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Dr. Helen Czerski: Everything around us exists somewhere
on a vast scale from cold...to hot.
Whether living or dead, solid or liquid, visible or
invisible, everything has a temperature.
It's the hidden energy contained within matter.
And the way that energy endlessly shifts and flows
is the architect that has shaped our planet
and the universe.
Across three programs, we're going to explore
the extremes of the temperature scale,
from some of the coldest temperatures...
to the very hottest
and everything in-between.
This time, the narrow band of temperature that's
led to life.
From the origins of life in a dramatic place,
where hot meets cold...
Man: You're bringing together these
chemical ingredients that could start, you know,
producing some of the building blocks for life.
Czerski: to the latest surgery that's using temperature to
push the human body to the very limits of survival...
Temperature is in every single story
that nature has to tell,
and in this series we'll show you why.
[Birds chirping]
This is a painted lady butterfly, and it's been kept
cool, around 6 degrees, but as it sits in the Sun, it's
warming itself up, fluttering it's flight muscles,
and getting ready to fly.
These insects can't control their own body temperature,
so they're reliant on heat from the Sun.
And there he goes.
The butterfly's survival depends on its unique
and delicate relationship with temperature.
And that's true of each and every living thing
on our planet.
Plant or animal,
large or small,
everything depends on temperature for its existence.
And that relationship is far more complicated than you
might think.
There's only one place in the universe where we're
absolutely sure that life exists...and that is
here on Earth.
And for many years, it was thought that the reason why
the Earth was so unique lay in its distance
from the Sun.
Not close enough to be too hot for life, or far away enough
to be too cold.
And this gave rise to the idea of a habitable zone,
a distance from the Sun that was just right for life.
[Dogs barking]
But it turns out that it's not quite that simple...
because the Earth's temperature isn't what you
might expect.
If you average out temperatures across the
planet, from deserts to poles, you get a very pleasant
14 degrees Celsius.
But that's around 30 degrees warmer than might be
expected, given the Earth's distance from the Sun.
So why is our planet warmer than it appears it should be?
The answer lies in one of the most intriguing substances to
be found anywhere in the universe...
and yet one of the most commonplace here on Earth.
[Water rushing]
This is the Skogafoss waterfall in Iceland.
Every day here, hundreds of millions of liters of water
tumble down towards the sea.
More than 70% of Earth's surface is covered with water,
but that wasn't always the case.
Early in our planet's history when the surface was far too
hot for liquid water, this planet was shrouded
in a thick atmosphere of carbon dioxide and water.
And all you'd have seen from space is the white cloud tops.
But as the planet cooled, the rains began, and a deluge
shifted most of that water from the atmosphere to
the oceans.
And then when the rain finished and the clouds
cleared, the liquid of our blue planet was on show to the
universe for the first time.
Ever since, the sheer physical power of water has been
carving and shaping the surface of our planet.
And crucially for our story, all this water has had huge
consequences for the Earth's temperature.
To understand why, we need to delve into the strange world
of water at the molecular scale.
And that journey begins with a chance discovery that revealed
for the first time what water is actually made of.
In 1766, a reclusive scientist,
Henry Cavendish, added various metals to a liquid called
Spirits of Salt, now known as Hydrochloric acid.
And what he saw was something that he called inflammable air,
but today we know as hydrogen, and Cavendish was
the first person to recognize its significance and to do
experiments on it to test its properties.
Cavendish collected the gas given off by his experiment.
When he had enough, he took a flaming splint and put it next
to the opening....
[Loud whoosh]
with explosive results.
[Loud whoosh]
Afterwards, Cavendish noticed something intriguing.
On the inside of the glass vessel, there were tiny
droplets of a clear liquid, and he wondered what that was.
He tasted it, he smelt it, and he came to the conclusion
that it was water.
And so Cavendish was the first person to realize that water
was a combination of hydrogen and oxygen.
And today, we know that the chemical formula is H2O--
2 hydrogens and 1 oxygen.
And that's sounds beautifully simple, but still, water is
one of the most fascinating molecules we know of.
The molecular structure of water is the key to why
Earth's temperature is warmer than you might expect...
yet it's in a cold place where we can begin to understand
just why that is.
This is Jokulsarlon lagoon, in Iceland.
Isn't this all stunning?
