Earth's mass extinctions | Peter Ward

So, I want to start out with

this beautiful picture from my childhood.

I love the science fiction movies.

Here it is: "This Island Earth."

And leave it to Hollywood to get it just right.

Two-and-a-half years in the making.

(Laughter)

I mean, even the creationists give us 6,000,

but Hollywood goes to the chase.

And in this movie, we see what we think is out there:

flying saucers and aliens.

Every world has an alien, and every alien world has a flying saucer,

and they move about with great speed. Aliens.

Well, Don Brownlee, my friend, and I finally got to the point

where we got tired of turning on the TV

and seeing the spaceships and seeing the aliens every night,

and tried to write a counter-argument to it,

and put out what does it really take for an Earth to be habitable,

for a planet to be an Earth, to have a place

where you could probably get not just life, but complexity,

which requires a huge amount of evolution,

and therefore constancy of conditions.

So, in 2000 we wrote "Rare Earth." In 2003, we then asked,

let's not think about where Earths are in space, but how long has Earth been Earth?

If you go back two billion years,

you're not on an Earth-like planet any more.

What we call an Earth-like planet is actually a very short interval of time.

Well, "Rare Earth" actually

taught me an awful lot about meeting the public.

Right after, I got an invitation to go to a science fiction convention,

and with all great earnestness walked in.

David Brin was going to debate me on this,

and as I walked in, the crowd of a hundred started booing lustily.

I had a girl who came up who said, "My dad says you're the devil."

You cannot take people's aliens away from them

and expect to be anybody's friends.

Well, the second part of that, soon after --

and I was talking to Paul Allen; I saw him in the audience,

and I handed him a copy of "Rare Earth."

And Jill Tarter was there, and she turned to me,

and she looked at me just like that girl in "The Exorcist."

It was, "It burns! It burns!"

Because SETI doesn't want to hear this.

SETI wants there to be stuff out there.

I really applaud the SETI efforts, but we have not heard anything yet.

And I really do think we have to start thinking

about what's a good planet and what isn't.

Now, I throw this slide up because it indicates to me that,

even if SETI does hear something, can we figure out what they said?

Because this was a slide that was passed

between the two major intelligences on Earth -- a Mac to a PC --

and it can't even get the letters right --

(Laughter)

-- so how are we going to talk to the aliens?

And if they're 50 light years away, and we call them up,

and you blah, blah, blah, blah, blah,

and then 50 years later it comes back and they say, Please repeat?

I mean, there we are.

Our planet is a good planet because it can keep water.

Mars is a bad planet, but it's still good enough for us to go there

and to live on its surface if we're protected.

But Venus is a very bad -- the worst -- planet.

Even though it's Earth-like, and even though early in its history

it may very well have harbored Earth-like life,

it soon succumbed to runaway greenhouse --

that's an 800 degrees [Fahrenheit] surface --

because of rampant carbon dioxide.

Well, we know from astrobiology that we can really now predict

what's going to happen to our particular planet.

We are right now in the beautiful Oreo

of existence -- of at least life on Planet Earth --

following the first horrible microbial age.

In the Cambrian explosion, life emerged from the swamps,

complexity arose,

and from what we can tell, we're halfway through.

We have as much time for animals to exist on this planet

as they have been here now,

till we hit the second microbial age.

And that will happen, paradoxically --

everything you hear about global warming --

when we hit CO2 down to 10 parts per million,

we are no longer going to have to have plants

that are allowed to have any photosynthesis, and there go animals.

So, after that we probably have seven billion years.

The Sun increases in its intensity, in its brightness,

and finally, at about 12 billion years after it first started,

the Earth is consumed by a large Sun,

and this is what's left.

So, a planet like us is going to have an age and an old age,

and we are in its golden summer age right now.

But there's two fates to everything, isn't there?

Now, a lot of you are going to die of old age,

but some of you, horribly enough, are going to die in an accident.

And that's the fate of a planet, too.

Earth, if we're lucky enough -- if it doesn't get hit by a Hale-Bopp,

or gets blasted by some supernova nearby

in the next seven billion years -- we'll find under your feet.

But what about accidental death?

Well, paleontologists for the last 200 years

have been charting death. It's strange --

extinction as a concept wasn't even thought about

until Baron Cuvier in France found this first mastodon.

