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妇女财产问题  似乎有两个方向,注意

V1

女性的财产,原来都是归丈夫的。然后法律改了后,归自己,但是仍然发生丈夫强迫妻子把财产给他。然后又改法律,禁止这种行为。Old V2

美国法律对已婚妇女的财产权力的保护问题-主要是讲历史沿革和学者的观点对比:

第一段:概括某一新法案M实施前的状况,在common law的情况下,妇女结婚后财产就归丈夫所有了。此时丈夫对妻子的财产有很大的支配权利。妇女只有通过一个似乎叫equity court的机构才有可能得到对自己财产的权利。有一题是关于婚后财产是归老公支配的。

第二 段:讲十九世纪中期,因为husbands担心破产会连带将妻子的财产也失去,于是出来了一个新的法案。S的观点是这个法案极大的改变了妇女的status and 对自己结婚前后的财产的权利。讲从某个时期起,不少州开始立法保护已婚妇女的财产权。(注意:说的是银行大批倒闭的时期,不少丈夫破产把妻子的财产也陪进去了,这个在后面的题里面 考了这些州立法的原因是什么。)还讲了一个具体的法律(这个法律是什么,年代,在后面也是考点)。里面有一题。

第三段:讲了不同学者间的评价。第一句话是某人b的观点,是他认为在M实施前已经有remedy可以达到保护妇女财产的作用了,认为法律的转变起到了积极作用。然后是第二个人S继续反对第一个人b的观点。 说以前的equity court在不同的州开展的情况不一样。认为并没有起到什么作用,ie 。Connectic 康涅狄可州和 Mass 州,很多传统保守实力,反 对这种社会、法律发展的趋势。(后面有道题考这些法律你能infer出什么,我选了not universial in all states,我觉得universial这个改写还soso。反正请大家读的时候,注意这种法律变化有什么社会影响,该怎么评价)最后一句话,讲了有些 人愿意接受这种法律,也是为了破产的丈夫把财产转移给妻子,赖债权人的钱。除了上述出题点,还有主旨题:我认为应该选提到了“讲述社会变化,对比学者观点 ”的那个选项,事实上,文章的重心是在第二个学者的言论,应该属于present观点的文章,一定要突出这个。里面还有一题,是说N的实施并不普遍,并且对它的接受不大好。


Old V3

女性财产权,3p,

1p史背景,说女性结婚后没有财产权,

2p是有个人S说pass women's property act有助于改善女性的状况(原文好像有一句是虽然没有平等但得到独立),

3p整个是对S观点的反驳,最后说有很多看起来对女性有利的判决还是因为她们的丈夫害怕贷款还是什么故意转到妻子那里的
问题有主旨,还有说文章是用property act和什么做对比的,选什么system,定位3p,还有个问有关S观点的。

Old V4

财产权颁布以前,对妇女有什么不利的地方。选有Creditor那个,大概是说如果老公欠了钱的话,债主可以用老婆的财产还账。
B,有一个学者赞成这个法案,这个学者的观点是,虽然这个法案不能使男女平等,但是可以有效的保护妇女的财产。选的时候关键词定位就可以了
C,有一个学者反对这个法案,他的理由是之前有Equity Court 已经可以有效的保护妇女的财产。题目问,这个者主要做了什么,选有Equity system 的那个选项


请各位考友注意,这下面的N个版本好像不是一个主题,请大家批判吸收!

Old V5

两段,比较长。

第一段:税收基于个人的财产和工资收入。viginia的某个地方妇女的财产和工资收入都不错,但税收很少。原因是因为很多妇女在overture?的法律制度下跟了丈夫的姓和财产。(有考题)关于美国妇女没有交很多税的问题,其实并不是她们没钱,而是很多document把她们都归到了丈夫的名下,不单独计算它们的财产,历史学家认为一些documentation没有把女性包括在内,是因为女性没有财产权。但是有一个人认为,不是这样的,而是因为税法的改变,举例,在家庭里起主导地位的women是可以被免税的,尽管她们有收入。1960-1970年文献记载的美国妇女经济地位为什么低?一个原因是Law把married的财产归到男人的名下(注意:这里有个考点) tax law能反映这一点 后面全在说一个女历史学家认为tax law怎么怎么反映 读仔细有2-3个考点呢,

第二段:一个叫HW的女经济学家根据税收的数据提出了一些研究结果。在这个地方的税务官员都很谨慎(有考题,证明这些官员不会错误)某个阶段妇女的税收越来越少。HW证明其原因是妇女获得的工作机会越来越少。

好像是四道题的。一道主体题。


Old V6

Married women's property rights and their social status.
Saying in the 18 and early 19 century, common laws dictated that when a woman is married, her husband takes over all her properties.  The man had control the right to use the woman's properties while she lived and became the owner of the properties upon the woman's death.  Only one thing can prevent this from happening, something like "pre-marriage settlement"
Then..some law about women's right of property was finally established!!  then blah blah blah, how good the law was and things like that.  Then, a scholar named Sammas? said this law substantially changed women's status. 
BUT, another scholar named Beard? disagreed with Sammas and said the effects of this new law  was overstated because before this new law was established, there always existed "equity court" that serve the same purpose.
BUT, a third scholar named Salmon came out to challenge Beard.  Salmon said equitty court can't do much because most states were very hostile against equity court and in the cases where the court gave women the right of properties, some were attempts made by men to transfer all properties to their women to avoid consequences of bankruptcy. 
题目有...
1. purpose of the passage
   answer should be to cronicle laws regarding women's right of properties and examine the implication to women's status.
2. inferred from the passage, what would Beard mostly likely think of equity court
   answer should be it substantially improve women's status

考题:

1. 说的是银行大批倒闭的时期,不少丈夫破产把妻子的财产也陪进去了,这个在后面的题里面考了这些州立法的原因是什么

2. 这个法律是什么,年代,在后面也是考点

3. 后面有道题考这些法律你能infer出什么,我选了not universial in all states,我觉得universial这个改写还soso

4. 主旨题

5. 原因是因为很多妇女在overture?的法律制度下跟了丈夫的姓和财产。(有考题)

6. 1960-1970年文献记载的美国妇女经济地位为什么低?一个原因是Law把married的财产归到男人的名下(注意:这里有个考点)

7. 他的理由是之前有Equity Court 已经可以有效的保护妇女的财产。题目问,这个者主要做了什么,选有Equity system 的那个选项

8. purpose of the passage
answer should be to cronicle laws regarding women's right of properties and examine the implication to women's status.

9. inferred from the passage, what would Beard mostly likely think of equity court
answer should be it substantially improve women's status


参考阅读


文艺复兴时期女性地位

2段 两个人的观点,第二个(地位有改变)驳斥第一个

V1

p1:中世纪以来欧洲妇女地位如何改变。结构清晰,第一句引出话题(有考题, 问你首句作用),先写一位女社会学家的看法被普遍认可,由于education啊,political的这些因素的影响,不论从经济上,社会地位上还是其它方面,从财产控制权等等之类来看中世纪妇女地位没有提高;在家庭和社会里仍然受压迫.

p2:反对,有改变,然后就是另一个作家站出来霹雳啪啦的说不是这样,认为女性在宗教方面有了很多进步,发表了一些宗教的文章. 尽管妇女在经济和社会地位上还是其它方面没有明显改善,但是不容忽视的是他们得以self expression(有考题),这主要体现在其宗教信仰和其它一些方面(大概就是说他们能够有一些独立选择权得以做出自己的选择吧)。他们的religious 对他们的地位的提高有很大影响(有题问religious具体在哪方面有影响,选self-expression那个)

文章很短,大概 2/3屏幕吧,我的理解是作者并没有明显表明支持哪位arguer观点的态度。(可能会考到)


考题:

1. 有题问religious具体在哪方面有影响,self-expression那个

2. 尽管妇女在经济和社会地位上还是其它方面没有明显改善,但是不容忽视的是他们得以self expression(有考题)

3. 第一句引出话题(有考题, 问你首句作用)

4. 我的理解是作者并没有明显表明支持哪位arguer观点的态度。(可能会考到)

5.  

