Related Story: Rising Ocean Acidity May Deplete Vital Phytoplankton
Despite their tiny size, plant plankton found in the world's oceans are crucial to much of life on Earth. They are the foundation of the bountiful marine food web, produce half the world's oxygen and suck up harmful carbon dioxide.
They also are declining sharply.
Worldwide phytoplankton levels are down 40 percent since the 1950s, according to a study published Wednesday in the journal Nature. The probable cause is global warming, which makes it hard for the plant plankton to get vital nutrients, researchers say.
The numbers are both staggering and disturbing, say the Canadian scientists who did the study and a top U.S. government scientist.
"It's concerning because phytoplankton is the basic currency for everything going on in the ocean," said Dalhousie University biology professor Boris Worm, a study co-author. "It's almost like a recession ... that has been going on for decades."
Half a million datapoints dating to 1899 show that plant plankton levels in almost all the world's oceans started to drop in the 1950s. The biggest changes are in the Arctic, southern and equatorial Atlantic and equatorial Pacific oceans. Only the Indian Ocean is not showing a decline. The study's authors said it is too early to say that plant plankton is on the verge of vanishing.
Virginia Burkett, the chief climate change scientist for the U.S. Geological Survey, said plankton numbers are worrisome and show problems that cannot be seen just by watching bigger more charismatic species like dolphins or whales.
"These tiny species are indicating that large-scale changes in the ocean are affecting the primary productivity of the planet," said Burkett, who was not involved in the study.
When plant plankton plummet, as they do during El Nino climate cycles, sea birds and marine mammals starve and die in huge numbers, experts said.
"Phytoplankton ultimately affects all of us in our daily lives," said lead author Daniel Boyce, also of Dalhousie University in Halifax, Nova Scotia. "Much of the oxygen in our atmosphere today was produced by phytoplankton or phytoplankton precursors over the past 2 billion years."