ABOUT THE SPEAKER
Peter Ward - Paleontologist
Peter D. Ward studies life on Earth -- where it came from, how it might end, and how utterly rare it might be.

Why you should listen

Paleontologist and astrobiologist Peter D. Ward studies the Cretaceous-Tertiary extinction event (the one that killed the dinosaurs) and other mass extinctions. He is a leader in the intriguing new field of astrobiology, the study of the origin, distribution and evolution of life in the universe.

In his book Rare Earth he theorizes that complex life itself is so rare, it's quite possible that Earth is the only planet that has any. But, he theorizes, simple life may exist elsewhere -- and possibly be more common than we think.

His upcoming book, The Medea Hypothesis, makes a bold argument that even here on Earth, life has come close to being wiped out several times. Contrary to the "Gaia hypothesis" of a self-balancing, self-perpetuating circle of life, Ward's Medea hypothesis details the scary number of times that life has come close to flatlining, whether due to comet strikes or an overabundance of bacteria.

In March 2009, Ward's 8-hour television series, Animal Armageddon, premieres on Animal Planet Network.

In April 2013, Ward published a surprisingly moving essay about his life's obsession: the chambered nautilus >>

More profile about the speaker
Peter Ward | Speaker | TED.com
TED2008

Peter Ward: A theory of Earth's mass extinctions

彼得沃德所發表的大滅絕

Filmed:
1,130,090 views

小行星的撞擊得到所有覆蓋面 ,但"美狄亞假說"的作者彼得沃德則認為大部分發生在地球上的大滅絕是因微小的細菌. 肇事者是一種叫硫化氫的毒藥,它可能對藥物應用有意外的貢獻.
- Paleontologist
Peter D. Ward studies life on Earth -- where it came from, how it might end, and how utterly rare it might be. Full bio

Double-click the English transcript below to play the video.

