不大知名的英国人威廉•史密斯发表对化石价值的见解。他是萨默塞特的科尔运河建筑工地上的年轻监督员。绘制英国的岩层图,成为近代地质学的奠基石~~~

❤《万物简史》推出部落节目版,戳这里订阅:http://bulo.hujiang.com/menu/6004/


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书本的朗读语音很charming的磁性英音~~~大家可以好好学着模仿哦~~~!!
因为原著为美国人所写,单词采用美式拼法,不抄全文,也不用写序号。答完一空换行继续下一空作答。文中需听写单词或词组用[-No-]表示,句子用[---No---]表示。请边听写边理解文意,根据下面的TIPS训练听写。这样可以提高听力准确度,并为训练听译打下基础哦~~~


TIPS听写训练点:单词拼写,时态,单复数,连读,长难句(请边听边用符号先记下内容,然后自己回头组织语句,最后校对,不要逐字逐句听写)

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Hints:
carboniferous
Devon
Cambrian
Wales


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In the same year—in fact, the same month—that the aristocratic and [-1-] Cuvier was propounding his extinction theories in Paris, on the other side of the English Channel a rather more obscure Englishman was [-2-] the value of fossils that would also have lasting ramifications. William Smith was a young supervisor of construction on the Somerset Coal Canal. On the evening of January 5, 1796, he was sitting in a coaching inn in Somerset when he jotted down the notion that would eventually make his reputation. [---3---] Smith's insight was to realize that the answer lay with fossils. At every change in rock strata certain species of fossils disappeared while others carried on into [-4-] levels. By noting which species appeared in which strata, you could work out the relative ages of rocks wherever they appeared. [-5-], Smith began at once to make a map of Britain's rock strata, which would be published after many trials in 1815 and would become a [-6-] of modern geology. (The story is [-7-] covered in Simon Winchester's popular book The Map That Changed the World.)

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celebrated having an insight into To interpret rocks, there needs to be some means of correlation, a basis on which you can tell that those carboniferous rocks from Devon are younger than these Cambrian rocks from Wales. subsequent Drawing on his knowledge as a surveyor cornerstone comprehensively
大名鼎鼎的贵族居维叶在巴黎提出了绝种论。同年--实际上是同月,在英吉利海峡对岸,一个不大知名的英国人在发表对化石价值的见解。他的见解也具有持久的影响。威廉•史密斯是萨默塞特的科尔运河建筑工地上的年轻监督员。1796年1月5日,他坐在萨默塞特一家马车旅店里,记下了那个最终会使他名扬天下的观点。若要解释岩石,你非得有某种并置对比的东西。在这个基础上,你可以知道德文的那些石炭纪岩石要比威尔士的这些寒武纪岩石年轻。随着岩层的每一变化,有的物种的化石消失了,而有的化石一直延伸到随后的岩层。通过发现哪种物种在哪个岩层出现,你就可以计算出岩石的年龄,无论这些岩石是在哪里。凭着他作为测量员所拥有的知识,史密斯马上动手绘制英国的岩层图。经过多次试用以后,这些图于1815年出版,成为近代地质学的奠基石。(西蒙•温切斯特在他深受欢迎的《改变世界的地图》一书里对这件事作了全面的记述。)