Sept. 8, 2026
Molten Planets and Solar Storms: Unveiling Cosmic Wonders
SpaceTime Series 29 Episode 108 Discovery of a new class of molten planet Astronomers have discovered a new type of molten planet beyond our Solar System. The mother of all solar storms New evidence in tree ring records is showing scientists that the Sun can become far more violent than previously thought. Two giant blobs of hot rock discovered on Earth’s core mantle boundary Scientists have discovered two immense, ultra-hot rock structures located at the base of Earth’s mantle, around 2,900 kilometres beneath Africa and the Pacific which are affecting the underlying liquid outer core. The Science Report A new study suggests El Niño is intensifying as the planet warms. Researchers have discovered that some centenarians have rare cancer killing cells in their bodies. A new study shows Tasmanian tigers were significantly different from both wolves and wild dogs. Warnings that Artificial Intelligence is making writing styles more similar and losing the individual identity. Alex on Tech Apple’s new iphone fold Ultra.
Our Guests This Week Dr Benjamin Pope from Macquarie University Chelsea Gohd NASA Public Engagement Specialist Astrophysicist Jason Rhodes NASA JPL Astrophysicist DIda Markovic NASA JPL Astrophysicist Eric Huff NASA JPL 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/
Our Guests This Week Dr Benjamin Pope from Macquarie University Chelsea Gohd NASA Public Engagement Specialist Astrophysicist Jason Rhodes NASA JPL Astrophysicist DIda Markovic NASA JPL Astrophysicist Eric Huff NASA JPL 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/
The Astronomy, Space, Technology & Science News Podcast.
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This is Space Time, Series 29, Episode 108, for broadcast
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on the 9th of September, 2026. Coming up on Space Time.
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Discovery of a new class of molten planet. Ancient tree
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warnings about the next big solar storm. And two giant
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blobs of hot rock discovered on the Earth's core mantle boundary.
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All that and more coming up on Space Time.
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Welcome to Space Time with Stuart Gary.
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Astronomers have discovered a new type of molten planet beyond
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our solar system.
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The findings, reported in the journal Nature.
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Astronomy, suggest this strange exoplanet stores large amounts of sulfur
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deep within a permanent ocean of magma. The exoplanet, known
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as L9859d, is about 1.6 times the size of the
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Earth and orbits a small red dwarf star about 35
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light-years away. Observations with NASA's Webb Space Telescope suggested something unusual.
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The planet had an especially low density given its size,
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and it peaced to contain significant amounts of hydrogen sulfide
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in its atmosphere. Until now, astronomers would have placed a
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planet like this into one of two very familiar categories,
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either a rocky gas dwarf with an atmosphere of hydrogen,
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or a water world made up of deep.
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Oceans and ice.
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But the new findings show that L9859d fits neither description. Instead,
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it appears to belong to an entirely different class of planet,
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one containing heavy sulfur molecules. To try and work out
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what's going on, astronomers used computer simulations to try and
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reconstruct this strange world's evolution over the past 5 billion years.
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By directly linking telescope observations to these physical models of
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planetary interiors and atmospheres, the authors were able to determine
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what must be going on deep inside the planet. And
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their results revealed that the mantle of L9859D is likely
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molten silicate similar to lava here on Earth, with a
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global magma ocean extending thousands of kilometers beneath. This vast
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molten reservoir allows the planet to store extremely large amounts
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of sulfur deep inside its interior and maintain that over
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geologic timescales. The magma ocean also helps L9859D to retain
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a thick hydrogen-rich atmosphere containing sulfur-bearing gases.
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Like hydrogen sulfide.
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And normally, this would be lost into space over time
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due to X-ray radiation produced by the host star. The
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study's lead author, Harrison Nichols from Oxford University, says the
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findings suggest that L9859d may be the first recognized member
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of a broader population of gas-rich sulfurous planets sustaining long-lived
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magma oceans. Now, if that's the case, it means the
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diversity of worlds within our galaxy, the universe for that matter,
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may be even greater than previously imagined. Web observations from
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2024 pointed to the presence of sulfur dioxide among other
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sulfur gases high in L9859D' s upper atmosphere.
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The new models show that these.
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Gases can be created when ultraviolet light from the host star,
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the red dwarf L9859, triggers chemical reactions. At the same time,
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the magma ocean below acts as a massive reservoir for
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buffering these volatile gases, storing and releasing them over billions
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of years after the planet was formed. This combination of
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deep volatile gases within its interior and ultraviolet-driven atmospheric chemistry
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explains the planet's notable properties. According to the simulations, L9859d
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likely formed with a large amount of volatile material. It
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may once have looked more like sort of a large
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sub-Neptune planet. And over billions of years, it gradually shrank
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as it cooled and lost some of its atmosphere. Of course,
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magma oceans represent the universal initial states of all rocky planets,
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including planets like the Earth and Mars. So the new
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insights into magma ocean physics can inform scientists about our
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own world and its primordial history. This is space time.
