Tick, tock goes the clock
The geologic time scale of Earth is almost unimaginable to us. This is because humans’ lifespans are so short in comparison than the entire lifespan of Earth.
- We work in hours, days, months and years.
- But the Earth works in hundreds of thousands and millions of years.
Geologists divide time into eons, eras, periods, epochs and ages (from longest to shortest). So that means that timing is everything when it comes to the geologic time scale.
How long is the geologic calendar?
Earth’s age is approximately 4.5 billion years so that’s why we use billions, millions and thousands of years as time markers. Typically, we use abbreviations like ‘Ga’ (giga-annum), ‘Ma’ (mega-annum), and ‘Ka’ (kilo-annum).
- ‘Ga’ or ‘Gya’ (billion) is 1,000,000,000 years ago
- ‘Ma’ or ‘Mya’ (million) is 1,000,000 years ago
- ‘Ka’ or ‘Kya’ (thousand) 1,000 years ago
For example, 2.5 Ga refers to 2.5 billion years ago. Because Earth is about 4.5 billion years old, we subdivide long chunks of time into eons, eras, periods, epochs and ages.
What are the units of geologic time?
Eons are the longest division of geologic time. Generally, we measure eons as billions of years ago (Ga) and millions of years ago (Ma). Geologists divide the lifespan of Earth into a total of 4 eons. From origin to now, Earth’s 4 eons are the Hadean, Archean, Proterozoic and Phanerozoic Eon. The Hadean, Archean and Proterozoic eons are sometimes grouped as the Precambrian Eon.
Eras are divisions of geologic time shorter than eons but longer than periods. In terms of geochronological units, there are 10 defined eras which generally span several hundred million years. For example, the Paleozoic, Mesozoic, and Cenozoic eras are within the Phanerozoic Eon.
There are 22 defined periods. Periods are divisions of geologic time longer than epochs but shorter than an era. Each period spans a length of tens to one hundred million years. Next, there are 34 defined epochs which generally last for tens of millions of years. The geologic time scale conceptually consists of periods that we break down into smaller epochs.
Epochs are then divided into ages, which are the shortest division of geologic time. In terms of the number of geochronological units, there are 99 defined which can stretch over millions of years. Epochs contain minor differences between each unit. Some geologists divide ages even further. If you do so, chrons are the smallest working geochronological unit. However, these are less common.
What’s an example of geologic time scale?
Let’s put what we know into practice. The Triassic period lasted about 50 million years and has a well-defined start and endpoint. Both the start and end concluded with catastrophic mass extinctions.
If you look at the table above, you can see that the Triassic Period is part of the Mesozoic Era and Phanerozoic Eon. The Triassic period has 3 epochs and 7 ages. Each of these shorter divisions of time identify a notable event or characteristic feature based on their record.
The Triassic period started 252 million years ago after Earth’s largest extinction event in history. It’s also known as the “Great Dying” because it killed 96% of all marine species and an estimated 70% of land species. Then, it had an abrupt ending in 201.3 mya during a less severe Triassic–Jurassic extinction event.
Who is the International Commission of Stratigraphy (ICS)?
The International Chronostratigraphic Graph is like a giant directory of geologic time units. From signatures inherent in rocks, geologists can estimate the true age of the earth. By tracing back on embedded fossilized organisms in rock strata, we can achieve a context of time.
Because we can date rocks through stratigraphy, we can achieve a better understanding of geological events in Earth’s history. Based on our geological time scale, we can better understand the theory of evolution and origin of life on our planet.
An overview of geologic time
Tick, tock fellow geologists. Now, you have a good understanding that time is foundation if geology.
Also, you have a good background in how to break up time into geological units.
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