Oligocene (Pt 6): Devil's Corkscrews and the Grasseater That Wasn't

Leptomeryx

The Grande Coupure was, strictly defined, an event unique to Europe, caused by the drying up of the water channels separating it from Asia. However, it was compounded by a dramatic worldwide cooling event, and, if the Coupure itself didn't affect more distant lands, the climate changes certainly did. Due to some particularly well-preserved geological deposits of the right age, as well as the obvious convenience for Western researchers, this is particularly well-studied in North America.

Deposits across the continent show a sudden change in the climate at around the dawn of the Oligocene. By 'sudden' in this context, we mean over the course of hundreds of thousands of years, so it's hardly something you would have noticed had you been there at the time, but it's still rapid as such things go. The exact nature of the changes, and the speed at which they appear to have happened, depend on which part of the continent we're talking about, but nowhere was unaffected.