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Mammals.

They live in almost every corner of the planet.

Thousands of different species.

From tiny desert creatures

to giant ocean beasts

to us.

But when did our shared history begin?

You might think the start of the mammal story

was the extinction of the dinosaurs

some 66 million years ago...

...but the story actually begins much, much earlier...

We have the very earliest ancestors of mammals.

Those animals are four times as old

as the oldest T. rex.

...in a time when mysterious animals ruled.

They looked very different from anything alive today.

In some ways,

they looked like reptiles.

But it's from here that mammals took shape...

They were our ancestors.

...surviving a tumultuous period

in Earth's history.

It became apparent

that there were two extinction events.

Our ancestors made it through

for very specific reasons.

We had very specific adaptations as a group,

and that allowed us to make it past these extinction events.

What was the secret to our ancestors' survival

in the face of deadly catastrophes?

"Mammal Origins."

Right now, on "NOVA."

Mammals are

spectacularly diverse.

They not only survive,

but thrive in all kinds of environments.

Mammals have basically taken over the world.

There's mammals all over the land.

There's mammals that fly in the air.

There's mammals that swim in the oceans.

They range in size

from tiny elephant shrews

to gargantuan 200-ton whales.

Yet all mammal species-- more than 6,000 of them--

share many of the same basic traits.

They have hair or fur

and four chambers in their hearts.

Mammals produce milk for their young.

And they are all warm-blooded,

a trait that has long puzzled scientists.

The creatures that mammals evolved from

were cold-blooded,

and so it's a really key thing

in the history of mammals,

figuring out how and when and why

our ancestors changed their metabolism

and started warming up their bodies.

So, where does the mammal story begin?

Where do we come from?

Rewind the clock 270 million years,

to a time even before the dinosaurs.

Back then, our planet was home not only

to the ancestors of the dinosaurs and other reptiles,

but to another group, also now long gone.

Among them, creatures that would one day give rise to mammals:

the therapsids.

Paleontologists have known about them for decades,

but in 2023,

some of the oldest known remains of these enigmatic animals

were discovered in South Africa.

This skull is 266 million years old,

which is really interesting,

because it's one of the oldest fossils we have.

The snout is here, in this direction.

You can also clearly see its teeth.

This creature would have been the size of a large dog,

but with sprawling limbs like a reptile

and a cold-blooded metabolism.

So what is it that has scientists convinced

it's not a reptile?

Here is the eye.

And here, behind the eye,

there's a pit called the temporal fossa,

which is an attachment point

for the muscle that closes the jaw.

It's a defining characteristic of therapsids.

Dinosaurs, crocodiles, and many reptiles

have two of these pits, called temporal fossae,

on each side of their skulls.

But therapsids have just one pit behind each eye.

It's the place where the jaw muscles

that control biting and chewing are anchored.

And the only other group that has one pit behind each eye

is our group: mammals.

This anatomical similarity was one of the first clues

that led scientists to suspect

that mammals and therapsids

are part of the same evolutionary line.

But that's not the only evidence.

BENOÎT You can see another characteristic

that distinguishes therapsids from other animals,

and that's their teeth.

Therapsids have specialized teeth,

incisors for nipping

and back teeth known as "cheek teeth."

The two groups of teeth

are separated by rather impressive canines.

Just like mammals today,

including us humans.

These shared features helped convince scientists

that therapsids gave rise to mammals.

BENOÎT However,

if you came across any of them here today,

you wouldn't realize

that they were the ancestors of mammals,

because they looked a lot like reptiles.

Some were as big as rhinoceroses

and others as small as mice.

Some were carnivores, others herbivores.

There wasn't just one type of therapsid, but lots.

In fact, six main groups of therapsids roamed ancient Earth,

and each group included many different species,

including the 2023 fossil,

which may be from a group called the biarmosuchians,

the most ancient and primitive therapsids found so far.

Many of the other groups have more specialized traits,

like dinocephalians,

recognizable by their heads--

thick skulls with bumps.

And dicynodonts,

which are distinguished by a horny beak and tusks.

Gorgonopsians are characterized by their oversized canines,

some even larger than the teeth of a T. Rex.

Therocephalians had smaller jaws and teeth,

but were more upright and agile.

