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Fact check: Did the Mediterranean go dry and then flood 5.3 million years ago?

Checked on March 7, 2025

1. Summary of the results

Yes, scientific evidence strongly confirms that the Mediterranean Sea experienced a dramatic drying and flooding event known as the Messinian salinity crisis. The crisis began around 5.96 million years ago when the Mediterranean basin was cut off from the Atlantic Ocean [1]. The basin dried out within approximately 1,000 years, creating a deep depression 3-5 km below normal sea level [1]. The crisis ended dramatically with the Zanclean flood around 5.33 million years ago [1] [2] [2].

2. Missing context/alternative viewpoints

The original question omits several crucial details about this extraordinary event:

  • Scale and Speed of the Flood:
  • 90% of the basin flooded within several months to two years [2] [2]
  • Water levels rose at an astounding rate of up to 10 meters per day [2] [2]
  • This may have been the largest flood in planetary history [3]
  • Geographical Details:
  • The sea level dropped by 1.7-2.1 kilometers in the eastern Mediterranean and about 850 meters in the western sector [4]
  • The flood created a massive 200-km channel when the land bridge between Spain and Morocco was breached [3]
  • The Mediterranean lost up to 70% of its total water volume during the crisis [4]
  • Scientific Context:
  • The event involved complex interactions between tectonic settings, climate fluctuations, and sea-level changes [5]
  • Massive salt deposits formed during this period [5]

3. Potential misinformation/bias in the original statement

The original question oversimplifies what was actually a complex geological event. While there is scientific consensus about the fundamental occurrence of the crisis [6], ongoing debates continue about precise details [6]. The question's simple framing might lead readers to underestimate the extraordinary nature and complexity of this event, which involved multiple phases and geological processes over hundreds of thousands of years [5]. The event was not just a simple case of drying and flooding, but rather a complex crisis involving significant changes in water chemistry, geology, and regional climate patterns.

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