00:18
So, I want to start開始 out with
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好,我先由
00:20
this beautiful美麗 picture圖片 from my childhood童年.
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我這幅美麗的童年照開始講起
00:22
I love the science科學 fiction小說 movies電影.
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我喜愛看科幻電影
00:24
Here it is: "This Island Earth地球."
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這套: "飛碟征空"
00:26
And leave離開 it to Hollywood好萊塢 to get it just right.
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最適合在美國荷里活上映.
00:28
Two-and-a-half兩個半 years年份 in the making製造.
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用了兩年半的時間製作.
00:30
(Laughter笑聲)
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(笑聲)
00:33
I mean, even the creationists神創論 give us 6,000,
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我是說,當時創作人給了我們$6000
00:36
but Hollywood好萊塢 goes to the chase.
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但荷里活緊緊跟隨
00:38
And in this movie電影, we see what we think is out there:
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還有在這電影裡, 我們看到所認為的外太空:
00:42
flying飛行 saucers飛碟 and aliens外星人.
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飛碟和外星人.
00:45
Every一切 world世界 has an alien外僑, and every一切 alien外僑 world世界 has a flying飛行 saucer茶托,
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每個世界都有外星人, 而每個外星人世界都有飛碟,
00:48
and they move移動 about with great speed速度. Aliens外星人.
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他們行動很快捷. 外星人.
00:53
Well, Don Brownlee布朗利, my friend朋友, and I finally最後 got to the point
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我和我的朋友唐布朗利都覺得
00:56
where we got tired of turning車削 on the TV電視
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我們厭倦開電視
00:59
and seeing眼看 the spaceships飛船 and seeing眼看 the aliens外星人 every一切 night,
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每一晚都看著太空船和外星人
01:02
and tried試著 to write a counter-argument相反的觀點 to it,
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也厭倦寫有關外太空正反觀點
01:05
and put out what does it really take for an Earth地球 to be habitable可居住,
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改為想有什麼條件令地球適合居住
01:09
for a planet行星 to be an Earth地球, to have a place地點
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就是地球, 不單有地方住
01:11
where you could probably大概 get not just life, but complexity複雜,
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能讓人生存, 更有複雜性
01:14
which哪一個 requires要求 a huge巨大 amount of evolution演化,
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這需要長時間的進化
01:16
and therefore因此 constancy恆常 of conditions條件.
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所以需要環境的稳定性
01:19
So, in 2000 we wrote "Rare罕見 Earth地球." In 2003, we then asked,
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所以2000年我們寫了 "Rare Earth". 在2003年,我們便說
01:22
let's not think about where Earths地球 are in space空間, but how long has Earth地球 been Earth地球?
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不要只想著地球在太空的位置,而去想想地球有幾長時間為地球
01:27
If you go back two billion十億 years年份,
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如果你回到20億年前,
01:29
you're not on an Earth-like類似地球 planet行星 any more.
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那行星不像你今日所見的地球
01:31
What we call an Earth-like類似地球 planet行星 is actually其實 a very short interval間隔 of time.
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我們所稱為地球的行星其實很年輕
01:35
Well, "Rare罕見 Earth地球" actually其實
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在"Rare Earth"裡
01:37
taught me an awful可怕 lot about meeting會議 the public上市.
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教導我極多關於面對群眾的要訣
01:40
Right after, I got an invitation請帖 to go to a science科學 fiction小說 convention慣例,
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有次我收到一個科幻電影會展的邀請
01:43
and with all great earnestness語重心長 walked in.
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我帶著一股熱誠步入場地
01:46
David大衛 Brin布林 was going to debate辯論 me on this,
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David Brin 正在與我爭辯
01:48
and as I walked in, the crowd人群 of a hundred started開始 booing起哄 lustily好色.
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當我行入會塲,幾百人開始發出很大的噓聲
01:52
I had a girl女孩 who came來了 up who said, "My dad says you're the devil魔鬼."
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有個小女孩走到我面前說:"我爸說你是一個魔鬼."
01:55
You cannot不能 take people's人們 aliens外星人 away from them
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你不可以從別人身上取走外星人
01:59
and expect期望 to be anybody's任何人的 friends朋友.
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然後同所有人做朋友.
02:03
Well, the second第二 part部分 of that, soon不久 after --
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第二部分,這之後..
02:05
and I was talking to Paul保羅 Allen艾倫; I saw him in the audience聽眾,
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我和Paul Allen 聊天,因我在觀眾席見到他
02:08
and I handed him a copy複製 of "Rare罕見 Earth地球."
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我給他一本"Rare Earth"
02:10
And Jill吉爾 Tarter塔特 was there, and she turned轉身 to me,
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Jill Tarter 聽到,她臉向我
02:14
and she looked看著 at me just like that girl女孩 in "The Exorcist祓魔師."
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她看我的表情就像剛才那女孩在看"驅魔人"
02:17
It was, "It burns燒傷! It burns燒傷!"
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就像說"著火了!著火了!"
02:19
Because SETISETI doesn't want to hear this.
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因為SETI不想聽到這話. (SEIT: Search for Extra-Terrestrial Intelligence 尋找外太空星球智慧生命計畫)
02:21
SETISETI wants there to be stuff東東 out there.
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SETI一直想在太空找到外星人
02:24
I really applaud鼓掌 the SETISETI efforts努力, but we have not heard聽說 anything yet然而.
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我要為SETI的努力鼓掌,但我們未聽到什麼消息.
02:27
And I really do think we have to start開始 thinking思維
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我真的認為我們要開始思考
02:29
about what's a good planet行星 and what isn't.
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怎樣才是一個好或不好的行星
02:32
Now, I throw this slide滑動 up because it indicates指示 to me that,
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現在我放這投影片因它向我顯示
02:35
even if SETISETI does hear something, can we figure數字 out what they said?
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就算SETI真的聽到什麼,我們如何理解那些話?
02:39
Because this was a slide滑動 that was passed通過
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因為這張投影片經過
02:41
between之間 the two major重大的 intelligences智能 on Earth地球 -- a Mac蘋果電腦 to a PC個人計算機 --
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兩個地球上智能產品 -- Mac 和 PC
02:45
and it can't even get the letters right --
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但它們都不能辨認那些字
02:48
(Laughter笑聲)
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(笑聲)
02:50
-- so how are we going to talk to the aliens外星人?
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所以我們如何和外星人溝通?
02:52
And if they're 50 light years年份 away, and we call them up,
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如果他們在50光年以外,而我們打電話給他們
02:55
and you blah胡說, blah胡說, blah胡說, blah胡說, blah胡說,
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然後你叭啦叭啦說了一大堆
02:57
and then 50 years年份 later後來 it comes back and they say, Please repeat重複?
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50年後訊號回來是:請再說一遍
03:00
I mean, there we are.
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所以我們就是這樣
03:02
Our planet行星 is a good planet行星 because it can keep water.
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我們的地球是一個好行星因它能儲存水.
03:05