 

参考阅读

Historians who study European women of the Renaissance try to measure independence,” “options,” and other indicators of the degree to which the expression of women’s individuality was either permitted or suppressed. Influenced by Western individualism, these historians define a peculiar form of personhood:  an innately bounded unit, autonomous and standing apart from both nature and society.  An anthropologist, however, would contend that a person can be conceived in ways other than as an “individual.”  In many societies a person’s identity is not intrinsically unique and self-contained but instead is defined within a complex web of social relationships. 

In her study of the fifteenth-century Florentine widow Alessandra Strozzi, a historian who specializes in European women of the Renaissance attributes individual intention and authorship of actions to her subject.  This historian assumes that Alessandra had goals and interests different from those of her sons, yet much of the historian’s own research reveals that Alessandra acted primarily as a champion of her  sons’ interests, taking their goals as her own.  Thus Alessandra conforms more closely to the anthropologist’s notion that personal motivation is embedded in a social context.  Indeed, one could argue that Alessandra did not distinguish her personhood from that of her sons.  In Renaissance Europe the boundaries of the conceptual self were not always firm and closed and did not necessarily coincide with the boundaries of the bodily self.

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 旧金山妇女工会female团体产生及阻力

讲female团体是怎么产生的,以及产生过程中遇到的阻力(来自male团体的阻力,有题)。这种阻力主要是由于他们有conflict on 高亮部分(有题,问高亮部分啥意思,我选的conflict的同义词disagreement)

大概是讲20世纪初旧金山妇女工会的问题。女性工会成立的原因,没分段。先说女性工会没有成立的原因。然后又说了什么原因促成女性单独成立all female union。

 

考题:

1. 有题,问高亮部分啥意思,我选的conflict的同义词disagreement


女性主义

第一段讲有学者认为女性主义与农奴废除(1850s)的出现(advent)是一起发生的。等等。但是, 过去的历史学家将1850年的废奴运动作为妇女运动的发源,是错误的。女性主义和女权主义不一样。

第二段讲女性主义的特征,说包括什么什么,感觉上是范围比较广的那种。说妇女运动老早就开始了,在1800年左右就有了。它分为两种, 女性主义和女权主义。然后分别说了两种的异同: 女权运动与正常的女行政区一般的权力不同,前者很激进,很多的要求,后者好像只要求与男性一样的权利,如教育权等

第三段讲女权主义的特征,是为妇女争取一些权益,例如选举权之类的。妇女们很早就搞过一个啥啥的协会,目的是。。。后来才和废奴主义勾搭上的。。。女权运动要早于废奴主义,最后好像说的是女权运动产生于1800年后,但是1850年后才有了废奴主义

第四段 讲妇女进行的很多活动什么的

第五段忘了。。。

 

考题:

1.态度题:问用一个词形容作者态度的,我选的negative

2.细节题:(定位第二段)女性主义和女权主义的区别,我选的女性主义包括的范围更广

3.态度题:好像是问作者怎么看待历史学家对女权运动起源的研究,我选的是忽视了1850年以前的活动

4.细节题:(定位第二段)问women's rights活动记录imply了什么,不太确定,我选了他们不仅参加了废奴运动还参加了女权运动。好像是错了,忘NN补充。

5.主题题:primary purpose of the passage,选项跟JJ里的不太一样,我选的好像是说历史学家在女权问题的研究有flaw,有点忘了,但这个题比较简单,做到的时候看一下,主要是说方法有问题。


妇女工作问题-比较韩国台湾两地


悬崖上的印第安艺术 rock art

V1

RC2nd     Indian art on the cliff

1.a kind of carving on the cliff in northwestern us regions where a indian group lived is called vertical something.

2.because a female researcher found this kind of art in lakota people's territory and the territory of other oyata culture (oyata includes lakota), she attributed the kind of art exclusively to oyata people. she also found this kind of art to be a communication system.

3.the author thinks the existing archeaological evidences are not strong enough to support the female researcher's conclusion that the kind of art on the cliff only belongs to oyata culture. the author thinks this kind of art belongs to many culture of a certain time. his evidence is that in some place in canada, there is also this kind of art.


V2

两段,长,过页

第一段S expert提出一个理论,讲一种rock art的叫什么vertical bla bla (有题)。说这个rock arttradition是originate from L 和 O 部落。原因有123

第二段作者反驳说S的理论不对,理由有123虽然 rock art 和O有着千丝万缕的联系,但也不能说它就只是originate from O吧。这不,其他部落也可能有这个rock art…(有主旨题,我选了argue against开头的选项)


考题:

1.  讲一种rock art的叫什么vertical bla bla (有题)

2. 有主旨题,我选了argue against开头的选项

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C、社会科学类


夏威夷的temple 高分的最后一篇

Old V1新旧JJ集合 
第一段:最新研究证明夏威夷社会政治的发展比预想快。口述历史讲述17世纪初有个大牛人P统一了夏威夷整个岛,把国家变成宗教国家。夏威夷有个岛,上面有些庙,以前被认为是在几百年内慢慢起来的。但是又没有确实的理论来支持。可能比传统学者完成的时间要早。但无法证明,因为相关证据无法用C14测定年代。
第二段:科学家有一种新的科技,新的科技或者是利用同位素测试uranium test中装饰这个塔的某个海生植物。检测庙里的珊瑚饰物的年代,发现是1620年左右吧,测出其丰收的时间等等. 大概gap20年。(两个表述不一,注意:所以这个发现证明的当地人的说法。Or就是说明了这个塔修时间和原来想的不一样 )。发现Hawaii的temple大都建于2,3十年间,而不是之前人们认为的250年。并围此出题。由于这个庙是当地多余(surplus)物品的聚集和交换地,有重要的作用。因此都出这社会文明结构(这个复合词不认识)may serve one generation. 科学家用了新方法,证明 大量用于分配产品的寺庙建于17世纪初,从而证明了口述历史中17世纪初的大变革。

V3

Temples in Hawaii - Maui. Oral history told by Hawaii locals states that King B united two tribes during ... Researchers think the social politics change of Hawaii happened in a single period of history.Recently, researchers are able to date the temple by U..230..(two elements of temple wall)... It proves that many temples were built using the same material during a short period of time. Temples were used as a center to control the production and collect surplus foods. Therefore, it confers what oral history said. 



考题:

1.原文的目的:选项实在看不出来.我混淆的选项是 A新的证据证明这个文明结构reform非常短 还是Enovelty技术描述了历史,

2. q1有两个选型比较混淆:一个说文章是用新的科学技术证实了一个地区的历史;另一个选项是说,文章证实了口述者的话,并让人们对于某个地区的了解更正确了,(我现在比较肯定这题答案应该是第一个,因为整篇文章强调新证据改变了科学家对进程的pace见解的change,总之大家读原文好好体会,抓好最主要的意思)

3.serve vone generation 的作用。我选:这个文明结构比原想的更uneven

3.原文暗示了什么?其中B是 这个塔primarily是物品(无多余)的交换和集合地.我觉得不像.我选的是"这个水生植物被装饰到塔得时候还是活的,when harvest time." 选项如此,我也没太读懂

4.主旨题

5.有道except题

6.最后一段single generation那句话是指什么有道题,我选的大概是指这个span比较短的那个

7.人们从一种uranium test中发现Hawaii的temple大都建于2,3十年间,而不是之前人们认为的250年。并围此出题。

 

参考阅读

 

2007年4月RC机经多次出现夏威夷寺庙(Hawaii Temples),通过google终于找到原文(我没看过原文,这是基于各前辈所写的机经内容而找的,对照之后觉得十分相似,请看过原文的前辈看看是否就是这东东)。内容如下:

Proto-historic Hawaiian temples on the island of Maui may have mushroomed up within just 30 years, not 250 as previously supposed, scientists say. The findings could significantly alter researchers' understanding of the pace of precontact sociopolitical change in the Pacific.

Hawaiian genealogies and oral histories hold that sometime around 1600 A.D. a ruler named Pi'ilani united two opposing chiefdoms on Maui into a peaceful kingdom, marking the emergence of a religious state on the island. Archaeologists had been unable to confirm that sequence of events, however, in part because of the limitations of carbon dating.

