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We live on a world of wonders. | 0:00:08 | 0:00:10 | |
A place of astonishing beauty and complexity. | 0:00:10 | 0:00:16 | |
There are vast oceans and incredible weather. | 0:00:17 | 0:00:21 | |
Giant mountains | 0:00:22 | 0:00:25 | |
and stunning landscapes. | 0:00:25 | 0:00:27 | |
I'm a physicist, and I'm fascinated by the way that the universal laws of nature | 0:00:30 | 0:00:37 | |
that made all this, also created such diverse and different worlds | 0:00:37 | 0:00:42 | |
out there in the solar system. | 0:00:42 | 0:00:45 | |
I think we're living through the greatest age of discovery our civilisation has known. | 0:00:47 | 0:00:52 | |
We've voyaged to the farthest reaches of the solar system. | 0:00:52 | 0:00:56 | |
We've photographed strange new worlds, | 0:00:56 | 0:01:00 | |
stood in unfamiliar landscapes, tasted alien air. | 0:01:00 | 0:01:05 | |
But the one thing we haven't found on those worlds | 0:01:08 | 0:01:12 | |
is the thing that makes our planet unique. | 0:01:12 | 0:01:16 | |
Life. | 0:01:19 | 0:01:21 | |
But is that really true? | 0:01:21 | 0:01:23 | |
Is the Earth the only place in the solar system that could support life? | 0:01:23 | 0:01:28 | |
In this film we will search the solar system for worlds that harbour the conditions to support life. | 0:01:30 | 0:01:37 | |
What we find on these worlds may help us answer the question, are we alone in the universe? | 0:01:40 | 0:01:47 | |
That's not only one of the great fundamental questions for science, | 0:01:51 | 0:01:56 | |
but one of the great unanswered questions in human history. | 0:01:56 | 0:02:01 | |
Floating in the Sea of Cortez off the cost of Mexico is the research vessel Atlantis, | 0:02:31 | 0:02:38 | |
the mother ship for the exploration of one of the most alien worlds we know. | 0:02:38 | 0:02:43 | |
But it's an alien world on our planet. | 0:02:48 | 0:02:50 | |
The Atlantis is the launch vessel for Alvin, | 0:03:05 | 0:03:08 | |
one of the world's most rugged submarines. | 0:03:08 | 0:03:13 | |
Built like a spacecraft, | 0:03:13 | 0:03:15 | |
it's designed to explore the deepest depths of the ocean. | 0:03:15 | 0:03:19 | |
And I'm lucky enough to have hitched a ride down to the sea floor, | 0:03:21 | 0:03:25 | |
two kilometres beneath the surface. | 0:03:25 | 0:03:28 | |
That has got to be the closest thing to going into space that you can do. | 0:03:32 | 0:03:36 | |
And, given that I'm not going to go into space any time soon, I think it's the next best thing. | 0:03:36 | 0:03:41 | |
See you in eight hours. | 0:03:43 | 0:03:45 | |
Roger, Alvin. Your checks are good. Permission to dive. | 0:04:00 | 0:04:04 | |
Roger. Alvin diving. | 0:04:05 | 0:04:07 | |
The parallels to spaceflight are obvious. | 0:04:15 | 0:04:19 | |
As the tiny capsule descends, we are leaving the familiar world | 0:04:19 | 0:04:24 | |
of the surface of our planet, and entering a strange, hostile world. | 0:04:24 | 0:04:29 | |
If anything goes wrong, we will be completely on our own. | 0:04:34 | 0:04:39 | |
MACHINE BEEPS | 0:04:46 | 0:04:50 | |
Beeping is never good. | 0:04:53 | 0:04:55 | |
'Fortunately, Alvin is one of only a handful of submarines | 0:04:57 | 0:05:02 | |
'that can withstand the colossal pressure of the deep ocean.' | 0:05:02 | 0:05:06 | |
At the Earth's surface, we're used to one atmosphere of pressure. | 0:05:08 | 0:05:13 | |
As we descend, the pressure increases by another atmosphere every ten metres. | 0:05:13 | 0:05:20 | |
And it soon adds up. | 0:05:20 | 0:05:22 | |
We're approaching a kilometre deep. The pressure outside there is now | 0:05:28 | 0:05:33 | |
100 atmospheres, that's higher than the atmospheric pressure on the surface of Venus. | 0:05:33 | 0:05:39 | |
Without knowing, if you were asked a question, could life exist down here, 100 atmospheres, | 0:05:39 | 0:05:45 | |
cold, dark no sign of sunlight at all, | 0:05:45 | 0:05:49 | |
it's pitch black there, you would say no. | 0:05:49 | 0:05:53 | |
Well, I would say no. | 0:05:53 | 0:05:54 | |
But the depths of the ocean are not lifeless. | 0:06:00 | 0:06:04 | |
Illuminated by Alvin's lights, | 0:06:04 | 0:06:07 | |
we find oases of life in the deserts of the ocean floor. | 0:06:07 | 0:06:12 | |
So we have landed, after about an hour of descent. | 0:06:18 | 0:06:22 | |
We've just stopped in the most incredible place. | 0:06:22 | 0:06:25 | |
Look at those. | 0:06:25 | 0:06:28 | |
We've landed on top of the tube worms. | 0:06:28 | 0:06:31 | |
Amazing things. | 0:06:32 | 0:06:34 | |
This underwater city is one of the most bizarre environments on our planet. | 0:06:42 | 0:06:47 | |
It's built around a hydrothermal vent, a volcanic opening in the Earth's crust | 0:07:00 | 0:07:06 | |
that pumps out clouds of sulphurous chemicals and water heated to nearly 300 Celsius. | 0:07:06 | 0:07:14 | |
And somehow, life has found a way to thrive in these most extreme conditions. | 0:07:14 | 0:07:21 | |
This is a genuinely remarkable place. | 0:07:29 | 0:07:32 | |
There are mats, | 0:07:32 | 0:07:35 | |
carpets of yellow bacteria. | 0:07:35 | 0:07:40 | |
Look at that. It's not only just bacterial blobs, | 0:07:42 | 0:07:45 | |
there is real complex organisms. | 0:07:45 | 0:07:48 | |
Alien. I want to say that word, alien environment. | 0:07:48 | 0:07:51 | |
It really is alien to us. | 0:07:51 | 0:07:53 | |
For me, the fascinating thing about finding life down here | 0:07:57 | 0:08:01 | |
is that the conditions on the | 0:08:01 | 0:08:03 | |
deep ocean floor are more similar in many ways to the conditions on | 0:08:03 | 0:08:08 | |
worlds hundreds of millions of kilometres away out there | 0:08:08 | 0:08:12 | |
in the solar system than they are to the conditions just two kilometres from my head on the Earth's surface. | 0:08:12 | 0:08:18 | |
It's incredibly dark, there is no sunlight, | 0:08:18 | 0:08:22 | |