Mars火星 is a bad planet行星, but it's still good enough足夠 for us to go there
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火星是一個差的行星但它仍可接受
03:09
and to live生活 on its surface表面 if we're protected保護.
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如果我們受到保護就可以住在它的表面
03:11
But Venus金星 is a very bad -- the worst最差 -- planet行星.
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但金星很差-最差-的行星
03:14
Even though雖然 it's Earth-like類似地球, and even though雖然 early in its history歷史
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就算它外表像地球,就算它以前
03:17
it may可能 very well have harbored懷著 Earth-like類似地球 life,
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可能有海洋生態
03:20
it soon不久 succumbed屈服於 to runaway逃跑 greenhouse溫室 --
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它最終敗合一發不可收拾的溫室效應
03:23
that's an 800 degrees [Fahrenheit飛輪海] surface表面 --
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攝氏800度的表面
03:25
because of rampant猖獗 carbon dioxide二氧化碳.
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因為二氧化碳的泛濫
03:28
Well, we know from astrobiology天體生物學 that we can really now predict預測
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我們從天體生物學裡能預測
03:31
what's going to happen發生 to our particular特定 planet行星.
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地球將會發生的事
03:34
We are right now in the beautiful美麗 Oreo奧利奧
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我們正處於這漂亮的Oreo時期
03:37
of existence存在 -- of at least最小 life on Planet行星 Earth地球 --
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可能是地球上最後存在的生物
03:40
following以下 the first horrible可怕 microbial微生物 age年齡.
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接著是可怕的微生物時代
03:43
In the Cambrian寒武紀的 explosion爆炸, life emerged出現 from the swamps沼澤,
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寒武紀大爆發時生物從沼澤出來
03:46
complexity複雜 arose出現,
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成為更複雜的生物
03:48
and from what we can tell, we're halfway through通過.
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由此可見我們己經歷了一半
03:51
We have as much time for animals動物 to exist存在 on this planet行星
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動物在地球上一早生存著
03:54
as they have been here now,
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就如現況
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till直到 we hit擊中 the second第二 microbial微生物 age年齡.
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直至我們經歷第二次微生物時代
03:58
And that will happen發生, paradoxically自相矛盾 --
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接著反常態的情況-
04:00
everything you hear about global全球 warming變暖 --
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所有你聽到有關全球暖化-
04:02
when we hit擊中 COCO2 down to 10 parts部分 per million百萬,
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當減少二氧化碳到百萬分之十
04:05
we are no longer going to have to have plants植物
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我們便不再有植物
04:07
that are allowed允許 to have any photosynthesis光合作用, and there go animals動物.
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產生光合作用,然後動物也沒有
04:11
So, after that we probably大概 have seven billion十億 years年份.
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之後估計我們會有70億年時間
04:13
The Sun太陽 increases增加 in its intensity強度, in its brightness亮度,
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太陽會更猛烈更光
04:16
and finally最後, at about 12 billion十億 years年份 after it first started開始,
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最後,120億年後
04:21
the Earth地球 is consumed消費 by a large Sun太陽,
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地球會被太陽取代
04:24
and this is what's left.
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這是所剩下的
04:27
So, a planet行星 like us is going to have an age年齡 and an old age年齡,
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因行星就如我們有年輕和年老
04:31
and we are in its golden金色 summer夏季 age年齡 right now.
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而我們正處於它的黃金時期
04:35
But there's two fates命運 to everything, isn't there?
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但凡事都有兩面不是嗎?
04:37
Now, a lot of you are going to die of old age年齡,
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很多人都在年老時才去世
04:40
but some of you, horribly可怕 enough足夠, are going to die in an accident事故.
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但有些人,很慘,因他們是死於意外
04:43
And that's the fate命運 of a planet行星, too.
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這也是行星的命運
04:45
Earth地球, if we're lucky幸運 enough足夠 -- if it doesn't get hit擊中 by a Hale-Bopp海爾 - 波普,
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如果我們夠幸運,在未來70億年內不被彗星Hale-Bopp
04:49
or gets得到 blasted炮轟 by some supernova超新星 nearby附近
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或附近的超新星擊中
04:53
in the next下一個 seven billion十億 years年份 -- we'll find under your feet.
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我們腳下的地球仍在
04:56
But what about accidental偶然 death死亡?
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但那意外性的死亡呢?
04:58
Well, paleontologists古生物學家 for the last 200 years年份
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古生物學家在過去200年
05:00
have been charting製圖 death死亡. It's strange奇怪 --
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不斷記錄死亡數據. 很奇怪
05:02
extinction滅絕 as a concept概念 wasn't even thought about
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沒有人對絕種這概念有深入研究
05:05
until直到 Baron男爵 Cuvier居維葉 in France法國 found發現 this first mastodon乳齒象.
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直至法國的Baron Cuvier 發現第一隻乳齒象
05:08
He couldn't不能 match比賽 it up to any bones骨頭 on the planet行星,
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他不能找到地球上找到相類似的骸骨
05:10
and he said, Aha! It's extinct絕種.
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所以他說:呀哈!這已經絕種
05:12
And very soon不久 after, the fossil化石 record記錄 started開始 yielding生產
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不久,化石記錄變得更齊全
05:15
a very good idea理念 of how many許多 plants植物 and animals動物 there have been
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有一個很好的主意,估計多少種動植物
05:18
since以來 complex複雜 life really began開始 to leave離開
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只從複雜的生命體開始留下
05:20
a very interesting有趣 fossil化石 record記錄.
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一些很有趣的化石記錄
05:23
In that complex複雜 record記錄 of fossils化石,
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在這齊全的化石記錄
05:26
there were times when lots of stuff東東
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發現有很多物種
05:28
seemed似乎 to be dying垂死 out very quickly很快,
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很快便全部死亡
05:30
and the father父親/mother母親 geologists地質學家
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地質學家"之父"或"之母"
05:32
called these "mass extinctions滅絕."
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稱此為"大滅絕"
05:34
All along沿 it was thought to be either an act法案 of God
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有人猜想這可能是神的作為
05:36
or perhaps也許 long, slow climate氣候 change更改,
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或許是更漫長的氣候變化
05:38
and that really changed in 1980,
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直到1980年有了改變
05:40
in this rocky岩石 outcrop露出 near Gubbio古比奧,
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在古比奧附近的岩石面
05:43
where Walter沃爾特 Alvarez阿爾瓦雷斯, trying to figure數字 out
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Walter Alvarez希望在這裡弄清楚
05:46
what was the time difference區別 between之間 these white白色 rocks岩石,
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這些白色的岩石是出現在那個時期
05:49
which哪一個 held保持 creatures生物 of the Cretaceous白堊紀 period,
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那些岩石是白堊時期