All these bits of glacier that have just fallen off
from up there.
We take scenes like this for granted. This is our impression
of the Arctic and the Antarctic, floating icebergs.
But from a material science point of view this,
that thing, is really weird, because it's floating
with almost everything else.
When you cool things down and freeze them, the solid will
sink to the bottom of the liquid.
But water is different.
It floats.
As a liquid, the molecules of water are constantly sliding
past each other, always on the move.
But as it freezes, their positions become fixed
in a regular, hexagonal lattice.
Ice floats because the molecules in the lattice are
taking up more space than in the liquid, which makes ice
less dense than water.
This happens because of the forces holding the molecules
in position,
something that's more easily seen with water in its
liquid state.
I've got some plastic pipe here and a proper Icelandic
woolly jumper, because it's made of wool and therefore
it's good at charging up the plastic.
So this pipe now has an electric charge, and what I'm
gonna do is put it near a stream of water, and you can
see that it bends the stream really strongly.
And all the water's doing is falling, but it's being pulled
towards the electric field.
The reason for this phenomenon lies within the water
molecules themselves.
This is the water molecule. So we've got two Hs.
That's the H2, and then O is the oxygen at the top.
And the charge on the molecule isn't evenly distributed
so it's more positive round here, and it's more
negative up there.
So when the stream of water comes down, it's got all these
molecules moving round inside it.
When you bring the electrical field close, some of those
molecules will flip around, so that their opposite charge
is attracted in to the electric field, so the whole
stream of water moves.
And it's such a simple demo, but it shows you that
the water molecule itself has uneven charge distribution.
And this has a huge effect on how water behaves.
Within the liquid, the negatively charged oxygen
atom from one molecule is pulled towards the positively
charged hydrogen atoms of another, creating a strong
attraction known as a hydrogen bond.
And it's this bond that explains water's role
in distributing heat around the planet.
Hydrogen bonds are so strong, that it takes a lot of energy
to break them.
And that means that the water in the Earth's oceans can
absorb a huge amount of heat energy from the Sun, without
changing from a liquid to a gas.
The oceans act like a huge store of energy.
And as they move, they distribute heat from
the Equator to cooler latitudes north and south.
But it's not only in the oceans that water plays a part
in Earth's temperature.
While the bonds between liquid water molecules are extremely
strong, heat them up enough, and they'll break apart,
turning all that liquid into a vapor.
And in this form, as vapor in the atmosphere, water has
perhaps its greatest influence.
The atmosphere traps the Sun's heat, a process known as
the Greenhouse Effect.
But though we tend to associate this with carbon dioxide,
it's actually water vapor that accounts for much
of the trapped heat.
I've got a thermal camera here, and if I point it
at the sand and the pebbles, what you can see is that
they're bright, they're radiating away energy.
And you can see it's just the surface, because if I dig down
a little way down in the hole, everything is very dark blue.
The red areas, though, are warmer, and what's
happening is that they're emitting infrared radiation.
But while visible light can travel straight through the
atmosphere, infrared can't.
And one of the main things that stops it
is water vapor.
The water molecules are able to bend and stretch in
3 different ways, allowing them to absorb a lot of energy.
So as the infrared gets up into
the atmosphere, hits all those water molecules, some of its
absorbed and once it's been absorbed, the important point
is it isn't going straight up to space anymore.
It then gets scattered in lots of different directions,
and some of it comes back down to Earth.
It's a huge difference.
That invisible water vapor in the air is playing a huge role
in keeping us nice and warm.
Were it not for the water
in the oceans and the atmosphere keeping Earth's
temperature warm and stable, our planet would be as
inhospitable as Venus and Mars.
But the influence of temperature on life goes
far deeper.
Because the story of how life itself began is a story
of temperature,
and it starts with the Earth's complex geology.
[Wind blowing loudly]
This is the Deildartunguhver vent in Iceland,
and it's impossible to come here
and not wonder what's causing all of this.
What there is beneath my feet is a magma pool, and sea water
is seeping in through cracks and fissures.
And when it hits the hot rock, it boils.
And all of this is just the spout of a gigantic
natural kettle.
This is a thermal vent.
It gives us a rare glimpse of the heat at the Earth's core.
But here at the surface of the planet isn't the only place
where such vents exist.
