Scientists analyzing air bubbles that had been trapped in Antarctic ice during the Earth's last ice age found that the ice-age atmosphere had contained unusually large amounts of ferrous material and surprisingly small amounts of carbon dioxide. ███ █████████ █████ ████ █████ ██████ ██████ ███████ ████ ███ ███████████ ███ █████████ ████████████ ████ ███ ███████ █████████ █████ ███ █████████ ██ ███████████ █████ ███ ████████ █ █████ ████████ ██ ███ ██████████ ██ █████████ █████ ████ ██ ████████
The scientist hypothesizes that ferrous material in the atmosphere promoted a great increase in the population of Antarctic algae. This is supported by the observation that air bubbles in ice-age ice had surprisingly high levels of ferrous material and low levels of carbon dioxide. What's more, algae absorb carbon dioxide from the atmosphere.
The scientist assumes that more ferrous material causes more algae. This means assuming that ferrous material has a positive effect on algae growth, and that there isn’t some other cause that’s actually responsible algae growth. The scientist also assumes that algae were actually present in Antarctica at this time, in quantities sufficient to affect the composition of the atmosphere.
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