05:51
and the pink rocks岩石 above以上, which哪一個 held保持 Tertiary第三 fossils化石.
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有些粉色的是第三紀化石.
05:53
How long did it take to go from one system系統 to the next下一個?
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從一個時期到另一個需要多長時間?
05:57
And what they found發現 was something unexpected意外.
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他們發現一些意料之外的事
05:59
They found發現 in this gap間隙, in between之間, a very thin clay粘土 layer,
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他們發現有一個隙縫中有一層很薄的黏土層
06:02
and that clay粘土 layer -- this very thin red layer here --
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那黏土層有一層很薄的紅色表層
06:05
is filled填充 with iridium.
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裡面充滿銥
06:07
And not just iridium; it's filled填充 with glassy spherules小球,
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不單止銥; 還有玻璃球粒
06:10
and it's filled填充 with quartz石英 grains穀物
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和石英顆粒
06:12
that have been subjected to enormous巨大 pressure壓力: shock休克 quartz石英.
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曾遭受很大的壓力壓下去:撞擊石英
06:16
Now, in this slide滑動 the white白色 is chalk粉筆,
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在這投影片白色的部分是白堊
06:18
and this chalk粉筆 was deposited沉積 in a warm ocean海洋.
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白堊是在溫暖的海洋沈澱
06:21
The chalk粉筆 itself's本身是 composed by plankton浮游生物
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由浮游生物組成
06:23
which哪一個 has fallen墮落 down from the sea surface表面 onto the sea floor地板,
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浮游生物由海面沉到海底
06:27
so that 90 percent百分 of the sediment沉澱 here is skeleton骨架 of living活的 stuff東東,
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所以有九成的沈積物是生物的骸骨
06:30
and then you have that millimeter-thick毫米厚 red layer,
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你們看見幾毫米厚的紅色層
06:32
and then you have black黑色 rock.
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然後是黑色的石頭
06:34
And the black黑色 rock is the sediment沉澱 on the sea bottom底部
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黑石頭是海藏的沉積物
06:37
in the absence缺席 of plankton浮游生物.
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並沒有浮游生物
06:39
And that's what happens發生 in an asteroid小行星 catastrophe災難,
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小行星撞擊地球時,
06:43
because that's what this was, of course課程. This is the famous著名 K-TKT.
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就是因為這事,當然就是著名的K-T
06:46
A 10-kilometer-公里 body身體 hit擊中 the planet行星.
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一個十公里大的星體撞擊行星.
06:48
The effects效果 of it spread傳播 this very thin impact碰撞 layer all over the planet行星,
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這現象導致全個行星蒙一層薄薄的土層
06:52
and we had very quickly很快 the death死亡 of the dinosaurs恐龍,
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之後恐龍開始死亡
06:55
the death死亡 of these beautiful美麗 ammonites,
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還有這些美麗的鸚鵡螺化石
06:57
LeconteicerasLeconteiceras here, and CelaecerasCelaeceras over here,
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這是Leconteiceras,那是Celaeceras(兩者都是化石的一種)
06:59
and so much else其他.
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還有很多
07:01
I mean, it must必須 be true真正,
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我意思是,這肯定是真的
07:03
because we've我們已經 had two Hollywood好萊塢 blockbusters大片 since以來 that time,
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因從那時起荷里活有兩套風靡一時的電影
07:06
and this paradigm範例, from 1980 to about 2000,
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這例子在1980 至2000年期間
07:09
totally完全 changed how we geologists地質學家 thought about catastrophes災難.
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完全改變了地質學家對行星撞擊的想法
07:14
Prior to that, uniformitarianism均變 was the dominant優勢 paradigm範例:
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之前均變說是主要的學說:
07:17
the fact事實 that if anything happens發生 on the planet行星 in the past過去,
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事實是如果行星以前發生了什麼事
07:20
there are present-day今天 processes流程 that will explain說明 it.
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都會成為當代的理論
07:24
But we haven't沒有 witnessed目擊 a big asteroid小行星 impact碰撞,
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但我們沒有親眼目睹一個大的小行星撞擊的影響
07:27
so this is a type類型 of neo-catastrophism新災變,
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這是新災變論其中一種
07:29
and it took about 20 years年份 for the scientific科學 establishment編制
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科學家用了20年的時間才能
07:32
to finally最後 come to grips交手: yes, we were hit擊中;
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確定:是, 地球曾被撞擊
07:34
and yes, the effects效果 of that hit擊中 caused造成 a major重大的 mass extinction滅絕.
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而這撞擊導致大滅絕
07:39
Well, there are five major重大的 mass extinctions滅絕
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一共有五次主要的大滅絕
07:41
over the last 500 million百萬 years年份, called the Big Five.
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在過去的五億年, 它們被稱為 Big Five (大五)
07:44
They range範圍 from 450 million百萬 years年份 ago
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由4.5億年前
07:47
to the last, the K-TKT, number four,
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到最後, K-T, 第四個
07:49
but the biggest最大 of all was the P, or the Permian二疊紀 extinction滅絕,
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但最嚴重是P, 或作二疊紀滅絕
07:53
sometimes有時 called the mother母親 of all mass extinctions滅絕.
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有時被稱為大滅絕之母
07:55
And every一切 one of these has been subsequently後來 blamed指責
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而每次大滅絕也歸咎於
07:58
on large-body大身 impact碰撞.
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龐大行星帶來的影響
08:00
But is this true真正?
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但是否屬實?
08:03
The most recent最近, the Permian二疊紀, was thought to have been an impact碰撞
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最近二疊紀滅絕有個影響
08:06
because of this beautiful美麗 structure結構體 on the right.
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因這右面美麗的生物
08:08
This is a Buckminsterfullerene富勒烯, a carbon-碳-60.
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這是巴克敏斯特富勒烯,碳60的一種
08:11
Because it looks容貌 like those terrible可怕 geodesic domes圓頂
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因它看來像我60年代心愛的
08:14
of my late晚了 beloved心愛 '60s,
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網狀球頂
08:16
they're called "buckyballs巴基球."
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他們叫作巴克球
08:18
This evidence證據 was used to suggest建議
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這證據通常指出
08:20
that at the end結束 of the Permian二疊紀, 250 million百萬 years年份 ago, a comet彗星 hit擊中 us.
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在二疊紀的後期,2500萬年, 一顆彗星打中地球
08:24
And when the comet彗星 hits點擊, the pressure壓力 produces產生 the buckyballs巴基球,
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當彗星撞擊地球,壓力產生巴克球
08:27
and it captures捕獲 bits of the comet彗星.
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它捉住了少許彗星的尾巴
08:29
Helium-氦-3: very rare罕見 on the surface表面 of the Earth地球, very common共同 in space空間.
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氦-3:在地球上很罕有,在太空卻常見
08:34
But is this true真正?
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但是否屬實?
08:36
In 1990, working加工 on the K-TKT extinction滅絕 for 10 years年份,
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1990年,用了十年鑽研K-T 絕種
