The evolution of the sun, terrestrial planets and life is complex. Human …show more content…
less than 1% of its atmospheric composition. Early Earth likely composed of carbon dioxide, water vapour and minor amounts of ammonia (British Broadcasting Corporation 2014). Kasting and Siefert (2002) highlight the importance of microorganisms in the Earth's atmospheric evolutionary processes. The production of the majority of oxygen on Earth can be attributed directly and indirectly to these microorganisms. Photosynthesis was "co-opted from a precocious and ancient form of life known as cyanobacteria" (Kasting and Siefert 2002, p.1066). Cyanobacteria provided oxygen to the Earth's atmosphere along with nitrogen in the Earth's oceans (Kasting and Siefert 2002). Thus the evolution of the Earth's atmosphere is linked to the development of oxygen through photosynthesis, a process that began 800 million years ago (Rasool 1967, p.1467). Moreover, early Earth, which was exposed to a less bright and younger sun, had conditions essential for certain anaerobic bacteria that released vast volumes of methane (Kasting and Siefert 2002, p.1066). Together, these evolutionary processes led to Earth's warm and appealing climate. Ultimately, the evolution of the Earth's atmosphere is correlated to the development of its biota (Kasting and Siefert 2002,