Meteorite Myths, Daylight Fireballs & the Secrets of Ultra-Faint Galaxies
Space Nuts: Astronomy Insights & Cosmic DiscoveriesNovember 07, 2025
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00:48:2444.36 MB

Meteorite Myths, Daylight Fireballs & the Secrets of Ultra-Faint Galaxies

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Meteorite Myths, Fireballs, and the Enigmatic 3I Atlas
In this thrilling episode of Space Nuts, hosts Andrew Dunkley and Professor Jonti Horner dive into a variety of fascinating cosmic topics, from the truth behind a supposed meteorite impact on a car to the latest developments surrounding the comet 3I Atlas. This episode is packed with intriguing insights and lively discussions that will leave you pondering the mysteries of the universe.
Episode Highlights:
Meteorite or Not? Andrew and Jonti examine a peculiar incident involving a car in South Australia that was thought to have been struck by a meteorite. They explore the evidence, including an impressive impact crater on the windscreen, and discuss the likelihood that it was merely debris from a passing truck instead.
Daylight Fireball: The hosts report on a recent fireball sighting over southeastern Australia that captivated witnesses in broad daylight. They analyze the characteristics of this event and the implications it might have for potential meteorite recovery.
Updates on 3I Atlas: The episode features an update on the comet 3I Atlas, which recently passed perihelion. Andrew and Jonti discuss its unusual behavior, including rapid brightening and the theories behind its activity as it travels through the solar system.
Supermassive Black Holes in Tiny Galaxies: The discovery of a supermassive black hole in the ultra-faint dwarf galaxy Segue One raises intriguing questions about galaxy formation and evolution. The hosts delve into the implications of this finding and what it reveals about the nature of dark matter and galaxy interactions.
Life After Asteroid Impacts: A fascinating study from Finland sheds light on how life can rebound after an asteroid impact. The research team investigates the timeline of microbial recolonization in a crater formed 78 million years ago, revealing insights into the resilience of life on Earth.
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Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.

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00:00:00 --> 00:00:02 Andrew Dunkley: Hi there. Thanks for joining us on Space Nuts

00:00:02 --> 00:00:04 where we talk astronomy and space science. My

00:00:04 --> 00:00:07 name is Andrew Dunkley and hope, uh, you're.

00:00:07 --> 00:00:10 Well, coming up in this episode we are going

00:00:10 --> 00:00:12 to, uh, look at, oh, there's a whole bunch of

00:00:12 --> 00:00:14 stuff. We might not fit it all in. We'll do

00:00:14 --> 00:00:17 our very best. Uh, a meteorite versus a

00:00:17 --> 00:00:19 windscreen. Did it happen the way people

00:00:19 --> 00:00:21 think? We'll tell you. And over the

00:00:21 --> 00:00:24 weekend, uh, there was a fireball seen over,

00:00:25 --> 00:00:27 uh, southeastern states, uh, Victoria, New

00:00:27 --> 00:00:30 South Wales. The act. We'll talk about that.

00:00:31 --> 00:00:32 Uh, there's been a bit of chatter on social

00:00:32 --> 00:00:35 media, including the Space nuts podcast group

00:00:35 --> 00:00:38 about 3i Atlas. So we'll have

00:00:38 --> 00:00:41 an update on that. And time permitting, we

00:00:41 --> 00:00:44 will be looking at a huge black hole and a

00:00:44 --> 00:00:46 tiny galaxy. I mean tiny as in

00:00:46 --> 00:00:49 maybe only hundreds or thousands of stars. It

00:00:49 --> 00:00:52 sounds unusual, doesn't it? And life

00:00:52 --> 00:00:55 after an asteroid impact. That's all coming

00:00:55 --> 00:00:58 up on this episode of Space Nuts.

00:00:58 --> 00:01:00 15 seconds. Guidance is internal.

00:01:00 --> 00:01:03 10, 9, ignition

00:01:03 --> 00:01:04 sequence time.

00:01:04 --> 00:01:07 Jonti Horner: Uh, Space Nuts. 5, 4, 3, 2.

00:01:07 --> 00:01:09 Andrew Dunkley: 1, 2, 3, 4, 5, 5, 4, 3,

00:01:09 --> 00:01:12 2, 1. Space Nuts astronauts report

00:01:12 --> 00:01:13 it feels good.

00:01:14 --> 00:01:17 And with Fred still away, we are, uh,

00:01:17 --> 00:01:19 thrilled to welcome again Jonti Horner,

00:01:19 --> 00:01:21 professor of astrophysics at the University

00:01:21 --> 00:01:23 of Southern Queensland. Hello, Jonny.

00:01:24 --> 00:01:25 Jonti Horner: Good morning. How are you going?

00:01:25 --> 00:01:28 Andrew Dunkley: I am well. Good to see you. Nice backdrop

00:01:28 --> 00:01:29 too, by the way. What do you got there?

00:01:29 --> 00:01:31 Jonti Horner: Um, so another of the picks I've been playing

00:01:31 --> 00:01:33 around with with the telescope I bought about

00:01:33 --> 00:01:35 12 months ago. This is supplied ease I can

00:01:35 --> 00:01:36 slap out of shot.

00:01:36 --> 00:01:38 Andrew Dunkley: Um, very nice.

00:01:38 --> 00:01:40 Jonti Horner: My chair immediately interferes. The chair

00:01:40 --> 00:01:41 caption. Human being.

00:01:41 --> 00:01:43 Andrew Dunkley: But that was the, that was the Chair Nebula.

00:01:44 --> 00:01:47 Jonti Horner: Absolutely. But yes, I get the angle of the

00:01:47 --> 00:01:49 chair just right. The AI doesn't recognize it

00:01:49 --> 00:01:51 as a human being and we get to see it. Yeah,

00:01:51 --> 00:01:53 pretty good. But I'm going to have to have

00:01:53 --> 00:01:55 another go at that site. It doesn't quite

00:01:55 --> 00:01:56 feel right. It looks a little uncanny valley

00:01:56 --> 00:01:58 to me. So I may have to take some more photos

00:01:58 --> 00:02:00 later in the ah, year if the wonderful

00:02:00 --> 00:02:02 thunderstorms we're getting at the minute

00:02:02 --> 00:02:03 kind of stop because we've had some

00:02:03 --> 00:02:05 interesting weather appear again over the

00:02:05 --> 00:02:08 last few days. Um, there was a possible

00:02:08 --> 00:02:10 tornado within 30km of my house, which is

00:02:10 --> 00:02:13 cool. And some places got 10 centimeter

00:02:13 --> 00:02:16 diameter hail and lots of damage and

00:02:16 --> 00:02:18 yeah, tasty stuff going on and we might get a

00:02:18 --> 00:02:20 little bit more today and tomorrow. So it's

00:02:20 --> 00:02:22 another of those events which is spectacular

00:02:22 --> 00:02:24 and fun to watch. But you also sympathise

00:02:24 --> 00:02:25 with those who are directly in the thyroid

00:02:25 --> 00:02:26 line.

00:02:26 --> 00:02:28 Andrew Dunkley: Yeah, I saw those, uh, tornado

00:02:28 --> 00:02:30 forecasts pop up. And, uh,

00:02:31 --> 00:02:34 the bureau does not often go that far,

00:02:34 --> 00:02:36 uh, with their forecasting, but they were

00:02:36 --> 00:02:39 pretty confident. So, yeah, we get a few of

00:02:39 --> 00:02:40 those down our way too.

00:02:40 --> 00:02:42 Jonti Horner: It is an interesting one. I mean, growing up

00:02:42 --> 00:02:44 in the uk, I grew up in the country or one of

00:02:44 --> 00:02:46 the few countries that has the most tornadoes

00:02:46 --> 00:02:49 per year, which shocks everybody. But they're

00:02:49 --> 00:02:51 really, really itty bitty diddy ones that are

00:02:51 --> 00:02:53 associated with frontal systems. And I think

00:02:53 --> 00:02:55 a lot of Americans say, oh, no, they're not

00:02:55 --> 00:02:57 tornadoes, they're just gusnados or something

00:02:57 --> 00:02:59 like that. But in terms of the really

00:02:59 --> 00:03:01 damaging thunderstorms around the world,

00:03:02 --> 00:03:04 you've got the Great Plains in the US and

00:03:04 --> 00:03:05 then you've got the kind of area around

00:03:05 --> 00:03:08 Bangladesh, I think. But after that kind of

00:03:08 --> 00:03:09 Southeast Queensland, northeast New South

00:03:09 --> 00:03:12 Wales is the New South Wales is the third

00:03:12 --> 00:03:14 best place in the world for these kind of

00:03:14 --> 00:03:17 storms. And we get fewer tornadoes than

00:03:17 --> 00:03:18 the Great Plains because we get less wind

00:03:18 --> 00:03:21 shear at high altitudes. But we get

00:03:21 --> 00:03:24 equivalent amounts of mega hail and guerrilla

00:03:24 --> 00:03:25 hail is what they're calling it nowadays when

00:03:25 --> 00:03:28 you're bigger than giant hail. So we do get

00:03:28 --> 00:03:29 some really tasty and interesting stuff. And

00:03:29 --> 00:03:32 I did have one day not long after we built

00:03:32 --> 00:03:34 this house and moved in where the garage was

00:03:34 --> 00:03:37 still full of boxes, um, which is always a

00:03:37 --> 00:03:38 good thing. And this thunderstorm came in and

00:03:38 --> 00:03:40 suddenly there's the roaring of a freight

00:03:40 --> 00:03:42 train kind of noise, which was so weird, and

00:03:42 --> 00:03:45 hailstones, hailstones as my fist started

00:03:45 --> 00:03:47 coming down and I had to run out with

00:03:47 --> 00:03:50 blankets and a doona, uh, to cover the

00:03:50 --> 00:03:51 windscreen of my car to prevent it getting

00:03:51 --> 00:03:53 damaged. And unfortunately it didn't. Well,

00:03:53 --> 00:03:54 fortunately it didn't get much worse than

00:03:54 --> 00:03:56 that. But it was an interesting experience

00:03:56 --> 00:03:57 for someone who grew up in the uk, where the

00:03:57 --> 00:03:59 worst weather gets a bit of drizzle and a lot

00:03:59 --> 00:04:00 of wind.

00:04:00 --> 00:04:02 Andrew Dunkley: Yeah, yeah, it can get pretty volatile, uh,

00:04:02 --> 00:04:04 in Australia, and especially in the eastern

00:04:04 --> 00:04:05 parts.

00:04:06 --> 00:04:08 Uh, speaking of volatile, our first story

00:04:08 --> 00:04:11 is about, um,

00:04:12 --> 00:04:14 what people thought was a meteorite hitting

00:04:14 --> 00:04:17 the windscreen of a car. And when you see the

00:04:17 --> 00:04:19 photo, it's. It's one heck of a crack. It's,

00:04:19 --> 00:04:22 um, it's come in hard, whatever it was. Uh,

00:04:22 --> 00:04:23 what is the story here?

00:04:24 --> 00:04:27 Jonti Horner: It's a slightly weird one. Um, there's a

00:04:27 --> 00:04:30 guy driving along. Um, he's a vet down

00:04:30 --> 00:04:32 in South Australia, goes by the name of

00:04:32 --> 00:04:35 Melville Smith. It's his name, Andrew M.