In the new work, Patrick V. Kirch and Warren D. Sharp of the University of California and Berkeley used another kind of radiometric technique involving thorium-230, rather than carbon-14, to date bits of branch coral that were collected from living reefs and left as divine offerings at seven different temples during construction. Dates for these corals, which had been incorporated into walls and platform fill, all fell in a narrow range of 1565 to 1638 A.D., give or take a few years on either end. Moreover, dates on the samples that best reflect the time they were harvested from the sea--those from the coral branch tips--ranged from 1608 to 1638 A.D., an interval of just 30 years. These findings thus point to intensive temple-building during that time. Because temples served as centers for control of production and the collection of surplus goods, the team contends, it seems likely that the construction boom accompanied a profound shift in sociopolitical structure.

Kirch and Sharp observe that the conquests described by local oral traditions coincide with these new dates, and would have more than doubled the size of the Maui polity to upwards of 2,360 square kilometers--the magnitude of expansion expected with the formation of an archaic state. "The temples provide tangible archaeological evidence of the speed with which a fundamental sociopolitical transition occurred in proto-historic Hawaii," the authors conclude. Indeed, they note, it may have happened in the span of a single generation of Hawaiians.

科学家称,M岛上夏威夷古庙兴盛发展并非像先前预计长达约250年,而是在约30年间完成的。这一发现很大程度上改变了学者对当时社会政治发展进程的理解。

    夏威夷人后裔和野史一直认为,在公元1600年左右,一位叫P的统治者将M岛上对抗的两国统一成一个新的国家,这是岛上出现宗教的标志。研究人员由于受碳元素追踪技术的限制,无法确认这些事件的时间顺序。

    在 新的研究中,K和S用一种T-230同位素技术(取代常用的C-14)对一块从7个古庙中找到的礁石上的珊瑚(该珊瑚是当时从活的珊瑚礁上取下作为一种供 奉品放在古庙里的)进行时间追踪定位。这些珊瑚是从古庙的墙和屋顶中发现的,定位出的时间落在一段很窄的范围内——公元1565-1638年间(或前后波 动几年)。而且,对珊瑚尖部——最能反映真实时间的部分——的定位落在更窄的范围——公元1608-1638年间,仅30年。这些发现显示了当时大范围的 建庙活动。因为考虑到古庙在当时是控制商品生产和聚集的中心,研究小组推测,这些建筑的兴起伴随着社会意识形态结构的转变。

    K和 S考察发现,当地民间记载的“统一过程”和实验测定的新结果时间吻合,而且将M政权领土扩大了一倍到2360平方公里——重要的古代帝国建成与扩张的过 程。“这些古庙为古代时期夏威夷基础社会意识形态转变的进程速度提供了考古学依据”,笔者总结道。他们说到,实际上,这一转变可能就发生在一代夏威夷人中。



cost disease古典音乐艺术资金投入musical表演

V1:  长, 3段。

p1:关于艺术和生产力的。生产力发展了,各个行业的成本都降低了,但是艺术就不是这样。比如做表的,机器可以节省很多人力。但是比如做violin的,就没有多大改变。关于一个模型叫做cost disease,就是认为古典音乐艺术之类的成本没有随着经济发展大幅增加,因为科技发展可以使得其他生产规模化降低成本,但是每个观众的成本却没有增加……(有逻辑题,说哪一项最像cost disease的应用)一个什么人认为资金在音乐艺术方面投入不够多,然后他的观点立即被否定,否定他主要有两个原因。

p2:批判,其实不是这样,1P观点的人忽略了扩音器什么的,技术发展减少了很多人。还有直播,也是。科技发展也使得古典音乐能在更大的礼堂公开演出使得更多的观众得以享受;好像是说资金投入在功放(amplification)上了,如果没有amplification,那么表演者只能表演给更少的人听(这里有考题)。recording和broadcast也是得益于科技发展。

p3:他还忽略了啥啥,其实因为agency和经理使得一些star出场费非常非常高,也使得整个音乐艺术成本增加,使得这一项商业成为一种什么和什么的混合体,大意好像是市场竞争和个人什么……

考点集中在一,二段


考题:

1.有逻辑题,说哪一项最像cost disease的应用,我选了A,不是很确定,但是BCDE,尤其是cde差的太远了。

2.如果没有amplification,那么表演者只能表演给更少的人听(这里有考题)。

3.下列哪项是对的?有两个选项很混淆,(另外3个明显错)一个说,stars 要的钱越来越多,另一个说,agent要的钱越来越多了。我考虑挺久选stars。因为我觉得agent 是帮助star 得到更多的钱,但是没说agent本身能得更多的钱。

4.音乐的费用会降下来,如果下列哪项假设成立?选最后一个E,说free market的。确定。最后一段明确说了现在不是free market.

参考阅读

1 cost disease成本病

传统理论:工资和劳动力生产率紧密相关

成本病:一些行业工资提高,劳动生产率却未提高(劳动力密集代表的服务业很难实现产率的提高)

经 济学家认为,未获得产率提高就抬高劳动者工资是出于与同行竞争拉拢劳动力的考虑。例如,一个音乐家被付给19世纪水平的工资,他便会退出行业,转而进入类 似汽车工业这种提高产率从而获得工资增长的行业。由此可见,音乐家工资提高并不是因为产率提高,而是其他行业工资的提高。

http://en.wikipedia.org/wiki/Baumol%27s_cost_disease

Baumol's cost disease (also known as the Baumol Effect) is a phenomenon described by William J. Baumol and William G. Bowen in the 1960s. It involves a rise of salaries in jobs that have experienced no increase of labor productivity in response to rising salaries in other jobs which did experience such labor productivity growth. This goes against the theory in classical economics that wages are always closely tied to labor productivity changes.

The rise of wages in jobs without productivity gains is caused by the necessity to compete for employees with jobs that did experience gains and hence can naturally pay higher salaries, just as classical economics predicts. For instance, if the music industry pays its musicians 19th century style salaries, the musicians may decide to quit and get a job at an automobile factory where salaries are commensurate to high labor productivity. Hence, musicians' salaries are increased not due to labor productivity increases in the music industry, but rather due to productivity and wage increases in other industries.

The original study was conducted for the performing arts sector. Baumol and Bowen pointed out that the same number of musicians are needed to play a Beethoven string quartet today as were needed in the 1800s; that is, the productivity of Classical music performance has not increased. On the other hand, wages of musicians (as well as in all other professions) have increased greatly since the 19th century.

In a range of businesses, such as the car manufacturing sector and the retail sector, workers are continually getting more productive due to technological innovations to their tools and equipment. In contrast, in some labor-intensive sectors that rely heavily on human interaction or activities, such as nursing, education, or the performing arts there is little or no growth in productivity over time. As with the string quartet example, it takes nurses the same amount of time to change a bandage, or college professors the same amount of time to mark an essay, in 2006 as it did in 1966.

Baumol's cost disease is often used to describe the lack of growth in productivity in public services such as public hospitals and state colleges. Since many public administration activities are heavily labor-intensive there is little growth in productivity over time. As a result growth in the GDP will generate little more resources to be spent in public sector. Thus public sector production is more depended on taxation level than growth in the GDP.


拉丁美洲的文学起源

V1: 

第二篇:

拉丁美洲的文学起源,讲1960年之前就有非常出色的作家但是成就一直不被发现,直到1960年后。第一段讲拉美文学的影响,第二段讲什么忘记了……第三段举例,两个作家很早的作品和成就直到1994年才得到认可。

考题:

参考阅读

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D、生命科学类


 

参考阅读

引进北美洲大型动物 高频

V1

RC:引进大型动物那个(4个大长段)

P1:环境保护学家建议复活古代大型生物,(引进大型动物),因为会对生态ECO SYSTEM有好处,用来改善生态环境,维持生态平衡。(由于某些原因在美洲的一些大型动物灭绝了,但是其他地方还有,就想引进他们改善恶化的生态系统)

P2: 举例非洲,说非洲的生态比较完善,因为物种之间达到了一种平衡。引进的好处(主要是举目前生态环境的现况,比如small 动物多什么的,已经了就会减低他们,切大象推倒一些树木对一些小动物居住有益,可以控制一些树木的疯长。)

P3:说引进这种大型动物会给北美现在的生态带来哪些好处。 最后还说了还有经济上的好处,而且COST不高,只需要让那些大型动物在保护区内闲逛,就可以吸引很多观光客。具体很多动物的例子(elephant lion )有 一道考题问下面什么动物的引进会带来经济 benefits (而不是生态benefits)我用了5分钟也没找到这个经济benefits。大家看到经济的要注意了。也可能不在这一段。

P4:有人要反对了。说引进大型生物带来的问题。可能没有环境保护学家想的那么乐观。(说以前的大型动物和现在的不像,现在的不能在这住。支持者就说根据DNA检验,可以啊(有结构题,问DNA出现的作用——就是证明它们可以在这生活; 又有人反对说现在和以前环境不一样了啊,支持者又说了(忘了)Many have expressed concern about the fact that North America’s ecosystems are not the same today as they were 13,000 years ago and that reintroduced animals might therefore be unable to survive in them. Whereas habitats are and will continue to be dynamic on a timescale of thousands of years, very few plants or small mammals went extinct during the late Pleistocene. The major missing component of North American ecosystems today compared with the Pleistocene is the megafauna, which we can infer are critical cogs in the wheels.


