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The History of Earth - How Our Planet Formed - Full Documentary HD

1h 31m 54s5,561 words1,220 segmentsEnglish

FULL TRANSCRIPT

0:12

[Music]

0:14

The Earth, as far as we know, it's the

0:18

only home to life in the

0:22

universe. So, what makes our planet so

0:25

special?

0:30

To find answers, we must travel back in

0:35

time. See the first humans walk the

0:39

earth. Ride each colliding

0:44

continent. Face killer

0:49

dinosaurs. Dive into oceans full of

0:53

bizarre life

0:55

forms. Feel the bitter chill of global

0:59

ice ages and experience the fury of

1:03

cosmic missile

1:11

attacks. By traveling back in time, we

1:15

can piece together our planet's

1:16

incredible story and discover why all of

1:20

this and all of us are here.

1:35

[Music]

1:40

[Music]

1:42

The journey starts almost 5 billion

1:45

years

1:48

ago. There's no sign of Earth just yet.

1:55

Only the sun, a newborn star surrounded

1:58

by

2:04

dust. The Earth hasn't formed yet.

2:19

But through time, gravity pulls the dust

2:22

into tiny rocks.

2:39

To our surprise, something as complex as

2:42

a planet is made from nothing more than

2:45

dust and

2:48

rocks. Over millions of years, gravity

2:52

pulls these rocks together to form the

2:55

Earth, one of at least 100 planets

2:59

circling the sun.

3:03

[Music]

3:17

[Music]

3:25

[Music]

3:31

But 4 and a half billion years ago,

3:33

Earth looks more like hell than home.

3:37

[Music]

3:41

Up close, the temperature is over 2,000°

3:46

F. There's no air, just carbon dioxide,

3:51

nitrogen, and water

3:53

vapor. It's so hot and toxic that if we

3:57

got any closer, we'd be incinerated and

4:00

suffocated in seconds.

4:13

This newborn planet is a boiling ball of

4:16

liquid

4:24

rock. An endless ocean of

4:37

lava. A young planet called Thea is

4:40

heading straight for

4:44

Earth. The size of Mars, it travels

4:47

nearly 10

4:49

m/s, 20 times faster than a bullet.

4:53

[Music]

5:01

The intruder's gravity distorts the

5:03

Earth's surface.

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[Music]

5:17

[Music]

5:33

The blast wave races around the

5:36

planet. It's as though both young

5:39

planets turn to liquid.

5:51

Trillions of tons of debris blast out

5:53

into

6:05

[Music]

6:12

space. But over the course of a thousand

6:15

years, gravity turns the rubble into a

6:18

ring of red hot dust and rock that

6:20

circles the

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[Music]

6:28

Earth. From this ring, a balls over

6:32

2,000 m wide.

6:42

It's the birth of our

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[Music]

6:50

moon, but it's much closer than the moon

6:53

today.

6:55

just 14,000 mi away instead of a quarter

6:59

of a million

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[Music]

7:17

miles. The sun rises over a cooling

7:20

Earth and sets just 3 hours later.

7:26

The earth is spinning so fast that an

7:29

entire day lasts 6

7:34

hours. The days may pass quickly, but

7:37

the earth changes

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[Music]

7:40

slowly. To understand the making of our

7:43

planet, we need to fast forward through

7:46

millions of years.

8:12

3.9 billion years ago, a hail of meteors

8:16

attacked the Earth.

8:20

It's debris left over from the solar

8:22

systems

8:31

formation. Inside the medas are crystals

8:34

that look like grains of

8:39

salt. And inside the crystals are minute

8:42

droplets of water.

8:46

[Applause]

8:52

These deadly missiles could contain the

8:54

vital ingredient for life on Earth.

9:12

Only a small amount of water exists

9:14

inside each meteorite. But as they

9:17

bombard the Earth for over 20 million

9:19

years, pools of water

9:25

grow. The Earth's core remains molten,

9:28

but its surface has cooled enough to

9:30

form a crust.

9:32

The air is around

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[Music]

9:38

170°. In the future, there's a chance we

9:41

could swallow this very

9:43

water. Every sip, every puddle, every

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drop of water in every ocean is billions

9:51

of years old.

9:54

And it may have traveled millions of

9:56

miles to reach us, carried inside a

10:03

meteor. The Earth looks more familiar,

10:06

but it's still a dangerous

10:10

place. Winds are faster than the most

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destructive hurricanes

10:15

today. It's a mega storm whipped up by

10:18

the planet's rapid rotation.

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[Music]

10:32

The moon is so close to Earth that its

10:34

gravity is overwhelmed, creating huge

10:37

tides that race across the planet's

10:40

surface.

10:46

[Music]

11:13

But over time, the moon moves way. The

11:17

waves calm down and the planet spins

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[Music]

11:25

slower. 700 million years after the

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planet's birth, life-giving water covers

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its

11:34

surface and scattered throughout are

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tiny

11:44

islands. They seem to have appeared from

11:51

nowhere. So, how did they get

11:59

here? Molten rock bursts through the

12:02

Earth's crust and rises up through the

12:08

ocean. Over time, the lava cools,

12:11

forming a volcanic island.

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In the future, these islands will join

12:22

together to form the first

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continents. Earth now has water and

12:31

land. It's beginning to look like the

12:33

planet we call

12:36

home. But the atmosphere is still toxic

12:40

and the temperature is scorching.

