The piece of crust, which was subsequently covered by young lava during volcanic eruptions on the island, seems to be a tiny piece of ancient continent, which broke off from the island of Madagascar, when Africa, India, Australia and Antarctica split up and formed the Indian Ocean.
"We are studying the break-up process of the continents, in order to understand the geological history of the planet," said Professor Lewis Ashwal from University of the Witwatersrand in South Africa.
"Earth is made up of two parts - continents, which are old, and oceans, which are "young". On the continents you find rocks that are over four billion years old, but you find nothing like that in the oceans, as this is where new rocks are formed," said Ashwal.
"Mauritius is an island, and there is no rock older than nine million years old on the island. However, by studying the rocks on the island, we have found zircons that are as old as three billion years," he said.
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"The fact that we have found zircons of this age proves that there are much older crustal materials under Mauritius that could only have originated from a continent," said Ashwal.
This is not the first time that zircons that are billions of years old have been found on the island. A study done in 2013 has found traces of the mineral in beach sand.
"The fact that we found the ancient zircons in rock (six-million-year-old trachyte), corroborates the previous study and refutes any suggestion of wind-blown, wave-transported or pumice-rafted zircons for explaining the earlier results," said Ashwal.
Ashwal suggests that there are many pieces of various sizes of "undiscovered continent", collectively called "Mauritia", spread over the Indian Ocean, left over by the breakup of Gondwanaland.
"According to the new results, this break-up did not involve a simple splitting of the ancient super-continent of Gondwana, but rather, a complex splintering took place with fragments of continental crust of variable sizes left adrift within the evolving Indian Ocean basin," Ashwal added.