 

Old V2 06/8 主题内容略有不同

文章体题材:结论解释型

说大型动物的灭绝, 在北美和亚洲的情况和澳洲等的情况比较,
说明这是大型动物对人类狩猎活动的适应的不同造成的

第一段讲为何大型动物在亚洲及非洲灭绝的时间和在澳洲美洲时间不同,blah(列举各地灭绝时间),那是因为人类文明使用火的影响,因为区块文明进展不同,所以灭绝时间不同.

第二段讲-那有人会说是气候影响来反驳我,但我说不是,blah(举反证反驳气候影响-如大家应同一时间同一物种一起消失等)

第三段讲-那有人会说原始人是打猎和采果并用取得食物,非吃肉肉过活来反驳,但我又说不是,blah(再举反证反驳) the end


 

考题:

1.     有一道考题问下面什么动物的引进会带来经济 benefits (而不是生态benefits)

2.    有结构题问DNA出现的作用——就是证明它们可以在这生活

3.    第一段 起到什么作用,我选了那个答案:专家提出proposal和给出背景知识

4.    (定位第二段)专家最可能在proposal中plan 什么但跟文章最相关:1是提供大型动物居住地2是创造经济效益3是 fencing off 什么植物4 是做大型动物的DNA测试 5是plant什么什么,记不清了我选C,不肯定对,

5.    有道问你是哪两种动物在文中做例子的,我选了大象和狼

6.    细节题:(定位第二段)说北美缺少那个动物(M开头的一个词),最有可能引起的什么效果?我选的是引起fragment ECOSYSTEM什么什么,大意是说ECOSYSTEM不完整之类的。其他选项都是比较具体的,比如说狼怎么怎么了,狮子怎么怎么了之类的。

7.    主题题:Main idea of the passage,我选的是评估专家的一个proposal。其他选项都是比较具体:比如是否应该引进M这个动物之类的。

 

参考阅读

Restoring America’s big, wild animals


In the fall of 2004 a dozen conservation biologists gathered on a ranch in New Mexico to ponder a bold plan. The scientists, trained in a variety of disciplines, ranged from the grand old men of the field to those of us earlier in our careers. The idea we were mulling over was the reintroduction of large vertebrates—mega fauna—to North America.

Most of these animals, such as mammoths and cheetahs, died out roughly 13,000 years ago, when humans from Eurasia began migrating to the continent. The theory—propounded 40 years ago by Paul Martin of the University of Arizona—is that overhunting by the new arrivals reduced the numbers of large vertebrates so severely that the populations could not recover. Called Pleistocene overkill, the concept was highly controversial at the time, but the general thesis that humans played a signifi cant role is now widely accepted. Martin was present at the meeting in New Mexico, and his ideas on the loss of these animals, the ecological consequences, and what we should do about it formed the foundation of the proposal that emerged, which we dubbed Pleistocene rewilding.

Although the cheetahs, lions and mammoths that once roamed North America are extinct, the same species or close relatives have survived elsewhere, and our discussions focused on introducing these substitutes to North American  ecosystems. We believe that these efforts hold the potential to partially restore important ecological processes, such as predation and browsing, to ecosystems where they have been absent for millennia. The substitutes would also bring economic and cultural benefi ts. Not surprisingly, the published proposal evoked strong reactions. Those reactions are welcome, because debate about the conservation issues that underlie Pleistocene rewilding merit thorough discussion.


Why Big Animals Are Important

Our approach concentrates on large animals because they exercise a disproportionate effect on the environment. For tens of millions of years, megafauna dominated the globe, strongly interacting and co-evolving with other species and infl uencing entire ecosystems. Horses, camels, lions, ele-phants and other large creatures were everywhere: megafauna were the norm. But starting roughly 50,000 years ago, the overwhelming majority went extinct. Today megafauna inhabit less than 10 percent of the globe.

Over the past decade, ecologist John Terborgh of Duke University has observed directly how critical large animals are to the health of ecosystems and how their loss adversely affects the natural world. When a hydroelectric dam fl ooded thousands of acres in Venezuela, Terborgh saw the water create dozens of islands—a fragmentation akin to the virtual islands created around the world as humans cut down trees, build shopping malls, and sprawl from urban centers. The islands in Venezuela were too small to support the creatures at the top of the food chain—predators such as jaguars, pumas and eagles. Their disappearance sparked a chain of reactions. Animals such as monkeys, leaf-cutter ants and other herbivores, whose populations were no longer kept in check by predation, thrived and subsequently destroyed vegetation—the ecosystems collapsed, with biodiversity being the ultimate loser.

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Similar ecological disasters have occurred on other continents. Degraded ecosystems are not only bad for biodiversity; they are bad for human economies. In Central America, for instance, researchers have shown that intact tropical ecosystems are worth at least $60,000 a year to a single coffee farm because of the services they provide, such as the pollination of coffee crops.

Where large predators and herbivores still remain, they play pivotal roles. In Alaska, sea otters maintain kelp forest ecosystems by keeping herbivores that eat kelp, such as sea urchins, in check. In Africa, elephants are keystone players; as they move through an area, their knocking down trees and trampling create a habitat in which certain plants and animals can fl ourish. Lions and other predators control the populations of African herbivores, which in turn influence the distribution of plants and soil nutrients.

In Pleistocene America, large predators and herbivores played similar roles. Today most of that vital influence is absent. For example, the American cheetah (a relative of the African cheetah) dashed across the grasslands in pursuit of pronghorn antelopes for millions of years. These chases shaped the pronghorn’s astounding speed and other biological aspects of one of the fastest animals alive. In the absence of the cheetah, the pronghorn appears “overbuilt” for its environment today.

Pleistocene rewilding is not about recreating exactly some past state. Rather it is about restoring the kinds of species interactions that sustain thriving ecosystems. Giant tortoises, horses, camels, cheetahs, elephants and lions: they were all here, and they helped to shape North American ecosystems. Either the same species or closely related species are available for introduction as proxies, and many are already in captivity in the U.S. In essence, Pleistocene rewilding would help change the underlying premise of conservation biology from limiting extinction to actively restoring natural processes.

At first, our proposal may seem outrageous—lions in Montana? But the plan deserves serious debate for several reasons. First, nowhere on Earth is pristine, at least in terms of being substantially free of human influence. Our demographics, chemicals, economics and politics pervade every part of the planet. Even in our largest national parks, species go extinct without active intervention. And human encroachment shows alarming signs of worsening. Bold actions, rather than business as usual, will be needed to reverse such negative influences. Second, since conservation biology emerged as a discipline more than three decades ago, it has been mainly a business of doom and gloom, a struggle merely to slow the loss of biodiversity. But conservation need not be only reactive. A proactive approach would include restoring natural processes, starting with ones we know are disproportionately important, such as those influenced by megafauna.  

Third, land in North America is available for the reintroduction of megafauna. Although the patterns of human land use are always shifting, in some areas, such as parts of the Great Plains and the Southwest, large private and public lands with low or declining human population densities might be used for the project. Fourth, bringing megafauna back to America would also bring tourist and other dollars into nearby communities and enhance the public’s appreciation of the natural world. More than 1.5 million people visit San Diego’s Wild Animal Park every year to catch a glimpse of large mammals. Only a handful of U.S. national parks receive that many visitors. Last, the loss of some of the remaining species of megafauna in Africa and Asia within this century seems likely—Pleistocene rewilding could help reverse that.

