Sept. 20, 2026
Solar Superflares and Gondwana's Legacy: Unpacking Earth's Cosmic Changes
SpaceTime Series 29 Episode 113 New evidence of superflares on the Sun A new study has found that a giant sunspot observed back in 1947 had the potential to trigger a massive solar super flare. How Gondwana changes life on Planet Earth A new study has rewritten the evolution of one of planet Earth’s greatest ancient land masses, the super continent of Gondwana. The incredibly shrinking planet Mercury A new study suggests that the planet Mercury may have shrunk by as much as 30 percent since its creation. The Science Report Studies warn that a third of the world’s population are exposed to second hand smoke. New figures show deradicalization programs have failed. A new study has found that 2025 was one of the driest years in the past three decades. It was in this month in 1936, that the world’s the last known Tasmanian Tiger died at the Hobart Zoo. Skeptics guide to the Nazi’s hollow Earth conspiracy. Our Guest This Week Professor Bill Collins from Curtin University Our regular guests: Alex Zaharov-Reutt from techadvice.life Tim Mendham from Australian Skeptics 🌏 Get Our Exclusive NordVPN deal here ➼ www.bitesz.com/nordvpn . The discounts and bonuses are incredible! And it’s risk-free with Nord’s 30-day money-back guarantee! ✌ If you’d like to support the podcast and gain access to bonus content by becoming a SpaceTime crew member, you can do just that through The Big Bang editions on Patreon, Spotify and Apple Podcasts. Details on the Support page on our website https://www.bitesz.com/show/spacetime/support/ For more SpaceTime and show links: https://linktr.ee/biteszHQ If you love this podcast, please get someone else to listen too. Thank you…
The Astronomy, Space, Technology & Science News Podcast.
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This is Space Time, Series 29, Episode 113, for broadcast
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on the 21st of September, 2026. Coming up on Space Time,
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new evidence of super flares on the Sun, how Gondwana
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changed life on planet Earth, and the incredibly shrinking planet Mercury.
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All that and more coming up on Space Time.
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Welcome to Space Time with Stuart Garry.
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A new study has found that a giant sunspot observed
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back in 1947 had the potential to trigger a massive
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solar superflare. Now, we all know the sun's capable of
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some massive eruptions. Solar flares and chronal mass ejections repeatedly
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hurl billions of tons of particles and radiation into space.
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This solar bombardment can be dangerous for life here on Earth.
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It can destroy technical infrastructure, damage satellites, disrupt navigation and
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communication systems, cause massive power blackouts over wide areas, and
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subject astronauts in space and even people in high-flying aircraft
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to high doses of radiation. The Sun offered its most
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impressive demonstration of its strength back in 1859. The solar
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storm which struck Earth during the Sircord Carrington event was
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so strong, the auroral lights, normally confined to higher latitudes,
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were clearly visible in the tropics. There wasn't much in
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the way of electrical circuits at the time, but there
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were telegraphs, many of which were short-circuited, and the operators
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working them electrocuted. Now, as we reported in last week's show,
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there have been hints of far bigger events through history,
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recorded through ancient tree rings. but as far as we know,
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nothing for hundreds of years. But now a new look
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at a massive sunspot recorded back in 1947 has raised
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some interesting questions. And the biggest is could this event
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have triggered a super flare, an event so violent it
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would have had more energy than trillions of hydrogen bombs?
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Now so far such powerful blasts have only ever been
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observed directly on distant stars, never on our own sun.
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But now astronomers from the Max Planck Institute and the
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University of Colorado have been exploring this observation in a
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detailed study reported in the journal Philosophical Transactions of the
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Royal Society A. The amount of energy the Sun releases
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during your average solar flare can be measured directly only
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outside the Earth's atmosphere, using high-flying balloons or spacecraft. But
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both have really only been possible from the beginning of
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the space age about 70 years ago. And in those
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3 score and 10 years there's been no super flare action.
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The study's lead author Natalie Krivova from the Planck Institute
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says there's some evidence to suggest that the Sun too
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can produce super flares. And these clues can be found
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by looking at other sun-like stars. In late 2024, Krivova
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and colleagues were able to show that super flares occur
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roughly once a century on stars that resemble our Sun
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in key characteristics, such as similar metallicity, luminosity and mass.
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So the authors analysed data collected by NASA's Solid Dynamics
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Observatory spacecraft between 2010 and 2016. They correlated the amount
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of energy released by the 300 strongest solar flares during
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this period and compared that with the size of the
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corresponding active region the flares came from on the Sun's
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visible surface. Active regions are areas on the Sun's surface
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where the magnetic field is especially strong and complex in structure.
