Around 7,600 years ago, the emergence of agricultural settlements in Southeastern Europe and subsequent progress of civilization suddenly came to a standstill. This was most likely caused by an abrupt sea level rise in the northern Aegean Sea.

Researchers of the Senckenberg Biodiversity and Climate Research Centre, the Goethe University in Frankfurt and the University of Toronto have now detected evidence of this oceanographic event and an earlier sudden sea-level rise in the fossils of tiny calcifying marine algae preserved in seafloor sediments in the Aegean Sea.

The impact of these events on historical societal development emphasizes the potential economic and social consequences of a future rise in sea levels due to global climate change, the researchers write in the study recently published in the journal Scientific Reports.

Originating in the Middle East, the Neolithic Age witnessed one of the most significant upheavals of civilization in human history: the transition from a culture of hunter-gatherers to an agricultural and sedentary lifestyle. During the Neolithic revolution, agricultural societies also began to spread toward Southeastern Europe. However, archeological digs show that the development of settlements temporarily declined about 7,600 years ago. Researchers from Frankfurt have now identified one of the likely causes for this.

"Approximately 7,600 years ago, the sea level must have risen abruptly in the Mediterranean regions bordering Southeastern Europe. The northern Aegean, the Marmara Sea and the Black Sea recorded an increase of more than one meter. This led to the flooding of low-lying coastal areas that would have been ideal areas for settlement", says lead author Professor Dr. Jens Herrle of the German Senckenberg Biodiversity and Climate Research Centre and Goethe University.

The new study is based on a sediment core from the ocean floor of the northern Aegean Sea, which allowed Herrle and his collaborators to reconstruct the level of salinity in this part of the Mediterranean between 11,000 and 5,000 years ago.

The ocean floor is richly abundant in tiny fossils of the calcified algae species Emiliania huxleyi. Viewed up-close under a scanning electron microscope, size changes in these algae preserved a signal of the level of salinity in the surface water of the Aegean during their lifetime.

"These calcifying algae evidence two rapid decreases in the salt content, at approximately 8,400 and again 7,600 years ago, which can only be explained by the fact that a higher volume of low-saline surface water flowed from the Black Sea into the northern Aegean at these times.

"A prerequisite for this is a rapid rise in sea levels that would lead to an increased outflow of surface water in this direction. The source of this may have been Lake Agassiz in North America. This glacial meltwater lake was enclosed in ice and experienced a massive breach during this period, which emptied an enormous volume of water into the ocean," explains Herrle.

The new evidence supports a conclusion of extensive flooding along the edges of the northeastern Mediterranean, coinciding with two standstills in the Neolithic revolution.

The earlier change in sea-level approximately 8,400 years ago highlighted by the new salinity record coincides with archeological dates suggesting that settlement on low-lying areas had already been significantly impeded by rising sea levels and the subsequent climatic changes. The renewed rise in sea levels 800 years later likely further hampered the transition to agricultural communities.

"Our results show that the timing and severity of past fluctuations in sea level has already had a significant effect on human history during its early agricultural development", explains Herrle in closing. "Due to climate change, we expect global sea levels to rise by up to one meter over the next 100 years. Millions of people could thus be displaced from coastal regions, with severe social and economic consequences."

Research paper

Related Links
Goethe University Frankfurt
All About Human Beings and How We Got To Be Here

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