00:04:35 --> 00:04:37 Melville Smith. Driving along in his

00:04:37 --> 00:04:39 Tesla. And the Tesla part is important to the

00:04:39 --> 00:04:42 story. Apparently about 40km out from

00:04:42 --> 00:04:45 a place called Port Garmin, when suddenly

00:04:45 --> 00:04:46 there's a really loud smash on his

00:04:46 --> 00:04:49 windscreen. Um, him and his partner in the

00:04:49 --> 00:04:52 front seats get showered with glass from this

00:04:52 --> 00:04:54 shattered windscreen and there's an impact

00:04:54 --> 00:04:57 crater on the windscreen. Um, and

00:04:57 --> 00:04:59 obviously the car just kept on driving

00:04:59 --> 00:05:01 because it's a Tesla and they don't seem to

00:05:01 --> 00:05:03 notice when they hit things, they just carry

00:05:03 --> 00:05:05 on. Um, all is good

00:05:07 --> 00:05:09 now. He thought it was weird, so he reached

00:05:09 --> 00:05:12 out to the museum in South Australia with

00:05:12 --> 00:05:14 the idea that this could have been a

00:05:14 --> 00:05:17 meteorite hitting a car. And that would be

00:05:17 --> 00:05:19 very unusual. Now we've had occasions in the

00:05:19 --> 00:05:22 past, um, most famously the Peekskill

00:05:22 --> 00:05:23 meteorite, and I think it was 1994, where

00:05:23 --> 00:05:26 meteorites have hit parked cars and done a

00:05:26 --> 00:05:28 lot of damage. And I think in the case of the

00:05:28 --> 00:05:31 Peekskill meteorite, it was a fairly hefty

00:05:31 --> 00:05:33 iron ore, stony iron meteorite that basically

00:05:33 --> 00:05:36 wrote off the rear end of the car. And the

00:05:36 --> 00:05:37 person who owned the car was very upset until

00:05:37 --> 00:05:39 a museum bought the car for a six figure sum,

00:05:39 --> 00:05:42 which kind of the blow. This, um,

00:05:42 --> 00:05:45 case, part of the reason that they thought it

00:05:45 --> 00:05:47 was a meteorite was that there was melting of

00:05:47 --> 00:05:50 the windscreen as well as just shattering of

00:05:50 --> 00:05:53 the windscreen. And this, the people at South

00:05:53 --> 00:05:55 Australia Museum basically came out with a

00:05:55 --> 00:05:56 fairly neutral statement and said, we're

00:05:56 --> 00:05:58 going to investigate this. It sounds really

00:05:58 --> 00:06:00 weird. The melting sounds odd. We're not sure

00:06:00 --> 00:06:03 what's going on. To me as an

00:06:03 --> 00:06:04 astronomer though, it speaks to one of the

00:06:04 --> 00:06:07 kind of really big Hollywood movie driven

00:06:07 --> 00:06:10 myths, I think, about meteorites.

00:06:10 --> 00:06:12 There's this idea that if a meteorite falls

00:06:12 --> 00:06:13 through the atmosphere and you pick it up

00:06:13 --> 00:06:15 immediately, it'll burn your hands, it'll be

00:06:15 --> 00:06:18 super, super hot. And that just really

00:06:18 --> 00:06:20 isn't the case now. I mean, it would be the

00:06:20 --> 00:06:23 case if something like the dinosaur killing

00:06:23 --> 00:06:25 asteroid hit the Earth. Uh, that'd get really

00:06:25 --> 00:06:26 hot, but you wouldn't be picking it up

00:06:26 --> 00:06:29 because you'd be vaporized and dead. Right.

00:06:29 --> 00:06:31 Um, for the smaller things that hit the, uh,

00:06:31 --> 00:06:34 Earth but can make it to the ground intact,

00:06:35 --> 00:06:37 they typically are slowed down by the

00:06:37 --> 00:06:39 atmosphere such that by the time they're 10

00:06:39 --> 00:06:41 or 20 kilometers above the ground, they've

00:06:41 --> 00:06:44 slowed down to below the speed of sound. And

00:06:44 --> 00:06:45 so that's why when you see the fireball for

00:06:45 --> 00:06:48 these things, that fireball terminates still

00:06:48 --> 00:06:50 quite high in the atmosphere. And while it

00:06:50 --> 00:06:51 might look like it was just over the next

00:06:51 --> 00:06:54 hill from you. The thing was still 20 or 30

00:06:54 --> 00:06:56 kilometers up. That's because the air

00:06:56 --> 00:06:58 resistance has been enough to slow them down.

00:06:58 --> 00:07:00 And at that point, they're falling at just a

00:07:00 --> 00:07:02 couple of hundred kilometers per hour at

00:07:02 --> 00:07:04 terminal velocity. Now, that's still pretty

00:07:04 --> 00:07:06 fast. And I mean, I wouldn't want to fall at

00:07:06 --> 00:07:09 200km an hour into the ground. No, but it

00:07:09 --> 00:07:11 means that from a height of 20 or 30 km, it

00:07:11 --> 00:07:13 takes a few minutes to reach the ground.

00:07:14 --> 00:07:16 What that means is that there's time for the

00:07:16 --> 00:07:19 rock to equilibrate to get

00:07:20 --> 00:07:22 the temperature equalized across this entire

00:07:22 --> 00:07:24 object. Now, the object's been held in space

00:07:24 --> 00:07:27 in cold storage for millions of years. Years.

00:07:27 --> 00:07:29 So the interior of the rock is bitterly,

00:07:29 --> 00:07:32 bitterly, bitterly cold. And, um, they've got

00:07:32 --> 00:07:35 rocky asteroids, rocky meteorites have a

00:07:35 --> 00:07:38 fairly high thermal inertia. They're not very

00:07:38 --> 00:07:40 conductive. And so what

00:07:40 --> 00:07:42 happens is that the thin outer layer gets

00:07:42 --> 00:07:44 super hot when it's coming through the

00:07:44 --> 00:07:46 atmosphere and it's luminous and that's

00:07:46 --> 00:07:48 getting ablated away. But very little

00:07:48 --> 00:07:51 of that heat actually is conducted to the

00:07:51 --> 00:07:53 interior. Once this thing slows down,

00:07:54 --> 00:07:56 it just keeps falling. And you've got a huge

00:07:56 --> 00:07:58 amount of cold material and a very, very tiny

00:07:58 --> 00:08:01 thin layer of hot material. So by the time it

00:08:01 --> 00:08:03 reaches the ground, meteorites are typically

00:08:03 --> 00:08:05 cold to the touch. And you're more likely to

00:08:05 --> 00:08:08 see frost forming on them or water vapor

00:08:08 --> 00:08:10 condensing on them. It's a bit like maybe

00:08:10 --> 00:08:12 deep fried ice cream. You deep fry the ice

00:08:12 --> 00:08:14 cream, you get a hot layer on the outside,

00:08:14 --> 00:08:16 but the ice cream in the middle stays cold.

00:08:16 --> 00:08:19 Same kind of idea. The one caveat to that

00:08:19 --> 00:08:21 is if you get an iron meteorite, a metal

00:08:21 --> 00:08:23 meteorite, that'll have a much higher thermal

00:08:23 --> 00:08:25 conductivity. So that can be quite warm when

00:08:25 --> 00:08:28 it reaches the ground. But rather than being

00:08:28 --> 00:08:30 super hot like the atmosphere, it's probably

00:08:30 --> 00:08:31 going to be nearer to room temperature.

00:08:32 --> 00:08:35 That's fine. What was pointed out to me,

00:08:35 --> 00:08:38 um, famous astronomer called Rob McNaught got

00:08:38 --> 00:08:39 in touch with me after he heard me on the

00:08:39 --> 00:08:41 radio talking about this one. Because I got

00:08:41 --> 00:08:43 called out, I got cold about this while I was

00:08:43 --> 00:08:45 driving back from the airport, having picked

00:08:45 --> 00:08:48 up colleague talked about it and Rob got

00:08:48 --> 00:08:50 in touch and pointed out that space junk,

00:08:51 --> 00:08:53 because it comes in at a much shallower

00:08:53 --> 00:08:56 angle, it actually ablates in the atmosphere

00:08:56 --> 00:08:58 for much, much, much longer. And it's usually

00:08:58 --> 00:09:00 much more conductive material. So you put

00:09:00 --> 00:09:03 those two things together and if a bit of

00:09:03 --> 00:09:05 space junk were to reach the Ground,

00:09:06 --> 00:09:08 there is a good chance that would be hot to

00:09:08 --> 00:09:11 the touch at the time you get to it. So one

00:09:11 --> 00:09:12 of the. Another thing that you could possibly

00:09:12 --> 00:09:14 use to differentiate, uh, between whether

00:09:14 --> 00:09:16 this is a meteorite or a bit of SpaceX

00:09:16 --> 00:09:19 material. All of that put together

00:09:19 --> 00:09:21 means that the melting of the windscreen and

00:09:21 --> 00:09:24 this rock being hot to me, actually kind of

00:09:24 --> 00:09:26 rules out it being a meteorite.

00:09:26 --> 00:09:26 Andrew Dunkley: Yeah.

00:09:26 --> 00:09:29 Jonti Horner: What adds to my argument that it's almost

00:09:29 --> 00:09:30 certainly not a meteorite is it was a

00:09:30 --> 00:09:32 nighttime event, the skies were clear in the

00:09:32 --> 00:09:34 area, nobody saw a fireball. There are no

00:09:34 --> 00:09:37 reports of a bright fireball, added to

00:09:37 --> 00:09:40 which are also no reports of sonic events

00:09:40 --> 00:09:42 or tremors, you know, things that would show

00:09:42 --> 00:09:44 up in the seismograph. So I think we can

00:09:44 --> 00:09:47 fairly definitively rule out a meteorite as

00:09:47 --> 00:09:49 the source of this impact on this car.

00:09:50 --> 00:09:52 Um, there is the amusing option that it could

00:09:52 --> 00:09:54 have been a SpaceX on Tesla impact, which

00:09:54 --> 00:09:56 would have been very entertaining. You know,

00:09:56 --> 00:09:57 it could have been a bit of space debris

00:09:58 --> 00:10:00 falling through the atmosphere and almost be

00:10:00 --> 00:10:02 friendly fire. But again, that would have

00:10:02 --> 00:10:04 created a very bright fireball that people

00:10:04 --> 00:10:05 would have seen. So I think we can rule that

00:10:05 --> 00:10:07 out as well. And the thing that to me

00:10:08 --> 00:10:11 tells the story here and will point me in a

00:10:11 --> 00:10:12 direction of investigation is in his

00:10:12 --> 00:10:15 interview, um, Dr. Melville Smith

00:10:15 --> 00:10:18 says a truck went past. Five or ten seconds

00:10:18 --> 00:10:20 later, there was an enormous explosion. Now,

00:10:20 --> 00:10:22 I've been hit by bits of gravel falling off

00:10:22 --> 00:10:24 trucks before and had my windscreen damaged.