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They're associated with sunspots, dark areas on the Sun's visible
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surface that are cooler than the rest of the surface
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and are considered the potential starting points for solar eruptions.
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Graverbus says while no superflares occur during the observation period,
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the statistical relationship found between the release of energy and
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the size of an active region should also hold true
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for more powerful events. And that's when they turn their
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attention to the largest sunspots ever seen on the Sun. Now,
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sunspots have been systematically and regularly recorded on the surface
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of the Sun over the past 400 years. And they
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offer astronomers a way to look back through the Sun's history.
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So using their new comparison chart, based on the size
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of the sunspot, the authors were able to infer the
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size of the associated active region, and thus the strength
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of a possible eruption. And that's where the massive sunspot
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of April 1947 comes in. It covered some 0.6% of
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the visible solar disk, or to put that another way,
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its diameter was about 40 times that of the Earth's. Now,
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there was no super flare at the time, but the
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study shows that a sunspot of this size could have
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triggered a super flare. Provova says it shows the Sun
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has super flare potential. She says it can produce massive
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sunspots that, in principle, can serve as the starting point
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for some of the most extreme bursts of radiation. Has
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such a super flare ever actually occurred on the Sun? Well,
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for now at least, that remains one of our local
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star's mysteries. This is Space Time. Still to come, how
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God wanted to change life on planet Earth, and the
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incredibly shrinking planet Mercury. All that and more still to
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come on Space Time. A new study has rewritten the
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evolution of one of planet Earth's greatest ancient landmasses, the
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supercontinent Gondwana. The new research, led by Bill Collins from
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Curtin University, shows Gondwana was far larger than previously recognized.
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Using geochemical isotope comparisons that allow scientists to identify the
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age and origins of rocks deep beneath the planet's surface,
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Collins and colleagues identified vast regions stretching through Asia that
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were once part of this larger, greater Gondwana. Collins says
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the new work's reshaping cites his understanding of one of
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Earth's most important ancient landmasses. He says the findings could
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also help explain the dramatic environmental changes which paved the
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way for complex life to develop on Earth. You see,
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Gondwana's formation triggered profound global changes, including shifts in climate,
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in atmospheric chemistry, and in geological processes that ultimately helped
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create the conditions for what we call the Cambrian Explosion
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of Life. And that changed everything.
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The Earth is divided up into these tectonic plates, sort
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of rigid blocks and crusts. And there's maybe just over
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half a dozen of those plates. And the reason why
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they move around the Earth, and because of them we
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have earthquakes and volcanoes, which everyone knows about. But the
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reason why they move around is because the mantle underneath
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and the plates are these They're about 30 to 100
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kilometres thick, depending on where you are. And they sit
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on a mantle which flows very, very slowly, but it
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flows nonetheless. So fake tectonics really is a response to
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convection of the mantle beneath. And so, as you would
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be aware, they float around on the surface, but the
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surface is a sphere. And so what happens through time
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is that all these continents come together at one particular time,
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but then they break apart again. and move around and
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tend to meet on the other side of the planet. So,
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plate tectonics is a response to the mantle convecting, and
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because the Earth is a sphere, the continents bang into
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each other to form a supercontinent every now and again,
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and that's probably every 500 or so million years.
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And Gondwanda was one of these supercontinents.
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Yeah, Tangier was the one that formed about 300 to
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200 million years ago. And the one that formed before
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that was Gondwana. And Gondwana formed as a supercontinent between
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about 550 and 500 million years ago.
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That's interesting because that's about the same time as the
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Cambrian explosion in life, isn't it?
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Oh, bang on. Exactly the time that the Cambrian explosion
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of life happened.
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And that saw life diversify to the multi-celled plethora of
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existence we have today.
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Yes, yes, definitely. At that time, the limited animal that
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did exist, they tended to be soft-bodied creatures, no backbone,
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and they had very limited ability to evolve because the
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conditions were very harsh leading up to the formation of Kronmata.
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But once Kronmata formed, at least in our mind, things
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became a lot easier. for life to explode, and it did.
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Now, you've been looking at just how extensive Gondwana was.
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What have you found?
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Gondwana's been known about for over 100 years. In fact,
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it goes back to about the 1880s. This guy, Edward Zeus,
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realised that fossils that could be found in India were
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found in Australia and Antarctica, South America, Africa, and it
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made him think that there was a supercontinent, and he
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called it the Great Southern Continent. So that was the
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beginning of understanding it. But over time, and maybe... towards
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the end of the last century, people started to add
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a bit to this core, this continental core. And so
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they were seeing bits of Eastern America and bits of
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Europe and bits of Southern Asia like Pakistan, Iran, and
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even Turkey as being part of it. So although there
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was the core, there were these little bits around what
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at the time was the edge that had been added.
