Underwater 'lost city' found to be geological formation

The ancient underwater remains of a long lost Greek city were actually created by a naturally occurring phenomenon, and not man-made, a new study has found.
When underwater divers discovered what looked like paved floors, courtyards and colonnades, they thought they had found the ruins of a long-forgotten civilisation that perished when tidal waves hit the shores of the Greek holiday island Zakynthos.
But new research uncovered that the site was created by a natural geological phenomenon that took place in the Pliocene era -- up to five million years ago.
"The site was discovered by snorkelers and first thought to be an ancient city port, lost to the sea. There were what superficially looked like circular column bases, and paved floors. But mysteriously no other signs of life - such as pottery," said Julian Andrews from University of East Anglia (UEA) in the UK.

Researchers from UEA and University of Athens in Greece investigated in detail the mineral content and texture of the underwater formation in minute detail, using microscopy, X-ray and stable isotope techniques.
"We investigated the site, which is between two and five metres under water, and found that it is actually a natural geologically occurring phenomenon," said Andrews.

"The disk and doughnut morphology, which looked a bit like circular column bases, is typical of mineralisation at hydrocarbon seeps - seen both in modern seafloor and palaeo settings," he said.
"We found that the linear distribution of these doughnut shaped concretions is likely the result of a sub-surface fault which has not fully ruptured the surface of the sea bed. The fault allowed gases, particularly methane, to escape from depth," he added.

Microbes in the sediment use the carbon in methane as fuel. Microbe-driven oxidation of the methane then changes the chemistry of the sediment forming a kind of natural cement, known to geologists as concretion, researchers said.
"In this case the cement was an unusual mineral called dolomite which rarely forms in seawater, but can be quite common in microbe-rich sediments," said Andrews.
"These concretions were then exhumed by erosion to be exposed on the seabed today. This kind of phenomenon is quite rare in shallow waters. Most similar discoveries tend to be many hundreds and often thousands of meters deep underwater," he said.

"These features are proof of natural methane seeping out of rock from hydrocarbon reservoirs. The same thing happens in the North Sea, and it is also similar to the effects of fracking, when humans essentially speed up or enhance the phenomena," he added.
The findings were published in the journal Marine and Petroleum Geology.