GEOL 102 Historical Geology
Spring Semester 2008
The Archean Eon II: The Origin of Life
Origin of Life was apparently very early in Archean.
Evidence of Archean life:
- Fractionated carbon isotopes at 3.8 Ga (Isua Fm., Greenland)
- Filaments of cyanobacteria (blue-green algae) in 3.4 Ga cherts (in western
Australia, South Africa)
- Stromatolites at 3.3-3.5 Ga (Warrawoona Group, Australia)
Earliest life was probably exceedingly simple: far simpler than any modern form.
Would have been:
- Anaerobic: evolved outside the presence of free oxygen (free oxygen would
probably poison it!)
- Heterotrophic: a consumer, absorbing molecules from water
- Prokaryotic: no nucleus nor other complex organelles
Once thought to have appeared in "quite little pond" ("primordial soup").
More likely: formed near the (then more active) oceanic vents along mid-ocean ridges:
- Abundant energy supply and mineral supply
- Far more common in Archean than now (due to higher geothermal activity)
- Ocean water would protect early life from UV rays
- Even today many exceedingly simple prokaryotes live near vents, black smokers, etc.
As fuel supply decreased, various new forms appeared from among the proto-organisms:
- Photosynthesizers ("blue green algae"), first to use sunlight directly.
- 1rst order consumers: absorb other cells.
With photosynthesizers come free oxygen: begin to change global atmosphere. Has most
direct effect as the Proterozoic begins.
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Last modified: 2 January 2008