The Archaean A Cooling Crust

3.8 to 2.5 Billion Years Ago

The Archaean period was a time of continent-building and the first stages of early life. In fact, 70% of our continental land masses are formed around cores of rock, or shields, that date from this period.

With this said, let’s take a look at the various conditions that may have been in existence during this time period.

First, the atmosphere would not have been like it is today. It would have had no oxygen. Instead, it would have been filled with:

  • hydrogen
  • methane
  • ammonia

This kind of atmosphere is called a reducing atmosphere. It is just the kind of atmosphere that could support the organic chemistry for first life. In fact, there is fossil evidence of ancient bacteria.

One type of bacteria present then were the cyanobacteria or blue-green algaes. These bacteria appear to have had a very strong cell-wall and the ability to form layers in the ancient sediments. The formations are called stromatolites. They can be found in Archaean rock formations of Western Australia.

The very oldest rocks of the Archaean are very rare, most likely because they have been changed by the pressure created by many layers or even “recycled” by being pushed so deep as to be returned to a molten state.

But the younger rocks can still be found in South Africa, Western Australia, Canada and India. These rock shields give us clues to the formation of our continents.

The forming of the continents during the Archaean probably began as lava flow under the ancient oceans. The youngest of the Archaean rock layers look like giant pillows of lava and resemble underwater lava flows from modern times.

Based on this resemblance, it seems likely that most of the continents were covered by water during the Archaean time, roughly 3 billion to 2.5 billion years ago. One can look at the Hawaiian Islands, yet underwater, to get a glimpse of modern pillow lavas.

While the Cambrian Period with its explosion of life generally marks the beginning of the Paleozoic Era and life on our planet, there are many indications that the preparation for life and the earliest forms of it all got going during the Archaean Period.

Photo credit:US National Oceanic and Atmospheric Administration

Before life forms could evolve, there had to have been chemical transformations to set the stage. The now-famous experiment performed by Miller and Urey in 1953 showed how an atmosphere of:

  • methane
  • carbon dioxide
  • hydrogen

a reducing atmosphere) exposed to heat and electrical charges would have produced organic molecules such as amino acids and simple sugars.

Even though this experiment has been questioned and refuted, many modern biochemists agree that such simultaneous events could have been the impetus behind our first life on Earth.

Amino acids would have gradually come together into increasingly more complex molecules.

The earliest life forms were anaerobic, forms that did not use oxygen to exist. In our modern world, anaerobic organisms are those that work in the process of fermentation.

These organisms lived on consumable organic matter or on other anerobic life forms. Thus they were heterotrophs, like modern fungi, that feast on organic material. The ancient heterotrophs, like fungi, were dependent on the presence of organic materials and would have eventually perished once the organic material had all been consumed.

But autotrophs appeared, saving the day! These new organisms fed on the pure energy source of the sun. They were the predecessors of our modern blue-green algae and were the cyanobacteria that formed the stromatolites.

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Following the Archaean Era is the Proterozoic

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