Similar vents can be found deep on the ocean floor.
And even in this dark, inhospitable place, many
are teeming with life,
a profusion of organisms found in few other places on Earth.
It's a spectacle that Dr. Jon Copley from the University
of Southampton has seen firsthand.
Copley: When you get a moment to pause and think, you're struck
by how you are next to a truly awesome force of nature.
Czerski: Jon is part of a research project exploring the
life that exists around these deep sea vents.
Stuff that's gushing out, what's in it?
Copley: That's a very hot mineral-rich fluid.
How hot? Well, these vents-- 401 degrees C.
Which is enormous! Enormous!
Copley: Yeah, and it's still liquid.
It doesn't boil into steam because of the pressure,
because we're at 500 times atmospheric pressure.
It's still liquid.
And it's mineral-rich because that hot fluid is the end
product of seawater percolating down into
the ocean crust.
There it's reacting with the surrounding rocks and it's
leaching a lot of minerals and elements from those rocks.
So we've got microbes that can use some of those dissolved
minerals as an energy source.
Czerski: There's some thinking that these sorts of places
might have been where life originated.
What makes them so good for that?
Copley: When we're making a temperature measurement
at the throat of one of these vents, and we're reading
401 degrees, if we move that temperature probe a few
centimeters in that flow coming out of the top of that
what we call "chimney," it'll drop off by 120 degrees.
And then the chemistry is changing over that distance as
well from being really rich in these dissolved minerals to
being much more influenced by, you know, normal sea water
and that's mixing.
So we've got changes in chemistry and in temperature
over very, very small spaces.
And that means you can get very exciting reactions.
Reactions will run more rapidly at higher
temperatures, and you're bringing together these
chemical ingredients that, you know, could start producing
some of the building blocks for life.
Czerski: Even looking at the pictures, feels like you're
looking at something very primitive, that there was one
moment at some point that might have happened
in an environment like this that just tipped chemistry
into biology and it's a huge thought!
When we explore these today, we become aware that,
you know, there are several thousand of these out there
dotted around the world's oceans, and they're roiling
away all the time.
Give yourself millions of years, and at some point,
it was enough.
And it tipped things over, you know, to give us life from
just physics and chemistry.
Czerski: If life did begin at these vents, then to move beyond
them, it was going to need a different source
of energy altogether...
one derived not from the heat of the planet, but from
somewhere else.
And that source was revealed by a chance discovery
in the 18th century by a scientist who wasn't even
looking for it.
In the 1770s, there was a Dutch physician called
Jan Ingenhousz, and he was a medical doctor who'd become
famous for smallpox inoculations.
But he had a lively mind.
He paid attention to the science of his day, and that
decade he turned his mind to leaves.
Ingenhousz had recently read of an experiment involving
plant leaves submerged in water, which had resulted
in the appearance of bubbles of a mystery gas.
Some scientists of the day thought that the bubbles were
attracted by the leaves from the water, but Ingenhousz
wasn't convinced and he did his own experiments.
The first observation that he made was that the bubbles
didn't form when the leaves were in shadow, but they did
form when you put them in the sunlight.
And he checked very carefully that it wasn't just the warmth
of the Sun, it was actually the light itself.
And the gas wasn't coming from the water.
It seemed to be coming from the leaves.
Ingenhousz tested the gas and discovered that it was
pure oxygen.
He had uncovered one of the most fundamental processes
in all of nature.
Photosynthesis.
Plants absorb energy from the Sun and use it to break
molecules of water into hydrogen and oxygen.
The oxygen is released, as Ingenhousz observed.
And just as important is what happens to the hydrogen.
It combines with carbon dioxide to form carbohydrates,
specifically sugars, making the plants a store of energy.
By tapping into the energy from sunlight, life could now
move away from thermal vents and spread across the globe,
first in the oceans and eventually onto land...
endlessly harvesting energy from the Sun and locking it
into the chemical bonds of sugar molecules, a process
that's crucial to all life on Earth today.
The sugars formed
in photosynthesis are the beginning of almost every
food chain.
Further up the chain, complex life forms unlock that energy,
using it as the fuel that powers the thousands
of chemical reactions that take place in their cells to
keep them alive.
But here, temperature poses an intriguing problem.
