Making Sense of the Mid-Pleistocene Transition (MPT)
I recently read a fascinating study looking to understand why the “Mid-Pleistocene Transition” (MPT) happened about 1 million years ago. The MPT refers to the change where the glacial-interglacial cycles of the Pleistocene (the last 2.6 million years) changed from cycles of ~41,000 years to ~100,000 years. Both periodicities are synced to Milankovitch Cycles. During the early Pleistocene, the periodicity matches cycles in the earth’s obliquity, but after the MPT the glacial-interglacial cycles began to track more closely with variations in the earth’s orbital eccentricity. So the big question has been why the change? A recent paper by Willeit published in Science Advances [1] examined this by producing a model that was able to reproduce the MPT. In fact it accurately reproduced the maximum extent of the ice sheets as well as extent of sea level rise. It made use of the carbon cycle, volcanic activity, and changes in regolith cover. The model results indicate that continents had built u...