Life recovers, and then we're in the Devonian period after that.

生命恢复，然后我们进入盆。

The long-ago seas of the Carboniferous and Devonian swarmed with tiny plankton that wrapped themselves inside tiny protective shells.

盆和石炭的古代海洋里生活着大批微小的浮游生物。它们躲在小小的保护性壳里。

The Ordovician (440 million years ago) and Devonian (365 million) each wiped out about 80 to 85 percent of species.

奥陶（44000万年以前）和盆（36500万年以前）分别消灭大约80%——85%的物种。

The clue to this ancestor, it was assumed, would be found in the Devonian era, from about 400 million years ago.

据认为，这个祖先的线索要在大约4亿年以前的盆寻找。

But these creatures lived in a very different world from the Devonian.

但这些生物生活在 与盆截然不同的世界中。

The venerable family of Roach has been crawling around since at least the devonian.

至少从盆开始，可敬的 Roach 家族就一直在四处爬行。

While fish with jaws first appeared in the Silurian, they proliferated in the Devonian.

虽然有颚的鱼最早在 志留，但它们在盆大量繁殖。

Well, during the Devonian, things were … complicated.

好吧，在盆期间，事情… … 很复杂。

But in the Devonian, a new branch of the cephalopod family tree appeared: ammonites.

但在盆，头足类 家族树的一个新分支：菊石。

And Archaeopteris and other Devonian plants also  created more habitats for animals, and more food for them, too.

始祖蕨属和其他盆植物也为动物创造更多的栖息地，也为它们创造更多的食物。

By the end of the Devonian, all of the giant marine eurypterines had gone extinct.

到盆末期，所有巨大的海洋广翅目动物都灭绝。

But things started to change about a  quarter of the way into the Devonian Period.

但在进入盆的大约四分之一时，情况开始发生变化。

By the end of the Devonian period, plants had developed almost all of  the traits they would need to thrive.

到盆末期，植物已经发展它们茁壮成长所需的几乎所有特征。

And the wood in these plants was  directly responsible for a lot of the soil generation that  took place in the Devonian.

这些植物中的木材直接导致盆发生的大量土壤生成。

It's not really clear what caused the Devonian extinctions, which occurred in two main bursts.

目前还不清楚是什么导致盆的物种灭绝，它发生在两次主要的爆发中。

The Devonian seas were peopled by animals of these species, and deposited them by thousands in the rocks of the newer formation.

盆海洋中栖息着这些物种的动物，并将成千上万的它们沉积在较新地层的岩石中。

Fish began their transition onto land 400 million years ago, during in the Devonian period.

4 亿年前，在盆时期，鱼类开始向陆地过渡。

So, while they helped end  the world of the Devonian, if it wasn't for them, our world  might not have gotten started.

因此，虽然他们帮助终结盆世界，但如果不是他们， 我们的世界可能就不会开始。

Oxygen levels in the Devonian and Carboniferous periods, when terrestrial life first bloomed, were as high as 35 percent (as opposed to nearer 20 percent now).

在陆地生命大幅度增加的盆和石炭，空气中的氧的浓度高达35%（在是将近20%）。

It's now thought that wood evolved at least five different times across different  families by the Late Devonian.

在认为，到盆晚期，木材在不同的家族中至少演化五次。