How It Might Be Done

We are not talking about backing up a van and kicking some cheetahs out into your backyard. Nor are we talking about doing it tomorrow. We conceive of Pleistocene rewilding as a series of staged, carefully managed ecosystem manipulations. What we are offering here is a vision—not a blueprint—of how this might be accomplished. And by no means are we suggesting that rewilding should be a priority over current conservation programs in North America or Africa. Pleistocene rewilding could proceed alongside such conservation efforts, and it would likely generate conservation dollars from new funding sources, rather than competing for funds with existing conservation efforts.

The long-term vision includes a vast, securely fenced ecological history park, encompassing thousands of square miles, where horses, camels, elephants and large carnivores would roam. As happens now in Africa and regions surrounding some U.S. national parks, the ecological history park would not only attract ecotourists but would also provide jobs related both to park management and to tourism.

To get to that distant point, we would need to start modestly, with relatively small-scale experiments that assess the impacts of megafauna on North American landscapes. These controlled experiments, guided by sound science and by the fossil record, which indicates what animals actually lived here, could occur first on donated or purchased private lands and could begin immediately. They will be critical in answering the many questions about the reintroductions and would help lay out the costs and benefits of rewilding.

One of these experiments is already under way. Spurred by our 2004 meeting, biologists recently reintroduced Bolson tortoises to a private ranch in New Mexico. Bolson tortoises, some weighing more than 100 pounds, once grazed parts of the southwestern U.S. before disappearing around 10,000 years ago, victims of human hunting. This endangered tortoise now clings to survival, restricted to a single small area in central Mexico. Thus, the reintroduction not only repatriates the tortoise to the U.S., it increases the species’ chance for survival. Similar experiments are also occurring outside North America [see box on page 77].

The reintroduction of wild horses and camels would be a logical part of these early experiments. Horses and camels originated on this continent, and many species were present in the late Pleistocene. Today’s feral horses and asses that live in some areas throughout the West are plausible substitutes for extinct American species. Because most of the surviving Eurasian and African species are now critically endangered [see “Endangered Wild Equids,” by Patricia D. Moehlman; Scientifi c American, March 2005], establishing Asian asses and Przewalski’s horse in North America might help prevent the extinction of these animals. Bactrian camels, which are critically endangered in the Gobi Desert, could provide a modern proxy for Camelops, a late Pleistocene camel. Camels, introduced from captive or domesticated populations, might benefit U.S. ecosystems by browsing on woody plants that today are overtaking arid grasslands in the Southwest, an ecosystem that is increasingly endangered.

Another prong of the project would likely be more controversial but could also begin immediately. It would establish small numbers of elephants, cheetahs and lions on private property.

Introducing elephants could prove valuable to nearby human populations by attracting tourists and maintaining grasslands useful to ranchers (elephants could suppress the woody plants that threaten southwestern grasslands). In the late Pleistocene, at least four elephant species lived in North America. Under a scientifi c framework, captive elephants in the U.S. could be introduced as proxies for these extinct animals. The biggest cost involved would be fencing, which has helped reduce conflict between elephants and humans in Africa.

Many cheetahs are already in captivity in the U.S. The greatest challenge would be to provide them with large, securely fenced areas that have appropriate habitat and prey animals. Offsetting these costs are benefi ts—restoring what must have been strong interactions with pronghorn, facilitating ecotourism as an economic alternative for ranchers, many of whom are struggling financially, and helping to save the world’s fastest carnivore from extinction.

Lions are increasingly threatened, with populations in Asia and some parts of Africa critically endangered. Bringing back lions, which are the same species that once lived in North America, presents daunting challenges as well as many potential benefi ts. But private reserves in southern Africa where lions and other large animals have been successfully reintroduced offer a model—and these reserves are smaller than some private ranches in the Southwest.

If these early experiments with large herbivores and predators show promising results, more could be undertaken, moving toward the long-term goal of a huge ecological history park. What we need now are panels of experts who, for each species, could assess, advise and cautiously lead efforts in restoring megafauna to North America.

A real-world example of how the reintroduction of a top predator might work comes from the wolves of Yellowstone National Park [see “Lessons from the Wolf,” by Jim Robbins; Scientific American, June 2004]. The gray wolf became extinct in and around Yellowstone during the 1920s. The loss led to increases in their prey—moose and elk— which in turn reduced the distribution of aspens and other trees they eat. Lack of vegetation destroyed habitat for migratory birds and for beavers. Thus, the disappearance of the wolves propagated a trophic cascade from predators to herbivores to plants to birds and beavers. Scientists have started to document the ecosystem changes as reintroduced wolves regain the ecological role they played in Yellowstone for millennia. An additional insight researchers are learning from putting wolves back into Yellowstone is that they may be helping the park cope with climate change. As winters grow milder, fewer elk die, which means less carrion for scavengers such as coyotes, ravens and bald eagles. Wolves provide carcasses throughout the winter for the scavengers to feed on, bestowing a certain degree of stability.

The Challenges Ahead

As our group on the ranch in New Mexico discussed how Pleistocene rewilding might work, we foresaw many challenges that would have to be addressed and overcome. These include the possibility that introduced animals could bring novel diseases with them or that they might be unusually susceptible to diseases already present in the ecosystem; the fact that habitats have changed over the millennia and that reintroduced animals might not fare well in these altered environments;

and the likelihood of unanticipated ecological consequences and unexpected reactions from neighboring human communities. Establishing programs that monitor the interactions among species and their con sequences for the well-being of the ecosystem will require patience and expertise. And, of course, it will not be easy to convince the public to accept predation as an important natural process that actually nourishes the land and enables ecosystems to thrive. Other colleagues have raised additional concerns, albeit none that seems fatal [see box on opposite page].

Many people will claim that the concept of Pleistocene rewilding is simply not feasible in the world we live in today. I urge these people to look to Africa for inspiration. The year after the creation of Kruger National Park was announced, the site was hardly the celebrated mainstay of southern African biodiversity it is today. In 1903 zero elephants, nine lions, eight buffalo and very few cheetahs lived within its boundaries. Thanks to the vision and dedication of African conservationists, 7,300 elephants, 2,300 lions, 28,000 buffalo and 250 cheetahs roamed Kruger 100 years later—as did 700,000 tourists, bringing with them tens of millions of dollars.

In the coming century, humanity will decide, by default or design, the extent to which it will tolerate other species and thus how much biodiversity will endure. Pleistocene rewilding is not about trying to go back to the past; it is about using the past to inform society about how to maintain the functional fabric of nature. The potential scientifi c, conservation and cultural benefi ts of restoring megafauna are clear, as are the costs. Although sound science can help mitigate the potential costs, these ideas will make many uneasy. Yet given the apparent dysfunction of North American ecosystems and Earth’s overall state, inaction carries risks as well. In the face of tremendous uncertainty, science and society must weigh the costs and benefits of bold, aggressive actions like Pleistocene rewilding against those of business as usual, which has risks, uncertainties and costs that are often unacknowledged. We have a tendency to think that if we maintain the status quo, things will be fi ne. All the available information suggests the opposite.


What the Critics Say

Since we proposed the rewilding idea in print, in Nature in 2005, commentators have pointed out a number of concerns, some legitimate, some not. “We all remember ‘Jurassic Park,’” wrote Dustin Rubenstein and his colleagues in the journal Biological Conservation. “Pleistocene re-wilding of North America is only a slightly less sensational proposal.” We disagree

with this assessment because the majority of dinosaurs went extinct 65 million years ago, whereas many of North America’s original megafauna or very close relatives are alive today else where in the world and can be both studied and saved.  

