmost colony of penguins in the world, is a rocky promontory overlaid with dirty ice and the stench of pinkish guano. Beyond the croaking din of chicks pestering parents for regurgitated krill lies the Ross Sea, a southern extension of the Pacific Ocean that harbours over one-third of the world’s Adelie penguin population and a quarter of all emperor penguins, and which may be the last remaining intact marine ecosystem on earth.

The penguin colony is one of the longest-studied in the world. Data on its resident Adelie penguins was first acquired during the 1907-09 expedition of Ernest Shackleton, the eminent British explorer, whose wooden hut stands preserved nearby. “This is penguin nirvana,” David Ainley, an ecologist with the consulting firm H T Harvey and Associates who has been studying Ross Sea penguins for 40 years, said. Of the species that stand to be most affected by global warming, the most obvious are the ones that rely on ice to live. Adelie penguins are a bellwether of climate change, and at the northern fringe of Antarctica, in the Antarctic Peninsula, their colonies have collapsed as an intrusion of warmer seawater shortens the annual winter sea ice season.

Emperor colony now extinct

In the past three decades, the Adelie population on the peninsula, northeast of the Ross Sea, has fallen by almost 90 per cent. The peninsula’s only emperor colony is now extinct.

The mean winter air temperature of the Western Antarctic Peninsula, one of the most rapidly warming areas on the planet, has risen 10.8 degrees Fahrenheit in the past half-century, delivering more snowfall that buries the rocks the Adelie penguins return to each spring to nest – and favouring penguins that can survive without ice and breed later, like gentoos, whose numbers have surged by 14,000 per cent.

The warmer climate on the Antarctic Peninsula has also upended the food chain, killing off the phytoplankton that grow under ice floes and the krill, a staple of the penguin diet, that eat them, by as much as 80 per cent, according to a new study published this month in The Proceedings of the National Academy of Sciences. In the Ross Sea, a reverse trend is occurring: Winter sea ice cover is growing, and Adelie populations are actually thriving.

The Cape Royds colony grew more than 10 per cent every year, until 2001, when an iceberg roughly the size of Jamaica calved off the Ross Sea ice shelf and forced residents to move 70 kilometers north to find open water. (The iceberg broke up in 2006, and the colony of 1,400 breeding pairs is now recovering robustly.)

Good for some, bad overall...

Across Ross Island, the Adelie colony at Cape Crozier – one of the largest known, with an estimated 230,000 breeding pairs – has increased by 20 per cent.

Climate change has created a paradise for some pack ice penguin colonies and a purgatory for others, but the long-term fate of all Adelie and emperor penguins seems sealed, as relentless warming eventually pulls their rug of sea ice out from under them.

Scientists attribute the recent sea ice growth in the Ross Sea to the persistent ozone hole, a legacy of the human use of chlorofluorocarbons that cools the upper atmosphere over the continent, increasing the temperature difference with the lower atmosphere and equator, and over the last 30 years has delivered significantly brisker westerly winds in the summer and autumn. The warming of earth’s middle latitudes is having a similar effect, increasing that temperature difference and sending stronger winds that push sea ice off the coast and expose pockets of open water, called polynyas, that give nesting Adelie penguins easier access to food.

Researchers witnessed Ross Sea penguin colonies thrive during the 1970s when commercial whaling removed 20,000 Antarctic minke whales, also a food competitor of Adelies, from the penguins’ wintering area. Adelie populations eventually leveled off after 1986, after an international moratorium on whaling began (and remained static until the more recent influences of climate change). Japanese whaling of minkes resumed after the moratorium was instituted, purportedly for science, a claim that conservation groups dispute and that has incited a confrontation in the Ross Sea between the Japanese fleet and the Sea Shepherd Conservation Society, an antiwhaling vigilante group.

Tipping point in next 30-40 years?

Climate models predict that the winds and sea ice will continue to increase in the Ross Sea for the next 30 to 40 years, at which time the region is expected to experience a tipping point, as rising temperatures and the waning effect of the ozone hole, now getting smaller, transform the climate into the kind now seen in the Antarctic Peninsula.

Already, that process is underway. The average summer temperature at McMurdo Station, the American research base on Ross Island, has inched up 2.7 degrees Fahrenheit in the past 30 years, records show, more than the global average. Scientists conducting long-term studies of lakes in the McMurdo Dry Valleys, Antarctica’s largest ice-free area, report that after a decade of cooling, some lakes in the Taylor Valley are now gaining heat.

On Beaufort Island, north of Ross Island, glaciers have retreated over the rocky coastline farther than they have in 30,000 years, scientists estimate, a time before the last ice age. The receding ice has opened up more nesting habitat for the resident Adelie penguin colony, which has expanded to 55,000 breeding pairs from 40,000 in the last decade.

And as the ice melts...

As the sea ice retreats, researchers expect that Adelie penguins living in the Ross Sea will be forced to shift their range farther south toward the pole. In a study between 2003 and 2005, Ainley and colleagues from PRBO Conservation Science, Stanford University, NASA and the British Antarctic Survey used geolocation sensor tags to track penguins from Cape Royds and Cape Crozier to better understand their migration patterns.

Published last year in the journal Ecology, the study revealed how the penguins depart their nesting grounds in February, at the end of the austral summer, and head north on foot and ice floes to flee the protracted darkness of the Antarctic winter. They appear to stop on the sea ice about 300 miles from the boundary with open water, where they stay to forage and fatten before doubling back south to their island breeding sites ahead of the creeping northern night – an 8,000-mile journey.

By carbon-dating mummified penguin remains, researchers have been able to construct a long-term history of the Adelie in Antarctica, indicating that throughout the last ice age penguins changed their migration routes and colony locations in response to advances and retreats of the sea ice.

However, their range appears to have never extended farther south of where it is currently, for the simple reason that Adelie penguins appear to need light – if only twilight – to forage and navigate, and as comfort against predators. “Emperor and Adelie penguins have an obligatory association with sea ice,” Ainley said.

“As the sea ice goes, these species will go.” The Ross Sea is projected to be the last place on Earth where sea ice will endure. Ainley speculates that Adelie penguins face possible extinction not merely by a loss of habitat – but by an unshakable fear of darkness.