WEBVTT - SYSK Selects: How Fossils Work

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<v Speaker 1>Hey, ever you wanted, it's me Josh, And for this

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<v Speaker 1>week's s Y s K Selecta, I've chosen How Fossils Work,

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<v Speaker 1>which actually is one of the most scientifically interesting, amazing,

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<v Speaker 1>mind bending episodes that we've ever done. And I just

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<v Speaker 1>listened to it and it still holds up. So I

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<v Speaker 1>hope that you enjoy it. And as they say on

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<v Speaker 1>with the show, welcome to Stuff you should Know from

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<v Speaker 1>house Stuff Works dot com. Hey, and welcome to the podcast.

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<v Speaker 1>I'm Josh Clark with me as always as the intrepid

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<v Speaker 1>paleontologist Charles W. Chuck Bryant. It's terrible' no I like it. Okay,

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<v Speaker 1>I wish I was a paleontologist. Let your new nickname

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<v Speaker 1>or intrepid at least, let's just go with paleontologists. That'd

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<v Speaker 1>be great. Okay, we're talking fossils today, Dude, this isn't

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<v Speaker 1>really interesting stuff. It really is. And um, you can

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<v Speaker 1>tell that Tracy Wilson are esteemed head of the writing editor.

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<v Speaker 1>I think she's site director director, right. Um you can

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<v Speaker 1>tell that she was very, very excited. She took her

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<v Speaker 1>time and really doled this one out. I think um

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<v Speaker 1>savor is the right word. You can feel it her

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<v Speaker 1>smiling through the keyboard. Yeah, she's very happy to write

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<v Speaker 1>how fossils work. And um, we're happy to do it

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<v Speaker 1>because it's one of those very comprehensive articles on the

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<v Speaker 1>site that you just has everything you need. Sedimentary rock,

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<v Speaker 1>flat bones versus round bones, leaf impressions, has it all.

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<v Speaker 1>Unless you're an intrepid paleontologist. Then we'll get an email

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<v Speaker 1>saying it actually wasn't very comprehensive. You guys royally screwed

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<v Speaker 1>this up. We just wait until we get into punctuated

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<v Speaker 1>versus gradual evolution. Chuck. Um, you've heard of Lucy right,

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<v Speaker 1>the Australia Kiss. Yeah, okay, Well, um, she was I

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<v Speaker 1>think three point two million years old. That's one old lady.

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<v Speaker 1>It really is the earliest hominid we've found as far

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<v Speaker 1>as I know. Um. But there is a part of

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<v Speaker 1>her foot missing. It's always been missing that we've never

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<v Speaker 1>found before. So this thing, this bone, was so essential

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<v Speaker 1>and we couldn't tell how she walked until recently. Why

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<v Speaker 1>because the missing bone, we couldn't tell how she walked exactly.

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<v Speaker 1>We we we can tell so much from bones that

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<v Speaker 1>when we don't have the right bones we can't tell anything.

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<v Speaker 1>So she may have been in a knuckle dragger, she

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<v Speaker 1>may have hopped. We didn't know. Well. Recently, UM, some

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<v Speaker 1>people from the University of Missouri or Missouri, depending on

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<v Speaker 1>whether or not you live in the state. UM found

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<v Speaker 1>the Uh, the group of foot bones needed to show

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<v Speaker 1>what kind of walker Lucy was. And she walked up right?

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<v Speaker 1>How was her gate? Upright? Upright? Just like a human.

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<v Speaker 1>She had a hitch and her get along, she had

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<v Speaker 1>a pepper and her step. Possibly she knew she'd be

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<v Speaker 1>famous one day. She was loved with duc But but

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<v Speaker 1>consider this, right, Okay, three point two million year old

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<v Speaker 1>footbones were found, and we could tell from them how

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<v Speaker 1>she walked. This is the state of the field that

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<v Speaker 1>you remember paleontology. Pretty cool. This is how advanced it is.

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<v Speaker 1>And yet it's really just kind of using common sense

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<v Speaker 1>to figure out what old bones mean. Common sense and science.

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<v Speaker 1>Fossils go, let's talk about it, Chuck, what are some

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<v Speaker 1>of the different kinds of fossils. Uh, well, one of

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<v Speaker 1>my favorite kinds of trace fossil. Yeah, that's actually one

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<v Speaker 1>of my favorites too. It's like, um, that Jesus footprint thing.

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<v Speaker 1>Footprints in the sand. Yeah, sort of is josh um.

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<v Speaker 1>That is when it's actually not part of the organism

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<v Speaker 1>at all, but it's um like tooth marks in a

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<v Speaker 1>chunk of wood from a saber tooth tiger. Or footprints

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<v Speaker 1>or footprints or track ways as Tracy calls them. Yes,

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<v Speaker 1>footprints tracks. It's just unnecessary, but it has a pleasant tone,

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<v Speaker 1>you know science. Yeah, like they're not footprints, they're track ways.

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<v Speaker 1>I'm bored in Ethiopia, let's call him track ways. So

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<v Speaker 1>trace fossils is one. Of course, there's bone fossils, right,

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<v Speaker 1>the most famous fossils. Yeah, those are great too. They

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<v Speaker 1>got nothing on trace fossils. So actually, bone fossils, that's

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<v Speaker 1>that's what you really want. If you're going to reconstruct

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<v Speaker 1>the dinosaur for your museum. You can't deal it with footprints, No,

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<v Speaker 1>you can't. You need the bones, you do. And the

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<v Speaker 1>bones are of course the most famous ones in the dinosaur.

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<v Speaker 1>Bones are the most famous of all the bone types. Right.

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<v Speaker 1>So there's something that I think um is often missed

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<v Speaker 1>by lay people such as myself, um and in that

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<v Speaker 1>when you find a bone, right, so you find like

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<v Speaker 1>a big old dinosaur bone, it's really geologically speaking, it's

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<v Speaker 1>not a bone any longer. It's not like you find

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<v Speaker 1>a bone buried in your yard that was an animal

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<v Speaker 1>from like, you know, thirty five years ago, But that's

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<v Speaker 1>not a fossil. We'll not still bone. A fossil is

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<v Speaker 1>a bone or a piece of um once living organic

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<v Speaker 1>material that's undergone a transition from uh, an organic state

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<v Speaker 1>to an inorganic state. That's what a fossil is. It's

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<v Speaker 1>gone through the process of fossilization. And most of these fossils,

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<v Speaker 1>the vast majority of fossils, are found in sedimentary rock.

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<v Speaker 1>Before we're go any further, we should probably do a

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<v Speaker 1>little brief primerun sedimentary rock, right, which is awesome. Yeah,

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<v Speaker 1>it's pretty easy to Uh. We've talked about the Earth's

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<v Speaker 1>core um and layers. When I think we talked about

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<v Speaker 1>earthquakes and maybe some other stuff. We all know that

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<v Speaker 1>there's the intercore, outer core. We got the crust. Crust

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<v Speaker 1>is the thinnest layer, and that's where the fossils are.

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<v Speaker 1>That's where the goods are. And uh, most of the

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<v Speaker 1>rocks in the crust are sedimentary rocks that you've been

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<v Speaker 1>talking about off and on for the past eight minutes, right,

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<v Speaker 1>and that's like silty sandy stuff that hardened over the years, right,

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<v Speaker 1>I mean, but the the Earth. Remember we talked about, oh,

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<v Speaker 1>what was it, clouds. I can't remember what podcast it was,

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<v Speaker 1>but we talked about how much sand is transferred from

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<v Speaker 1>Africa to South America annually. Yeah, it wouldn't clouds, but yeah,

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<v Speaker 1>if you you remember the one I'm talking about. Okay, So,

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<v Speaker 1>the Earth's geo biogeochemical processes equal a lot of movement

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<v Speaker 1>of particulate matter. Right. The Earth is dynamic, baby, it is.

