What archaeology says
The investigation is a small model of how science should work. Because the visual resemblance to ruins was genuinely strong, the Greek authorities took the report seriously and put archaeologists in the water. What they found was suspicious in a different way: no ceramics, no amphora fragments, no anchors, no worked stone — nothing portable that every genuine ancient harbour site sheds in abundance. That absence triggered a mineralogical study led by Professor Julian Andrews of the University of East Anglia with Professor Michael Stamatakis of the University of Athens, published in 2016 in Marine and Petroleum Geology under a title that settled the matter: 'Exhumed hydrocarbon-seep authigenic carbonates from Zakynthos Island (Greece): Concretions, not archaeological remains'.
Microscopy, X-ray diffraction and stable isotope analysis showed the 'column bases' are made largely of dolomite — a mineral that rarely forms in normal seawater but is characteristic of microbe-rich, methane-charged sediments. The structures are the fossilised plumbing of hydrocarbon seeps: methane leaking up through a partially ruptured sub-seabed fault fed colonies of methane-oxidising microbes, whose chemistry cemented the surrounding sediment into concretions. Pipe-like conduits produced the 'columns', while broader cemented sheets became the 'pavements'; the linear arrangement that looked like town planning simply traces the fault. Later erosion exhumed the hard concretions from softer sediment, leaving them standing proud on the seabed like ruins. Similar seep concretions are well known from the North Sea and elsewhere — what is unusual at Zakynthos is that they formed in the Pliocene, up to five million years ago, and now sit in snorkelling depth where anyone can be fooled by them.
- Complete absence of pottery, coins, anchors or any artefact across the whole site despite shallow, clear water
- Dolomite mineralogy typical of microbial methane oxidation, not of any quarried building stone
- Stable isotope signatures showing carbon sourced from hydrocarbon seeps
- Alignment of concretions along a sub-seabed fault that channelled the escaping methane
- Peer-reviewed 2016 study by Andrews and Stamatakis in Marine and Petroleum Geology