Finally, the cynodonts,

many of which were small, burrowing creatures.

Altogether, there were perhaps hundreds,

if not thousands of therapsid species

among these groups.

They were hugely varied

in their appearance and size,

much like mammals are today.

One group would lead

to the emergence of mammals on Earth

225 million years ago,

eventually evolving and then likely passing down

the most iconic mammal features:

hair,

warm blood,

and lactation.

But which group was it?

Therapsid fossils have been found on every continent,

but one part of South Africa is especially rich in clues.

The Karoo is one of the most

important fossil sites in the world.

90% of fossils found in these rocks

are therapsids, the ancestors of mammals.

Many thousands of fossils

have been discovered in the Karoo,

and every field trip delivers more fossils and new species.

This has been the case

since the first therapsid fossil was found here

in the 1830s.

In the 1900s, during apartheid,

access to dig sites was mostly limited to white scientists.

But today,

the government has opened up access

and is supporting new projects.

Now discoveries are on the rise.

But why have so many therapsid fossils been found here?

What was this place like

hundreds of millions of years ago

that allowed therapsids not only to thrive,

but to be preserved as stone?

Well, over here, you can see these rocks

and these ball structures,

they form underwater.

And accompanying with these things,

we find fossilized fishes

and also fossilized wood,

which didn't grow here,

but it was transported in by the rivers.

We also find lots of ripple marks.

Fossil evidence suggests a watery past.

But to fully understand

what the Karoo of the therapsids' time looked like,

we need to go back 300 million years,

to a time when all of today's continents

existed as one landmass:

Pangaea.

What was to become South Africa

was much closer to the South Pole

and under an ice cap.

By 265 million years ago,

the Earth was warming up.

The ice that covered the Karoo had melted,

forming an inland sea.

Over the next few million years,

the Karoo Sea filled with sediments.

It nourished lush vegetation that grew in the new wetlands.

This was the environment

where therapsids were first preserved in the Karoo.

The remains of the animals that we are finding there,

the fossils,

were once living on the banks of these rivers.

But what was life like for these ancient therapsids?

Were any mammal-like traits beginning to appear?

One of the most exciting discoveries

was made in the mid-1980s

by South African fossil collector John Nyaphuli.

John was my preparator

at the National Museum in Bloemfontein, where I worked.

He and I spent many, many years

out living in a tent,

collecting fossils.

It's not easy to find fossil.

But your eyes must be trained.

You can't find fossil anywhere.

You must go to the right areas,

because geology must first tell you

that there was, there's good place to trace.

And you must love the thing, and then you can find them.

In 1984, he said to me,

"I found some big bone in the rock."

So I went to look at it, and it was big bone.

It was sort of this size.

John started opening it up,

and we found that by the middle of the day,

we had a complete skull of an animal.

There were some teeth sticking out.

It went on into the ground, and for several months,

we started excavating it.

It took 23 years to expose that skeleton fully.

But it was a completely new species of animal,

it had never been found,

and it was a very primitive dinocephalian.

This is the most complete dinocephalian skeleton

that's yet been found in the world.

Dinocephalians were a group of early therapsids.

This remarkable specimen was more than nine feet long.

The name "dinocephalian"

comes from the Greek for "terrible heads,"

because they had especially thick skulls--

in some areas, more than four inches of solid bone.

But what was all that extra skull thickness used for?

In the French Alps, scientists are looking for clues

with a powerful X-ray source called a synchrotron.

Here, in a ring larger than seven soccer fields,

electrons circulate at almost the speed of light.

VINCENT FERNANDEZ The synchrotron radiation is so intense

that it produces 10,000 billion times more intense X-rays

than a hospital or laboratory scanner.

With this very intense signal, we're able to see

through the thickness of the fossil

and produce beautiful images.

Paleontologist Vincent Fernandez

is scanning another dinocephalian skull

found in the Karoo.

His colleague, paleontologist Julien Benoît,

is doing the analysis.

BENOÎT: Here you can see, that's the brain cavity.

And it's very small compared to the large size of the skull,

and in particular, you have that thickness of bone.

This is all bone. Wow.

This is not rock.

Why is the bone so thick here?

Back at the University of the Witwatersrand,

Julien uses the synchrotron scans

to reconstruct a 3-D model

of the organs that were once inside the skull.

