Miocene (Pt 16): Giant Camels and High Llamas

One group of animals that you might expect to have done reasonably well as the climate dried out in the later stages of the Miocene epoch were the camels. Camels, of course, are not found wild in North America these days, but, back in the Miocene, it was the only place that they were found, having first evolved on that continent millions of years before.

Indeed, camels had been diverse in the Early and Middle Miocene, inhabiting a number of habitats that we would not associate with the animals today. Once those habitats changed with the shift into the Late Miocene, however, many of them failed to adapt, and a number of earlier forms died out. These included the stenomyline "gazelle-camels", the short-legged miolabines, and the floridatragulines, which had been adapted to the subtropical forests of the southern coasts.

Miocene (Pt 3): The Elephants Reach Europe

Gomphotherium angustidens

At the dawn of the Miocene, Europe was still relatively isolated from much of the rest of the world. The only other continent to which is was attached by land was Asia, and even with that, perhaps due to the higher sea levels and narrower land bridges of the day, there was less exchange of animals than one might expect. As a result, for a few million years at the dawn of the epoch, Europe remained a haven for animals that had died out elsewhere, or at least retreated. Tapirs, for example, were still common; today they are restricted to South East Asia and the Americas. The European rhinos of the day were also relatively small and primitive.

While the millions of years that they survived might actually have been quite notable, had we been talking about the much shorter, later epochs, in the grand sweep of the Miocene, we can say that they were quite rapidly replaced by immigrants from the east. The early tapirs were gone (although more modern forms did return for a while, much later), but the rhinos were instead replaced by larger and more sturdy, distinctly Miocene species.