12:43

Life here is

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[Music]

12:54

impossible. Since the planet's

12:57

formation, meteors have been pummeling

13:01

Earth. But now, 3.8 billion years ago,

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the assault enters a violent new phase.

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Something's disturbed the orbits of

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these

13:17

meteorites. In addition to water, the

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meteors carry something else.

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[Music]

13:32

As they dissolve, the meteorites release

13:35

minerals. Carbon and primitive proteins

13:38

made of amino acids are transported from

13:41

outer space to the bottom of the

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[Music]

13:49

ocean. Thousands of feet below the

13:52

waves, it is dark and close to freezing.

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But a dramatic illusion is taking

14:18

shape. Underwater chimneys spewing hot

14:22

liquid.

14:28

Seawater seeps down into the earth

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through cracks in the crust, collecting

14:33

minerals and gases along the way. This

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potent mixture is released back out into

14:39

the ocean, building these

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[Music]

14:47

towers. Combined with the minerals and

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chemicals from the meteorites, the water

14:52

becomes a chemical soup.

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It's impossible to know how or when, but

15:00

somehow these chemicals come together to

15:03

create

15:06

life. The water is now full of

15:09

microscopic organisms. These

15:12

single-sellled bacteria are the earliest

15:14

forms of life on Earth.

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[Music]

15:22

This is a defining moment in the making

15:25

of the

15:28

planet. Microscopic life is

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[Music]

15:42

underway. For hundreds of millions of

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years, nothing changes.

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[Music]

15:51

The only life is single-sellled

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[Music]

16:03

bacteria. To find more complex life, we

16:07

need to fast forward to 3.5 billion

16:10

years

16:14

ago and a shallow ocean.

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These look like rocks or even plants

16:29

growing out of the

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[Music]

16:34

seabed. Each mound is a colony of living

16:37

bacteria called a strummatalite.

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[Music]

16:45

These bacteria turn sunlight into food,

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a process called

16:51

photosynthesis. It uses the power of

16:53

sunlight to transform carbon dioxide and

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water into glucose, a simple form of

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sugar.

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[Music]

17:15

And this magical

17:17

transformation releases a

17:20

byproduct, a gas called

17:22

[Music]

17:26

oxygen. Underwater, the strumatalytes

17:29

slowly fill the oceans with oxygen.

17:37

The oxygen then turns traces of iron

17:40

into rust which fall to the ocean floor

17:44

to form deposits of ironrich rock. It's

17:47

this mineral that will one day be used

17:50

to build bridges, ships, and

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skyscrapers.

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[Music]

18:05

Above the waves, the oxygen transforms

18:08

the

18:09

atmosphere. These strumatalytes are

18:12

creating the most important element for

18:14

life on

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Earth. Without them, virtually every

18:19

living thing wouldn't

18:24

exist.

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[Music]

18:29

Over the next 2 billion years, oxygen

18:33

levels continue to rise. And as the

18:36

planet spin slows, the days get

18:40

longer, lasting at least 16 hours.

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[Music]

18:53

3 billion years after the planet's

18:56

birth, there's still no complex life, no

18:59

plants, no dinosaurs, no

19:05

humans. But the Earth has something

19:08

unlike any other planet in this solar

19:10

system. A force with the power to change

19:14

everything.

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[Music]

19:23

1 and a half billion years ago, the

19:26

Earth is a beautiful blue ball dotted

19:30

with volcanic

19:33

islands. Over millions of years, a

19:36

mysterious force rearranges these

19:39

islands. Hidden beneath the ocean, the

19:42

Earth's crust breaks into vast plates.

19:47

But even deeper, the Earth's core is so

19:50

hot that it generates movement in the

19:53

rock beneath the

19:56

crust. These movements push and pull the

19:59

plates around the

20:01

globe, carrying the oceans and islands

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with

20:04

[Music]

20:06

them. Millions of years race

20:09

by. Our planet is alive and

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changing. Over 400 million years, a vast

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new superc continent takes shape. It's

20:22

called Rodinia.

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[Music]

20:30

In the shallow waters surrounding

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Rodinia, strumatalytes work their magic

20:35

for more than 2 billion years, pumping

20:38

oxygen into the

20:41

atmosphere. The temperature is

20:44

85° and the days are 18 hours long.

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[Music]

20:57

But this planet looks more like Mars

20:59

than

21:04

Earth. To find life, we must fast

21:08

forward through time.

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[Music]

21:22

Washington State 750 million years

21:27

ago. A force deep inside the planet rips

21:31

the crust to

21:32

pieces. It's as though the world is

21:35

breaking

21:37

apart. And there's only one force

21:40

powerful enough to do

21:41

this.

21:44

Heat. It escapes from the Earth's molten

21:47

core, stretching and weakening the

21:50

crust.

21:52

Inch by inch, year by year, the great

21:56

superc continent is splitting in two.

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[Music]

22:01

[Applause]

22:06

[Music]

22:24

[Music]

22:35

[Music]

22:38

The intense geological activity spawns a

22:41

mass of

22:42

volcanoes. They pump carbon dioxide into

22:45

the atmosphere.

23:04

The carbon dioxide mixes with water and

23:08

creates acid rain.

