Carbon dioxide
The first era is the Precambrian Era. During this time, which makes up 85% of the earth's existence, life was not common, partly because there was a lack of an environment that creatures could survive in. Early life consisted of single celled organisms and, possibly, viruses. These early cells likely got their energy from chemicals produced in the earth - not from the sun's energy. Unlike todays life, which mostly uses oxygen to survive, early organisms found oxygen to be a poison. Possibly as early as 2.5 billion years ago, an organism arose which used the sun's energy in a process called photosynthesis. This organism, called cyanobacteria (also called blue-green algae) excreted oxygen in the process and this changed the living planet as oxygen levels rose and killed off many other ancient organisms. Evidence of this early life comes in the form of stromatolites, which are rocky mounds which the cyanobacteria created on the ocean floor. Stromatolites are still being created by cyanobacteria, in the oceans and in hypersaline lakes. There is evidence of other organisms grazing on stromatolites as early as 1 billion years ago, which means that these more complex organisms had already evolved.
oxygen
Photosynthetic bacteria produced oxygen, and as they continued to colonize the earth they produced more oxygen. Eventually all the oxygen sinks became saturated, and this resulted in the Great Oxygenation Event (GOE). Aerobic organisms would late evolve and utilize the free oxygen.
Phytoplankton refers to a broad category of organisms. Many belong to the kingdom Protista, and some belong to the kingdom Monera. They are all microscopic organisms that are capable of undergoing photosynthesis. Phytoplankton, or phytoplankton-like organisms are believed to be responsible for the Earth's first mass extinction, as their waste product, oxygen was suddenly released into the early atmosphere, which acted as a poison to early organisms that was used to the abundant sulfur in the atmosphere.
Oxygen was a waste product of the first organisms. They fed on the chemicals in the early sea, and spewed out oxygen, so much oxygen that oxygen replaced the carbon dioxide as an insulation layer. Plant today produce oxygen by photosynthesis.
Carbon Dioxcide
carbon dioxide
oxygen
unicellular prokaryoytes
early organisms created oxygen from other gases in the atomsphere
The first era is the Precambrian Era. During this time, which makes up 85% of the earth's existence, life was not common, partly because there was a lack of an environment that creatures could survive in. Early life consisted of single celled organisms and, possibly, viruses. These early cells likely got their energy from chemicals produced in the earth - not from the sun's energy. Unlike todays life, which mostly uses oxygen to survive, early organisms found oxygen to be a poison. Possibly as early as 2.5 billion years ago, an organism arose which used the sun's energy in a process called photosynthesis. This organism, called cyanobacteria (also called blue-green algae) excreted oxygen in the process and this changed the living planet as oxygen levels rose and killed off many other ancient organisms. Evidence of this early life comes in the form of stromatolites, which are rocky mounds which the cyanobacteria created on the ocean floor. Stromatolites are still being created by cyanobacteria, in the oceans and in hypersaline lakes. There is evidence of other organisms grazing on stromatolites as early as 1 billion years ago, which means that these more complex organisms had already evolved.
No! Stromatolites converted the toxic atmosphere into a breathable one.
Breathable oxygen, or O2, did not exist in large quantities in the atmosphere until after the evolution of photosynthetic organisms. Hence, early organisms had to have an anaerobic metabolism, or one that did not require oxygen. However, compounds containing oxygen, such as water, have always been necessary to organisms.
The early Earth atmosphere was toxic until the Stromatolites converted it to the nitrogen/oxygen mixture we now have. It is maintained by the trees and algae.
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oxygen
the appearance of oxygen-producing organisms