WEBVTT

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Okay, let's get into this. I want you to picture

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something for a second. You're holding a piece

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of rock. It's dark. It's from the Australian

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bush. And right there in the middle, there's

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this brilliant white shape of a leaf. It's an

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incredible image. And it's perfect. I mean, you

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can see every detail. It's been locked in that

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stone for about, what, 150 million years. And

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usually, you know, finding something that well

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-preserved is a win. You think, great, we know

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exactly what this is. Right. Case closed. We

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have the evidence. We have the photo. But this

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is where it starts to get really interesting.

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Because that rock, that perfect impression, it's

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a trap. It's a trap that paleontologists have

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been falling into for, well, over 100 years.

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Just because you have the body doesn't mean you

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know who the victim is. And that is the perfect

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setup for today's deep dive. We're looking at

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a botanical mystery. A species with a... I guess,

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a massive identity crisis. That's a good way

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to put it. It's a tree that's been dug up, named,

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then renamed, and then, well, questioned all

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over again. It can't seem to decide what it is.

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And it's such a fascinating window into how science

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actually works. You know, we think it's a straight

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line, but it's often a zigzag. We're looking

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at the records around a species called Agathys

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juraska. Or, depending on when your textbook

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was printed, Potosamites, Jurassic. I love that.

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We have to use air quotes around a tree's name.

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So our mission today is to figure out how this

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one plant can tell us about ancient clivates,

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volcanoes, and why just putting a label on something

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from the past is so tricky. Exactly. And to do

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that, we have to go back. Way back. Okay, so

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set the scene for us. Where are we? We're going

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to a place called the Talbergar Fishbeds. It's

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northwest of Sydney, Australia, out near the

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Talbergar River Valley. I think I know the area.

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I'm picturing, you know, dry Australian bush,

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lots of rocks, maybe forest hills nearby. It's

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very stark. Today, yes. But we need to wind the

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clock back to the early to middle Jurassic. We're

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talking the Tythonian age. Tythonian, okay. When

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is that, roughly? About 150 million years ago.

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And the world map looks totally different. Australia

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is still stuck to Gondwana, the supercontinent.

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And this area isn't dry bushland. It's sitting

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under the influence of the Tethys Sea. The Talbergar

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site itself was actually a large, shallow, freshwater

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lake. A lake. Okay, so forget the dust. We're

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picturing water. A lot of water and a lot of

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life. The sources describe lush, woody vegetation

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all around it. Essentially, a dense forest. We'd

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probably call it a cowry pine forest. That sounds

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nice. So a lake. Ancient pines. And it was teeming.

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It's called the fish beds for a reason. Huge

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fish populations, insects, and all this diverse

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flora along the shoreline. It was a warm, thriving

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world. And the atmosphere was different too,

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right? More CO2. Much more. And that high carbon

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dioxide level acted like a fertilizer, letting

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all that vegetation grow incredibly dense and

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fast. So we have this Jurassic paradise. Warm,

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lush, full of life. But... We're looking at fossils,

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and fossils usually mean something went very,

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very wrong. They do, and this is where the story

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takes a dark turn. The preservation there is

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amazing, thousands of specimens, but that's because

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of what the sources call a large -scale event.

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Which is science -speak for a disaster. A huge

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one. The evidence points to the lake being rapidly

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inundated with sediment. Volcanic ash, to be

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specific. Whoa. So, like a Pompeii, but for fish

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and trees. That's a very apt analogy. The ash

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came down fast, burying everything. The fish,

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the leaves, the branches, it all got trapped.

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And that's what preserved them so perfectly.

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Exactly. Because it was so fast, and because

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of the ash's chemistry, we get what are called

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salacious impressions. Salacious impressions.

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Break that down for me. Well, normally a leaf

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falls, it rots. But the ash sealed it all off

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from oxygen. So the organic matter decayed, but

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groundwater full of silica seeped in. Silica.

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Like in sand or glass. Basically, yeah. The silica

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filled in the space where the leaf was, leaving

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a perfect, stark white impression on the dark

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rock. It's almost like a photograph. It's haunting

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this vibrant green world and then, boom, ash.

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And everything is frozen in white. It is. But

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for scientists, it's a goldmine. It's a snapshot

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of exactly what was living there at that very

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moment. Which brings us to our mystery plant.

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The tree caught in the ash. Right. So let's jump

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forward in time. It's 1889. The Talbergar fish

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beds are discovered. And I'm guessing the paleontologists

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were pretty excited. Oh, absolutely. A guy named

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R. Etheridge Jr. publishes the first findings

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that same year. And this is where the identity

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crisis starts. What did he call our tree? He

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identified it as Podosomites lanceolatus. Podosomites

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lanceolatus. Sounds official. What does it mean?