there's a brutal mixture of hot and cold water, | 0:08:22 | 0:08:26 | |
and just rock and minerals. | 0:08:26 | 0:08:29 | |
So, if life can not only survive but even flourish in these conditions, | 0:08:29 | 0:08:35 | |
then you've got to feel that it's much more likely that life can | 0:08:35 | 0:08:39 | |
also survive and flourish out there in the solar system. | 0:08:39 | 0:08:43 | |
Ever since the invention of the telescope 400 years ago, | 0:08:52 | 0:08:56 | |
we have looked to our neighbouring worlds for signs of life. | 0:08:56 | 0:09:01 | |
As technology has improved, we've been able to search the planets in more and more detail, | 0:09:05 | 0:09:10 | |
and we have found nothing. | 0:09:10 | 0:09:13 | |
But that doesn't mean the rest of the solar system is dead, | 0:09:14 | 0:09:18 | |
because we're only beginning to scratch the surface of what's out there. | 0:09:18 | 0:09:22 | |
There are literally hundreds of other worlds. | 0:09:27 | 0:09:31 | |
Planets and their moons which we have barely explored. | 0:09:31 | 0:09:35 | |
Among them may be worlds that hold the conditions to support life. | 0:09:39 | 0:09:44 | |
And the best way to find out what those conditions are | 0:09:48 | 0:09:51 | |
is to look at the one place we know life flourishes. | 0:09:51 | 0:09:55 | |
The Earth. | 0:09:58 | 0:10:00 | |
Life is pretty much only chemistry. | 0:10:11 | 0:10:14 | |
It's just the reactions between atoms and molecules. | 0:10:14 | 0:10:18 | |
And so for life to exist, you only really need three things. | 0:10:18 | 0:10:21 | |
First of all, you need the right chemistry set. | 0:10:21 | 0:10:24 | |
Now, I'm made of something like 40 elements, | 0:10:24 | 0:10:28 | |
almost half of the known elements, which is pretty complicated. | 0:10:28 | 0:10:31 | |
But actually 96% of me is only made of four of them, carbon, nitrogen, oxygen and hydrogen. | 0:10:31 | 0:10:37 | |
Secondly, you need a power source. | 0:10:37 | 0:10:40 | |
You need a battery, something to make a flow of electrons | 0:10:40 | 0:10:44 | |
that powers the processes of life. | 0:10:44 | 0:10:47 | |
Now here on Earth, most life uses the power of the sun. | 0:10:47 | 0:10:53 | |
And thirdly, you need some kind of medium for life to play itself out in, | 0:10:53 | 0:10:59 | |
for processes to happen. | 0:10:59 | 0:11:01 | |
And here on Earth, | 0:11:01 | 0:11:04 | |
you don't have to look very far at all to find that medium, that solvent. | 0:11:04 | 0:11:07 | |
Because it's this, water. | 0:11:07 | 0:11:10 | |
If you want to see how important water is to life, | 0:11:32 | 0:11:35 | |
there's no better place to come than the Atacama desert in Chile. | 0:11:35 | 0:11:40 | |
The soil here is more sterile than a hospital operating theatre. | 0:11:46 | 0:11:52 | |
In fact, scientists have looked for the most basic form of life, bacteria, | 0:11:52 | 0:11:56 | |
in some parts of the Atacama, and they found absolutely nothing. | 0:11:56 | 0:12:01 | |
All deserts are characterised by a lack of moisture. | 0:12:05 | 0:12:09 | |
But the Atacama takes that to the extremes. | 0:12:09 | 0:12:12 | |
The Sahara is 50 times wetter than the Atacama. | 0:12:14 | 0:12:18 | |
There are weather stations here that have measured 1mm of rainfall in 10 years. | 0:12:18 | 0:12:23 | |
There are river valleys that have been dry for 120,000 years. | 0:12:23 | 0:12:27 | |
There are rocks that haven't seen rainfall for 20 million years. | 0:12:27 | 0:12:33 | |
It's this dryness that explains why nothing can survive here. | 0:12:39 | 0:12:44 | |
Even the most primitive form of life on Earth, the bacteria, | 0:12:44 | 0:12:49 | |
need water for their survival. | 0:12:49 | 0:12:52 | |
And there are no exceptions. | 0:12:52 | 0:12:54 | |
And this seemingly fundamental link between water and life | 0:12:54 | 0:12:58 | |
is driving the search for life out there in the solar system. | 0:12:58 | 0:13:02 | |
Because, wherever we find water, | 0:13:02 | 0:13:05 | |
that will be the best place to look for life beyond the Earth. | 0:13:05 | 0:13:09 | |
The Earth is the only planet that currently has liquid water on its surface. | 0:13:14 | 0:13:20 | |
The other planets are either too close to the sun, | 0:13:20 | 0:13:23 | |
like Mercury, and baked dry. | 0:13:23 | 0:13:27 | |
Or they are too far away. | 0:13:27 | 0:13:30 | |
Saturn's rings are made of water, but in the depths of space, it's frozen into lumps of solid ice. | 0:13:30 | 0:13:38 | |
But that doesn't mean that liquid water has never existed elsewhere in the solar system. | 0:13:42 | 0:13:48 | |
And if it has, we should be able to find the evidence, | 0:13:48 | 0:13:52 | |
because wherever water goes, it leaves its footprints. | 0:13:54 | 0:13:58 | |
These are the Scablands, a remote part of the North Western United States. | 0:14:09 | 0:14:14 | |
It's one of the most spectacular places to come to see how water | 0:14:14 | 0:14:20 | |
carves its signature into the landscape. | 0:14:20 | 0:14:23 | |
The largest flood on Earth went through this area here. | 0:14:30 | 0:14:34 | |
Jim Rice is an astro-geologist. He believes that understanding the events that created this landscape | 0:14:34 | 0:14:39 | |
can help in the search for water on other planets. | 0:14:39 | 0:14:43 | |
We are kind of like CSI arriving at the scene of a crime, this is the evidence left here. | 0:14:43 | 0:14:47 | |
-We've come to piece it together. -I can see this is not a normal river system. | 0:14:47 | 0:14:52 | |
You can see, because it is so straight. | 0:14:52 | 0:14:54 | |
There is no meandering of a river here, it's just a big hole. | 0:14:54 | 0:15:00 | |
This entire landscape was created at the end of the last Ice Age. | 0:15:07 | 0:15:12 | |
200 miles to the east lay a huge lake, held in place by a wall of glacial ice. | 0:15:15 | 0:15:23 | |
When that wall ruptured, over 2,000 cubic kilometres of water swept out in a single catastrophic event. | 0:15:24 | 0:15:33 | |