He couldn't match it up to any bones on the planet,

and he said, Aha! It's extinct.

And very soon after, the fossil record started yielding

a very good idea of how many plants and animals there have been

since complex life really began to leave

a very interesting fossil record.

In that complex record of fossils,

there were times when lots of stuff

seemed to be dying out very quickly,

and the father/mother geologists

called these "mass extinctions."

All along it was thought to be either an act of God

or perhaps long, slow climate change,

and that really changed in 1980,

in this rocky outcrop near Gubbio,

where Walter Alvarez, trying to figure out

what was the time difference between these white rocks,

which held creatures of the Cretaceous period,

and the pink rocks above, which held Tertiary fossils.

How long did it take to go from one system to the next?

And what they found was something unexpected.

They found in this gap, in between, a very thin clay layer,

and that clay layer -- this very thin red layer here --

is filled with iridium.

And not just iridium; it's filled with glassy spherules,

and it's filled with quartz grains

that have been subjected to enormous pressure: shock quartz.

Now, in this slide the white is chalk,

and this chalk was deposited in a warm ocean.

The chalk itself's composed by plankton

which has fallen down from the sea surface onto the sea floor,

so that 90 percent of the sediment here is skeleton of living stuff,

and then you have that millimeter-thick red layer,

and then you have black rock.

And the black rock is the sediment on the sea bottom

in the absence of plankton.

And that's what happens in an asteroid catastrophe,

because that's what this was, of course. This is the famous K-T.

A 10-kilometer body hit the planet.

The effects of it spread this very thin impact layer all over the planet,

and we had very quickly the death of the dinosaurs,

the death of these beautiful ammonites,

Leconteiceras here, and Celaeceras over here,

and so much else.

I mean, it must be true,

because we've had two Hollywood blockbusters since that time,

and this paradigm, from 1980 to about 2000,

totally changed how we geologists thought about catastrophes.

Prior to that, uniformitarianism was the dominant paradigm:

the fact that if anything happens on the planet in the past,

there are present-day processes that will explain it.

But we haven't witnessed a big asteroid impact,

so this is a type of neo-catastrophism,

and it took about 20 years for the scientific establishment

to finally come to grips: yes, we were hit;

and yes, the effects of that hit caused a major mass extinction.

Well, there are five major mass extinctions

over the last 500 million years, called the Big Five.

They range from 450 million years ago

to the last, the K-T, number four,

but the biggest of all was the P, or the Permian extinction,

sometimes called the mother of all mass extinctions.

And every one of these has been subsequently blamed

on large-body impact.

But is this true?

The most recent, the Permian, was thought to have been an impact

because of this beautiful structure on the right.

This is a Buckminsterfullerene, a carbon-60.

Because it looks like those terrible geodesic domes

of my late beloved '60s,

they're called "buckyballs."

This evidence was used to suggest

that at the end of the Permian, 250 million years ago, a comet hit us.

And when the comet hits, the pressure produces the buckyballs,

and it captures bits of the comet.

Helium-3: very rare on the surface of the Earth, very common in space.

But is this true?

In 1990, working on the K-T extinction for 10 years,

I moved to South Africa to begin work twice a year

in the great Karoo desert.

I was so lucky to watch the change of that South Africa

into the new South Africa as I went year by year.

And I worked on this Permian extinction,

camping by this Boer graveyard for months at a time.

And the fossils are extraordinary.

You know, you're gazing upon your very distant ancestors.

These are mammal-like reptiles.

They are culturally invisible. We do not make movies about these.

This is a Gorgonopsian, or a Gorgon.

That's an 18-inch long skull of an animal

that was probably seven or eight feet, sprawled like a lizard,

probably had a head like a lion.

This is the top carnivore, the T-Rex of its time.

But there's lots of stuff.

This is my poor son, Patrick.

(Laughter)

This is called paleontological child abuse.

Hold still, you're the scale.

(Laughter)

There was big stuff back then.

Fifty-five species of mammal-like reptiles.

The age of mammals had well and truly started

250 million years ago ...

... and then a catastrophe happened.

And what happens next is the age of dinosaurs.

It was all a mistake; it should have never happened. But it did.