You can see the brain in green.

What's really interesting about this scan

is that we can also very clearly see

this animal's inner ear.

It's shown here in purple.

This organ is used for hearing,

but also for balance,

particularly these three semicircular canals.

One here, a second here,

and the third.

Let me move the image-- it's here.

The orientation of these ear canals in the skull

suggests that this dinocephalian's head

would usually point down,

a bit like that of a goat or a sheep today.

And if mammals like these are any guide,

that might mean that the dinocephalians also engaged

in social behaviors like ramming.

As the sun rose on ancestral Earth,

dinocephalians awoke.

Living in a swampy landscape where food was abundant,

they thrived,

great herds of them perhaps living together

and interacting as a group.

With behaviors similar to some of today's mammals,

could these dinocephalians

have been the mammal ancestors?

Fossils found in the Karoo reveal

that 265 million years ago--

nearly 40 million years before

the appearance of mammals--

five therapsid groups

were living here.

And the dinocephalians

were likely the most dominant.

This is the skull of Anteosaurus,

a particularly menacing type of dinocephalian.

BENOÎT: The top of the snout is there,

and the back of the skull is there.

And this was a therapsid,

because you can see this temporal fenestra here.

It's very big,

so the jaw muscle must have been incredibly powerful.

And it is a dinocephalian

because of the thickness of the bones

that make up the whole skull.

But it's also very different

from the other species of thick-skulled dinocephalians

Julien studies.

BENOÎT: That canine here is beautifully recurved,

which is really a signature of carnivorous animals.

These Anteosaurus were large creatures,

likely predators,

some 20 feet long when fully grown.

But as successful as they might have been,

the dinocephalians weren't the only therapsid group.

They were just one part of a complex ecosystem

that included other therapsid groups.

Based on fossils found in the Karoo,

we know that many species

from all five groups of therapsids

existed alongside each other.

Like dicynodonts.

Equipped with unique beaks,

these therapsids had their own specialized feeding habits,

able to efficiently tear and clip plant material.

Carnivorous therapsids,

such as gorgonopsians, would have been a threat.

But the most fearsome was still the Anteosaurus.

This dinocephalian beast was a true apex predator

in the ancient Middle Permian Karoo.

Therapsids lived here about 265 million

to 125 million years ago.

Within that time, they came up

against more than one global catastrophe

that threatened to wipe out nearly all life on Earth.

And today, the Karoo still bears the scars.

For more than 15 years,

paleontologist Mike Day and his team have been

accumulating evidence of these large-scale extinctions.

If you were to go a little further south,

into slightly older rocks,

you'd find all those typical Middle Permian faunas:

the large dinocephalians,

the big therocephalians, and lots of dicynodonts.

But by the time you get to this sandstone behind us here,

they've all gone extinct.

Victims of a mass extinction event

called the Permian Extinction.

Fossil evidence suggests

that for as long as eight million years,

life on Earth was under tremendous pressure.

And as more and more fossils have been found

and plotted along the rock record,

scientists now believe

that within these eight million years,

there were actually two distinct extinction events.

Now, both of these mass extinctions

affected therapsids badly,

but there were survivors.

And those survivors include the ancestors of mammals.

But what caused the first of these huge events,

a global catastrophe known as the Capitanian crisis?

In terms of a smoking gun here in the Karoo,

we haven't really found any good evidence

for what caused this mass extinction here.

We do know that in Southeast China,

there was huge outpourings of lava

at about the same time,

so it's very likely that that had something to do

with the Capitanian extinction here in the Karoo.

Around 260 million years ago,

far away from the Karoo,

at the other end of Pangaea,

Earth's surface was volatile.

In what was to become China, immense molten lava flows

spread across around 100,000 square miles,

releasing vast quantities

of carbon dioxide, methane, and sulfur

into the atmosphere.

The oceans became acidified and depleted of oxygen,

and the climate changed.

This is most likely the event

that caused the Capitanian crisis.

It was disastrous for life,

particularly for large animals.

But we know that at least

some therapsids survived.

Otherwise, we wouldn't be here.

But which ones?

And how?

During the crisis,

environmental disturbances like acid rain

and a rapidly changing climate

likely ravaged the vegetation,

causing the extinction

of the large plant-eating dinocephalians.