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Podizomites is a genus of extinct conifers, and

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lanceolatus just refers to the lance -shaped

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leaves. Long and pointy. So he sees a long, skinny

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leaf and says, yep, that's a podizomite. Case

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closed. For a while, yeah. I mean, you have to

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understand, they were just sorting through thousands

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of these things. It's easy to group by what you

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see on the surface. Looks like a duck. Quacks

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like a duck. Precisely. And in 1921, another

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scientist, Walkam, did a more detailed review.

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He upheld the name. But he added a little note,

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didn't he? He did. He said the flora was likely

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coniferous. He was getting close. He knew they

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were cone -bearing trees, but he didn't challenge

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the name itself. So what was wrong with the name?

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Why wasn't it a podosomites? It's all in the

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details. The real podosomites has pin -eyed leaflets

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that grow from opposite sides of the stem. Think

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of it like a feather, sort of symmetrical. Okay,

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opposite each other. Got it. But the Talbergar

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fossils... They didn't really do that. But for

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almost 100 years, nobody really dug into it.

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That's amazing. It just sat in the books for

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a century. Until. Until 1981. And our detective

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arrives, Mary White. Mary White. She does this

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intensive review of everything from Talbergar.

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And she starts noticing the little things everyone

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else had kind of. glossed over. Right. She got

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out the magnifying glass, so to speak. She really

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did. She saw that the leaf sizes varied along

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the smaller branches, which suggested they were

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foliage spurs. Foliage spurs. Is that like how

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pine needles grow in little bunches? A similar

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idea, yes. A specific kind of growth on short

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stems. And that is not how porosomites grow.

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Uh -huh. There's the tell. And she kept going.

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She measured the leaves four to seven centimeters

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long, lance -shaped. And she looked at their

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arrangement. The arrangement, right. You said

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podosomites were opposite. And these weren't.

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Mary White saw they had a spiral phyllotaxy.

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They grew in a spiral around the stem. Okay,

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totally different structure. Completely. Plus,

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she looked at the veins. Parallel veins, about

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five to eight per leaf. Wow, that's specific.

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It has to be. But the real kicker. It wasn't

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just the leaves, it was the cones. The reproductive

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parts. Exactly. For decades, the cones found

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at the site were classified as a totally separate

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species, something called Orocarites grandus.

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So they thought they were just two different

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plants mixed together. Yes. But Mary White looked

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at these cylindrical cones and realized, wait

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a minute, these... These belong to the leaves.

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She put them together. That's a huge connection,

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connecting the fruit to the tree. It was. And

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with the spiral leaves, the foliage spurs, and

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now the cones, she concluded it was much closer

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to the modern genus Agathys. Agathys. Okay, for

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those of us who aren't botanists, what is that?

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Think of the giant cowry pines in New Zealand

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and Australia. These massive ancient conifers,

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giants of the forest. So she's saying this Jurassic

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fossil isn't some random extinct plant. It's

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a direct ancestor of the modern cowrie. That's

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exactly what she's saying. And she renames it

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Agathys Jurassic. Agathys Jurassic. It has a

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good ring to it. And that feels like a big moment.

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Yeah. You're tracing this modern giant all the

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way back to the age of dinosaurs. It was a massive

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aha moment. It rewrote the evolutionary history

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of that whole forest. It meant the cowrie pines

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were incredibly ancient survivors. I can hear

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the butt in your voice. There's always a butt.

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There is always a but. This is where it gets

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good. You'd think, okay, 1981, she does the work,

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case closed, we have our name. You'd think. But

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science is skeptical. Fast forward to 1999. Two

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researchers, Hill and Broderib, are reviewing

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the whole fossil family, Arachariaceae. That's

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the family these trees belong in. Yes. And they

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hit a snag, a chronological snag. What do you

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mean? They looked at the whole fossil record

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globally, and they noticed that the oldest...

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The most reliably identified Agathys fossils,

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the ones everyone agrees on, are from the Middle

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Eocene. The Eocene. Okay. How far is that from

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the Jurassic? It's a huge gap. The Jurassic is

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about 150 million years ago. The Middle Eocene

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is more like 40, maybe 50 million years ago.

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Oh. That's a hundred million year gap in the

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fossil record. It's enormous. It's a huge problem.

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If this thing from the Jurassic really is Agathys,

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where are all its descendants for the next hundred

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million years? There's just nothing. It's like

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finding a Roman chariot and then a brand new

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Ferrari and saying one led directly to the other

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with no cars in between. That's a great way to

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put it. You need the intermediate steps. Without

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them, it's just a wild coincidence. So what do

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they do? Do they just say Mary White was wrong?

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Well, they cast major doubt on it. They said,

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you know, the visual match is there, but the

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timeline just doesn't work. It's suspicious.