00:10:24 --> 00:10:26 Yep. Quite possible that this was a rock that

00:10:26 --> 00:10:29 fell off that truck that went past, or that

00:10:29 --> 00:10:31 the truck kicked up a bit of rock from the

00:10:31 --> 00:10:32 surface of the road that bounced along the

00:10:32 --> 00:10:35 road and hit the windscreen. I still

00:10:35 --> 00:10:38 find it hard to see how that would have

00:10:38 --> 00:10:40 generated heat from the thing that hit the

00:10:40 --> 00:10:42 windscreen that will cause a bit of melting.

00:10:42 --> 00:10:44 Even though it's been really hot there, the

00:10:44 --> 00:10:46 road surface could have been hot. You still

00:10:46 --> 00:10:48 don't expect the surface of the road to be

00:10:48 --> 00:10:51 hot enough to melt glass. But the

00:10:51 --> 00:10:53 kinetic energy of an impact, if you've got a

00:10:53 --> 00:10:55 more massive impactor coming in a bit more

00:10:55 --> 00:10:57 slowly, you still can put a lot of energy in.

00:10:57 --> 00:10:59 And it may well just be that what they're

00:10:59 --> 00:11:02 mistaking for melting is actually this

00:11:02 --> 00:11:04 deformation, this crater in the windscreen,

00:11:04 --> 00:11:06 with all of the material in the windscreen

00:11:06 --> 00:11:08 that is designed to stop your windscreen

00:11:08 --> 00:11:10 shattering. And that's done a really good

00:11:10 --> 00:11:11 job. I know when I've had cracks in my

00:11:11 --> 00:11:13 windscreen, I'm always surprised how you get

00:11:13 --> 00:11:15 a break but it doesn't shatter, doesn't

00:11:15 --> 00:11:18 create a whole windscreen. Modern windscreens

00:11:18 --> 00:11:20 are designed to be like this multi layer

00:11:20 --> 00:11:22 thing that stops them doing that. And I'm

00:11:22 --> 00:11:25 wondering if what they think looked as signs

00:11:25 --> 00:11:27 of melting was actually the structure of the

00:11:27 --> 00:11:29 wind windscreen behaving as it's expected to,

00:11:29 --> 00:11:32 with a bigger impact. And um, because this is

00:11:32 --> 00:11:33 substantial, I mean it's bigger than some of

00:11:33 --> 00:11:35 the pictures of hail damage I saw over the

00:11:35 --> 00:11:37 weekend, for example. And it's bigger than

00:11:37 --> 00:11:39 the usual chip you see kicked up off the

00:11:39 --> 00:11:42 road. It's at a size that people might not

00:11:42 --> 00:11:44 expect it to look like that. So my take on

00:11:44 --> 00:11:47 this one is very confident it's not a rock

00:11:47 --> 00:11:48 from space, but it might have been a rock

00:11:48 --> 00:11:49 from truck.

00:11:49 --> 00:11:52 Andrew Dunkley: Yes, well, the timing sounds about right. And

00:11:52 --> 00:11:55 um, yeah, good picture of you on the ABC

00:11:55 --> 00:11:56 story on the website too, by the way.

00:11:57 --> 00:11:59 Jonti Horner: Yeah, back when I was younger and slimmer.

00:11:59 --> 00:12:01 Andrew Dunkley: Yeah, they generally use those photos for us.

00:12:01 --> 00:12:04 It's very nice. But yeah, it

00:12:04 --> 00:12:07 reminds me once when um, we, we had a brand

00:12:07 --> 00:12:09 new car and we decided to take it for a run

00:12:09 --> 00:12:12 and we were approaching roadworks and we were

00:12:12 --> 00:12:14 teaching our son to drive at the time. So

00:12:14 --> 00:12:17 he's hammering along at the minimum,

00:12:17 --> 00:12:20 you know, maximum, minimum speed of a, ah, a

00:12:20 --> 00:12:23 learner. And I told him to hit the brakes

00:12:23 --> 00:12:25 because I didn't want to hit that road work

00:12:25 --> 00:12:27 when a truck approached and that's exactly

00:12:27 --> 00:12:30 what happened. We got showered in gravel.

00:12:30 --> 00:12:33 That brand new car had so much,

00:12:33 --> 00:12:35 you know, chipping on the front. We were

00:12:35 --> 00:12:36 very, very upset.

00:12:37 --> 00:12:39 Jonti Horner: To say it's shocking. I mean, one of the good

00:12:39 --> 00:12:41 things is, and it's not often that you can

00:12:41 --> 00:12:44 readily praise insurance companies, but I got

00:12:44 --> 00:12:47 a big chip on my windscreen at the turn of

00:12:47 --> 00:12:50 the year last year and um, got in touch with

00:12:50 --> 00:12:52 my insurance company and they soldered a

00:12:52 --> 00:12:55 windscreen replacement free of charge without

00:12:55 --> 00:12:57 it impacting my excess or anything like that.

00:12:57 --> 00:12:58 Now, well, I guess it's not free of charge

00:12:58 --> 00:13:00 because I'm paying the insurance premiums.

00:13:00 --> 00:13:02 But you know, it didn't impact my insurance

00:13:02 --> 00:13:05 rates, it didn't cause an excess. And I'm

00:13:05 --> 00:13:06 guessing that's because if you don't fix

00:13:06 --> 00:13:08 that, uh, it can become a much bigger problem

00:13:08 --> 00:13:10 and cause them a much bigger accident. So

00:13:10 --> 00:13:11 from their point of view, it's a very

00:13:11 --> 00:13:14 valuable investment. But it does mean that

00:13:14 --> 00:13:16 when we get these kind of events, we can get

00:13:16 --> 00:13:18 our windscreens fixed fairly easily and

00:13:18 --> 00:13:20 probably means that the trucks that are

00:13:20 --> 00:13:21 driving around shedding their loads get off A

00:13:21 --> 00:13:23 little bit scot free compared to having

00:13:23 --> 00:13:25 people chasing them down to pay for repairs.

00:13:25 --> 00:13:28 Andrew Dunkley: Yes, yes indeed. Okay,

00:13:28 --> 00:13:31 so probably not a meteorite, but probably

00:13:31 --> 00:13:32 a rock. Um.

00:13:35 --> 00:13:36 Jonti Horner: Roger, you're allowed to clear also.

00:13:37 --> 00:13:40 Andrew Dunkley: Space nuts to another event that uh,

00:13:40 --> 00:13:42 happened over uh, Victoria, New South Wales

00:13:43 --> 00:13:46 and the act, which, which are next door

00:13:46 --> 00:13:48 to each other, a fireball, um,

00:13:49 --> 00:13:51 as recently as yesterday as we

00:13:51 --> 00:13:52 speak.

00:13:52 --> 00:13:55 Jonti Horner: Yes. So this is very much breaking news. So

00:13:55 --> 00:13:57 I'm aware this doesn't air immediately. So

00:13:57 --> 00:13:59 this was a fireball that was seen on Sunday

00:13:59 --> 00:14:02 2nd November, which as we're recording at

00:14:02 --> 00:14:04 the minute, this was actually about 18 hours

00:14:04 --> 00:14:07 ago from now, roughly. And so that means

00:14:07 --> 00:14:10 information's still coming in. It was at uh,

00:14:10 --> 00:14:13 just about 20 to 5 in the evening,

00:14:13 --> 00:14:16 which means it was broad daylight. So this is

00:14:16 --> 00:14:18 a daylight fireball. And to me that's always

00:14:18 --> 00:14:21 a really exciting flag that this could be a

00:14:21 --> 00:14:23 bigger event because to be bright enough to

00:14:23 --> 00:14:25 be seen in broad daylight, and particularly

00:14:25 --> 00:14:27 to be bright enough to be seen widely in

00:14:27 --> 00:14:29 broad daylight by the general public means

00:14:29 --> 00:14:31 that this was a fairly substantial thing

00:14:31 --> 00:14:33 coming into the atmosphere. There are

00:14:33 --> 00:14:35 observations of this in New South Wales, in

00:14:35 --> 00:14:38 the act, the Australian Capital Territory

00:14:38 --> 00:14:41 and down into Victoria. Um, it's also

00:14:41 --> 00:14:43 a sonic boom and rumbles have been heard

00:14:43 --> 00:14:46 across Victoria recorded on seismograph

00:14:46 --> 00:14:49 in Nurbuchen in eastern Victoria.

00:14:50 --> 00:14:52 So it kind of sounds really promising from

00:14:52 --> 00:14:54 the point of view of something that is big

00:14:54 --> 00:14:56 enough to potentially drop a meteorite.

00:14:56 --> 00:14:58 There's a lot of good footage popping up on

00:14:58 --> 00:15:00 Facebook groups like the Australian Meteor

00:15:00 --> 00:15:03 Reports Facebook group. And the

00:15:03 --> 00:15:05 one thing that gives me a little bit of

00:15:05 --> 00:15:06 caution about something making it to the

00:15:06 --> 00:15:09 ground here is on some of those videos I've

00:15:09 --> 00:15:11 seen, this single looks like it was a very

00:15:11 --> 00:15:13 fast moving object. Now

00:15:13 --> 00:15:16 typically really fast moving things

00:15:16 --> 00:15:18 coming into the atmosphere have a lower

00:15:18 --> 00:15:20 likelihood of leaving anything to make it to

00:15:20 --> 00:15:22 the ground. Couple of reasons for that.

00:15:22 --> 00:15:25 Firstly, they tend to detonate higher up in

00:15:25 --> 00:15:27 the atmosphere and ah, more things get

00:15:27 --> 00:15:29 destroyed. But the other thing which I think

00:15:29 --> 00:15:31 is more to the point is things that come in

00:15:31 --> 00:15:34 really, really fast are typically moving on

00:15:34 --> 00:15:36 more comet like orbits and asteroid like

00:15:36 --> 00:15:39 orbits and therefore are more likely to be

00:15:39 --> 00:15:41 cometary material than asteroidal material,

00:15:41 --> 00:15:43 which means they're likely to be more

00:15:43 --> 00:15:45 friable, more fragile, more dust and

00:15:45 --> 00:15:48 ice rather than rock and metal. And that

00:15:48 --> 00:15:50 means that uh, when you see something coming

00:15:50 --> 00:15:51 in at really high speed, like some of these

00:15:51 --> 00:15:54 videos seem to show, that possibly

00:15:54 --> 00:15:56 means that there is a lower chance of

00:15:56 --> 00:15:59 something surviving to the surface. Doesn't

00:15:59 --> 00:16:02 mean that there won't be a meteorite found

00:16:02 --> 00:16:04 from this. Particularly because this, like I

00:16:04 --> 00:16:06 said, was bright enough to see in broad

00:16:06 --> 00:16:08 daylight and bright enough to be quite widely

00:16:08 --> 00:16:11 observed. The fact that the explosion, the

00:16:11 --> 00:16:13 terminal detonation, the air burst happened

00:16:13 --> 00:16:15 low enough for people to hear the sonic booms

00:16:15 --> 00:16:17 and for it to pick up on seismographs, all of

00:16:17 --> 00:16:19 these things are kind of things that we'd

00:16:19 --> 00:16:21 look for to say this is a promising event.