Their carnivorous cousins

eventually suffered the same fate.

Earth's first giants, the dinocephalians,

did not survive to become our direct ancestors.

But what about the other four groups

alive in the Karoo at this time,

the gorgonopsians, with their huge teeth,

the upright and agile therocephalians,

the beaked dicynodonts,

and the primitive biarmosuchians?

Did the rest of them make it?

The Karoo fossil record reveals the survivors.

This is the Rubidge Collection of Fossils.

It was amassed largely through the enthusiasm

of my grandfather from the 1930s.

These fossils were collected by Sidney Rubidge

from sediment above a volcanic ash layer

dated to the end of the Capitanian crisis.

They show that in the Karoo,

all therapsid groups other than the dinocephalians made it,

but only some of the smallest species of each.

The largest were lost.

The question then becomes, which of these remaining groups

would give rise to the mammal line?

One of the most interesting fossils

in the Rubidge Collection

is a member of the gorgonopsian group.

Gorgonopsians were the apex predators of the time.

With the dinocephalians gone,

they became top of the food chain,

and the new species that evolved were much larger in size.

And this one is called Rubidgea atrox.

These large gorgonopsians

might have been three-and-a-half meters long.

They probably had a more leathery skin,

something like a rhino or an elephant.

They're characterized by having very large canine teeth

and large incisors for flesh eating.

Only small species of gorgonopsians

survived the Capitanian crisis,

but the Rubidge Collection shows

that as the ecosystem recovered and food returned,

these small gorgonopsians not only survived, but thrived.

Over time, they evolved to be the size of modern-day bears.

And in the fossil record, there is evidence

that some new traits might have been developing.

A gorgonopsian fossil originally found in the 1940s

recently provided new clues

to how they might have lived.

Inside this skull are the remains

of an encounter with another animal.

BENOÎT Here is a tooth stuck in its snout,

and this tooth isn't just any tooth,

it's the tooth of another gorgonopsian.

The same species.

And you can even see

that it survived the fight,

because the wound around the tooth has healed.

For Julien,

this is a sign of how these animals may have interacted.

These animals fought among themselves,

biting each other on the snout,

exactly as mammals do today

to determine dominance within groups

and also to find mates and claim territories.

Until this discovery,

the teeth of carnivorous therapsids

had been considered solely hunting weapons.

And although not direct evidence of mammal ancestry,

using them for more social interactions,

like competition,

is certainly a characteristic seen

in many mammals alive today.

But the gorgonopsians

weren't the only ones developing new behaviors.

The dicynodonts were adapting

in the post-extinction world, as well.

Perhaps the most varied of the therapsids,

they came in a wide range of sizes,

some as small as guinea pigs.

The only known therapsid group with beaks,

some also had tusks.

What was it about the dicynodont group that helped it survive?

A fossil in South Africa might hold the answer.

Here we see a new behavior in the late Permian,

where animals were starting to burrow underground

and create these really interesting spirals

with a chamber underneath, where they would live.

We can see it here because it's actually preserved as a cast.

This cast is natural.

A flood poured sediment into a hollow burrow,

which hardened into rock over time.

But what were these burrows used for?

How were they an advantage?

To see through this mass of rock,

a dicynodont burrow cast

was sent to the synchrotron.

And hidden inside,

fossilized remains.

This is the burrow that was discovered

with the dicynodont.

Removing the rock reveals a spectacular find.

We have the adult dicynodont.

We can see, like,

right in the middle, this big eye socket

and teeth in front.

The beak would be there, as well.

That's not all this ancient burrow was hiding.

There was another, more unexpected find.

It's like it's a,

it's a baby version of the same species.

So basically, it's telling us

that dicynodont, they were using burrows

kind of as nurseries to take care of their babies.

It appears that a semblance

of today's mammalian parent-child bond

may have existed 260 million years ago,

but it's an idea that scientists are still exploring.

What we do know is that these burrows

allowed dicynodonts to survive tough post-crisis conditions.

That kind of group sharing behavior

has a lot of different advantages.

If you're in a burrow, you're protected from predators.

You're protected from the sun.

It's, it's pretty good to be in a burrow

if it's hot outside-- hot and dry.