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<v Speaker 1>It's also very fluid. To write, a lot of that

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<v Speaker 1>matter is at at one point as suspended particles in

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<v Speaker 1>water that's moving around, right. Yeah. So um, as this

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<v Speaker 1>as the water leaves and the sediment is deposited, it

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<v Speaker 1>builds up and up and up. Over time, it hardens

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<v Speaker 1>into rock and eventually we have sedimentary rock, yeah, which

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<v Speaker 1>is below our feet. We don't normally see it unless say,

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<v Speaker 1>the Colorado River um winds over it for you know,

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<v Speaker 1>millions and millions and millions of years, revealing the sedimentary

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<v Speaker 1>rock that's in the Earth's crust. Grand Canyon exactly. So

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<v Speaker 1>you're talking about, Yeah, I forgot the Grand Canyon Park

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<v Speaker 1>So you know how I said the Earth was dynamic, baby, Yeah, Uh,

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<v Speaker 1>that's important. I didn't just throw that in there as

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<v Speaker 1>a factoid. It's important because when these plates shift around,

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<v Speaker 1>that's how fossils are. On Earth. Things can be moved

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<v Speaker 1>great distances and pushed to the surface eventually or close

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<v Speaker 1>enough to where a dig can unearth it. And it's like,

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<v Speaker 1>just because it's fossilized doesn't mean it's stuck in that

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<v Speaker 1>one spot forever, because Earth is always moving. So the

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<v Speaker 1>point of all this is is sedimentary rock um is,

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<v Speaker 1>like you said, dynamic. It moves around. Sometimes fossils pop

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<v Speaker 1>up or it becomes exposed all of the Colorado River um,

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<v Speaker 1>and that is where fossils are, right Chuck. Yes, So

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<v Speaker 1>let's say that at some point in time there was

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<v Speaker 1>a dinosaur or a sabertooth tiger or a cyanobacteria woly

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<v Speaker 1>mammoth wooly mammoth, sure um, and it's um hanging out

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<v Speaker 1>around a riverbed and it has a massive heart attack

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<v Speaker 1>and falls over in the river bed and very quickly

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<v Speaker 1>it becomes covered with sediment and silt, right Yeah, And

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<v Speaker 1>that's important because once it starts getting covered up with stuff,

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<v Speaker 1>it's sort of being protected from like all of fossil.

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<v Speaker 1>Let's just break the news. All of fossil means is

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<v Speaker 1>that something has been protected from the natural decomposition process.

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<v Speaker 1>Otherwise we just decompose like everything else, and you wouldn't

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<v Speaker 1>see it anymore. You've just totally betrayed Tracy in the

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<v Speaker 1>tone she lent to this, that the whole drama drawing

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<v Speaker 1>out suspense. But that's true. So what you said was right.

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<v Speaker 1>So you'd fall over in a riverbed, you start getting

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<v Speaker 1>covered up with the sediment and silt, and it's it's

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<v Speaker 1>immediately starting to protect you in a way. Um, not you,

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<v Speaker 1>but whatever, the wooly mammoth, the wooly mammoth. Um. The

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<v Speaker 1>thing is the in this sediment, in this silt, you

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<v Speaker 1>can't really hide from macrobacteria, uh and other forms of

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<v Speaker 1>life that are basically dedicated to breaking down organic matter,

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<v Speaker 1>soft tissue, hair, eyeballs, um, genitalia, all that kind of stuff.

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<v Speaker 1>It eventually becomes broken down and what's left is the

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<v Speaker 1>hard stuff the bone, right, But the bone also has

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<v Speaker 1>organic material within it as well. Yeah, and that'll break down.

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<v Speaker 1>We're talking blood cells, collagen, fat, that's going to break

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<v Speaker 1>down to the key here is the inorganic parts of

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<v Speaker 1>the bone remain intact. And it's the other keyword here's porous. Yeah.

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<v Speaker 1>You take calcium, I imagine for your hips. Yeah, sure, glucosamine, calcium. Sure.

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<v Speaker 1>So what you're doing is, um, you're fortifying the calcium

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<v Speaker 1>that's already in your hips, supposedly, um, because the bone

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<v Speaker 1>is made in large part of calcium, which is a mineral,

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<v Speaker 1>which is inorganic. So it's all the organic stuff dies out.

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<v Speaker 1>What's left is, like you said, the inorganic like calcium, whatever, minerals,

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<v Speaker 1>and that holds the shape, right, Yeah, the initial structure

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<v Speaker 1>is kept intact. Right, But like you said, this bone

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<v Speaker 1>is also porous. That's the key. And over time, um,

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<v Speaker 1>other mineral sediment kind of um, it enters into these

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<v Speaker 1>these microscopic pores iron right, carbonate yea and fortifies this,

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<v Speaker 1>ultimately turning this but what was once an organic bone

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<v Speaker 1>into an inorganic rock in the shape of the bone.

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<v Speaker 1>But for all intensive purposes, it's still the bone. It

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<v Speaker 1>still has that original calcium. It's still the same thing.

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<v Speaker 1>It's not like a replica of it. It's just become fossilized. Yeah,

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<v Speaker 1>and Tracy in the article uses a pretty good example.

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<v Speaker 1>I thought, it's like filling a sponge with glue. The

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<v Speaker 1>sponge is gonna keep the shape, but the glue is

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<v Speaker 1>gonna ooze through all the spots that it can ouze harden,

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<v Speaker 1>and there you go. You've got a hard sponge, hard sponge,

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<v Speaker 1>which is basically what a fossil is. And this takes

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<v Speaker 1>place Josh over the course of millions of years, the

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<v Speaker 1>sediment reinforcing the bones eventually becoming rock. It's not the

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<v Speaker 1>kind of thing that happens willy nilly over thousands of years.

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<v Speaker 1>It's a long time, and it's just this isn't just

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<v Speaker 1>um happening by itself. All of the surrounding area UM

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<v Speaker 1>is being deposited with sediment as well. It's also turning

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<v Speaker 1>into rock um. And then the ultimate test of time

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<v Speaker 1>for a fossil is that it can withstand the pressure

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<v Speaker 1>of the that's mounted by the hardening rock sedimentary rock

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<v Speaker 1>that's growing around it, so it can be crushed. Is

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<v Speaker 1>that how A lot of fossils are definitely crushed, crushed

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<v Speaker 1>the death poor guys um. But if it survives and

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<v Speaker 1>you can find this, you will eventually be able to

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<v Speaker 1>get to it. And then you remove the rock from

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<v Speaker 1>around the fossil, and there's your bone that you can

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<v Speaker 1>take to the Natural History Museum and get at least

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<v Speaker 1>five dollars for when you were a kid, Josh, let

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<v Speaker 1>me ask you this. Did you ever go into the

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<v Speaker 1>woods on a little nature course from like a science center,

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<v Speaker 1>let's say, and do a cast plaster cast of a

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<v Speaker 1>animal footprint? Did you ever do that? No? Really, really,

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<v Speaker 1>I did that. We went and found like deer hoof prints,

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<v Speaker 1>you fill it with plaster, and there was some way

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<v Speaker 1>of doing it where you an inverse plaster cast of

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<v Speaker 1>a deer hoof print. That can happen actually in a

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<v Speaker 1>way that with trace fossils, so you can you know,

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<v Speaker 1>sediment can act the same way. And one of these,

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<v Speaker 1>let's say, uh, the wooly mammoth makes a footprint in

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<v Speaker 1>some loose but sturdy soil that fills up with sediment

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<v Speaker 1>and creates basically a mold, just like I did as

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<v Speaker 1>a kid with the plaster cast. Yeah, as long as

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<v Speaker 1>the sediment that fills it in is lighter or thinner, yeah,

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<v Speaker 1>than the soil that the impression is made in, then yeah,

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<v Speaker 1>it would it would, it would preserve that track. Yeah,

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<v Speaker 1>and plants can do the same thing. It's not just

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<v Speaker 1>bones we're talking about. Um. It can also fill in

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<v Speaker 1>in a different way, I guess the opposite way to

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<v Speaker 1>where it makes a basically a cast of the foot

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<v Speaker 1>that made the track. Oh yeah. And then so it's

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<v Speaker 1>like a kind of like a fossil of a ghost

0:13:50.960 --> 0:13:54.640
<v Speaker 1>foot that's not really there, but it makes the foot.

