There's a good chance you've heard of

hydrothermal vents.

Located in the deep ocean,

thousands of meters from the surface, these towering chimneys

spew black, acidic, metal-rich water from deep within the Earth.

Hydrothermal vents are some of the most extreme environments on the planet—and home to some

of the most interesting creatures alive.

But in 2000, scientists discovered a vent unlike any other—one not quite so deep down

with white chimneys that's been around at least ten times longer than any other vent

field.

And some of them think it may help us understand how all life began.

The researchers on the Alvin submersible weren't looking for a massive hydrothermal vent field

when they were exploring a mountainous region of the Atlantic seafloor about 750 to 900

meters below the waves.

They basically stumbled upon it: a sprawling field of huge, white spires and chimneys up

to sixty meters tall.

Because of these dramatic structures, and the site's location on the Atlantis Massif,

the researchers named the site the Lost City Hydrothermal Field.

And it turns out Lost City is really different from other hydrothermal vents.

Most vents are what scientists call “black smokers”, and they form where there's

lots of volcanic activity.

In those cases, water in the Earth's crust gets superheated by underground, molten rock

and bursts out into the deep ocean.

We're talking water that's hotter than boiling—like, up to —which is only kept

from becoming gas by the intense pressure of the deep sea.

This super hot water strips the rocks it comes into contact with of minerals like iron sulfide,

which turns it black.

Lost City's white smoker chimneys are basically the exact opposite of that because they form

by a process known as serpentinization instead.

It occurs when seawater meets olivine, a greenish mineral containing magnesium, iron and silicate.

You might have actually seen some of this stuff before—the gem-quality version is

known as peridot.

Olivine is formed naturally in the Earth's mantle—that viscous layer of molten rock

/below/ the crust.

And at Lost City, the olivine-rich mantle is closer to the surface than usual—perhaps

because it sits near the intersection of a mid-ocean ridge and a fault.

Whatever the reason, the mantle is close enough that the seawater can seep down through the

cracks in the crust and come into contact with this olivine.

And that sets off a chemical reaction.

As water infiltrates the gaps of olivine's crystal structure, it changes into serpentinite.

As that happens, some of the oxygen atoms combine with the iron from the olivine to

form magnetite——and the hydrogen atoms come together to make hydrogen gas.

But in the presence of carbon dioxide—like the carbon dioxide that's in seawater—something

else happens.

Carbon atoms from the CO2 and those extra hydrogen atoms from serpentinization come

together to form methane gas.

Which for the record, makes Lost City really special… but we'll get to that in a bit.

The important things to know for now are that these reactions give off some heat, so the

surrounding water gets a little toasty—but only about 40 to 90 degrees Celsius [104 - 194°F]

, so it's cool in comparison to black smokers.

And during this process, CO2 gets removed from the seawater, which ultimately makes

the water much less acidic.

You see, dissolved carbon dioxide reacts with ocean water to form carbonic acid, which can

further react with water to form carbonate and bicarbonate ions.

That ultimately releases hydrogen ions and, therefore, makes the water more acidic.

If you remove CO2, though, the reactions go the other way.

Which is why the chimneys at Lost City have a pH of about nine—closer to baking soda

than plain water.

That's the exact opposite of other hydrothermal vents, which spew very acidic water.

It also happens to be why Lost City has white smoke.

You may have heard of the mineral calcium carbonate because it's that white stuff

that shells and corals are made of.

And it's an awesome building material—if your water isn't too acidic.

If it is, those roaming hydrogen ions will react with the carbonate ions instead of the

calcium.

Hydrogen and calcium ions are both positively charged, so when they're in seawater, both

could potentially pair up with negatively-charged carbonate ions.

But what usually happens is a hydrogen covalently bonds to the carbonate, turning it into bicarbonate—which,

even though it's negatively charged, the positive calcium ions don't do much with.

If you raise the pH and remove those hydrogen ions, the carbonate stays carbonate and can

combine with calcium.

And voilà, you get white-tinted water.

There's one more way Lost City differs from most hydrothermal vents: It's a lot older.

Black smokers are fueled by the heat from volcanic activity.

And once that source of heat is consumed or otherwise disappears thanks to tectonic shifts,

they die.

Since Lost City doesn't rely on the fickle whims of volcanic activity to flourish, it's

estimated to be 120,000 years old—roughly twelve times the age of its black smoker cousins!

And it doesn't seem to be in danger of dying any time soon.

So, Lost City is a pretty fascinating place.

But it doesn't just stand out amongst hydrothermal vents: It may also give us clues as to the

origin of life.

Remember that methane we talked about?

Well, methane is the simplest hydrogen- and carbon-containing molecule, or hydrocarbon.

On Earth, hydrocarbons are usually made by living organisms—and all living organisms

we know of need them to build essential molecules like proteins, fats, and starches.

So back before there were any living things, the first life would have needed a non-biological

source of hydrocarbons.

And that source could have been serpentinization.

While white smoker hydrothermal vents are rarer than their counterparts, and Lost City

is certainly the largest and most famous example, it isn't the only one.

So scientists think that a site like Lost City could have been responsible for the origin

of life on our planet, and maybe even elsewhere in the solar system

—on far-off moons like Titan, Europa, or Enceladus.

Of course, we still don't know how life began on this planet, and it might not have

begun in the depths of the sea.

But understanding where the building blocks of life can come from is definitely a good

start.

And there may be other biological secrets hidden in Lost City, too.

After all, scientists have only begun to study its unique microbial community and how they

survive the warm, alkaline waters they call home.

So who knows what else we might learn from this incredible and magnificent geological

oddity.

For more of the Earth's strangest spots, you can check out our compilation episode

featuring six weird places!

{♫Outro♫}