But how well did the other therapsid groups fare?

After the Capitanian crisis,

not all therapsid groups had the same fate.

The dinocephalians disappeared completely.

The gorgonopsians emerged as the apex predators.

As for the therocephalians,

they took second place to their larger cousins.

The biarmosuchians

were still holding on,

but also remained the most primitive.

It was the dicynodonts

who adapted best

to the changing environments.

But as some groups struggled,

the picture grew more complicated.

A new group emerged

in a post-crisis therapsid boom,

taking the number of existing therapsid groups

back up to five:

the cynodonts.

They shared a common ancestor with the therocephalians,

and it's possible that they were

actually just a sub-group of therocephalians themselves.

But one thing is certain:

one of the secrets

to their success

was their size.

Cynodonts generally were quite small.

You could hold most of them in your arms.

They also had relatively larger brains

and more specialized teeth.

With the Karoo ecosystem having recovered

from the Capitanian crisis,

the five groups of therapsids stabilized.

Cynodonts thrived, feeding off insects and other small animals.

Meanwhile, dicynodonts continued with their plant-eating diets

and still used burrows as their homes.

But this wasn't always an advantage.

Dicynodonts were also the prey of choice for therocephalians.

These larger predators were perhaps able to hunt down

entire dicynodont families.

Even so, gorgonopsians remained

the apex predators.

But, at the end of the Permian period,

another crisis.

In the rock layers of the Karoo dating to the period

after 252 million years ago,

most big dicynodonts and gorgonopsians disappear,

signaling another extinction crisis.

Was it something local to the Karoo

or more global?

Since the 1990s,

scientists have suspected that the Siberian Traps,

enormous volcanic eruptions in what is today's Russia,

were responsible.

In 2023, an international team of scientists

published a project testing the idea.

When scientists studied the rocks in Siberia,

they found that there was

an increase in mercury

in the rocks that they sampled.

So there was a mercury spike,

and they found this associated

with those volcanic eruptions.

Mercury is often associated with volcanoes.

As a volcano erupts, spewing out lava,

it also releases mercury vapor into the atmosphere.

This vapor can be transported across continents

by currents and winds.

But we did not know

whether we had such a spike in the Karoo Basin of South Africa.

If found, that spike could be evidence

that these Siberian eruptions

were responsible for the climate changes

that caused the extinction event seen in the Karoo.

So our team went to the field and we collected samples,

and we ran the analyses,

and we found that indeed,

we are finding a mercury spike in South Africa.

The therapsid extinctions in the Karoo

252 million years ago

were indeed part of a global crisis.

In the northeastern corner of Pangaea,

in what is now Siberia,

one of the biggest volcanic eruptions

life on Earth has ever seen

began.

The scale of this event would dwarf the Capitanian crisis.

The lava spread across nearly three million square miles,

an area almost as large as the U.S. Lower 48.

The eruptions lasted for at least 200,000 years.

Consequences for life were terrible.

On land, around 70% of species disappeared.

In the seas, the toll was even heavier.

Changes in acidity and oxygen levels

wiped out as many as 95% of species.

The greenhouse effect also went into overdrive,

causing temperatures to rise dramatically.

Paleontologists have dubbed this event "the Great Dying,"

and it marked the end of the Permian period.

This was the closest life has ever come

to completely dying out.

Our ancestors,

they were there when it happened and they made it through.

And if they didn't, then we wouldn't be here today.

This crisis heralded the start of a new geological era.

It transformed the planet's climate and landscape,

including in the Karoo.

But what was it like to be there?

And what did this mean for the many therapsids

that called this part of the world home?

At the Iziko South African Museum,

a dicynodont fossil sheds light on the Karoo's climate.

So here we have the skull of the animal.

The head.

There's the outline of one of its eyes, front of its nose.

And then coming around, we have the front foot.

The fingers are missing.

Then, if you follow it along,

here's the beautifully articulated

complete spine of the animal.

And the animal's kind of spread-eagle.

This unusual position can tell us

how this dicynodont died.

One of the ways in which

an animal dies of exhaustion

is actually by collapsing,

and collapsing with its feet spread out

in this very distinctive spread-eagle pose.

In the Triassic Karoo, therapsids struggled.