0:13:54.720 --> 0:13:58.040
<v Speaker 1>It's like an inverse cast. Okay, yeah, of not the track,

0:13:58.120 --> 0:14:00.680
<v Speaker 1>but the foot that made the track. Yeah. Yeah, got cool.

0:14:01.000 --> 0:14:04.240
<v Speaker 1>You know what other another my favorite trace fossil is

0:14:06.240 --> 0:14:08.480
<v Speaker 1>it's not a track way, it's copper light. I changed

0:14:08.520 --> 0:14:11.440
<v Speaker 1>my mind. That is a good one. That's dunge. It's poop,

0:14:11.640 --> 0:14:14.480
<v Speaker 1>fossilized poop. That's right. I can tell you a lot

0:14:14.520 --> 0:14:17.440
<v Speaker 1>about an animal. It can tell you about its fiber intake.

0:14:18.320 --> 0:14:23.600
<v Speaker 1>It can tell you about what size it's poop was, um, chuck.

0:14:23.680 --> 0:14:27.520
<v Speaker 1>You know. In the eighties, the CIA found out much

0:14:27.720 --> 0:14:30.920
<v Speaker 1>about Gorbachof and his health. They found out he had

0:14:30.960 --> 0:14:35.520
<v Speaker 1>like cancer or some sort of chronic illness um by

0:14:35.640 --> 0:14:38.960
<v Speaker 1>stealing his poop when he was when he came on

0:14:39.040 --> 0:14:42.080
<v Speaker 1>a state visit to the US. They took his poop

0:14:42.120 --> 0:14:45.920
<v Speaker 1>and analyzed it, and when they he was in the US,

0:14:46.000 --> 0:14:48.400
<v Speaker 1>they des grabbed it from the toilet. Did he not flush?

0:14:48.760 --> 0:14:51.320
<v Speaker 1>I just want more specifics. You probably don't have. As

0:14:51.360 --> 0:14:54.880
<v Speaker 1>far as I understand, they probably it's hotel room or

0:14:54.880 --> 0:14:58.080
<v Speaker 1>wherever he was staying. They were prepared to do this.

0:14:58.120 --> 0:15:02.440
<v Speaker 1>This was like toilet rigged. Probably, yes, But wherever Reagan went,

0:15:03.200 --> 0:15:05.240
<v Speaker 1>they had a portable toilet that he used. It was

0:15:05.280 --> 0:15:07.400
<v Speaker 1>the only one he was allowed to use. I'm not kidding,

0:15:07.480 --> 0:15:13.400
<v Speaker 1>so no one could steal his poop. Talk about paranoid. Yeah, seriously,

0:15:13.520 --> 0:15:17.760
<v Speaker 1>when you point one finger, there's three pointing back at you.

0:15:17.760 --> 0:15:20.320
<v Speaker 1>You know what I mean? Yeah? Yeah? Uh so, Josh,

0:15:20.360 --> 0:15:22.640
<v Speaker 1>that is sedimentary rock and that's to me one of

0:15:22.680 --> 0:15:26.360
<v Speaker 1>the cooler ways you can get a fossil. Uh petrified

0:15:26.400 --> 0:15:28.280
<v Speaker 1>would too? Don't leave that one out. Oh yes, it's

0:15:28.320 --> 0:15:31.560
<v Speaker 1>basically the same thing that we just described for bone,

0:15:31.600 --> 0:15:34.640
<v Speaker 1>but for wood. Yeah, hard as a rock because it

0:15:34.760 --> 0:15:37.200
<v Speaker 1>is a rock. Here you go, alright, So, like I

0:15:37.240 --> 0:15:40.120
<v Speaker 1>just said, um, that was sedimentary rock and that's kind

0:15:40.160 --> 0:15:44.040
<v Speaker 1>of fun. But you can also uh get a fossil.

0:15:44.120 --> 0:15:47.560
<v Speaker 1>Has that funny because one dies in a cave that's

0:15:47.560 --> 0:15:52.160
<v Speaker 1>really dry. Yeah, desiccation. Yeah, desiccation is basically, uh, sort

0:15:52.160 --> 0:15:54.880
<v Speaker 1>of a mummification, but it's not like we think of

0:15:54.880 --> 0:15:58.680
<v Speaker 1>with mummification with the Egyptian tombs or anything like that. Well,

0:15:58.720 --> 0:16:02.280
<v Speaker 1>that's because there's no reservation techniques that have been undertaken.

0:16:02.320 --> 0:16:05.440
<v Speaker 1>It's natural. Basically, it dries out. It's like throwing an

0:16:05.480 --> 0:16:08.480
<v Speaker 1>orange in a dehydrator. So when it's really dry, there's

0:16:08.480 --> 0:16:11.160
<v Speaker 1>not gonna be any place for bacteria to thrive. That's

0:16:11.200 --> 0:16:14.680
<v Speaker 1>the reason beef jerky is not um refrigerated. If you

0:16:14.720 --> 0:16:18.200
<v Speaker 1>refrigerate your beef jerky, you're you're doing something wrong. Yeah,

0:16:18.200 --> 0:16:20.640
<v Speaker 1>that's true. Well, if you have beef jerky long enough

0:16:20.640 --> 0:16:24.760
<v Speaker 1>to need refrigeration, then you're doing something wrong or something

0:16:24.880 --> 0:16:29.600
<v Speaker 1>really really right. Uh. So desiccation actually works so well

0:16:29.680 --> 0:16:33.520
<v Speaker 1>sometimes that it can preserve the skin and soft tissues

0:16:33.640 --> 0:16:36.080
<v Speaker 1>as well, which is something that sedimentary rock cannot do.

0:16:36.360 --> 0:16:38.800
<v Speaker 1>Have you been to the Smithsonian I have they have

0:16:39.120 --> 0:16:43.040
<v Speaker 1>um a very cool I guess a prehistoric cow or

0:16:43.080 --> 0:16:46.920
<v Speaker 1>a musk ox I can't remember, but it's the thing's head, um,

0:16:47.200 --> 0:16:50.120
<v Speaker 1>much of its back, I guess, the cape, two of

0:16:50.160 --> 0:16:52.560
<v Speaker 1>its legs, and the skin is still there. It's just

0:16:52.720 --> 0:16:56.320
<v Speaker 1>right there. Probably it's tens of thousands of years old

0:16:56.920 --> 0:16:59.800
<v Speaker 1>and it's just sitting right there. Did they could they

0:16:59.800 --> 0:17:01.720
<v Speaker 1>read build it or just put the parts up? It's

0:17:01.760 --> 0:17:04.320
<v Speaker 1>just the parts, but it's laid out so that like

0:17:04.760 --> 0:17:06.520
<v Speaker 1>it gives you the impression of what you're looking at,

0:17:06.640 --> 0:17:09.639
<v Speaker 1>but its face is still there. It's very cool. Uh.

