Earth has a secret reservoir of water

PARIS, France — A hundred and fiffty years ago, in "Journey to the Centre of the Earth", French science- ction forerunner Jules Verne pictured a vast sea that lay deep under our planet's surface.

Today, that strange and haunting image has found an unexpected echo in a scienti c paper.

Writing in the journal Nature, scientists on Wednesday said they had found an elusive mineral pointing to the existence of a vast reservoir deep in Earth's mantle, 400-600 kilometres ( 250- 375 miles) beneath our feet.

It may hold as much water as all the planet's oceans combined, they believe.

The evidence comes from a water-loving mineral called ringwoodite that came from the so-called transition zone sandwiched between the upper and lower layers of Earth's mantle, they said.

Analysis shows that a whopping 1.5 percent of the rock comprises molecules of water.

The nd backs oncecontested theories that the transition zone, or at least signi cant parts of it, is water-rich, the investigators said.

" This sample really provides extremely strong confirmation that there are local wet spots deep in the Earth in this area," said Graham Pearson of Canada's University of Alberta, who led the research.

"That particular zone in the Earth, the transition zone, might have as much water as all the world's oceans put together."

Ringwoodite is named after Australian geologist Ted Ringwood, who theorised that a special mineral was bound to be created in the transition zone because of the ultra-high pressures and temperatures there.

A piece of this mineral has been a long- sought goal. It would resolve a long- running debate about whether the poorly-understood transition zone is bone-dry or water-rich.

But , until now , ringwoodite has only ever been found in meteorites. Geologists had simply been unable to delve deep enough to nd any sample on Earth. Worthless diamond

brings luck Good fortune, though, changed all this.

In 2008, amateur gem-hunters digging in shallow river gravel in the Juina area of Mato Grasso, Brazil, came across a tiny, grubby stone called a brown diamond.

Measuring just three millimetres ( 0.12 inches) across and commercially worthless, the stone was acquired by the scientists when they were on a quest for other minerals.

But the accidental acquisition turned out to be a bonanza.

In its interior, they found a microscopic trace of ringwoodite -- the very rst terrestrial evidence of the ultra-rare rock.

" It's so small, this inclusion, it's extremely difficult to nd, never mind work on," Pearson said in a press release, paying tribute to the diligent work of grad student John McNeill.

"It was a bit of a piece of luck, this discovery, as are many scienti c discoveries."

The team theorise that the brown diamond rocketed to the surface during a volcanic eruption, hitchhiking in a stream of kimberlite, the deepest of all volcanic rocks.

Years of analysis, using spectroscopy and X- ray diffraction, were needed in specialised labs to confirm the nd officially as ringwoodite.

Scientists have debated for decades about whether the transition zone has water, and if so, how much of the precious stuff there might be.

None, though, has embraced Verne's fancy of a subterranean sea with a rocky coastline dotted with forests of giant mushrooms and petriffied trees.