Scientists have long wondered whether the West Antarctic Ice Sheet is a ticking time bomb in terms of sea level rise. New evidence from the DNA of a small octopus that lives in the Southern Ocean suggests that the ice sheet is indeed at risk of collapsing, according to a study published Thursday in the journal Science.

The research doesn’t predict when this might happen, but it indicates that 1.5 degrees Celsius of global warming over the preindustrial global average, or perhaps even less than that, might be a tipping point for the ice sheet.

The Earth is close to that temperature level now.

Several distinct populations of Pareledone turqueti, commonly known as Turquet’s octopus, live in the waters around Antarctica. These octopuses crawl along the sea floor and generally don’t stray far from home. A few individuals or their eggs might occasionally drift on currents to neighboring groups, but populations in the Ross Sea and Weddell Sea are separated by the impassable West Antarctic Ice Sheet.

And yet, genetic analysis of octopuses from different locations around Antarctica show that these two populations were mingling and swapping DNA about 120,000 years ago. This was a time in Earth’s history, called the Last Interglacial period, before the most recent ice age, when temperatures were similar to today.

The observed patterns in the octopus gene pool would only be possible if the West Antarctic ice sheet wasn’t there at the time and relatively open seaways across the continent allowed the octopuses to travel freely between the Ross and Weddell Seas, according to the researchers.

Scientists know sea levels were several feet higher then. But whether the additional water came from West Antarctica is “the question that the geoscience community has been trying to answer for nearly 50 years,” said Sally Lau, a postdoctoral researcher at James Cook University in Townsville, Australia, and lead author on the new study.

Today, the global average temperature is about 1.2 degrees Celsius higher than it was from 1850 to 1900, when the burning of fossil fuels began warming the climate. During the Last Interglacial, the global average temperature was similarly about 0.5 to 1.5 degrees Celsius warmer than that preindustrial baseline, but sea levels were about 16 to 32 meters higher than today. If climate change melts the West Antarctic ice sheet entirely, sea levels could rise by an average of up to 16 feet. (The East Antarctic Ice Sheet holds even more frozen water, but it is considered more stable.)

The researchers did not explicitly state whether today’s temperatures had already committed the planet to a complete collapse of the western ice sheet.

“We’re still not able to say for certain, but that’s definitely the implication,” said Nicholas Golledge, a professor of glaciology at Victoria University of Wellington in New Zealand and another author of the study.