0:17:09.760 --> 0:17:13.160
<v Speaker 1>My favorite kind of fossil, though, Josh, is I'm gonna

0:17:13.160 --> 0:17:16.480
<v Speaker 1>say that, like every five minutes is a frozen fossil,

0:17:16.720 --> 0:17:19.800
<v Speaker 1>because if you get trapped, let's say your wooly mammoth

0:17:19.800 --> 0:17:22.560
<v Speaker 1>trapped in ice, not only is that going to keep

0:17:22.640 --> 0:17:25.119
<v Speaker 1>other like vultures and things from picking up your bones

0:17:25.160 --> 0:17:28.680
<v Speaker 1>and skin, but it's also going to keep it from

0:17:28.680 --> 0:17:33.280
<v Speaker 1>breaking down and you can get hair fully preserved sometimes

0:17:33.920 --> 0:17:35.800
<v Speaker 1>if you're in skin and like a big mammoth. Have

0:17:35.880 --> 0:17:39.399
<v Speaker 1>you seen pictures of Liuba? Now? Liuba is a baby

0:17:39.440 --> 0:17:43.159
<v Speaker 1>wooly mammoth that was found um by a reindeer herder

0:17:43.160 --> 0:17:47.720
<v Speaker 1>in Siberia and um it was pounds or something like that,

0:17:47.760 --> 0:17:49.639
<v Speaker 1>but it would have gotten up to several tons. It

0:17:49.720 --> 0:17:54.880
<v Speaker 1>is adorable because it is a fully preserved wooly mammoth

0:17:54.880 --> 0:17:57.680
<v Speaker 1>baby with the wrinkles in the skin and everything. Yet

0:17:57.720 --> 0:18:00.920
<v Speaker 1>it spent forty five years in the permafros, but it's

0:18:00.960 --> 0:18:04.760
<v Speaker 1>like completely intact. It's very cute. That's why it's my favorite.

0:18:04.840 --> 0:18:06.840
<v Speaker 1>It's one of the cutest dead things you'll ever see.

0:18:09.080 --> 0:18:11.920
<v Speaker 1>Another couple of ways you can get a fossil josh,

0:18:11.920 --> 0:18:16.720
<v Speaker 1>which are not my favorite aur tar librea tar pits,

0:18:16.720 --> 0:18:19.040
<v Speaker 1>although that is one of my favorites, which librea tar

0:18:19.119 --> 0:18:21.959
<v Speaker 1>pit is actually redundant because Librea means the tar, so

0:18:22.000 --> 0:18:25.200
<v Speaker 1>it's calling it the tar tar pit and not the tartar.

0:18:25.960 --> 0:18:27.520
<v Speaker 1>Did I ever tell you about when I shot a

0:18:27.520 --> 0:18:30.199
<v Speaker 1>commercial there? Have you? Did you go by there in

0:18:30.320 --> 0:18:32.600
<v Speaker 1>l A? No? I want to. I forgot about it

0:18:32.600 --> 0:18:34.919
<v Speaker 1>when we're there last Well, for those of you haven't been,

0:18:34.960 --> 0:18:37.960
<v Speaker 1>it's right in the middle of Los Angeles, like south

0:18:38.000 --> 0:18:40.720
<v Speaker 1>of Hollywood on Wilson Boulevard, and it's um. The main

0:18:40.840 --> 0:18:46.040
<v Speaker 1>tar pit is uh. Tar pits are fenced off, obviously,

0:18:46.520 --> 0:18:48.919
<v Speaker 1>and they have little recreations. It's it's actually the saddest

0:18:48.960 --> 0:18:51.000
<v Speaker 1>thing you'll ever see. The recreation they have in there

0:18:51.080 --> 0:18:53.680
<v Speaker 1>is of a like I guess it's a mother wooly

0:18:53.760 --> 0:18:56.280
<v Speaker 1>mammoth trapped in the tar trying to get out and

0:18:56.320 --> 0:18:59.800
<v Speaker 1>the father and the baby on shore like howling at her.

0:19:00.440 --> 0:19:03.280
<v Speaker 1>It's awful, but it's still active, like all the tars

0:19:03.320 --> 0:19:06.400
<v Speaker 1>bubbling up and everything. And shot a commercial there once

0:19:06.400 --> 0:19:08.000
<v Speaker 1>and I was on the other side of the property,

0:19:08.960 --> 0:19:11.560
<v Speaker 1>far away from the main pit, and I looked down

0:19:12.440 --> 0:19:15.399
<v Speaker 1>and there was a little mini tar pit, a little

0:19:15.400 --> 0:19:20.080
<v Speaker 1>tar puddle about a foot wide, bubbling right beneath my feet.

0:19:20.640 --> 0:19:22.760
<v Speaker 1>I could have scooped it up with my finger if

0:19:22.760 --> 0:19:26.800
<v Speaker 1>I had been so inclined. Yeah, instead, you're like, that stinks. Well,

0:19:26.840 --> 0:19:30.560
<v Speaker 1>it's just crazy to think that that's still like it's happening. Apparently,

0:19:30.760 --> 0:19:33.680
<v Speaker 1>Um I looked it up. There's um there's like you said,

0:19:33.720 --> 0:19:36.480
<v Speaker 1>main pits that are chained off and that are still

0:19:36.480 --> 0:19:39.479
<v Speaker 1>being excavated. But they have them like in neighborhoods all

0:19:39.520 --> 0:19:42.880
<v Speaker 1>around the area and parks. They're just kind of all

0:19:42.920 --> 0:19:45.200
<v Speaker 1>over the place around there. That's like parts of stone

0:19:45.200 --> 0:19:47.760
<v Speaker 1>Mountain popping up all over the place. We used to

0:19:47.800 --> 0:19:50.560
<v Speaker 1>have We had a big chunk of stone mountain in

0:19:50.560 --> 0:19:53.760
<v Speaker 1>our backyard growing up, all right. For those of you

0:19:53.800 --> 0:19:56.359
<v Speaker 1>don't know, Stone Mountain is the world's largest exposed piece

0:19:56.359 --> 0:19:58.760
<v Speaker 1>of granite, and it is right here in our home state,

0:19:59.040 --> 0:20:01.359
<v Speaker 1>and it takes like thirty minutes to hike, but you

0:20:01.400 --> 0:20:02.800
<v Speaker 1>still get to get to the top and be like

0:20:02.840 --> 0:20:06.320
<v Speaker 1>I just hiked a mountain, which I have, Josh. You

0:20:06.320 --> 0:20:10.720
<v Speaker 1>can also get a pete mossy pete can preserve life forms,

0:20:10.720 --> 0:20:14.320
<v Speaker 1>including human beings like Tolin Man was. It was that

0:20:14.520 --> 0:20:16.639
<v Speaker 1>Toland Man. I don't know about him. How do you

0:20:16.680 --> 0:20:21.000
<v Speaker 1>know all these people people? The first the first um

0:20:21.240 --> 0:20:25.040
<v Speaker 1>multi syllable word I could spell was archaeology. Really, I've

0:20:25.080 --> 0:20:27.840
<v Speaker 1>always been interested in that. I could see that, Yeah,

0:20:27.880 --> 0:20:31.439
<v Speaker 1>Tolin Man. Also, it doesn't you can hate archaeology like

0:20:31.480 --> 0:20:34.119
<v Speaker 1>some people hate art, and you'll still be interested in

0:20:34.160 --> 0:20:37.720
<v Speaker 1>Totland man Um he was. He's found in Denmark. He

0:20:37.800 --> 0:20:43.000
<v Speaker 1>lived years ago and he was murdered, uh sacrificially, they think,

0:20:43.440 --> 0:20:45.840
<v Speaker 1>and cast into the peat bog, which pete is just

0:20:45.920 --> 0:20:49.680
<v Speaker 1>decomposing moss and lots of it, but it has a tendency.

0:20:49.720 --> 0:20:53.159
<v Speaker 1>I think it's anaerobic, so um tissue is preserved really well.