Rubenstein and colleagues go on to say, “Modern day proxies species are wrong . . . different genetically from the species that occurred in North America during the Pleistocene.” True, but not that different. Available evidence indicates that the lions in Africa and Asia today are the same species, albeit of smaller stature, as the lions that prowled North America 13 millennia ago. Recent studies of ancient DNA have elucidated close relationships between extinct elephant and horse species and those alive today. Further, introduction of proxies for now extinct species has proved successful in other experiments. Hundreds of peregrine falcons from Australia, Europe and South America were used, for example, in captivebreeding programs to reintroduce the peregrine falcon to parts of the U.S. and Canada where DDT had wiped it out. Those birds were certainly different genetically from the ones that once soared over the Midwest, yet they have done well in their new homes. “One can only imagine ... farmers coping with crop destruction by herds of elephants, or lions and cheetah attacking cattle, or even children,” Rubenstein and his colleagues warn. One need not merely imagine the challenges of coexisting with large predators and herbivores. Africa and Asia have been struggling with them for centuries, and substantial progress has been made; in our plan the animals will not be unrestrained.

“Global climate change since the Pleistocene extinctions makes the restoration of vanished ecosystems through large-mammal introduction quite unlikely,” wrote Christopher Smith in a letter to Nature in the weeks following the initial proposal. Many have expressed concern about the fact that North America’s ecosystems are not the same today as they were 13,000 years ago and that reintroduced animals might therefore be unable to survive in them. Whereas habitats are and will continue to be dynamic on a timescale of thousands of years, very few plants or small mammals went extinct during the late Pleistocene. The major missing component of North American ecosystems today compared with the Pleistocene is the megafauna, which we can infer are critical cogs in the wheels. —C.J.D.

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动物鸟类预知地震 高分标志

V1

鸟类对灾难的预测(没有第二篇长,也不难)长,过页,但讲得是我们中国人熟悉的概念。主要是说动物可以在地震来临前预知并提前逃离。

1p在一个地方2月一直是气候stable weather的夏天,说那是古人的wisdom(大概是说他们能准确预估气候),但是某日发生的一件事,误导了当地对天气很了解的当地人。这件事就是seabird鸟群突然一窝蜂的从 coast往内陆飞(这个很重要,我会讲清楚)。后来发现原来在他们有这种行为之后一个多小时后发生地震,揭示了这个现象。举了两个其它历史上发生的果的类似事件:鸟类异常行为——〉地震(这里好像有题,是问说这些古人的wisdom认为这群鸟类群体飞走后聚在一块通常代表什么,我选代表天气要变坏了还是什么stable weather要结束了之类的)

2p 开始解释那种鸟类是如何有这些行为的,假设(有两种猜测),要么鸟群是感知到了微震(人感知不到),要么是。。。(忘了)。但如果是鸟群感知道了微震,就会知道有地震危险,不会向内陆 飞,而是远离危险,应该向海上飞.那么这是为什么呢?解释说可是这样的,鸟群错误的把感知到的什么什么当成了indicator of storm,他们以为暴风雨来了,所以远离大海,往内路飞。(这段要看清楚,我说得已经八九不离十了)海鸟除了感应到地震前地壳的微妙变化,一定还有其他方法预知地震。

3p 举了3-4个动物预测地震的例子,说了鹅、鸭子什么的在地震前都有反常举动。中国发现鸭子不下水,哪发现鸡不回笼等等。举了中国的一些地方,还有其它国家的一些地方都有出现这些情况,有一题是问作者举这么多地方的例子都提到什么共通的东西? 最后一句话总结,说这么多动物都能感知,可能还是大气中电子什么阐释了微妙的变化。


考题:

1.  文中所有例子都提到了什么 A wildlife E birds 我选的鸟,大家上考场再扫一眼

2.  按照那些“对天气很了解的人”一直以来的认识,应该怎样:“typically,seabird如果往内陆飞,多是天气要发生变化(很确定)

3.  有一题是问作者举这么多地方的例子都提到什么共通的东西?


两栖动物在水下和陆地生存的解释 皮肤呼吸

V1 

第一段讲两栖动物有特殊的供氧系统保证它们在水下的生存;(有题关于这个系统) 说原来科学家觉得皮肤相对于肺是其次的,现在有新证据否定老观点

第二段讲着个系统是如何运做的,然后讲到了皮肤的作用,把2只青蛙蝌蚪,放进2个杯子里。一个杯子的的水氧气很足,另外一个却很少。2个礼拜后发现 DIFFUSION BARRIER不同了。结果缺氧的,皮层(DIFFUSER  BARRIER?)变薄,加强了呼吸功能,青蛙可以在短时间内把自己的皮肤变得薄,进而适应缺氧的环境,

第三段讲在陆地后 它们如何变换用肺呼吸供养而停止水下供氧系统的转化(有题) 讲repetile 和Amphibian的incomplete heart dividor 如何帮助gas exchange.说有一些动物心脏功能不强,很多的已经耗费了氧气的血液在进入肺部之前会先到皮下流一遍,这样是很好地利用了皮肤呼吸的功能

4段。 后面的结论是,  Contrary to previous prevailing concept,心脏的结构在两栖和爬行动物中PLAY A IMPORTANT ROLE TO DELIVER BLOOD WITH OXYGEN TO .....UNDER SKIN.....

细节题和高亮作用.文章很长 一屏多.其它记不清楚了.


考题:

1.      它们如何变换用肺呼吸供养而停止水下供氧系统的转化

2.      第二段的后半段(高亮部分,介绍那个实验)说明了什么?

3.      选项中哪个最能支持解剖学家对于心脏功能不好的两栖动物的看法(好像是)

4.      主题题

5.      两栖动物有特殊的供氧系统保证它们在水下的生存;(有题关于这个系统)

 

Sea butterflies

V1

Sea butterflies, also known as Thecosomata or flapping snails, are a taxonomic suborder of pelagic swimming sea snails.

Then talk about the relationship the shrimp and the sea butterflies.

They are neither the model of coexist nor parasitism. The ETS give a new concept and blalalalala

考题:

1. Question: Ask main Idea?

2. Ask the new relationship the shrimp & sea butterflies


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爬虫动物和两栖 动物的灭绝原因

V1

RC3rd     the extinction of reptile and amphibian(两栖动物) and Trias (geology majors maybe glad to see this article)

1.the academics has long been discussing how animals such as reptile and amphibian became extinct.

2.some says the appearance of dinosaur caused it.

3.there is counterevidence. some says environmental changes. there is also counterevidence.

4.the author also found meteor陨石in canada has been related to the extinction.

5. so the author thinks the extinction is not caused by any single factor, but rather by multiple factors.

Q1: the function of citing the meteor in Canada

Q2:强调陨石撞击时间的作用是什么,我选的是为了证明跟其中一些动物的灭绝时间吻合来说明一些动物确实是被陨石撞击所造而灭绝的。

Q3: 科学家已经能做到下面哪一项了...答案选estimate陨石的时间.其他的还包括1.确定争抢栖息地一定不是灭绝的原因2.那一段时间内各个事件发生的先后顺序...


V2

科学家在一个lake地带研究某一时期动物大量灭绝的原因,最初认为是因为恐龙的出现导致了很多生物被捕杀而灭绝。后来这一理论被推翻,因为有人认为是气候变化,尤其是一个时期的严重干旱导致的动物灭绝,但后来研究发现,虽然这个干旱确实导致了一些动物的灭绝,但没能导致大量动物灭绝。后来又认为是一个时期某刻陨石撞击所致,因为有人在加拿大附近发现了一个大坑,而且根据化石研究,时间也吻合,但这个理论还是只推出这一撞击只导致少量灭绝,不能导致大量灭绝。

最后一段说,科学家只能认为什么原因都有,包括干旱阿,恐龙出现阿,陨石撞击阿,可能还因为很多其他原因,所以不能确定哪个是其主导地位的。

问题有一个是强调陨石撞击时间的作用是什么,我选的是为了证明跟其中一些动物的灭绝时间吻合来说明一些动物确实是被陨石撞击所造而灭绝的。

还有一题是,最后一段infer什么,应该是。。。。我忘了,反正认真看最后一段题目不难。


又找到一个
陨石,恐龙 和史前动物灭绝
http://www.thefreelibrary.com/Impact+crater+may+lie+beneath+Lake+Huron.-a09396611


4.短文章,新老观点吧,忘记了
有一道题目是问作者的attitude,5个选项
B negative
E laudatory赞美的

另外三个都是正面词汇,同学们,千万别像我一傻就选了E,这个词的意思是"赞美的"...选negative!!!(我还想,学术文章,不应该用negative形容作者的态度,就选了那个不认识的E-_-#)


考题:

1.  the function of citing the meteor in Canada

2.  强调陨石撞击时间的作用是什么,我选的是为了证明跟其中一些动物的灭绝时间吻合来说明一些动物确实是被陨石撞击所造而灭绝的。

3.  科学家已经能做到下面哪一项了...答案选estimate陨石的时间.其他的还包括1.确定争抢栖息地一定不是灭绝的原因2.那一段时间内各个事件发生的先后顺序...