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Still to come, what ancient tree rings are telling us
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about the next big solar storm, and two giant blobs
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of hot rock discovered on the Earth's core mantle boundary.
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All that and more still to come. on Space Time.
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New evidence in tree ring records are warning scientists that
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our sun can become far more violent than previously thought.
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The findings, reported in the journal Communications Earth and Environment,
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demonstrates how a local star can unleash a solar storm
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far larger than we've ever recorded. And a study of
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some of the planet's oldest trees suggested we could soon
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be due for one of these events. The first clear
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signs of exceptionally high solar activity came from Japanese cedar trees.
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In 2012, Fusamiaki was studying slices of ancient Japanese cedar
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taken from a tree filled in the 1950s. It had
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grown on Yakushima Island, a protected site famed for its
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long-lived trees, some of which have stood for millennia, laying
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down one ring of wood after another, year after year.
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These tree rings are not just markers of age. They're
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also annual records of the Earth's atmosphere, and studying them
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could help scientists predict and prepare for future disruptive solar storms.
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The key is the relative proportion of carbon-14 in each
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tree ring. It reveals how active the sun was each year.
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While examining these ancient tree records, Miyake discovered that between
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the years 774 and 775, the amount of this isotope, carbon-14,
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in the cedar jumped by about 12 parts per thousand,
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roughly 20 times larger than the change expected from ordinary
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variations in the sun. The massive spike means Earth's atmosphere
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must have been hit by a sudden burst of unusually
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energetic particles, and the same signature was later identified in
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trees from North America and Europe. And the measurements of
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another radioisotope, beryllium-10, in ice core samples further confirmed the discovery.
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Scientists initially speculated the cause may have been a nearby
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supernova explosion, a gamma-ray burst, or maybe a blast from
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a neutron star. These have all been ruled out because
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the nearest possible sources are far too distant. And that
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left solar flares from the Sun as the most likely cause.
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Solar flares happen when magnetic energy that's been building up
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in the Sun's atmosphere is suddenly released.
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In a matter of minutes, a patch of.
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The Sun can brighten violently, ejecting radiation across the electromagnetic
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spectrum from radio waves to X-rays. Often, these eruptions are
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accompanied by streams of high-speed charged particles and vast bubbles
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of magnetized plasma, known as coronal mass ejections. Scientists know
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unusually large solar flares have hit the Earth before, the
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most famous being the Carrington event in 1859. That eruption
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was so intense that telegraph lines across Europe and North
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America caught fire, telegraph operators suddenly got electric shocks, and
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auroral lights normally confined to polar latitudes were seen deep
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into the tropics. Ever since, Carrington has been the benchmark
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for solar violence. But the strange thing is, even Carrington
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wasn't powerful enough to leave a clear carbon-14 signature in
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tree rings. To do that, the sun would need to
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unleash a storm at least 10 times larger, a super flare. Now,
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since Miyake's first discovery, scientists have found five more Miyake events,
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occurring roughly every 2,000 years. In 2013, Miyake's team found
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a second spike in cedar and cypress rings confirmed in
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European oak and Siberian larch. Then using beryllium-10 measurements from
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Greenland ice cores and matching the carbon-14 signatures in Polish oak,
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scientists were able to identify another in the year 664.
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In 2022, two more events were identified, followed by a
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fifth in sub-fossil scots pine from the French Alps in 2023.
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That one dated back to a massive blast some 14,350
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years ago. Although these super flares are rare, they still
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represent a challenge for science's understanding of solar physics. That's
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because stars like our Sun aren't expected to produce events
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on this scale. However, the evidence is clear. They have
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happened in the past, and could happen again. To determine
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how likely these super flares are, scientists have been sifting
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through the records, combining high-resolution carbon-14 data from tree rings
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spanning almost an entire millennium. And they've now come up
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with eight more signatures, not quite as big as the
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Miyake super flares, but significant nevertheless. Five of these were
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newly measured in European oak, mainly from Germany and France,
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while three came from existing tree ring datasets. They then
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modelled Earth's carbon cycle to search for abrupt increases in carbon-14,
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finding four candidate intermediate events around the years 14, 553,
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675 and 954, meaning a frequency of around 1 every
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200 years. Benjamin Pope from Macquarie University says the exact
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nature of the danger posed by these intermediate class events
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depends on what's actually causing them. Pope says if the
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culprit is a coronal mass ejection, the main threat would
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come from the way the event distorts Earth's magnetic field.