23:21

When the continent tore apart, many

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rocks were

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[Music]

23:29

exposed. These rocks absorbed the acid

23:32

rain, including its carbon dioxide. Vast

23:36

quantities of CO2 are absorbed out of

23:39

the atmosphere.

23:46

[Music]

23:49

Now, there's not enough carbon dioxide

23:51

in the air to trap the sun's heat around

23:54

the

23:56

planet. In just a few thousand years,

23:59

the temperature plummets to around -60°.

24:06

This frozen wasteland is southern

24:08

Australia 650 million years

24:13

ago. It's the start of what some

24:16

scientists call snowball

24:19

Earth. A period they believe to be the

24:21

longest, coldest ice age ever to grip

24:25

the planet.

24:30

A vast wall of ice looms thousands of

24:34

feet

24:36

high and it's

24:40

unstoppable. The more ice there is, the

24:43

more sunlight it reflects away from the

24:45

planet and the faster the ice

24:50

spreads. Nearby is a second ice sheet

24:53

just as

24:54

high. The two sheets spread away from

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the poles toward each other to meet at

25:00

the equator.

25:25

Now, an ice sheet up to 10,000 ft thick

25:28

covers the entire

25:33

planet. Earth first began as a molten

25:37

ball of fire. Now it's a frozen ball of

25:42

[Music]

25:45

ice. Virtually all the sun's light and

25:48

warmth reflects back into

25:51

[Music]

26:00

space. And it seems as though nothing,

26:03

not even the sun, can rescue the planet

26:06

now.

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[Music]

26:19

650 million years ago, ice intombs the

26:24

planet. For 15 million years, the Earth

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is a vast frozen

26:32

snowball. But it can't last forever.

26:35

Something must release the Earth from

26:37

this frozen

26:39

prison. And when it does, who knows

26:43

whether life has survived beneath the

26:46

ice. The surface is frozen, but the core

26:49

is still hotter than the sun's

26:58

surface. Volcanoes have been erupting

27:01

since the world began to freeze. But up

27:04

until now, even their heat and power

27:07

made no impact on the

27:12

ice. Volcanoes pump out billions of tons

27:16

of carbon

27:18

dioxide. Before the big freeze, the

27:21

Earth's rocks absorbed most of the

27:26

CO2. But now, with the rocks smothered

27:29

in ice, there's nothing to absorb the

27:32

gas. So it fills the

27:42

atmosphere like a blanket. It traps the

27:45

sun's warmth around the planet, allowing

27:48

the temperatures to

27:51

rise. Now, after 15 million years, the

27:56

ice begins to melt.

28:21

It's thought that during snowball Earth,

28:24

the ice pushed the crust down, but now

28:27

as it melts, the crust bounces

28:30

up creating fissures and weak

28:34

spots and more

28:41

volcanoes. The volcanoes release more

28:44

carbon dioxide and push the temperature

28:47

up even

28:49

higher. The melt gathers

28:54

momentum and oxygen levels rise.

28:59

Through a series of chemical reactions,

29:02

the ice has created

29:05

oxygen. While the planet was frozen, the

29:08

sun's ultraviolet rays reacted with

29:11

water molecules in the ice to produce

29:14

hydrogen peroxide, a chemical rich in

29:17

oxygen.

29:21

[Music]

29:30

Now, as the ice melts, the hydrogen

29:33

peroxide breaks down and releases

29:36

massive amounts of oxygen.

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[Music]

29:47

The earth is waking

29:49

up and it's a very different place.

30:31

600 million years ago, the atmosphere is

30:34

warmer, like a summer day.

30:39

And the days are about 22 hours

30:44

[Music]

30:49

long. Add all this water and it's the

30:52

perfect recipe for

30:59

life. Before Snowball Earth, primitive

31:02

bacteria emerged in the oceans.

31:06

But surely they couldn't have survived

31:08

an ice age 75 times longer than the

31:12

entire span of human

31:15

history. If something has survived, then

31:18

life may be found where it was last

31:21

seen, in the oceans.

31:25

[Music]

31:28

Now, 540 million years ago, in an ocean

31:32

full of oxygen, those primitive bacteria

31:36

have

31:37

evolved. A handful must have clung on

31:40

through the big

31:41

[Music]

31:42

freeze. There are plants scattered on

31:45

the

31:46

[Music]

31:49

seafloor and something else.

31:53

[Music]

31:55

What looks like an armored slug takes up

31:58

residence. It's called

32:02

Rewaxia. A new generation of complex

32:05

multi-selled

32:07

organisms. The Earth enters one of the

32:10

most dynamic periods in its history, the

32:13

Cambrian

32:16

Explosion. Increased oxygen levels allow

32:19

creatures to grow larger and develop

32:22

bony skeletons.

32:26

There are

32:29

worms,

32:33

sponges, and these

32:36

trilobyes. Distant relatives of insects,

32:39

lobsters, even scorpions.

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[Music]

32:51

Life in the oceans

32:54

[Music]

32:55

blossoms from microscopic bacteria to

33:00

monsters.

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[Music]

33:12

This is

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Anomalaris. Nearly 2 ft

33:17

long. It has large

33:20

eyes, razor sharp teeth, and grasping

33:24

limbs.

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[Music]

33:41

[Music]

33:43

All it has to do is take its

33:49

[Music]

33:55

pick. The trilobyte can't ride itself.

33:58

Its soft belly is exposed.