4. 问题有一个是强调陨石撞击时间的作用是什么,我选的是为了证明跟其中一些动物的灭绝时间吻合来说明一些动物确实是被陨石撞击所造而灭绝的。

5.  还有一题是,最后一段infer什么,

  6.有好多段,两栖动物和爬行类动物灭绝的原因,有恐龙出现、干旱和陨石,但是最后发现无论哪个都不是原因(考到了主旨题)

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E、自然科学类


 

拆除大坝对生态系统(ecological system)的影响

三段式

第一段好处,第二三段将由此带来的problem以及解决方法。

V1:

讲的是DAM要不要拆的问题,
我现在好象觉得在哪里看到过,不过当时没印象。

第一段讲的是 DAM建造了造成生态损害,主要有阻拦鱼类migration(后面某道题问水坝有什么问题,其中提到阻拦Nonnative的鱼migration,是干扰答案,因为这里应该指的是native的鱼的迁移), 造成 nonnative的鱼入侵等等。然后就后者展开描述:因为水坝把水拦起来了,水温会上升,含氧量也会变化,有些合适这种条件的非本地鱼喜欢这里的环境威胁到本来就在这里生活的鱼类。如果把水坝拆了,水温下降了,一些喜欢冷水的鱼(如trout——记得这个名字因为我最爱吃trout,呵呵)就会重返这里。如果拆除,那些外来的鱼就会离开,保护本地的鱼类,主要是ECOLOGY方面的,这里有一个题目。

第二段=贸然拆除DAM也会有很多损害,比如会使得一些不受欢迎的鱼溯江而上危害生态,主要是淤泥(sediment)可能会堵塞水道(choke the waterway——此处考到了,问的是拆除水坝的危害),还有由于大坝上游积累的淤泥中有很多毒素,拆除大坝也会时这些毒素随淤泥流向下游,所以很多工程师先用推土机和pipe运走淤泥再拆除水坝(这里又考了,问工程师拆除水坝的时候会干什么,我选的是移走沉积物。)还有其他例子说有什么沉积物之类的对生态有影响(没看太懂)

第三段也讲的是其实拆了DAM也会有其他的不好的情况发生。举了美国Arizona那边一个大坝的例子,说拆除大坝可以拯救一种什么青蛙,但同时又会使一些危害鱼类得以跑到上游。于是科学家们想了种方法,就是把想要保护的青蛙鱼类的给捕起来,,搞了很多复杂的方式,又要保留水坝后面的湖,又把水改了道(可能为了疏通迁徙吧),。然后往大坝下游投毒杀死crayfish(此处我没有看太明白,但是没有影响后面的做题)再拆除大坝放生这些保护物种。但是结果却是那些危害鱼类没给完全毒死,问题里有涉及到大坝的usually effect,没太看明白,因为每个选项都是文中说的影响,大概关键在于usually吧。
很多细节题目。有个题目是问,文章接下来的一段最没有可能出现什么内容(我越写越觉得做过,大家翻翻GWD,我没有找到,大家帮忙)。

          

考题:

1.     一个题是关于沉积物的,说engineer随敏感的是什么当他们再移走大坝之前,我选的是移走沉积物。

2.     问的是拆除水坝的危害主要是淤泥(sediment)可能会堵塞水道choke the waterway

3.     问工程师拆除水坝的时候会干什么很多工程师先用推土机和pipe运走淤泥再拆除水坝

问水坝有什么问题,其中提到阻拦Nonnative的鱼migration,是干扰答案,因为这里应该指的是native的鱼的迁移
4. 一题问remove a dam usually会导致什么。我仔细看选项,真的每个选项原文都有提到,我不知道题目的重点是a dam还是usually,随便选了。


参考阅读

Dams have long been acknowledged for providing electricity without the pollution of other methods, for flood protection, and for making water available for agriculture and human needs. Within recent decades, however, the environmental impacts of dams have been debated. While dams do perform important functions, their effects can be damaging to the environment. People have begun to question whether the positive contributions of some dams are outweighed by those negative effects. Because water is held behind the dam and often released from some depth, the temperature of the water below the dam is usually lower than it would be prior to dam emplacement. The temperature of the water flow is often constant, not reflecting the natural seasonal variations that would have been the case in the free-flowing river. Similarly, the chemistry of the water may be altered. Water exiting the lake may be higher in dissolved salts or have lower oxygen levels than would be the case for a free-flowing river.The environmental changes described above create a new environment in which native species may or may not be able to survive. New species frequently invade such localities, further disrupting the system. Early photographs of rivers in the southwest desert illustrate the dramatic modern invasion of non-native plants. Entire lengths of these rivers and streams have been transformed from native desert plants to a dense riparian environment. Native species that formerly lived in this zone have been replaced as a result of the changes in river flow patterns. The most commonly cited species affected by the presence of dams is the salmon. Salmon have been isolated from their spawning streams by impassable dams. The situation has been addressed through the use of fish ladders and by the use of barges to transport the fish around the obstacles, but with only limited success.


Medical tests(病症检测)

V1

就一段,关于medical里面一个screen tests and screen strategies的。分别给false positive和false negative下定义:是有病症却没有检测到和没有病症却检测到(这里大家去google一下到底哪个是哪个,我有点晕了)。然后说为了防止false positive和false negative分别采用了两种方法一个是se..tive(词记不起来了,针对的是false negative),另一个是re..tive(词记不起来了,针对的是false positive),也分别给他们下了定义,并说了其中一个比另一个好。


Old V2  Q49 V40 TOTAL 730 the second reading

 Medical diagnostic Screen Test 医学界有一部分学者一直强调Medical diagnostic screen test 的重要性。这种sreen test就是定期对一大群并没有任何症状的人进行检查。通过这样普遍性的screen test,如果有发现问题可以尽早得出解决办法(pre-exempt treatment)。然而也有人说这种方法的是一种浪费。首先,这样大规模的检查是很昂贵的。再说了,早期诊断出病症和能够治疗病症是两回事,因为医学 上的一些限制,很多情况下,就算诊断出病症,也是无法根治。而且,这种screen test还经常有错误errors。它只要有两种错误。第一种叫做false positive errors,就是当被检查的人没有病的时候,检查结果却说他有病。第二种叫做false negative errors,就是当被检查人有病的时候,却说他没有病。第一种错误是非常costly的,因为一旦检查结果是positive,医生们就需要 followup treatment,还有再研究,如果最后发现其实结果的错误的话,就浪费了很多人力物力。所以医学界大部分人宁可检查结果多一点false negative errors.因为如果有人第一次被漏掉了,很有可能会在下一次的检查中被发现。

考了一道主题题,一个关于false positive and false negative errors 的细节题, 一个关于pre-exempt的细节题。

考题:

1.     考了一道主题题,我选了比较了两种方法

2.     一个关于false positive and false negative errors 的细节题

3.     一个关于pre-exempt的细节题

4. 如果要使screening test更加specific,应该怎么样。

5.细节题:作者做了下列事情Except,我选得E(这个比较确定)

  A define false positive

  B define false negative

  C 说明了运用se..tive的好处

  D 说明了运用re..tive的好处

  E说哪种病可以更好的被采用这种screen strategies

6. 细节题:以下哪个是re..tive的(即针对false positive):选E,定位到re..tive的定义处说fewer false positive即可解决。E选项是:replacing 10%的false positive with 5%的false positive。


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methane甲烷on global warming

共4段

V1 新旧JJ混合

1P说甲烷和二氧化碳一样是一种温室气体;也会造成global warming。列举了造成大气中M物质增加的原因,如燃烧石化燃料等。fuel fossil burn, fire and other.(有题考这段的作用,我认为是提供背景资料)

2P “Surprisingly”(转折)科学家发现植物plant也会释放M,提出如卫星空照的证据,说热带地区因为有较密集的丛林tropical forest,所以大气中的M特别集中。The article listed two studys to demonstrate that the plants really emit the methane.

