New evidence confirms presence of oceans on Earth 4 bln yrs ago

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Sydney, March 15 (ANI): A study of crystals found in Greenland has provided for new evidence of the theory that oceans covered the Earth four billion years ago.

According to a report by ABC Science, the Australian and Swedish researchers, led by geochronologist Dr Chris Kirkland, from the Western Australian Department of Mines and Petroleum, have found evidence from sandstones in the Morfneso Formation in North Greenland, which confirms the presence of oceans on the early Earth.

The researchers analysed the ratio of heavy to light isotopes of oxygen in zircons ranging from 900 to 3900 million 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 Dr Martin Van Kranendonk, also from the Department of Mines and Petroleum.

"Before we only had that data from one locality, now we have the same result literally from the other side of the world," he added.

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.

"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)," said Van Kranendonk.

"The volume of water must have been significant," he added.

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, according to the researchers.

Van Kranendonk said that the evidence points to a weaker, hotter crust sinking at a shallower angle into the underlying mantle.

The research 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," Van Kranendonk said. (ANI)

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