Octopus DNA contains grave warning for sea level rise

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Australia; New Zealand; Pacific; QLD; WA
The Amundsen Sea from Marie Byrd Island. Image: Jasmine Lee
The Amundsen Sea from Marie Byrd Island. Image: Jasmine Lee

Aussie and NZ scientists have used octopus DNA to discover that the West Antarctic Ice Sheet (WAIS) likely collapsed during the Last Interglacial period around 120,000 years ago – when global temperatures were similar to today. The team compared the genetic profiles of Turquet’s octopus found in the Weddell, Amundsen, and Ross seas and found genetic connectivity dating back to the Last Interglacial. According to the team, this genetic connectivity would only be possible if a complete collapse of the WAIS occurred during the Last Interglacial, opening seaways linking the present-day Weddell, Amundsen and Ross seas.

Media release

From: James Cook University

Scientists have used octopus DNA to discover that the West Antarctic Ice Sheet (WAIS) likely collapsed during the Last Interglacial period around 120,000 years ago – when global temperatures were similar to today.

This provides the first empirical evidence that the tipping point of this ice sheet could be reached even under the Paris Agreement targets of limiting warming to 1.5 - 2 °C.

The study published in the journal Science today was led by Professor Jan Strugnell, Chief Investigator, and Dr Sally Lau, Postdoctoral Research Fellow, from ARC Securing Antarctica’s Environmental Future at James Cook University.

Professor Strugnell said the team’s research solves a long-running mystery that has puzzled scientists about whether the WAIS collapsed during the Last Interglacial.

“This was a period when global average temperatures were 0.5 – 1.5 °C warmer than preindustrial levels, but global sea level was 5 – 10 metres higher than today.”

“What makes the WAIS important is that it is also Antarctica’s current biggest contributor to global sea level rise. A complete collapse could raise global sea levels by somewhere between 3 and 5 metres.

“Understanding how the WAIS was configured in the recent past, when global temperatures were similar to today, will help us improve future global sea level rise projections,” said Professor  Strugnell.

Dr Lau said that population genetics offered an exciting and novel approach to answering this question.

“DNA holds a history of its past and can be used to look back in time to pinpoint when different populations of animals were mixing and exchanging genetic material.”

The team compared the genetic profiles of Turquet’s octopus found in the Weddell, Amundsen, and Ross seas and found genetic connectivity dating back to the Last Interglacial.

“This genetic connectivity would only be possible if a complete collapse of the WAIS occurred during the Last Interglacial, opening seaways linking the present-day Weddell, Amundsen and Ross seas.

“This would have allowed octopus to travel across the opened straits and exchange genetic material, which we can see in the DNA of today’s populations,” said Dr Lau.

Professor Strugnell said the findings will support decision-making around adaptation and mitigation measures in coastal regions around the world.

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Journal/
conference:
Science
Research:Paper
Organisation/s: James Cook University, Western Australian Museum, Victoria University of Wellington
Funder: Australian Research Council (ARC) Discovery grant DP190101347 (JMS, NGW, NRG, TRN) New Zealand Ministry of Business, Innovation and Employment through the Antarctic Science Platform (ANTA1801) (NRG, TRN) Thomas Davies Research grant (Australian Academy of Science) (JMS) David Pearse bequest (SCYL) Antarctic Science Bursary (SCYL) Antarctic PhD student support grant (Antarctic Science Foundation) (SCYL) Australasian eResearch Organisations (AeRO) Cloud Grant (SCYL) CoSyst grant (JMS, PCW) Finnish Academy grant 305532 (PCW) Australian Research Council (ARC) SRIEAS Grant SR200100005 Securing Antarctica’s Environmental Future Scientific Committee on Antarctic Research (SCAR) INSTANT programme
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