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[Music]

34:13

[Music]

34:17

Also found in the sea is picaya. Only an

34:20

inch and a half long. They may be the

34:23

first organism with a

34:26

[Music]

34:30

spine. Over millions of years, this

34:34

simple structure will evolve into the

34:36

spine that keeps us standing.

34:46

[Music]

34:52

[Music]

34:57

expecting to find life in ruins. The

35:00

oceans are in fact full of

35:05

life. Where trilobyes

35:08

scavenge, monsters

35:11

prowl, and where creatures begin to take

35:14

on familiar

35:16

[Music]

35:18

forms. Beneath the waves, there are

35:21

already tens of thousands of plant and

35:24

animal species.

35:27

The advance of life seems

35:30

[Music]

35:31

[Applause]

35:45

[Music]

35:46

unstoppable. 460 million years ago, the

35:50

plates had been moving again.

35:53

A new continent now

35:55

exists,

36:00

Gonduana. It's 90° and oxygen levels are

36:04

close to what they are

36:07

today. The land should be covered with

36:10

plants and crawling with

36:12

creatures, but there's not much here

36:15

besides a few patches of algae.

36:20

[Music]

36:27

There's only one

36:34

explanation, the

36:39

sun. It blasts the surface with deadly

36:42

radiation.

36:46

So, the complex life in the ocean

36:48

doesn't stand a chance on

36:53

land. But 30 m up, where the rays enter

36:57

the Earth's atmosphere, something is

37:03

happening. When oxygen meets the sun's

37:06

radiation, it turns into another kind of

37:08

gas called ozone.

37:14

This gas forms a blanket around the

37:16

planet and absorbs the lethal

37:21

radiation. Over 120 million years, the

37:25

ozone layer gets thicker and prevents

37:27

more and more radiation from reaching

37:30

the Earth's

37:31

surface. Without this layer, life on

37:34

land simply wouldn't

37:36

exist. Now, shielded from radiation,

37:40

life takes off.

37:46

Small mossy lumps are the first land

37:51

plants. They pump out even more

37:55

oxygen. Levels soar.

37:58

[Music]

38:07

375 million years ago, a new species

38:11

lives in the

38:13

water

38:18

[Music]

38:25

swimming. It's a strange fish called

38:28

Tectalic.

38:32

[Music]

38:53

It uses its neck to raise itself up.

38:58

[Music]

39:05

[Applause]

39:06

[Music]

39:12

And its fins function as

39:18

legs, allowing it to move out of the

39:20

water.

39:33

[Music]

39:34

This is one of the most important

39:36

moments in the making of our

39:39

planet. Over 15 million years, creatures

39:43

like these

39:46

evolve. They grow stronger limbs and

39:49

spend more time out of the water where

39:51

plant life is exploding.

39:55

Until 360 million years ago, their

39:59

relatives, called tetropods, make the

40:02

land their

40:03

home. From tetropods, four-legged

40:07

vertebrates evolve into dinosaurs,

40:09

birds, mammals, and

40:12

eventually humans.

40:18

There are mosses and ferns everywhere,

40:22

some at least 100 ft

40:26

tall. A seed is carried by the

40:29

[Music]

40:34

wind. Until now, plants reproduced using

40:38

spores, single cell particles that need

40:41

plenty of water to grow.

40:46

But this seed is miles from

40:51

water. This embryionic plant has its own

40:55

food and water

40:57

supply. Unlike a spore, this seed can

41:01

survive far from water for months, even

41:04

years.

41:11

[Applause]

41:19

The humble seed spreads life across the

41:21

plant, and each tree and plant pumps out

41:25

even more oxygen.

41:31

[Music]

41:41

It's an environment very much like

41:44

today.

42:02

The planet has come a long way. From a

42:06

lump of burning rock and dust to a blue

42:09

and green world bursting with life.

42:19

There are now fish,

42:22

plants, and

42:28

this the

42:33

dragonfly. It's called

42:37

Megura. This insect is the size of an

42:40

eagle.

42:42

What were once legs have evolved into

42:44

wings, extending the dragonflyy's

42:47

hunting territory over a vast

42:50

[Music]

42:54

area. There are also millipedes and

42:57

spiders down there.

43:02

[Music]

43:05

These creatures, called arthropods, were

43:08

among the first to set foot on land

43:10

hundreds of millions of years ago. They

43:14

look almost identical to the bugs that

43:16

invade our homes today. Except for one

43:19

big difference. Like the megaura,

43:23

they're monsters.

43:25

It's a world full of giants where

43:28

millipedes are 6 ft long and scorpions

43:32

are the size of

43:34

[Music]

43:37

wolves. This is because the oxygen level

43:40

is much higher than it is today, which

43:43

allows their respiratory systems to be

43:45

more efficient, fueling their bodies to

43:48

grow larger.

43:55

[Music]

44:00

So far, animals have been laying their

44:02

eggs in the

44:05

water. But a lizard-like creature called

44:08

the Hyonamus prefers

44:12

land. Its eggs contain all the water and

44:15

nutrients that the developing fetus

44:18

needs. The babies grow in their own

44:20

self-contained pond.

44:23

The egg is a major evolutionary

44:27

breakthrough, allowing animals to leave

44:30

the water behind and conquer

44:32

[Music]

44:45

land. This baby Hilanos leads the

44:48

advance.

