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  • Well, I'm an ocean chemist.

    我是一個海洋化學家

  • I look at the chemistry of the ocean today.

    我關注現在的海洋變化

  • I look at the chemistry of the ocean in the past.

    我關注過去的海洋變化

  • The way I look back in the past

    我探索過去的法則

  • is by using the fossilized remains of deepwater corals.

    是利用已經變成化石的深海珊瑚的遺骸

  • You can see an image of one of these corals behind me.

    你可以看到在我身後 其中一張珊瑚的照片

  • It was collected from close to Antarctica, thousands of meters below the sea,

    我們在毗鄰南極洲幾千米之下的深海處找到它

  • so, very different than the kinds of corals

    因此 如果你在熱帶旅遊的時候能夠有幸看到一些珊瑚

  • you may have been lucky enough to see if you've had a tropical holiday.

    會發現二者很不一樣

  • So I'm hoping that this talk will give you

    我真誠地希望我的演說

  • a four-dimensional view of the ocean.

    能夠為你帶來一個四維的海洋

  • Two dimensions, such as this beautiful two-dimensional image

    二維的海洋

  • of the sea surface temperature.

    比如這張美麗的海洋表面溫度的二維的圖像

  • This was taken using satellite, so it's got tremendous spatial resolution.

    这是由卫星拍摄的 所以拥有极好的空间辨析度

  • The overall features are extremely easy to understand.

    图片上关于整体的特征极其容易了解

  • The equatorial regions are warm because there's more sunlight.

    赤道地区比较温暖 因为那裡接收了更多的阳光

  • The polar regions are cold because there's less sunlight.

    极地地区比较严寒 因为那裡光照稀少

  • And that allows big icecaps to build up on Antarctica

    这让巨大的冰盖在南极洲和北半球上部形成

  • and up in the Northern Hemisphere.

    如果你俯冲入深海之中 或者把你的脚趾放进海里

  • If you plunge deep into the sea, or even put your toes in the sea,

    你就知道越往下水温越低

  • you know it gets colder as you go down,

    那是大多是因为流動在海洋深處的海水

  • and that's mostly because the deep waters that fill the abyss of the ocean

    来自寒冷的极地地区 它们的密度更高

  • come from the cold polar regions where the waters are dense.

    如果我们進行時間旅行 回到两万年前

  • If we travel back in time 20,000 years ago,

    会发现地球看起来有很大不同

  • the earth looked very much different.

    如果你真的回到那麼久以前的地球

  • And I've just given you a cartoon version of one of the major differences

    将会看到我用图像给你们展现其中一个最大的不同之处

  • you would have seen if you went back that long.

    冰川面積更大

  • The icecaps were much bigger.

    它們覆蓋了很多的陸地 而且延伸到了海洋

  • They covered lots of the continent, and they extended out over the ocean.

    海平面比现在低了120米

  • Sea level was 120 meters lower.

    二氧化碳含量也比現在低了許多

  • Carbon dioxide [levels] were very much lower than they are today.

    所以可能全球平均氣溫要低了3到5度

  • So the earth was probably about three to five degrees colder overall,

    在極地地區要更加寒冷

  • and much, much colder in the polar regions.

    我希望了解的

  • What I'm trying to understand,

    我的其他同事們希望了解的

  • and what other colleagues of mine are trying to understand,

    是我們的地球怎麼從一個極寒的星球

  • is how we moved from that cold climate condition

    變成一個适宜人类居住的家園

  • to the warm climate condition that we enjoy today.

    通過對冰核的探索

  • We know from ice core research

    我們了解到這一個從嚴寒到溫暖的轉變過程並不平穩

  • that the transition from these cold conditions to warm conditions

    這也可以從緩慢增長的太陽輻射推測出來

  • wasn't smooth, as you might predict from the slow increase in solar radiation.

    而我們從冰核中得到這些結論

  • And we know this from ice cores, because if you drill down into ice,

    因為如果你鑽入到冰川深處

  • you find annual bands of ice, and you can see this in the iceberg.

    就能看到年復一年形成的冰層

  • You can see those blue-white layers.

    在冰川上它們肉眼可見

  • Gases are trapped in the ice cores, so we can measure CO2 --

    你能看到那些藍白相間的層

  • that's why we know CO2 was lower in the past --

    氣體被困在冰核之中

  • and the chemistry of the ice also tells us about temperature

    所以我們可以測量氣體中CO2的含量

  • in the polar regions.

    因此我們知道過去的CO2含量要低得多

  • And if you move in time from 20,000 years ago to the modern day,

    而且冰的元素組成

  • you see that temperature increased.

