The results are published in PNAS.
"Every year we go back to the dome area with our research vessel, and every year I am anxious to see if one of these domes has become a crater," says lead author of the study Pavel Serov, PhD candidate at CAGE at UiT The Arctic University of Norway.
These domes are the present-day analogue to what scientists think preceded the craters found in the near-by area, which were recently reported in Science. The craters were formed as the ice sheet retreated from the Barents Sea during the deglaciation some 12.000 years ago.
At the time, 2km thick ice-cover loaded what now is the ocean floor with heavy weight. Under the ice sheet the methane became stored as hydrate, a solid form of frozen methane.
"We believe that one step before the craters are created, you get these domes. They are mounds of hydrates, technically we call them gas hydrate pingos. They are hydrate and methane saturated relics of the last ice-age. They haven't collapsed yet. And the reason is a matter of narrow margins" states Serov.
20 meters from the brink of collapse
The dome area is situated on the Arctic Ocean floor just north of the craters. It is deeper, but not by much. The domes are found some 20 meters deeper. Essentially the height of the Buckingham Palace keeps these methane domes from blowing out the gas and becoming craters.
"Hydrates are stable in low temperatures and under high pressure. So, the pressure of 390 meters of water above is presently keeping them stabilised. But the methane is bubbling from these domes. This is actually one of the most active methane seep sites that we have mapped in the Arctic Ocean. Some of these methane flares extend almost to the sea surface" says Serov.
He is reluctant to speculate as to how much methane may be released into the ocean should the domes collapse entirely and abruptly. It is not possible to predict when it may happen either. But every sediment core collected in the area is full of hydrates.
This is actually the first time that domes such as these have been found outside of the permafrost areas.
More stable than in permafrost
However unstable these domes on the Arctic Ocean floor may be, they are still more stable than the pingos found in sub- sea permafrost in Canadian and Russian Arctic.
"The gas hydrate pingos in permafrost are formed because of the low temperatures. But the water-depth that supports gas hydrates in sub-sea permafrost is only 40 to 50 meters. There is no significant pressure there to keep them in check. Sub-seabed permafrost is deteriorating constantly and quickly" notes Serov.
Even though they are more stable than the permafrost pingos, the Barents Sea domes are on the limit of their existence.
"A relatively small change in the water temperature can destabilise these hydrates fairly quickly. We were actually very lucky to observe them at this point. And we will probably be able to observe significant changes to these domes during our lifetime."
Pavel Serov | EurekAlert!
Scientists discover Earth's youngest banded iron formation in western China
12.07.2018 | University of Alberta
Drones survey African wildlife
11.07.2018 | Schweizerischer Nationalfonds SNF
For the first time ever, scientists have determined the cosmic origin of highest-energy neutrinos. A research group led by IceCube scientist Elisa Resconi, spokesperson of the Collaborative Research Center SFB1258 at the Technical University of Munich (TUM), provides an important piece of evidence that the particles detected by the IceCube neutrino telescope at the South Pole originate from a galaxy four billion light-years away from Earth.
To rule out other origins with certainty, the team led by neutrino physicist Elisa Resconi from the Technical University of Munich and multi-wavelength...
For the first time a team of researchers have discovered two different phases of magnetic skyrmions in a single material. Physicists of the Technical Universities of Munich and Dresden and the University of Cologne can now better study and understand the properties of these magnetic structures, which are important for both basic research and applications.
Whirlpools are an everyday experience in a bath tub: When the water is drained a circular vortex is formed. Typically, such whirls are rather stable. Similar...
Physicists working with Roland Wester at the University of Innsbruck have investigated if and how chemical reactions can be influenced by targeted vibrational excitation of the reactants. They were able to demonstrate that excitation with a laser beam does not affect the efficiency of a chemical exchange reaction and that the excited molecular group acts only as a spectator in the reaction.
A frequently used reaction in organic chemistry is nucleophilic substitution. It plays, for example, an important role in in the synthesis of new chemical...
Optical spectroscopy allows investigating the energy structure and dynamic properties of complex quantum systems. Researchers from the University of Würzburg present two new approaches of coherent two-dimensional spectroscopy.
"Put an excitation into the system and observe how it evolves." According to physicist Professor Tobias Brixner, this is the credo of optical spectroscopy....
Ultra-short, high-intensity X-ray flashes open the door to the foundations of chemical reactions. Free-electron lasers generate these kinds of pulses, but there is a catch: the pulses vary in duration and energy. An international research team has now presented a solution: Using a ring of 16 detectors and a circularly polarized laser beam, they can determine both factors with attosecond accuracy.
Free-electron lasers (FELs) generate extremely short and intense X-ray flashes. Researchers can use these flashes to resolve structures with diameters on the...
13.07.2018 | Event News
12.07.2018 | Event News
03.07.2018 | Event News
13.07.2018 | Event News
13.07.2018 | Materials Sciences
13.07.2018 | Life Sciences