0:20:53.440 --> 0:20:55.600
<v Speaker 1>But it's this guy that they dug up, and he's

0:20:55.640 --> 0:20:57.280
<v Speaker 1>so well preserved that when they found him in the

0:20:57.359 --> 0:20:59.760
<v Speaker 1>nineteen fifties, they called the cops because they thought they'd

0:20:59.760 --> 0:21:02.720
<v Speaker 1>found a murder victim really like a recent one. He

0:21:02.760 --> 0:21:05.400
<v Speaker 1>looks kind of funny, but he's got his whiskers are preserved.

0:21:05.640 --> 0:21:08.200
<v Speaker 1>He's wearing a cap. He still has this the garrett

0:21:08.280 --> 0:21:11.480
<v Speaker 1>around his neck. Um, it's really awesome. So what is

0:21:11.520 --> 0:21:15.359
<v Speaker 1>he dated at? Like three four hundred BC? Is the

0:21:15.359 --> 0:21:18.760
<v Speaker 1>one who was killed and he's wearing a hat yeah, sheepskin,

0:21:18.920 --> 0:21:23.600
<v Speaker 1>leather cap. Yeah, no last chance garage for him? No?

0:21:23.720 --> 0:21:26.399
<v Speaker 1>Well uh? And then my favorite way, Josh, that you

0:21:26.400 --> 0:21:30.239
<v Speaker 1>can get a fossil is uh, you're joking? Did you

0:21:30.280 --> 0:21:33.160
<v Speaker 1>say it again? I did? Is amber? They just keep

0:21:33.200 --> 0:21:35.880
<v Speaker 1>getting better and better, like the movie Jurassic Park. Yeah,

0:21:35.920 --> 0:21:38.760
<v Speaker 1>that's how we get dinosaurs again. Yeah, dino d n A.

0:21:39.440 --> 0:21:43.760
<v Speaker 1>So you found something on on whether or not that's feasible, right, yeah,

0:21:43.800 --> 0:21:46.200
<v Speaker 1>because I always wondered. You know, when you see Jurassic Park,

0:21:46.280 --> 0:21:48.879
<v Speaker 1>you see the little video they made it clearly to

0:21:48.920 --> 0:21:51.040
<v Speaker 1>explain to the movie going audience how this is done.

0:21:51.320 --> 0:21:55.720
<v Speaker 1>It's better than Ellen Page running around. What was that

0:21:55.760 --> 0:22:00.680
<v Speaker 1>movie inception? Um, so the mosquito flies in tree residentry

0:22:00.680 --> 0:22:04.639
<v Speaker 1>resident eventually becomes hard as copal, than it eventually becomes

0:22:04.720 --> 0:22:07.560
<v Speaker 1>inert as amber. You get the little mosquito in there.

0:22:07.600 --> 0:22:10.400
<v Speaker 1>They extracted the dino DNA from the blood of the mosquito,

0:22:11.080 --> 0:22:14.879
<v Speaker 1>filled in the gaps with I think frog DNA, and

0:22:14.880 --> 0:22:16.600
<v Speaker 1>that was all there was to it. And at the

0:22:16.640 --> 0:22:19.280
<v Speaker 1>time I thought boom. But being bon Jovi, yeah, at

0:22:19.320 --> 0:22:22.080
<v Speaker 1>the time, I thought that seems plausible, and it sort

0:22:22.119 --> 0:22:24.040
<v Speaker 1>of is. But I did look up today and there

0:22:24.080 --> 0:22:27.520
<v Speaker 1>was a researcher that was interviewed at the or closer

0:22:27.560 --> 0:22:30.160
<v Speaker 1>to that time. I think that basically debunked it and said,

0:22:30.960 --> 0:22:33.920
<v Speaker 1>we could potentially maybe get some DNA, even though it's

0:22:33.960 --> 0:22:38.400
<v Speaker 1>really fragile and loses his signature really quickly. Even if

0:22:38.400 --> 0:22:42.479
<v Speaker 1>you could get the DNA, he said that you couldn't

0:22:42.520 --> 0:22:44.919
<v Speaker 1>construct a dinosaurs just you can't fill in the blanks

0:22:44.920 --> 0:22:46.879
<v Speaker 1>like that. There's way too many blanks. You have a

0:22:47.320 --> 0:22:52.240
<v Speaker 1>giant frog, yeah, with little tiny arms forearms that Steven

0:22:52.240 --> 0:22:54.720
<v Speaker 1>Spielberg made us belief when you saw those dinosaurs walk

0:22:54.760 --> 0:22:57.320
<v Speaker 1>across that field. That guy can make me believe in anything.

0:22:57.840 --> 0:23:01.639
<v Speaker 1>That aliens came to the American Southwest, that there was

0:23:01.680 --> 0:23:06.440
<v Speaker 1>a World War two, that um each phone home. Yeah,

0:23:07.640 --> 0:23:33.800
<v Speaker 1>good stuff. Though, where are we here, chuck it. We're

0:23:33.840 --> 0:23:35.800
<v Speaker 1>kind of painting this picture where if like you just

0:23:35.920 --> 0:23:38.159
<v Speaker 1>stick a shovel anywhere on the Earth, you're gonna yield

0:23:38.200 --> 0:23:41.160
<v Speaker 1>like all sorts of bones and fossils. Note no, it's

0:23:41.160 --> 0:23:46.320
<v Speaker 1>not um First of all, a mere fraction that I

0:23:46.320 --> 0:23:49.200
<v Speaker 1>don't think could possibly be calculated, because we rely on

0:23:49.240 --> 0:23:53.080
<v Speaker 1>the fossil record to show us what existed back when,

0:23:53.720 --> 0:23:56.720
<v Speaker 1>and it's incomplete. Therefore we've entered to catch twenty two.

0:23:57.200 --> 0:24:00.159
<v Speaker 1>But there's just a mere fraction of all of the

0:24:00.200 --> 0:24:06.480
<v Speaker 1>species and organisms that's ever lived that become fossilized um Like. Basically,

0:24:06.480 --> 0:24:09.800
<v Speaker 1>a perfect storm of chance has to occur for a

0:24:09.840 --> 0:24:12.800
<v Speaker 1>fossil to be created. As we've seen, even when it

0:24:12.880 --> 0:24:16.679
<v Speaker 1>is created, it can still be crushed into oblivion. Um.

0:24:17.160 --> 0:24:21.280
<v Speaker 1>And so there are few and far between. To begin with,

0:24:22.720 --> 0:24:24.760
<v Speaker 1>what we have to figure out where to find them.

0:24:25.000 --> 0:24:26.960
<v Speaker 1>While then you got to find it. That's the other problem.

0:24:26.960 --> 0:24:29.680
<v Speaker 1>And the way we find it is by identifying rock

0:24:29.880 --> 0:24:33.520
<v Speaker 1>that will likely have the type of fossil that we're

0:24:33.520 --> 0:24:36.640
<v Speaker 1>looking for. Yeah, so you want something that from that year.