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And when they calculated up the percentage, of landmass that
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Gondwanas seemed to be, they said it was around 64%.
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And some guy had arbitrarily said that it is 75%
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of landmass, total landmass, excluding oceans, to produce continents. And
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so people then started turning around and saying, well, maybe
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Gondwana isn't really a supercontinent. because it's not big enough.
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That was a state of play until quite recently.
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Yeah, there's one of those in every group, isn't there?
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Well, it did cause a lot of problems because the
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thing about Gondwana is there's all these isotope proxies. Now,
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isotopes of different elements are used as proxies for all
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sorts of things. And the reason why we know about
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past climate is because of carbon isotope changes and oxygen
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isotope changes. And there are other elements that have the
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same sort of capacity. Another one is strontium, which records
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seawater compositional changes. And there's even one in rock and granite.
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And all of those isotopes were showing us that Around
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550 million years ago, everything changed. And it's the biggest
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change that you're actually seeing in the isotopic record can
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be measured back to 4,000 million years. This is the
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biggest switch. So to me, there was always this paradox
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of why does Godwina have this really big switch? in
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all these proxy systems that record dynamic change in the Earth.
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Why do they all have this big switch around 550,
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500 million years ago if gone one and one for
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the supercontinent? And so that was always in the back
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of my mind as a paradox.
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There's always a problem when... You start putting arbitrary lines
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in things instead of seeing the grayness between one genre
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and another.
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I can't agree with you more. Until you hit the
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nail on the head, there's always gray areas between what
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people classify as an artificial thing and what is reality.
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There's always transition, gray areas.
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So you looked at different isotopes and ratios to work
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out exactly what was where. And from that, you were
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able to determine that Gondwanda was much bigger than some
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estimates had placed it at.
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This isotopic system that we use is called samarium neodymium.
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Samarium breaks down the form neodymium. It's a parent-daughter type
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isotope system. It's rare earth. is one that's very robust.
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It can survive temperatures of resetting that might tend to 1,000
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degrees centigrade. So it holds the information that's sending back
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to its origin.
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So it doesn't get destroyed by volcanic activity and things
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like that, which is, what, 800 degrees?
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Yeah, exactly. And so I was just going to say, like,
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underneath Every volcano is a magma, which is usually composed
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of granite, particularly on the continent. And if you looked
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at the Himalayas today, for example, there are granites in
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the Himalayas that are 20 million years old. There are
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others that are 50 million years old, others that are
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100 million years old, and so on. But they all
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extend back until 500, 550 million years ago. And that's
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what the barium, neodymium isotopic composition tells us, that they
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all come from this material, which is about the age
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of what we thought Gondwana was when it formed.
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The link between Greater Gondwana and ending Snowball Earth. Snowball
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Earth was 717 million years ago. I know that because
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I just did a story on it.
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It went for over 100 million years. It was a very,
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very long period of time that Snowball Earth existed. And
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the thing about Snowball Earth, it defines that all the
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continents were covered in ice, that it didn't matter whether
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or not they were at the poles or.
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At the equator.
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Snowball Earth actually continued for at least 100 million years,
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up to maybe 580. People argue about when it stopped,
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but certainly there was a time between 500 and... 600
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million years when we started coming out of Snowball Earth.
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And it does coincide with when Gondwana was forming. And
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most of it had formed between about 600 and 700,
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but we know that it kept forming until about 550.
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And when Gondwana was a supercontinent, as it finally came together,
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Snowball Earth did persist up to about that time when
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it changed, which was around the time that Gondwana.
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How did Gondwana change our climate?
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The critical thing was all these fragments that went to
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form Gondwana, all the big continental landmasses came together between
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600 and 500 million years ago, forming a huge mountain
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range that crisscrossed Gondwana land, a little bit like what
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the Himalayas are today. But like the Himalayas, they don't
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erupt volcanoes from them. Large mountain belts don't do that.
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So when Gondwana formed and all these big mountain belts existed,
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the mantle of the Earth had to convect. And so
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the way that it did it, it reconfigured itself to
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start producing volcanoes around the edge of Gondwana. And this
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was the first ring of fire. I'm sure you know
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about the Pacific ring of fire.
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Yeah, I've been watching Krakatoa very closely, or should I
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