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Saturn.
The rings are made of ice particles.
We also now know that Saturn is orbited
by over 60 natural satellites.
The largest of Saturn's satellites is a moon called Titan.
It is enveloped in a thick atmosphere,
one filled with orange haze.
In 2005,
a NASA probe penetrated the veil of mystery,
and sent back the first images of the surface.
The terrain looked amazingly familiar.
Black lines branched out over the surface.
They looked just like rivers.
And numerous lakes were discovered.
This was the first time any celestial object had been found
with liquid on its surface.
The more the probe investigated,
the more Earth-like Titan seemd to be.
It was at this point that scientists began to suspect
that life might be present.
Maybe in the seas, more interesting things happen.
Maybe you get self-replicating chemical systems
much like those that are the first steps
towards living systems that are deep in our own history.
So Titan gives us a whole new set of possibilities.
There's the possibility that maybe there is life on Titan
that has somehow found a way to make use
of all of these building blocks
that the atmosphere is making for it.
However, the temperature on Titan
is -180 degrees Celsius.
Could life really exist there?
How do we know it's too cold?
Imagine you're living on Titan
and you're looking at the Earth.
You'd say, "Oh, there's a liquid, there's organics",
"there's energy, but it's too hot."
Titan has both an atmosphere and liquids.
Could life exist there?
This planetary body, very similar to Earth.
Saturn's moon, Titan.
Imagine the journey from Earth to Titan.
If you could travel at the speed of light,
you'd pass Mars about four minutes into the voyage.
At the 30-minute mark or so,
you would pass the giant ball of gases known as Jupiter.
Then, some 70 minutes after departure,
you would finally arrive at Saturn
surrounded by those beautiful rings.
Like Jupiter, Saturn is a large gaseous planet.
Finally, you'd reach Titan.
With a diameter of 5,000 kilometers,
Titan is about three-fourths the size of Mars.
It's a moon the size of a planet.
Fully cloaked in that orange haze,
Titan's true appearance was not known
until the 21st century.
1997 saw the launch of the Cassini-Huygens mission.
The Cassini orbiter equipped with cameras
and other instruments, and carrying the Huygens probe
was sent to investigate Saturn and its moons,
especially Titan.
In 2004, seven years after liftoff,
Cassini-Huygens reached the vicinity of Saturn,
1.4 billion kilometers from the Sun.
Cassini then proceeded to enter into orbit around the planet
and its satellites, and to commence scientific observations.
It took this image of Titan.
For the first time,
Titan's true features began to show
from under that thick haze.
The day was approaching when we would finally be able
to see the surface of Saturn's giant moon.
In December 2004,
the Huygens probe separated from Cassini,
and coasted to Titan.
The target landing site was near Titan's equator.
What that site would be like, no one knew.
Titan's atmosphere is 1,000 kilometers thick.
The probe entered it.
Huygens deployed a parachute and drifted down,
jettisoning its heat shield.
This image, taken from a height of 152 kilometers,
was Huygens' fist view of Titan,
which was still obstructed by haze.
Huygens was shooting still images as it descended.
Its microphone also captured the sound
of the wind rushing by.
This was the first sound recording ever
made of an alien environment.
These images of Titan's surface
were taken by Huygens from 16,000 kilometers up.
Black veins like the branchings of a river are visible.
It does look as though they're flowing
to the mouth of a river.
Now, from 8,000 meters above Titan.
It looks just like the sort of coastline
we're used to seeing on Earth.
Finally, the landing.
This is an image taken by Huygens just after landing.
What look like rocks and pebbles
strewn about over a flat plain,
are actually chunks of ice.
The surface temperature is -180 degrees Celsius.
Atmospheric pressure is a little higher than Earth's,
1.5 bars.
The horizon seems blurred by mist.
This is exactly like some rocky desert landscape on Earth.
High above, the Cassini orbiter continued its observations.
In the equatorial region where the Huygens probe landed,
Cassini discovered a strange pattern.
Some sort of regular striping.
Further observations found similar striations
covering some 20% of Titan's surface.
Ralph Lorenz has dedicated himself
to investing the strange striped pattern.
He is trying to solve the mystery of Titan's stripes
by comparing them to patterns he finds on Earth.
