That Time Oxygen Almost Killed Everything

Summary

"That Time Oxygen Almost Killed Everything" by PBS Eons explores a paradoxical moment in Earth's history when an overabundance of oxygen nearly wiped out all life. Starting 3 billion years ago in the Archaean Eon, Earth's oceans were filled with iron, rendering them green. Around 2.3 billion years ago, photosynthetic bacteria began producing oxygen, altering the planet's chemical balance and wiping out anaerobic life. Oxygen began accumulating in the atmosphere, reacting with greenhouse gases, and ushering in Earth's first major ice ages, including the 300-million-year Huronian glaciation. This event, known as the Oxygen Catastrophe, drastically changed climate and threatened life, but it eventually led to a more hospitable planet, paving the way for complex life and the formation of an ozone layer. Thus, while oxygen initially posed a threat, it ultimately facilitated the thriving of new life on Earth.

Highlights

• Oceans were once green due to iron, not algae! 🟢
• Photosynthetic bacteria's oxygen changed the planet's chemical balance. ⚛️
• Oxygen led to red oceans filled with iron oxide – rust! 🛤️
• Greenhouse gas reduction caused dramatic cooling and ice ages. ❄️
• The Huronian glaciation lasted 300 million years! ⏳
• An ozone layer formed, setting the stage for diverse new life. 🌞

Key Takeaways

• Oxygen almost wiped out life 2.3 billion years ago, changing the Earth dramatically! 🌍
• Photosynthetic bacteria farted out oxygen, altering the biosphere! 🦠
• Oxygen accumulation led to Earth's first major ice ages. 🧊
• Despite its dangers, oxygen eventually enabled more complex life. 🌿
• The event is known as the Great Oxygen Catastrophe! 🌀

Overview

Turn back the clock to 3 billion years ago in the Archaean Eon, where Earth was a foreign planet with mostly iron-swamped, green oceans and very little dry land. At this time, our atmosphere was low on oxygen—a good thing for the anaerobic life thriving then! 🚀 But things took a wild turn when photosynthetic bacteria started pumping oxygen into the mix, setting off a series of jaw-dropping events known as the Great Oxygen Catastrophe. 😮

As these bacteria filled the seas and air with oxygen, the very fabric of Earth started to unravel in a chemical dance. Oxygen reacted with iron, turning green seas to red with rust! 🌊 Oops! With the increase in atmospheric oxygen, anaerobic species hit the ropes, and Earth's climate shifted to icy extremes in epic ice ages known as the Huronian glaciation. Our comfy ocean world turned into a global popsicle! 🧊🍦

Surprise! While this might sound like all gloom, the aftermath of the Oxygen Catastrophe set the stage for a brand new world. 🌎 The leftover life adapted to an oxygen-rich atmosphere and benefited from an ozone shield against solar radiation. This allowed life to diversify and thrive like never before. So, from chaos to creation, oxygen didn't just threaten life—ironically, it nurtured it for us to marvel at today! 🌿

Chapters

• 00:00 - 00:30: Introduction to Oxygen's Impact In the introduction to the chapter on "Oxygen's Impact," the narrator opens with a rhetorical question, suggesting that everyone views oxygen positively, but hints at a surprising twist—oxygen once threatened all life on Earth. The chapter begins in the Archaean Eon, more than 3 billion years ago, describing an unrecognizable Earth with only 2-3% dry land. This sets the stage for discussing how excess oxygen, while essential for life as we know it, posed a significant danger.
• 00:30 - 01:00: Archaean Eon and Ocean Composition During the Archaean Eon, the Earth's surface was mostly covered by oceans rich in iron. These iron-laden waters gave the oceans a green hue, not due to algae, but because of green rust. This phenomenon occurred because the environment was low in oxygen, allowing iron to react with hydroxides, sulfur, and chlorine, resulting in widespread green rust in the oceans.
• 01:00 - 01:30: Rise of Photosynthesizers The chapter titled 'Rise of Photosynthesizers' discusses the Earth's atmosphere billions of years ago, which was primarily composed of nitrogen, water vapor, carbon dioxide, and methane, with very little oxygen. At that time, life on Earth was mainly anaerobic. Around 2.3 billion years ago, photosynthesizers emerged, including bacteria like cyanobacteria and possibly halobacteria, which utilized sunlight to convert carbon dioxide and water into food, thus contributing to the gradual increase of oxygen in the atmosphere.
• 01:30 - 02:00: Oxygen's Effects on the Oceans The chapter 'Oxygen's Effects on the Oceans' discusses how microbes began producing oxygen as waste, significantly altering the chemical balance of the biosphere. This process affected the oceans by causing the oxygen to react with iron, changing the ocean's color from green to red due to the formation of iron oxide, or rust, over approximately 200 million years.
• 02:00 - 02:30: Oxygen Enters the Atmosphere This chapter discusses the emergence of oxygen in Earth's atmosphere, marked by Banded Iron Formations. As oxygen levels increased, they caused significant environmental changes, including the reduction of anaerobic microbes and the spread of photosynthetic life. These shifts marked a pivotal transformation in the composition of both the ocean and the atmosphere.
• 02:30 - 03:30: Huronian Glaciation and Extinction During the Huronian Glaciation, large amounts of free oxygen began accumulating in Earth's atmosphere for the first time, drastically changing the climate. The spread of photosynthetic bacteria contributed to the reduction of carbon dioxide, a greenhouse gas, leading to a drop in global temperatures. Additionally, oxygen reacted with atmospheric methane, further influencing climate conditions.
• 03:30 - 04:30: Survival and New Opportunities The chapter, 'Survival and New Opportunities', discusses a period in Earth's history when greenhouse gases were significantly reduced, leading to the planet's first major ice ages. These drastic temperature drops triggered global glaciation, with the most significant event being the Huronian glaciation, which lasted 300 million years. These changes in climate and Earth's chemistry nearly caused the extinction of most life forms on the planet.
• 04:30 - 06:00: Closing and Sponsor Message The chapter discusses the historical phenomenon known as the Oxygen Catastrophe, where photosynthetic bacteria that produced oxygen also required carbon dioxide to survive. The accumulation of their 'waste' oxygen eventually led to their own extinction, highlighting a major extinction event in history.