The flood waters were at least 400 feet deep here. | 0:15:38 | 0:15:40 | |
But actually they were another 200 feet stacked on top of that, coming across here. | 0:15:40 | 0:15:44 | |
So we would be under 200 feet of water standing right here. | 0:15:44 | 0:15:48 | |
So am I to imagine a wave? | 0:15:48 | 0:15:51 | |
Yeah, a massive wave rolling, rumbling, this water would | 0:15:51 | 0:15:55 | |
be charged full of big chunks of ice from that ice dam. | 0:15:55 | 0:15:57 | |
It would be loaded with big chunks of the salt bed rock being gouged, ripped out of here. | 0:15:57 | 0:16:03 | |
It would be an impressive sight. | 0:16:03 | 0:16:05 | |
As the floodwaters tore across the landscape, they carved out this 20 mile long canyon. | 0:16:15 | 0:16:21 | |
And at its head, it left these giant horseshoes. | 0:16:24 | 0:16:28 | |
At over 400 feet high and five miles across, | 0:16:28 | 0:16:32 | |
this was the largest waterfall the world has ever known. | 0:16:32 | 0:16:37 | |
The easiest way of thinking about it is if you took every river in the world, put them in | 0:16:44 | 0:16:49 | |
the same location, had them flowing at the same time, these floods are 10 times larger than that. | 0:16:49 | 0:16:55 | |
And how long do we think it took to sculpt this landscape? | 0:16:55 | 0:17:00 | |
48 hours to a week. | 0:17:00 | 0:17:02 | |
It's instantaneous, geologically. | 0:17:02 | 0:17:04 | |
The Scablands reveal the characteristic signature | 0:17:07 | 0:17:11 | |
that water carves into the landscape. | 0:17:11 | 0:17:14 | |
It's a signature that can be seen from space, and not just on the Earth. | 0:17:15 | 0:17:21 | |
When we turn our telescopes on our next door neighbour and prime candidate for finding | 0:17:24 | 0:17:30 | |
alien life, the planet Mars, | 0:17:30 | 0:17:32 | |
we find almost identical features cut into its surface. | 0:17:32 | 0:17:37 | |
The Red Planet is covered in outflow channels. | 0:17:44 | 0:17:49 | |
Straight, wide canyons, exactly like the Scablands. | 0:17:49 | 0:17:53 | |
And they are filled with identical geological features. | 0:17:55 | 0:18:00 | |
It all suggests that similar huge floods once tore across the surface of Mars. | 0:18:10 | 0:18:17 | |
This is a picture of here from the air. | 0:18:17 | 0:18:21 | |
I am sat somewhere around here. | 0:18:21 | 0:18:23 | |
And here are the horseshoe shapes of the dry folds which are just over there. | 0:18:23 | 0:18:31 | |
This is a picture taken of the surface of Mars, | 0:18:31 | 0:18:36 | |
and you see those typical horseshoe shapes of the folds. | 0:18:36 | 0:18:41 | |
Also, you see the structures upstream of the folds, these grooves cut into the landscape. | 0:18:41 | 0:18:48 | |
And you see that here, grooves cut into the landscape as the water | 0:18:48 | 0:18:53 | |
cascades down and then flows over the folds | 0:18:53 | 0:18:57 | |
and cuts the gigantic valleys out as it moves downstream. | 0:18:57 | 0:19:01 | |
So, all this adds up, I think, to an overwhelming smoking gun | 0:19:02 | 0:19:09 | |
that there were vast amounts of water that flowed very quickly | 0:19:09 | 0:19:14 | |
over the surface of Mars at some point in the past. | 0:19:14 | 0:19:17 | |
But although the outflow channels are proof that liquid water once flowed across Mars, | 0:19:21 | 0:19:28 | |
it may not point to the existence of life. | 0:19:28 | 0:19:30 | |
Because if the Martian landscapes were formed by the same processes that formed the Scablands on Earth, | 0:19:34 | 0:19:41 | |
the floods that created them may only have lasted a matter of days. | 0:19:41 | 0:19:46 | |
For life to get a foothold, you need more than that. | 0:19:51 | 0:19:54 | |
You need areas of standing water. | 0:19:54 | 0:19:59 | |
Lakes and rivers that persist for millions of years. | 0:19:59 | 0:20:05 | |
In order to look for evidence of that standing water, we've done the only thing we can, | 0:20:05 | 0:20:11 | |
we have sent an army of robotic explorers to the surface of the planet. | 0:20:11 | 0:20:16 | |
We have touch down, we have touch down. | 0:20:17 | 0:20:19 | |
Over the last 35 years, | 0:20:25 | 0:20:27 | |
we've landed six robot probes on Mars. | 0:20:27 | 0:20:32 | |
And one of them, Opportunity, is still rolling across the surface, investigating the Martian geology. | 0:20:32 | 0:20:39 | |
The Mars rovers has really captured our imaginations. | 0:20:50 | 0:20:54 | |
I suppose, because they genuinely are explorers in the old-fashioned sense. | 0:20:54 | 0:20:59 | |
They are the extension of our senses to the surface of another world. | 0:20:59 | 0:21:04 | |
But they have also been very important scientifically, because | 0:21:04 | 0:21:08 | |
you can't really get to know another planet from orbit. | 0:21:08 | 0:21:11 | |
You have got to get down to the surface, you've got to touch it, | 0:21:11 | 0:21:15 | |
you've got to dig down and examine it microscopically. | 0:21:15 | 0:21:19 | |
And the Rovers really have, by doing that, | 0:21:19 | 0:21:23 | |
made some extremely important scientific discoveries. | 0:21:23 | 0:21:27 | |
One of the most significant of those discoveries was made in November 2004. | 0:21:35 | 0:21:42 | |
The Opportunity rover was examining an impact feature called the Endurance crater, | 0:21:42 | 0:21:48 | |
when it detected deposits of a remarkable mineral. | 0:21:48 | 0:21:52 | |
This is the world's largest salt works on the Baha peninsula in Mexico. | 0:22:08 | 0:22:13 | |
And what they do here is pump sea water into these lagoons and let it evaporate. | 0:22:13 | 0:22:20 | |
What they're after is this stuff, which is sodium chloride, table salt. | 0:22:20 | 0:22:25 | |
But, at different stages, different salts, different minerals, crystallise out. | 0:22:25 | 0:22:29 | |
So all the things really that are in sea water emerge, crystallise out | 0:22:29 | 0:22:34 | |
at different stages of the process. | 0:22:34 | 0:22:37 | |