    也告訴我們過去極地的溫度信息

  • It didn't increase smoothly.

    如果你的思緒从20,000年前回到现在

  • Sometimes it increased very rapidly,

    你會發現溫度上升了

  • then there was a plateau,

    它提升得並不平穩

  • then it increased rapidly.

    有時候它迅速上升

  • It was different in the two polar regions,

    接著是穩定狀態

  • and CO2 also increased in jumps.

    然後再次迅速上升

  • So we're pretty sure the ocean has a lot to do with this.

    兩極的狀況有所不同

  • The ocean stores huge amounts of carbon,

    而CO2含量同樣猛漲

  • about 60 times more than is in the atmosphere.

    所以我們相當確定海洋影響了這個過程

  • It also acts to transport heat across the equator,

    海洋儲存了大量的碳元素

  • and the ocean is full of nutrients and it controls primary productivity.

    大約是空氣中的60倍

  • So if we want to find out what's going on down in the deep sea,

    海洋也影響了热量跨越赤道传播

  • we really need to get down there,

    而且它富有養分 控制了初級生產力

  • see what's there

    所以我們想弄明白深海中到底發生了什麼事情

  • and start to explore.

    我們真的需要下到那裡

  • This is some spectacular footage coming from a seamount

    看看有什麼事物

  • about a kilometer deep in international waters

    然後開始挖掘與探索

  • in the equatorial Atlantic, far from land.

    這是一些美麗的海丘的影像

  • You're amongst the first people to see this bit of the seafloor,

    在公海海域大概一千米深處

  • along with my research team.

    在鄰近赤道 遠離陸地的大西洋海域

  • You're probably seeing new species.

    你們是第一批看到這海底一隅的人

  • We don't know.

    和我的團隊一起

  • You'd have to collect the samples and do some very intense taxonomy.

    你可能已經看到了新物種

  • You can see beautiful bubblegum corals.

    也許吧

  • There are brittle stars growing on these corals.

    你需要收集樣本然後進行認真的分類

  • Those are things that look like tentacles coming out of corals.

    你可以看到美麗的泡泡珊瑚

  • There are corals made of different forms of calcium carbonate

    那裡有柔軟的海星生長在上面

  • growing off the basalt of this massive undersea mountain,

    那看起來就像珊瑚裡伸出了觸手

  • and the dark sort of stuff, those are fossilized corals,

    那裡有由各種形式的碳酸鈣組成的珊瑚

  • and we're going to talk a little more about those

    生長在巨大的海底玄武岩山脈上

  • as we travel back in time.

    而那些黑色物質是變成化石的珊瑚

  • To do that, we need to charter a research boat.

    隨著我們對過去的探究

  • This is the James Cook, an ocean-class research vessel

    我们也會對它們進行更多的討論

  • moored up in Tenerife.

    為了完成這件事 我們要租一艘科研船

  • Looks beautiful, right?

    這是James Cook 一艘遠洋探索船舶

  • Great, if you're not a great mariner.

    它停泊在特納夫利島

  • Sometimes it looks a little more like this.

    看起來美極了 對吧?

  • This is us trying to make sure that we don't lose precious samples.

    然而 如果你不是一名好的船員

  • Everyone's scurrying around, and I get terribly seasick,

    有時候情況更多是這樣的

  • so it's not always a lot of fun, but overall it is.

    為了不要錯過一個珍貴的樣本

  • So we've got to become a really good mapper to do this.

    所有人來回跑動 我劇烈地暈船

  • You don't see that kind of spectacular coral abundance everywhere.

    所以這並不總是很愉快的 但總體來說它是

  • It is global and it is deep,

    為了做這件事 我們必須成為非常優秀的製圖人

  • but we need to really find the right places.

    你不可能在所有地方都看到那樣壯觀的大片珊瑚

  • We just saw a global map, and overlaid was our cruise passage

    隻有在極少數的 深海的地方才能看到

  • from last year.

    但我們迫切地需要找到正確的地方

  • This was a seven-week cruise,

    我們參考一張標明去年巡遊路線的世界地圖

  • and this is us, having made our own maps

    這是一次持續七周的巡遊

  • of about 75,000 square kilometers of the seafloor in seven weeks,

    而這是我們自己製作的

  • but that's only a tiny fraction of the seafloor.

    關於75,000平方千米的海底的地圖

  • We're traveling from west to east,

    它是花費7周的成果

  • over part of the ocean that would look featureless on a big-scale map,

    但這只是海底很小的一部分

  • but actually some of these mountains are as big as Everest.

