Antarctica’s magnetic link to ancient neighbours

British Antarctic Survey

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 hidden beneath Antarctica’s thick ice sheets and link Antarctica better to its former neighbours.

Not only is Antarctic sub-ice geology important to understand global supercontinent cycles over billions of years that have shaped Earth’s evolution, it is also pivotal to comprehend how the solid Earth itself influences the Antarctic ice sheet above it.

The research team from Germany’s Kiel University, British Antarctic Survey and National Institute of Oceanography and Applied Geophysics, and Witwatersrand University in South Africa has recently published their findings in the Nature journal Scientific Reports.

Map
Magnetic data links Antarctica to its ancient neighbours. Credit_University of Kiel.

Their new study shows that satellite and aeromagnetic data combined together provide a key missing link to connect Antarctica’s hidden geology with formerly adjacent continents, namely Australia, India and South Africa that formed keystones of a continent called Gondwana.

The fact that Antarctica is about as remote as you can get and the land below is covered by a massive ice sheet, makes collecting geophysical information both challenging and expensive.

Thanks to magnetic data from the Swarm mission, along with airborne measurements, scientists are able to link Antarctica to its ancient neighbours with which it has shared a long tectonic history that needs piecing together like a jigsaw puzzle.

A satellite in space
Swarm constellation

The team processed aeromagnetic data from aircraft from over Southern Africa, Australia and Antarctica in a consistent manner with the help of Swarm satellite magnetic data.

Aeromagnetic data do not cover everywhere on Earth, so magnetic models complied from Swarm data help to fill the blanks, especially over India were aeromagnetic data are still not widely available. Furthermore, satellite data help to homogenise the airborne data, which were acquired over a period of more than 60 years and with varying accuracy and resolution.

Lead author Jörg Ebbing, from Kiel University, explains:

“With the available data, we only had pieces of the puzzle. Only when we put them together with satellite magnetic data, we can see the full picture.” The resulting combined datasets provide a new tool for the international scientific community to study the cryptic sub-ice geology of Antarctica, including its influence on the overlying ice sheets.”

Gondwana was an amalgam of continents that incorporated South America, Africa, Arabia, Madagascar, India, Australia, New Zealand and Antarctica. As the tectonic plates collided in the Precambrian and early Cambrian times (some 600-500 million years ago), they built huge mountain ranges comparable to the modern Himalayas and Alps. This supercontinent started to breakup in the Early Jurassic, about 180 million years ago, ultimately leaving Antarctica stranded and isolated at the South Pole, and covered in ice for around 34 million years.

Using the new magnetic data, the animation illustrates how the tectonic plates have moved over millions of years after the breakup of Gondwana.

Fausto Ferraccioli, Director of Geophysics at the National Institute of Oceanography and Applied Geophysics in Italy, and also affiliated with the British Antarctic Survey, says:

“We have been trying to piece together the connections between Antarctica and other continents for decades. We knew that magnetic data play a pivotal role, because one can peer beneath the thick Antarctic ice sheets to help extrapolate the geology exposed along the coast into the continent interior.

“But now we can do much better. With the satellite and aeromagnetic data combined, we can look down deeper into the crust. Together with plate reconstructions, we can start building tantalising new magnetic views of the crust to help connect geological and geophysical studies in widely separated continents. Ancient cratons and orogens in Africa, India, Australia and East Antarctica are now better connected magnetically than ever before”.

ESA’s Roger Haagmans, says:

“This research has been carried out within ESA’s Science for Society 3D Earth study where we are using gravity data from the GOCE mission and magnetic data from the Swam mission to understand the structure and dynamic processes deep within Earth. In this instance, Swarm’s magnetic data have played a starring role.

East Antarctica magnetically linked to its ancient neighbours in Gondwana by

Jörg Ebbing1*, Yixiati Dilixiati1, Peter Haas1, Fausto Ferraccioli2,3 &

Stephanie Scheiber‑Enslin4 is published in the journal Scientific reports here

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