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GoNorth 2023

Discovers new hydrothermal field between Svalbard and Greenland

Scientists taking part in the 2023 GoNorth expedition have discovered a new hydrothermal field – an area with sea floor hot springs – in the Lena Trough, part of a mid-ocean ridge between Svalbard and Greenland.

GoNorth expedition 2023

Producer:
SINTEF/GoNorth

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The expedition came to a successful conclusion despite an incident a few days in that forced the ship to go to Tromsø for repairs.

Svarte skorsteiner på havdypet

These hydrothermal chimneys had never been seen by human eyes before. They are of a type called black smoker, because the hot water they spew out has been rendered black by chemical interactions with rocks.

Photo:
Ægir 6000/NORMAR/UiB

A long search

Research vessel Kronprins Haakon spent nine days scouring the Lena Trough with a remotely operated vehicle (ROV) for signs of hydrothermal activity. The ROV found many such signs: minerals produced by hydrothermal activity, fauna commonly associated with these areas, and hot water coming out of the sea floor.

Fauna funnet i nærheten av varmekilder på havbunden.

Certain types of fauna are commonly found near hydrothermal vents. Left of centre, the shrimp-like creatures you can see are called amphipods. The curly threads on the right are tubeworms. The white part most likely consists of a mix of bacteria and minerals – yet another telltale sign of hydrothermal activity.

Photo:
Ægir 6000/NORMAR/UiB

At first, the springs (geologists call them “vents”) found by the ROV were of the shimmering kind; these spew out crystal-clear water, which makes them visible on video because they cause a shimmer in the water, but almost impossible to see on still images. The holy grail of hydrothermal activity, though, is the black smoker: these vents spew out hot water (sometimes as hot as 400°C) turned black by chemical interactions with underground rocks.

Hydrothermal vents are often associated with tall, chimney-like structures created by the outflow of chemically laden water. Scientists found several inactive chimneys during their search. Late at night, on what was slated to be the ROV’s very last dive of the expedition, they found one that was very much active and estimated to be as much as 10 metres tall.

Strukturer laget av sulfider på havbunnen

Just before coming to the chimney, the ROV filmed this sulphide structure. It is covered in amphipods, shrimp-like creatures enjoying the hydrothermal warmth and chemical nutrients in the fluids.

Photo:
Ægir 6000/NORMAR/UiB

første bilde av ny skorstein

This is the moment the scientists saw the chimney for the very first time. It is dark down in the deep, and the ROV needs to get quite close to be able to see anything.

Photo:
Ægir 6000/NORMAR/UiB

Et annet sted i området var det også varmt vann som kom ut som ikke var svart. Fargen kommer av at vannet reagerer med steinene i undergrunnen.

At another location in the same vicinity, hot water that had not changed colour to black was coming out of the rock. The colour change is the result of chemical reactions between the water and the rocks below the seabed.

Photo:
Ægir 6000/NORMAR/UiB

Storjubel på Kronprins Haakons konferanserom etter oppdagelsen av den svarte skorsteinen. På bildet: Maja Jæger (UiB), Sabina Strmic Palinkas (UiT), Håvard Stubseid (UiB), Rolf Birger Pedersen (UiB) og Eszter Sendula (UiT)

Hugs and high fives in RV Kronprins Haakon’s conference room after the discovery of the black smoker. Left to right: Maja Jæger (UiB), Sabina Strmic Palinkas (UiT), Håvard Stubseid (UiB), Rolf Birger Pedersen (UiB) and Eszter Sendula (UiT).

Photo:
Ægir 6000/NORMAR/UiB

Building on previous results

It was known that there was hydrothermal activity in this particular area (called Lucky Ridge) since 2004. That’s when German research vessel Polarstern dredged up some rocks rich in sulphides, which suggests that they were hydrothermal mineral deposits. They also registered temperature anomalies in the water column; another sign that hot water is coming up from the sea floor somewhere in the area.

Lucky Ridge is a 1600-metre-tall subsea mountain (the same height as Trollveggen), sitting in a 4000-metre-deep valley. GoNorth explored it extensively over the past days. Scientists not only found several active sites but created a detailed seafloor map of the area with the ROV. In total, over 100 samples have been collected (80 in the Lucky Ridge area), and their analysis over the coming months will shed even more light on the geological characteristics of the new vent field.

“At first glance, this seems like a very special field,” says expedition leader Rolf Birger Pedersen. “It has many traits that differentiate it from similar areas other places around the world.”

These differences will no doubt be explained as the scientists carry out their analyses over the coming months. Rolf Birger Pedersen expects the area to get a lot of attention, moving forward.

“Lucky Ridge is composed of mantel rock that are normally covered by the crust. Reactions between the mantel minerals and seawater leads to the release of hydrogen, which is a source of energy for certain types of microorganisms. These microorganisms are in turn a source of food for other, bigger creatures. The areas mapped by GoNorth can become a living laboratory for the study of this interplay between life, water and minerals.”

Utdødd skorstein på havbunnen som ble oppdaget under toktet

An inactive chimney discovered earlier during the expedition. It has an unusual look, according to the geologists on board. It also has a thick manganese crust, which suggests it’s been inactive for a while.

Photo:
Ægir 6000/NORMAR/UiB

Damaged instrumentation

On 10 July, just three days after setting out from Longyearbyen, the expedition was hit by an unfortunate incident. A steel rod holding a crucial positioning device underneath the hull of the ship was bent when it was hit by sea ice. Kronprins Haakon had to go to Tromsø for repairs, at reduced speed, which amputated the research time by several days.

The repairs were carried out quickly thanks to the good work of the ship’s crew, with support from Maritim Sveiseservice for crane operations, Fagdykk for the diving operation needed to remove the bent steel rod, and Kongsberg Support for rapidly sending a spare part to Tromsø.

Heavy sea ice

Unusually heavy ice conditions – when compared to recent years at least – meant that the ship was unable to reach the Nansen and Amundsen Basins, where some research activities were planned. Even German research vessel Polarstern, a heavier, more powerful icebreaker than Kronprins Haakon, struggled in these conditions. This is how the expedition came to spend more time than initially planned in the Lena Trough.

Collaboration with Polarstern

Even though sea ice dictated where the ships could be, the planned collaboration between Norwegian vessel Kronprins Haakon and German vessel Polarstern was carried out. The ROV picked up an ocean-bottom seismometer that Polarstern had not managed to release from the sea floor. Polarstern in turn provided coordinates to interesting areas in both the Aurora vent field (where the ships met) and in the Lucky Ridge area.

A multidisciplinary expedition

GoNorth’s objective is to push the boundaries of knowledge about Norway’s neighbourhood in the Arctic Ocean, from the sea floor and subsea geology to the sea ice, via the water column. As such, a diverse group of scientists with various areas of expertise have participated in the expedition.

Next up: Morris Jesup Rise

GoNorth’s third expedition is slated to start in September of 2024, with the goal being Morris Jesup Rise, an underwater projection of the Northern Greenland shelf into the Arctic Ocean.

GoNorth on Dagsrevyen

GoNorth was featured on NRK evening news show Dagsrevyen, on 18 August. You can watch the segment (in Norwegian) here: Unike havbilder

 

Skjermdump fra Dagsrevyen på NRK
Photo:
Skjermdump NRK