0:24:36.720 --> 0:24:40.320
<v Speaker 1>So if you know that this animal from yeah, if

0:24:40.359 --> 0:24:42.280
<v Speaker 1>you if you know this this animal lived, you know,

0:24:42.320 --> 0:24:44.520
<v Speaker 1>thirty million years ago, you're gonna go find rock that

0:24:44.560 --> 0:24:47.280
<v Speaker 1>you know is thirty million years old and start poking

0:24:47.320 --> 0:24:51.200
<v Speaker 1>around and you know, looking this sort of a very

0:24:51.800 --> 0:24:55.119
<v Speaker 1>chance thing, and we know that, um, we know, like

0:24:55.280 --> 0:24:58.520
<v Speaker 1>say a layer of rock or strata of rock is

0:24:58.640 --> 0:25:01.880
<v Speaker 1>thirty million years old because of a technique we have

0:25:02.000 --> 0:25:07.560
<v Speaker 1>called radiocarbon dating. Right, yeah, you want to do this one? Well? Sure,

0:25:08.160 --> 0:25:10.359
<v Speaker 1>Carbon fourteen dating is what a lot of people toss

0:25:10.400 --> 0:25:12.959
<v Speaker 1>around because it's probably the most well known, But that

0:25:13.000 --> 0:25:16.960
<v Speaker 1>can only take you back sixty thousand years. We're talking

0:25:17.040 --> 0:25:20.240
<v Speaker 1>millions and billions of years. So they need to uh

0:25:20.800 --> 0:25:25.280
<v Speaker 1>study isotopes like potassium forty and uranian two thirty eight

0:25:25.320 --> 0:25:27.640
<v Speaker 1>because that goes back millions of years. Evidently. The half

0:25:27.640 --> 0:25:31.160
<v Speaker 1>life yeah, and the half life is where an atom

0:25:31.240 --> 0:25:35.879
<v Speaker 1>loses half of its life isotopes to decay. Yeah, okay,

0:25:36.160 --> 0:25:39.840
<v Speaker 1>and these the this um radioactive decay takes place at

0:25:39.840 --> 0:25:44.080
<v Speaker 1>a predictable rate depending on the atom, the type of atom. Right, Yeah,

0:25:44.160 --> 0:25:47.720
<v Speaker 1>that's how I understand it. So if we find a

0:25:47.800 --> 0:25:52.240
<v Speaker 1>type of atom missing x number of isotopes, we can say, well,

0:25:52.280 --> 0:25:55.320
<v Speaker 1>this is roughly thirty million to thirty one million years old,

0:25:55.400 --> 0:25:59.240
<v Speaker 1>or thirty million to thirty million and three hundred years old.

0:25:59.640 --> 0:26:02.000
<v Speaker 1>I'm not sure what window we can date it to, right,

0:26:03.160 --> 0:26:04.840
<v Speaker 1>but I think it's enough so that you know, we

0:26:04.920 --> 0:26:07.919
<v Speaker 1>have a rough estimate of of you know, when this

0:26:08.040 --> 0:26:11.680
<v Speaker 1>fossil lived in the sediment was buried around it. So, Josh,

0:26:11.720 --> 0:26:16.320
<v Speaker 1>let's say that you're lucky enough and skilled enough as

0:26:16.359 --> 0:26:20.840
<v Speaker 1>an intrepid paleontologist to come across your fossil. What do

0:26:20.880 --> 0:26:25.479
<v Speaker 1>you do? Well, as I said, you dig it up

0:26:25.520 --> 0:26:27.800
<v Speaker 1>and take it to the museum and sell it for

0:26:27.840 --> 0:26:31.480
<v Speaker 1>five Smolan Well, I don't know about that, but you

0:26:31.480 --> 0:26:34.040
<v Speaker 1>should call a museum. Even if you think you know

0:26:34.080 --> 0:26:37.000
<v Speaker 1>what you're doing, Uh, you're probably gonna need some help

0:26:37.000 --> 0:26:39.399
<v Speaker 1>if it's something major. I think you should probably go

0:26:39.440 --> 0:26:41.960
<v Speaker 1>on the assumption that you don't know what you're doing

0:26:43.160 --> 0:26:46.840
<v Speaker 1>unless you're a trained paleontologist. Um. Part of the problem

0:26:46.920 --> 0:26:50.560
<v Speaker 1>is is we assume that these fossils, being rocks, are sturdy.

0:26:50.680 --> 0:26:53.240
<v Speaker 1>That's not always the case. So there's a lot of

0:26:53.359 --> 0:26:58.480
<v Speaker 1>danger of damage um in a just an average joe

0:26:58.920 --> 0:27:01.720
<v Speaker 1>trying to excavate him. Also, if you just pull a

0:27:01.720 --> 0:27:05.000
<v Speaker 1>bone up and walk away with it, Uh, it immediately

0:27:05.040 --> 0:27:07.840
<v Speaker 1>loses context. Yeah, it's like removing a piece of evidence

0:27:07.880 --> 0:27:10.960
<v Speaker 1>from a crime scene almost exactly. I can't do that. Well,

0:27:10.960 --> 0:27:14.359
<v Speaker 1>you're not supposed to. Uh. So you know, they have

0:27:14.440 --> 0:27:18.360
<v Speaker 1>these huge cranes and uh digging tools where they can

0:27:18.400 --> 0:27:21.680
<v Speaker 1>remove huge slabs of earth, which is a really good

0:27:21.680 --> 0:27:23.760
<v Speaker 1>way to do it. And sometimes if they're you know,

0:27:23.800 --> 0:27:26.440
<v Speaker 1>if it's something that could be fragile, they will remove

0:27:26.480 --> 0:27:29.639
<v Speaker 1>the entire slab, cast it in plaster and just go

0:27:29.680 --> 0:27:32.439
<v Speaker 1>ahead and ship that thing off to a facility to

0:27:32.480 --> 0:27:35.040
<v Speaker 1>handle it from there. And the cool thing is is,

0:27:35.080 --> 0:27:38.760
<v Speaker 1>even though rock has formed around this bone, yeah, that's

0:27:38.840 --> 0:27:41.800
<v Speaker 1>key right up right, all up on it, all up

0:27:41.800 --> 0:27:45.640
<v Speaker 1>in it. If you um flake it away properly, if

0:27:45.640 --> 0:27:48.680
<v Speaker 1>you flake the surrounding sedimentary rock away, um, you're going

0:27:48.760 --> 0:27:51.400
<v Speaker 1>to find that there's what's called the plane of weakness,

0:27:52.080 --> 0:27:55.120
<v Speaker 1>which is where the bone and the rock are still

0:27:55.400 --> 0:27:59.360
<v Speaker 1>on this very microscopic level. They're not fused together. You're

0:27:59.359 --> 0:28:02.200
<v Speaker 1>gonna hit that and the rock should chip right away,

0:28:02.400 --> 0:28:04.879
<v Speaker 1>right and and leave the bone. Yeah, And I think

0:28:04.960 --> 0:28:07.080
<v Speaker 1>sometimes they missed it with water too, to soften it

0:28:07.160 --> 0:28:10.159
<v Speaker 1>up and help the whole process. Another thing too, if

0:28:10.160 --> 0:28:13.679
<v Speaker 1>they find that is really brittle, they can actually reinforce

0:28:13.760 --> 0:28:17.080
<v Speaker 1>the bone with resin and thin glue. But you need

0:28:17.119 --> 0:28:20.920
<v Speaker 1>to be careful there too, which is pretty much helping

0:28:20.960 --> 0:28:24.000
<v Speaker 1>along the fossilization process. Yeah, I would think so. I

0:28:24.040 --> 0:28:26.240
<v Speaker 1>mean it's the same thing. It's like artificial forcing it

0:28:26.320 --> 0:28:29.320
<v Speaker 1>with something sturdy. Well, and then you can date it

0:28:29.400 --> 0:28:33.080
<v Speaker 1>using your little mass spectrometer that's in your pocket, and

0:28:33.400 --> 0:28:36.760
<v Speaker 1>or a cat scan sometimes they use cat scans computer

0:28:36.840 --> 0:28:39.440
<v Speaker 1>imaging stuff like that. Yeah, I didn't I didn't get

0:28:39.440 --> 0:28:41.640
<v Speaker 1>how they were dating it from cat scan. I don't

0:28:41.640 --> 0:28:45.400
<v Speaker 1>know if they're dating it with a cat scan or

0:28:45.480 --> 0:28:48.400
<v Speaker 1>just sussen the whole thing out. Gotcha. I don't think

0:28:48.400 --> 0:28:50.840
<v Speaker 1>it's a dating situation. Tracy was just throwing out some

0:28:51.680 --> 0:28:56.320
<v Speaker 1>extra tools of the trade. Huh Yeah, exactly, gotcha. So, um, chuck,

0:28:56.720 --> 0:28:59.400
<v Speaker 1>what is all this worth? I mean, we we have

0:28:59.560 --> 0:29:03.880
<v Speaker 1>a thirst for knowledge. Obviously people think bones are very cool,

0:29:04.480 --> 0:29:08.760
<v Speaker 1>But ultimately, what's the pursuit of paleontology to to put

0:29:08.840 --> 0:29:13.160
<v Speaker 1>together the piece of the puzzle of how we got here? Right?