This is the Mojave Desert
in the western United States.
Lorenz believes Titan's stripes
are like the peaks and troughs of desert sand dunes.
There are, indeed, real similarities.
It's remarkable somehow that despite
the different gravity, the thicker atmosphere,
and the different material that the sand is made of,
somehow the landscape ends up looking
almost exactly the same as many places on Earth.
By comparing the shape of the dune
and the interaction with the rest of the environment,
we can get an understanding
of how these structures formed.
For example, different shapes of dunes
form in different wind patterns.
So the goal is to solve the mystery
of Titan's stripes by investigating
terrestrial desert dunes.
Lorenz's first step is to send up a kite with a camera
for an aerial overview.
He is looking for a place
that has a striped pattern like Titan's.
Next, he mounts a dune buggy equipped with GPS.
He wants to measure the heights of dunes
and the angles of their slopes.
The shapes of sand dunes change by the minute.
Lorenz plants a stake with a streamer attached.
In fact, he plants a whole line of them along this slope.
This will show what sort of wind creates this type of dune.
The wind is blowing from screen left across a gentle slope.
Then it swirls around
as if to carve out that slope to the right.
So it's become clear that here,
the wind flows from the milder slope
over and down the sharper slope.
Lorenz believes that the stripes on Titan
are also wind-sculpted sand dunes.
A closer look at that image of Titan's stripes
shows ridges with milder and sharper slopes,
similar to those in the Mojave Desert.
So Lorenz conjectures that the wind on Titan
must've been blowing from left to right.
The winds blowing on Titan's dunes, however,
are thought to be weaker than the winds on Earth.
The reason for that is that Titan's gravitational force
is only one-seventh of Earth's.
A relatively small lashing can produce a big result.
So on Titan, effects similar to those seen on Earth
are being produced by mild winds.
Titan is still an active world
where, geologically speaking,
processes are still happening.
And the fact that we can see sand dunes for example,
suggest that the winds that move the sand around
are still active, that we're seeing a dynamic planet
much like the Earth.
There was another unexpected aspect
to those images taken by Huygens.
Look closely at those chunks of ice on the ground.
They are reminiscent of stones turned over and over
by rivers on Earth.
Sharp edges are worn down.
They're rounded like pebbles.
So there may well be liquid on Titan.
This discovery attracted attention and astonishment.
Meanwhile, the Cassini orbiter
made a surprising discovery of its own.
Black spots and blotches were visible
near Titan's north pole.
Radar observations showed them to be lakes
filled with some liquid.
They number in the hundreds,
and some of them are huge.
This is the first time liquid has been found on the surface
of any celestial body other than Earth.
The lakes are dotted with islands and fed by rivers.
But with a surface temperature of -180 degrees,
any water on Titan would've frozen.
What liquid could it be in these lakes and rivers?
This is it.
Liquid methane.
On Earth, it's normally a vapor,
but at extremely low temperatures,
it condenses into a liquid.
Methane melts at -182 degrees Celsius.
It boils at -161 degrees.
In the 20 degree range between those two extremes,
it exists in a liquid state.
The temperatures on Titan's surface
are just right for liquid methane.
Methane is composed of one carbon atom
and four hydrogen atoms.
It's the simplest hydrocarbon,
and it constitutes the bulk of the liquid in Titan's lakes.
A portion of the liquid is ethane,
another hydrocarbon with similar characteristics.
Scientists at the Jet Propulsion Laboratory are trying
to determine how Titan's methane lakes were created
by conducting experiments here on Earth.
Christophe Sotin is an expert on bodies of ice
found in the solar system.
This device is called the Titan Chamber.
With internal air pressure at 1.5 bars
and a temperature of -180 degrees Celsius,
it reproduces Titan's environmental conditions.
Inside is placed a disc of ice
standing in for the terrain on Titan.
They then release droplets of liquid methane
onto the surface of the ice.
The methane disappears immediately,
absorbed by the ice,
like water being swallowed up by a thirsty earth.
So it was a big surprise, something we did not expect,
is that when the methane falls on the ice,
actually the methane got sucked into the ice.
It gets absorbed.
It doesn't run on the ice.
