Tectonic degassing drove global temperature trends since 20 Ma

The Miocene Climatic Optimum (MCO) from similar to 17 to 14 million years ago (Ma) represents an enigmatic reversal in Cenozoic cooling. A synthesis of marine paleotemperature records shows that the MCO was a local maximum in global sea surface temperature superimposed on a period from at least 19 Ma to 10 Ma, during which global temperatures were on the order of 10 degrees C warmer than at present. Our high-resolution global reconstruction of ocean crustal production, a proxy for tectonic degassing of carbon, suggests that crustal production rates were similar to 35% higher than modern rates until similar to 14 Ma, when production began to decline steeply along with global temperatures. The magnitude and timing of the inferred changes in tectonic degassing can account for the majority of long-term ice sheet and global temperature evolution since 20 Ma.

Automated summary

The Miocene Climatic Optimum, which occurred from 17 to 14 million years ago, was a reversal in the cooling trend during the Cenozoic era. Analyzing marine paleotemperature records and ocean crustal production rates, researchers found that the rates of crustal production had a significant impact on global temperatures, explaining the long-term ice sheet and global temperature evolution over millions of years.