44:52

as a new creature, the

45:09

reptile. Inevitably, with life comes

45:13

death.

45:16

Dead plant matter builds up and decays

45:18

into dense, soggy

45:21

layers. Over hundreds of millions of

45:23

years, rocks cover these layers, and

45:26

heat from the Earth's core and pressure

45:28

from the overlying rocks transform these

45:31

layers into seams of

45:35

coal. Each lump of coal burned today is

45:39

made of plants that died 300 million

45:42

years ago.

45:46

[Music]

45:56

amidst the decay. Hidden from sight,

45:59

life is

46:00

stirring. Soon, seeds will germinate,

46:03

plants will grow, and this wasteland

46:06

will live

46:07

again. Life seems to have conquered the

46:11

planet.

46:12

But will it

46:14

[Music]

46:28

last? A herd of creatures graze the

46:32

Siberian

46:34

plains and they are big.

46:42

[Music]

46:45

Evolution takes a huge leap forward.

46:48

Small lizards are now giant

46:53

reptiles. These scooteraurs are distant

46:57

relatives of turtles.

46:59

[Music]

47:04

If these planteaters look tough, the

47:07

carnivores must be seriously

47:15

mean. Like this

47:18

Gorgonopsit, a perfectly engineered

47:21

prehistoric killing machine.

47:35

[Music]

47:41

The Gorgalopsit's saber teeth wound the

47:44

scooter.

47:50

[Music]

47:56

The predator watches as its prey grows

47:59

weak from blood

48:02

loss. But before it can make its final

48:09

move, something strange

48:12

happens. The ground gets hot.

48:23

Enormous pressure builds beneath the

48:25

surface and lava spews into the air.

48:37

[Music]

48:52

[Music]

48:58

But the lava isn't from one single

49:01

volcano. The entire landscape is

49:04

[Music]

49:06

erupting. It's a flood basalt eruption.

49:10

A massive plume of mantle rises up from

49:13

deep inside the earth and pushes molten

49:16

rock out through fissures in the earth's

49:20

[Music]

49:23

crust. The lush paradise is now a

49:26

lifeless hell. The scooter and the

49:30

gorgonopsits are dead.

49:34

They're the first casualties in the

49:36

greatest mass extinction the world has

49:38

ever seen, the Perian

49:50

[Music]

49:52

extinction. On the other side of the

49:55

continent Gondana, nothing's changed

49:58

yet.

50:10

It appears to be snowing, but the

50:12

temperature is about

50:16

70°. It's actually ash, fallout from the

50:20

eruptions some 10,000 mi away.

50:28

The ash burns and suffocates the

50:30

animals, killing them around the

50:45

world. Sulfur dioxide from the eruptions

50:48

fills the

50:51

atmosphere. As it rains, the gas turns

50:54

to sulfuric acid and burns everything it

50:58

falls

51:02

on. What was a local

51:05

disaster has now turned

51:19

global. The Siberian eruptions increase

51:23

the Earth's carbon dioxide levels. The

51:26

atmosphere gets

51:28

hotter, water

51:32

evaporates, and vegetation dies.

51:46

Around the world, life on land is being

51:49

wiped

51:51

out and life in the oceans has also been

51:57

compromised. The waters turn

52:06

pink. Plants, trilobyes, and predators

52:10

disappear.

52:16

[Music]

52:21

The new hotter atmosphere heated the

52:23

oceans and stripped them of

52:26

oxygen. Now this pink algae is one of

52:29

the few life forms that can survive in

52:32

the stagnant

52:34

water. The Siberian eruptions transform

52:37

the entire planet. Nothing, not even the

52:40

deepest ocean floor is beyond their

52:44

[Music]

52:51

reach. Bubbles of methane gas escape

52:55

from beneath the

53:00

seabed. Methane is a greenhouse gas, at

53:04

least 20 times deadlier than carbon

53:07

dioxide.

53:09

Until now, the gas has been frozen. But

53:13

as the sea temperature rises, it begins

53:16

to

53:19

[Music]

53:30

melt. Released into the atmosphere, this

53:34

powerful gas pushes up temperatures even

53:37

further.

53:39

It's now almost

53:42

105°, 11° hotter than before the

53:45

Siberian

53:51

eruptions. Creatures that survive the

53:53

initial destruction now face a new and

53:56

deadly

53:58

environment. Few will live.

54:03

It's been 500,000 years since the

54:06

eruptions first began. And all this

54:08

time, the lava's been pouring

54:12

out. By now, it covers an area the size

54:16

of the United States with a layer of

54:18

molten rock nearly 4 miles

54:25

deep. 95% of the species are gone.

54:33

A few survive by eating anything they

54:35

can find and living in burrows

54:43

underground. But everything else is

54:48

dead. 250 million years ago, the Earth

54:52

reverts back to an almost lifeless

54:55

planet.

54:57

But that's about to change

55:01

[Music]

55:05

again. It's been 50 million years since

55:09

virtually all life on Earth was wiped

55:12

out and the planet has been transformed.

55:19

It's now 200 million years ago and just

55:24

one superc continent pangia stretches

55:27

from pole to

55:35

pole. After the trauma of the mass

55:37

extinction, the planet

55:40

heals, temperatures

55:43

stabilize, the acid rain neutralizes,

55:46

and vegetation

55:49

returns. With 95% of all life on Earth

55:52

wiped out, the field opens for a new

55:56

species to

55:57

emerge, one that will dominate the

56:00

planet like no other.