However, if methane continues to drip
onto the ice, eventually,
it begins to pool on the surface.
This suggests that wherever there are lakes on Titan,
the surrounding ice must be saturated with methane.
During its landing on Titan,
Huygens measured the concentration of methane.
That concentration gradually rose
the closer the probe got to the surface.
Then, the moment it landed, there was a sharp increase.
It is thought that this was due to the heat from Huygens
vaporizing the methane that permeates the ice.
On Titan, liquid methane acts in ways
similar to water on Earth.
In June 2012, for example,
Cassini observed a strange phenomenon
near Titan's south pole.
An oddly-shaped mass seemed to be squirming about
in the atmosphere.
It was a cloud swirling.
A cloud made up of methane.
On Earth, water is recycled as water vapor and rain.
One of the factors prompting this is seasonal change.
On Titan, the same sort of mechanism seems to be at work.
Titan is tilted on its axis,
some 26 degrees off vertical.
The Earth has a 23.4 degree tilt.
It's another point of similarity.
Along with its parent planet, Saturn, not shown here,
Titan takes 30 Earth years to orbit the Sun.
The tilt of its axis gives birth to different seasons.
At this location, Titan's northern hemisphere
experiences the long days of summer.
The northern hemisphere is warm,
producing rising atmosphere currents.
Liquid methane on Titan's surface evaporates
and is carried southward.
Near the south pole, it is winter.
The methane gases cool
condensing into a liquid or even solid state.
It can form clouds
like that huge swirling cloud Cassini spotted.
When it's winter in the northern hemisphere,
the cycle reverses.
Now, the methane cloud forms near the north pole.
Underneath that cloud, methane rain begins to fall.
Since methane is more viscous than water,
its raindrops are larger,
with diameters of about a centimeter.
But as Titan's gravity is weaker than Earth's,
the droplets fall more slowly,
about one meter per second,
like a soft snow on Earth.
They soak the icy ground on Titan and form lakes.
Wind blows.
Rain falls.
When people could finally see Titan close-up,
they were astonished at how much it resembles Earth.
In 2007,
the Cassini orbiters spotted something truly peculiar
on Titan's surface.
A land formation, some 70 kilometers across
in the shape of a flower.
What could it be?
Perspective can be gained by combining images
taken from two different points of view.
A three-dimensional image of the topography emerges.
That strange formation turns out to be a rugged mountain,
featuring a 1,500-meter high peak.
There is also a chasm that looks
like it might be a volcanic crater.
From that, one can infer a formally-active volcano.
That volcano has been an object of particular interest
to Jonathan Lunine,
an expert on Titan's internal structure.
He says that the volcano did not spew lava.
Rather, it pumped up a mixture of ammonia and water.
One thing to remember is that when water
is mixed with ammonia, it can stay liquid
down to very low temperatures.
Down, in fact, to -100 Celsius.
But at that point, within a few degrees of that point,
the liquid is actually very viscous.
It's almost like basalt.
So if that is what is flowing out on the surface,
we would see very thick flows.
Lunine believes that under the ice
beneath the volcano, there's an ocean.
He came to this conclusion due to changes in Titan's shape.
Titan completes its elliptical orbit around Saturn
once every 16 days.
During that time, it regularly feels the changing effect
of Saturn's gravity.
In short, it experiences tidal forces.
At its farthest point from Saturn,
Titan is almost perfectly spherical.
But at its closest point
where Saturn's gravitational pull is the strongest,
Titan grows fatter.
Its diameter alters by as much as 10 meters.
Lunine says that Titan can transform so dramatically
because internally, it is not made entirely of solid rock.
Lunine's observations suggest the following picture
of Titan's structure.
The outer crust of ice is some 50 to 100 kilometers thick.
The center is comprised of two types of bedrock.
In between the ice and the rock, however,
is a layer of liquid water.
The bedrock generates heat, says Lunine,
permitting the water to remain in a liquid state.
This ocean layer is some 300 kilometers deep.
Ammonia, present in Titan since its origin,
has also dissolved into the water.
It is thanks to this ocean layer
that Titan can change shape so flexibly.
The interior's warm enough that really only liquid water
is a suitable, stable material in that region,
so we're pretty sure from the gravity experiment
that Titan has a liquid water layer under its surface.