    我們從西邊走到東邊

  • So with the maps that we make on board,

    走過在過於簡略的世界地圖上看起來毫無特點的海洋

  • we get about 100-meter resolution,

    但事實上這些海洋底部的山脈與珠穆朗瑪峰一樣巨大

  • enough to pick out areas to deploy our equipment,

    有了這張我們在船上繪製的地圖

  • but not enough to see very much.

    我們得到了100米的分辨率

  • To do that, we need to fly remotely-operated vehicles

    足以讓我們選擇一個區域並布置我們的儀器

  • about five meters off the seafloor.

    但不足以讓我們看到太多的東西

  • And if we do that, we can get maps that are one-meter resolution

    為了看到更多 我們需要让遠程遙控機器人

  • down thousands of meters.

    遊動在大概距海底5米的地方

  • Here is a remotely-operated vehicle,

    如果我們這樣做

  • a research-grade vehicle.

    我們就能夠在數千米之下的海底得到1米的分辨率

  • You can see an array of big lights on the top.

    這是我們的遠程遙控機器人

  • There are high-definition cameras, manipulator arms,

    一個研究型的機器人媒介

  • and lots of little boxes and things to put your samples.

    你可以在它的頭上看到一列的大燈

  • Here we are on our first dive of this particular cruise,

    和高清攝像機以及人工機械臂

  • plunging down into the ocean.

    許多箱子之類的東西來收集樣品

  • We go pretty fast to make sure the remotely operated vehicles

    終於到了我們在這個特殊的巡遊中

  • are not affected by any other ships.

    第一次入海的時候

  • And we go down,

    猛潛入海洋

  • and these are the kinds of things you see.

    我們下潛地很快

  • These are deep sea sponges, meter scale.

    來保證機器人不會被任何其他船隻影響

  • This is a swimming holothurian -- it's a small sea slug, basically.

    然後我們持續下潛

  • This is slowed down.

    這就是在海水中你能夠看到的景象

  • Most of the footage I'm showing you is speeded up,

    這是一隻米級的深海海綿

  • because all of this takes a lot of time.

    一個正在海洋中徜徉的海參

  • This is a beautiful holothurian as well.

    本質上也就是一個小小的海洋鼻涕蟲

  • And this animal you're going to see coming up was a big surprise.

    這個影像被放慢了

  • I've never seen anything like this and it took us all a bit surprised.

    大多數我展現給你們的影像都是快進的

  • This was after about 15 hours of work and we were all a bit trigger-happy,

    因為所有的這些拍攝花費了大量的時間

  • and suddenly this giant sea monster started rolling past.

    這也是一個漂亮的海參

  • It's called a pyrosome or colonial tunicate, if you like.

    而這個將要出現的生物是給我們帶來了巨大的驚喜

  • This wasn't what we were looking for.

    我從來沒有見過這樣的生物 它讓我們都很驚訝

  • We were looking for corals, deep sea corals.

    在這時我們已經工作了15個小時 都處於亢奮的狀態

  • You're going to see a picture of one in a moment.

    突然這個巨大的海洋怪物蠕動着經過

  • It's small, about five centimeters high.

    它被稱為火體蟲 或者群體性被囊動物

  • It's made of calcium carbonate, so you can see its tentacles there,

    隨你怎麼叫

  • moving in the ocean currents.

    但是這不是我們在尋找的生物

  • An organism like this probably lives for about a hundred years.

    我們在尋找着珊瑚 深海的珊瑚

  • And as it grows, it takes in chemicals from the ocean.

    你將會看到一張深海珊瑚的照片

  • And the chemicals, or the amount of chemicals,

    它很小 大概只有5釐米高

  • depends on the temperature; it depends on the pH,

    它由碳酸鈣構成

  • it depends on the nutrients.

    你可以看到它的那些小觸手隨着洋流飄動

  • And if we can understand how these chemicals get into the skeleton,

    它大概已經生活了幾百年了

  • we can then go back, collect fossil specimens,

    當它生長的時候 它會吸收海洋中的元素

  • and reconstruct what the ocean used to look like in the past.

    而海洋中的元素種類

  • And here you can see us collecting that coral with a vacuum system,

    或者元素含量

  • and we put it into a sampling container.

    取決於溫度 取決於酸堿度

  • We can do this very carefully, I should add.

    也取決於海洋中的養分

  • Some of these organisms live even longer.

    如果我們能夠明白這些元素是怎麼進到珊瑚遺骨里的

  • This is a black coral called Leiopathes, an image taken by my colleague,

    我們就能通過收集化石樣品

  • Brendan Roark, about 500 meters below Hawaii.

    重新構建過去的海洋景觀

  • Four thousand years is a long time.

