Gardens of giant sponges have been found thriving on extinct volcanic peaks in the depths of the ice-covered Arctic waters — despite the lack of light and food.

These surprisingly rich and densely populated marine ecosystems were found by researchers led from the Max Planck Institute for Marine Microbiology in Germany.

The sponge gardens are located on ‘seamounts’ along the Langseth Ridge, a submarine mountain range in the high Central Arctic, close to the North Pole.

Nutrients are scarce in this dark domain, as the low light levels in the waters above the gardens limit the productivity of photosynthetic algae.

In fact, activity in the waters over the study area could only supply less than one per cent of the sponge’s carbon needs, according to the researchers. 

However, surveys using towed camera platforms showed that the biomass of the sponges was comparable to those living in shallow, nutrient-rich waters. 

The researchers suggest the gardens are able to grow because the sponges feed on the fossil remnants of animals that lived along the ridge thousands of years ago.

Gardens of giant sponges (pictured) have been found thriving on extinct volcanic peaks in the depths of the ice-covered part of the Arctic ocean — despite the lack of light and food

Gardens of giant sponges (pictured) have been found thriving on extinct volcanic peaks in the depths of the ice-covered part of the Arctic ocean — despite the lack of light and food

Gardens of giant sponges (pictured) have been found thriving on extinct volcanic peaks in the depths of the ice-covered part of the Arctic ocean — despite the lack of light and food

These surprisingly rich and densely populated marine ecosystems were found by researchers led from the Max Planck Institute for Marine Microbiology in Germany

These surprisingly rich and densely populated marine ecosystems were found by researchers led from the Max Planck Institute for Marine Microbiology in Germany

These surprisingly rich and densely populated marine ecosystems were found by researchers led from the Max Planck Institute for Marine Microbiology in Germany

SPONGES: BASAL BUT HIGHLY SUCCESSFUL

Despite being considered among the most basal of all forms of animal life, sponges are extremely successful and found across all of the world’s oceans.

Many sponges — including those the team found in the unexpected Central Arctic ecosystem — harbour symbiotic microorganisms.

These tiny microbes are beneficial for the sponges because they perform actions like produce antibiotics, dispose of waste excretions and transfer nutrients.

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The study was undertaken by geomicrobiologist Antje Boetius of the Max Planck Institute for Marine Microbiology in Bremen and her colleagues.

‘Thriving on top of extinct volcanic seamounts of the Langseth Ridge we found massive sponge gardens, but did not know what they were feeding on,’ explained Professor Boetius. 

To solve this puzzle, the researchers used remotely operated vehicles specially designed to travel under the sea ice to take samples of the sponges.

The team found that the gardens were dominated by sponges of the genus Geodia, which are characterised by being made up of a high density of silica-based, spiny structural elements called ‘spicules’. 

‘Our analysis revealed that the sponges have microbial symbionts that are able to use old organic matter,’ said paper author and marine biologist Teresa Morganti, also of the Max Planck Institute.

‘This allows them to feed on the remnants of former, now extinct inhabitants of the seamounts, such as the tubes of worms composed of protein and chitin and other trapped detritus.’

Nutrients are scant in this dark domain, as the low light levels in the waters above the gardens limit the productivity of photosynthetic algae

Nutrients are scant in this dark domain, as the low light levels in the waters above the gardens limit the productivity of photosynthetic algae

Nutrients are scant in this dark domain, as the low light levels in the waters above the gardens limit the productivity of photosynthetic algae

The gardens are able to grow, the researchers said, because the sponges feed on the fossil remnants of animals that lived along the ridge thousands of years ago

The gardens are able to grow, the researchers said, because the sponges feed on the fossil remnants of animals that lived along the ridge thousands of years ago

The gardens are able to grow, the researchers said, because the sponges feed on the fossil remnants of animals that lived along the ridge thousands of years ago

These fossilised creatures had lived on the Central Arctic seabed thousands of years ago, at which time substances leaking from the sea floor was able to support a diverse ecosystem.