Hunger, thirst, and exhaustion were all common threats.

What adaptations made it possible

for any of them to survive?

In Bethulie, east of the Karoo,

the remains of a species of dicynodont known as Lystrosaurus

have given us clues.

This is an area that I like to call

the Lystrosaurus killing fields.

I've been able to map the actual embedded skeletons

throughout this entire area.

And I have 600 in situ skeletons already.

So originally, there must have been

literally many thousands.

These dicynodonts represent 95% of the therapsid fossils

discovered in this area from this time period.

But why were there so many here?

Paleontologist Jennifer Botha has discovered a clue hidden

in the microstructure of their bones.

What you are looking at here

is a cross-section through the bone.

The organic components of the bone have disappeared,

but the position of all the bone fibers

have remained in place.

So we can tell certain things about how the animal grew.

I can see these lines

running down through here through the bone.

And they represent yearly growth marks.

So if I count the number of growth marks,

I can tell how old the animal was when it died.

But how can the age at death shed light

on why Lystrosaurus was so prolific in the Karoo

during the Triassic after the Permian crisis?

Here I have a Lystrosaurus species from the Permian

on the left

and a Lystrosaurus species from the Triassic

on the right.

And highlighted in green are the number of growth marks

I have been able to count.

So I can tell that this animal

was at least eight years old when it died.

In comparison, this Triassic specimen

was only at least two years old when it died.

And very importantly,

this is a large Lystrosaurus Permian species,

and this is the largest known Triassic specimen.

So even the largest Triassic specimens

that we have ever discovered

are not fully grown.

They are at most two or three years old.

After the crisis, Lystrosauruses were dying young.

So what explains their large population?

In order to be so abundant,

they had to be breeding quite abundantly.

This suggests that the birth rate increased rapidly.

During periods of drought,

times were tough for all the animals here.

Predators, who depended on the herbivores for food,

went hungry.

The carnivorous gorgonopsians

succumbed to the hostile conditions and vanished.

And so did the biarmosuchians.

The dicynodonts were dying young,

but their rapid reproduction rates and their burrowing habits

helped them survive this period's climate chaos.

The therocephalians initially made it,

but as time went on, they, too, eventually died out.

The cynodonts survived this tumultuous period, barely.

Only two groups remained:

the dicynodonts

and the cynodonts.

The fossil record shows just how successful the dicynodonts were.

This is what this animal looked like.

It was about 50 to 70 centimeters long,

so about the size of a small pig.

Dicynodonts literally swarmed

during the first five million years of the Triassic period.

So much so that they rediversified

and gave rise to large herbivores,

as illustrated here by this skull,

which belonged to an animal that must have been roughly

the size of a modern wildebeest, weighing several hundred kilos.

And these giant dicynodonts repopulated the world.

They spread across the whole of Pangaea.

Fossil remains of dicynodonts have been found

on every continent.

But the dicynodonts weren't the only group

that found a way to adapt to their new environment.

Paleontologist Roger Smith has found a fossil

that reveals that some of the cynodonts

had discovered some of the same tricks.

Here we have an underground burrow cast

made into the ancient floodplain by a cynodont.

The architecture of the cynodont burrow

is a tube going into the ground, and when it gets to the end,

it forms this round terminal chamber.

This doesn't have a skeleton in it.

If it did have a skeleton--

and we do have skeletons in these--

they're curled up generally

with their back to the outside,

with the tail curled around against the wall.

This burrow cast could well be

a behavioral adaptation of the cynodonts to go underground

to escape the extremes of heat during the day and night,

and perhaps to even breed.

Being able to burrow,

that was a major survival strategy.

Being able to hide away.

And that is probably one of the things

that enabled our ancestors to endure.

The same adaptations that helped the dicynodonts

emerge from the first crisis eight million years before

also helped the cynodonts survive.

As the ecosystem recovered from the crisis,

the cynodonts led a relatively stable existence.

But according to the fossil record,

the dicynodonts really thrived.

Freed from the gorgonopsian threat,

they took full advantage of available ecological niches

and grew many times larger.

Meanwhile, the therapsids

weren't the only creatures doing well.

Others were starting to appear.

The top predators of the late Triassic

are things called pseudosuchians.

They're sort of the cousins of dinosaurs.

