National Post

A MOUNTAIN OF TROUBLE ... SORT OF

GIANT SPACE ROCK MADE EARTH’S OCEAN BOIL AND SENT UP HUGE WAVE BUT ALSO HELPED EARLY LIFE

- JOEL ACHENBACH

EARLY IMPACTS COULD HAVE BEEN POSITIVE FOR EARLY LIFE IN A NUMBER OF DIFFERENT WAYS. THEY COULD HAVE DELIVERED, FOR INSTANCE, KEY ELEMENTS OR MOLECULES THAT WERE MISSING IN THE NEAR-SURFACE THAT PERHAPS COULD HAVE BEEN IMPORTANT FOR EARLY LIFE. — SIMONE MARCHI

The young Earth got beat up a lot, including one day 3.26 billion years ago when a rock four times the size of Mount Everest slammed into the planet. Scientists believe that the rock, which was much bigger than the Chicxulub object that ended the reign of the dinosaurs, probably landed in the ocean, since Earth had barely begun to form continents.

The collision was so violent it boiled off the top layer of that ocean and, near the impact site, created a tsunami as high as a New York skyscraper. Molten rock rained from the sky. The atmosphere was choked with ash and dust. The planet descended into darkness.

That was the counterint­uitive implicatio­n of three presentati­ons at the American Geophysica­l Union’s fall meeting in San Francisco last month. The scientists, working independen­tly, found that the bludgeonin­g of young Earth by giant space rocks may have primed the planet to be more congenial to life.

Calamity is followed by opportunit­y: There is a lesson here for everyone, written in the geophysica­l record. Earth has been through hell and back — smashed, melted, frozen, depending on which eon or epoch is under discussion.

But the first couple billion years of Earth’s history remain hazy. No one knows how, amid the chaos and tumult of that time, life emerged and evolved into more complex organisms.

The story of how this planet became habitable is relevant to the young science of astrobiolo­gy, which probes the hypothetic­al existence of life on other worlds. Our own solar system has abundant examples of planets and moons that are inhospitab­le. Earth is an anomaly, riotous with living things. What happened to make it so?

As researcher­s probe the distant past, giant impacts loom large.

“These giant impacts certainly have a negative effect on the atmosphere. If you put a lot of dust in the atmosphere, it gets very dark, and you’re boiling off a lot of the ocean,” Nadja Drabon, an early-earth geologist at Harvard who presented her research at the AGU meeting, said in an interview.

“At the same time, these negative effects probably didn’t last very long,” she said.

And in their wake, conditions for supporting life improved, at least for some period of time.

For example, the tremendous tsunami that was probably created by the impact 3.26 billion years ago would have mixed up the water column in the global ocean and brought more iron, a key nutrient for metabolism, to shallow seas. Other nutrients would have eroded into the ocean from land masses, according to Drabon.

Nick Wogan, a scientist at NASA Ames Research Center who presented at AGU, described how early impacts would have given Earth a “hot steam atmosphere” but also might have triggered life-relevant chemistry.

“Early impacts could have been positive for early life in a number of different ways,” said Simone Marchi, a planetary scientist at the Southwest Research Institute in Boulder, Colo., who also presented at the AGU meeting.

“They could have delivered, for instance, key elements or molecules that were missing in the near-surface that perhaps could have been important for early life.”

Young Earth is a mystery because it left little record of itself, and scientists must conjure it with scraps of evidence and clever computer models.

It was a water world, the models suggest. Life was scarce and primitive, and nothing remotely resembling an animal had come into being. Scientists investigat­ing the chemistry of the early atmosphere aren’t sure if the sky was blue or orange.

“Probably there was some orange haze, maybe like Los Angeles in the 1980s,” said John Tarduno, a geophysici­st at the University of Rochester.

“You can think of the early Earth as an alien planet,” Marchi said.

It was also a planet under assault from pretty much the day it was born. Early Earth endured a steady bombardmen­t for hundreds of millions of years, including a collision with a Mars-size object that led to the formation of the moon.

Those impacts are key to the planet’s biography. They helped form Earth itself, adding mass. The battering gradually eased as the clutter was cleaned out, but the planet remained vulnerable to globally catastroph­ic impacts.

Scientists have given the event 3.26 billion years ago the parsimonio­us name of “S2.” It was among the biggest of the 16 major impacts from 3.5 billion to 2.4 billion years ago that have been identified by scientists, Marchi said.

These events left behind no craters. But crafty scientists can find their signatures in thin layers of sedimentar­y rock. The “S” of S2 stands for spherules, tiny glassy droplets that rained from the sky after the impact.

The spherules and other debris from the impact form a distinct layer in sedimentar­y rocks that, like a detective’s chalk outline, carry the narrative of a murderous moment.

There wasn’t much to be slain in those early eons, however. The Great Leap Forward came with the evolution of bacteria that pumped oxygen into the atmosphere. Later came organisms that leveraged that oxygen as metabolic fuel. Only in the past billion years did life become multicellu­lar, and the first things that could creep across the sea floor — the first creatures we could call animals — appeared less than 600 million years ago.

Would life on Earth and its endless forms most beautiful have happened without early impacts? No one can say. When they happened there were no people around, or dinosaurs, or even jellyfish — just bacteria.

But microbes were potentiall­y well-positioned to benefit from catastroph­e. They are remarkably hardy, capable of surviving under extreme conditions, such as in the hydrotherm­al pools of Yellowston­e or around hot vents at the bottom of the sea.

“Back then, life was basically very, very simple organisms. So perhaps that’s why they managed to survive,” Marchi said. “If we had evolved life like you and I back then, we’d probably have been extinct.”

 ?? PHOTOS: SWRI / SIMONE MARCHI. ?? An illustrati­on shows how early Earth might have looked under bombardmen­t from space, with circular impact features dotting
the daylight side while hot lava glows on the night side, all under a thick, yellowish, hazy atmosphere.
PHOTOS: SWRI / SIMONE MARCHI. An illustrati­on shows how early Earth might have looked under bombardmen­t from space, with circular impact features dotting the daylight side while hot lava glows on the night side, all under a thick, yellowish, hazy atmosphere.
 ?? ?? Impact-generated lava lakes sizzled under a thick greenhouse atmosphere during the Hadean eon, when Earth
first formed roughly 4.5 billion years ago. The first multicellu­lar life would not appear for billions of years.
Impact-generated lava lakes sizzled under a thick greenhouse atmosphere during the Hadean eon, when Earth first formed roughly 4.5 billion years ago. The first multicellu­lar life would not appear for billions of years.

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