    現在你能夠看到我們在用真空吸器收集珊瑚

  • If you take a branch from one of these corals and polish it up,

    將它放進一個樣品收集箱

  • this is about 100 microns across.

    應當說明的是 我們非常小心地做這件事

  • And Brendan took some analyses across this coral --

    有些海底生物甚至活得更久

  • you can see the marks --

    這是一張珊瑚黑礁的照片

  • and he's been able to show that these are actual annual bands,

    是由我的同事Brendan Roark

  • so even at 500 meters deep in the ocean,

    在夏威夷海域500米水下拍攝的

  • corals can record seasonal changes,

    4000年很漫長

  • which is pretty spectacular.

    從這些珊瑚礁上取下一條枝條並將它處理乾淨

  • But 4,000 years is not enough to get us back to our last glacial maximum.

    它大概有100微米長

  • So what do we do?

    Brendan對這些珊瑚礁進行了一系列的分析

  • We go in for these fossil specimens.

    你們可以看到那些痕跡

  • This is what makes me really unpopular with my research team.

    他發現那真真切切是年齡層

  • So going along,

    所以即使生活在500米水深下

  • there's giant sharks everywhere,

    珊瑚也能夠記錄季節性變化

  • there are pyrosomes, there are swimming holothurians,

    這十分令人驚艷

  • there's giant sponges,

    但4000年還不足以讓我們回到末次冰盛期

  • but I make everyone go down to these dead fossil areas

    那麼我們該怎麼做呢?

  • and spend ages kind of shoveling around on the seafloor.

    我們要繼續收集化石樣品

  • And we pick up all these corals, bring them back, we sort them out.

    這讓我在我的隊伍里很不得人心

  • But each one of these is a different age,

    我們一直在海底前進

  • and if we can find out how old they are

    到處都是巨大的鯊魚

  • and then we can measure those chemical signals,

    有火體蟲 有遊動的海參

  • this helps us to find out

    有巨大的海綿

  • what's been going on in the ocean in the past.

    但是我讓所有人去到那死氣沉沉的化石區域

  • So on the left-hand image here,

    花上幾個世紀的時間時間 在海底鏟來鏟去

  • I've taken a slice through a coral, polished it very carefully

    然後我們帶回所有的珊瑚樣品 將它們分類

  • and taken an optical image.

    每一株珊瑚的年代都是不同的

  • On the right-hand side,

    但是如果我們能夠發現它們到底生活了多久

  • we've taken that same piece of coral, put it in a nuclear reactor,

    我們就能量化那些化學信號

  • induced fission,

    這幫助我們了解

  • and every time there's some decay,

    過去的海洋到底發生了什麼

  • you can see that marked out in the coral,

    所以在左邊的這張圖片

  • so we can see the uranium distribution.

    我從珊瑚上取下了一小片 並十分小心地清潔它

  • Why are we doing this?

    然後拍了一張光學圖像

  • Uranium is a very poorly regarded element,

    右邊這張圖

  • but I love it.

    我再取了這個珊瑚的一小片 把它放進核反應堆

  • The decay helps us find out about the rates and dates

    激發核裂變

  • of what's going on in the ocean.

    經過足夠長的時間它開始衰變

  • And if you remember from the beginning,

    你看到那些在珊瑚上的痕跡

  • that's what we want to get at when we're thinking about climate.

    是肉眼可見的珊瑚中鈾的分布

  • So we use a laser to analyze uranium

    我們為什麼要做這樣的事情呢?

  • and one of its daughter products, thorium, in these corals,

    鈾是一種很不常見的元素

  • and that tells us exactly how old the fossils are.

    但我愛死它了

  • This beautiful animation of the Southern Ocean

    它的衰變幫助我們了解海洋中事情發生的頻率和時間

  • I'm just going to use illustrate how we're using these corals

    如果你還記得的話

  • to get at some of the ancient ocean feedbacks.

    這就是我們為了探索氣候想要得到的數據

  • You can see the density of the surface water

    所以我們用激光去探測珊瑚中的鈾元素

  • in this animation by Ryan Abernathey.

    以及它的其中一個衰變產物釷

  • It's just one year of data,

    這能告訴我們這些化石的確切壽命

  • but you can see how dynamic the Southern Ocean is.

    這是一張美麗的南部海洋的動畫

  • The intense mixing, particularly the Drake Passage,

    我將會利用它來說明我們如何利用這些珊瑚

  • which is shown by the box,

    獲得遠古海洋的訊息

  • is really one of the strongest currents in the world

    在這個動圖中你可以看出表面海水的密度

  • coming through here, flowing from west to east.

