Researchers focused on the climate of the Pliocene, over 3 million years ago, the last time Earth has seen concentrations of over 400 PPM CO2 in the atmosphere, similar to today’s concentrations. The Pliocene prompts a long-standing question: despite the similarity to the present-day, why were dry areas like the Sahel in Africa and Northern China much wetter and greener in the Pliocene than they are today?
Click here for original story, Ice sheet retreat and forest expansion turned ancient subtropical drylands into oases
Source: ScienceDaily