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Dive into the intricate History of the Carbon Cycle and the fascinating evolution of Oxygen in Earth's atmosphere. Learn about the Plant Cell organelles, the Endosymbiotic theory, Cyanobacteria, and Stromatolites.
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Carbon Cycle • A biogeochemical cycle by which carbon is exchanged among the biotic and abiotic factors of the Earth.
Organelles Mitochondrion: breaks down organic molecules in the presence of oxygen to create energy for the cell (cellular respiration)
Chloroplast: Stores energy in the form of organic molecules from carbon dioxide and releases oxygen by using sunlight (photosynthesis)
Endosymbiotic theory: a host cell engulfed prokaryotic cells capable of photosynthesis and cellular respiration
Evidence of Oxygen in the Atmosphere • Cyanobacteria: bacteria that get their energy through photosynthesis and are the only photosynthetic prokaryotes able to produce oxygen.
Stromatolites: originally formed by the growth of layer upon layer of cyanobacteria • These growths primarily contributed to the formation of oxygen of earth's atmosphere • https://ca.pbslearningmedia.org/resource/nvmn-sci-stromatolites/wgbh-nova-making-north-america-stromatolites-worlds-oldest-living-fossil/#.Wdv1O2hSzcs
The oxygen produced from the cyanobacteria was used to make rust (iron + oxygen) • Rust in rock layers begins to form about 2.7 billion years ago (bya) • This is after the first stromatolite fossil appears in our fossil record (3.7 bya)