Lectures On Biology
Lectures On Biology
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In our eReader you can find the full English version of the book. Read Lectures On Biology Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Lectures On Biology
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E. , carbon hydrogen, oxygen, nitrogen and sulphur or, iron, lead, gold and silver were decomposed into still more elementary substances. This fiery ball, continually emitting its heat into the icy space, continually lost warmth ; thus slowly but steadily the cooling process went on. Then came the time when the first chemical compounds came into existence, followed by the period of the formation of a strong earth-crust. Never- theless, we must assume that the temperature of the earth and the ga...ses surrounding it the atmosphere was at that time yet so high that water could only be present in the atmosphere in a gaseous form.
The period of the formation of the earth-crust was probably followed by a very long waterless period. When afterwards, corresponding to the continued loss of heat, water became deposited on the solid earth-crust and when this primeval ocean had further cooled there were then at last present the conditions of the possibility of existence of organisms like those that exist to-day.
What to read after Lectures On Biology?
You can find similar books in the "Read Also" column, or choose other free books by Curt Thesing to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
E. , carbon hydrogen, oxygen, nitrogen and sulphur or, iron, lead, gold and silver were decomposed into still more elementary substances. This fiery ball, continually emitting its heat into the icy space, continually lost warmth ; thus slowly but steadily the cooling process went on. Then came the time when the first chemical compounds came into existence, followed by the period of the formation of a strong earth-crust. Never- theless, we must assume that the temperature of the earth and the ga...ses surrounding it the atmosphere was at that time yet so high that water could only be present in the atmosphere in a gaseous form.
The period of the formation of the earth-crust was probably followed by a very long waterless period. When afterwards, corresponding to the continued loss of heat, water became deposited on the solid earth-crust and when this primeval ocean had further cooled there were then at last present the conditions of the possibility of existence of organisms like those that exist to-day.
What to read after Lectures On Biology?
You can find similar books in the "Read Also" column, or choose other free books by Curt Thesing to read onlineMoreLess
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