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Press Release - Moss brought back to life after 1,500 years frozen in ice

Issue date: 17 Mar 2014
Number: 06/2014

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Drilling the frozen moss core on Signy (Photo: Peter Boelen)

Researchers from the British Antarctic Survey and Reading University have demonstrated that, after over 1,500 years frozen in Antarctic ice, moss can come back to life and continue to grow. For the first time, this vital part of the ecosystem in both polar regions has been shown to have the ability to survive century to millennial scale ice ages. This provides exciting new insight into the survival of life on Earth.

The team, reporting in Current Biology this week, observed moss regeneration after at least 1,530 years frozen in permafrost. This is the first study to show such long-term survival in any plant; similar timescales have only been seen before in bacteria. Mosses are known to survive environmental extremes in the short-term with previous evidence confirming up to a 20 year timescale for survival. Their potential to survive much longer timescales had not previously been examined.

Mosses are an important part of the biology of both polar regions. They are the dominant plants over large areas and are a major storer of fixed carbon, especially in the north.

Co-author Professor Peter Convey from the British Antarctic Survey explains:

“What mosses do in the ecosystem is far more important than we would generally realise when we look at a moss on a wall here for instance. Understanding what controls their growth and distribution, particularly in a fast-changing part of the world such as the Antarctic Peninsula region, is therefore of much wider significance.”

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A frozen moss core from deep in the moss bank (Photo: Esme Roads)

The team took cores of moss from deep in a frozen moss bank in the Antarctic. This moss would already have been at least decades old when it was first frozen. They sliced the frozen moss cores very carefully, keeping them free from contamination, and placed them in an incubator at a normal growth temperature and light level. After only a few weeks, the moss began to grow. Using carbon dating, the team identified the moss to be at least 1,530 years of age, and possibly even older, at the depth where the new growth was seen. Regeneration also occurred in a liverwort embedded in organic material at the base of the core.

According to Professor Convey:

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A moss core from near the surface (Photo: Esme Roads)

“This experiment shows that multi-cellular organisms, plants in this case, can survive over far longer timescales than previously thought. These mosses, a key part of the ecosystem, could survive century to millennial periods of ice advance, such as the Little Ice Age in Europe.

“If they can survive in this way, then recolonisation following an ice age, once the ice retreats, would be a lot easier than migrating trans-oceanic distances from warmer regions. It also maintains diversity in an area that would otherwise be wiped clean of life by the ice advance.

“Although it would be a big jump from the current finding, this does raise the possibility of complex life forms surviving even longer periods once encased in permafrost or ice.”

Lead author, Dr Royce Longton added:

“This work provides further evidence of the low decomposition rate generally attributed to mosses, and strengthens my conviction that the growth of mosses should be encouraged globally to act as a carbon sink and thus reduce global warming”.

This work was funded by the Natural Environment Research Council.

ENDS

Issued by the British Antarctic Survey Press Office.

Contact: Paul Seagrove, Tel: +44 (0)1223 221414; Mob: +44 (0)7736 921693; Email: psea@bas.ac.uk

Author contact: Peter Convey, British Antarctic Survey, Tel: +44 (0) 1223 221588; Email: pcon@bas.ac.uk

Reading press office contact: James Barr, Tel: +44 (0) 118 378 7115; Email: j.w.barr@reading.ac.uk

Notes for editors

The paper: Millennial timescale regeneration in a moss from Antarctica by Esme Roads, Royce E. Longton and Peter Convey is published in Current Biology on Monday 17 March 2014. View the paper at

Images are available on request.

Permafrost: Rock or soil that remains frozen throughout the year.