0:29:13.480 --> 0:29:15.640
<v Speaker 1>I mean that's what I think. Yeah, that's my understanding

0:29:15.680 --> 0:29:18.120
<v Speaker 1>as well. Yeah, you can learn a lot by not

0:29:18.240 --> 0:29:21.239
<v Speaker 1>only finding the fossil, but finding what was with the

0:29:21.280 --> 0:29:26.920
<v Speaker 1>fossil in that same strata. Ah, I can tell you, like, hey,

0:29:26.960 --> 0:29:30.480
<v Speaker 1>this is a t rex bone and there's also a

0:29:30.480 --> 0:29:33.280
<v Speaker 1>bit of pine tree, so we know pine trees were around,

0:29:33.840 --> 0:29:35.480
<v Speaker 1>and they may have eaten pine trees while not the

0:29:35.480 --> 0:29:38.800
<v Speaker 1>t rex because they were carnivores, right, Um, yeah, they

0:29:38.800 --> 0:29:44.720
<v Speaker 1>were herbivore. Let's say, you know what I mean, Abronosaurus. Sure. Um.

0:29:44.800 --> 0:29:47.960
<v Speaker 1>And ultimately all of these fossils come together, plant and well,

0:29:47.960 --> 0:29:50.719
<v Speaker 1>everything that we can get our hands on to form

0:29:50.880 --> 0:29:53.840
<v Speaker 1>what is called the fossil record, right, and this is

0:29:53.880 --> 0:29:57.680
<v Speaker 1>basically the record of life on Earth. Uh. It's also

0:29:57.800 --> 0:30:01.800
<v Speaker 1>used to support evolution big time. And uh it's here

0:30:01.840 --> 0:30:09.240
<v Speaker 1>that paleontology gets most contentious, right yeah, sure, because there's, um,

0:30:09.440 --> 0:30:13.480
<v Speaker 1>the the idea that beings evolved if you go far

0:30:13.600 --> 0:30:17.719
<v Speaker 1>enough back from a single common ancestor, right. And so

0:30:17.840 --> 0:30:21.520
<v Speaker 1>if we can put together a complete fossil record, we

0:30:21.560 --> 0:30:24.880
<v Speaker 1>would be able to see how everything alive today evolve

0:30:25.040 --> 0:30:29.600
<v Speaker 1>from this common ancestor or common ancestors. Right. Yeah. The

0:30:29.680 --> 0:30:33.080
<v Speaker 1>problem is fossil records incomplete, and one of the really

0:30:33.240 --> 0:30:37.200
<v Speaker 1>key parts that it's often missing are called transitional fossils. Right.

0:30:37.720 --> 0:30:40.520
<v Speaker 1>My favorite kind of fossil, Josh is a transitional fossil.

0:30:41.080 --> 0:30:45.240
<v Speaker 1>And one example Tracy used was the baleen whale. Uh.

0:30:45.280 --> 0:30:47.080
<v Speaker 1>There there's a picture of one actually in the article

0:30:47.160 --> 0:30:49.640
<v Speaker 1>twenty five million year old fossil of of the baleen

0:30:49.680 --> 0:30:53.880
<v Speaker 1>whale with sharp teeth. Um. Today's bailing whales don't have

0:30:53.960 --> 0:30:56.920
<v Speaker 1>sharp teeth, but we know that once before this had

0:30:56.960 --> 0:31:00.560
<v Speaker 1>sharp teeth and legs. So this is a transitional fossil

0:31:00.600 --> 0:31:03.560
<v Speaker 1>that shows, well, they used to have legs and sharp teeth,

0:31:03.560 --> 0:31:05.400
<v Speaker 1>then they just had sharp teeth, and now they don't

0:31:05.400 --> 0:31:08.959
<v Speaker 1>have legs or sharp teeth. They're defenseless, which is why

0:31:09.000 --> 0:31:13.960
<v Speaker 1>they're baling whales, right and not sharks or megalodon's right. Um.

0:31:14.040 --> 0:31:16.800
<v Speaker 1>And so a transitional fossil is one that that pops

0:31:16.880 --> 0:31:20.800
<v Speaker 1>up between old and new, and it makes sense. Our

0:31:20.880 --> 0:31:24.240
<v Speaker 1>understanding of evolution is that it takes a little while,

0:31:24.320 --> 0:31:27.760
<v Speaker 1>and um, something like teeth aren't just gonna go away

0:31:27.800 --> 0:31:30.480
<v Speaker 1>in one generation. It's gonna take more and more and more,

0:31:30.520 --> 0:31:32.680
<v Speaker 1>and then um, we should be able to find them

0:31:32.720 --> 0:31:35.640
<v Speaker 1>along the way where maybe the teeth gets smaller. There's

0:31:35.680 --> 0:31:39.960
<v Speaker 1>fewer and fewer um baling whale teeth in the average

0:31:39.960 --> 0:31:45.520
<v Speaker 1>baling whale mouth, and you're putting together the puzzle exactly. UM. Again,

0:31:45.560 --> 0:31:48.520
<v Speaker 1>the fossil records a little incomplete, and there aren't as

0:31:48.560 --> 0:31:51.440
<v Speaker 1>many transitional fossils as I think people would like to.

0:31:52.280 --> 0:31:55.640
<v Speaker 1>UM have tied all together, right, UM, and then some

0:31:55.720 --> 0:31:58.200
<v Speaker 1>of the UH. Some of the explanations are Probably the

0:31:58.240 --> 0:32:02.680
<v Speaker 1>most famous explanation for this is that UM evolution isn't gradual.

0:32:03.480 --> 0:32:05.400
<v Speaker 1>I think it's Stephen J. Gould came up with the

0:32:05.480 --> 0:32:10.280
<v Speaker 1>idea of punctuated equilibrium, and that is basically that UM

0:32:10.440 --> 0:32:15.960
<v Speaker 1>evolution takes place suddenly in these huge quick fits and starts,

0:32:16.560 --> 0:32:19.840
<v Speaker 1>which would explain why there's not like teeth don't go

0:32:19.880 --> 0:32:22.640
<v Speaker 1>away in a generation, but they go away a lot

0:32:22.720 --> 0:32:27.080
<v Speaker 1>faster than we used to suspect. And that's why these

0:32:27.280 --> 0:32:31.680
<v Speaker 1>UM fossils UM, accompanied with the idea that not every

0:32:31.880 --> 0:32:34.680
<v Speaker 1>animal that's ever died has become fossilized, explained why there's

0:32:34.720 --> 0:32:37.640
<v Speaker 1>huge gaps in the fossil record, which will inevitably always

0:32:37.680 --> 0:32:42.200
<v Speaker 1>be incomplete. Is that a hypothesis at this point? I

0:32:42.200 --> 0:32:46.320
<v Speaker 1>guess it is not a theory yet I don't. I

0:32:46.360 --> 0:32:48.880
<v Speaker 1>don't think so. I think it is a hypothesis. I

0:32:48.960 --> 0:32:51.040
<v Speaker 1>got one more thing, Okay, I'd like to finish with

0:32:51.080 --> 0:32:53.960
<v Speaker 1>my favorite kind of fossil, and that is a living fossil.