They look a bit like modern crocs.

They're covered in body armor along their back.

Soon to be found in almost every corner of the globe,

they are evidence

of yet another planet-wide environmental change:

one that would greatly impact

the therapsids and their mammal descendants.

232 million-year-old plant fossils

show new flora was developing:

the type of plants that only exist

in extremely rainy climates.

Heavy rainfall was a planet-wide phenomenon,

and paleontologists have dubbed this period

"the Carnian pluvial episode."

Over about two million years,

the climate changed from extreme to extreme:

cold to hot,

dry to wet.

In the Karoo, the desert turned green.

But only one therapsid lineage would survive this time.

Would it be the thriving and vastly varied dicynodonts

or the newly emerged cynodonts?

Which would give rise to all of mammal-kind?

To us?

The remaining therapsids had to contend

with new creatures dominating the Karoo.

Dinosaurs, like the ones in front of me,

soon become the most dominant large-bodied animals

on the landscape.

The therapsids and the other animals

that were once so common on landscapes

become much more rare.

And instead of seeing therapsids eating plants,

we'd be seeing dinosaurs like this one

browsing on the vegetation.

It was also a time when new characteristics

that would prove helpful for survival

were appearing.

And one in particular, a very mammal-like quality,

may have been the biggest advantage of all:

a metabolism that kept the body warm.

Being warm-blooded is really important.

It means that we can go outside when it's wintertime.

It means that we can be active in the morning

or when the sun's not out.

You're not like a cold-blooded animal

that's at the mercy of the sun.

And that's really unusual.

It's a superpower.

Modern-day mammals are warm-blooded.

When did this trait emerge?

And how?

It is really challenging

to figure out if a fossil species

was warm-blooded or cold-blooded.

You can't just stick a thermometer into them

and see how their body temperature changes

over the day.

So you have to look for clues in the fossils.

There's one very interesting clue,

this opening in the top of the head

for what's called a third eye.

It's, it's a bunch of cells that sense light.

It's thought that the third eye

helped ancient cold-blooded therapsids

regulate their daily activities.

In modern species, the third eye only exists

among cold-blooded animals.

Therefore, the disappearance of the third eye may be linked

to the appearance of warm-blooded metabolism.

My colleagues and I decided to look

for when the therapsids lost this third eye.

Julien and his team have studied fossils

from across the reign of the therapsids,

all the way back to almost 270 million years ago,

in the Permian period, before the Great Dying.

In the Permian, almost all therapsids had a third eye.

Then, when we enter the Triassic,

the first Triassic species still had a third eye.

But a little later,

we begin to encounter species that no longer have

a hole at the top of their skull.

They no longer had a third eye.

By 240 million years ago, the third eye

had all but vanished from the fossil record

of one therapsid group, the cynodonts.

This isn't definitive proof of warm blood,

but scientists have found another clue.

BENOÎT The most decisive argument was the study of the inner ear.

The warmer the internal body temperature of an animal,

the runnier their ear canal fluid becomes

and the thinner the tubes can be.

We were able to measure changes

in the size of the canals in cynodonts

and determine precisely that the body temperature

had increased by ten degrees

exactly here,

between this Triassic animal

and this animal

233 million years ago.

Evidence suggests that the cynodonts

were warm-blooded during the Carnian pluvial episode.

There was a time of, of fairly rapid change

in climate and in precipitation,

and being warm-blooded

would have been beneficial at that time,

because if you can control your own body temperature,

that can protect you from the whims of the weather.

What did this mean for therapsids

that were not warm-blooded?

This Carnian rainfall event had

a huge impact on the therapsids.

By about 200 million years ago,

the dicynodonts disappear from the fossil record.

There was one small group that came out on top,

the cynodonts.

And this group is the one that gave rise to mammals.

It was the small size of these cynodonts,

their ability to dig burrows, being able to grow fast,

being able to eat lots of different foods.

That's what helped make them through.

And then on the other side, they would have found

this wide-open world,

a land of new frontiers and opportunities.

230 million years ago, the cynodonts were just starting

to adapt to this new world.

How did they give rise to mammals

just five million years later?

When did the other key mammal traits,

lactation and hair,

appear in their evolution?

