Our planet’s plants and soils reached the peak of their ability to absorb carbon dioxide in 2008, and their sequestration rate has been falling ever since, according to a new analysis by a father-and-son team in the United Kingdom.

At first, the added carbon led to warmer temperatures, vegetation growth and a longer growing season. Once a tipping point was reached, however, the combination of heat stress, wildfires, drought, flooding, storms and the spread of new diseases and pests led to a reduction in the amount of carbon plants can soak up.

“The rate of natural sequestration of CO2 from the atmosphere by the terrestrial biosphere peaked in 2008.

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