LauraRobinson_2014X[劳拉·罗宾逊][神秘海底世界的奥秘].pdf
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1、www.XiYuS锡育软件Well,Im an ocean chemist.我是一位海洋化学家。00:12I look at the chemistry of the ocean today.我研究现代海洋的化学特性。00:14I look at the chemistry of the ocean in the past.我也研究古代海洋的化学特性。00:16The way I look back in the past is by using the fossilizedremains of deepwater corals.我研究古代海洋的方式,是借助深海珊瑚的化石遗体。00:19You
2、 can see an image of one of these corals behind me.各位可以在我的背后看到这样一张图片。00:24It was collected from close to Antarctica,thousands of metersbelow the sea,so,very different than the kinds of corals youmay have been lucky enough to see if youve had a tropicalholiday.这是在南极洲附近,海平面以下的数千米处采集的。所以这些珊瑚跟其它种类非常不同,比
3、如说你去热带度假的时候有幸见到的一些。00:27So Im hoping that this talk will give you a four-dimensionalview of the ocean.我希望我的演讲能够为大家00:37Two dimensions,such as this beautiful two-dimensionalimage of the sea surface temperature.其中的两个维度,正如这个漂亮的平面图,描述了海平面的温度。00:41This was taken using satellite,so its got tremendous spat
4、ialresolution.这张照片是卫星拍摄的,所以有着极高的空间分辨率。00:47fossilized:adj.石化的;僵化的;老化的/v.石化(fossilize的过去式和过去分词)deepwater:adj.深海的 corals:n.无脊椎珊瑚(coral的复数)different than:不同于 four-dimensional:adj.四维的;四次元的 dimensions:n.规模,大小 two-dimensional:adj.二维的;缺乏深度的 tremendous:adj.极大的,巨大的;惊人的;极好的 spatial:adj.空间的;存在于空间的;受空间条件限制的The
5、overall features are extremely easy to understand.照片的大致内容是相当容易理解的。00:51The equatorial regions are warm because theres moresunlight.赤道地区比较温暖,因为接受的日照很多。00:54The polar regions are cold because theres less sunlight.极地比较寒冷,因为接受的日照较少。00:58And that allows big icecaps to build up on Antarctica and upin the
6、Northern Hemisphere.所以这就让南极洲的土地上生成了巨大的冰盖,同样还有北半球的顶部。01:01If you plunge deep into the sea,or even put your toes in thesea,you know it gets colder as you go down,and thatsmostly because the deep waters that fill the abyss of theocean come from the cold polar regions where the waters aredense.如果你深潜入大海里
7、,或者只是让脚趾头碰到海水,你就会知道越深处越寒冷,这主要是因为,填充海底沟壑的深海海水 是来自寒冷的极地地区,而那里的水密度更大。01:06If we travel back in time 20,000 years ago,the earth lookedvery much different.如果我们让时光倒流两万年,整个地球看上去非常不同。01:19And Ive just given you a cartoon version of one of the majordifferences you would have seen if you went back that long.我
8、刚刚给你们看的是其中一个巨大变化的漫画示意图,那个时代的景象就像这样。01:24The icecaps were much bigger.冰盖要比现在大很多。01:30They covered lots of the continent,and they extended outover the ocean.它们覆盖了大面积的陆地,而且延展到各大洋。01:32polar:adj.极地的;两极的;正好相反的/n.极面;极线/icecaps:n.冰盖;常积不消的冰 Hemisphere:n.半球 abyss:n.深渊;深邃,无底洞,地狱Sea level was 120 meters lower.
9、海平面比现在低了120米。01:35Carbon dioxide levels were very much lower than they aretoday.二氧化碳水平比现在要低很多。01:38So the earth was probably about three to five degrees colderoverall,and much,much colder in the polar regions.地球上的平均气温比现在大概要低3到5摄氏度,而且在极地地区要更加寒冷。01:42What Im trying to understand,and what other colleag
10、ues ofmine are trying to understand,is how we moved from thatcold climate condition to the warm climate condition that weenjoy today.我想要研究清楚的东西,也是我的同事们想要弄明白的东西,就是我们如何从那种极端寒冷的气候 转变成现在我们所享受的这种温暖气候的。01:49We know from ice core research that the transition fromthese cold conditions to warm conditions was
11、nt smooth,as对冰芯的研究告诉我们,从寒冷气候到温暖气候的转变并不是非常平缓的,你们可以通过太阳辐射的缓慢增加中推测出来。01:59TED演讲者:Laura Robinson|劳拉罗宾逊演讲标题:The secrets I find on the mysterious ocean floor|神秘海底世界的奥秘内容概要:Hundreds of meters below the surface of the ocean,Laura Robinson probes the steepslopes of massive undersea mountains.Shes on the hunt
12、 for thousand-year-old corals that shecan test in a nuclear reactor to discover how the ocean changes over time.By studying thehistory of the earth,Robinson hopes to find clues of what might happen in the future.在海平面以下数百米的地方,劳拉罗宾逊在仔细研究着绵延的海底山脉的悬崖峭壁。她在寻找着具有千年历史的珊瑚,将它们放在核反应堆中测试,以探究海洋是如何随着时间推移而演变的。通过学习