56:09

The

56:12

dinosaurs. These are called

56:16

Amosaurs. Like all

56:20

dinosaur the Perian

56:23

[Music]

56:25

extinction. At 15 ft tall, their size

56:29

makes them slow and vulnerable.

56:40

Nearby is the

56:46

[Applause]

56:48

Dilophosaur. It's

56:54

small and fast.

57:17

The Amosaurus is too big a meal for one

57:21

Dilophosaurus, but not for two.

57:31

[Music]

57:39

The dinosaurs have repopulated the

57:42

earth, but no species can tame this

57:45

restless, volatile planet.

57:52

[Music]

57:54

The Earth's crust is thinning. It's

57:56

releasing lava and shaking with

57:58

earthquakes as if being stretched by

58:01

some unseen

58:08

force. It's also happening near what

58:11

will become North America's eastern

58:14

seabboard.

58:24

The Earth's plates are on the move

58:27

again. 190 million years ago, the great

58:31

superc continent of Pangia tears

58:38

apart. A vast slab of land breaks away,

58:41

creating a chasm.

58:44

It fills with a new ocean called the

58:47

Teethus over what will one day be the

58:49

Middle

58:56

East. Currents push nutrients up into

59:00

the coastal

59:04

waters and the nutrients attract fish in

59:08

the millions.

59:14

But again, with so much life also comes

59:19

[Music]

59:21

death. Dead fish and plankton carpet the

59:25

ocean

59:27

floor. Over the next 10 million years,

59:31

layers of rock will bury and heat the

59:33

dead

59:35

creatures. Ancient fish and plankton

59:37

will become oil.

59:40

[Music]

59:56

Every gallon of gas in our

59:58

cars, every piece of plastic on the

60:01

planet, the paint on our walls, the

60:04

carpet under our feet, even the soap we

60:07

wash with, almost all originate ated in

60:10

this

60:11

[Music]

60:24

way. 180 million years ago, the North

60:27

American plate is still moving away from

60:30

the European and Asian plate.

60:40

It's shifting about 1 inch each year,

60:42

the same speed at which our fingernails

60:48

grow. But fast forward 35 million years

60:52

and a new ocean forms as well as new

60:58

continents. The United States breaks

61:00

away from Africa.

61:05

The world as we know it takes

61:08

shape. The chasm between the two

61:10

continents fills, creating the Atlantic

61:14

[Music]

61:22

Ocean. And in the middle lies a volcano.

61:30

Like before, currents deep beneath the

61:33

Earth's crust move the plates again.

61:36

[Music]

61:48

[Music]

61:55

The entire seafloor tears in two and is

61:58

pushed up into a ridge of mountains and

62:04

volcanoes. It grows higher than the

62:06

Himalayas and longer than the

62:09

Rockies. The water here is

62:12

hot as molten lava forces its way out

62:16

from deep inside the earth.

62:22

As the lava cools, it creates a new

62:25

range of volcanic mountains and a new

62:28

ocean

62:31

floor. Pangia breaks apart and our world

62:36

rearranges again.

62:42

[Music]

62:56

It's this geological activity that makes

62:59

the Earth restless, creative, and

63:04

unique. And every time the planet

63:06

reinvents itself, its inhabitants adapt

63:10

and evolve.

63:17

[Music]

63:20

Like the

63:24

ichthyossaurs, their reptile ancestors

63:26

lived on land. But as the planet

63:29

changed, so did these animals. They grew

63:32

fits and moved into the newly formed

63:34

Atlantic Ocean.

63:42

This one is 20 ft long and can travel at

63:45

a quick 25 m an

63:54

hour. It's the ocean's fastest creature

63:57

and most efficient predator. It rules

64:00

the oceans for 50 million years.

64:04

[Music]

64:19

But now there's a new contender.

64:31

[Music]

64:37

The

64:42

pllyiosaur. Longer than a bus and as

64:45

heavy as a truck, its jaws are eight

64:48

times more powerful than a great white

64:50

sharks. with teeth 12 in

64:54

[Music]

65:07

long. The Earth and its inhabitants have

65:11

changed beyond

65:13

recognition. This was once solid

65:16

ground. Now it's the Atlantic Ocean.

65:20

The very spot where Amosaurs grazed and

65:23

Dilophoshaurs stalk their

65:26

prey. The dinosaurs world may be

65:28

different, but they're as dominant as

65:31

ever. They appear

65:34

[Music]

65:44

invincible. They're one of the planet's

65:46

most successful species.

65:49

They've survived volcanic

65:51

eruptions, earthquakes, and entire

65:54

continents splitting

65:57

apart. The dinosaurs have thrived for

66:01

165 million

66:09

years. A number of mammals have also

66:12

survived like this shrewlike animal.

66:21

They're prey to the dinosaurs, so they

66:24

live in trees or underground and venture

66:27

out only at

66:30

night. Mammals pose no threat to the

66:33

[Music]

66:40

dinosaurs. Nothing on Earth can

66:42

challenge their dominance.

66:56

Nothing on

67:02

Earth. A large piece of space rock heads

67:05

toward Earth.

67:14

This asteroid is at least 6 miles across

67:17

and traveling over 40,000 m an

67:21

hour. It's bigger than Mount

67:24

[Music]

67:27

[Applause]

67:28

[Music]

67:31

Everest and heads straight for the Gulf

67:33

of Mexico.

