When the Earth was formed over 4500 million years ago, the composition of the atmosphere was very different from that we experience today. At that time, the largest component of the primitive atmosphere was carbon dioxide, followed by nitrogen and hydrogen (which soon escaped from the planet) with almost no oxygen at all. This atmosphere resulted largely from the gases released as the molten planet cooled and during volcanic eruptions. There was virtually no oxygen except for that produced by the action of ultraviolet radiation from the Sun on water vapour in the atmosphere. The proportion of carbon dioxide decreased rapidly as the gas dissolved in the oceans and was removed as sedimentary rocks (see also 'The Carbon Cycle'). Later, when the first plant cells formed, photosynthesis gradually increased the oxygen content.
|
|
 Click for larger image |
|