According to Lunine,
the tidal forces caused by Saturn, in turn,
stimulate volcanic activity.
Tidal forces cause friction along the boundary
between ice and the subsurface ocean.
The water heated in this way melts some of the icy crust.
It builds up by terretrial magma,
and eventually forces its way up above the surface.
This ammonia-laden water flows out
from Titan's volcanoes like lava.
Lunine believes such volcanoes are proof
of an underground ocean.
Beneath Titan's icy shell,
a whole new world lies hidden.
Saturn has over 60 moons.
Among them are Enceladus, ice-covered like Titan.
And Hyperion, pockmarked with craters.
Mimas has this huge crater.
Those are just a few of Saturn's moons,
but they all have practically no atmosphere.
Only Titan boasts an atmosphere that extends
as far as 1,000 kilometers into space.
Actual measurements reveal that this atmosphere
is 98% nitrogen.
The rest is largely methane.
Why is Titan the only one of Saturn's moons
with a thick atmosphere?
Solving that mystery through experimentation on Earth
has been a preoccupation of Yasuhito Sekine.
Sekine believes that Titan's atmosphere was generated
by an extraordinary mechanism.
The mechanism?
Collisions with small celestial objects.
Sekine is trying to reproduce that effect using a laser.
When Titan was first formed,
its icy land mass contained about 1% ammonia.
So inside a vacuum chamber,
a disc of ammonia-water ice stands in for the young Titan.
The laser beam enters from the left of your screen.
It strikes a projectile,
which then impacts the ammonia disc.
That was the laser shot.
Gases released by the impact are measured.
One is nitrogen
released by the disintegration of the ammonia.
Titan's thick atmosphere contains large amounts of nitrogen.
According to Sekine's calculations,
based on his experiments,
repeated impacts by small celestial objects
could have produced just such an atmosphere.
For example, Enceladus,
one of Saturn's other moons,
is merely 500 kilometers across.
That is one-tenth of Titan's diameter.
Saturn's other satellites are also small,
with weak gravitational fields.
So even if they've been similarly impacted,
they haven't been able to hold on to any atmosphere.
But did Titan, in fact, experience repeated bombardment
by small celestial objects?
Hal Levison uses computers to calculate
the history of the solar system.
He has advancd the revolutionary theory
that some four billion years ago,
the entire solar system was shaken by a massive event.
Levison argues that when the solar system was forming
4.6 billion years ago,
Uranus and Neptune were closer to the Sun
than they are now.
He inputs the location and size of the planets
and also of the small celestial objects
that lie further out.
Then the simulation begins.
At first, the basic situation did not change much.
But some 600 million years later,
Uranus and Neptune were suddenly flown
to the outer realms of the solar system.
Du, du, du, du, then out.
And that caused the giant planets to slowly spread.
It was infinitesimal, you wouldn't have noticed it
but the orbits were slowly changing.
And that continued until Jupiter and Saturn
got to the point where Jupiter was going around the Sun
exactly twice every time Saturn went around once,
and that configuration
is what set the whole instability off.
So you went, almost overnight,
from a time when there was a little bit going on
but not much, to this very violent period
where all hell breaks loose.
The smaller celestial objects shown here in green,
had formed a ring at the outer edge of the solar system.
But then the gravitational force of Uranus and Neptune
violently scattered these objects.
The result was that in the period from four billion
to 3.9 billion years ago,
the planets of the solar system encountered
a barrage of small celestial objects.
During this period, Titan also was hit repeatedly,
developing a nitrogen-rich atmosphere.
That made it a very special moon.
1977 saw the lauch of Voyager one.
Its mission.
To explore and observe the outer planets
from Jupiter to Neptune.
This was its view of Titan.
It was a close look,
but still, the moon was shrouded in a thick orange haze.
However, even then,
one scientist maintained that the haze
held the secret to sparking life below.
Bishun Khare has been trying to penetrate
the mystery of Titan's haze since the early 1970s.
He participated in the Voyager mission.
He is focused on the haze as being itself,
a source of life.
Khare introduces a nitrogen-methane mix into a sealed flask
to simulate Titan's atmosphere.
