Antarctica once housed swampy rainforests and had an average temperature of around 12C, according to a new study.
Researchers said they have discovered evidence that the South Pole had a temperate climate around 90 million years ago when dinosaurs roamed the earth.
The findings, published in the journal Nature, are based on soil samples believed to be from the mid-Cretaceous period (115-80 million years ago).
The team, which included scientists from the UK and Germany, said analysis of preserved roots and other plant remains in the soil suggests the world at that time was warmer than previously thought.
Professor Tina van de Flierdt, from the department of earth science and engineering at Imperial College London, and one of the study authors, said: “The preservation of this 90 million-year-old forest is exceptional, but even more surprising is the world it reveals.
“Even during months of darkness, swampy temperate rainforests were able to grow close to the South Pole, revealing an even warmer climate than we expected.”
After analysing an ice core extracted from the seabed near the Pine Island and Thwaites glaciers in West Antarctica, the team discovered well-preserved forest soil, including the remains of flowering plants.
The study also suggests there were higher levels of carbon dioxide in the atmosphere during the age of the dinosaurs.
Professor Ulrich Salzmann, a paleoecologist at Northumbria University and one of the study authors, said: “The numerous plant remains indicate that 93 to 83 million years ago the coast of West Antarctica was a swampy landscape in which temperate rainforests grew – similar to the forests that can still be found, say, on New Zealand’s South Island.”
The researchers also assessed the conditions that would have been suitable for the plants found in the soil sample, to get a better idea of what the climate was like at that time.
Simulations revealed summer temperatures would have been around 19C while water temperatures in the rivers and swamps would have reached up to 20C.
The amount and intensity of rainfall in West Antarctica would have been similar to that seen in today’s Wales, the researchers said.
“Before our study, the general assumption was that the global carbon dioxide concentration in the Cretaceous was roughly 1,000 ppm (parts per million)," said Professor Gerrit Lohmann, a climate modeller at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research in Germany and study co-author.
“But in our model-based experiments, it took concentration levels of 1,120 to 1,680 ppm to reach the average temperatures back then in the Antarctic.”
The researchers are yet to figure out what caused the climate to eventually cool to form ice sheets in Antarctica.
Prof Lohmann added: “Our climate simulations haven’t yet provided a satisfactory answer.”