In one of the lagoons, pond number nine, the sea water is at exactly the right concentration | 0:22:46 | 0:22:53 | |
to precipitate out these beautiful crystals that cover the entire floor of the lagoon. | 0:22:53 | 0:22:59 | |
This is gypsum, | 0:23:08 | 0:23:11 | |
and it's exactly the same stuff that Opportunity found on the surface of Mars. | 0:23:11 | 0:23:17 | |
Now, what's interesting about that discovery is how you make gypsum. | 0:23:17 | 0:23:22 | |
You see, its chemical formula is CaSO4. | 0:23:22 | 0:23:26 | |
So it's calcium sulphate. | 0:23:29 | 0:23:33 | |
Dihydrate, 2H2O. | 0:23:33 | 0:23:37 | |
That's water. | 0:23:37 | 0:23:39 | |
So, the only way we know of, the only way to make gypsum here on Earth, is to have calcium | 0:23:39 | 0:23:47 | |
and sulphate ions in the presence of liquid water. | 0:23:47 | 0:23:51 | |
So, large deposits of gypsum on the surface of Mars tells you | 0:23:51 | 0:23:56 | |
that there must have been big areas of water present for a very long time. | 0:23:56 | 0:24:02 | |
The discovery of gypsum has helped to build a picture | 0:24:05 | 0:24:08 | |
of an ancient Mars that was much warmer and wetter. | 0:24:08 | 0:24:12 | |
Subsequent discoveries of gypsum in networks of sand dunes | 0:24:14 | 0:24:19 | |
suggest that large areas of Mars were once covered in standing water. | 0:24:19 | 0:24:24 | |
And where there is standing water, there is the chance of life. | 0:24:29 | 0:24:33 | |
This area of the salt flats is, we think, | 0:24:37 | 0:24:40 | |
very similar to areas that have been seen on Mars. | 0:24:40 | 0:24:44 | |
And it certainly looks extremely inhospitable. | 0:24:44 | 0:24:48 | |
It's hard at first sight to see how anything could live here. | 0:24:48 | 0:24:51 | |
But, if you just dig | 0:24:51 | 0:24:54 | |
a tiny bit below the surface, | 0:24:54 | 0:24:56 | |
then you see that this layer of gypsum is only a few millimetres thick, | 0:24:56 | 0:25:02 | |
and then immediately the ground beneath it turns this greeny colour. | 0:25:02 | 0:25:07 | |
It's green because that is bacteria that thrive in these seemingly inhospitable conditions. | 0:25:07 | 0:25:14 | |
Now if these bacteria can survive here, | 0:25:14 | 0:25:17 | |
then there seems to be no good reason why they couldn't also have survived and even flourished on Mars | 0:25:17 | 0:25:24 | |
when there was water present at some point in the very distant past. | 0:25:24 | 0:25:28 | |
But although it may once have been more hospitable, | 0:25:33 | 0:25:36 | |
any liquid water has long since disappeared from the surface of Mars. | 0:25:36 | 0:25:41 | |
About three billion years ago, it died as a planet. | 0:25:44 | 0:25:50 | |
Its core froze and the volcanoes that had produced its atmosphere seized up. | 0:25:50 | 0:25:56 | |
The solar wind stripped away the remains of that atmosphere. | 0:25:59 | 0:26:03 | |
Any liquid water would have evaporated | 0:26:03 | 0:26:06 | |
or soaked into the soil where it froze. | 0:26:06 | 0:26:10 | |
It left the surface of Mars too cold, too exposed | 0:26:11 | 0:26:15 | |
and too dry to support life. | 0:26:15 | 0:26:18 | |
It's highly unlikely that there will be life on the surface of Mars today. | 0:26:24 | 0:26:29 | |
But that's not to say that life couldn't exist somewhere on the Red Planet, | 0:26:29 | 0:26:33 | |
maybe we're just looking in the wrong place. | 0:26:33 | 0:26:36 | |
There are other potential habitats for life on Mars. | 0:26:39 | 0:26:42 | |
Detailed pictures of the surface show the entrances to caves, | 0:26:44 | 0:26:49 | |
revealing the existence of a world beneath the Martian surface. | 0:26:49 | 0:26:53 | |
We know there may be water down there. | 0:26:57 | 0:26:59 | |
Satellite data shows permafrost, ice frozen in the soil. | 0:26:59 | 0:27:06 | |
Deep below the surface, that ice may melt to form liquid water. | 0:27:06 | 0:27:11 | |
It all hints at an undiscovered subterranean world | 0:27:16 | 0:27:21 | |
that may be a more likely place to find life. | 0:27:21 | 0:27:25 | |
If you were to imagine the perfect habitat for life, | 0:27:46 | 0:27:50 | |
then it would surely be somewhere like this. | 0:27:50 | 0:27:53 | |
A warm climate, lots of liquid water, | 0:27:53 | 0:27:55 | |
a beautiful, dense atmosphere. | 0:27:55 | 0:28:00 | |
You see the results everywhere, just life everywhere you look. | 0:28:00 | 0:28:04 | |
All the life we're familiar with thrives in pretty much the same | 0:28:07 | 0:28:11 | |
conditions that we do, driven by the heat and light of the sun. | 0:28:11 | 0:28:17 | |
But this is by no means the only life on Earth. | 0:28:17 | 0:28:20 | |
There's another living planet hidden beneath the surface | 0:28:24 | 0:28:29 | |
that exists in completely different conditions. | 0:28:29 | 0:28:32 | |
It raises fascinating possibilities for the caves on Mars. | 0:28:32 | 0:28:38 | |
This is the Cueva de Villa Luz in Tabasco, Mexico, | 0:28:46 | 0:28:49 | |
the Cave of the House of Light. | 0:28:49 | 0:28:51 | |
And it is the definition of a hostile environment to me. | 0:28:51 | 0:28:56 | |
Because (HE SNIFFS) it's full of hydrogen sulphide gas, hence | 0:28:56 | 0:29:01 | |
the gas monitor which says at the moment one part per million hydrogen sulphide, very toxic for me, | 0:29:01 | 0:29:07 | |
which is why I have got this gas mask in case it all gets too much. | 0:29:07 | 0:29:12 | |
So, it's a place where you, at first sight, | 0:29:12 | 0:29:16 | |
would not expect a great many life forms to survive and flourish. | 0:29:16 | 0:29:21 | |
Although the cave is a death-trap for us, that doesn't mean that nothing lives here. | 0:29:49 | 0:29:55 | |
In fact, it's teeming with life. | 0:29:55 | 0:29:57 | |
Look at these fish, just everywhere in the cave water. And they're | 0:30:00 | 0:30:05 | |
adapted to live in these conditions. | 0:30:05 | 0:30:08 | |
In fact, if you look at them closely, | 0:30:08 | 0:30:10 | |
