5. Mineral, Plant And Animal Creation

GA 232/1923-12-01/p006 ·1923-12-01 · English HighHigh alignmentThis translation's paragraph count matches the German original — the locus maps cleanly to the same paragraph in DE.
Record: unknown. How this text was taken down (shorthand transcript, listeners' notes or manuscript) is not on record here. Unknown is not an assurance of a stenogram: check the edition's own notes before resting an argument on one word.

Let us begin by thinking of our present atmosphere which we regard as being devoid of life. Even this atmosphere proves to be quite different from anything to be found in early periods of the Earth’s evolution. Still further in the past something resembling the solid core of the Earth as we know it today is in evidence, surrounded by an atmosphere. But in those days there was nothing at all like the air we breathe today. In this air oxygen and nitrogen play the most prominent part, carbon and hydrogen a subsidiary role, sulphur and phosphorus a role of less importance still.

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Cite: GA 232/1923-12-01/p006 · edition English