The flask is fitted with electrodes.
Now Khare discharges them.
This is meant to reproduce the effect of lightning
or other energy surges on Titan's atmosphere.
It's about 10 hours since the start of the experiment.
A reddish-brown substance has become visible
inside the flask.
Khare claims that this is the very same substance
as the haze enveloping Titan.
So what happened inside that glass vessel?
First off, the electrical surges split apart
the molecules of nitrogen and the methane.
Their atoms recombine with carbon
and other atoms in all sorts of ways
forming a variety of new organic compounds.
Analysis showed that some 200 types of organic compounds
had been created in this experiment.
Organic compounds are the materials
out of which our own bodies are made.
They are the building blocks of life.
It was thanks to Khare's work that Titan came
to be considered one of the celestial objects
on which life might exist.
The Cassini orbiter's close-up observations of Titan
have come some 30 years after Khare's experiments.
Will they confirm that Titan's hazy atmosphere
has in fact given rise to organics?
The INMS is a device that measures molecular mass.
Cassini has used it to determine the composition
of Titan's atmosphere.
Cassini's data were streamed back to Earth,
where they were analyzed by Hunter Waite and his colleagues.
Waite led the team that designed the INMS instrument package
carried aboard Cassini.
Waite's lab was able to reproduce and confirm Cassini's data
by utilizing the same INMS system.
They could then analyze accurately whatever molecules
or compounds the instrument had detected.
The results were astonishing.
Rendered in the form of a chart,
each of the different molecules identified by Cassini
is represented by its own colored area.
Various organic substances were created
in Titans' atmostphere,
ranging from ones with a single carbon atom
to more complex ones with six or seven carbon atoms.
When Cassini sent back data,
we found out that the upper atmosphere
was much more relevant than we ever thought,
that most of the chemistry seemed to be going on
in the upper atmosphere,
that very large molecules were being created
in the upper atmosphere way beyond our expectations.
Titan is one of the best
organic factories in the solar system.
Bathed in ultraviolet and cosmic rays,
Titan's upper atmosphere is continually engaged
in converting nitrogen and methane
into a rich array of organic compounds.
As these compounds collect in the lower atmosphere,
they produce Titan's famous orange haze.
Finally, they are precipitated with methane rain
onto the surface as well.
It's been four billion years
since Titan's atmosphere was formed.
During that time, it is estimated
the organic settling onto the surface
have created a layer dozens of meters thick.
The dunes discovered near Titan's equator
are thought to be a large deposit of these organics.
Now on Titan, the sand is made,
we think, from organic material.
And we think that material comes down
and gets built up into sand-size particles
that are then accumulated by the wind
to form dunes much like these.
Amidst this accumulation of organics
on Titan's surface,
are substances of vital importance to the emergence of life.
That finding was made by a young researcher
with a specialty in organic chemistry, Sarah Hörst.
Hörst has undertaken a minute examination
of the organic compounds discovered in Titan's atmosphere.
She's written her own computer program to do that.
Based on Cassini's observational data,
she faithfully simulates the composition
of Titan's atmosphere and produces the same organics.
Next, she uses her computer program
to determine the molecular structure of every compound.
These peaks right here are the masses of the ions
in the mass spectrum data,
and then it's the number of carbon, nitrogen,
oxygen, and hydrogen in each of those peaks.
So then what the code does is it goes through
and compares this information to a list that I've given it
of all of the amino acids and nucleobases
that we're looking at.
Here, we have 136, we have the molecular formula of adenine
which is five carbons that matches,
it has five nitrogens that matches,
no oxygen, and then five hydrogens.
So we know from this that we have the molecular formula
of adenine in this sample.
Genetic information for all life on Earth
is encoded in DNA.
Adenine is one of its four major components
or nucleobases.
And all four had been produced in Hörst's experiments.
If these nucleobases combine
in such a way that they create DNA,
then a huge step forward will have been taken
towards life itself.
With this discovery, speculation mounted that Titan
might actually be capable of harboring life.
Life on Titan?
It may, in fact, already exist.
If it does, what would it look like?
The search is on for the answer.
Trinidad and Tobago form an island country
in the Southern Caribbean.
They have a population of about 1.3 million.