00:16:22 --> 00:16:23 The one thing that's giving me some caution

00:16:23 --> 00:16:26 is a very high speed. So this is very much a

00:16:26 --> 00:16:28 developing story. It might be that by the

00:16:28 --> 00:16:31 time people listen to this episode, they can

00:16:31 --> 00:16:32 go online and have a look and there'll be

00:16:32 --> 00:16:35 more information available. I'm honestly

00:16:35 --> 00:16:36 quite surprised that there's not been more

00:16:36 --> 00:16:38 media interest in this this morning. Usually

00:16:38 --> 00:16:40 when there's a bright event like this,

00:16:40 --> 00:16:42 journalists are ringing up and saying, what

00:16:42 --> 00:16:44 do you think? And what's happened? Yeah, so

00:16:44 --> 00:16:46 it may be a little bit of a slow burn, but

00:16:46 --> 00:16:48 it'll be interesting to see what develops on

00:16:48 --> 00:16:50 this in the next week or two. Maybe that

00:16:50 --> 00:16:52 nothing had always found, but it could be yet

00:16:52 --> 00:16:53 another rock dropping to the surface of

00:16:53 --> 00:16:55 Australia to give us something to study.

00:16:55 --> 00:16:58 Andrew Dunkley: Yeah, indeed. Yeah, yeah. Um, I've never

00:16:58 --> 00:17:00 seen one myself, but we've, we've had a few

00:17:00 --> 00:17:03 over the years, um, crossing the. The

00:17:03 --> 00:17:06 sky in Dubbo. One particular daytime

00:17:06 --> 00:17:09 one that someone filmed many, many years ago.

00:17:09 --> 00:17:11 And, uh, yeah, quite spectacular.

00:17:12 --> 00:17:14 Okay, uh, this is Space Nuts with

00:17:14 --> 00:17:17 Andrew Dunkley and John de Horner.

00:17:21 --> 00:17:22 Jonti Horner: Space Nuts.

00:17:22 --> 00:17:25 Andrew Dunkley: Uh, now this next story takes, um,

00:17:26 --> 00:17:28 us back to 3I Atlas, the, um,

00:17:29 --> 00:17:31 exo comet, I

00:17:31 --> 00:17:34 suppose, um, that's currently moving through

00:17:34 --> 00:17:37 our solar system. Uh, the reason it's

00:17:37 --> 00:17:39 sort of gained more traction is because

00:17:39 --> 00:17:42 things have changed and it's

00:17:42 --> 00:17:44 doing weird things. And of course, that's

00:17:44 --> 00:17:46 brought out the popular press and a few of

00:17:46 --> 00:17:48 those other comments that we're not going to

00:17:48 --> 00:17:50 talk about, but, um, bit of chatter on

00:17:50 --> 00:17:52 Facebook through the Space Nuts podcast

00:17:52 --> 00:17:55 group. Uh, what's happening with 3i

00:17:55 --> 00:17:55 Atlas?

00:17:57 --> 00:18:00 Jonti Horner: Well, the latest update is that it got a lot

00:18:00 --> 00:18:02 of coverage last week. Not really because

00:18:02 --> 00:18:04 anything special was happening, but because

00:18:04 --> 00:18:06 last week was the point at which Comet Atlas

00:18:06 --> 00:18:08 went through perihelion. Yeah, so that was

00:18:08 --> 00:18:09 the time it was closest to the sun.

00:18:09 --> 00:18:11 Perihelion was on about 30 October,

00:18:12 --> 00:18:15 so people are obviously interested. Um, I see

00:18:15 --> 00:18:17 the astronomer who Shall Not Be Named and

00:18:17 --> 00:18:19 they'll call him Voldemort for now, has come

00:18:19 --> 00:18:21 out with new stories saying that this Thing

00:18:21 --> 00:18:23 is changing direction and the aliens are

00:18:23 --> 00:18:25 definitely invading and rocket engines have

00:18:25 --> 00:18:28 kicked off. And, um, all this stuff,

00:18:28 --> 00:18:30 um, and it clearly isn't, you know, we are

00:18:30 --> 00:18:31 safe, we're not going to be invaded by

00:18:31 --> 00:18:33 aliens. You don't have to worry and protect

00:18:33 --> 00:18:35 yourself and buy some wine, Cokes or whatever

00:18:35 --> 00:18:38 you need to do. Um, does open up the question

00:18:38 --> 00:18:40 at what point this guy lost his credibility

00:18:40 --> 00:18:42 with the scientific community. The best part

00:18:42 --> 00:18:44 of a decade ago. But I wonder at what point

00:18:45 --> 00:18:47 the Boy who Cried Wolf syndrome will kick in

00:18:47 --> 00:18:49 to such an extent to overwhelm the Harvard

00:18:49 --> 00:18:52 affiliation and that the stories this

00:18:52 --> 00:18:54 guy puts out will stop getting oxygen. That's

00:18:54 --> 00:18:56 going to be an interesting study in the,

00:18:57 --> 00:18:59 um, I guess the scientific literacy of

00:18:59 --> 00:19:01 journalists at the lowest common denominator

00:19:01 --> 00:19:03 publications. That might be the way I put it,

00:19:04 --> 00:19:05 but it is definitely not aliens. But what is

00:19:05 --> 00:19:08 happening with Comet 3i Atlas is it's giving

00:19:08 --> 00:19:11 us this unprecedented window into the

00:19:11 --> 00:19:12 behavior of a comet that formed around

00:19:12 --> 00:19:15 another star. It's also a comet that's coming

00:19:15 --> 00:19:17 in and traveling through the solar system at

00:19:17 --> 00:19:19 a higher speed than typical comets do. And

00:19:19 --> 00:19:20 that's of course, how we know it's from

00:19:20 --> 00:19:23 another star. What that means, though, is

00:19:23 --> 00:19:26 that, uh, the typical process by which

00:19:26 --> 00:19:29 comets do their thing will happen

00:19:29 --> 00:19:30 in a slightly different way for this object,

00:19:30 --> 00:19:32 naturally, because it's coming through

00:19:32 --> 00:19:34 quicker. So things happen at an accelerated

00:19:34 --> 00:19:37 rate. And that might be what's happening.

00:19:37 --> 00:19:39 That ties into a paper that's just been

00:19:39 --> 00:19:41 published that you can read on the archive,

00:19:41 --> 00:19:43 the preprint server that we as astronomers

00:19:43 --> 00:19:46 use to spread the word of our work and

00:19:46 --> 00:19:48 circumvent the exorbitant prices that

00:19:48 --> 00:19:50 journals charge for you to read. Then we put

00:19:50 --> 00:19:52 all our papers on Arxiv as well and say,

00:19:52 --> 00:19:54 don't pay the journal, read it for free here,

00:19:54 --> 00:19:57 because we're nice like that. Um, this paper

00:19:57 --> 00:20:00 has been looking at the light curve of this

00:20:00 --> 00:20:02 comet, so how it's brightening over time.

00:20:02 --> 00:20:05 And what it's found is that, ah3i Atlas has

00:20:05 --> 00:20:08 been brightening faster than typical OC cloud

00:20:08 --> 00:20:10 comets do at this distance from the sun.

00:20:11 --> 00:20:13 So when you've got a comet coming in from the

00:20:13 --> 00:20:16 sun, it brightens in

00:20:16 --> 00:20:18 a slightly predictable rate. And the reason I

00:20:18 --> 00:20:21 say slightly predictable rate is, uh, there's

00:20:21 --> 00:20:23 a famous quote from a comet astronomer called

00:20:23 --> 00:20:25 David Levy that says comets are like cats.

00:20:26 --> 00:20:28 They have tails and they do whatever the hell

00:20:28 --> 00:20:30 they want. And there's a truth in that. So

00:20:30 --> 00:20:33 what we tend to do is when we first find a

00:20:33 --> 00:20:36 comet, we can work out Fairly quickly, what

00:20:36 --> 00:20:39 orbit it's moving on around the sun to some

00:20:39 --> 00:20:41 degree, how far away it is from the sun and

00:20:41 --> 00:20:43 how quickly it's moving. And, um, by knowing

00:20:43 --> 00:20:45 how far away it is and how bright it is, when

00:20:45 --> 00:20:47 we find it, we can work out

00:20:48 --> 00:20:50 an absolute magnitude for it, which is a

00:20:50 --> 00:20:52 quantity that characterizes whether it's a

00:20:52 --> 00:20:54 big, bright comet or a small, faint comet.

00:20:55 --> 00:20:57 And we can use that and, um, the orbit it's

00:20:57 --> 00:20:59 going around the sun to make a first

00:20:59 --> 00:21:00 prediction of how the comet will brighten or

00:21:00 --> 00:21:03 fade. Then, as we observe it over a little

00:21:03 --> 00:21:06 bit of time, we can characterize how its

00:21:06 --> 00:21:08 activity is changing and work out not only

00:21:08 --> 00:21:10 whether it's a big comet or a small comet,

00:21:10 --> 00:21:12 but whether it's an active comet or whether

00:21:12 --> 00:21:15 it's a very quiescent comet. So whether it's

00:21:15 --> 00:21:18 brightening rapidly or brightening slowly

00:21:18 --> 00:21:20 for a comet of that size. And over time, this

00:21:20 --> 00:21:22 allows people to predict the brightness of

00:21:22 --> 00:21:25 the comet going forward. And assuming the

00:21:25 --> 00:21:27 comet doesn't do anything unusual, like

00:21:27 --> 00:21:29 fragmenting or having an outburst or

00:21:29 --> 00:21:32 something like this, we can get a fairly good

00:21:32 --> 00:21:35 handle several months ahead of time, of how

00:21:35 --> 00:21:37 bright the comet's going to be with a certain

00:21:37 --> 00:21:39 degree of uncertainty. And so we've got a

00:21:39 --> 00:21:42 fairly good feeling for how a comet coming in

00:21:42 --> 00:21:44 from the Oort Cloud that is about the size of

00:21:44 --> 00:21:46 Comet ATLAS should brighten.

00:21:47 --> 00:21:48 Now, some comets brighten a bit quicker

00:21:48 --> 00:21:50 because they're more active. Some brighten a

00:21:50 --> 00:21:53 bit slower. What's happened with Comet ATLAS

00:21:53 --> 00:21:55 is it started to brighten significantly

00:21:55 --> 00:21:58 quicker than we'd expect a typical Oort cloud

00:21:58 --> 00:22:00 comet to brighten at the same distance from

00:22:00 --> 00:22:02 the Sun. And that's what this paper's all

00:22:02 --> 00:22:04 about. Basically, the comet's brightening

00:22:04 --> 00:22:06 unusually quickly. Now, there's a

00:22:06 --> 00:22:08 variety of possible explanations for that,

00:22:08 --> 00:22:11 and we won't know which answer is true until

00:22:11 --> 00:22:13 we do more study. The most common reason

00:22:13 --> 00:22:16 for a comet to brighten unusually quickly

00:22:16 --> 00:22:18 is often linked to the comet's head becoming

00:22:18 --> 00:22:20 a bit more diffuse because it's a comet

00:22:20 --> 00:22:23 fragmentation event. So the comet's

00:22:23 --> 00:22:25 falling apart. You release a lot of

00:22:25 --> 00:22:27 dust as the comet falls apart, but you also

00:22:27 --> 00:22:29 increase the surface area exposed to

00:22:29 --> 00:22:31 sunlight, which means you increase the

00:22:31 --> 00:22:33 activity. And the analogy here will be the

00:22:33 --> 00:22:34 difference. If you've ever had the

00:22:34 --> 00:22:36 effervescent tablets you put in water and you

00:22:36 --> 00:22:39 let them dissolve. If you get two of them and

00:22:39 --> 00:22:41 you put one in a glass of water fully intact,

00:22:41 --> 00:22:43 and you crumble the other one up and drop in

00:22:43 --> 00:22:45 the crumbled one, the crumbled one reacts

00:22:45 --> 00:22:47 much quicker, and it foams up really quickly.

