Hear researcher Andy Wheeler speaking about an expedition to discover new hydrothermal vent field in the middle of the Atlantic Ocean

My name's Andy Wheeler. I'm the vice-head of the School of Biological, Earth, and Environmental Sciences, and I'm the acting head of Geology discipline within that school. But I'm the chief scientist on this expedition.

We had a very challenging expedition. It was a voyage of discovery, very much so. We set out to discover a new hydrothermal vent field.

So we went 1,500 kilometers out to sea, way, way out in the Atlantic. We couldn't really have got further away from land. Right to the very center, the middle of the Atlantic, where the plates are pulling apart, where the sea bed is cracking open, and Europe and America are pulling it apart.

And then, when we got there, we sent a robotic camera system down to the bottom, 3 kilometers down to the bottom of the sea bed, onto an active volcano, where we discovered-- after a lot of hunting, we discovered this new hydrothermal vent field. And what I mean by that is this is where seawater is being pumped out through the volcanic edifice.

It's a bit like-- it's a bit like geysers, on land-- or geysers, on land, I should say, like Old Faithful in Yellowstone Park. That's where rain water is pumped down towards the magma chain, and then it gushes up as a big explosion of water. If you have this same situation on the seabed, the amount of water pumping through these systems is so much greater. And the water comes out at about 350 degrees C, extremely hot, and full of metals that it's picked up from the magma and from the rocks that it's had to pass through. So it comes out really, really hot, full of lots of metals, extremely toxic-- but eventually actually fertilizes the ocean, replenishing metals in the ocean, making ore-grade metal sulfide deposits and also supporting quite intriguing and strange life forms, as well.

In 2008, the National Oceanography Center in the UK had an expedition out looking at the volcanics going on on this ridge. And at the end of that expedition, they caught a trace in the water column, a very faint trace in the water column, of these so-called black smokers, the plumes off this hydrothermal system. But they ran out of time and had to go back. So through UCC's collaborations with the National Oceanography Center-- they contacted us. They contacted myself and Professor John Gamble in the Geology discipline in the School of BEES, and asked us if we could get a ship, if we could go out there and launch an expedition.

So we did. We applied for funding from the Marine Institute, who supplied the vessel and the ROV. We planned the expedition. It took a lot of planning, a lot work. We pulled a team together from UCC, from NOC, from the University of Southampton, from the Geological Survey of Ireland, and also NUIG. We set out on this expedition, picked up that signal in the water column again, and then traced it down to source very efficiently and effectively. Usually takes about a week to try to box in and find these vent sites.

We did it in two days, which is very impressive. Everyone was impressed by that. And to put it in context, the vent sight's about the size of a football pitch, 3 kilometers down. And we started about 20 kilometers away and sort of found these faint chemical signatures, worked our way down to the sea bed, eventually dove on it, and then within two hours, we bumped into the black smoke in the water column. And we struggled down even deeper, pretty much just about beyond the capacity of the ROV. We really pushed it, and we struggled down to 3,000 meters.

It's a 3,000-meter ROV. People were very nervous. And I said, we've just got to go a little bit more, a little bit more, and then eventually found the site. And then we spent the next week or so mapping this site and investigating it, really at the capacity of the ship and of the ROV. It was a gigantic effort. But we pulled it off, and we're delighted.