they're quite pink. | 0:30:10 | 0:30:12 | |
That's thought to be because they've got lots of haemoglobin | 0:30:12 | 0:30:16 | |
because there's not much oxygen down here, | 0:30:16 | 0:30:18 | |
so they need to have an efficient way of moving oxygen around their bodies. | 0:30:18 | 0:30:23 | |
Beautiful. | 0:30:23 | 0:30:25 | |
But the really interesting life is found in the depths of the caves, | 0:30:31 | 0:30:35 | |
where the concentration of poisonous gas is high enough to set off my alarm. | 0:30:35 | 0:30:41 | |
Down here, far from the light of the sun, | 0:30:42 | 0:30:45 | |
are organisms whose energy source comes from the air around them. | 0:30:45 | 0:30:50 | |
They use the hydrogen sulphide gas bubbling up through these springs. | 0:30:52 | 0:30:58 | |
The same gas that could be fatally poisonous to me | 0:30:58 | 0:31:02 | |
is their source of life. | 0:31:02 | 0:31:04 | |
These things are what I came deep underground to see. | 0:31:15 | 0:31:18 | |
These are snottites. And you can see why they're called that. | 0:31:18 | 0:31:24 | |
They're really one of the most alien life forms that I can conceive of | 0:31:24 | 0:31:29 | |
on the Earth | 0:31:29 | 0:31:31 | |
Because they metabolise hydrogen sulphide, so they metabolise this | 0:31:31 | 0:31:36 | |
faintly acidic and nasty gas that I'm just breathing in now. | 0:31:36 | 0:31:40 | |
You can almost feel it on your tongue, actually, the acidity of it. | 0:31:40 | 0:31:45 | |
They metabolise it, they react it with oxygen, and they produce sulphuric acid. | 0:31:45 | 0:31:50 | |
So their breathing process, if you like, their version of what I do, | 0:31:50 | 0:31:55 | |
I breathe in oxygen, react that with sugars and breathe out CO2 and get energy | 0:31:55 | 0:31:59 | |
these guys breathe in hydrogen sulphide and oxygen and produce sulphuric acid. | 0:31:59 | 0:32:05 | |
In fact, I can test it here with this. | 0:32:05 | 0:32:07 | |
Yes, you see, look at that. | 0:32:16 | 0:32:18 | |
That, well, what looks like water, that secretion of dripping off the snottites, has actually got a pH... | 0:32:18 | 0:32:24 | |
well, it's now about between 0.5 and 0. | 0:32:24 | 0:32:29 | |
That's strong acid. | 0:32:29 | 0:32:30 | |
That's as strong as battery acid. | 0:32:30 | 0:32:33 | |
It's actually highly concentrated sulphuric acid. | 0:32:33 | 0:32:37 | |
So, what a strange organism. | 0:32:37 | 0:32:41 | |
Alien in every sense of the word. | 0:32:41 | 0:32:43 | |
Except that it's present on, well, just below the surface, of our planet. | 0:32:43 | 0:32:48 | |
And the snottites are not alone. | 0:32:52 | 0:32:55 | |
Organisms that can extract energy from the minerals around them | 0:32:55 | 0:32:59 | |
are found under the ground all over the world. | 0:32:59 | 0:33:01 | |
In fact, this way of life is so successful that it's thought there | 0:33:03 | 0:33:08 | |
may be more life living beneath the Earth's surface than there is on it. | 0:33:08 | 0:33:13 | |
And that raises an intriguing possibility. | 0:33:15 | 0:33:18 | |
If life can thrive below the Earth's surface, | 0:33:18 | 0:33:22 | |
why couldn't organisms like snottites survive and flourish | 0:33:22 | 0:33:27 | |
beneath the surface of Mars? | 0:33:27 | 0:33:29 | |
If you think about it, living below the surface of Mars might actually | 0:33:33 | 0:33:37 | |
be quite a good idea, because the surface is incredibly hostile. | 0:33:37 | 0:33:41 | |
It's subjected to intense ultraviolet radiation from the sun. | 0:33:41 | 0:33:45 | |
It's a very cold place, and the atmospheric pressure doesn't | 0:33:45 | 0:33:48 | |
allow liquid water to exist on the surface. | 0:33:48 | 0:33:52 | |
But, if there is life below the surface of Mars, then obviously we have a problem. | 0:33:52 | 0:33:57 | |
How could you possibly detect it? | 0:33:57 | 0:33:59 | |
Well, actually, there is a perhaps tantalising clue that | 0:33:59 | 0:34:03 | |
there might be something interesting going on below the Martian surface. | 0:34:03 | 0:34:10 | |
These are termites, or white ants. | 0:34:21 | 0:34:25 | |
And they're very unusual animals because they eat wood. | 0:34:25 | 0:34:31 | |
This is their food. | 0:34:31 | 0:34:33 | |
There are many, many species of these, billions of individuals across the planet. | 0:34:33 | 0:34:40 | |
And, in the process of digesting wood, they produce the gas methane. | 0:34:40 | 0:34:45 | |
Because there are so many of them, they actually produce an estimated | 0:34:45 | 0:34:49 | |
50 million tonnes of methane | 0:34:49 | 0:34:51 | |
and pump it into the Earth's atmosphere every year. | 0:34:51 | 0:34:56 | |
And it's not just termites. | 0:34:56 | 0:34:59 | |
There's lots of methane naturally in our atmosphere. | 0:34:59 | 0:35:03 | |
It's all produced either biologically... | 0:35:03 | 0:35:06 | |
or by active geological processes like mud volcanoes. | 0:35:08 | 0:35:13 | |
And that makes it all the more surprising that methane | 0:35:19 | 0:35:22 | |
has been detected in the atmosphere of the supposedly dead planet Mars. | 0:35:22 | 0:35:28 | |
It was telescopes on Earth, using infrared spectroscopy, | 0:35:32 | 0:35:37 | |
that first identified methane in Mars's tenuous atmosphere. | 0:35:37 | 0:35:41 | |
Those first measurements appeared to show only tiny amounts. | 0:35:46 | 0:35:51 | |
But closer observations have revealed that the gas | 0:35:51 | 0:35:55 | |
is concentrated in a handful of plumes that vary with the seasons. | 0:35:55 | 0:36:01 | |
In the warmer summer months, | 0:36:02 | 0:36:04 | |
thousands of tonnes of the gas is released from vents in the surface. | 0:36:04 | 0:36:10 | |
Something under the surface of Mars must be producing it. | 0:36:10 | 0:36:15 | |
It may be coming from previously unknown geological processes. | 0:36:15 | 0:36:20 | |
But it could be that it's coming from a biological source. | 0:36:23 | 0:36:27 | |
