Did meteorite impacts help create life on Earth and beyond?

Gordon Osinski

Team of Western planetary scientists, led by Gordon Osinski, exploring melt rock at Haughton impact crater in Nunavut. These melt rocks provided key evidence for the existence of hydrothermal alteration, meaning habitats for life.

What if impact craters, long seen as harbingers of death, turned out to be the cradle of life?

For Western University planetary scientist Gordon Osinski, this isn’t just the big question posed in his latest study, but an overriding theme of his celebrated academic career.

The new study, published today in Astrobiology, posits that impact craters should absolutely be considered by space agencies like NASA and ESA as top exploration targets, not just for their invaluable post-impact geological records, but also – and perhaps more importantly – as prime locations for seeking potential habitats for extraterrestrial life.

Four Authors Ries Crater

The four authors of this new Astrobiology study — Charles Cockell, Haley Sapers, Alexandra Pontefract and Gordon Osinski — pictured at the Ries impact crater in Germany in 2010.

“There are a lot of hypotheses for where life started on Earth and where we should look for life on Mars, but we are actually overlooking a major geological force and a key habitat in understanding the origin of life and that’s meteorite impacts and their resulting craters,” said Osinski, Director of Western’s Institute for Earth and Space Exploration (Western Space).

Leading an international team with investigators from the University of Edinburgh, Georgetown University, and the University of Southern California, this new study is grounded in Osinski’s extensive field work and laboratory studies of meteorite impacts over the past two decades.

“If you ask anyone to imagine what happens when you have kilometre-size chunks of rock hitting the Earth, it’s typically destructive. It’s an extinction event like the one that killed the dinosaurs,” said Osinski. “What we’re trying to do here is turn that idea up on its head and say yes, the impact is initially destructive, but it also delivers the building blocks for life and creates new habitats for life. They [impact craters] essentially create an oasis for life.”

Osinski and collaborators propose that given the pervasive nature of impact events and their increased frequency during the first 500 million years of Solar System history that meteorite impact craters may represent the most likely sites where life originated on Earth. Unfortunately, says Osinski, we’ll never really know.

“I put my money on meteorite impacts as the place where life could have originated on Earth, but we’ll never know,” said Osinski, also Professor in Western’s Department of Earth Sciences. “Unfortunately, due to billions of years of erosion, plate tectonics, and volcanism, we’ve lost the vast majority of the ancient rock record on Earth. So we’re never going to know exactly where or even when, to be honest, life originated on Earth.”

But maybe it’s not too late for the Red Planet.

By exploring Mars with rovers like Perseverance and ExoMars, Osinski believes planetary scientists might eventually figure out the origin of life – and they just might – as long as they are looking in the right place.

“There are other impact craters on Mars that may have been better to explore with these ideas in mind,” said Osinski. “But Perseverance is going to land in Jezero Crater and there is evidence of minerals such as clays formed through hydrothermal activity. It’s a good place to start to explore the role of meteorite impacts in the origin of life, as long as they look out for the habitats, nutrients, and building blocks for life that we outlined in our study.”

To date, 200 impact craters have been investigated and confirmed on Earth using fieldwork, geophysics, satellite data, and various laboratory analysis techniques in pioneering laboratories at Western and others around the world.

Osinski and his team have collected and posted relevant data for all 200 craters as part of Western’s Impact Earth initiative.

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Images

Impact Melt Rock Haughton
Team of Western planetary scientists, led by Gordon Osinski, exploring melt rock at Haughton impact crater in Nunavut. These melt rocks provided key evidence for the existence of hydrothermal alteration, meaning habitats for life.
Haughton Camp
Panoramic view of camp at Haughton impact crater in Nunavut taken at midnight.
Four Authors Ries Crater
The four authors of this new Astrobiology study -- Charles Cockell, Haley Sapers, Alexandra Pontefract and Gordon Osinski -- pictured at the Ries impact crater in Germany in 2010.