Did you know that the central Mediterranean Sea's surface temperatures have been fluctuating for millions of years? Scientists have reconstructed a detailed record of these temperature changes, known as sea surface temperatures (SSTs), using tiny sea creatures called G. ruber and their fossilized shells. This record spans a crucial time period called the Pliocene/Pleistocene transition, which marks the beginning of the Northern Hemisphere Glaciation.

By examining these fossils, researchers found that the temperature changes followed a specific pattern over time. The most noticeable pattern was a cycle that repeated every 47, 000 years, driven by the Earth's tilt, called obliquity. This cycle is responsible for the repeating glacial (cold) and interglacial (warm) periods we see in Earth's history.

But that's not all. There were also shorter, more frequent temperature fluctuations, occurring every 5, 000 and 8, 000 years. These quick changes were especially pronounced during a specific cold period known as Marine Isotope Stage 100. This instability could be due to abrupt disruptions in the Atlantic Ocean's current system, leading to the production of colder, less salty water. Or, it might be the result of distant climate influences, like those from the tropics, resonating in the Mediterranean region.

Even though the exact causes of these temperature shifts are still a mystery, one thing is clear: the central Mediterranean holds valuable clues for understanding our planet's past climate. It serves as a vital reference point for studying paleoclimatic changes in the Neogene and Quaternary periods.

Temperature Fluctuations in the Central Mediterranean: A Closer Look

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