At our everyday temperatures, most biochemical reactions
happen too slowly to sustain life.
To make them happen fast enough requires a special kind
of molecule, one that itself can only exist within the
tiniest band of temperature.
And there's a simple way of showing this.
I've got two glasses here, both of them have a little bit
of corn starch in water and a little bit of iodine which is
what's made them purple.
And I'm gonna add some of my own saliva using one of these
and a cheek swab just to one of them.
Here we go.
Lovely.
And I'm gonna stir it into that one.
Starch is present in foods like bread and potatoes.
It's a complex carbohydrate with long-chain molecules.
And over 5 minutes, we can see that adding saliva to our
starch mixture has caused an obvious change.
You can see that the one with the spit in has definitely
changed color.
A chemical reaction's happened, and it's actually
one that happens all the time in all of us, both in our
mouths and further down our digestive system.
What's going on is that there's an enzyme,
a biological catalyst in my saliva, which is breaking that
carbohydrate down into simple sugars.
And enzymes like this are the root of all biology,
because they speed reactions up.
They don't change what happens, but they make them
happen faster.
There are 3,000 different types of enzymes in our body.
Each one speeds up a specific reaction sometimes more than
a million times.
Behind every process in our body--breathing, moving,
thinking--lies a series of very precise reactions powered
by particular enzymes.
Enzymes are fabulous little biological machines,
but they've got a limitation connected to temperature.
Like most chemical reactions, if you increase the
temperature, an enzyme will work a little bit faster,
until you increase the temperature past a certain
point, and at that point everything stops happening.
And there's a simple reason why.
An egg white is made of protein molecules.
The familiar way its color and texture change when cooked
is because those protein molecules change in structure
when they get hot.
Enzymes are also proteins.
Like the egg white, if they get too hot, their structure
changes permanently,
and they're no longer able to perform their
specialized function.
So, keeping them at precisely the right temperature
is crucial.
Plants and animals that live in the oceans have it
relatively easy, thanks to the water providing a stable
temperature environment,
but living on land has always presented much more
of a temperature challenge.
The fluctuations between night and day and from season to
season mean that animals need to be able to control their
body temperature.
Throughout most of the history of animal life, there's one
method that's endured.
And there's one animal here at Colchester Zoo that's
perfected it.
Man: All right, so I'll ask you to wait there.
Czerski: All right.
His keeper is Glenn Fairweather.
Fairweather: Telu!
Telu!
Come on. That's it.
Good boy. Here he comes.
This is Telu, an adult male Komodo dragon.
Czerski: That is a lot of lizard.
- He's enormous. - He is big, yeah.
Czerski: Slightly clumsy lizard.
Komodo dragons, like Telu, are the largest lizard to be
found anywhere on Earth.
Fairweather: OK, well I'm just gonna give Telu a little snack.
Czerski: OK.
Oh, didn't notice it. Ha ha!
He's having a good look around there.
- Oh. - Yeah.
Fairweather: Fantastic.
In the wild, dragons will eat 10 to 12 meals a year, maybe.
12 meals a year sounds like almost nothing.
Fairweather: They have a very slow metabolism, so it would
take Telu several weeks to digest a large meal
of 10, 15, 20 kilos.
Czerski: The reason Telu eats so little
is that he's cold-blooded.
Instead of using energy from his food to warm himself up,
he takes in heat from his surroundings.
In his natural habitat in Indonesia, he'd do that simply
by basking in the Sun.
In captivity, he has special lamps to provide both heat
and ultraviolet light.
This unique footage filmed at Chester Zoo, shows how rapidly
a Komodo dragon can alter its body temperature.
In just 90 minutes, this animal's body warms from
its nighttime temperature of 22 degrees, to 35 degrees.
To stay active for the rest of the day,
it must now keep its body in a narrow range
of between 34 and 36 degrees.
Paleontologist Dr. Darren Naish explains how they do it.
So he's in front of his heat lamp, and he's done
something quite distinctive, which he's sort of spread
himself out flat.
Why has that happened?
Yeah, in order to basically be the best shape to
absorb as much heat as possible from the environment,
a lot of reptiles adopt specific poses.
And the most obvious thing they do is they do spread out
and flatten the rib cage so they're presenting a larger
surface area to the Sun.