08:40
I moved移動 to South Africa非洲 to begin開始 work twice兩次 a year
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一年兩次我會搬到南非卡魯沙漠
08:43
in the great Karoo卡魯 desert沙漠.
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工作
08:45
I was so lucky幸運 to watch the change更改 of that South Africa非洲
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我很幸運能看到南非轉變
08:48
into the new South Africa非洲 as I went year by year.
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成一個新的南非因我每年都去
08:51
And I worked工作 on this Permian二疊紀 extinction滅絕,
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我研究二疊紀絕種
08:53
camping露營 by this Boer波爾 graveyard墓地 for months個月 at a time.
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在波爾墓地露宿了幾個月
08:56
And the fossils化石 are extraordinary非凡.
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那裡的化石很特別
08:59
You know, you're gazing凝視 upon your very distant遙遠 ancestors祖先.
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你知道嗎,你在注視著遙遠的祖先
09:01
These are mammal-like哺乳動物樣 reptiles爬行動物.
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他們都是類似哺乳動物的爬蟲
09:03
They are culturally文化 invisible無形. We do not make movies電影 about these.
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他們的文化已消失了, 所以我們不能拍有關他們的電影
09:06
This is a Gorgonopsian麗齒獸亞目, or a Gorgon芡實.
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這是Gorgonopsian (一種爬行動物),也叫Gorgon
09:08
That's an 18-inch-英寸 long skull頭骨 of an animal動物
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這是一隻動物18寸長的頭骨
09:12
that was probably大概 seven or eight feet, sprawled like a lizard蜥蜴,
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大概7-8尺, 四肢爬起來像一隻蜥蜴
09:16
probably大概 had a head like a lion獅子.
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大概頭像獅子
09:18
This is the top最佳 carnivore肉食動物, the T-RexT-雷克斯 of its time.
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這是頂級食肉動物, 在那時期是T-Rex
09:20
But there's lots of stuff東東.
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但還有很多東西
09:22
This is my poor較差的 son兒子, Patrick帕特里克.
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這是我可憐的兒子 Patrick
09:24
(Laughter笑聲)
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(眾笑)
09:25
This is called paleontological古生物 child兒童 abuse濫用.
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這叫作古生物式的兒童虐待
09:28
Hold保持 still, you're the scale規模.
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別動, 你要作標準尺
09:30
(Laughter笑聲)
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(眾笑)
09:36
There was big stuff東東 back then.
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後面還有很多
09:39
Fifty-five五十五 species種類 of mammal-like哺乳動物樣 reptiles爬行動物.
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55種類似哺乳動物的爬蟲
09:42
The age年齡 of mammals哺乳動物 had well and truly started開始
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哺乳動物時代已經開始
09:45
250 million百萬 years年份 ago ...
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由2500萬年前開始
09:47
... and then a catastrophe災難 happened發生.
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然後有一個災難發生
09:50
And what happens發生 next下一個 is the age年齡 of dinosaurs恐龍.
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接著是恐龍時代
09:52
It was all a mistake錯誤; it should have never happened發生. But it did.
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這完全是一個錯失, 事情不應這樣發生,卻發生了
09:56
Now, luckily,
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幸運地
09:58
this Thrinaxodon三尖叉齒獸屬, the size尺寸 of a robin知更鳥 egg here:
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這蛇頸龍,羅賓蛋的體積
10:01
this is a skull頭骨 I've discovered發現 just before taking服用 this picture圖片 --
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在拍照前我發現這骸骨
10:04
there's a pen鋼筆 for scale規模; it's really tiny --
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這鉛筆作比較,可見它很細小
10:06
this is in the Lower降低 Triassic三疊紀, after the mass extinction滅絕 has finished.
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這是下三疊統,大滅絕之後結束
10:10
You can see the eye socket插座 and you can see the little teeth in the front面前.
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你可以見到眼窩和前面的小牙齒
10:13
If that does not survive生存, I'm not the thing giving this talk.
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如果這沒生存過,今天我不會在此分享
10:18
Something else其他 is, because if that doesn't survive生存, we are not here;
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另一點是,如果它沒有生存過,我們不會在此
10:22
there are no mammals哺乳動物. It's that close; one species種類 ekesEKES through通過.
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這裡不會有哺乳動物, 很近, 一個物種之隔
10:26
Well, can we say anything about the pattern模式 of who survives生存 and who doesn't?
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那我們可以說有一個模式決定誰生存嗎?
10:29
Here's這裡的 sort分類 of the end結束 of that 10 years年份 of work.
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這差不多十年的工作
10:31
The ranges範圍 of stuff東東 -- the red line is the mass extinction滅絕.
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還有其他--紅色線代表大滅絕
10:34
But we've我們已經 got survivors倖存者 and things that get through通過,
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但我們發現有大滅絕的生還者
10:36
and it turns out the things that get through通過 preferentially優先 are cold bloods血液.
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其中優先生還都是冷血動物
10:40
Warm-blooded溫血的 animals動物 take a huge巨大 hit擊中 at this time.
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恒溫的動物卻無法生存
10:45
The survivors倖存者 that do get through通過
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能經過大滅絕的生還者
10:47
produce生產 this world世界 of crocodile-like鱷魚一樣 creatures生物.
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繁殖了類似鱷魚的生物
10:50
There's no dinosaurs恐龍 yet然而; just this slow, saurian蜥蜴, scaly有鱗的, nasty討厭,
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未有恐龍,只有這種又慢又蜥蜴狀的又有鱗又惡心的
10:54
swampy沼澤的 place地點 with a couple一對 of tiny mammals哺乳動物 hiding in the fringes條紋.
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沼澤地方有些細小的哺乳動物在邊緣之間躲藏著
10:59
And there they would hide隱藏 for 160 million百萬 years年份,
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牠們能躲藏1600萬年
11:02
until直到 liberated解放 by that K-TKT asteroid小行星.
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直至K-T小行星幫牠們擺脫約束
11:05
So, if not impact碰撞, what?
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如果不是影響,是什麼?
11:07
And the what, I think, is that we returned, over and over again,
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我想我們會不斷重複又重複經歷
11:11
to the Pre-Cambrian前寒武紀 world世界, that first microbial微生物 age年齡,
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前寒武紀, 第一個微生物時代
11:14
and the microbes微生物 are still out there.
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微生物還存在
11:16
They hate討厭 we animals動物.
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它們討厭我們這些動物
11:18
They really want their world世界 back.
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它們很想要回自己的地方
11:20
And they've他們已經 tried試著 over and over and over again.
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而它們也不斷不斷地嘗試
11:24
This suggests提示 to me that life causing造成 these mass extinctions滅絕
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這提起我導致大滅絕的生命
11:27
because it did is inherently本質 anti-Gaian抗蓋亞.
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因這是反生態的固有天性
11:30
This whole整個 Gaia蓋亞 idea理念, that life makes品牌 the world世界 better for itself本身 --
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這個生態主意,是生命會改變環境使它們更適應
11:35
anybody任何人 been on a freeway高速公路 on a Friday星期五 afternoon下午 in Los洛杉磯 Angeles洛杉磯
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有無人星期五下在洛杉磯的高速公路上
11:39
believing相信 in the Gaia蓋亞 theory理論? No.
