Quaternary (Cenozoic 3)

Cenozoic Era 3: Quaternary PeriodA Cycle of Ice Ages

Key Events

  • We are living in the Quaternary Period.
  • Glaciation comes and goes in cycles. We are currently in an ‘interglacial’ period, with glaciers remaining at the north and south poles and in some mountain regions.•Past glacial cycles have taken place over tens or hundreds of thousands of years. 
  • The last glacial period ended ~11,700 years ago. Many large mammals, like the mammoth and sabre-tooth tiger became extinct. 
  • Modern humans evolved ~200,000 years ago. They co-existed with other human species until ~40,000 years ago.
  • Human-induced emissions of ‘greenhouse’ gases are contributing to a warming of the atmosphere at a global scale and appear to be causing large-scale shifts in weather patterns. 
  • While there have been periods of drastic change throughout Earth’s history, the current large human population means that many people suffer the impacts of today’s climate change.
Illustration of life during the Quaternary Period.
Illustration of life during the Quaternary Period. Copyright: Vix Southgate

Facts, Debates & Trivia

  • The Quaternary’s name comes from an outdated classification system for geological time. The terms Primary, Secondary and Tertiary are no longer used, but the Quaternary’s name stuck.
  • The causes of the cycles of glaciation are complicated and include climate system interactions, variations in Earth’s orbit, volcanism and solar activity.

Conditions

  • The climate experiences large-scale temperature fluctuations and associated sea level changes.
The Earth today. The red dot marks the location of Cornwall. Credit: C.R. Scotese/I. Webster

Timeline

2.58  million years ago – present day  

(2.58 million years)

1 metre = 10 million years

Where have you reached on the trail?

Each sign in the Earth Story trail comes with a shelf that can be used to hold rock samples to illustrate the geology of the eon, era or geological period described.
Each sign in the Earth Story trail comes with a shelf that can be used to hold rock samples to illustrate the geology of the eon, era or geological period described. Credit: A Heward/Cornwall Sea to Stars