Now no-one, I don't think, is seriously suggesting that there | 0:36:28 | 0:36:32 | |
are termites running around beneath the surface of Mars. | 0:36:32 | 0:36:36 | |
But it's not actually the termites that are particularly interesting about this story. | 0:36:36 | 0:36:41 | |
It's the way they digest the wood. | 0:36:41 | 0:36:44 | |
You see, they use symbiotic bacteria, bacteria that live in their guts, called Archaea. | 0:36:44 | 0:36:50 | |
And Archaea, these bacteria that can digest wood and produce methane, | 0:36:50 | 0:36:56 | |
are the most common organisms beneath the surface of the Earth. | 0:36:56 | 0:37:01 | |
The snottites are members of the Archaea, | 0:37:03 | 0:37:08 | |
as are many of the microorganisms found living around deep-sea hydrothermal vents. | 0:37:08 | 0:37:16 | |
In fact, it's Archaea that we find thriving in many of the Earth's most extreme environments. | 0:37:16 | 0:37:23 | |
So I think it's quite a fascinating prospect that the methane we see | 0:37:26 | 0:37:32 | |
in Mars's atmosphere might just be produced by organisms like Archaea, | 0:37:32 | 0:37:39 | |
living below the Martian surface. | 0:37:39 | 0:37:42 | |
But while Mars remains a tantalising possibility, | 0:37:44 | 0:37:48 | |
it's no longer the only place in the solar system | 0:37:48 | 0:37:52 | |
we think could harbour alien life. | 0:37:52 | 0:37:54 | |
Far out, a billion kilometres from the sun, | 0:38:00 | 0:38:04 | |
the solar system becomes a very different place. | 0:38:04 | 0:38:08 | |
The planets, like Saturn, are made of gas, not rock. | 0:38:10 | 0:38:14 | |
There's plenty of water out here, but it's frozen solid. | 0:38:18 | 0:38:21 | |
The planets are surrounded by networks of moons, carved from ice. | 0:38:24 | 0:38:30 | |
They're cold and desolate. | 0:38:30 | 0:38:33 | |
They don't seem likely places to find life. | 0:38:35 | 0:38:40 | |
Any places on Earth remotely similar are completely barren. | 0:38:40 | 0:38:45 | |
This is central Iceland. | 0:39:04 | 0:39:06 | |
And, at this time of year, in mid-November, it's an increasingly inhospitable place. | 0:39:06 | 0:39:12 | |
It's about 3 o'clock in the afternoon, it's already well below freezing. | 0:39:12 | 0:39:16 | |
The sun is dipping below the horizon. | 0:39:16 | 0:39:19 | |
And it will stay this way for another six months. | 0:39:19 | 0:39:22 | |
And there's pretty much no visible life here at all. | 0:39:22 | 0:39:29 | |
There are no trees, no grass, and just listen. | 0:39:29 | 0:39:34 | |
SILENCE | 0:39:34 | 0:39:36 | |
No insects, no birds. | 0:39:38 | 0:39:41 | |
Nothing. | 0:39:41 | 0:39:43 | |
But it's because these places are so cold and inhospitable | 0:39:47 | 0:39:51 | |
that they're of increasing interest to astro-biologists. | 0:39:51 | 0:39:55 | |
Because discoveries in these frozen places of Earth have raised new hope | 0:39:57 | 0:40:01 | |
of finding life among the icy worlds of the outer solar system. | 0:40:01 | 0:40:07 | |
And in those frozen wastes | 0:40:09 | 0:40:11 | |
we have found one world that is of particular interest. | 0:40:11 | 0:40:15 | |
It's one of Jupiter's moons. | 0:40:16 | 0:40:18 | |
Jupiter has a vast network of moons. | 0:40:25 | 0:40:29 | |
The four largest have been known | 0:40:29 | 0:40:32 | |
since they were discovered by Galileo in 1610. | 0:40:32 | 0:40:36 | |
And they're a varied bunch. | 0:40:36 | 0:40:38 | |
Closest to the planet is the tortured moon Io. | 0:40:41 | 0:40:45 | |
It's torn apart by volcanoes that carpet its surface with bright yellow sulphur. | 0:40:45 | 0:40:52 | |
In total contrast to the heat of Io comes its neighbour, | 0:40:58 | 0:41:03 | |
the ice moon Europa. | 0:41:03 | 0:41:06 | |
It's about the same size as our moon. | 0:41:09 | 0:41:13 | |
And it's the smoothest body in the solar system. | 0:41:13 | 0:41:16 | |
Its surface is made of an unbroken shell of ice. | 0:41:19 | 0:41:25 | |
Though it's etched with a network of mysterious red markings. | 0:41:25 | 0:41:30 | |
It exists at a chilly minus 160 Celsius. | 0:41:34 | 0:41:39 | |
It seems an incredibly unlikely home for life. | 0:41:39 | 0:41:43 | |
The photographs of Europa from space | 0:41:50 | 0:41:54 | |
reveal a vast, icy wilderness. | 0:41:54 | 0:41:59 | |
But, if you look more closely, then you start to see surface features. | 0:42:00 | 0:42:06 | |
And those features tell you a lot about what's going on deep beneath the ice. | 0:42:06 | 0:42:13 | |
Close-up, we can see deep cracks that criss-cross the surface of Europa. | 0:42:21 | 0:42:26 | |
At higher magnification | 0:42:30 | 0:42:32 | |
we see areas where the ice has been broken into icebergs | 0:42:32 | 0:42:36 | |
and jumbled up before refreezing. | 0:42:36 | 0:42:39 | |
We see the same formations in sea ice on Earth, | 0:42:42 | 0:42:46 | |
where the movements of the ocean have caused the ice to bend and crack. | 0:42:46 | 0:42:51 | |
It suggests something similar may be happening on Europa. | 0:42:53 | 0:42:57 | |
But it's the way the cracks are broken and fractured that provide | 0:42:59 | 0:43:03 | |
the compelling evidence that there is liquid water on Europa. | 0:43:03 | 0:43:08 | |
You see, as Europa orbits around Jupiter, | 0:43:12 | 0:43:15 | |
Jupiter's intense gravity stretches and squashes the moon. | 0:43:15 | 0:43:20 | |
And that stresses the ice and causes it to fracture and crack. | 0:43:20 | 0:43:25 | |
But the position of those cracks is not quite where you would expect it to be. | 0:43:25 | 0:43:30 | |
And the explanation for that is that the icy surface of Europa | 0:43:30 | 0:43:35 | |
has shifted, it's moved relative to the rocky core. | 0:43:35 | 0:43:39 | |
And the only way that could happen is if there's a layer, or an ocean of liquid water, | 0:43:39 | 0:43:46 | |
surrounding the rocky core that allows the outer ice surface to slip around. | 0:43:46 | 0:43:52 | |
Measurements of Europa's magnetic field have confirmed that its icy shell | 0:43:56 | 0:44:01 | |