00:22:48 --> 00:22:49 The solid one takes a while to go.

00:22:51 --> 00:22:53 That could be the case. We'll only know if we

00:22:53 --> 00:22:54 observe for a little bit of time. And that

00:22:54 --> 00:22:56 wouldn't necessarily be that unsurprising.

00:22:56 --> 00:22:58 There is a suspicion that this comet, 3i

00:22:58 --> 00:23:01 atlas never actually got close enough to its

00:23:01 --> 00:23:03 parent star to be active as a comet. So it

00:23:03 --> 00:23:05 will be more equivalent to what we call the

00:23:05 --> 00:23:07 new Oort cloud comets coming through for the

00:23:07 --> 00:23:09 very first time, rather than one that's had

00:23:09 --> 00:23:12 multiple perihelion passages. And, um, we do

00:23:12 --> 00:23:14 know that new comets have a tendency to

00:23:14 --> 00:23:16 fragment more often than older comets that

00:23:16 --> 00:23:18 have been more baked in, essentially. So

00:23:18 --> 00:23:19 that's one possible explanation.

00:23:19 --> 00:23:21 But I think another one that's really

00:23:21 --> 00:23:23 interesting and would probably fit quite well

00:23:23 --> 00:23:26 is that our models of cometary

00:23:26 --> 00:23:29 activity have built within them. Though, uh,

00:23:29 --> 00:23:31 we don't normally think about it, the time at

00:23:31 --> 00:23:34 which activity driven by different ices

00:23:34 --> 00:23:36 kicks in. So as the comet gets closer to the

00:23:36 --> 00:23:39 sun and it gets hotter, different ices on

00:23:39 --> 00:23:41 the surface will reach the temperature where

00:23:41 --> 00:23:43 they can no longer be ices, and they turn

00:23:43 --> 00:23:45 from ice to gas in a process called

00:23:45 --> 00:23:46 sublimation. And that's what drives the

00:23:46 --> 00:23:49 activity of the comet. And as a comet heats

00:23:49 --> 00:23:51 up, different ices turn on, effectively.

00:23:52 --> 00:23:55 Now, when you're far from the sun, water ice

00:23:55 --> 00:23:57 is really cold and stays as water ice. But

00:23:57 --> 00:24:00 other volatile materials like carbon monoxide

00:24:00 --> 00:24:02 and carbon dioxide are, uh, what drive the

00:24:02 --> 00:24:04 activity of a comet when it's further from

00:24:04 --> 00:24:07 the Sun. Now, as it comes in closer, it

00:24:07 --> 00:24:09 heats up and water turns on. And certainly

00:24:09 --> 00:24:11 within a few astronomical units of the sun.

00:24:11 --> 00:24:13 Water is usually the dominant driving factor

00:24:13 --> 00:24:16 of comet reactivity. With Comet

00:24:16 --> 00:24:19 atlas, this brightening is happening

00:24:19 --> 00:24:21 interior to the distance where most comets

00:24:21 --> 00:24:23 would have turned on their water emission.

00:24:23 --> 00:24:26 But Comet ATLAS is coming in quicker, and

00:24:26 --> 00:24:29 so therefore, it is heating up

00:24:29 --> 00:24:31 due to the radiation from the Sun. But as

00:24:31 --> 00:24:34 it's coming in quicker, maybe it was closer

00:24:34 --> 00:24:36 to the sun by the time that the heat from the

00:24:36 --> 00:24:39 sun got to be enough to penetrate the surface

00:24:39 --> 00:24:41 material and start kicking on the water

00:24:41 --> 00:24:43 activity. But then that heating is happening

00:24:43 --> 00:24:45 really quickly because the distance to the

00:24:45 --> 00:24:48 sun is dropping quite fast. And so therefore,

00:24:48 --> 00:24:49 you've had this spike in temperature and

00:24:49 --> 00:24:52 therefore a spike in activity as the water

00:24:52 --> 00:24:55 activity is turned on, not so much as a

00:24:55 --> 00:24:57 trickle, but as a flood. And that ties in

00:24:57 --> 00:24:59 actually quite nicely to some of the recent

00:24:59 --> 00:25:01 stories in the last few weeks about the water

00:25:01 --> 00:25:03 vapor, uh, and the water being emitted from

00:25:03 --> 00:25:06 the comet I saw some article about the comet

00:25:06 --> 00:25:09 emitting a jet of water like a firehose. So

00:25:09 --> 00:25:11 this is one of those narratives that seems to

00:25:11 --> 00:25:13 fit together really, really well. And it

00:25:13 --> 00:25:14 could just be that the high speed of the

00:25:14 --> 00:25:16 comet means that it got closer in before the

00:25:16 --> 00:25:19 water turned on. And now it's catching up for

00:25:19 --> 00:25:22 lost time. What this means for the future is

00:25:22 --> 00:25:24 that, in all honesty, we are

00:25:24 --> 00:25:26 less confident in predicting the future

00:25:26 --> 00:25:28 brightness of the comet than we normally

00:25:28 --> 00:25:30 would be. Because it's all this cometary

00:25:30 --> 00:25:32 activity going on. It's effectively having a

00:25:32 --> 00:25:35 bit of an outburst. When we were talking

00:25:35 --> 00:25:36 about it months ago, we always said it would

00:25:36 --> 00:25:38 never get brighter than about magnitude 11,

00:25:38 --> 00:25:41 magnitude 12. There's a chance it might get a

00:25:41 --> 00:25:42 little bit brighter than that now. But it's

00:25:42 --> 00:25:44 really hard to model. We don't know whether

00:25:45 --> 00:25:46 the comet will brighten further than

00:25:46 --> 00:25:49 expected, brighten really rapidly, go back to

00:25:49 --> 00:25:52 behaving as normal. It might fade away

00:25:52 --> 00:25:54 because suddenly it's had this outburst. It's

00:25:54 --> 00:25:56 clogged itself up. It might even go out

00:25:56 --> 00:25:58 relatively quickly like a bit of a snuff

00:25:58 --> 00:26:00 torch if it has fully fragmented and

00:26:00 --> 00:26:03 disintegrated. And we saw that with the great

00:26:03 --> 00:26:06 comet earlier this year, Comet Atlas, which

00:26:06 --> 00:26:07 was really bright and spectacular. And then

00:26:07 --> 00:26:09 became the headless comet because its head

00:26:09 --> 00:26:12 just totally disintegrated. And all you were

00:26:12 --> 00:26:14 left was this tail gradually drifting through

00:26:14 --> 00:26:17 space with no comet to call its own. Yeah, so

00:26:17 --> 00:26:19 we just, honestly, we just don't, um, know

00:26:19 --> 00:26:22 There's a lot more to learn. And, yeah, this

00:26:22 --> 00:26:24 is getting a lot of hyperbolic stories

00:26:25 --> 00:26:27 about it and people arguing that it's

00:26:27 --> 00:26:29 actually the mass driver engine that's turned

00:26:29 --> 00:26:31 on as it will reroute itself to the Earth.

00:26:31 --> 00:26:33 Courtesy Harvard astronomer of doom.

00:26:34 --> 00:26:36 But in reality, this is why these objects are

00:26:36 --> 00:26:38 so exciting, because they give us a window

00:26:38 --> 00:26:40 into comets with different compositions that

00:26:40 --> 00:26:42 formed around different stars. And also how

00:26:42 --> 00:26:44 comets behave at higher speed. You know,

00:26:45 --> 00:26:46 this is why it's cool.

00:26:46 --> 00:26:49 Andrew Dunkley: Yeah. Uh, I must say I'm surprised that this

00:26:49 --> 00:26:52 one's receiving so much attention. But I

00:26:52 --> 00:26:54 shouldn't be surprised because it is a little

00:26:54 --> 00:26:56 bit different to most.

00:26:56 --> 00:26:59 And, um, being an ex. Extra, um,

00:27:00 --> 00:27:03 solar comet, um,

00:27:03 --> 00:27:05 it just, Just makes it that much more

00:27:05 --> 00:27:07 interesting. So, yeah, um, lots to learn,

00:27:07 --> 00:27:10 really. Uh, so, yeah, this one, uh, will no

00:27:10 --> 00:27:13 doubt, uh, be getting some attention for some

00:27:13 --> 00:27:16 time to come. Um, would be a pity if

00:27:16 --> 00:27:17 it kind of, you know,

00:27:19 --> 00:27:21 lost itself in our solar

00:27:21 --> 00:27:24 system. But, um, that's just the way it goes

00:27:24 --> 00:27:24 sometimes.

00:27:26 --> 00:27:26 Jonti Horner: Absolutely.

00:27:26 --> 00:27:27 Andrew Dunkley: Well, there it is.

00:27:28 --> 00:27:28 Jonti Horner: Yeah.

00:27:29 --> 00:27:31 I was going to say, while we're on the topic

00:27:31 --> 00:27:32 of comets, I should just flag up to everyone,

00:27:32 --> 00:27:34 particularly the Northern Hemisphere people,

00:27:34 --> 00:27:37 but also us in the Southern Hemisphere, a

00:27:37 --> 00:27:39 tiny little bit. Comet Lemon, which is

00:27:39 --> 00:27:41 getting a lot of media coverage, is at its

00:27:41 --> 00:27:44 brightest pretty much bang at the minute.

00:27:44 --> 00:27:46 It's about magnitude 4.3, which means

00:27:46 --> 00:27:47 technically it's visible to the naked eye.

00:27:47 --> 00:27:50 But in reality, because comets are diffuse

00:27:50 --> 00:27:52 objects, it'll be a very hard spot unless

00:27:52 --> 00:27:54 you're somewhere incredibly dark. But it is

00:27:54 --> 00:27:57 very photogenic comet. It is most visible to

00:27:57 --> 00:27:59 people in the Northern Hemisphere. For those

00:27:59 --> 00:28:02 of us in Australia, it's basically lost in

00:28:02 --> 00:28:04 the glare of twilight, even though it's at a

00:28:04 --> 00:28:06 declination where it could be visible if it

00:28:06 --> 00:28:08 was in a dark sky. It's too near the sun in

00:28:08 --> 00:28:10 the sky. But these few days around now,

00:28:10 --> 00:28:12 the next week or so, it's the best chance

00:28:12 --> 00:28:15 we'll get to see it from Australia while it's

00:28:15 --> 00:28:17 bright. And, um, that'll be very low in the

00:28:17 --> 00:28:20 west after sunset, um, as the sky

00:28:20 --> 00:28:22 gets darker. Have a look on

00:28:22 --> 00:28:24 planetarium programs like Stellarium to find

00:28:24 --> 00:28:27 the location. But my memory is that, uh, the

00:28:27 --> 00:28:29 planet Mercury is going to be visible low to

00:28:29 --> 00:28:30 the west after sunset. And if you can find

00:28:30 --> 00:28:33 Mercury and you go to the right of Mercury,

00:28:33 --> 00:28:35 it's about the same height as Mercury on the

00:28:35 --> 00:28:38 7th or 8th of November. So worth

00:28:38 --> 00:28:41 looking at. It is not the best comet of the

00:28:41 --> 00:28:42 year. We already have that back in January,

00:28:42 --> 00:28:44 despite what some of the articles said. But

00:28:44 --> 00:28:45 if you do want to see a comet that's

00:28:46 --> 00:28:47 borderline bright enough to see the naked

00:28:47 --> 00:28:49 eye, that's your one. It should be quite good

00:28:49 --> 00:28:52 in binoculars and certainly for people doing

00:28:52 --> 00:28:54 astrophotography. Have a look online. Some of

00:28:54 --> 00:28:55 the photos of this thing are really

00:28:55 --> 00:28:57 spectacular. There's people who've done, um,

00:28:57 --> 00:28:59 yeah, pretty clever things imaging it with

00:28:59 --> 00:29:02 lovely foreground views like lakes or rocks

00:29:02 --> 00:29:04 or castles or whatever. So there's lovely

00:29:04 --> 00:29:07 images of this comet out there if you want to

00:29:07 --> 00:29:08 feast your eyes on what people who are

00:29:08 --> 00:29:09 talented photographers can do.

