Exploring the climate history and the geological structure and evolution of the rocks and mountains of Antarctica’s continental interior provides clues to past, present and future environmental change. Under-ice lakes, mountain chains buried by up to 4km ice, and sea bed sediments surrounding the frozen continent provide an unparalleled record of how the Earth’s climate has changed over millions of years.

Antarctica — our fifth largest continent — is 58-times the size of the UK. Buried beneath the snow and ice that cover more than 99% of its surface are chains of mountains the size of the Alps, while around the edge of the continent, and running across its centre, are other large mountain ranges that rise above the ice.

Geologists have studied the rocks in these mountains for more than a century. These rocks reveal that Antarctica has moved vast distances over millions of years. More than 500 million years ago, Antarctica straddled the equator, and the warm, shallow seas that covered the continent supported trilobites and other organisms long since extinct.

For hundreds of millions of years, Antarctica was locked in the centre of a giant continent called Gondwana. Around 150 million years ago, this supercontinent began to split apart, forming the modern continents of Australia, India, South America and Africa. At that time, instead of ice and snow, Antarctica was covered in dense forest and dinosaurs roamed its coastal plains.

Rocks and fossils tell us that the continent began to cool about 80 million years ago and around 35 million years ago, a vast ice sheet blanketed East Antarctica.

Locked in Antarctica’s rocks and in the sea bed around the continent is an unparalleled record of how the Earth’s climate has changed over millions of years. During the past 50 years, geologists at British Antarctic Survey (BAS) have built up the world’s largest archive of Antarctic rocks and fossils and made major contributions to our understanding of Antarctica’s ancient history.

Today, using BAS’s Royal Research Ship James Clark Ross to carry out surveys at sea and BAS aircraft to study remote corners of the continent, BAS geologists are using these ancient records to help predict how future climate change will affect not only Antarctica, but also the rest of the world.

Scientists at BAS are using advanced computer models to show what the Antarctic may have looked like 3 million years ago. The models suggest that during the mid-Pliocene warm period, the ice retreated significantly from the edges of the continent and was replaced by a sparse tundra vegetation. That a rise in temperature of only a few degrees centigrade had such a profound effect on Antarctica is a stark reminder of what might happen in the near future.


KANG-GLAC

The Greenland Ice Sheet is decaying at an accelerating rate in response to climate change. Warm ocean waters moving through the fjords eventually meet the faces of marine-terminating glaciers, increasing …


Bedmap

Bedmap is a collaborative community project with the aim to produce a new map and datasets of Antarctic ice thickness and bed topography for the international glaciology and geophysical community, …


HEXPLORES

The HEXPLORES project aims to explore for active hydrothermal vents in the Red Sea Rift. Although the Red Sea Rift hosts the world’s largest submarine metalliferous sulphide deposit, no active …


IceAGE

The international IceAGE (Icelandic marine Animals: Genetics and Ecology) project, initiated in 2008 and managed by Drs Saskia Brix and Karin Meißner from DZMB Hamburg, Germany, builds on data obtainedby …


GRADES-IMAGE

The GRADES-IMAGE science programme was a British Antarctic Survey-funded project over the Antarctic Peninsula and Filchner-Ronne Ice Shelf. The aim of the programme was to image englacial layering and bedrock …


SIWHA

The NERC funded SIWHA_CO2 project “Sea Ice and Westerly winds during the Holocene in coastal Antarctica, to better constrain oceanic CO2 uptake” will be a breakthrough in our understanding of how …


P-RAID

The ice sheets of Antarctica can be several kilometres thick, and contain precious information about the past climate. However, the bottoms of the ice sheets are melting, erasing this information. …





BAS staff recognised with Royal Society Fellowships

6 May, 2021

We are delighted to announce that today (6 May 2021) Professor Dame Jane Francis, Director of British Antarctic Survey, and Professor Richard Horne, Head of Space Weather and Atmosphere team, …


Antarctica’s magnetic link to ancient neighbours

10 March, 2021

For the first time, an international team of scientists has used satellite magnetic data from ESA’s Swarm mission, together with aeromagnetic data, to help reveal the mysteries of the geology …


Do your PhD with British Antarctic Survey in 2021

25 November, 2020

Applications for PhD projects with British Antarctic Survey (BAS) are now open for October 2021 admission. There are currently over 100 PhD students associated with BAS, working on a huge variety …


Traces of rainforests found in West Antarctica

1 April, 2020

An international team of researchers has provided a new and unprecedented perspective on the climate history of Antarctica. From a sediment core collected from the seafloor in West Antarctica, they …


Discovery of rare lava lake on remote sub-Antarctic island

3 July, 2019

A team of scientists has discovered a rare lava lake on a remote and inaccessible sub-Antarctic island. This volcano in the South Sandwich Islands is only the 8th to be identified worldwide to have a persistent lava lake. 





New magnetic anomaly map helps unveil Antarctica

17 July, 2018

The most comprehensive magnetic map of Antarctica ever produced is published this week (15 July 2018). The new map – which includes 3.5 million line-kilometres of magnetic anomaly data collected …