What archaeology says
Marine geologists agree the Black Sea was reconnected to the Mediterranean in the early Holocene, but the emerging consensus favours a more gradual and less apocalyptic process than the famous catastrophic model. In the 'outflow' and gradualist readings, championed by researchers such as Ali Aksu, Richard Hiscott and Valentina Yanko-Hombach, the transition was staged and in places two-way: fresh water may even have been flowing out through the Bosphorus while marine water worked its way in. Evidence cited includes back-stepping barrier islands and beach ridges on the Black Sea shelf, an underwater delta in the Marmara Sea near the strait, and microfossil and mollusc sequences showing a measured change in salinity rather than an overnight marine invasion.
On this view the sea level rose over centuries, perhaps rising a metre or so per year at most during the fastest phase, submerging coastlines steadily enough that people could retreat inland without a single drowning cataclysm. The reconnection is now generally placed somewhere in the window from about 6800 to 5600 BC, with the exact tempo still argued. Crucially, most specialists caution that even if the flooding was real and locally dramatic, tying it directly to a specific myth is speculative, since deluge stories appear independently across many cultures.
- Back-stepping barrier islands and beach ridges on the Black Sea shelf indicating a staged transgression
- An underwater delta in the Marmara Sea consistent with two-way flow through the Bosphorus (Aksu, Hiscott)
- Microfossil and mollusc sequences showing gradual rather than instantaneous salinity change
- Yanko-Hombach's synthesis of geological and archaeological data favouring a non-catastrophic model
- Submerged Bulgarian coastal settlements documenting slower, survivable coastline migration