They also have one of the most unusual lakes in the world.
It's called Pitch Lake.
It contains not water,
but naturally-occurring asphalt.
It bubbles up from an oil field that lies underneath,
creating a lake of asphalt that's 40 hectares in area
and 80 meters deep.
Strangely enough,
Pitch Lake is the side of fieldwork being done
by astrobiologist, Dirk Schulze-Makuch.
He thinks that Titan is the best candidate
for the location of extraterrestrial life.
He's come here to try to envision
what lifeforms on Titan might be like.
Asphalt, like methane,
is a hydrocarbon comprised entirely of carbon and hydrogen.
You wouldn't think this was a substance that harbors life.
But Schulze-Makuch says it actually does
contain microorganisms.
This is one of the few environments
where it's similar to Saturn's moon, Titan,
where we know that we have hydrocarbon lakes on the surface.
Obviously, Titan is very cold,
so it's still different from over here.
But we do have the liquid methane and ethane
which are also hydrocarbons.
And if we can find out what kind of organisms
are living here in the asphalt lake
and how they adapt to living in the hydrocarbons,
we think we can get some ideas to how life
could operate on a moon like Titan.
Asphalt contains almost no water.
Did you say that there's microbes in there?
Yes, there's microbial organisms in the liquid asphalt.
In this thing?
In this thing, yeah.
Like maybe one, two?
Millions.
Millions? Yeah.
Genetic analysis identified some 600 new types
of microorganisms living in the asphalt.
Most are archaebacteria
related to the primordial microorganisms
that live in extreme environments.
So for them, actually, it's a great environment,
it's a great food source,
and basically, a never-running-out food source
because it's getting supply from deep down there.
On Earth, there are microorganisms
that can use asphalt for sustenance instead of water.
Schulze-Makuch is convinced that in Titan's lakes,
there must be lifeforms that exploit methane
in a similar way.
Another scientist, Chris McKay,
holds that the methane lakes on Titan
contain creatures so unlike Earth creatures
that they exceed our wildest imaginations.
Think of fish living in water
and ask them to imagine a bird which lives in air.
They probably can't conceive of an organism
that is so much denser than the medium in which it lives.
Fish move through water by floating,
so they would imagine a bird must float in the air.
We humans live in an environment called Earth.
We produce energy by causing oxygen
and organic matter to interact.
That is our lifestyle.
But McKay is arguing that on Titan,
lifeforms would be based on a Titan lifestyle
that makes use of what's available on Titan.
Titan's atmosphere contains minuscule amounts
of hydrogen and acetylene.
McKay thinks that there may be lifeforms on Titan
that exist by deriving energy from the interaction
of those two substances in a methane environment.
McKay says that life could very well already exist on Titan.
So instead of being small and round,
I would guess that a single-celled organism on Titan
might be big and flat like a sheet of paper
to maximize its contact with the nutrients
in this thin soup.
It's living in an environment where there's not a lot
of food, so it's gotta access the food with big area
and maybe on this area, it has active molecules.
So it's like a big flat sheet of paper
with little traps on it to collect food.
To that lifeform,
that will be the normal environment.
It was not until the 21st century
that Titan's thick veil was lifted.
Now that we're getting a closer look,
what new discoveries await?
So Titan gives us a whole new set of possibilities
and there are, for sure, perhaps hundreds,
maybe millions of worlds like Titan around other stars.
Do those have life?
Titan maybe can give us some clues.
If life is found on Titan,
humanity's view of the universe will surely change.
The best place for me, in terms of finding
another type of life, would be Titan.
Because if we find it on Titan,
then we know that it really is two.
It's not the same as us.
When we go to Mars, we may find life on Mars
but we won't be sure that it's not the same life as Earth.
So my best hope would be we find life on Titan
'cause then I know that we found
two completely different types of life.
Then I can go on to some other science problem.
There is only one body in space
that we know of other than Earth,
that has a thick atmosphere and lakes.
Titan.
If life is found on Titan,
it will instantly increase the possibility
that life exists in many other places
in the universe as well.
We may not be alone in the universe.
We may have many comrades.
The quest to find out for sure continues.
Clues to solving that great mystery
lie hidden on Titan.
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