A study of arctic crystals found in Greenland has given a boost to the theory that the earth was covered by oceans as far back as four billion years ago.

The research by Australian and Swedish geochronologists also sheds light on the processes that formed the continents and crust in the Archaen Era between 2.5 and four billion years ago.

Scientists believe because of weathering and recycling of the earth’s crust by subduction into the mantle, most of the rocks of that era have been lost. However, clues are preserved in the ancient isotopic signatures of chemicals in crystals called zircons, said the researchers.

They found the evidence from sandstones in the Moraeneso Formation in North Greenland, which confirms the presence of oceans on the early earth, the CBS News reported.

The researchers, led by Chris Kirkland from the Western Australian Department of Mines and Petroleum, analysed the ratio of heavy to light isotopes of oxygen in zircons ranging from 900 million to 3.9 billion years old. They compared this isotopic ratio to the current average isotopic ratio of oceans called the “standard mean ocean water“.

“The nice thing is there is one grain that confirms the Jack Hills results and that is really critical in science,” said study co-author Martin Van Kranendonk, also from the Department of Mines and Petroleum.

A research on zircons from Jack Hills in Western Australia in 2005 had first suggested the existence of an ocean four billion years ago.

“Before we only had that data from one locality, now we have the same result literally from the other side of the world,” said Van Kranendonk.

The isotopic composition of this grain shows that it must have been altered by low temperature, near surface conditions, which points to weathering by liquid water, he said.

“Rain is probably not enough to give this sort of a signature because we are dealing with large areas of exposed rocks and they have been significantly altered (by weathering).

“The volume of water must have been significant.”

Since subduction is needed to drag water into the crust, the finding also confirms that plate tectonics — the cycling of the Earth’s crust — was happening at this time, albeit in a different way, said the researchers.

According to them, the evidence points to a weaker, hotter crust sinking at a shallower angle into the underlying mantle.

The research, published in the current issue of the journal Lithosphere, also confirms a suspected shift in the composition of the Earth’s crust 2.5 billion years ago.

“We think this oxygen isotope value shows changes in the style of continental crust, and reflects the continents getting stiffer,” added Van Kranendonk.

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