Wikiwand AI

Tortonian Thermal Maximum

Neogene climate event From Wikipedia, the free encyclopedia

The Tortonian Thermal Maximum (TTM) was an interval of relatively warm global climate that occurred during the Tortonian age of the Neogene period.

Timing

The TTM occurred around 10.8 million years ago, during the early part of the Tortonian.[1]

Effects

Global mean surface temperature was around 61.5 °F (16.4 °C) (16.4 °C) during the TTM.[2] Lake Pannon, the largest lake in Europe, experienced enhanced nutrient inputs that caused blooms of nannoplankton.[3] Potamidids experienced an expansion in their geographic range, with them entering the Paratethys from the Mediterranean Sea.[4]

References

Related Articles

Timelines

Top Qs

Fact Checks