The Pliocene as an analogue for near-future climate change?
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The Pliocene as an analogue for near-future climate change?

In 1958, atmospheric scientist Charles David Keeling installed an instrument at the Mauna Loa Observatory, in Hawaii, designed to measure the average global concentration of carbon dioxide (CO2) in the atmosphere. Little did he realise at the time that the results of this experiment, driven by a desire to characterise the composition of Earth’s atmosphere, … Continue reading