While this food source is now long dried up, the animals it nourished have now taken its place, allowing life to continue to thrive in this unexpected setting. 

‘The microbes have just the right toolbox for this habitat,’ said paper author and marine microbiologist Ute Hentschel of the GEOMAR Helmholtz Centre for Ocean Research in Kiel.

‘The microbes have the genes to digest refractory particulate and dissolved organic matter and use it as a carbon and nitrogen source, as well as a number of chemical energy sources available there.’

The team also found that the sponges produce mats made of spicules on which they crawl, and may also help to trap detrital particles to feed the sponges and the microbes that live within them.

The researchers used remotely operated vehicles specially designed to travel under the sea ice — launched from their vessel, the RV Polarstern (pictured) to take samples of the sponges

The researchers used remotely operated vehicles specially designed to travel under the sea ice — launched from their vessel, the RV Polarstern (pictured) to take samples of the sponges

The researchers used remotely operated vehicles specially designed to travel under the sea ice — launched from their vessel, the RV Polarstern (pictured) to take samples of the sponges

‘This is a unique ecosystem. We have never seen anything like it before in the high Central Arctic,’ Professor Boetius added.

‘This sponge garden may be a transient ecosystem, but it is rich in species, including soft corals.’

With the Arctic being one of the regions most severely affected by climate change, the findings of the study could help us to preserve the sponge gardens in the future.

‘With sea-ice cover rapidly declining and the ocean environment changing, a better knowledge of hotspot ecosystems is essential for protecting and managing the unique diversity of these Arctic seas under pressure,’ Professor Boetius concluded. 

The full findings of the study were published in the journal Nature Communications.

HOW DO RISING TEMPERATURES IN THE ARCTIC CREATE COLD WEATHER IN EUROPE?

As long ago as 1973, a study suggested that an ice-free Arctic Ocean could make regions further south colder.

That ‘warm Arctic, cold continent’ (WACC) pattern is sometimes dubbed ‘wacc-y’ or ‘wacky’ among climate scientists.

When unusually warm air enters the region, it melts ice covering the waters of the Arctic Ocean.

This ice normally serves as an insulator, stopping the flow of thermal energy from the water’s surface into the atmosphere.

Without the ice in place, the oceans can transfer a huge amount of this energy into the air above.

This in turn increases air temperatures and this warm air rises up into the upper atmosphere, where it reaches the jet stream.

Jet streams are fast flowing, narrow currents of air that carry warm and cold air across the planet, much like the currents of a river.

They cover thousands of miles as they meander near the tropopause layer of our atmosphere.

The strongest jet streams are the polar jets, found 30,000 to 39,000 ft (5.7 to 7.4 miles/ 9 to 12 km) above sea level at the north and south pole.

In the case of the Arctic polar jet this fast moving band of air sits between the cold Arctic air to the north and the warm, tropical air to the south.

When uneven masses of hot and cold meet, the resulting pressure difference causes winds to form.

During winter, the jet stream tends to be at its strongest because of the marked temperature contrast between the warm and cold air.

The bigger the temperature difference between the Arctic and tropical air mass, the stronger the winds of the jet stream become.

The Arctic polar jet, which can reach speeds of up 200mph (320kph), flows over the middle to northern latitudes of North America, Europe, and Asia and their intervening oceans.

It moves from East to West, although its exact route varies and can be affected by various factors.

With the ice melt in the Arctic and the introduction of warmer air, the route of the jet stream becomes wavier and more erratic.

That means that the colder air it carries from the Arctic can penetrate further south and warmer airs from the tropics is carried further north. 

If the jet stream’s meander buckles south of the UK, it attracts cold air from the Arctic.

Conversely when it swings north, it sucks warm air from the tropics. 

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This post first appeared on Dailymail.co.uk

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