How a single celled organism almost wiped all life on earth during the first mass-extinction by giving us oxygen.
source: Wikimedia Commons
Back in January I wrote about the near immortality of certain microbes found in the mud covering the floor of the deep sea, and how different they are from all other life found on the planet. You can read that post here. Especially the low energy requirements for these life-forms to exist and their total independence from sunlight makes them remarkable. This is because all other life on earth depends for its energy on sunlight: plants transform carbon-dioxide and water into sugar and oxygen through photosynthesis. And animals eat these plants, or other animals that eat plants to get their energy; all life as we know it depends on the energy from sunlight, either directly or indirectly. Except for those microbes in the oceans' mud...
I'll now share with you why these microbes are so different: they existed in our oceans billions of years ago, even before the first oxygen-producing plants existed! When we look at the early earth's history, it's a beautiful tale of how life as we know it developed from the earliest single celled organisms; our mud-dwelling microbes or anaerobic cells. These anaerobic cells were the dominant life-form om earth for a billion years.
Back then, approximately three billion years ago, almost the entire planet was still covered with water. This water, the oceans from today, was full of iron and contained almost no oxygen. Above the water, the atmosphere was mostly nitrogen, water-vapor, carbon-dioxide and methane, but almost no oxygen at all. Then, approximately 2.8 - 2.5 billion years ago, the first photosynthesizing creatures appeared near the water's surface; cyanobacteria, also known as blue-green bacteria. They photosynthesized oxygen from water and carbon-dioxide.
This oxygen, that was also released into the water of course, was toxic to the anaerobic cells alive back then, and hence the earths first mass-extinction was a fact; most of these early life-forms died and only the ones that literally fled into the mud from the deepest ocean-floors survived. Another effect was that all the iron in the seas began to rust, depositing thick layers of red-brown sediment which can be seen today in archaeological stratification.
Chloroplast-Cyanobacterium comparison - source: Wikimedia Commons
Isn't it wonderful how the very process upon which almost all life depends, the process of producing oxygen with sunlight, long ago was the death of almost all existing life on earth? Through some genetic mutation some of the cells developed the ability to capture energy directly from sunlight by photosynthesis. There were no animals yet, so carbon-dioxide levels kept reducing while oxygen levels kept rising, so the cyanobacteria also died off in massive numbers as they consumed all carbon-dioxide with their photosynthesis; this is why there's several bands of red-brown layers in the earths crust as the raining down of rusted iron lasted almost a billion years in several stages.
One of the hypotheses about the early evolution of life is that animals evolved to act as a counter balance against the oxygen production of plants; with a high oxygen level in the atmosphere everything would spontaneously burn with the lightest spark. Also the higher oxygen levels back then explain why there were so many extremely large animals and insects.
I hope you find this as interesting as I do. If so, here's a ten minute video that explains all of this and something extra: there's a possibility that the chloroplasts, the organelles inside plant-cells responsible for photosynthesis, are in fact directly descendant from the cyanobacteria from two and a half billion years ago!
Evolution and Oxygen
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