Now, luckily,

this Thrinaxodon, the size of a robin egg here:

this is a skull I've discovered just before taking this picture --

there's a pen for scale; it's really tiny --

this is in the Lower Triassic, after the mass extinction has finished.

You can see the eye socket and you can see the little teeth in the front.

If that does not survive, I'm not the thing giving this talk.

Something else is, because if that doesn't survive, we are not here;

there are no mammals. It's that close; one species ekes through.

Well, can we say anything about the pattern of who survives and who doesn't?

Here's sort of the end of that 10 years of work.

The ranges of stuff -- the red line is the mass extinction.

But we've got survivors and things that get through,

and it turns out the things that get through preferentially are cold bloods.

Warm-blooded animals take a huge hit at this time.

The survivors that do get through

produce this world of crocodile-like creatures.

There's no dinosaurs yet; just this slow, saurian, scaly, nasty,

swampy place with a couple of tiny mammals hiding in the fringes.

And there they would hide for 160 million years,

until liberated by that K-T asteroid.

So, if not impact, what?

And the what, I think, is that we returned, over and over again,

to the Pre-Cambrian world, that first microbial age,

and the microbes are still out there.

They hate we animals.

They really want their world back.

And they've tried over and over and over again.

This suggests to me that life causing these mass extinctions

because it did is inherently anti-Gaian.

This whole Gaia idea, that life makes the world better for itself --

anybody been on a freeway on a Friday afternoon in Los Angeles

believing in the Gaia theory? No.

So, I really suspect there's an alternative,

and that life does actually try to do itself in --

not consciously, but just because it does.

And here's the weapon, it seems, that it did so over the last 500 million years.

There are microbes which, through their metabolism,

produce hydrogen sulfide,

and they do so in large amounts.

Hydrogen sulfide is very fatal to we humans.

As small as 200 parts per million will kill you.

You only have to go to the Black Sea and a few other places -- some lakes --

and get down, and you'll find that the water itself turns purple.

It turns purple from the presence of numerous microbes

which have to have sunlight and have to have hydrogen sulfide,

and we can detect their presence today -- we can see them --

but we can also detect their presence in the past.

And the last three years have seen

an enormous breakthrough in a brand-new field.

I am almost extinct --

I'm a paleontologist who collects fossils.

But the new wave of paleontologists -- my graduate students --

collect biomarkers.

They take the sediment itself, they extract the oil from it,

and from that they can produce compounds

which turn out to be very specific to particular microbial groups.

It's because lipids are so tough, they can get preserved in sediment

and last the hundreds of millions of years necessary,

and be extracted and tell us who was there.

And we know who was there. At the end of the Permian,

at many of these mass extinction boundaries,

this is what we find: isorenieratene. It's very specific.

It can only occur if the surface of the ocean has no oxygen,

and is totally saturated with hydrogen sulfide --

enough, for instance, to come out of solution.

This led Lee Kump, and others from Penn State and my group,

to propose what I call the Kump Hypothesis:

many of the mass extinctions were caused by lowering oxygen,

by high CO2. And the worst effect of global warming, it turns out:

hydrogen sulfide being produced out of the oceans.

Well, what's the source of this?

In this particular case, the source over and over has been flood basalts.

This is a view of the Earth now, if we extract a lot of it.

And each of these looks like a hydrogen bomb;

actually, the effects are even worse.

This is when deep-Earth material comes to the surface,

spreads out over the surface of the planet.

Well, it's not the lava that kills anything,

it's the carbon dioxide that comes out with it.

This isn't Volvos; this is volcanoes.

But carbon dioxide is carbon dioxide.

So, these are new data Rob Berner and I -- from Yale -- put together,

and what we try to do now is

track the amount of carbon dioxide in the entire rock record --

and we can do this from a variety of means --

and put all the red lines here,

when these -- what I call greenhouse mass extinctions -- took place.

And there's two things that are really evident here to me,

is that these extinctions take place when CO2 is going up.

But the second thing that's not shown on here:

the Earth has never had any ice on it

when we've had 1,000 parts per million CO2.

We are at 380 and climbing.

We should be up to a thousand in three centuries at the most,

but my friend David Battisti in Seattle says he thinks a 100 years.

So, there goes the ice caps,

and there comes 240 feet of sea level rise.