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相信生態主意?沒有
11:41
So, I really suspect疑似 there's an alternative替代,
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所以我懷疑有另一種可能性
11:44
and that life does actually其實 try to do itself本身 in --
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生命真的有嘗試自己做
11:46
not consciously自覺, but just because it does.
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不是有意識地,只是它確實如此
11:48
And here's這裡的 the weapon武器, it seems似乎, that it did so over the last 500 million百萬 years年份.
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這個是武器,好像有5億年歷史
11:52
There are microbes微生物 which哪一個, through通過 their metabolism代謝,
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微生物會透過新陳代謝
11:55
produce生產 hydrogen sulfide硫化物,
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生產硫化氫
11:57
and they do so in large amounts.
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它們能大量生產
12:00
Hydrogen sulfide硫化物 is very fatal致命 to we humans人類.
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硫化氫對人類是致命的
12:03
As small as 200 parts部分 per million百萬 will kill you.
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只需每百萬分之200就可以殺死你
12:09
You only have to go to the Black黑色 Sea and a few少數 other places地方 -- some lakes湖泊 --
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你只需要去黑海和一些湖
12:13
and get down, and you'll你會 find that the water itself本身 turns purple紫色.
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然後落水,便會發現水變成紫色
12:17
It turns purple紫色 from the presence存在 of numerous眾多 microbes微生物
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因大量的微生物存在而變成紫色
12:20
which哪一個 have to have sunlight陽光 and have to have hydrogen sulfide硫化物,
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但首先需要陽光和硫化氫
12:23
and we can detect檢測 their presence存在 today今天 -- we can see them --
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今天我們仍能察覺它們, 我們能看見它們
12:27
but we can also detect檢測 their presence存在 in the past過去.
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我們也能察覺以前的它們
12:29
And the last three years年份 have seen看到
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前三年
12:31
an enormous巨大 breakthrough突破 in a brand-new全新的 field領域.
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在全新的領域上有一個重大的突破
12:34
I am almost幾乎 extinct絕種 --
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我差不多絕種
12:36
I'm a paleontologist古生物學家 who collects收集 fossils化石.
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我是一個搜集化石的古生物學者
12:38
But the new wave of paleontologists古生物學家 -- my graduate畢業 students學生們 --
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但新的古生物學者浪潮, 我已畢業的學生
12:41
collect蒐集 biomarkers生物標記物.
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搜集生物標誌物
12:43
They take the sediment沉澱 itself本身, they extract提取 the oil from it,
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他們拿了沉澱物,把裡面的油提煉出來
12:47
and from that they can produce生產 compounds化合物
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然後再製成複合物
12:49
which哪一個 turn out to be very specific具體 to particular特定 microbial微生物 groups.
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這複合物對某些微生物是很特別
12:53
It's because lipids血脂 are so tough強硬, they can get preserved罐頭 in sediment沉澱
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因脂質很硬,能保存在沉澱物中
12:57
and last the hundreds數以百計 of millions百萬 of years年份 necessary必要,
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如有需要能保存過千萬年
13:00
and be extracted提取 and tell us who was there.
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再被我們提煉出來
13:02
And we know who was there. At the end結束 of the Permian二疊紀,
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我們知道誰曾在那裡.二疊紀的最後期
13:05
at many許多 of these mass extinction滅絕 boundaries邊界,
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有很多類似的大滅絕界限裡
13:07
this is what we find: isorenierateneisorenieratene. It's very specific具體.
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找到: isorenieratene (化學物的一種),它很獨特
13:11
It can only occur發生 if the surface表面 of the ocean海洋 has no oxygen,
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它只能出現在沒有氧氣的海洋
13:15
and is totally完全 saturated飽和的 with hydrogen sulfide硫化物 --
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它完全被硫化氫飽和
13:18
enough足夠, for instance, to come out of solution.
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足夠的份量,例如,便會分解
13:21
This led Lee背風處 KumpKump酒店, and others其他 from Penn佩恩 State and my group,
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這是李·孔普, 其他人從賓夕法尼亞州立大學和我那隊
13:25
to propose提出 what I call the KumpKump酒店 Hypothesis假設:
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提出我名為孔普假設
13:28
many許多 of the mass extinctions滅絕 were caused造成 by lowering降低 oxygen,
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很多大滅絕都是因氧氣含量下降
13:31
by high COCO2. And the worst最差 effect影響 of global全球 warming變暖, it turns out:
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二氧化碳含量上升.最慘是全球暖化導致:
13:35
hydrogen sulfide硫化物 being存在 produced生成 out of the oceans海洋.
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硫化氫不斷在海洋裡產生
13:38
Well, what's the source資源 of this?
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源頭在那裡?
13:40
In this particular特定 case案件, the source資源 over and over has been flood洪水 basalts玄武岩.
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這事的源頭都是洪水玄武岩
13:44
This is a view視圖 of the Earth地球 now, if we extract提取 a lot of it.
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這是地球,如果我們提取從地球很多
13:47
And each of these looks容貌 like a hydrogen bomb炸彈;
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每個都像氫氣炸彈
13:49
actually其實, the effects效果 are even worse更差.
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其實,影響更加差
13:51
This is when deep-Earth深地球 material材料 comes to the surface表面,
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因當地球深層的物質移到表層
13:54
spreads利差 out over the surface表面 of the planet行星.
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就能廣散到行星的表面
13:56
Well, it's not the lava岩漿 that kills殺死 anything,
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不是熔岩殺死生物
13:59
it's the carbon dioxide二氧化碳 that comes out with it.
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而是從熔岩出來的二氧化碳
14:01
This isn't Volvos沃爾沃; this is volcanoes火山.
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這是火山
14:04
But carbon dioxide二氧化碳 is carbon dioxide二氧化碳.
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二氧化碳怎樣也是二氧化碳
14:07
So, these are new data數據 Rob Berner伯爾尼 and I -- from Yale耶魯 -- put together一起,
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這些新數據是我和Rob Berner 從耶魯裡放在一起
14:10
and what we try to do now is
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現在我們試著
14:12
track跟踪 the amount of carbon dioxide二氧化碳 in the entire整個 rock record記錄 --
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記錄二氧化碳在全部石頭裡的含量
14:15
and we can do this from a variety品種 of means手段 --
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我們可以用不同的方法
14:18
and put all the red lines here,
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把紅色的線放在一起
14:20
when these -- what I call greenhouse溫室 mass extinctions滅絕 -- took place地點.
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這就是我說溫室大滅絕發生的時刻
14:23
And there's two things that are really evident明顯 here to me,
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有兩樣對我來說是很可信的證據
14:25
is that these extinctions滅絕 take place地點 when COCO2 is going up.
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一是這絕種發生在二氧化碳含量上升時
14:28
But the second第二 thing that's not shown顯示 on here:
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第二樣未能在這裡顯示:
14:31