What Telu here is doing is absorbing heat from his
heat lamp.
He's also receiving heat from the ground which has obviously
been warmed by the heat lamp and through his own behavior.
He's very good at controlling his temperature, keeping it
quite high and in a very specific band.
Czerski: Being cold-blooded does come with an obvious limitation.
You need enough heat in your environment.
Naish: We definitely do see a massive dropoff
in the diversity of cold- blooded reptiles like lizards
once you get away from the Equator, once you get further
towards the north, so clearly they are disadvantaged
in cooler environments.
Today, we mostly associate cold- blooded animals with places
where there are warm conditions, year-round.
Czerski: So, for cold-blooded animals,
the challenge of keeping warm enough
tends to limit them to the hotter regions
of the planet.
To thrive in cooler places, you need a different way to
keep your body temperature warm and stable.
And evidence for this comes from perhaps the last group
of animals you'd expect.
Dr. Adam Smith is a curator here at Wollaton Hall Natural
History Museum.
Smith: When I was a kid growing up, the picture
of the environment that dinosaurs lived in was
a swampy environment surrounded by volcanos.
But we now know that dinosaurs were much more diverse than
that, and the environments that they occupied were much
more diverse than that as well.
Some of them were adapted for living in forests, some were
adapted for living in open landscapes.
Some lived on the shore.
Even quite snowy areas would have been occupied
by dinosaurs.
Czerski: For decades, the spread of dinosaurs into cooler regions
away from the tropics posed a question.
How could large cold-blooded creatures survive
in colder climates?
Then, in 1996, a fossil was discovered in China that
changed everything.
So this specimen is obviously beautifully preserved.
What is it?
Smith: This is a genuine fossil of a Sinosauropteryx dinosaur.
It was living in a climate that was similar to
Northern Europe, and so you would have had warm seasons
and cold seasons.
And the special thing about it is that in addition to
the bones being preserved, we have evidence of the soft
tissues as well.
You can see it most clearly running along the back
of the tail here, this dark line, and, especially
at the every tip of the tail, it looks very tuft-like.
Czerski: The dark line on this 125-million-year-old
Sinosauropteryx fossil is only faint, but it's tantalizing
evidence for something you wouldn't expect on a dinosaur.
Smith: It's very similar to the downy material that you find
on a newly hatched chick.
And that's why this has been interpreted as feathers.
Czerski: So this is a dinosaur, and it's got feathers.
Smith: And not true feathers as you would think of as
a bird's feathers, but they were the structures that led
to true feathers.
They're fuzzy feathers, so they've been given
the name proto-feathers.
Czerski: For paleontologists, these fuzzy feathers were
a spectacular revelation.
Smith: The fuzz in the dinosaurs suggests that they were using
it for insulation.
And in that case, you would expect the dinosaurs to be
generating their own heat, rather than basking in the Sun
to get warm from the outside environment.
Czerski: Cold-blooded animals tend not to have feathers,
in part because their skin needs to absorb heat from
the environment.
So this animal, that suggests, was not cold-blooded?
It's very likely, based on the evidence from the
feathers, that this particular dinosaur was warm-blooded.
This discovery is helping scientists to reimagine
the world of dinosaurs.
Smith: In the case of these dinosaurs, we know that they
were very active animals, very agile dinosaurs,
very intelligent animals as well.
[Water rushing]
[Roars]
Czerski: It's now thought that many dinosaurs may have been
at least partly warm-blooded.
This would have made them less reliant on the Sun and allowed
them to thrive in cooler habitats.
Had an asteroid impact not contributed to their
extinction, some of them might still exist today.
The dinosaurs that did survive evolved into modern birds,
which are warm-blooded.
And alongside them grew the rapidly expanding class
of warm-blooded mammals.
Birds and mammals use the energy from food to generate
their own body heat.
And one area that's particularly sensitive to
temperature is the brain.
This powerful but fragile organ generates intense heat
of its own.
So animals need a way to keep it at precisely
the right temperature.
And that's especially true of us big-brained humans.
We're used to the idea that our body temperature is
37 degrees, but we don't often think about just how hard our
system has to work to make sure that's true.
I do a lot of sport, so I run around all the time, and that
sort of exercise puts a lot of stress on the system,
and the body has a challenge to get rid of that heat.