I live in a view house now;

I'm going to have waterfront.

All right, what's the consequence? The oceans probably turn purple.

And we think this is the reason that complexity took so long

to take place on planet Earth.

We had these hydrogen sulfide oceans for a very great long period.

They stop complex life from existing.

We know hydrogen sulfide is erupting presently a few places on the planet.

And I throw this slide in -- this is me, actually, two months ago --

and I throw this slide in because here is my favorite animal, chambered nautilus.

It's been on this planet since the animals first started -- 500 million years.

This is a tracking experiment, and any of you scuba divers,

if you want to get involved in one of the coolest projects ever,

this is off the Great Barrier Reef.

And as we speak now,

these nautilus are tracking out their behaviors to us.

But the thing about this is that every once in a while

we divers can run into trouble,

so I'm going to do a little thought experiment here.

This is a Great White Shark that ate some of my traps.

We pulled it up; up it comes. So, it's out there with me at night.

So, I'm swimming along, and it takes off my leg.

I'm 80 miles from shore, what's going to happen to me?

Well now, I die.

Five years from now, this is what I hope happens to me:

I'm taken back to the boat, I'm given a gas mask:

80 parts per million hydrogen sulfide.

I'm then thrown in an ice pond, I'm cooled 15 degrees lower

and I could be taken to a critical care hospital.

And the reason I could do that is because we mammals

have gone through a series of these hydrogen sulfide events,

and our bodies have adapted.

And we can now use this as what I think will be a major medical breakthrough.

This is Mark Roth. He was funded by DARPA.

Tried to figure out how to save Americans after battlefield injuries.

He bleeds out pigs.

He puts in 80 parts per million hydrogen sulfide --

the same stuff that survived these past mass extinctions --

and he turns a mammal into a reptile.

"I believe we are seeing in this response the result of mammals and reptiles

having undergone a series of exposures to H2S."

I got this email from him two years ago;

he said, "I think I've got an answer to some of your questions."

So, he now has taken mice down

for as many as four hours, sometimes six hours,

and these are brand-new data he sent me on the way over here.

On the top, now, that is a temperature record of a mouse who has gone through --

the dotted line, the temperatures.

So, the temperature starts at 25 centigrade,

and down it goes, down it goes.

Six hours later, up goes the temperature.

Now, the same mouse is given 80 parts per million hydrogen sulfide

in this solid graph,

and look what happens to its temperature.

Its temperature drops.

It goes down to 15 degrees centigrade from 35,

and comes out of this perfectly fine.

Here is a way we can get people to critical care.

Here's how we can bring people cold enough to last till we get critical care.

Now, you're all thinking, yeah, what about the brain tissue?

And so this is one of the great challenges that is going to happen.

You're in an accident. You've got two choices:

you're going to die, or you're going to take the hydrogen sulfide

and, say, 75 percent of you is saved, mentally.

What are you going to do?

Do we all have to have a little button saying, Let me die?

This is coming towards us,

and I think this is going to be a revolution.

We're going to save lives, but there's going to be a cost to it.

The new view of mass extinctions is, yes, we were hit,

and, yes, we have to think about the long term,

because we will get hit again.

But there's a far worse danger confronting us.

We can easily go back to the hydrogen sulfide world.

Give us a few millennia --

and we humans should last those few millennia --

will it happen again? If we continue, it'll happen again.

How many of us flew here?

How many of us have gone through

our entire Kyoto quota

just for flying this year?

How many of you have exceeded it? Yeah, I've certainly exceeded it.

We have a huge problem facing us as a species.

We have to beat this.

I want to be able to go back to this reef. Thank you.

(Applause)

Chris Anderson: I've just got one question for you, Peter.

Am I understanding you right, that what you're saying here

is that we have in our own bodies

a biochemical response to hydrogen sulfide

that in your mind proves that there have been past mass extinctions

due to climate change?

Peter Ward: Yeah, every single cell in us

can produce minute quantities of hydrogen sulfide in great crises.

This is what Roth has found out.

So, what we're looking at now: does it leave a signal?

Does it leave a signal in bone or in plant?

And we go back to the fossil record and we could try to detect

how many of these have happened in the past.

CA: It's simultaneously

an incredible medical technique, but also a terrifying ...

PW: Blessing and curse.