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So they took the name away again. Not officially,

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but because of their work, other scientists started

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calling it Podosomite's Jurassic. It swung back.

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Unbelievable. The poor tree is just getting tossed

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back and forth. It gets even messier. As of 2017,

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the name Podosomites jurassica hadn't even been

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validly published. What does that mean? In taxonomy,

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there are strict rules for naming a species.

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You have to follow a process. And no one had

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actually done the official paperwork to make

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that name stick. So it's in taxonomic limbo.

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Completely. It's not the original podozomites.

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It might be Agathys, but the timeline is a huge

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problem. And it might be a new kind of podozomites,

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but nobody's officially named it that way. That

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is just, it's absurd. We have thousands of perfect

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fossils. But we can't agree on what to call them.

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And it matters. It's a really important debate

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about ancestry. Is this a direct grandfather

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of modern Kairi Pines? Or is it just a distant

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cousin that evolved to look very similar and

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then went extinct? Convergent evolution. Exactly.

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Like a shark and a dolphin. They look similar,

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but they're not closely related at all. If this

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is a lookalike, then the carapine is a much younger

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species than Mary White thought. And what about

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its range? It was mostly an Australian thing?

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Primarily southern hemisphere, yes. This was

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Gondwana, remember. But the sources do mention

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some marginal expanses into the northern hemisphere.

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It's a southern specialist, then. It seems so,

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yeah. Adapted to that warm, high CO2 world. Okay,

00:10:53.039 --> 00:10:55.659
so let's recap this whole journey. We start...

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In a Jurassic forest. A forest that gets flash

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frozen by volcanic ash. We dig it up in 1889

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and call it Podosomites. Then in 1981, Mary White

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sees the spiral leaves and calls it Agathys.

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And then the timeline police show up in 1999,

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point out the 100 million year gap, and push

00:11:13.580 --> 00:11:16.100
it back towards Podosomites. Where it sits today,

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kind of nameless. It just goes to show you that

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science isn't this neat collection of facts,

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it's an argument. A long, slow argument. It is.

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And that's what's so cool. The rock itself hasn't

00:11:26.700 --> 00:11:29.899
changed. The fossil is the same. But our understanding,

00:11:30.120 --> 00:11:32.299
our framework for interpreting it keeps shifting.

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And I think that's what's so fun about these

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deep dives. You realize even something as solid

00:11:36.500 --> 00:11:39.759
as a rock is. It's up for debate. Absolutely.

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And it's a good reminder to be humble. We're

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looking at a shadow of the past, literally, and

00:11:44.740 --> 00:11:46.639
trying to build an entire history from it. So

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I guess the takeaway for you listening is next

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time you see a pine tree, you can wonder, is

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its family tree 50 million years old or 150 million?

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And are there ghosts in that tree we just haven't

00:11:56.700 --> 00:11:59.620
found the right name for yet? Exactly. I want

00:11:59.620 --> 00:12:01.440
to leave you with a final thought on this. We

00:12:01.440 --> 00:12:04.139
talked about those stark white impressions. The

00:12:04.139 --> 00:12:08.100
ash preserved the shape. Nature's own photograph.

00:12:08.600 --> 00:12:12.659
It is. But think about it this way. We have the

00:12:12.659 --> 00:12:15.000
photograph. It's perfectly clear. But we are

00:12:15.000 --> 00:12:16.860
still fighting over the caption underneath it.

00:12:17.279 --> 00:12:21.299
If Mary White was right, if it is Agathys, that

00:12:21.299 --> 00:12:24.500
means that genus survived the asteroid that killed

00:12:24.500 --> 00:12:28.500
the dinosaurs. It survived the breakup of Gondwana.

00:12:28.620 --> 00:12:30.980
It survived ice ages. It would be one of the

00:12:30.980 --> 00:12:33.539
planet's ultimate survivors. And if she was wrong.

00:12:33.679 --> 00:12:36.820
If she was wrong. Yeah. Then that Jurassic forest

00:12:36.820 --> 00:12:39.440
at Talbogar was filled with some other kind of

00:12:39.440 --> 00:12:41.399
giant that just happened to look exactly like

00:12:41.399 --> 00:12:43.980
a cowry pine and then vanished completely. So

00:12:43.980 --> 00:12:46.080
what was that tree? The rock shows us the what,

00:12:46.120 --> 00:12:48.700
but it just refuses to tell us the who. And that's

00:12:48.700 --> 00:12:50.580
the mystery that keeps us digging. And that's

00:12:50.580 --> 00:12:52.080
where we'll leave it. Thanks for diving deep

00:12:52.080 --> 00:12:54.720
with us into the identity crisis of Agathys,

00:12:54.720 --> 00:12:57.299
Jurassic. My pleasure. Always fun. See you next

00:12:57.299 --> 00:12:57.519
time.
