Clearly, Antarctica’s biodiversity took a hit after the Eocene.

显然，南极洲的生物多样性 之后受到了打击。

Eocene, so, by about 40 million years ago, many of them had gone extinct.

，因此，到大约 4000 万年前， 其中许多已经灭绝。

But what happened to these Eocene animals?

但是这些动物发生了什么？

As a result, our world is warming faster than it did back in the Eocene.

结果，我们的界变暖的速度 比。

So given its size, it was able to support many different ecosystems in the Eocene.

所以考虑到它的大小，它能够支持 许多不同的生态系统。

In the United States, Boverisuchus shows up fully-formed and ready to run in the early Eocene.

美国，，Boverisuchus 已经完全成形并准备好奔跑。

Other residents of Eocene Antarctica probably came from South America as well.

南极洲的其他居民可能 也来自南美洲。

Over the course of the Eocene epoch, the climate slowly began to cool.

，气候 开慢慢变冷。

By the late Eocene, practically all of the primates on those continents died out.

到晚， 这些大陆上几乎所有的灵长类动物都灭绝了。

Floristic Region, but their family was clearly much more widespread during the Eocene Epoch.

植物区的地区发现，但它们的科显然 要远得多 广泛存。

Though the Cretaceous asteroid cleared the stage, mammals did not really get going until 10m years later, in the Eocene epoch.

尽管白垩纪的小行星灭绝了居统治地位的恐龙，但哺乳动物却一直到1000万年后的才真正兴起繁盛起来。

But about 49 million years ago, in the mid-Eocene, the climate began to get cooler and drier.

但大约 4900 万年前，中，气候开变得更凉爽和干燥。

In the early Eocene Epoch, probably before mustelids appeared, our planet had a warm climate.

，可能鼬科动物出现之前，我们的星球气候温暖。

What we do know is that the late Eocene and early Oligocene was a time of global cooling.

我们所知道的是，晚和 渐是全球降温的。

The Paleocene-Eocene Thermal Maximum, 55 million years ago, was so warm, crocodiles swam the waters of the Arctic Circle.

5500 万年前的古-极热非常温暖，以至于鳄鱼北极圈的水域中游来游去。

Around 34 million years ago, the Eocene-Oligocene Transition  marked the first major period of global cooling and glaciation.

大约 3400 万年前，-渐过渡标志着全球变冷和冰川作用的第一个主要。

Let's rewind back to the Eocene, about 45 million years ago.

让我们回到大约 4500 万年前的。

So by the time the Eocene Epoch was over, North America no longer had the right habitat for primates.

因此， 当结束，北美不再有适合灵长类动物的栖息地。

And a big environmental change was also underway in the last half of the Eocene, thanks to the chemistry of mountain-building.

由于造山的化学作用，后半也发生了巨大的环境变化。

And they arrived in South America by the middle Eocene Epoch, around 42 million years ago.

他们大约 4200 万年前的中到达南美洲。