One obvious way our bodies do this is to sweat.
But to see what else is going on, we need to use a thermal
imaging camera.
This will show the temperature at the interface between the
skin and the surrounding air.
The lighter and brighter the color, the hotter
the temperature.
Watching the thermal footage of me playing is fascinating
because there's so much detail.
And you can see that my surface temperature's
different in different places.
So my face is obviously very warm.
Under my arms are very warm, all the places where there's
blood flow close to the surface.
Those show up really, really brightly, and the really
interesting bit here is when you look just after
I've stopped.
And you can see how hard my body is working to get rid
of that heat.
My blood vessels on my arms are just shining out, 'cause
they're so warm.
That's because when we're getting too hot, our brain
tells the blood vessels supplying our skin to widen.
This increases the flow of blood to the surface
of the skin, where it can dissipate heat.
The shifting of blood to and from the skin's surface is
an effective way to control our body temperature.
It helps keep our bodies within a very narrow and safe
window of temperature, even during the most
intense exercise.
The amazing thing about this is, I run around in this
sports hall all the time, and I never have to think
about this.
My body just takes care of it all.
But when we get cold, our bodies face
the opposite challenge.
Not dissipating heat, but hanging onto it.
To understand how our bodies deal with cold, we've come to
the University of Portsmouth to meet Professor Mike Timpton,
an expert in cold-water survival.
Woman: Further round.
OK, have to go back in there a sec.
Czerski: He's going to show us what happens when the human body
is immersed in a tank of water that's been chilled down to
18 degrees Celsius,
nearly 20 degrees below normal core body temperature.
The test begins with a few simple manual tasks that will
be repeated later.
Plimpton: 3, 2, 1, go.
Now come back.
- That's good, well done. - OK.
- Right, done. - Yep, 22 seconds.
- OK. - We'll remember that.
[Click]
Finally the test can begin.
I sudden have immense sympathy for witches
in the 16th century.
4, 3, 2, 1, go.
Czerski: Oh, it's horrible.
It's amazing how the urge to breathe is very sudden.
With the body now submerged, its survival
mechanisms kick in.
I have started to shiver.
About a minute ago, I started to shiver.
Timpton: The skin receptors are sending messages into
the brain saying, "You've got a very cold skin."
And so that's being integrated in the center of the brain,
the hypothalamus of the brain, that's saying, "We need to
start generating heat."
And that's why you've started shivering.
Czerski: Shivering is the body's attempt to counteract the cold
by producing its own heat to prevent vital organs from
dropping in temperature.
I heard that. Yeah.
But in these conditions, shivering alone isn't enough.
A drop in core temperature of just 2 degrees Celsius would
cause hypothermia, so after half an hour, Mike calls
a halt to proceedings.
Timpton: I think it's probably time to bring you out.
- OK. - You ready? Here we go.
It's at this point that the thermal imaging camera reveals
another of the body's responses to cold.
Dark-blue areas indicate where the surface temperature has
dropped dramatically, as blood is diverted away from
the cold water.
Timpton: The body will sacrifice the extremities in order to
preserve the internal organs.
And you'll have people who have got frostbite, they're
losing extremities, but, to preserve their heart
and their brain temperatures, because once those
temperatures fall, then it's a threat to survival.
So what we're going to do now is just ask you to do that
nut and bolt test again.
3, 2, 1, go.
Czerski: My wrists are very cold and I feel that's stopping me
moving my fingers very well.
That's it. Done. No, there we are.
- Yeah. - Bang on a minute.
Really? So 3 times?
22 seconds before, a minute afterwards.
Czerski: What this test shows
is just how vulnerable the human body is to cold.
In fact, what enables us humans to survive and thrive
in cold temperatures isn't our inbuilt survival mechanisms.
It's something else.
Timpton: Our physiological responses to cold really
wouldn't let you move very far away from your
equatorial origins.
You know, once you start getting into 0 degrees
overnight, the level of heat production and the level
of heat retention you've got will have been very limiting.
And the really important thing is that it's underpinned
by intellect.
We've been using clothing 75,000 years.
We've been using fire, for 1 million years.
Now as soon as you've done that, you've got a source
of heat, you've got a source of light.
You can cook food, your diet can change.
You are a tropical animal that's taken those origins
with it thermally.
