Four ways to understand the Earths age Joshua M. Sneideman

How old is the Earth?

Well, by counting the number of isotopes

in a sample of rock

that’s undergone radioactive decay,

geologists have estimated the Earth’s birthday,

when it first formed from a solar nebula,

to be 4.6 billion years ago.

But just how long is that really?

Here’s some analogies

that might help you understand.

For example, let’s imagine the entire history of Earth

until the present day

as a single calendar year.

On January 1st, the Earth begins to form.

By March 3rd, there’s the first evidence

of single-celled bacteria.

Life remains amazingly unicellular until November 11th

when the first multicellular organisms,

known as the Ediacaran fauna, come along.

Shortly thereafter, on November 16th at 6:08 p.m.

is the Cambrian Explosion of life,

a major milestone,

when all of the modern phyla started to appear.

On December 10th at 1:26 p.m.,

the dinosaurs first evolve

but are wiped out by an asteroid

just two weeks later.

On December 31st, the mighty Roman empire

rises and falls in just under four seconds.

And Columbus sets sail

for what he thinks is India

at three seconds to midnight.

If you try to write the history of the Earth

using just one page per year,

your book would be 145 miles thick,

more than half the distance

to the international space station.

The story of the 3.2 million year-old

Australopithecine fossil known as Lucy

would be found on the 144th mile,

just over 500 feet from the end of the book.

The United States of America’s Declaration of Independence

would be signed in the last half-inch.

Or if we compared geologic time

to a woman stretching her arms

to a span of six feet,

the simple act of filing her nails

would wipe away all of recorded human history.

Finally, let’s imagine the history of the Earth as your life:

from the moment you’re born

to your first day of high school.

Your first word,

first time sitting up,

and first time walking

would all take place while life on Earth

was comprised of single-celled organisms.

In fact, the first multicellular organism

wouldn’t evolve until you were 12 years old

and starting 7th grade,

right around the time

your science teacher is telling the class

how fossils are formed.

The dinosaurs don’t appear

until three months into 8th grade

and are soon wiped out right around spring break.

Three days before 9th grade begins,

when you realize summer is over

and you need new school supplies,

Lucy, the Australopithecine, is walking around Africa.

As you finish breakfast

and head outside to catch your bus

44 minutes before school,

the Neanderthals are going extinct throughout Europe.

The most recent glacial period

ends as your bus drops you off

16 minutes before class.

Columbus sets sail 50 seconds before class

as you’re still trying to find the right classroom.

The Declaration of Independence is signed

28 seconds later

as you look for an empty seat.

And you were born 1.3 seconds before the bell rings.

So, you see, the Earth is extremely,

unbelievably old

compared to us humans

with a fossil record

hiding incredible stories to tell us about the past

and possibly the future as well.

But in the short time we’ve been here,

we’ve learned so much

and will surely learn more

over the next decades and centuries,

near moments in geological time.

地球的年龄是多少?

好吧,通过计算

经历过放射性衰变的岩石样本中的同位素数量,

地质学家估计地球的生日是 46 亿年前

,它最初是由太阳星云形成的

但这到底有多长?

这里有一些

类比可以帮助你理解。

例如,让我们将地球到现在的整个历史想象

为一个日历年。

1 月 1 日,地球开始形成。

到 3 月 3 日,出现

了单细胞细菌的第一个证据。

直到 11 月 11 日

,被称为埃迪卡拉动物群的第一个多细胞生物出现时,生命仍然是惊人的单细胞生物

此后不久,11 月 16 日下午 6:08。

是寒武纪生命大爆发的

一个重要里程碑,

那时所有的现代门都开始出现。

12 月 10 日下午 1 点 26 分

,恐龙首次进化,

但仅在两周后就被一颗小行星消灭了

12 月 31 日,强大的罗马帝国

在不到四秒的时间内起起落落。

哥伦布在午夜前三秒启航

前往他认为是印度的地方

如果你试图每年只用一页纸来写地球的历史,那么

你的书就会有 145 英里厚,

是到国际空间站距离的一半以上

。 被称为露西

的 320 万年前的

南方古猿化石的故事

将在第 144 英里处被发现,

距离书尾仅 500 多英尺。

美利坚合众国的独立宣言

将在最后半英寸签署。

或者,如果我们将地质时间

比作一个女人将双臂伸展

到六英尺的距离,

那么简单的锉指甲的动作

就会抹去所有有记录的人类历史。

最后,让我们把地球的历史想象成你的生命:

从你出生的那一刻

到你上高中的第一天。

你的第一个词,

第一次坐起来

,第一次走路

都发生在地球上的生命

是由单细胞生物组成的时候。

事实上,第一个多细胞生物

直到你 12 岁

并开始 7 年级时才会进化,

就在

你的科学老师告诉全班同学

化石是如何形成的时候。

恐龙要

到 8 年级的三个月才出现

,很快就会在春假前后消失。

在 9 年级开学前三天,

当你意识到夏天结束了

,你需要新的学习用品时

,南方古猿露西正在非洲四处走动。

当你吃完早餐

在上学前 44 分钟赶上公共汽车时

,尼安德特人正在整个欧洲灭绝。

最近的冰期

结束时,您的巴士会

在上课前 16 分钟送您下车。

哥伦布在上课前 50 秒启航,

因为您仍在努力寻找合适的教室。

28 秒后,

当您寻找一个空座位时,独立宣言就签署了。

你在铃声响起前 1.3 秒出生。

所以,你看,与我们人类相比,地球极其

古老,令人难以置信

,它的化石记录

隐藏着令人难以置信的故事,可以告诉我们过去

,也可能是未来。

但在我们来到这里的短短时间里,

我们学到了很多东西,

而且

在接下来的几十年和几个世纪里,

在地质时代的临近时刻,我们肯定会学到更多。