    我的同事Ryan Abernathey製作了它

  • It's very turbulently mixed,

    上面隻展現了一年的數據

  • because it's moving over those great big undersea mountains,

    但你可以看到南部的海洋有多麼的活力四射

  • and this allows CO2 and heat to exchange with the atmosphere in and out.

    那些強烈的交匯

  • And essentially, the oceans are breathing through the Southern Ocean.

    特別是在圖中用黑色方框圈出來的大渡海的地區

  • We've collected corals from back and forth across this Antarctic passage,

    世界上最強的洋流之一

  • and we've found quite a surprising thing from my uranium dating:

    從那裡自西向東穿過

  • the corals migrated from south to north

    洶湧的洋流在那裡交匯

  • during this transition from the glacial to the interglacial.

    因為它們在那些巨大的海底山脈上方流動

  • We don't really know why,

    而這個過程讓CO2和熱量在海洋和大氣間交換

  • but we think it's something to do with the food source

    形象地說 就像海洋在通過南大洋呼吸著

  • and maybe the oxygen in the water.

    我們來來回回地在南極洲航路上收集珊瑚

  • So here we are.

    在對珊瑚的鈾年代測定中 發現了一件很令人驚訝的事情

  • I'm going to illustrate what I think we've found about climate

    這些珊瑚從南部遷徙到了北部

  • from those corals in the Southern Ocean.

    正在這個世界處於冰河期與間冰期的轉換期的時候

  • We went up and down sea mountains. We collected little fossil corals.

    我們不知道為什麼

  • This is my illustration of that.

    也許與食物來源有關

  • We think back in the glacial,

    或者是海水中的氧氣含量有關

  • from the analysis we've made in the corals,

    所以問題來了

  • that the deep part of the Southern Ocean was very rich in carbon,

    我會說明利用那些南大洋里的珊瑚

  • and there was a low-density layer sitting on top.

    我們到底發現了什麼

  • That stops carbon dioxide coming out of the ocean.

    我們徹底探索海底山脈

  • We then found corals that are of an intermediate age,

    收集那些小小的珊瑚化石

  • and they show us that the ocean mixed partway through that climate transition.

    那是我們的證據

  • That allows carbon to come out of the deep ocean.

    基於對珊瑚成分的分析

  • And then if we analyze corals closer to the modern day,

    我們認為在遙遠的冰河時期

  • or indeed if we go down there today anyway

    南大洋深處儲存了大量的碳元素

  • and measure the chemistry of the corals,

    但是有一層低密度的層覆蓋在那些碳元素上

  • we see that we move to a position where carbon can exchange in and out.

    阻止了CO2從海洋中釋放出來

  • So this is the way we can use fossil corals

    我們隨後找到了那些處於中間年齡的珊瑚樣本

  • to help us learn about the environment.

    它告訴我們海洋在氣候變化的中期匯合

  • So I want to leave you with this last slide.

    這讓碳元素從深海中被釋放

  • It's just a still taken out of that first piece of footage that I showed you.

    而如果我們分析現今的珊瑚成分

  • This is a spectacular coral garden.

    也就是下到海洋里去

  • We didn't even expect to find things this beautiful.

    并測量珊瑚的化學成分

  • It's thousands of meters deep.

    就會發現我們處於一個碳元素可以自由交換的年代

  • There are new species.

    我們利用珊瑚化石

  • It's just a beautiful place.

    幫助我們了解環境

  • There are fossils in amongst,

    所以我想為你展現著最後一張幻燈片

  • and now I've trained you to appreciate the fossil corals

    是一張一開始我呈現給你們的影像中的一張截圖

  • that are down there.

    這是一個壯觀的珊瑚王國

  • So next time you're lucky enough to fly over the ocean

    我們恐怕再也見不到比這還美麗的事物

  • or sail over the ocean,

    在幾千米的水下

  • just think -- there are massive sea mountains down there

    有新奇的物種

  • that nobody's ever seen before,

    那真是一個美麗的地方

  • and there are beautiful corals.

    那其中還有化石

  • Thank you.

    我剛剛告訴了你們海底化石的奧秘

  • (Applause)

    所以以後當你們飛越大洋

Well, I'm an ocean chemist.

我是一個海洋化學家

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B1 中級 中文 TED 海洋 深海 化石 元素 看到

【TED】勞拉-羅賓遜:我在神祕海底發現的祕密(The secrets I find on the mysterious ocean floor | Laura Robinson)。 (【TED】Laura Robinson: The secrets I find on the mysterious ocean floor (The secrets I find on the mysterious ocean floor | Laura Robinson))

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    richardwang 發佈於 2021 年 01 月 14 日
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