An extended drought after the destruction of Nestor’s Palace in Pylos is likely to have brought an end to the Mycenaean civilization in the western Peloponnese. That conclusion was reached following analysis of a stalactite from a cave in the area that provided a clear picture about the climatic conditions in the eastern Mediterranean in the Late Bronze Age.
The researchers reached their conclusions from the analysis of a stalactite from a cave on the islet of Schiza just off the Peloponnesian coast [Credit: Navarino Environmental Observatory] |
The researchers drew their conclusions from the analysis of a stalactite from a cave on the islet of Schiza just off the Peloponnesian coast. By studying the layers of the stalactite, the team was able to establish the climatic conditions that existed in the region from around 1200 to 1180 BC with a high degree of precision.
“Evidently the centralized administrative system controlled by the palace could survive a relatively short-term dry period and remain in control. Some 50 years later, however, when the pronounced period of aridity started to develop, the system would crumble,” the researchers write in their paper presenting their results.
The researchers argue that the long drought following the palace’s destruction led to the end of the “Mycenaean way of life in Pylos,” as agricultural surpluses were eliminated, thus making it difficult “for social elites to re-form and for the palatial system to be re-established.”
While they note that the collapse of the Mycenaean civilization cannot be attributed to one single factor, the researchers conclude that climate change was certainly a “critical component.”
Author: Giorgos Lialios | Source: Kathimerini [May 17, 2018]