00:29:10 --> 00:29:13 Andrew Dunkley: Yes, very good. Uh, that's Three Eye, Three

00:29:13 --> 00:29:15 Eye Atlas. Uh, now, um,

00:29:16 --> 00:29:18 oh, and you can, you can read, uh, about

00:29:18 --> 00:29:21 that, uh, on, um, the archive website,

00:29:21 --> 00:29:22 as Jonti mentioned.

00:29:25 --> 00:29:25 Jonti Horner: Okay.

00:29:25 --> 00:29:27 Andrew Dunkley: We checked all four systems and being with a

00:29:27 --> 00:29:30 girl, space nats, uh, let's move on to

00:29:30 --> 00:29:33 this really interesting story. An enormous

00:29:33 --> 00:29:36 black hole has been found. But what's really

00:29:36 --> 00:29:39 interesting is the galaxy that it's in is

00:29:39 --> 00:29:42 tiny. And when I, when I read into the

00:29:42 --> 00:29:45 details of this Story. We're talking about a

00:29:45 --> 00:29:47 galaxy with very few stars,

00:29:48 --> 00:29:49 surprisingly few stars.

00:29:50 --> 00:29:52 Jonti Horner: And, um, this fascinated me reading it now. I

00:29:52 --> 00:29:54 always say, particularly when we're doing the

00:29:54 --> 00:29:56 questions, and we get lots of cosmology type

00:29:56 --> 00:29:58 questions. I'm not a cosmologist, I'm not a

00:29:58 --> 00:30:01 galactic type astronomer. Uh, my expertise

00:30:01 --> 00:30:03 and my focus is very much on the things

00:30:03 --> 00:30:05 closer to home. So I tend to try and pick

00:30:05 --> 00:30:07 stories where I can talk from a position of

00:30:07 --> 00:30:09 some authority rather than no authority, if

00:30:09 --> 00:30:12 that makes sense. But this story was so cool,

00:30:12 --> 00:30:14 I thought we had to include it, even if, um,

00:30:14 --> 00:30:16 it might be a little bit of the blind leading

00:30:16 --> 00:30:17 the blind in a way. But this is one of the

00:30:17 --> 00:30:19 Milky Way's satellite galaxies. And our

00:30:19 --> 00:30:22 galaxy has many, many satellites, from the

00:30:22 --> 00:30:24 incredibly large and bright, large and Small

00:30:24 --> 00:30:27 Magellanic Clouds, which we can see here in

00:30:27 --> 00:30:28 the Southern Hemisphere, really high in the

00:30:28 --> 00:30:31 sky at the minute, really spectacular, down

00:30:31 --> 00:30:33 to really, really tiny satellite galaxies

00:30:33 --> 00:30:36 that almost push our understanding of what it

00:30:36 --> 00:30:39 means to be a galaxy. And this galaxy

00:30:39 --> 00:30:41 is one such galaxy. It's what's described as

00:30:41 --> 00:30:44 an ultra faint dwarf galaxy. And there are

00:30:44 --> 00:30:47 likely an enormous number of these in space

00:30:47 --> 00:30:49 that we just don't find. I guess the analogy

00:30:49 --> 00:30:51 I'd use here is that if you go out and look

00:30:51 --> 00:30:53 at the stars in the night sky, the stars that

00:30:53 --> 00:30:55 you're seeing are very much the superstars of

00:30:55 --> 00:30:57 our galaxy. They're stars that are much more

00:30:57 --> 00:30:59 massive than the sun that we're seeing from

00:30:59 --> 00:31:02 great distances. The most common stars in

00:31:02 --> 00:31:05 the galaxy are the dim little red dwarfs like

00:31:05 --> 00:31:07 Proxima Centauri. And Proxima is fairly

00:31:07 --> 00:31:10 massive and fairly luminous for a red dwarf.

00:31:10 --> 00:31:12 It is the closest star to the solar system,

00:31:12 --> 00:31:14 and it's too fancy with the naked eye by a

00:31:14 --> 00:31:17 factor of 100 times. So there's lots and lots

00:31:17 --> 00:31:19 of very small, faint things that until we

00:31:19 --> 00:31:21 have telescopes, we couldn't find at all.

00:31:21 --> 00:31:23 There are always more small things than big

00:31:23 --> 00:31:26 things. So it seems likely that there are,

00:31:26 --> 00:31:28 uh, many, many, many faint,

00:31:28 --> 00:31:31 ultra faint dwarf galaxies that have simply

00:31:31 --> 00:31:33 not been discovered even in our local area,

00:31:33 --> 00:31:36 never mind at the far parts of the cosmos.

00:31:36 --> 00:31:38 When we talk about galaxies that are many

00:31:38 --> 00:31:40 hundreds of millions of light years away,

00:31:40 --> 00:31:41 we're only seeing the superstars. We're not

00:31:41 --> 00:31:44 seeing the little baby ones like this. The

00:31:44 --> 00:31:47 galaxy in the story here is called Segue one.

00:31:47 --> 00:31:50 And I must admit that I don't think I'd ever

00:31:50 --> 00:31:51 heard of this, or I'd only ever heard of it

00:31:51 --> 00:31:54 in passing before this story came out. It is

00:31:54 --> 00:31:57 really tiny and very Anonymous. It's about

00:31:57 --> 00:31:59 75 light years from the Earth.

00:32:00 --> 00:32:01 Like I say, it's one of our satellite

00:32:01 --> 00:32:03 galaxies. And, uh, our, uh, best

00:32:03 --> 00:32:05 observations. There's a photograph in the

00:32:05 --> 00:32:07 Space.com article which is fabulous. It says,

00:32:07 --> 00:32:09 you know, here's this dwarf galaxy with only

00:32:09 --> 00:32:11 a handful of stars, and I'm not sure where

00:32:11 --> 00:32:13 the galaxy is because there's so little in

00:32:13 --> 00:32:15 the photograph. That's what it's like. And so

00:32:15 --> 00:32:17 you're talking here of just a few hundred or

00:32:17 --> 00:32:20 a few thousand stars held together.

00:32:21 --> 00:32:23 Now, that's been a puzzle for galaxy

00:32:23 --> 00:32:25 astronomers for a long time, because so few

00:32:25 --> 00:32:28 stars have so little mass that the

00:32:28 --> 00:32:30 galaxy shouldn't hold itself together. The

00:32:30 --> 00:32:33 galaxy should have dispersed over time. And

00:32:33 --> 00:32:35 for a long time, the best explanation people

00:32:35 --> 00:32:37 have had for this is that these are kind of

00:32:37 --> 00:32:40 dark matter galaxies, that they've got a

00:32:40 --> 00:32:42 massive dark matter agglomerated as a big

00:32:42 --> 00:32:45 dark matter halo, giving you enough mass

00:32:45 --> 00:32:47 there that we can't see to provide enough

00:32:47 --> 00:32:49 gravity to hold this very small number of

00:32:49 --> 00:32:51 stars together to keep them kind of whizzing

00:32:51 --> 00:32:54 around one another. And that kind of makes

00:32:54 --> 00:32:57 sense. We know that a lot of galaxies have

00:32:57 --> 00:32:58 big amounts of dark matter. In fact, all

00:32:58 --> 00:33:01 galaxies do. So you could almost have dark

00:33:01 --> 00:33:02 matter galaxies where you've got a clump of

00:33:02 --> 00:33:04 dark matter with very few stars. That kind of

00:33:04 --> 00:33:07 made sense. But the new story

00:33:08 --> 00:33:10 comes from improved observations of this

00:33:10 --> 00:33:12 galaxy, coupled with some computational

00:33:12 --> 00:33:14 numerical orbital modeling. And what they've

00:33:14 --> 00:33:16 found is that the stars near the middle of

00:33:16 --> 00:33:19 Segue one are, uh, going round the middle

00:33:19 --> 00:33:21 really, really quickly. Now, that allows us

00:33:21 --> 00:33:24 to take a measurement of the mass that is

00:33:24 --> 00:33:26 closer to the middle of the galaxy than those

00:33:26 --> 00:33:29 stars are. So anything feels

00:33:29 --> 00:33:31 gravity from the things closer to the middle

00:33:31 --> 00:33:34 than they do fundamentally. So what this

00:33:34 --> 00:33:36 means is by observing those stars that are in

00:33:36 --> 00:33:38 the middle of this galaxy, seeing them move,

00:33:38 --> 00:33:41 we can weigh the very innermost parts of that

00:33:41 --> 00:33:44 galaxy. And, um, what that tells us is that

00:33:44 --> 00:33:46 there is about 450 times

00:33:46 --> 00:33:48 more mass in the middle of that galaxy than

00:33:48 --> 00:33:51 the mass of our sun that we cannot see.

00:33:51 --> 00:33:51 Andrew Dunkley: Yeah.

