WEBVTT - BrainStuff Classics: Why Don't All Skeletons Become Fossils?

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<v Speaker 1>Welcome to brain Stuff production of I Heart Radio. Hey

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<v Speaker 1>brain Stuff, Lauren bog Obam here with a classic episode

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<v Speaker 1>from our previous host, Christian Sagar. In this one, we

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<v Speaker 1>wanted to explore why there have been billions of living

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<v Speaker 1>things on this earth across billions of years that life

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<v Speaker 1>has existed, but only a very few have left direct

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<v Speaker 1>fossil evidence. Hey brain Stuff, it's me Christian Sager. You know,

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<v Speaker 1>when I'm digging a six ft hole in the middle

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<v Speaker 1>of the desert, I start to wonder where are all

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<v Speaker 1>the dead animals? Shouldn't we be waiting knee deep in

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<v Speaker 1>fossils every time we go outside. I know that's morbid,

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<v Speaker 1>but you can probably guess that not every animal that

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<v Speaker 1>dies leaves behind fossil evidence. But why is that? Well,

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<v Speaker 1>just to get our terms straight, a fossil is any

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<v Speaker 1>physical remnant left behind by an organism that died long ago.

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<v Speaker 1>In many cases, fossils might only be things like preserved

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<v Speaker 1>foot prints or nest sites. But today we're looking at

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<v Speaker 1>direct remains of animal bodies, like bones. The likelihood that

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<v Speaker 1>any particular animal body will become fossilized is amazingly small.

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<v Speaker 1>It's actually less than one percent so let's look at

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<v Speaker 1>the stations of the obstacle course to fossilization. First, there's

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<v Speaker 1>body type. Fossilization has a strong preference for animals with

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<v Speaker 1>hard body parts like bones, teeth, and shells. Animals with

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<v Speaker 1>soft bodies like slugs and jellyfish, well, they usually just

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<v Speaker 1>decompose completely and disappear after death, and except in a

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<v Speaker 1>very few rare cases like freezing, dry momification and peat

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<v Speaker 1>bog preservation, the same thing happens to the soft tissues

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<v Speaker 1>on all animal bodies skin, organs, eyeballs, et cetera. They

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<v Speaker 1>all make excellent meals from microorganisms and are thus consigned

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<v Speaker 1>to the ravages of rot. The second main hurdle defossilization

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<v Speaker 1>is exposure. To become a fossil, you need to be

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<v Speaker 1>one of the rare animal bodies that is rapidly buried

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<v Speaker 1>soon after the animal dies. This is most likely to

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<v Speaker 1>happen in or near the site of a moving body

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<v Speaker 1>of water, like a river or a floodplain, where runoff

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<v Speaker 1>floodwaters or regular flow may quickly cover a dead body

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<v Speaker 1>in sediment. It might also happen in arid desert settings,

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<v Speaker 1>where wind can quickly bury animal remains in sand dunes.

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<v Speaker 1>If the remains are not rapidly buried, scavenging animals are

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<v Speaker 1>likely to scatter and then consume them. After all, nature

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<v Speaker 1>hates to pass up a free lunch, and even a

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<v Speaker 1>clean skeleton left out exposed to the elements will eventually

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<v Speaker 1>be erased by the ravages of the weather. That's decalcification, erosion,

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<v Speaker 1>and corrosion. But let's say your bones are lucky enough

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<v Speaker 1>to be rapidly buried somehow. The next big hurdle is

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<v Speaker 1>a sediment itself. A nice dry sand or alkaline mud

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<v Speaker 1>might be a good place to become a fossil, but

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<v Speaker 1>if your bones are buried in soil with a higher

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<v Speaker 1>temperature and higher acidity, your prospects are a lot slimmer.

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<v Speaker 1>Acidic environments, meaning soils with a low pH tend to

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<v Speaker 1>dissolve hydro zappatite, a calcium phosphate mineral that is a

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<v Speaker 1>main structural ingredient in our bones. So many soil types

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<v Speaker 1>on Earth will simply destroy all the bones they swallow.

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<v Speaker 1>But even in friendly sediment, over a long enough period

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<v Speaker 1>of time, bones can break down the organic proteins and

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<v Speaker 1>bones like collagen, eventually decompose and the inorganic molecules, and

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<v Speaker 1>bones can be crushed, dissolved, or otherwise destroyed by physical

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<v Speaker 1>force over the centuries. So if you want your actual

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<v Speaker 1>bone structure to survive, you have to be lucky enough

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<v Speaker 1>to undergo a little transformation. Most really ancient bones we find,

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<v Speaker 1>such as dinosaur bones, aren't the unaltered original bones that

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<v Speaker 1>were bare eed millions of years ago. Instead, they're either

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<v Speaker 1>a minerally modified versions of those bones or be stone photocopies.

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<v Speaker 1>Two processes represent the majority of these cases, perma mineralization

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<v Speaker 1>and replacement. In perma mineralization, mineral rich water seeps into

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<v Speaker 1>the buried bones and fills the pores of the bones

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<v Speaker 1>with its mineral content. These minerals form crystals inside the bones,

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<v Speaker 1>causing them to modify and harden over time. Sometimes this

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<v Speaker 1>process is also called petrification. In replacement, the original bones

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<v Speaker 1>can be completely dissolved but still leave fossil copies as

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<v Speaker 1>the mineral in the groundwater completely replaces the shape of

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<v Speaker 1>the bones over long periods of time. So let's say

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<v Speaker 1>you're the rare dead animal that wins the fossilization lottery,

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<v Speaker 1>and you just happen to pass all these tests. You

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<v Speaker 1>still have to be found. The total surface of the

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<v Speaker 1>Earth is almost two hundred millions square miles, and even

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<v Speaker 1>for a guy like me, there's only so much time

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<v Speaker 1>to dick. Today's episode was written by Joe McCormick and

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<v Speaker 1>produced by Tyler Clang. For more on this and lots

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<v Speaker 1>of other topics, was it how stuff works dot com.

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<v Speaker 1>Brain Stuff is production of iHeart Radio. For more podcasts

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