Elisabet Sahtouris writes: The constant hail of meteors, leaving craters such as we see on the Moon, was a serious threat. Though meteors may have contributed important molecules such as lipids to the formation of microbes, they might also have killed them off again. Every day these space rocks of all sizes came hurling from the sky like bullets. If nothing had happened to protect the Earth from them, it might well have ended up as lifeless and pockmarked as the Moon and our neighboring planets. There may also have been another problem, though scientists differ on this matter. The Sun’s energy was most helpful in splitting molecules so that new ones could form, but as the first microbes formed and multiplied, the strong Sunlight may have been too much for many of them to stand, putting them in need of protection from the burning part of Sunlight we call ultraviolet radiation. Some ultraviolet is good for living creatures, but too much can burn them, and our young Sun probably produced far more ultraviolet than it does today, when we are concerned about our own threat to the shield of ozone protecting us from it — a shield that did not exist at all around the early Earth, though the smoggy early atmosphere may have offered some protection. In any case, the first microbes seem to have formed on the seafloor, in seawater or wet mud deep enough to filter out the dangerous rays. There, as we saw in the last chapter, bits of a rich soup of organic molecules and seawater were probably trapped in liposome spheres where the molecules could move about and begin new kinds of chemical cycles. These would have included, had they not already been formed elsewhere, the construction of the giant RNA and DNA molecules that became useful as a storage system for information life needed. (04/16/02)
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