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Question 4 of 10

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According to paragraph 1, how do dendrochronologists deal with the problem of individual tree variability?

A. They only use samples from trees that have been living for at least twenty-five to thirty years

B. They select samples from tree species that are known to show little variation over time and within a particular location

C. They do not use samples from trees that show evidence of an unknown genetic makeup

D. They average together the measurements from samples of many different trees from the same location and time

Paragraph 1 is marked with []

我的答案 D 正确答案 D

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    【答案】D

    【题型】事实信息题

    【解析】题干问的是“树木年代学家如何处理树木个体之间的不同?”,根据题干内容可以定位到原文“These kinds of factors produce significant variations...”这句,后半句“and that fact means...”就能够回答题干问题,也就是“研究人员需要将同一时间段内同一地区同一树种的多个样本进行平均”来解决前面提到的问题。这部分信息可以对应选项D的主干信息 “他们将所有的测算值取平均。”

    选项A,注意绝对词only易错,说的是他们只使用活了至少25到30年的树木的样本,原文未提及。原文后一句说的意思是“测量一个地区25-30个年轮记录的平均值是解决问题的第一步”。

    选项B,他们从一些树种中挑选样本,这些树种已知在特定地点随时间变化不大。原文未提及。

    选项C,他们没有用“显示了未知基因构成的”树作为样本,原文未提及。

    综上答案为D。

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译文
Challenge of Dendrochronology

Dendrochronology is the technique of counting tree rings to determine a tree's age and measuring the width of these rings to determine characteristics of past climates. This might seem simple: each ring represents one year, and wider rings generally mean better growing conditions-plentiful rainfall, moderate temperatures, and so forth. But the seasonal growth of a particular tree is affected by factors other than the weather. Trees vary, one from another, just like people do. The genetic makeup of each individual tree is unique, so one particular tree may grow a bit more quickly that another. Highly local conditions can also change over time. It is easy enough to see that if part of the soil near a tree has been eroded, this will impact the tree's root system and limit its growth, at least until the situation stabilizes. Then again, an infestation of insects may affect a tree in one valley more than the same type of tree ten miles away. Or one tree may suddenly start to get a lot more sunlight when an old, big tree in the neighborhood finally falls. These kinds of factors produce significant variations among individual specimens, and that fact means that researchers need to average together samples from many specimens of a single tree species in one region over the same time period. Some dendrochronologists think that measuring an average of twenty-five to thirty tree-ring records in a locale is an essential first step in getting around the problem of individual variability. While it may be easy enough to find thirty samples in some locations for particular periods, it obviously becomes less and less likely the more ancient the wood samples are.

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Another issue is more general. Trees that are fortunate enough to live on good soil and near local sources of groundwater often grow at steady rates. Such growth translates into attractive trees that are tall and well formed; they also have rings that are wide and quite uniform in thickness, but their uniform growth rings make them entirely useless when it comes to inferring anything about past weather patterns. That is why, instead of looking at superb botanical specimens, dendrochronologists focus their work on wood from trees that are living a tough life due to poor soil, steep slopes, the absence of local groundwater, or some other challenge. It is these "tortured" trees that are the most likely to grow very little during years of scarce rains or do poorly after a harsh winter and a late spring. What this means, of course, is that few trees in the woods are likely to be good samples for the scientist. Indeed, it may be quite a small fraction that yields useful ring patterns. Again, this increases the challenge of finding enough good samples to say with much certainty what past conditions were like.

Another factor of dendrochronology relates to wood itself. In the spring, a tree grows rapidly, creating new cells on the outside of its trunk and branches, just under the bark. These cells, called "earlywood" or "springwood," are large and have thin cell walls; both these factors contribute to making the wood relatively lightweight for its volume. In the summer, growth slows. Denser "latewood" is formed, creating the band that is relatively dark when you look at the end of a piece of lumber. But occasionally the sequence of a perfect pair of springwood and latewood does not hold up. If conditions-weather or disease-severely test a tree one year, it will not grow over all its surfaces. That may mean that a particular sample of wood taken by the dendrochronologist will have a missing ring in it, which will result in the scientist's inferences being off base by a year

A few trees also may trip up scientists by revealing a "false ring" made of latewood that's in the middle of springwood. These features, sometimes known as double rings, usually can be distinguished from true rings because the unusual dark ring is likely to change gradually rather than more abruptly into the springwood that lies on either side of the false latewood. It is not clear what creates such double rings, although people have speculated that unusual conditions during the middle of the growing season or even highly local issues might be the cause.