is sitting on top of a salty ocean that may be a staggering 100km deep. | 0:44:01 | 0:44:09 | |
That would mean that there is more than twice as much life-giving | 0:44:24 | 0:44:28 | |
liquid water on this tiny moon than there is on planet Earth. | 0:44:28 | 0:44:34 | |
But it's not just the discovery of the hidden ocean | 0:44:38 | 0:44:41 | |
that makes us believe that Europa may be the most likely home to alien life. | 0:44:41 | 0:44:47 | |
And that's why I've come to this spectacular ice cave in the Vatnajokull glacier. | 0:44:48 | 0:44:55 | |
You see, the laws of nature are universal. | 0:44:55 | 0:44:58 | |
That may not only apply to laws of physics, but also to the laws of biology as well. | 0:44:58 | 0:45:03 | |
And if that's the case, | 0:45:03 | 0:45:05 | |
then what we find in these ice caves of Iceland may tell us something | 0:45:05 | 0:45:11 | |
about what we could expect to find below the frozen surface of Europa. | 0:45:11 | 0:45:16 | |
It's hard to describe this place. | 0:45:42 | 0:45:45 | |
It's absolutely magnificent. | 0:45:47 | 0:45:50 | |
Visually, the quality of the ice, it's just completely | 0:45:50 | 0:45:55 | |
transparent and clear. | 0:45:55 | 0:45:58 | |
You can see straight through it. | 0:45:58 | 0:46:01 | |
The cave tunnels into the heart of the glacier, | 0:46:03 | 0:46:07 | |
where the ice has been frozen for a thousand years. | 0:46:07 | 0:46:12 | |
It's what astro-biologists find in this ice | 0:46:12 | 0:46:16 | |
that makes us think that Europa could be teeming with life. | 0:46:16 | 0:46:22 | |
NASA scientist Richard Hoover | 0:46:30 | 0:46:33 | |
has spent his career looking for life in unlikely places. | 0:46:33 | 0:46:37 | |
Well, that went very well. | 0:46:40 | 0:46:42 | |
-OK. -So, will any organisms that you find in that ice be living in a sense that I would understand it? | 0:46:44 | 0:46:50 | |
They're actually alive now, and metabolising? | 0:46:50 | 0:46:53 | |
For a long time it was thought that ice microorganisms | 0:46:53 | 0:46:59 | |
were present only in a state of what is called deep anabiosis. | 0:46:59 | 0:47:03 | |
Suspended animation. It's now becoming quite clear that that isn't necessarily | 0:47:03 | 0:47:08 | |
the case for all the microorganisms, there may be others that are actually actively living in the ice. | 0:47:08 | 0:47:15 | |
So in this glacier, the whole place, this whole cave | 0:47:15 | 0:47:19 | |
may be populated by living things, not frozen things? | 0:47:19 | 0:47:24 | |
Things existing, living, cell dividing, reproducing, all the things you do? | 0:47:24 | 0:47:29 | |
All of this. | 0:47:29 | 0:47:30 | |
It's this prospect of finding things living in solid ice | 0:47:36 | 0:47:40 | |
that has had the greatest impact | 0:47:40 | 0:47:42 | |
on our ideas of where life could survive in the solar system. | 0:47:42 | 0:47:47 | |
OK, we're at lowest magnification. | 0:47:49 | 0:47:51 | |
So, that is 100,000 millionths of a metre? | 0:47:51 | 0:47:53 | |
Yes. We have bacteria. | 0:47:53 | 0:47:57 | |
So, these are organisms that have been trapped in that glacier for thousands of years? | 0:47:59 | 0:48:04 | |
Yes, look at this. | 0:48:04 | 0:48:06 | |
Beautiful. You're seeing life in ice. | 0:48:06 | 0:48:09 | |
We now know that some microorganisms | 0:48:09 | 0:48:13 | |
are capable of actually causing the ice to melt, | 0:48:13 | 0:48:18 | |
because they generate, essentially, anti-freeze proteins. | 0:48:18 | 0:48:23 | |
They change the temperature at which ice goes from a solid state to a liquid state. | 0:48:23 | 0:48:29 | |
And they could have been forming little tiny pockets, | 0:48:29 | 0:48:32 | |
maybe only a few microns in diameter, | 0:48:32 | 0:48:34 | |
but if he can make a two or three micron diameter ball of liquid water, | 0:48:34 | 0:48:39 | |
and he has the ability to move, | 0:48:39 | 0:48:41 | |
then that bacterium is now not in a glacier, but he's in an ocean. | 0:48:41 | 0:48:47 | |
What are the implications of these discoveries? | 0:48:47 | 0:48:51 | |
The fact that you've got living bacteria inside ice on Earth, what are the implications for Europa? | 0:48:51 | 0:48:58 | |
You can clearly have bacteria like this in the frozen ice near the surface crust. | 0:48:58 | 0:49:04 | |
And the thing that is most exciting to me, | 0:49:04 | 0:49:07 | |
is that surface crust of Europa has a wide variety of colours | 0:49:07 | 0:49:12 | |
that are highly suggestive of microbial life. | 0:49:12 | 0:49:16 | |
And so there is a very, very strong possibility | 0:49:16 | 0:49:21 | |
that the ice of Europa may contain viable, living microorganisms. | 0:49:21 | 0:49:26 | |
It's a controversial idea, but it is a dizzying thought | 0:49:30 | 0:49:35 | |
that the mysterious red stains on the surface of Europa | 0:49:35 | 0:49:39 | |
could be the visible signs of alien life. | 0:49:39 | 0:49:44 | |
The discovery of the huge ocean of liquid water | 0:49:49 | 0:49:53 | |
under the surface of this tiny moon, combined with the potential for life in ice, | 0:49:53 | 0:49:59 | |
and the intriguing red markings that criss-cross its surface, | 0:49:59 | 0:50:04 | |
have made Europa the most fascinating and important alien world we know. | 0:50:04 | 0:50:10 | |
A true wonder of the solar system, | 0:50:20 | 0:50:23 | |
because it's our best hope of finding extraterrestrial life. | 0:50:23 | 0:50:29 | |
That question, are we alone in the universe? | 0:50:47 | 0:50:50 | |
Is this the only planet amongst the billions of planets in our galaxy, | 0:50:50 | 0:50:57 | |
amongst the billions of galaxies in the universe, that harbours life? | 0:50:57 | 0:51:02 | |
Is, I think, one of the most important questions, | 0:51:02 | 0:51:07 | |
perhaps THE most important question that we can ask. | 0:51:07 | 0:51:10 | |
Think about what it would mean for us | 0:51:10 | 0:51:13 | |
if the answer was that there was no other life in the solar system, | 0:51:13 | 0:51:18 | |