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It could trigger a geomagnetic storm, driving unwanted currents through
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power grids, pipelines and other long conductive systems. The damage
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would be uneven, shaped by geography, geology and the layout
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of the infrastructure.
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On the ground.
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Earp warns of a scenario in which an event may
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take out critical manufacturing capabilities. But interpreting solar events from
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carbon-14 can be complex. See, the carbon-14 spike is made
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high in the atmosphere. It then has to filter down
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into the air that the trees absorb. By then, a
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tree may already be growing new wood using carbon stored
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from previous years. Wood that's formed at the start of
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the annual growth season could be especially prone to this blurring,
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while later growing wood may offer a clearer annual signal.
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Pope says some tree rings start growing around spring, but
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the carbon they used to grow that ring could be
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from previous years. The point of this work isn't only
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to work out how often civilization might be jolted by
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a super solar storm. Miyake events may be telling us
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something profound about the sun itself. Pope says the real
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question remains, when will the next big solar storm come,
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and just how bad will it be?
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So there's this thing called radiocarbon dating, where you measure
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the content of carbon-14, an isotope that's radioactive, compared to carbon-12,
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which is most of the carbon in the world, which
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is stable. carbon-14 in something and you're able to tell
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how old it is because carbon-14 is produced by radiation
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hitting the atmosphere. It filters through the atmosphere, the carbon
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cycle into plants and animals you and me and we
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are all constantly being topped up with fresh carbon-14 from
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on the air and from the things we eat. The
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thing is, though, when we die, which does happen to
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all of us, this top-up stops happening. And so it
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means that now the amount of carbon-14, which is radioactive
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and starts to decay, is like a clock that can
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tell you how old something is. So the thing you
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need to know in order to tell how old something is,
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is you measure the amount of radiocarbon in it and
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you compare it to the amount it should have started with.
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But here's your problem. How do you know how much
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it started with? And so there's actually a different amount
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of radiation striking atmosphere every year, producing a different amount
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of radiocarbon. And so there's no really easy way to
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be able to say from a physical started with and
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therefore how old the sample is. So what you've got
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to do is take advantage of another type of clock
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that nature's provided us with, that is tree rings. So
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every tree ring records a year of growth. You can
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see these in your hardwood table. And so the trick
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is that a good year and a bad year are
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usually the same good year and the same bad year
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for all the trees of the same species in the
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same region. And so what it means is that the
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pattern of long and short tree rings is really the
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same across all the different trees of the same species
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in the same region, where I might mean all the
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Huon pines in Tasmania or all the oaks in Europe
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or something, right? So I mean quite a big region
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and quite a big species, right? And so what you
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can therefore do is you can read these like a
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barcode and say how old some tree rings are to
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the exact year. What you do is you start by
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daisy chaining them. You look at an old tree today
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and you know what the date is today and you
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count 200 years going back in time. But then you
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look at older trees, they might be in buildings or
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they might be fossilized in bulks or whatever. You look
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at these older trees and you try and say, okay,
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where do these barcodes overlap with the one we know?
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And so you can build up a library going back
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millennia sometimes for some species in some regions. of these
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tree ring barcodes that allow you to do a science
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called dendrochronology, which is Greek for tree timing. It means
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you can find a sample of wood from any given
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year going all the way back to the Ice Age.
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And so it means that you can say, I know
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exactly how old this wood is, and then I can
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measure the amount of radiocarbon in it, and therefore I
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can tell how much radiocarbon it started with. So, scientists
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have been using this for decades in order to do
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archaeology better. They've also been interested in doing astronomy with
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these trees. So, using the world's forests as the world's
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biggest telescope by saying, well, okay, we're interested not in
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the archaeology that we might be, but specifically in how
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and why it is the amount of radiation. hitting the
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atmosphere vary from year to year. And so it turns
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out that this is basically related mainly to solar activity.
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So the sun waxes and wanes in strength in terms
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of its magnetic fields every 11 years. And so when
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the magnetic field's strong, it blocks out a lot of
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radiation from reaching the Earth. And when it's weak, a
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lot of radiation is let through. It's like a force
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field protecting us from cosmic rays. So I mean, sometimes
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you have more radiocarbon, sometimes you have less. So far,
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so good. And so there was this scientist, Fusa Miyake
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was her name, and we call them Miyake events for
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this reason. who went and took a bunch of tree
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