0:32:55.160 --> 0:32:58.680
<v Speaker 1>And that, Josh, is when you've got a plant or

0:32:58.720 --> 0:33:03.320
<v Speaker 1>animal that looks so much like ancient fossils that they

0:33:03.360 --> 0:33:08.160
<v Speaker 1>consider a living fossil. Allah, the horseshoe crab. Right, apparently

0:33:08.160 --> 0:33:11.320
<v Speaker 1>the horseshoe crab has not changed. Didn't need too. It's perfect.

0:33:11.520 --> 0:33:15.160
<v Speaker 1>I look at it, it's gorgeous. What else, oh, Genko

0:33:15.200 --> 0:33:18.320
<v Speaker 1>baloba plants. And then a word that I don't know,

0:33:19.720 --> 0:33:22.640
<v Speaker 1>the Cela cant. What is that? Uh, it's this horrid

0:33:22.680 --> 0:33:26.720
<v Speaker 1>looking fish that they remember that VW commercial where he's

0:33:26.800 --> 0:33:28.880
<v Speaker 1>like it's like the Ceila camp and the guys like

0:33:28.920 --> 0:33:31.040
<v Speaker 1>what they're looking in the trunk and he's like a

0:33:31.080 --> 0:33:34.320
<v Speaker 1>full size spare tire. He's like, it's like a Ceila cant.

0:33:34.320 --> 0:33:36.720
<v Speaker 1>They used to think it was extinct. There was a fish,

0:33:36.760 --> 0:33:39.360
<v Speaker 1>and then they found it like in the nineteen thirties again.

0:33:39.840 --> 0:33:42.640
<v Speaker 1>But it's this dinosaur looking fish. Oh, I think I've

0:33:42.640 --> 0:33:44.880
<v Speaker 1>seen him that they thought was extinct for millions of

0:33:44.960 --> 0:33:47.280
<v Speaker 1>years and they called him and I think in South America,

0:33:47.280 --> 0:33:49.840
<v Speaker 1>off the coast of South America, and they're still around.

0:33:52.280 --> 0:33:55.120
<v Speaker 1>And the horseshoe Crab and Stephen J. Gould in the

0:33:55.120 --> 0:33:58.760
<v Speaker 1>Genko Baloba. Well, it's it for fossils, right, that's all

0:33:58.760 --> 0:34:00.640
<v Speaker 1>I have. I think we've got the point across. It's

0:34:00.640 --> 0:34:03.560
<v Speaker 1>an overview. A fossil is a rock. Just remember that,

0:34:03.640 --> 0:34:08.160
<v Speaker 1>Okay if you want to learn more about fossils. Um Seriously,

0:34:08.200 --> 0:34:10.000
<v Speaker 1>this is one of the better articles on the site.

0:34:10.040 --> 0:34:13.640
<v Speaker 1>Tracy did a great job with it. Type fossils into

0:34:13.800 --> 0:34:17.080
<v Speaker 1>the search bar, the handy search bar, and how stuff

0:34:17.080 --> 0:34:23.120
<v Speaker 1>works dot com, which means it's time for listener mail. Josh,

0:34:23.160 --> 0:34:26.640
<v Speaker 1>we made a young girl cry. That's what I'm gonna

0:34:26.640 --> 0:34:28.839
<v Speaker 1>call this one. Okay, It's probably happened more than once.

0:34:29.680 --> 0:34:32.000
<v Speaker 1>Uh I, guys and Jerry. My name is Ali. I'm

0:34:32.000 --> 0:34:35.080
<v Speaker 1>from Indiana. I was in the I S s M,

0:34:35.120 --> 0:34:39.200
<v Speaker 1>a band contest, playing a difficult marimba solo today. I

0:34:39.280 --> 0:34:41.759
<v Speaker 1>was pretty nervous, but being first chair and the only

0:34:41.800 --> 0:34:45.160
<v Speaker 1>female percussionist in my school really brought up my confidence.

0:34:45.200 --> 0:34:48.200
<v Speaker 1>I went in, I choked, and I stumbled through my piece.

0:34:49.239 --> 0:34:52.360
<v Speaker 1>You could get a gold, silver bronze, or a participation metal.

0:34:53.760 --> 0:34:56.279
<v Speaker 1>Got the bronze, which is equivalent to a score of

0:34:56.320 --> 0:35:00.000
<v Speaker 1>an F. I was really upset. Wait, what is participating?

0:35:00.760 --> 0:35:03.800
<v Speaker 1>That's sub f I didn't even know they made medals.

0:35:03.800 --> 0:35:05.680
<v Speaker 1>I thought it was just a ribbon. It's probably a ribbon.

0:35:06.880 --> 0:35:08.600
<v Speaker 1>I was really upset. I got home. I was trying

0:35:08.600 --> 0:35:11.239
<v Speaker 1>to cheer myself up by listening to your podcast on

0:35:11.280 --> 0:35:13.759
<v Speaker 1>What's the Deal with Stinkholes. I really love the show,

0:35:13.760 --> 0:35:15.880
<v Speaker 1>and I've listened almost everyone, But in the beginning, you

0:35:15.880 --> 0:35:19.759
<v Speaker 1>guys talked about how much the Bronze medals suck. Remember that.

0:35:19.880 --> 0:35:22.879
<v Speaker 1>Oh yeah, so we didn't lift spirits very much, Josh

0:35:22.960 --> 0:35:24.239
<v Speaker 1>and Chuck. I just want to let you know that

0:35:24.280 --> 0:35:27.320
<v Speaker 1>the two of you made me cry then from Ali

0:35:27.400 --> 0:35:29.799
<v Speaker 1>and I have since written Alie back and apologized, and

0:35:29.840 --> 0:35:32.439
<v Speaker 1>she said that she's feeling much better now and uh,

0:35:32.719 --> 0:35:35.080
<v Speaker 1>it wasn't our fault. And I told her that I've

0:35:35.160 --> 0:35:39.719
<v Speaker 1>choked under pressure many times in my life and it happens,

0:35:40.360 --> 0:35:42.960
<v Speaker 1>and it will happen again, and it doesn't mean you

0:35:42.960 --> 0:35:46.359
<v Speaker 1>don't have the goods with your solo every single time. Yeah,

0:35:46.520 --> 0:35:48.560
<v Speaker 1>but you know you pick yourself up. It sounds like

0:35:48.600 --> 0:35:50.239
<v Speaker 1>you gave her some good advice to choke. I think

0:35:50.239 --> 0:35:52.719
<v Speaker 1>so she's getting receptive to it. It's like a sweet girl.

0:35:53.600 --> 0:35:55.719
<v Speaker 1>I think that's an excellent lead in. If you have

0:35:55.800 --> 0:36:00.640
<v Speaker 1>a story about choking, not physically choking, but you there's

0:36:00.680 --> 0:36:03.080
<v Speaker 1>something you're good at and you didn't do it. Well,

0:36:03.520 --> 0:36:06.680
<v Speaker 1>say you're a television reporter in Los Angeles and you're

0:36:06.680 --> 0:36:10.000
<v Speaker 1>supposed to report on the Grammys like that. So you're

0:36:10.000 --> 0:36:11.680
<v Speaker 1>a podcaster and you have to do a show about

0:36:11.719 --> 0:36:14.600
<v Speaker 1>the sun to give one too, but we want to

0:36:14.600 --> 0:36:17.000
<v Speaker 1>hear about it. You can send it to us via email.

0:36:17.600 --> 0:36:22.120
<v Speaker 1>Just type in where it says to stuff podcast at

0:36:22.160 --> 0:36:33.000
<v Speaker 1>how stuff works dot com. For more on this and

0:36:33.080 --> 0:36:36.560
<v Speaker 1>thousands of other topics, does it how stuff works dot com.

0:36:36.719 --> 0:36:39.480
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0:36:39.560 --> 0:36:42.280
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