By Lloyd Pye
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It is extremely reactive with elemental oxygen, quickly forming iron oxide (rust) when the two combine. Thus, until all the exposed elemental iron could be converted to rust, oxygen would not be free for use by any complex life forms. 8 bya. Not until these strata and millions of miles like them formed could proto-Earth host the next phase of complex life development. Countless prokaryotes generated the oxygen that created the worldwide array of BIFs, but the undisputed O2 champions were the many forms of cyanobacteria, or blue-green algae.
Let’s assume that everywhere life exists—on Earth and beyond—it is every bit as resilient and prolific as here. Whether that is true or not, we do know that myriad varieties are here, and we know when the first prokaryotes appeared. Despite fanciful dogmas experts preach to the uninformed, when prokaryotes first appeared, Earth was as depicted above, as it would have been if our imagined Intragalactic Terraformers were actually at work. And if they were, they provide a much more plausible explanation.
With no clear linkage between early life forms, why can we not consider the glaringly obvious possibility that they all were in fact extrasolar? Because mainstream science enforces its selfproclaimed “authority” to insist that we can’t. ***** The illustration below encapsulates the timeline of life on Earth, which we must outline before discussing the far more complex “higher” forms of life that came after the Cambrian explosion. 8 bya. During this long stretch of turmoil across the seething surface, it was impossible for even the simplest life form to have spontaneously aggregated.