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Starts With A Bang

Starts With A Bang podcast #118 – Snowball Earth

The hunt for extraterrestrial life begins with planets like Earth. But our inhabited Earth once looked very different than Earth does today.
A grey, icy planet or moon with surface cracks is shown against a backdrop of stars and the Milky Way galaxy.
This illustration shows a frozen-over planet, but one that still possesses a significant liquid ocean beneath the surface ice. Many worlds in our Solar System may be described by this scenario at various points in cosmic history, including even planet Earth more than two billion years ago.
Credit: Pablo Carlos Budassi/Wikimedia Commons
Key Takeaways
  • When we look for life out there in the Universe beyond our own Solar System, it makes sense to go after the low-hanging fruit: planets similar to Earth in many ways.
  • Even though planet Earth has been known to harbor life for most of it’s history, more than 3 billion years for certain and possibly even more than 4 billion, Earth looked very different long ago.
  • One of those phases, critical to the development of modern biodiversity, was a stage called Snowball Earth, lasting hundreds of millions of years. Here’s why that matters for us.
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When we search for life in the Universe, it makes sense to look for planets that are similar to Earth. To most of us, those signatures would look the same as the ones we’d see if we viewed our planet today: blue oceans, green-and-brown continents, polar icecaps, wispy white clouds, an atmosphere dominated by nitrogen and oxygen, and even the modern signs of human activity, such as increasing greenhouse gas emissions, planet modification, and electromagnetic signatures that belie our presence.

But for most of our planet’s history, Earth was just as “inhabited” as it is today, even though it looked very different. One fascinating period in Earth’s history that lasted approximately 300 million years resulted in a planet that looked extremely different from modern Earth: a Snowball Earth period, where the entire surface, from the poles to the equator, was completely covered in snow and ice. This isn’t just speculation, but is backed up by a remarkable, large suite of observational and geological evidence.

So what was Earth like during this period? How did it fall into this phase, how did it remain trapped in that state for so long, and how did it finally thaw again? To help explore this topic, I’m so pleased to welcome PhD candidate Alia Wofford to the program, who conducts intricate climate models of early Earth to try to reproduce those early conditions. From that work, we’re learning about what we should be looking for when it comes to potentially inhabited exoplanets, because Earth has been inhabited for around 4 billion years, and wow, has its appearance changed over all that time. Have a listen and see for yourself!

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Travel the universe with Dr. Ethan Siegel as he answers the biggest questions of all.

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