00:33:51 --> 00:33:54 Jonti Horner: Which makes this a black hole, and it makes

00:33:54 --> 00:33:57 this a supermassive black hole, albeit a

00:33:57 --> 00:33:59 relatively low mass supermassive black hole

00:33:59 --> 00:34:01 compared to the one in the middle of Milky

00:34:01 --> 00:34:04 Way. Now, that in itself is not hugely

00:34:04 --> 00:34:06 unexpected. Pretty much all big galaxies have

00:34:06 --> 00:34:08 supermassive black holes, but we've not

00:34:08 --> 00:34:10 really seen them in teeny, tiny little

00:34:10 --> 00:34:13 galaxies like this before. Even

00:34:13 --> 00:34:16 more so, we've not really seen cases where

00:34:16 --> 00:34:18 there are galaxies whose black hole is, is

00:34:18 --> 00:34:20 more than 10 times the mass of all of the

00:34:20 --> 00:34:23 stars we can see in that galaxy. Feels like a

00:34:23 --> 00:34:25 really kind of weird imbalance. The black

00:34:25 --> 00:34:27 hole is more massive than the galaxy around

00:34:27 --> 00:34:29 it seems to suggest there would have been

00:34:29 --> 00:34:31 enough material for. But it's

00:34:32 --> 00:34:34 really weird from a few reasons, but really

00:34:34 --> 00:34:36 cool in the same way in that it's suggesting

00:34:36 --> 00:34:38 that this galaxy is not held together by dark

00:34:38 --> 00:34:40 matter, it's held together by this

00:34:40 --> 00:34:43 supermassive black hole at the middle. That

00:34:43 --> 00:34:45 maybe gives us an insight into how other

00:34:45 --> 00:34:48 ultra faint dwarf galaxies behave. This is

00:34:48 --> 00:34:50 probably not alone suggesting that there

00:34:50 --> 00:34:52 could be a lot more of these supermassive

00:34:52 --> 00:34:54 black holes out there in the cosmos than we

00:34:54 --> 00:34:56 thought. It also possibly is a bit of a

00:34:56 --> 00:34:59 hint that segue one was once a more massive

00:34:59 --> 00:35:01 galaxy. You know, if you think about the

00:35:01 --> 00:35:03 idea of the mass of this supermassive black

00:35:03 --> 00:35:05 hole and think, well, what kind of galaxy

00:35:05 --> 00:35:08 would normally expect to have a mass massive

00:35:08 --> 00:35:10 black hole like that in its center? How many

00:35:10 --> 00:35:13 stars should it have had? Maybe Segue one was

00:35:13 --> 00:35:15 like that in the past, but because it's so

00:35:15 --> 00:35:18 close to the Milky Way, it has been

00:35:18 --> 00:35:20 continually stripped and denuded of its stars

00:35:20 --> 00:35:23 from the outside inwards by our galaxy,

00:35:23 --> 00:35:25 essentially playing Pac man and gobbling it

00:35:25 --> 00:35:27 up going nom nom, nom, essentially, which is

00:35:27 --> 00:35:29 how galaxies grow. Galaxies grow through

00:35:29 --> 00:35:31 cannibalizing their neighbors. And we see

00:35:31 --> 00:35:33 that to an extent even with our largest

00:35:33 --> 00:35:35 satellite galaxies which have been disrupted

00:35:35 --> 00:35:37 and devoured a bit by the Milky Way and will

00:35:37 --> 00:35:39 eventually be gone. So there's a lot in this,

00:35:39 --> 00:35:42 it is a really fascinating story, albeit one,

00:35:42 --> 00:35:44 like I say, where I'm much further from being

00:35:44 --> 00:35:46 an expert than a lot of the other stuff that

00:35:46 --> 00:35:48 we talk about. Um, but you can find more

00:35:48 --> 00:35:50 about it online. And it is just a really cool

00:35:50 --> 00:35:53 little story, you know, it may well totally

00:35:53 --> 00:35:54 revolutionize our understanding of how the

00:35:54 --> 00:35:56 smallest galaxies work.

00:35:56 --> 00:35:59 Andrew Dunkley: Yes, indeed. Um, I, I, you kind of took the

00:35:59 --> 00:36:01 question out of my mouth, but I wasn't

00:36:01 --> 00:36:03 thinking of a neighboring galaxy stripping

00:36:03 --> 00:36:06 the, the stars away from segue. I was

00:36:06 --> 00:36:08 thinking the black hole might be devouring

00:36:08 --> 00:36:10 the stars within galaxy, but.

00:36:11 --> 00:36:13 Jonti Horner: Uh, you'd probably get a bit of that as well

00:36:13 --> 00:36:16 because the thing with the black hole is

00:36:16 --> 00:36:18 that uh, its gravitational pull is exactly

00:36:18 --> 00:36:20 the same as, ah, a group of objects of the

00:36:20 --> 00:36:23 same mass would have. Um, so it doesn't

00:36:23 --> 00:36:24 really pull things in any harder than the

00:36:24 --> 00:36:27 material that was there beforehand. But if

00:36:27 --> 00:36:28 you've got a neighboring galaxy like the

00:36:28 --> 00:36:31 Milky Way stirring up and um, numbing

00:36:31 --> 00:36:33 on this galaxy. It will also stir up the

00:36:33 --> 00:36:36 orbits of the stars in that galaxy, making

00:36:36 --> 00:36:38 some of them sufficiently elongated that they

00:36:38 --> 00:36:40 could fall onto that central black hole. So

00:36:40 --> 00:36:42 it's likely that the process of the Milky Way

00:36:42 --> 00:36:45 eating this galaxy has also led to the black

00:36:45 --> 00:36:47 hole in the middle of it getting a bit of a

00:36:47 --> 00:36:50 feed as well. A bit like the, um, white dwarf

00:36:50 --> 00:36:52 we were talking about last week, getting fed

00:36:52 --> 00:36:54 asteroids by the planets going around it.

00:36:54 --> 00:36:54 Same kind of idea.

00:36:55 --> 00:36:57 Andrew Dunkley: Yeah. It sounds like these stars, uh, in

00:36:57 --> 00:36:59 segue, are like a school of fish being

00:36:59 --> 00:37:02 attacked from all sides by predators, and

00:37:02 --> 00:37:05 eventually they'll just all be gone. Uh,

00:37:05 --> 00:37:07 yeah, you can read all about that@space.com

00:37:07 --> 00:37:10 or, or you can look at the paper that was

00:37:10 --> 00:37:12 published in astrophysical journal letters.

00:37:15 --> 00:37:18 3, 2, 1.

00:37:18 --> 00:37:19 Space nuts.

00:37:20 --> 00:37:22 I think we've got time for one more quick

00:37:22 --> 00:37:25 yarn, Jonti. And this is a story

00:37:25 --> 00:37:28 that I find fascinating, uh, and certainly

00:37:28 --> 00:37:31 relates to, um, the history of Earth in many

00:37:31 --> 00:37:33 ways. Uh, life after an

00:37:33 --> 00:37:36 asteroid impact. Now, a big

00:37:36 --> 00:37:39 asteroid conking the Earth, uh, can

00:37:39 --> 00:37:41 have cataclysmic effects, as

00:37:41 --> 00:37:44 we've seen in our history. And the,

00:37:44 --> 00:37:47 um, geology certainly backs that up.

00:37:47 --> 00:37:50 But, um, you know, fast forward a few

00:37:50 --> 00:37:53 gazillion years or whatever the number is,

00:37:53 --> 00:37:56 uh, and life does return. Um,

00:37:57 --> 00:37:59 they've been looking into this effect,

00:37:59 --> 00:37:59 haven't they?

00:38:00 --> 00:38:02 Jonti Horner: Now, this is some lovely research that's come

00:38:02 --> 00:38:05 out of Finland, where there's a beautiful

00:38:05 --> 00:38:07 impact crater. And I will apologize for

00:38:07 --> 00:38:08 anybody listening who speaks a beautiful

00:38:08 --> 00:38:11 Finnish language. Um, but there's a beautiful

00:38:11 --> 00:38:13 impact crater, uh, in Finland called Lake

00:38:13 --> 00:38:16 Lapijavi, which is an impact

00:38:16 --> 00:38:19 basin about 23 kilometers across that was

00:38:19 --> 00:38:22 formed 78 million years ago. It's a

00:38:22 --> 00:38:24 fairly hefty impact. It's the kind of thing

00:38:24 --> 00:38:26 that would be a bit of a drama if you lived

00:38:26 --> 00:38:28 in that part of the world, but not large

00:38:28 --> 00:38:30 enough to cause a global mass extinction

00:38:30 --> 00:38:32 event. So this is nothing like the one that

00:38:32 --> 00:38:35 killed the dinosaurs 65, 66 million

00:38:35 --> 00:38:37 years ago. This is a bit smaller, a bit more

00:38:37 --> 00:38:40 run of the mill. Now, there's a vague rough

00:38:40 --> 00:38:43 rule of thumb for impacts that if an impact

00:38:43 --> 00:38:45 happens, the size of the crater is about 19

00:38:45 --> 00:38:48 times the diameter of the impactor. So that

00:38:48 --> 00:38:50 tells me that the rock that hit to create

00:38:50 --> 00:38:53 this crater was probably a bit more than a

00:38:53 --> 00:38:56 kilometer across. So it's fairly substantial.

00:38:56 --> 00:38:59 That's the kind of impact that statisticians

00:38:59 --> 00:39:00 would argue would kill about a quarter of the

00:39:00 --> 00:39:03 world's human population. So not an

00:39:03 --> 00:39:05 extinction event, but a very bad day.

00:39:06 --> 00:39:09 The Team that have looked into this were

00:39:09 --> 00:39:11 really interested in how quickly

00:39:11 --> 00:39:14 life can reestablish itself in the

00:39:14 --> 00:39:16 rocks left behind from an impact. Because you

00:39:16 --> 00:39:19 have an impact happen, it superheats

00:39:19 --> 00:39:21 and sterilize the rocks. This would have

00:39:21 --> 00:39:23 sterilized the rocks in the impact site by

00:39:23 --> 00:39:25 heating them to more than 2 degrees C.

00:39:25 --> 00:39:28 That's 3 Fahrenheit for the American.

00:39:29 --> 00:39:31 Enough to kind of really sterilize the place

00:39:31 --> 00:39:34 it hit. It would have also, though, caused

00:39:34 --> 00:39:36 huge temperature gradients. It would have

00:39:36 --> 00:39:38 shattered the rocks, and it would have driven

00:39:38 --> 00:39:40 some interesting chemistry. So that means

00:39:40 --> 00:39:43 that, uh, once the clouds clear and there's

00:39:43 --> 00:39:45 time for things to settle down, you have a

00:39:45 --> 00:39:48 site here that is similar to the kind of

00:39:48 --> 00:39:50 conditions at, uh, locations where people

00:39:50 --> 00:39:52 think the first life on Earth may have got

00:39:52 --> 00:39:54 started. So there's some interesting

00:39:55 --> 00:39:58 what happened after. So to study that,

00:39:58 --> 00:40:01 this team have gone to the, um,

00:40:01 --> 00:40:03 store of drill cores that they can get to in

00:40:03 --> 00:40:06 Finland, where there are, uh, results,

00:40:06 --> 00:40:08 resources left behind from drilling

00:40:08 --> 00:40:11 expeditions that dug into this crater lake

00:40:11 --> 00:40:14 back in the 1980s, 1990s. Now this is a

00:40:14 --> 00:40:15 really good example, incidentally, of how

00:40:16 --> 00:40:19 legacy materials continue to have

00:40:19 --> 00:40:20 worth. And we've talked about that with the

00:40:21 --> 00:40:22 rocks from the Apollo missions, where they

00:40:22 --> 00:40:24 put a lot of them and preserve them for

00:40:24 --> 00:40:27 future use, because our technology improves

00:40:27 --> 00:40:29 all the time. So we can go back and look at

00:40:29 --> 00:40:30 things that were collected in the past and

00:40:30 --> 00:40:33 get new insights. So the team

00:40:33 --> 00:40:35 went back to these rocks that, uh, were dug

00:40:35 --> 00:40:38 up back in the 80s and 90s from drill

00:40:38 --> 00:40:41 cores that dug down all the way into this

00:40:41 --> 00:40:43 crater lake, into the floor of it. And they

00:40:43 --> 00:40:45 got 33 different drill core samples from

00:40:45 --> 00:40:48 different locations, looked at them

00:40:48 --> 00:40:49 essentially with a microscope and a pair of

00:40:49 --> 00:40:52 tweezers, and, um, plucked out a number of

00:40:52 --> 00:40:55 crystals of calcite and. And

00:40:55 --> 00:40:56 what was the other rock? There were a couple

00:40:56 --> 00:40:59 of things, calcite and pyrite, these rocks.