the Earth地球 has never had any ice on it
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地球上完全沒有冰
14:34
when we've我們已經 had 1,000 parts部分 per million百萬 COCO2.
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當有每百萬分之1000的二氧化碳
14:38
We are at 380 and climbing攀登.
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我們現在在380的水平,水平在上升
14:40
We should be up to a thousand in three centuries百年 at the most,
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我們在三個世紀便能升到1000的水平
14:43
but my friend朋友 David大衛 Battisti巴提斯蒂 in Seattle西雅圖 says he thinks a 100 years年份.
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但我在西雅圖的朋友David Battisti 認為只需100年
14:47
So, there goes the ice caps帽子,
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接著是冰冠
14:49
and there comes 240 feet of sea level水平 rise上升.
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如果水平線上升240呎
14:53
I live生活 in a view視圖 house now;
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我的屋外有境觀
14:55
I'm going to have waterfront濱水.
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我將會看到海旁區
14:57
All right, what's the consequence後果? The oceans海洋 probably大概 turn purple紫色.
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好,但結果是?海洋會變成紫色
15:01
And we think this is the reason原因 that complexity複雜 took so long
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我們以為這原因太複雜需要
15:04
to take place地點 on planet行星 Earth地球.
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很長時間才會在地球上發生
15:06
We had these hydrogen sulfide硫化物 oceans海洋 for a very great long period.
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我們有這些硫化氫的海洋已經很長時間
15:09
They stop complex複雜 life from existing現有.
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它們讓複雜的生命不再存在
15:13
We know hydrogen sulfide硫化物 is erupting爆發 presently目前 a few少數 places地方 on the planet行星.
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我們知道硫化氫正在侵蝕地球幾處地方
15:18
And I throw this slide滑動 in -- this is me, actually其實, two months個月 ago --
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我插入這投影片--這是兩個月前的我--
15:22
and I throw this slide滑動 in because here is my favorite喜愛 animal動物, chambered有房間的 nautilus鸚鵡螺.
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我放這投影片因是有我最喜歡的動物,鸚鵡螺
15:26
It's been on this planet行星 since以來 the animals動物 first started開始 -- 500 million百萬 years年份.
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它從5億年前就在在行星上
15:30
This is a tracking追踪 experiment實驗, and any of you scuba水肺 divers潛水員,
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這是一個追蹤實驗, 有無人是潛水員
15:33
if you want to get involved參與 in one of the coolest最酷 projects項目 ever,
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如因你想參與最酷的計劃
15:36
this is off the Great Barrier屏障 Reef.
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你就要到大堡礁
15:38
And as we speak說話 now,
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當我們在聊天
15:39
these nautilus鸚鵡螺 are tracking追踪 out their behaviors行為 to us.
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我們也在追蹤鸚鵡螺的行為
15:42
But the thing about this is that every一切 once一旦 in a while
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但是每隔一段時間
15:46
we divers潛水員 can run into trouble麻煩,
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潛水員便會遇到麻煩
15:48
so I'm going to do a little thought experiment實驗 here.
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所以我想現在做一些思想性實驗
15:50
This is a Great White白色 Shark鯊魚 that ate some of my traps陷阱.
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這是一條大白鯊吃掉我的魚餌
15:53
We pulled it up; up it comes. So, it's out there with me at night.
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我們拉它上來,它便來,到晚上便與我一起
15:56
So, I'm swimming游泳的 along沿, and it takes off my leg.
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我在游泳,它咬掉我的腿
15:59
I'm 80 miles英里 from shore支撐, what's going to happen發生 to me?
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我離岸80哩,我可以怎樣做?
16:02
Well now, I die.
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這樣的話我死定了
16:04
Five years年份 from now, this is what I hope希望 happens發生 to me:
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五年後, 我希望會發生在我身上:
16:06
I'm taken採取 back to the boat, I'm given特定 a gas加油站 mask面具:
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我被帶回船上, 有人給我面罩
16:09
80 parts部分 per million百萬 hydrogen sulfide硫化物.
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千萬分之80的硫化氫
16:12
I'm then thrown拋出 in an ice pond池塘, I'm cooled冷卻 15 degrees lower降低
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我被丟到冰湖,我的體溫降了15度
16:16
and I could be taken採取 to a critical危急 care關心 hospital醫院.
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我應該被帶到特級護理的醫院
16:20
And the reason原因 I could do that is because we mammals哺乳動物
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我能這樣做是因我們哺乳動物
16:22
have gone走了 through通過 a series系列 of these hydrogen sulfide硫化物 events事件,
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已經經歷過一連串硫化氫的事件
16:25
and our bodies身體 have adapted適應.
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我們的身體已經適應
16:27
And we can now use this as what I think will be a major重大的 medical breakthrough突破.
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這例子我認為可作為醫學上的大突破
16:31
This is Mark標記 Roth羅斯. He was funded資助 by DARPADARPA.
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他是Mark Roth,受DARPA贊助
16:33
Tried試著 to figure數字 out how to save保存 Americans美國人 after battlefield戰場 injuries受傷.
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想辦法救受戰傷的美國人
16:37
He bleeds出血 out pigs.
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他幫豬放血
16:39
He puts看跌期權 in 80 parts部分 per million百萬 hydrogen sulfide硫化物 --
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再灌入千萬分之八十的硫化氫--
16:42
the same相同 stuff東東 that survived倖存 these past過去 mass extinctions滅絕 --
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就是與以前大滅絕生還的東西一樣--
16:45
and he turns a mammal哺乳動物 into a reptile爬蟲.
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他由哺乳動物變成爬蟲類
16:47
"I believe we are seeing眼看 in this response響應 the result結果 of mammals哺乳動物 and reptiles爬行動物
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"我相信這反應是哺乳動物和爬蟲類
16:51
having undergone經歷 a series系列 of exposures曝光 to H2S."
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經過一連串在H2S暴露的結果"
16:54
I got this email電子郵件 from him two years年份 ago;
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我兩年前收到他的電郵
16:56
he said, "I think I've got an answer回答 to some of your questions問題."
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他說"我想你的問題我有了答案"
16:59
So, he now has taken採取 mice老鼠 down
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所以他現在用老鼠作實驗
17:01
for as many許多 as four hours小時, sometimes有時 six hours小時,
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一試就4小時,有時甚至6小時
17:05
and these are brand-new全新的 data數據 he sent發送 me on the way over here.
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於是有全新數據傳送給我
17:07
On the top最佳, now, that is a temperature溫度 record記錄 of a mouse老鼠 who has gone走了 through通過 --
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最上面,是一隻老鼠的溫度記錄,經過
17:12
the dotted line, the temperatures溫度.
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虛線,溫度
17:14
So, the temperature溫度 starts啟動 at 25 centigrade攝氏,
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溫度由攝氏25度開始
17:16
and down it goes, down it goes.
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不斷下降
17:17
Six hours小時 later後來, up goes the temperature溫度.
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6小時後,溫度上升
17:19
Now, the same相同 mouse老鼠 is given特定 80 parts部分 per million百萬 hydrogen sulfide硫化物
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同一隻老鼠現在給牠千萬分之八十的硫化氫
