Middle MioceneNeogene PeriodLanghian stageSerravallian stageMiddle Miocene Climatic Transition

Middle Miocene: A Critical Transition in Earth's Geological History

Middle Miocene: A Critical Transition in Earth's Geological History The Middle Miocene represents a pivotal sub-epoch within the Miocene epoch, serving as a bridge between the Early and L...

Middle Miocene: A Critical Transition in Earth's Geological History

The Middle Miocene represents a pivotal sub-epoch within the Miocene epoch, serving as a bridge between the Early and Late Miocene. As part of the broader Neogene Period, this era is characterized by significant geological shifts and a dramatic transformation in the Earth's climate that reshaped global ecosystems.

The Chronology of the Middle Miocene

According to the International Commission on Stratigraphy (ICS), the Middle Miocene spanned from approximately 15.97 ± 0.05 million years ago (Ma) to 11.608 ± 0.005 Ma. In the context of European land mammal ages, this specific sub-epoch is equivalent to the Astaracian age.

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Stratigraphic Subdivisions

The Middle Miocene is divided into two distinct stages, which allow geologists to categorize rock layers and fossils with precision:

  • Langhian: The earlier stage of the sub-epoch.
  • Serravallian: The subsequent stage that leads into the Late Miocene.

The Middle Miocene Climatic Transition

One of the most defining characteristics of this period was the Middle Miocene Climatic Transition. This event was marked by a sharp drop in global temperatures, moving the planet away from the warmer conditions of the Early Miocene and setting the stage for the cooling trends seen in later epochs.

Geological Context and Timeline

To understand where the Middle Miocene fits into the larger history of the Earth, it is helpful to view it within the hierarchy of the Neogene and Quaternary periods. The Neogene is characterized by a progression of epochs including the Miocene and Pliocene, eventually leading into the Quaternary period.

Subdivisions of the Neogene Period (ICS 2017)
Epoch Stage Age (Ma) - Older Limit Age (Ma) - Younger Limit
Miocene Messinian 7.246 5.333
Tortonian 11.63 7.246
Serravallian 13.82 11.63
Langhian 15.97 13.82
Burdigalian 20.44 15.97
Aquitanian 23.03 20.44

Key Facts

  • Timeframe: Lasted from 15.97 ± 0.05 Ma to 11.608 ± 0.005 Ma.
  • Composition: Comprised of the Langhian and Serravallian stages.
  • Climate Event: Defined by the Middle Miocene Climatic Transition (a sharp temperature drop).
  • Mammalian Age: Equivalent to the Astaracian age for European land mammals.
  • Position: Situated between the Early Miocene and the Late Miocene.

Frequently Asked Questions

What is the Middle Miocene?

The Middle Miocene is a sub-epoch of the Miocene epoch, occurring within the Neogene Period. It is defined by the Langhian and Serravallian stages.

When did the Middle Miocene occur?

It lasted from approximately 15.97 million years ago to 11.608 million years ago.

What was the Middle Miocene Climatic Transition?

It was a geological event during the Middle Miocene characterized by a sharp and significant decrease in global temperatures.

Which stages make up the Middle Miocene?

The Middle Miocene consists of two stages: the Langhian stage and the Serravallian stage.

How does the Middle Miocene relate to mammal ages?

For the purpose of establishing European land mammal ages, the Middle Miocene sub-epoch is equivalent to the Astaracian age.

References

  1. "ICS Timescale Chart". stratigraphy.org.