Hair is the insulating layer

that allows mammals to retain heat.

The rarity of hair or fur in the fossil record

has made it difficult for scientists to find exactly

when this mammal trait evolved.

But there is one type of hair that leaves a mark:

whiskers.

And although mammals are not the only animals

with whisker-like features today,

they're a sure sign that hair has evolved.

We can track the evolution of whiskers

thanks to traces left behind

by the nerve which makes them sensitive.

Whiskers help mammals detect small changes

in the world around them,

find prey, and even communicate.

They're incredibly sensitive to external surroundings.

This is because

they are connected directly to the brain

by the trigeminal nerve.

It's evidence of how this nerve emerged from cynodont skulls

that has revealed when whiskers first appeared in this line.

In animals that lived around 230 million years ago,

a single hole appears,

which is exactly what we find in modern mammals.

This single hole is the passageway

for the trigeminal nerve,

which innervates the whiskers, located here,

in this cavity.

This creature had whiskers

just after the Carnian pluvial episode,

around the same time warm-bloodedness appeared.

Coincidence?

Or could they be linked?

Typically, traits evolve at different rates

over millions of years

unless they are somehow connected.

The final missing piece in the puzzle

is the appearance of lactation,

mothers producing milk to feed their young.

When did that appear?

Lactation is tough to spot in the fossil record,

so scientists have instead turned to DNA for answers,

with tantalizing results.

The evolution of a single gene seems to be related

to all three mammalian traits.

The MSX2 gene controlled

not only the disappearance of the third eye

and the appearance of hair,

but also the appearance of mammary glands,

and, with that, lactation.

This is the most characteristic trait of mammals.

The evolution of MSX2 contributed to the emergence

of these mammalian features in cynodonts,

which they then passed on to their mammal descendants,

giving them the defining characteristics

of all mammal-kind.

But it's not the only gene responsible

for big evolutionary changes.

Whether it's turning fish fins into limbs

or developing a spoken language,

there is a set of key regulator genes

that have a profound impact

on development and evolutionary change.

At the boundary between the Triassic and Jurassic periods,

the dicynodont group had gone extinct

and the cynodonts were the last surviving therapsids.

So at last, we have an answer.

This is the group that gave rise to the mammal line

around 225 million years ago,

not long before the other therapsid lineages ended.

The very first true mammals

were tiny.

And if you saw one, it would have looked

like a little mouse or a little shrew.

They would have been covered in hair.

They would have had molar teeth.

They would have fed their babies milk.

You would recognize them as mammals,

but you would probably just think they were

some kind of little rodent scurrying around.

It wasn't easy for the newly evolved mammals,

as the dinosaurs reigned

for roughly the next 160 million years.

The fates of dinosaurs and mammals

have always been intertwined.

And while dinosaurs took over the world,

mammals went the other way.

They went small.

They evolved stronger jaw muscles

so they could bite harder.

They evolved a keener sense of hearing.

All these things would have helped them

survive in a world controlled by massive, enormous dinosaurs

that could have smashed one of these little mammals

with a single footstep.

As had been the case for the therapsids

in the extinction events they faced,

it would be primarily the smallest of the mammals

that would survive the next major crisis:

the asteroid strike that wiped out the dinosaurs

66 million years ago.

Our ancestors made it through that boundary

for very specific reasons.

We had very specific adaptations as a group

that allowed us to make it past these extinction events.

Over millions of years of evolution,

cynodonts, these small burrowing animals,

survived multiple crises,

adapting and changing to fit each new environment.

They gave rise to the mammals some 200 million years ago,

at a time when the dinosaurs

were just beginning their reign on Earth.

Mammals were not born

as a result of the extinction of the dinosaurs,

but had appeared millions of years before.

For 160 million years,

they lived alongside these giants.

And only once the dinosaurs were extinct

could the surviving mammals rise,

diversifying into the spectacular variety

we see today.

We and all mammals alive today,

we are the descendants of survivors.

So ultimately,

we come from this line

that's been small, adaptable,

a line that's been resilient, that could handle everything

that nature's been able to throw at us

over hundreds of millions of years.

With more than 270 million years

of shared evolution running through our veins...

...we are therapsids...

...just one of the thousands of modern mammal species

that are their descendants.

Long live the therapsids.