13、地球的历史,罗宾逊希望能够找到一些线索,以预测未来可能发生的事。these cold conditions to warm conditions wasnt smooth,asyou might predict from the slow increase in solar radiation.缓慢增加中推测出来。01:59And we know this from ice cores,because if you drill downinto ice,you find annual bands of ice,and you can see this inthe iceberg.我们可以得出这
14、种结论,是因为如果你在冰盖上钻孔,你可以发现按年份分层的冰,就像这幅冰山的图片里。02:10You can see those blue-white layers.你可以看到那些蓝白相间的条纹。02:16Gases are trapped in the ice cores,so we can measure CO2-thats why we know CO2 was lower in the past-and thechemistry of the ice also tells us about temperature in thepolar regions.气体被封闭在这些冰芯里,所以我们可
15、以据此测定二氧化碳。所以我们得知以前的二氧化碳水平比现在要低。冰的化学组成同样可以告诉我们02:18dioxide:n.二氧化物 know from:区别于 cores:n.晶体核心;芯部;要点;果心(core的复数形式)/v.挖去(水果的)果心(core的第三人称单数)bands:n.乐队;法官如果你从两万年前穿越到现代,你会发现气温出现了增长。02:29It didnt increase smoothly.它不是平缓地增长的。02:34Sometimes it increased very rapidly,then there was aplateau,then it increased
16、rapidly.有时候气温上升得非常迅速,然后就稳定一段时间,之后再次迅速上升。02:36It was different in the two polar regions,and CO2 alsoincreased in jumps.气温在两极地区有些差异,而且二氧化碳水平也以这种跳跃方式增长。02:40So were pretty sure the ocean has a lot to do with this.于是我们可以确定,海洋与这些变化有着密切联系。02:46The ocean stores huge amounts of carbon,about 60 timesmore tha
17、n is in the atmosphere.海洋里储存着大量的碳元素,比大气中的储量多了大约60倍。02:49It also acts to transport heat across the equator,and theocean is full of nutrients and it controls primary productivity.海洋还有的作用,就是跨赤道地区输送热量,而且海洋里富含养分,还提供了极高的初级产能。02:54So if we want to find out whats going on down in the deepsea,we really need
18、to get down there,see whats there andstart to explore.如果我们想要研究深海世界里发生了什么,我们真的需要潜入其中,看看那里有什么,并且开始努力探索。03:02This is some spectacular footage coming from a seamountabout a kilometer deep in international waters in theequatorial Atlantic,far from land.这是采自海底山峰的一些精彩镜头,这个山峰位于赤道地区的公海,而且远离大陆,大概在大西洋底1,000米深处
19、。03:09smoothly:adv.平稳地,平滑地;流畅地,流利地 plateau:n.高原/n.地名肯尼亚,美国普拉托/n.(活动或进程中的)稳定阶段,停滞时期/adj.高原印第安人的 equator:n.赤道 nutrients:营养盐/食品营养素 footage:n.英尺长度;连续镜头;以尺计算长度 seamount:n.海底山 international waters:国际海域Youre amongst the first people to see this bit of theseafloor,along with my research team.你们是最先欣赏到这个地区的海底
20、的一群人,跟我的研究团队差不多。03:17Youre probably seeing new species.你们可能看到的是一些新物种。03:23We dont know.然而我们并不了解。03:25Youd have to collect the samples and do some very intensetaxonomy.你得采集很多样本,然后做非常繁琐的生物学分类。03:26You can see beautiful bubblegum corals.你可以看到这些美丽的泡泡糖珊瑚。03:29There are brittle stars growing on these cora
21、ls.柔软的海星长在这些珊瑚上。03:31Those are things that look like tentacles coming out of corals.它们看起来就像珊瑚上延伸出的触手一样。03:34There are corals made of different forms of calciumcarbonate growing off the basalt of this massive underseamountain,and the dark sort of stuff,those are fossilizedcorals,and were going to tal
22、k a little more about those as wetravel back in time.这些珊瑚由不同形式的碳酸钙组成,在这个巨大的海底山峰的玄武岩上茁壮生长,那些颜色很黑的东西,就是变成化石的珊瑚,让我们回到过去,更仔细聊聊这些珊瑚的故事。03:37To do that,we need to charter a research boat.要做时光旅行,我们得租一条考察船,03:51seafloor:n.海底 intense:adj.强烈的;紧张的;非常的;热情的 taxonomy:n.分类学;分类法 bubblegum:adj.七至十三岁年龄儿童的/n.泡泡糖;摇滚舞曲
23、brittle:adj.易碎的,脆弱的;易生气的 tentacles:n.动触手;动触须(tentacle的复数)calcium:n.化学钙 carbonate:vt.使充满二氧化碳;使变成碳酸盐/n.碳酸盐 basalt:n.岩玄武岩;黑陶器 undersea:adj.水下的;海面下的This is the James Cook,an ocean-class research vesselmoored up in Tenerife.这是詹姆斯库克号,一艘大洋级的调查船,停泊在特纳里夫港口。03:53Looks beautiful,right?看上去很棒,对吧?03:57Great,if yo
24、ure not a great mariner.如果你不是个很好的海员,你会觉得不错的。03:59Sometimes it looks a little more like this.但是有时她看起来更像这样。04:01This is us trying to make sure that we dont lose precioussamples.我们正在努力保证珍贵的样品不丢失。04:04Everyones scurrying around,and I get terribly seasick,so itsnot always a lot of fun,but overall it is.每
25、个人都手忙脚乱,然后我也严重晕船,所以说这不全是有趣的经历,但是总体还是不错的。04:07www.XiYuS锡育软件So weve got to become a really good mapper to do this.我们必须要成为很好的测绘师才能做这个工作。04:13You dont see that kind of spectacular coral abundanceeverywhere.你不可能在处处都找到如此丰富的珊瑚储量。04:15It is global and it is deep,but we need to really find the rightplaces.我们
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