Rodinia: Fragments of ancient continent buried beneath Indian Ocean

A new study suggests that fragments of an ancient continent called Rodinia are buried beneath the floor of the Indian Ocean.

Researchers have found evidence for a landmass that would have existed between 2,000 and 85 million years ago.

The strip of land, which scientists have called Mauritia, eventually fragmented and vanished beneath the waves as the modern world started to take shape.

The study is published in the journal Nature Geoscience.

Until about 750 million years ago, the Earth’s landmass was gathered into a vast single continent called Rodinia.

And although they are now separated by thousands of kilometres of ocean, India was once located next to Madagascar.

Now researchers believe they have found evidence of a sliver of continent – known as a microcontinent – that was once tucked between the two.

The team came to this conclusion after studying grains of sand from the beaches of Mauritius.

While the grains dated back to a volcanic eruption that happened about nine million years ago, they contained minerals that were much older.

Professor Trond Torsvik, from the University of Oslo, Norway, said: “We found zircons that we extracted from the beach sands, and these are something you typically find in a continental crust. They are very old in age.”

The zircon dated to between 1,970 and 600 million years ago, and the team concluded that they were remnants of ancient land that had been dragged up to the surface of the island during a volcanic eruption.

A new study suggests that fragments of an ancient continent called Rodinia are buried beneath the floor of the Indian Ocean

Prof. Trond Torsvik said that he believed pieces of Mauritia could be found about 10 km down beneath Mauritius and under a swathe of the Indian Ocean.

It would have spanned millions years of history, from the Precambrian Era when land was barren and devoid of life to the age when dinosaurs roamed the Earth.

But about 85 million years ago, as India started to drift away from Madagascar towards its current location, the microcontinent would have broken up, eventually disappearing beneath the waves.

However, a small part could have survived.

“At the moment the Seychelles is a piece of granite, or continental crust, which is sitting practically in the middle of the Indian Ocean,” explained Prof. Trond Torsvik.

“But once upon a time, it was sitting north of Madagascar. And what we are saying is that maybe this was much bigger, and there are many of these continental fragments that are spread around in the ocean.”

Further research is needed to fully investigate what remains of this lost region.

Prof. Trond Torsvik explained: “We need seismic data which can image the structure… this would be the ultimate proof. Or you can drill deep, but that would cost a lot of money.”