2022-05-20 09:42:27



  Title: New evidence of River Hypothesis

  Listen to part of a lecture in a geology class.

  Professor: About 30 years ago, a geologist named Edward Cotter, that’s C-O-T-T-E-R, published a paper that contained a very interesting hypothesis.

  He was studying ancient rivers in the North American mountain chain. And he noticed that about 450 million years ago, rivers started to behave differently. Before then, rivers were wide, shallow and straight. But after that time, they became deeper and had move curves. They became increasingly meandering, and that’s actually how rivers behaved till these days.

  So why might this change have happened?[a1]

  Student: Maybe there was some kind of a climate shift?

  Professor: Well, lots of climate shifts have happened since then.

  Student: Was the change worldwide? Or just in that geographical area?

  Professor: Well Cotter speculated that rivers changed worldwide, but he couldn’t prove it. Because he only had evidence from the one North American mountain chain. But his studies gave him an idea about why rivers started to change. He hypothesized it had to do with the spread of plant life on earth.[a2]

  Student: So there was no plant life before 450 million years ago?

  Professor: Very little according to fossil records. Anyway, geologists were intrigued by this hypothesis which claims that as plants evolved and spread, they had an effect on terrain and rivers. In the past 30 years, more studies have been done. And now we have a lot of data about river systems from around 450 million years ago from all over the world.

  In a recent study, a couple of researchers gathered together the existing data and combine them with their own new field data to get a comprehensive picture of the situation.

  Their study was specifically designed to identify changes in the shapes of rivers during the time period when vegetation was evolving.

  And when the researchers compared the data about river shapes with data they have collected about plant life from the same period, the data seemed to prove Cotter’s hypothesis.[a3]

  Student: OK, but how did plant life affect rivers?

  Professor: Well, in order to answer that question, we need to look at the geological evidence.

  You see, as rivers flow, they leave layers of sediment behind that eventually fossilized. The content, thickness and shape of these fossilized layers and rocks gave us information about how rivers flowed. The earliest records from 500 million years ago show that the sediment in river deposits was largely composed of quartz grain of sand and gravel. That tells us that rivers weren’t defined, they were very shallow and wide, almost like floods.[a4]

  But around the time of the rise of plant life, the content of these sediment layers began to change. The quartz grains became much finer. And we see evidence of mud. This suggests that plants promoted the preservation of mud when they sent their roots into the ground. The roots helped to reinforce the ground, which in turn allowed for the creation of river banks.

  And we also see evidence of a process called lateral accretion.

  Lateral accretion happens when water flows around the curve or bend in the riverbed. Now the speed of the flow on the outside of the bend is fastest, and slowest on the inside of the bend. This sets up what’s called the secondary flow across the river bottom. The fast flowing water on the outside of the bend digs out material from the riverbank and pushes these material laterally across the bottom, and it gets deposited on the other side of the river, on the inner side of the bend.

  So, when we see in the sediment layers, evidence of lateral accretion, the erosion on one side and deposit on the other, that’s an indicator that meandering rivers existed.[a5]

  And according to the study, strong evidence of lateral accretion appears in the geological record. At the same time, there is also evidence of plants with underground root systems. This suggests that plants promoted the development of modern rivers by creating stable banks, which resulted in the flow of water in single meandering channels.

  Student: So it looks like the researchers were able to prove that hypothesis.

  Professor: Well, there is no denying that the study presents a very strong case. But some questions about this hypothesis remain. For example, it’s well-known that on other planets, like Mars, there is clear evidence of meandering rivers. But it’s there any evidence of vegetation on Mars?[a6] I think not.

  [a1]Q12 出题点

  [a2]Q13 出题点

  [a3]Q14 出题点

  [a4]Q15 出题点

  [a5]Q16 出题点

  [a6]Q17 出题点


  12、What does the professor mainly discuss?

  A. A hypothesis that rivers formed before the rise of plant life

  B. A study of the effects that rivers have on soil formation

  C. A debate surrounding two opposing hypotheses

  D. New evidence in support of a previously proposed hypothesis






  13、What limitation of Cotter's research does the professor mention?

  A. Cotter's research findings could not be replicated.

  B. Cotter’s research was based on one geographical area.

  C. Cotter's research did not take into account lateral accretion.

  D. Cotter's research did not account for changes in climate.


  解析:本题为细节题,题目问教授提出Cotter的研究的局限性是什么?由出题点可知 ,Cotter的研究证据仅仅来源于北美山脉,而河流的变迁则是一个全球性的问题,则Cotter的研究的局限性是它仅仅在一个区域,则B选项正确。


  C选项的意思为Cotter的研究没有考虑侧向堆积的影响,文章中的“lateral accretion”是教授提出的支持Cotter的观点的一个论据,故排除;


  14、What did researchers try to confirm about rivers in a recent study?

  A. That rivers now have the same shape worldwide

  B. That rivers were responsible for the spread of plant life

  C. That a change in the shape of rivers is linked to the spread of plant life

  D. That most rivers emerged during a specific geological time period






  15、Why does the professor describe the composition of the sediment of the earliest rivers?

  A. To identify the evidence used to determine how the rivers flowed

  B. To explain why the rivers could easily dry out

  C. To suggest that the sediment was once fine sand

  D. To suggest that the geological record might be flawed






  16、According to the professor, what is an effect of lateral accretion on a meandering river?

  A. Bends in the river become gradually straighter.

  B. Material from one riverbank is deposited on the other.

  C. The intensity of the river’s flow increases.

  D. The growth of plants on the outer riverbank is enhanced.






  17、重听题:Why does the professor say this:

  A. To find out what the students know about Mars

  B. To question certain geological studies of other planets

  C. To express a reservation he has about the hypothesis

  D. To indicate that he is going to change the topic


  解析:本题为功能题,需要重听一段内容后再作答。重听部分,教授明确提到这个假设还存在一些问题,所提他应该是持怀疑态度的。再结合重听部分下文中,教授说的“I think not”,可以进一步确定对于这个假设,教授的态度是有所保留的,故正确答案为C。