00:40:59 --> 00:41:01 And they use these for chemical analyses. And

00:41:01 --> 00:41:03 what they were interested in doing was

00:41:03 --> 00:41:06 getting a chronology of what happened in the

00:41:06 --> 00:41:09 years after this crater was formed.

00:41:09 --> 00:41:11 Now, similar work has been done before for

00:41:11 --> 00:41:13 the Rhys Crater in Germany and the Horton

00:41:13 --> 00:41:16 Crater in Canada, which suggested for those

00:41:16 --> 00:41:19 craters, the material under and around the

00:41:19 --> 00:41:21 crater cooled fairly quickly in geological

00:41:21 --> 00:41:24 times. For those craters, it cooled to about

00:41:24 --> 00:41:26 50 degrees C within a quarter of a million

00:41:26 --> 00:41:28 years. For the Reese Crater and for the

00:41:28 --> 00:41:30 Horton Crater in Canada for about 50

00:41:30 --> 00:41:32 years. So that cooled down fairly quickly.

00:41:33 --> 00:41:35 But this Finnish team, looking at these

00:41:35 --> 00:41:38 crystals from, um, this beautiful Lake

00:41:38 --> 00:41:41 Lapiavi, found that it took about 4 million

00:41:41 --> 00:41:44 years for the rocks to cool to 50 degrees C,

00:41:44 --> 00:41:47 which to me is astonishingly long time.

00:41:47 --> 00:41:49 That's very slow cool. And they're saying, we

00:41:49 --> 00:41:51 don't really understand why it took so long,

00:41:51 --> 00:41:52 but it's probably to do with the kind of

00:41:52 --> 00:41:54 rocks that were around and the kind of

00:41:54 --> 00:41:57 insulating properties. But what they did

00:41:57 --> 00:41:59 then was that they looked at the chemistry of

00:41:59 --> 00:42:01 these samples. They used mass spectrometry

00:42:01 --> 00:42:04 to look at basically the different isotopes

00:42:04 --> 00:42:07 of oxygen, carbon and sulfur in the rock.

00:42:07 --> 00:42:09 And they were doing that because microbes

00:42:09 --> 00:42:12 tend to process oxygen, carbon and sulfur and

00:42:12 --> 00:42:14 preferentially use one isotope over the

00:42:14 --> 00:42:16 other. So they can put this very distinctive

00:42:16 --> 00:42:19 chemical signature in to what's left behind.

00:42:19 --> 00:42:22 So the team were very much looking for, in

00:42:22 --> 00:42:25 addition to this cooling data, uh, the point

00:42:25 --> 00:42:27 at which you started to get the fingerprints

00:42:27 --> 00:42:29 of microbial life once again. And what they

00:42:29 --> 00:42:31 found was that, uh, 4 million year point when

00:42:31 --> 00:42:34 it cooled to about 50 degrees C. That was

00:42:34 --> 00:42:36 when you started to get life there again. And

00:42:36 --> 00:42:38 you started to get life that was turning

00:42:38 --> 00:42:41 sulfates into sulfides. I think that was

00:42:41 --> 00:42:43 the chemical terminology there.

00:42:44 --> 00:42:47 So there were processing materials and

00:42:47 --> 00:42:50 life had recolonized effectively, yes,

00:42:50 --> 00:42:53 sulfate into sulfide. That was after 4

00:42:53 --> 00:42:55 million years. 10 million years after that,

00:42:55 --> 00:42:57 the temperature dropped to about 30 degrees

00:42:57 --> 00:42:59 C. And you got the kind of microbes that make

00:42:59 --> 00:43:02 methane recolonize there. So you've now got

00:43:02 --> 00:43:04 this really nice chronological timeline of

00:43:04 --> 00:43:07 the recolonization of this site. And, um,

00:43:07 --> 00:43:09 they talk about this being a surprisingly

00:43:09 --> 00:43:12 quick time. To me, this is surprisingly slow

00:43:12 --> 00:43:14 given how much life we've got around on the

00:43:14 --> 00:43:17 Earth. So obviously they are more expert than

00:43:17 --> 00:43:20 I am, and I'm happy to take their

00:43:20 --> 00:43:21 word that this is a very quick

00:43:21 --> 00:43:24 recolonisation. But to me, it's interesting

00:43:24 --> 00:43:26 that it took it so long to cool down and for

00:43:26 --> 00:43:29 life to get going again afterwards. That's

00:43:29 --> 00:43:30 maybe telling us something about the kind of

00:43:30 --> 00:43:33 rocks the impact happened in. I don't know

00:43:33 --> 00:43:34 whether it could also be telling us something

00:43:34 --> 00:43:36 about the underlying geology of the area at

00:43:36 --> 00:43:39 the time. I'm just not expert enough. But

00:43:39 --> 00:43:42 it's a really fascinating study and it's a

00:43:42 --> 00:43:45 really good example of how the science of

00:43:45 --> 00:43:47 astrobiology, which is the science of the

00:43:47 --> 00:43:49 search for life elsewhere and the science of

00:43:49 --> 00:43:51 the question of how we learn in the universe

00:43:51 --> 00:43:53 and of how did life get started on Earth, all

00:43:53 --> 00:43:56 those really thorny questions. That's not a

00:43:56 --> 00:43:57 science that can be answered by just one

00:43:57 --> 00:44:00 discipline within astronomy. It's a really

00:44:00 --> 00:44:02 multidisciplinary area where you need people

00:44:02 --> 00:44:04 from an incredibly wide and diverse

00:44:06 --> 00:44:08 variety of areas in the sciences to come

00:44:08 --> 00:44:10 together because no one area has the

00:44:10 --> 00:44:11 knowledge and the skill set and the

00:44:11 --> 00:44:14 methodology and the samples to provide an

00:44:14 --> 00:44:17 answer on their own. It's why conference

00:44:17 --> 00:44:19 on this kind of topic are so, uh, fascinating

00:44:19 --> 00:44:21 to me because you go to talks from biology

00:44:21 --> 00:44:24 and chemistry and geophysics rather than just

00:44:24 --> 00:44:26 a lot of talks from astronomers on astronomy

00:44:26 --> 00:44:29 things. And um, this is the kind of study no

00:44:29 --> 00:44:30 one I work with directly would have been able

00:44:30 --> 00:44:33 to do. But these people have been able to

00:44:33 --> 00:44:35 drill down, do this awesome work and get some

00:44:35 --> 00:44:38 really fascinating results. So I'm looking

00:44:38 --> 00:44:40 forward to hearing more about this. And to be

00:44:40 --> 00:44:41 honest, this would almost set the scene for

00:44:41 --> 00:44:43 groups elsewhere in the world to start

00:44:43 --> 00:44:45 drilling down into other creators to see if

00:44:45 --> 00:44:47 we can get a feel for. Is this unusual? Is

00:44:47 --> 00:44:50 this common? And, um, the other two unusual,

00:44:50 --> 00:44:52 essentially, what's going on?

00:44:52 --> 00:44:54 Andrew Dunkley: Yeah, yeah. And uh, as you said, it's just

00:44:54 --> 00:44:57 great that historical studies,

00:44:57 --> 00:45:00 uh, being dredged back up and

00:45:00 --> 00:45:03 reused with modern, um,

00:45:03 --> 00:45:06 techniques and technology to, to uh, find out

00:45:06 --> 00:45:08 more. I think that's amazing. And uh,

00:45:08 --> 00:45:11 keeping rocks for future reference,

00:45:11 --> 00:45:14 um, when we can do things even

00:45:14 --> 00:45:17 better, um, may reveal more answers.

00:45:17 --> 00:45:19 So, ah, that's. That. That in itself is a

00:45:19 --> 00:45:22 terrific part of that particular story.

00:45:22 --> 00:45:25 Uh, and I was just wondering about the Tim

00:45:25 --> 00:45:28 Horton, the uh, Horton crater. It couldn't

00:45:28 --> 00:45:30 be named after Tim Horton the famous ice

00:45:30 --> 00:45:31 hockey player, could it?

00:45:32 --> 00:45:34 Jonti Horner: Ice hockey player. Are there not some famous

00:45:34 --> 00:45:37 pancakes? Uh, Tim Hortons.

00:45:37 --> 00:45:37 Andrew Dunkley: Yeah.

00:45:37 --> 00:45:38 Jonti Horner: Well, that's. Yeah.

00:45:38 --> 00:45:40 Andrew Dunkley: I mean you can't go to Canada and not go to

00:45:40 --> 00:45:41 Tim Hortons.

00:45:41 --> 00:45:43 Jonti Horner: Um, I think the spelling may be different.

00:45:43 --> 00:45:46 This is Horton. H, A, U, G, H. Right.

00:45:46 --> 00:45:48 So probably a distant relative.

00:45:48 --> 00:45:51 Andrew Dunkley: You never know. Uh, okay, that brings us to

00:45:51 --> 00:45:52 the end. Johnny, thank you so much.

00:45:53 --> 00:45:54 Jonti Horner: Matt, it's an absolute pleasure. Thank you.

00:45:55 --> 00:45:57 Andrew Dunkley: Good, uh, to see you. Jonti Horner, professor

00:45:57 --> 00:45:59 of Astrophysics at the University of Southern

00:45:59 --> 00:46:02 Queensland, joining us. Don't forget to visit

00:46:02 --> 00:46:05 us online, uh, at our website and check

00:46:05 --> 00:46:06 everything out. You can, uh, send us

00:46:06 --> 00:46:09 questions via the uh, website as well and

00:46:09 --> 00:46:11 check out the shop and maybe, uh, sign up to

00:46:11 --> 00:46:14 become a supporter. Whatever floats your

00:46:14 --> 00:46:16 boat. Uh, it's@Space

00:46:16 --> 00:46:19 Nutspodcast.com uh, and

00:46:19 --> 00:46:21 thanks to Huw in the studio who couldn't be

00:46:21 --> 00:46:22 with us today. I don't know if you know this

00:46:22 --> 00:46:25 about Huw, but he's a bit old. He doesn't use

00:46:25 --> 00:46:27 satnav, but he heard about this great new

00:46:27 --> 00:46:29 book and he's gone to a bookshop to try and

00:46:29 --> 00:46:32 get it today. Uh, it's, um. It's the

00:46:32 --> 00:46:33 Three Eye Atlas book.

00:46:35 --> 00:46:38 Um, I'm not going to tell him. And from me,

00:46:38 --> 00:46:39 Andrew Dunkley, thanks for your company.

00:46:39 --> 00:46:41 We'll see you on the next episode of Space

00:46:41 --> 00:46:43 Nuts. Bye. Bye. You'll be

00:46:43 --> 00:46:45 listening to the Space Nuts.

00:46:45 --> 00:46:48 Jonti Horner: Podcast, available at

00:46:48 --> 00:46:50 Apple Podcasts, Spotify,

00:46:50 --> 00:46:53 iHeartRadio or your favorite podcast player.

00:46:53 --> 00:46:56 You can also stream on demand@bytes.com M.

00:46:57 --> 00:46:59 Andrew Dunkley: This has been another quality podcast

00:46:59 --> 00:47:01 production from bytes.com.