So you've re-created a microclimate next to your
skin, which would be the same as if you were living naked
in a 28-degree environment from which you evolved.
Czerski: While all life on Earth has adapted to survive the
temperature of its habitat, only we humans are able to
create micro-habitats of our own.
[Barking]
We can maintain our ideal temperature wherever we go,
thanks to our intelligence.
But human ingenuity hasn't just enabled us to manipulate
the temperature of our environment.
It's also allowed us, in very special circumstances, to push
the boundaries of life itself.
It's 8 A.M., and a team from Papworth Hospital is getting
ready to perform a radical type of surgery.
It involves cooling a patient's body to
a temperature that would normally be fatal, taking them
to the very edge of life.
Justine Giller has a life- threatening condition.
Clots are blocking the blood vessels in her lungs, leaving
her struggling for breath.
Giller: I've continuously got a tightness in my chest,
just doing normal things like going up and down the stairs.
I'm out of breath.
It's quite daunting, but I know obviously I've got to
have this operation.
if I don't, I don't know how long I'm gonna be able to
continue for.
So, I know that I have to do it in order to be able to take
my little girl to the park and play.
[Sniffs]
It's down to surgeon David Jenkins to remove the clots
from Justine's lungs.
But while blood is flowing through her lungs,
the operation is impossible.
Jenkins: Well, the main problem is that lungs usually have
5 liters of blood every minute being pumped through them.
And for this operation, we need a completely clear
field in the small vessels in the lungs.
So the only way to do that is to drain all the blood out
of the body.
Czerski: Removing a patient's entire blood supply is a truly
extraordinary procedure, and David is a leading
specialist in the technique.
Once Justine is under anesthetic, the first step is
to divert her blood supply to a heart-lung machine.
At this stage, her blood is still delivering fresh oxygen
to her vital organs and, crucially, her brain.
- Running OK? - It's running well.
At David's command, the machine drains all of
Justine's blood from her body.
He can now begin to remove the clots from her lungs, but he
has to work against the clock.
Because without blood circulating, Justine no longer
has a supply of oxygen.
Normally, the human brain can only survive for around
4 minutes without fresh oxygen before permanent
damage occurs.
But in the controlled environment of the operating
theatre, Justine is being kept alive by temperature.
Over the past two hours, Justine's body has slowly been
cooled to just 20 degrees.
This is the key to the entire procedure.
Her body is in a temporary state of stasis.
At this temperature, the function of Justine's
brain is slowed down, and it can survive 20 minutes
without oxygen.
The process is being supervised by anesthetist
Dr. Joe Arrowsmith.
Our body has all these mechanisms to stop us getting
that cold.
Why isn't she shivering?
Arrowsmith: Well, the anesthetic I've given her has disabled all
of those mechanisms.
I've paralyzed her skeletal muscle, so she physically
cannot shiver.
Czerski: To reduce the need for oxygen as much as possible,
the team have cooled Justine's brain still further.
Arrowsmith: We have this cap wrapped around Justine's head,
and it's got a continuous flow of ice-cold water that comes
from this ice bath here with freezer ice packs in.
What we believe this does is keep the outer centimeter or two
of the brain slightly cooler than the rest
of the brain, where the brain matter is where all
of the cell bodies and most of the metabolism is, and so we
think that buys us just a little bit of extra
brain protection.
Jenkins: So the right side is done, and we managed to do
that in just under 15 minutes, so that's good.
And we're back on the heart-lung machine now.
Czerski: With the clot removed, Justine's blood is returned
via the machine.
It gradually warms up her blood and, in turn, her body.
And after a while, her heart spontaneously restarts.
After 6 hours in surgery, Justine has returned safely
from her remarkable journey down the temperature scale...
a living testament to how our ability to manipulate
temperature is beginning to open up a whole new field
of medical possibilities.
We're alive, you and I, which means that we're
directly connected to the web of life that covers this
planet and extends back through almost all
of its history.
And all of that web, in all of its variety, only exists
within a very narrow temperature range.
And we barely appreciate the temperatures of life.
But next time you hold someone's hand or give
them a hug, it's worth remembering that
it's not just about the physical gesture.
You're sharing the warmth of life.
And it's a nice thought that that shows just how intimately
temperature and life are intertwined.
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