17:24
in this solid固體 graph圖形,
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在這固體圖
17:26
and look what happens發生 to its temperature溫度.
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看溫度的轉變
17:28
Its temperature溫度 drops滴劑.
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牠的體溫下降
17:30
It goes down to 15 degrees centigrade攝氏 from 35,
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由35度下降到15度
17:34
and comes out of this perfectly完美 fine.
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但完全無事
17:37
Here is a way we can get people to critical危急 care關心.
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這就是我們帶人到特級護理
17:40
Here's這裡的 how we can bring帶來 people cold enough足夠 to last till直到 we get critical危急 care關心.
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這也是如何使人凍到要帶入特級護理的時候
17:46
Now, you're all thinking思維, yeah, what about the brain tissue組織?
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你們全在想,對,那腦細胞呢?
17:50
And so this is one of the great challenges挑戰 that is going to happen發生.
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這是最富挑戰性
17:53
You're in an accident事故. You've got two choices選擇:
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你在一個意外. 你有兩個選擇:
17:55
you're going to die, or you're going to take the hydrogen sulfide硫化物
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你就快死或你就快要吸入硫化氫
17:58
and, say, 75 percent百分 of you is saved保存, mentally精神上.
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當中75%生還,只是精神上
18:01
What are you going to do?
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那你怎樣辦?
18:03
Do we all have to have a little button按鍵 saying, Let me die?
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那我們可能要有個按鈕說:讓我死?
18:06
This is coming未來 towards us,
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這正朝著我們
18:08
and I think this is going to be a revolution革命.
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我想這會是一塲革命
18:10
We're going to save保存 lives生活, but there's going to be a cost成本 to it.
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我們要拯救生命,但這是在代價的
18:13
The new view視圖 of mass extinctions滅絕 is, yes, we were hit擊中,
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這是大滅絕的一個新觀點,對,我們被撞中
18:15
and, yes, we have to think about the long term術語,
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對,我們要向長遠方向想
18:17
because we will get hit擊中 again.
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因我們可能再被撞中
18:19
But there's a far worse更差 danger危險 confronting面對 us.
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但我們面對著更危險的事
18:21
We can easily容易 go back to the hydrogen sulfide硫化物 world世界.
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我們很容易回到硫化氫的世界
18:24
Give us a few少數 millennia千年 --
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給我們幾千年 -
18:26
and we humans人類 should last those few少數 millennia千年 --
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我們人類應該可活多幾千年 --
18:28
will it happen發生 again? If we continue繼續, it'll它會 happen發生 again.
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會再發生嗎?如果我們繼續,它會再次發生
18:32
How many許多 of us flew here?
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有多少人在這裡?
18:34
How many許多 of us have gone走了 through通過
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在這有多少人經歷迥
18:36
our entire整個 Kyoto京都 quota配額
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整過京都配額
18:39
just for flying飛行 this year?
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只是今年飛行?
18:41
How many許多 of you have exceeded突破 it? Yeah, I've certainly當然 exceeded突破 it.
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有多少人已經超過? 我就一定已經超過
18:44
We have a huge巨大 problem問題 facing面對 us as a species種類.
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我們作為一個物種正面對很大的難題
18:47
We have to beat擊敗 this.
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我們要擊敗它
18:49
I want to be able能夠 to go back to this reef. Thank you.
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我希望能夠回到這珊瑚礁. 多謝
18:53
(Applause掌聲)
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(掌聲)
18:59
Chris克里斯 Anderson安德森: I've just got one question for you, Peter彼得.
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克里斯安德森 (CA): 我有條問題給你,彼得
19:01
Am I understanding理解 you right, that what you're saying here
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我是否理解正確,你是說
19:03
is that we have in our own擁有 bodies身體
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我們體內
19:05
a biochemical生化 response響應 to hydrogen sulfide硫化物
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對硫化氫有生化反應
19:09
that in your mind心神 proves證明 that there have been past過去 mass extinctions滅絕
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你的思想證明以前的大滅絕
19:12
due應有 to climate氣候 change更改?
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都是因氣候變化而形成?
19:14
Peter彼得 Ward病房: Yeah, every一切 single cell細胞 in us
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彼得沃德(PW):對,我們每個細胞
19:16
can produce生產 minute分鐘 quantities數量 of hydrogen sulfide硫化物 in great crises危機.
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在遇到大危機時都能產生一定數量的硫化氫
19:20
This is what Roth羅斯 has found發現 out.
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這是羅斯所找到的
19:21
So, what we're looking at now: does it leave離開 a signal信號?
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所以現在我們要探究:它有無剩下一個?
19:23
Does it leave離開 a signal信號 in bone or in plant?
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它有無剩下一個在骨頭裡或植物裡?
19:25
And we go back to the fossil化石 record記錄 and we could try to detect檢測
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當我們看化石報告,我們嘗試偵測
19:28
how many許多 of these have happened發生 in the past過去.
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有多少發生在在以前
19:30
CACA: It's simultaneously同時
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CA: 同時
19:32
an incredible難以置信 medical technique技術, but also a terrifying可怕的 ...
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這是令人難以置信的醫學技術,卻又好可怕
19:35
PWPW: Blessing祝福 and curse詛咒.
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PW: 是福又是禍
Translated by Joyce Leung
Reviewed by Felix Leung

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ABOUT THE SPEAKER
Peter Ward - Paleontologist
Peter D. Ward studies life on Earth -- where it came from, how it might end, and how utterly rare it might be.

Why you should listen

Paleontologist and astrobiologist Peter D. Ward studies the Cretaceous-Tertiary extinction event (the one that killed the dinosaurs) and other mass extinctions. He is a leader in the intriguing new field of astrobiology, the study of the origin, distribution and evolution of life in the universe.

In his book Rare Earth he theorizes that complex life itself is so rare, it's quite possible that Earth is the only planet that has any. But, he theorizes, simple life may exist elsewhere -- and possibly be more common than we think.

His upcoming book, The Medea Hypothesis, makes a bold argument that even here on Earth, life has come close to being wiped out several times. Contrary to the "Gaia hypothesis" of a self-balancing, self-perpetuating circle of life, Ward's Medea hypothesis details the scary number of times that life has come close to flatlining, whether due to comet strikes or an overabundance of bacteria.

In March 2009, Ward's 8-hour television series, Animal Armageddon, premieres on Animal Planet Network.

In April 2013, Ward published a surprisingly moving essay about his life's obsession: the chambered nautilus >>

More profile about the speaker
Peter Ward | Speaker | TED.com

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