ENV100Y5 Lecture Notes - Lecture 6: Cambrian Explosion, Carbon Cycle, Chemosynthesis

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7 Jul 2016
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ENV100Y5 Full Course Notes
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Matter and energy earth as a planet 2. Hot and dense(high atmospheric pressure) and not hospitable. The surface then cooled to sustain liquid water, oceans accumulates but still hot, water precipitated and re-evaporated, water +gases= acids= weathering of minerals. Then life comes into the picture and everything changes. Life originated from inorganic chemicals in the ocean first life forms used organic compounds for energy. Panspermiahypothesis ( seeds fromspace) microbes delivered to earth on meteorites. Chemoautotrophichypothesis(oceandepths) life originated at deep-sea hydro thermal vents. First organisms were chemoautotrophs fossil- remnant of long dead organism fossil record-gives information about history of past life not all fossils are macro-fossils, Chemosynthetic, thermophilic bacteria appeared by ~4 ga at latest. Photosynthetic cyanobacteria( blue-greenalgae ) appeared ~3. 9 ga at latest: life had two main influences on the chemistry of the atmosphere: Seafloor sediments recorded changing ocean-atmosphere compositions ( red/black handed iron formation) Free oxygen in the atmosphere by 2ga ago.

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