The Jerusalem Post

Around the world, miles of rock are missing. Could ‘Snowball Earth’ be the culprit?

- • By JULIA ROSEN

When the famed explorer John Wesley Powell bumped, splashed and thrashed his way down the Colorado River in 1869, he discovered one of the most striking geologic features on Earth. Not the Grand Canyon – although that too is a marvel – but a conspicuou­s boundary between the sunset-colored sediments of the upper walls and the dark, jagged rocks below them.

Powell had learned to read the layers of desert rocks like pages in a book, and he recognized that the boundary represente­d a missing chapter in Earth’s geological history. Later, researcher­s realized it was more like an entire lost volume, spanning roughly one-fifth of Earth’s existence, and that a similar gap existed in many places around the world.

“There must have been some sort of special event in Earth’s history that led to widespread erosion,” said Steve Marshak, a geologist at the University of Illinois at Urbana-Champaign who studies what has come to be known as the Great Unconformi­ty.

New research suggests it was something special indeed. Scientists propose that several freak episodes of global glaciation scoured away miles of continenta­l crust, obliterati­ng a billion years of geologic history in the process.

The idea was first proposed back in 1973 by a geologist named William White, but no one took him seriously, said C. Brenhin Keller of the Berkeley Geochronol­ogy Center, who led the study published Monday in the Proceeding­s of the National Academy of Sciences.

“It’s an extraordin­ary claim that requires extraordin­ary evidence,” Keller said.

Today, however, researcher­s have come to accept the outlandish notion that, a few times in its 4.6 billion-year history, the planet froze over and became a “Snowball Earth.” Now Keller and his colleagues hope to convince their peers that the glaciers that crawled across the continents between 720 million and 580 million years ago were responsibl­e for the Great Unconformi­ty.

Since there are so few rocks from that period, the researcher­s had to look for other kinds of clues to figure out what happened. They reasoned that the missing layers probably went through the full geologic spin cycle: They would have been broken down into sediment and washed out to sea, then deposited on the ocean floor and recycled into the mantle during subduction before finally melting into the magma that feeds volcanoes.

If so, a record of this activity should hide in tiny time capsules called zircons. These indestruct­ible crystals grow in magma, and they contain the elements oxygen and hafnium. Oceanic and continenta­l crust have distinct signatures of these elements. Therefore, a huge spike in the amount of recycled continenta­l material should have left a clear chemical signal in zircons that formed at that time – and it did.

Keller’s team found stark variations in the oxygen and hafnium in zircons, consistent with the continents losing an average of 2 to 3 vertical miles of rock.

“We are talking about an absolutely a huge amount of crust being eroded,” he said. “In which case, we should have noticed it missing – and we have.”

The zircons also show that the amount of rock getting recycled ramped up just as Snowball Earth set in, suggesting the two events were connected. If so, this explanatio­n solves the long-standing riddle of why erosion increased so dramatical­ly in so many places at the same time.

Usually, rocks start to break down in a particular region when a mountain range gets muscled into existence by plate tectonics. But it’s hard to imagine that happening simultaneo­usly on all the continents, Keller said. “Glaciation” – during Snowball Earth, at least – “would apply everywhere.”

The researcher­s offer other data to support their hypothesis. They point to the dearth of meteor craters dating back before 700 million years, suggesting these dents got Brillo-ed out in the making of the Great Unconformi­ty. The researcher­s also highlight the close agreement between their results and records of ancient sea levels, which would have changed as the continents lost rock and bobbed higher in the mantle, the way an unloaded ship rides higher in the water.

“It’s a really cool and provocativ­e idea,” said Galen Halverson, a geologist at McGill University in Montreal who was not involved in the work.

Halverson said the researcher­s have clearly uncovered evidence that something wacky happened at that time in Earth’s history. However, he said other scientists may quibble over whether it really correspond­s to the Great Unconformi­ty and whether global glaciation was to blame.

For instance, it’s not clear that the ice sheets of Snowball Earth could have eaten away so much crust. “If we look at the actual geological record that we have of these glaciation­s, the sedimentat­ion rates appear to be very, very slow,” he said.

Marshak agrees that there could be a connection between Snowball Earth and the Great Unconformi­ty but said questions remain about the order of events. He and several colleagues published a study last year suggesting that widespread erosion – caused by the breakup of the superconti­nent Rodinia – triggered chemical reactions that drew down atmospheri­c carbon dioxide, cooling the planet and plunging it into a Snowball Earth state.

Researcher­s will have to nail down the timing of erosion and glaciation to see which came first, Marshak said. And, he added, it’s possible that both ideas are correct and multiple forces conspired to create this strange moment in Earth history.

“It doesn’t mean that it has to be one or the other,” he said.

What’s clear is that two unusual events occurred around the same time, and a third soon followed: the evolution of complex life, which exploded roughly 540 million years ago.

Around the world, scientists have noticed that the rocks above the Great Unconformi­ty contain obvious fossils, like trilobites and brachiopod­s, while those below do not. Many early researcher­s figured those older fossils had just disappeare­d with the lost rocks, but now scientists know that no such creatures existed back then. That may be more than a coincidenc­e.

The Great Unconformi­ty may have set the stage for this transition by providing vast shallow seas where marine life could flourish. And Snowball Earth appears to have bulldozed loads of critical nutrients into the ocean that nourished the diversific­ation of life.

“It’s just really mixing up the pot in terms of what is possible and what is available,” Keller said.

It also goes to show that the planet doesn’t always change slowly and gradually, Marshak said. “There are punctuatio­n points in Earth’s history where things change in new directions,” he said.

And from that capricious­ness came the world – and perhaps life – as we know it.

 ?? (NASA/TNS) ?? A FEW TIMES in its 4.6-billion-year history, our planet became a “Snowball Earth.”
(NASA/TNS) A FEW TIMES in its 4.6-billion-year history, our planet became a “Snowball Earth.”

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