When will the next mass extinction occur Borths DEmic and Pritchard

About 66 million years ago,

something terrible happened
to life on our planet.

Ecosystems were hit with a double blow

as massive volcanic eruptions filled
the atmosphere with carbon dioxide

and an asteroid roughly the size
of Manhattan struck the Earth.

The dust from the impact reduced or
stopped photosynthesis from many plants,

starving herbivores and the carnivores
that preyed on them.

Within a short time span,

three-quarters of the world’s species
disappeared forever,

and the giant dinosaurs,

flying pterosaurs,

shelled squids,

and marine reptiles
that had flourished for ages

faded into prehistory.

It may seem like the dinosaurs
were especially unlucky,

but extinctions of various severities have
occurred throughout the Earth’s history,

and are still happening
all around us today.

Environments change,

pushing some species
out of their comfort zones

while creating new opportunities
for others.

Invasive species arrive in new habitats,
outcompeting the natives.

And in some cases,
entire species are wiped out

as a result of activity
by better adapted organisms.

Sometimes, however, massive changes
in the environment

occur too quickly
for most living creatures to adapt,

causing thousands of species to die off
in a geological instant.

We call this a mass extinction event,

and although such events may be rare,

paleontologists have been able
to identify several of them

through dramatic changes
in the fossil record,

where lineages that persisted
through several geological layers

suddenly disappear.

In fact, these mass extinctions are used
to divide the Earth’s history

into distinct periods.

Although the disappearance
of the dinosaurs

is the best known mass extinction event,

the largest occurred long before
dinosaurs ever existed.

252 million years ago,
between the Permian and Triassic periods,

the Earth’s land masses gathered together
into the single supercontinent Pangaea.

As it coalesced,
its interior was filled with deserts,

while the single coastline eliminated
many of the shallow tropical seas

where biodiversity thrived.

Huge volcanic eruptions
occurred across Siberia,

coinciding with very high temperatures,

suggesting a massive greenhouse effect.

These catastrophes
contributed to the extinction

of 95% of species in the ocean,

and on land, the strange
reptiles of the Permian

gave way to the ancestors of the
far more familiar dinosaurs we know today.

But mass extinctions are not just a thing
of the distant past.

Over the last few million years,

the fluctuation of massive ice sheets
at our planet’s poles

has caused sea levels to rise and fall,

changing weather patterns
and ocean currents along the way.

As the ice sheets spread,
retreated, and returned,

some animals were either
able to adapt to the changes,

or migrate to a more suitable environment.

Others, however,
such as giant ground sloths,

giant hyenas,

and mammoths went extinct.

The extinction of these large mammals

coincides with changes in the climate
and ecosystem due to the melting ice caps.

But there is also
an uncomfortable overlap

with the rise of a certain hominid species
originating in Africa 150,000 years ago.

In the course of their adaptation
to the new environment,

creating new tools and methods
for gathering food and hunting prey,

humans may not have single-handedly caused
the extinction of these large animals,

as some were able to coexist with us
for thousands of years.

But it’s clear that today,

our tools and methods
have become so effective

that humans are no longer reacting
to the environment,

but are actively changing it.

The extinction of species
is a normal occurrence

in the background of ecosystems.

But studies suggest
that rates of extinction today

for many organisms

are hundreds to thousands of times higher
than the normal background.

But the same unique ability that makes
humans capable of driving mass extinctions

can also enable us to prevent them.

By learning about past extinction events,

recognizing what is happening today
as environments change,

and using this knowledge to lessen
our effect on other species,

we can transform humanity’s impact
on the world

from something as destructive
as a massive asteroid

into a collaborative part
of a biologically diverse future.

大约 6600 万年前,

我们星球上的生命发生了可怕的事情。

大规模的火山喷发
使大气中充满了二氧化碳

,并且一颗大约曼哈顿大小的小行星
撞击了地球,生态系统受到了双重打击。

撞击产生的灰尘减少或
停止了许多植物、

饥饿的食草动物和
捕食它们的食肉动物的光合作用。

在很短的时间内,

世界上四分之三的物种
永远消失了

,繁盛多年的巨型恐龙、

飞行翼龙、

带壳鱿鱼

和海洋爬行动物

消失在史前时代。

恐龙似乎
特别不幸,

但在整个地球历史上都发生了各种严重程度的灭绝

并且今天仍在
我们周围发生。

环境发生变化,

将一些物种
赶出舒适区,

同时为其他物种创造新机会

入侵物种到达新的栖息地,
胜过当地人。

在某些情况下,由于适应性更好的生物的活动,
整个物种都被消灭了

然而,有时,环境的巨大变化

发生得太快
,大多数生物都无法适应,

导致数千个物种
在地质瞬间死亡。

我们将此称为大规模灭绝事件

,尽管此类事件可能很少见,但

古生物学家已经能够通过化石记录的巨大变化
来识别其中的几个,

其中持续
通过几个地质层的谱系

突然消失。

事实上,这些大灭绝被
用来将地球的历史

划分为不同的时期。

虽然恐龙的消失

是最著名的大规模灭绝事件

,但最大的一次发生在
恐龙存在之前很久。

2.52 亿年前,
在二叠纪和三叠纪之间

,地球的陆块聚集在一起
形成了单一的超大陆盘古大陆。

当它合并时,
它的内部充满了沙漠,

而单一的海岸线消除了
许多

生物多样性繁盛的热带浅海。

整个西伯利亚发生了巨大的火山喷发,

与非常高的温度同时发生,

这表明存在巨大的温室效应。

这些灾难

导致海洋中 95% 的物种灭绝,

而在陆地上,二叠纪奇怪的
爬行动物

让位于
我们今天所知的更为熟悉的恐龙的祖先。

但大规模灭绝不仅仅是
遥远的过去。

在过去的几百万年里,地球两极

巨大冰盖的波动

导致海平面上升和下降,沿途

改变了天气模式
和洋流。

随着冰盖的扩张、
退缩和回归,

一些动物要么
能够适应变化,

要么迁移到更合适的环境。

然而,其他的,
如巨型地懒、

巨型鬣狗

和猛犸象已经灭绝。

这些大型哺乳动物的灭绝

恰逢
冰盖融化导致气候和生态系统发生变化。

但是,

与 150,000 年前起源于非洲的某些原始人物种的兴起也存在令人不安的重叠

在它们
适应新环境、

创造新的工具和方法
来采集食物和猎杀猎物的过程中,

人类可能不是单枪匹马地导致
了这些大型动物的灭绝,

因为有些动物能够与我们共存
数千年 .

但很明显,今天,

我们的工具和方法
变得如此有效

,以至于人类不再
对环境做出反应,

而是在积极地改变它。

物种灭绝是

生态系统背景下的正常现象。

但研究
表明,

今天许多生物

的灭绝率比正常背景高出数百到数千倍

但是,使
人类能够推动大规模灭绝的独特能力

也可以使我们能够阻止它们。

通过了解过去的灭绝事件,

认识到当今环境变化正在发生的事情

并利用这些知识来减少
我们对其他物种

的影响,我们可以将人类对世界的影响

从像巨大的小行星这样具有破坏性的事物

转变为协作的一部分
。 生物多样性的未来。