67:46

It travels so fast that its impact would

67:49

be missed in a blink of an

67:55

eye. A split second changes the world

67:59

forever.

68:07

At impact, the asteroid's back edge

68:10

stands at 35,000 ft.

68:30

It strikes with such immense force that

68:33

it destroys everything it hits.

68:53

The asteroid itself instantly

68:58

[Applause]

69:01

vaporizes, unleashing the energy of

69:03

millions of nuclear

69:11

weapons. Nowhere is safe with debris

69:14

flying everywhere.

69:21

Debris as big as entire city blocks

69:24

circle the earth.

69:41

The blast wave races out from the impact

69:43

zone like shrapnel from an exploding

69:46

bomb.

70:23

Minutes after impact, hundreds of miles

70:25

from where the asteroid struck, the

70:28

Earth is under attack.

70:36

Boulders rain

70:44

down. Earthquakes shake the

70:47

[Music]

70:51

ground. And tsunamis batter the coasts.

71:08

But the onslaught has only just

71:11

begun. The plume of molten rock and dust

71:14

spreads out and engulfs the

71:18

planet. The entire sky acts like a giant

71:22

lamp.

71:28

Heating the Earth's surface to over

71:31

500°, vegetation spontaneously

71:47

ignites. Even months after the impact,

71:50

smoke and ash still block out the sun's

71:54

rays. And with less sunlight, plants die

71:58

and the animals

72:16

starve. 65 million years ago, the impact

72:20

has blasted, stoned, and burnt the

72:22

dinosaurs.

72:32

Their665 millionyear reign is

72:43

over. But the dinosaur's demise brings

72:47

opportunity for another

72:49

[Music]

72:52

species. a

72:54

[Music]

72:58

mammal. By living underground, mammals

73:01

have avoided the heat and

73:04

fires. And by eating anything, they

73:07

thrive while more selective eaters

73:12

[Music]

73:14

die. They are the unlikely inheritors of

73:17

the dinosaurs crown.

73:19

[Music]

73:27

And as one story ends, another

73:31

begins. With the dinosaurs out of the

73:34

way, our ancestors may now have a chance

73:38

at life.

73:41

[Music]

73:57

The dinosaurs are long

74:00

dead. The planet is

74:04

[Music]

74:06

peaceful. In this new world, our mammal

74:10

ancestors are evolving.

74:13

[Music]

74:23

47 million years ago, this lake in what

74:27

will one day be Germany is the perfect

74:30

place to spot them.

74:33

[Music]

74:48

Unlike earlier mammals, its eyes and

74:51

brain are

74:52

[Music]

74:54

bigger. This is Darwinius Masel or

74:58

Edida.

75:00

She looks nothing like humans, but

75:02

fossil evidence today indicates that

75:05

these creatures might evolve into

75:07

monkeys, apes, and eventually

75:15

humans. Looking back through 47 million

75:18

years of evolution might reveal one of

75:21

our earliest known ancestors.

75:27

The lake sits on a volcanic

75:29

crater. It belches out noxious

75:35

gas that eventually

75:38

[Music]

75:46

kills. The lake preserves her in its

75:49

oxygen depleted depths.

75:55

One day, when the water is gone and

75:58

Edah's fossil is

76:00

[Music]

76:01

found, this primitive primate could help

76:04

piece together the beginning of our own

76:07

story, the story of human life.

76:16

We're closer to understanding how

76:18

everything we've seen from ocean

76:20

bacteria through walking fish and

76:23

subterranean rodents leads to

76:27

us and to understanding how our planet

76:30

was

76:31

[Music]

76:35

made 47 million years ago. The

76:38

atmosphere is much like today.

76:45

The temperature is

76:48

75° and the day lasts just under 24

76:53

hours. The Earth is now almost identical

76:56

to the planet we call

76:59

home. Almost.

77:01

[Music]

77:09

[Music]

77:17

the Earth's plates are on the move

77:23

again. India moves north toward Asia.

77:28

[Music]

77:40

The Indian and Asian plates are locked

77:43

in a titanic

77:46

[Music]

77:52

struggle and neither play was

77:57

winning. As they buckle, the ocean floor

78:01

contorts upward along a 1500m

78:11

line. A vast mountain range rises up

78:15

over 27,000 ft.

78:27

[Music]

78:38

These are the Himalayas.

78:40

[Music]

78:51

and the highest mountain of all, Mount

78:54

[Music]

79:01

Everest. Its summit reaches up into the

79:04

Earth's jetream, the same altitude where

79:07

planes fly.

79:19

[Music]

79:33

When the snow on the peaks melts, it

79:35

feeds rivers like the Ganges, Indis,

79:39

Yellow, and Yangy.

79:41

[Applause]

79:43

[Music]

79:47

The Himalayas are like a vast water

79:49

tower. One day, their rivers will supply

79:52

water for almost half the world's

79:54

population.

79:57

[Music]

80:07

[Music]

80:11

20 million years ago. This is our

80:15

planet with every continent and every

80:18

ocean as we know

80:23

[Music]

80:25

it. Except one thing is still

80:28

missing, the human

80:31

[Music]

80:35

race. And for humans to evolve,

80:38

something needs to

80:42

[Music]

80:52

[Music]

80:57

change. Along the African coast, a great

81:00

rift opens up.

