GEOLOGIC TIME SCALE (GTS) - GEOGRAPHY

News: Anthropocene epoch declaration unlikely soon, but the idea lives on

 

What's in the news?

       Scientists recently proposed to formalise an ‘Anthropocene Epoch’ on the geologic time scale, triggering several debates.

       The earth’s geological history is divided into multiple epochs depending on their natural evolution.

 

Key takeaways:

       The SQS-AWG is a commission responsible for recognising time units within our most recent period of geologic time.

 

Geological Time Scale:

       Geological Time Scale (GTS) is a way to divide Earth’s history into different time intervals based on significant geological events and changes.

       It allows scientists to study and understand the Earth’s history and how it has evolved over time.

 

Eon:

       The largest time period of the GTS, represents billions of years.

       There are only four eons in Earth’s history: the Hadean, Archean, Proterozoic, and Phanerozoic.

 

Era:

       A division of an eon, representing tens to hundreds of millions of years.

       The Phanerozoic eon, which began about 541 million years ago, is divided into three eras: the Palaeozoic, Mesozoic, and Cenozoic.

 

Period:

       A division of an era, representing millions of years to tens of millions of years.

       For example, the Mesozoic era is divided into three periods: the Triassic, Jurassic, and Cretaceous.

 

Epoch:

       A division of a period, representing hundreds of thousands of years to tens of millions of years.

       The Cenozoic era is divided into three epochs: the Paleogene, Neogene, and Quaternary.

 

It’s worth noting that the boundaries between these subunits of the GTS are not always well-defined, and may vary depending on the region being studied.