in our galaxy, perhaps even in the universe. | 0:51:18 | 0:51:21 | |
How valuable would that make planet Earth? | 0:51:21 | 0:51:25 | |
How valuable would that make us? | 0:51:25 | 0:51:27 | |
But then imagine that the answer is that, on every moon of every planet | 0:51:27 | 0:51:33 | |
where the conditions are right, then life survives and flourishes. | 0:51:33 | 0:51:38 | |
That makes us part of a wider cosmic community, | 0:51:38 | 0:51:43 | |
if the universe is teeming with life. | 0:51:43 | 0:51:47 | |
If knowing the answer to the question is so profoundly important, | 0:51:48 | 0:51:53 | |
then surely striving to find the answer should be of overwhelming importance. | 0:51:53 | 0:51:59 | |
I believe it's the most important question you can possibly ask. | 0:51:59 | 0:52:03 | |
Because we have a chance of answering it. | 0:52:03 | 0:52:06 | |
What we've learned from the extreme places on Earth | 0:52:21 | 0:52:24 | |
is that, if there is life out there in the solar system, it will almost certainly be simple. | 0:52:24 | 0:52:30 | |
Single-celled organisms like bacteria eking out an existence in the most hostile of environments. | 0:52:30 | 0:52:38 | |
One thing seems certain. | 0:52:50 | 0:52:52 | |
The only place in the solar system where there is complex life, | 0:52:52 | 0:52:57 | |
life that can build a civilisation, | 0:52:57 | 0:53:00 | |
is here on planet Earth. | 0:53:00 | 0:53:03 | |
But how did that happen? What is it that makes our world so special? | 0:53:04 | 0:53:11 | |
Because, after all, everything in the solar system shares the same genesis. | 0:53:11 | 0:53:18 | |
It was all created out of nothing more than a spinning cloud of gas and dust 4.5 billion years ago. | 0:53:20 | 0:53:29 | |
Solid worlds condensed out of the swirling mists. | 0:53:38 | 0:53:42 | |
But those worlds were radically different. | 0:53:42 | 0:53:46 | |
Around the solar system, there are worlds that erupt with volcanoes of sulphur. | 0:53:50 | 0:53:56 | |
And others with geysers of ice. | 0:53:58 | 0:54:00 | |
There are worlds with rich atmospheres and swirling storms. | 0:54:03 | 0:54:08 | |
And there are moons carved from ice | 0:54:11 | 0:54:14 | |
that hide huge oceans of liquid water. | 0:54:14 | 0:54:17 | |
But there's only one world where the laws of physics have conspired | 0:54:22 | 0:54:27 | |
to combine all these features in one place. | 0:54:27 | 0:54:30 | |
On Earth, the temperature and atmospheric pressure are just right | 0:54:33 | 0:54:38 | |
to allow oceans of liquid water to exist on the surface of the planet. | 0:54:38 | 0:54:43 | |
And it's big enough to have retained its molten core | 0:54:46 | 0:54:51 | |
that not only powers geysers and volcanoes, | 0:54:51 | 0:54:54 | |
but also produces our magnetic field | 0:54:54 | 0:54:58 | |
that fends off the solar wind and protects our thick, nurturing atmosphere. | 0:54:58 | 0:55:03 | |
It's the combination of all those wonders in one place | 0:55:12 | 0:55:16 | |
that allowed life to begin and to get a foothold here on Earth. | 0:55:16 | 0:55:21 | |
But, to allow that life to evolve into such complex creatures as ourselves | 0:55:21 | 0:55:27 | |
requires one more ingredient. | 0:55:27 | 0:55:30 | |
And that's time. Deep time. | 0:55:30 | 0:55:33 | |
The kind of time over which mountains rise and fall, and planets are formed and stars live and die. | 0:55:33 | 0:55:41 | |
And it's perhaps that that makes the earth so rare and so precious in the cosmos. | 0:55:41 | 0:55:48 | |
Because it's been stable enough for long enough for life to evolve | 0:55:48 | 0:55:53 | |
into such magnificent complexity. | 0:55:53 | 0:55:56 | |
The life we have on Earth today is the result of millions of years of stability. | 0:56:05 | 0:56:11 | |
And the pinnacle of that is us, humankind. | 0:56:13 | 0:56:17 | |
A species that has developed to the point where we can bend | 0:56:19 | 0:56:23 | |
and shape and change the world around us. | 0:56:23 | 0:56:28 | |
We have even left our own planet behind | 0:56:30 | 0:56:34 | |
to begin exploring our cosmic surroundings. | 0:56:34 | 0:56:38 | |
You could take the view that our exploration of the universe | 0:56:49 | 0:56:54 | |
has made us somehow insignificant. | 0:56:54 | 0:56:57 | |
One tiny planet around one star amongst hundreds of billions. | 0:56:57 | 0:57:04 | |
But I don't take that view. | 0:57:04 | 0:57:06 | |
Because we've discovered that it takes the rarest combination of chance, and the laws of nature, | 0:57:06 | 0:57:13 | |
to produce a planet that can support a civilisation. | 0:57:13 | 0:57:18 | |
That most magnificent structure | 0:57:18 | 0:57:21 | |
that allows us to explore and understand the universe. | 0:57:21 | 0:57:26 | |
And that's why, for me, our civilisation is THE wonder of the solar system. | 0:57:26 | 0:57:33 | |
MUSIC: "Calling Occupants Of Interplanetary Craft" by the Carpenters | 0:57:34 | 0:57:38 | |
# Calling occupants of interplanetary craft | 0:57:39 | 0:57:43 | |
# Calling occupants... | 0:57:46 | 0:57:48 | |
And if you were to be looking at the Earth from outside the solar system, | 0:57:48 | 0:57:54 | |
that much would be obvious. | 0:57:54 | 0:57:56 | |
# Calling occupants of interplanetary craft... | 0:57:57 | 0:58:01 | |
We have written the evidence of our existence onto the surface of our planet. | 0:58:04 | 0:58:11 | |
Our civilisation has become a beacon that identifies our planet as home to life. | 0:58:11 | 0:58:18 | |
# We'd like to make a contact with you | 0:58:18 | 0:58:23 | |
# Calling occupants of interplanetary, anti-adversary craft | 0:58:29 | 0:58:36 | |
# We are your friends | 0:58:41 | 0:58:45 | |
# We are your friends...# | 0:58:49 | 0:58:52 | |
If you'd like to know more about the solar system, | 0:58:57 | 0:59:01 | |
go to bbc.co.uk/science. | 0:59:01 | 0:59:06 | |
Subtitles by Red Bee Media Ltd | 0:59:06 | 0:59:09 |