That Time Oxygen Almost Killed Everything Transcription

• 00:00 - 00:30 This episode is supported by Squarespace. Are you like me? Do you think oxygen is … pretty great? Of course you do! But what if I told you that there was a time when oxygen almost wiped out all life on Earth? This is a story about how too much of a good thing can ruin everything for everybody. Let’s start 3 billion years ago, in the Archaean Eon, when the world was a place you’d never recognize. Or … even be able to survive in. Back then, only 2 or 3% of the planet’s surface was dry land.
• 00:30 - 01:00 The rest was covered in oceans, and … they were chock full of iron. Because of all that iron, the oceans were probably not blue, but green -- and not because of algae or other life, but because of rust. You might think of rust as being brown, but green rust is a thing too! It forms where there’s a lack of oxygen, and back in the Archaean, oxygen was in short supply everywhere. So in the oceans, iron reacted with hydroxides and elements like sulfur and chlorine, covering much of the world in green rust.
• 01:00 - 01:30 Above the green oceans, the atmosphere was mostly nitrogen -- as it is today -- along with water vapor, carbon dioxide, and methane. But, again, very little oxygen. Which was fine at the time, because microscopic life on Earth back then was probably anaerobic. Then about 2.3 billion years ago, some new kids showed up: Photosynthesizers. But not the kind that we're used to These were bacteria, like the familiar blue-green cyanobacteria, or maybe even a kind of purple microbe known as halobacteria. Either way, they used the Sun’s energy to convert CO2 and water into food -- releasing
• 01:30 - 02:00 oxygen as waste. Which was ... ok … for a while. But not for long. Because when these little microbes started farting out oxygen, it changed the chemical balance of the entire biosphere and, eventually, altered the face of our planet. First, within about 200 million years, the oxygen from these new bacteria began reacting with the iron in the oceans. This turned the oceans from a mellow green to a deep blood-red, as the seas began to fill with iron oxide -- what we know as rust.
• 02:00 - 02:30 In fact, you can still see exactly when and where this happened, in strata known as Banded Iron Formations, where huge swaths of rust settled out of oceans to form layers of red-brown rock. But beyond making water rusty, rising oxygen levels also shifted the balance of power among living things. Anaerobic microbes started to die off, as they were basically poisoned by the oxygen. Meanwhile, the newer, more efficient, photosynthetic life began to spread. And things changed even more when the oxygen in the ocean left the water … and entered
• 02:30 - 03:00 the air. For the first time in Earth’s history, large amounts of free oxygen started building up in the atmosphere. And this is what scientists call a game-changer. Because then, the climate started to change too. Drastically. As the photosynthetic bacteria kept spreading, they used up more and more of the carbon dioxide in the atmosphere. And CO2 is a greenhouse gas, so as its levels went down, so did the temperature. On top of that, oxygen also started reacting with the methane in the atmosphere, taking
• 03:00 - 03:30 it out of circulation. With greenhouse gases at an all-time low, our planet started to see the first major ice ages in its history. Temperatures dropped so drastically that it triggered a global glaciation, and our once balmy waterworld became shrouded in ice. There may have been several pulses of these icy events, but by far the biggest of them came to be known as the Huronian glaciation -- and it lasted for 300 million years. Between these huge changes in the climate, and the radically different chemistry of the planet, most life on Earth was pushed to the brink of extinction.
• 03:30 - 04:00 And this included the new guys -- the photosynthetic bacteria that were pumping out all the oxygen in the first place! Because, remember, they needed CO2 to survive. So they were basically being suffocated by their own waste, which … when I say that out loud, that’s just gotta be a terrible way to go. We don’t know the full extent of the damage. But the effects of this whole episode -- sometimes called the Oxygen Catastrophe -- is considered one of the biggest extinction events in history. But, you know how this movie ends, right?
• 04:00 - 04:30 By the time the Huronian glacial period ended, about 2.1 billion years ago, some life remained. And the life-forms that survived inherited a better, more hospitable planet. Oxygen was now abundant in the air and water, and a new thing also appeared in the atmosphere: an ozone layer. This coating of molecular oxygen helped block dangerous ultraviolet radiation from the sun, and suddenly new things became possible. From there, well, you know what happens. Life became more complex and awesome and wonderful, and here we are.
• 04:30 - 05:00 It seems strange that bacteria could end up covering the whole world in ice. And who’da thought oxygen would be responsible for wiping out … almost everybody? But it just goes to show you that, sometimes, things gotta get worse before they get better. I want to thank our friends at Squarespace for supporting this episode. Whether you need a domain, a website or an online store, Squarespace can make it happen. And don’t you need a place to blog about whether T. rex had feathers? Of course you do!
• 05:00 - 05:30 Well, Squarespace gives you an all-in-one platform – with templates that let you set up a website with ease. There’s nothing to install, patch or upgrade, ever. And since you’re an Eons viewer, you can get a special deal! Start your free trial with Squarespace at squarespace.com/eons and enter offer code “EONS” to get 10% off your first purchase. What do you want to know about the story of life on Earth? Let us know in the comments. And don’t forget to go to youtube.com/eons and subscribe! Now do yourself a favor and check out some of our sister channels from PBS Digital Studios.
• 05:30 - 06:00 Your brain will thank you!