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Everything You Need to Know About the Eras and Eons That Shaped Life on Earth

Lou Farrell By Lou Farrell
about a 6 MIN READ 1 view
an artist interpretation of the timeline of life on earth

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While the Earth may feel like it has not changed much in the last generation or so, this is a relatively short time frame compared to the length of time it has been around. The timeline of life on Earth is extensive, dating back billions of years, when this floating rock in the middle of space would be barely recognizable.

Centuries of researchers have explored rocks, fossils and geography to determine how the modern world came to be.

What Is an Eon Versus an Era?

To begin understanding the timeline of life on Earth, people must first understand the scope and scale of the terminology used. An eon is the largest unit of measurement researchers have to describe the times of ancient Earth. This is usually represented in billions of years. An era is much smaller, typically measured in the hundreds of millions of years.

An eon will sometimes contain multiple eras under its umbrella. If curious minds continue to zoom into this hierarchy of Earth’s history, they can dive into more specific time-based markers, such as periods, epochs and ages, which detail more specific and nuanced times in history.

The Precambrian Supereon

Around 90% of known geologic time occurred during this period, which spanned 3.9 billion years. Also known as the Age of Early Life, the Precambrian period comprises several eons. It is the foundational timeline of life for countless species.

The Hadean Eon

The name of this eon may sound familiar because it evokes the fire and heat of Hades’s underworld. This moniker reflects the planet’s birth, when it was merely a collection of rocks, dust and gases in the middle of space. During this time, which was over four billion years ago, Earth was constantly pelted with rogue asteroids and other space objects. It is one of the most mysterious times in Earth’s history. The temperatures were so extreme that little remains from this time.

At this stage, nothing could live on Earth. It underwent constant change until it could eventually support it. In the meantime, everything from the core to the crust was being created, though it was unstable. The Hadean Eon also witnessed the creation of Earth’s moon, forged in a collision that catapulted a large chunk of rock into orbit. Eventually, the planet slowly lost heat and cooled off, creating water from the condensed vapors.

Archean Eon

The Archean Eon lasted around 1.5 billion years, signifying the first step toward permanent life. However, these living things looked very different from what they do now.

These prokaryotic lifeforms were incredibly simple, consisting of a single cell. They lacked a nucleus and reproduced in hot spots such as hydrothermal vents on the ocean floor. This was still a time when oxygen was scarce, and these organisms could survive without it.

Cyanobacteria were part of this group, and their livelihood depended on photosynthesis. As cyanobacteria populations increased, oxygen availability also boosted as a by-product of converting light into energy.

These creatures also left the earliest recorded fossils, which are called stromatolites. All these microorganisms changed the world. Oceans that were once green with iron began to transform. This is the true start to the timeline of life.

Proterozoic Eon

The Proterozoic Eon lasted about two billion years and is characterized primarily by the rise in atmospheric oxygen, which supported even more diverse life. While oxygen is essential for human life, too much of it can be toxic. The cyanobacteria were too productive and made an atmosphere that catalyzed a mass extinction known as the Great Oxidation Event.

Researchers were able to validate the presence of this much oxygen because of red beds, densely packed red sandstone rich in iron oxide. With this much oxygen, anything wanting to thrive on the planet would have to adapt, especially because of the temperature extremes throughout these years. Many glacial deposits prove there were Ice Ages during the Proterozoic that would have stressed any living species.

There were also massive continental shifts during this time. This eon was the earliest evidence of plate tectonics and mountain-building, as revealed by rock analyses from this time. Other common structures were shallow-water rocks on stable continental shelves, which meant the continents were more solidly taking shape.

However, there are still many details researchers need to uncover, including whether or not the Earth’s plates move in the same way now as they did during the Proterozoic eon.

The Phanerozoic Eon

All life on Earth presently exists in the Phanerozoic Eon, which comprises several eras. It has lasted over 500 million years and began with a notable explosive event.

Paleozoic Era

This era started around 540 million years ago and lasted around 300 million years. It began with the Cambrian Explosion, and life on Earth began moving from the ocean to the land. Creatures began taking more substantial shapes, as fossil records would dictate.

The Paleozoic Era was a period of flux. Everything, including living things, the land and waters, was all moving and shifting. While the ocean was still full of life, including lush seafloor communities and vertebrates emerged alongside new plant life. It did not take long for them to spread, leading to the proliferation of many animals known today, such as insects and amphibians.

The flourishing beauty of the Paleozoic Era would end in one of the most thorough extinction events. The Permian-Triassic extinction — also called The Great Dying — wiped out almost all land and aquatic life. The next era would have to start nearly from scratch.

Mesozoic Era

Another 200 million years pass, representing the Age of Reptiles. During the Mesozoic, the dinosaurs appeared and ruled over the lands and skies.

While seemingly uniform, dinosaurs were diverse, from tame herbivores to intense apex predators. Larger-than-life creatures, like the plesiosaurs, dominated the seas.

As the era progressed, Pangaea began to split into the continents people recognize today due to plate tectonics.  While this led to greater separation of life, it also fostered the evolution of more diverse species in new parts of the world, including flowering plants.

However, a massive asteroid crashed into Earth about 66 million years ago. Its impact was so powerful that it wiped out all dinosaurs and the majority of other species with them.

Cenozoic Era

The Cenozoic Era began over 60 million years ago and is the one in which all living things currently reside. Long gone are the days of the reptile and water-based life. This is the time for mammals to shine, though several Ice Ages threatened their permanence.

Without the towering dinosaurs, mammals were able to reproduce rather freely, leading to what many call the Age of Mammals, though it was more diverse than this. They were versatile and adapted to diverse environments across the planet, even as they grew increasingly distinct from one another. Grazing animals thrived in the grasslands, and primates learned to walk upright in Africa.

Eventually, early hominins advanced. Their brains grew bigger, they invented tools and discovered fire. Their capabilities were seemingly unmatched until homo sapiens came about.

The advent of homo sapiens has created an Earth unlike any era preceding. It is full of innovation, technology and surprises. Whatever happens over the next 100 million years is uncertain, but the Cenozoic Era will be remembered for the diversity and evolution of mammal species.

Precambrian Eon

Precambrian Eon

The Lives and Times of Planet Earth

The separation between eons and eras feels dramatic, with explosions and mass extinctions marking pivotal moments in life’s history. It makes everyone curious about what the next big event will be that marks the end of the Phanerozoic Eon and the beginning of what comes after.

Fortunately, for the curious minds educating themselves on these subjects in the modern age, the next eon will be so far in the distant future that you won't have to worry about it.

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