81:08

[Music]

81:09

It stretches nearly 4,000

81:14

[Music]

81:18

miles with mountains growing along its

81:21

edge.

81:28

[Music]

81:40

This apeike creature may stay in these

81:43

trees forever, but its world is

81:49

changing. The growing mountains act like

81:51

a wall, prohibiting moisture from the

81:54

Indian Ocean from passing over the land.

81:59

It's getting hotter and

82:02

drier. The lush rainforest becomes an

82:06

arid

82:09

savannah. The new hotter climate changes

82:12

the creature's habitat, forcing them to

82:14

search further for

82:16

food. Soon they stop dragging their

82:19

knuckles like apes and begin to stand

82:23

and walk on two feet.

82:27

It's the most important step in the

82:29

human

82:35

story. This mountain range could be the

82:38

reason humans walk on two feet.

82:48

The random movement of two plates may

82:51

have kickstarted a chain of events that

82:54

leads to the first

82:55

[Music]

83:11

humans. A man and child. a scene very

83:14

much like today, but it's one and a half

83:18

million years

83:20

ago. They are an early species of human

83:24

called Homo

83:27

erectus. And these are the first

83:30

footprints like our

83:32

[Music]

83:34

own. Civilizations past and present.

83:38

Everyone that's ever lived. The greatest

83:42

inventions, the most brilliant ideas.

83:46

Human history in all its complexity and

83:50

splendor begins here and now.

83:53

[Music]

83:56

[Applause]

83:58

[Music]

84:10

The climate changes

84:12

again. 70,000 years ago, sea levels

84:16

fall and the gap between Africa and

84:19

Arabia shrinks to just 8

84:27

m. The Red Sea is now narrow and shallow

84:31

enough for a small group to cross out of

84:35

Africa.

84:38

They're another later species of human

84:41

called Homo

84:45

[Music]

84:53

[Music]

84:58

sapiens. Scientists believe that the

85:01

entire world beyond Africa was populated

85:04

from descendants of these 200

85:11

individuals. Over time, our ancestors

85:14

multiply and spread

85:16

out to

85:19

India onto

85:21

Asia and into Europe.

85:33

[Music]

85:36

But while humans head north, a giant

85:39

wall of ice travels

85:43

[Music]

85:46

south. Europe 40,000 years

85:50

ago. Homo sapiens arrive only to find a

85:54

world that's quickly

85:57

changing. It should be the height of

85:59

summer, but it's getting colder. The

86:02

plants are frostbitten and the rivers

86:05

are

86:07

frozen. Natural changes in the Earth's

86:10

orbit, CO2 levels, and the flow of warm

86:13

water around the planet conspired to

86:16

lower the Earth's temperature.

86:18

The Earth and its inhabitants enter an

86:22

ice

86:23

age. Glaciers as high as skyscrapers

86:27

creep over the northern hemisphere about

86:29

a foot every

86:32

day. Slow and powerful, they sculpt the

86:36

landscape, gouging out great

86:40

depressions. The planet will never look

86:43

the same again.

86:49

Now, around 20,000 years ago, they grind

86:53

to a

86:54

halt. Much of the northern hemisphere is

86:58

covered by ice sheets up to 1 and 1/2

87:00

miles

87:01

[Music]

87:08

thick. With trillions of gallons of

87:11

water locked up as ice, sea levels

87:15

[Music]

87:17

fall. A strip of land emerges from the

87:20

ocean between Siberia and Alaska.

87:25

[Music]

87:30

It's a bridge between two vast

87:34

continents. A gateway that takes humans

87:37

from Asia to a new world, the

87:42

Americas. They're the last great

87:44

continents to be colonized, the last

87:48

great human

87:49

migration, and the first Americans.

87:57

[Music]

88:04

Now, 14,000 years ago, the changes that

88:08

triggered the ice age

88:11

reverse. As the ice retreats, it reveals

88:15

a very different northern hemisphere.

88:19

The huge depressions that the glaciers

88:21

create fill with water to become North

88:24

America's Great

88:39

Lakes. 6,000 years ago, the ice retreats

88:43

back to the poles toward the Arctic and

88:46

Antarctic.

88:50

[Music]

89:05

After a 4 and 12 billionyear journey,

89:08

we're finally

89:11

home. This is our world, our time.

89:19

The planet's incredible story helps us

89:22

understand how and why everything around

89:25

us is here

89:27

[Music]

89:32

today. From the skies

89:39

above to water, the essential ingredient

89:43

for life.

89:45

[Music]

89:47

to the ground beneath our

89:49

[Music]

89:55

feet and finally

89:58

[Music]

90:01

life. A chain of catastrophes and

90:05

coincidences creating a spectacular

90:08

result.

90:10

Each triumph and disaster is a step

90:13

leading to

90:16

here to each and every one of us right

90:22

now. But the Earth's story isn't

90:28

over. This journey is only half the

90:32

story. A lot more is yet to come.

90:38

The Earth will live for at least another

90:41

4.5 billion

90:43

[Music]

90:52

years. More

90:54

wonders, more

90:57

terrors, and more strange creatures lie

91:00

ahead for our restless and creative

91:03

planet.

91:08

The next chapter of Earth's story is

91:11

still to be written.

91:13

[Music]

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