3P (有些地方没读通) 继续说这一发现可以用于解释ice age前后甲烷的变化;似乎是说植物释放M也可以解释古老的冰块中的气泡浬为何也有M…植物排放M的事实也解释了另一个科学谜题,即为什么古老的冰层 取样中有小气泡含有S(又一个不认识的单词)。。。。可能是说随着冰河入到海洋,海底也沉积了很多M,上一个冰河时期的结束可能就是这些储存在海底的M被释放的结果。但是证据显示海底大概四万年都没有剧烈变动,所以这个应该不是导致冰河期结束的原因。推测应该是植物大量的繁衍,释放出M,导致平均气温越来越高才使得冰河期结束。

4P 虽然植物会释放M,但是希望藉由减少植物来阻止溫室效应仍然是不对的,但是全球变暖是不可逆的,还得有植物。因为植物可以吸收其它更多的温室气体。想要缓和温室效应还是应该从减少石化原料fuel.的使用下手。


考题:

1.  有题考这段的作用,我认为是提供背景资料

2.  有考一题问文章”主题”

3.   

REM  Sleep helps to forget 睡眠和记忆

文章好像有4段,但后面3段都不长,而且条理很清晰。

V1

关于睡眠和记忆。一开始说之前人觉得睡眠可以增进记忆,但后来发现这个观点时错的。It is about sleep. Originally accepted  theory stated that the sleep helps memory, however, recent study states that sleep helps to forget rather than to remember.

然后举了一个叫Tonion (就这几个字母拼程的人)人的实验结果和理论说,睡眠和记忆的关系。And then provide some evidence to show that sleep really helps to forget. The REM is involved in this reading.

考题:


碳化物与气温关系 GWD或PREP题 待求证,请帮忙吧
    V1

温室效应,又是篇超长文章,整个第二段被highlight了。。。题目基本是第二段的,

第一段:Aerosol导致了温室效应不明显,让空气的温度变低,atlantic海水冷了,paradoxly,原因竟然是由于CO2过多造成的南极冰川融化导致的。

第二段:讲的是由于大气中的carbon dioxide收支不平衡之类的导致气候变冷,然后讲了具体过程,说是石头之类的东东里的CO2被一种叫weathering process的东东给弄出来了,然后到海里,然后被植物和动物吸收,最后变成化石被掩埋。然后说是一种updrift的地壳运动之类的东东会加速weathering process。说了三个problem,第一个是对海洋的影响比对海洋上的冰的影响大,有题(希望牛牛补充)。第三个影响最严重。

基本上认真看第二段是可以做题了,题目也好想有6道。

        

Old V2

洋流让北半球变冷的那道

第一段:说有一个mini-ice age小冰河期要imminent,有意思的是小型冰川效应却是由温室效应引起的。然后就解释了一下为什么,就是说南极的冷水流入大西洋,和一个什么洋流碰上了,那个洋流的作用是吧来自tropic(这词不明白)的热量散发到大气里,会让大西洋两边都变暖,剩下的忘了。

第二段这里出现一个trans开头的circular结尾的词,有两道定位题围绕它出,就是这个词的意思就是当暖流的热量放出后,平常从墨西哥湾流出来的暖流能给大西洋两岸提供热量,本来是Gulf 暖流会把热带的海水带到大西洋然后给它加温的,有一个process,我考到这个process的细节题,但是因为南极冰水的注入,使得这个process被打乱了所以大西洋海水反而冷了。现在由于某种作用,冷的更密度大的水进OCEAN之后的影响水变冷了之后沉到下面去了,冷水就会sink到海平面下1英里的地方去,所以不能再给大西洋两岸提供热量,导致气温变冷。有一题是问水变冷了之后沉到水下有什么后果,我选的是导致大西洋两岸的陆 地气温下降。这样导致一种V开头的什么现象会减缓最终停止。gulf会将从赤道的暖流往北推-流动途中会将沿途温度提升-温度降低了的水会沉到海面一英里下(隐含:这里就是暖流结束的地方-有考点叫某某front),由于温室效应-北极冰融-至北向南的寒流加强(gulf的暖流是至南向北)-将寒流暖流交汇处往南推(增加了交汇处往北的地区,这些地方无法被暖流加热于是总体温度降低),原本平衡大西洋俩岸温度的从赤道来的暖水会被阻慢。关于这个海水为啥变冷的地方有题。

          

Old V3 不同内容,注意

科学家发现最近40million years,地球不再是原来那么warm和wet了(此处有题),先给出了一个流派的若干解释:随着二氧化碳的增多,大气的降水中融解了二氧化碳,这些水降到海面,被各种过程吸收,然后沉积到海底,虽然到海底这些c最终还是要回到大气中,但是这个过程需要hundreds of millions of years(隐含40百万年对它来说是相对短的过程,此处有题),另外陆面也对二氧化碳的吸收起到一定作用,而且随着内海的面积逐渐减少,陆面的面积越来越大因而吸收c也越多。第一段的末尾说这个解释不错,但作为唯一的解释未免不让人信服。下一段是讲好像叫M R的人提出一种观点,对第一段的解释起到支持作用,他说地质演变抬高了陆地某些位置,高了之后会有更多的fresh岩石吸收c,而且因为抬高了后这些位置比较陡,降水可以更好的冲走这些吸收了c的岩石。4个问题,比较长。


考题:

1.      有一题是问水变冷了之后沉到水下有什么后果,我选的是导致大西洋两岸的陆 地气温下降

2.      我考到这个process的细节题,但是因为南极冰水的注入,使得这个process被打乱了所以大西洋海水反而冷了。

3.      关于这个海水为啥变冷的地方有题

4.      有考点叫某某front  (这里就是暖流结束的地方)

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参考阅读 http://www.columbia.edu/~vjd1/carbon.htm

The Carbon Cycle and Earth's Climate

Carbon dioxide is an atmospheric constituent that plays several vital roles in the environment. It is a greenhouse gas that traps infrared radiation heat in the atmosphere. It plays a crucial role in the weathering of rocks. It is the carbon source for plants. It is stored in biomass, organic matter in sediments, and in carbonate rocks like limestone.

The Carbon Cycle

The primary source of carbon/CO2 is outgassing from the Earth's interior at midocean ridges, hotspot volcanoes, and subduction-related volcanic arcs. Much of the CO2 released at subduction zones is derived from the metamorphism of carbonate rocks subducting with the ocean crust. Much of the overall outgassing CO2, expecially as midocean ridges and hotpot volcanoes, was stored in the mantle when the Earth formed. Some of the outgassed carbon remains as CO2 in the atmosphere, some is dissolved in the oceans, some carbon is held as biomass in living or dead and decaying organisms, and some is bound in carbonate rocks. Carbon is removed into long term storage by burial of sedimentary strata, especially coal and black shales that store organic carbon from undecayed biomass and carbonate rocks like limestone (calcium carbonate).

 

 

Photosynthesis

Plants and photosynthetic algae and bacteria use energy from sunlight to combine carbon dioxide (C02) from the atmosphere with water (H2O) to form carbohydrates. These carbohydrates store energy. Oxygen (O2) is a byproduct that is released into the atmosphere. This process is known as photosynthesis.

carbon dioxide + water + sunlight -> carbohydrate + oxygen

CO2 + H2O + sunlight -> CH2O + O2

 

Respiration

Plants (and photosynthetic algae and bacteria) then use some of the stored carbohydrates as an energy source to carry out their life functions. Some of the carbohydrates remain as biomass (the bulk of the plant, etc.). Consumers such as animals, fungi, and bacteria get their energy from this excess biomass either while living or dead and decaying. Oxygen from the atmosphere is combined with carbohydrates to liberate the stored energy. Water and carbon dioxide are byproducts.

oxygen + carbohydrate -> energy + water + carbohydrate

O2 + CH2O -> energy + H2O + CO2

Notice that photosynthesis and respiration are essentially the opposite of one another. Photosynthesis removes CO2 from the atmosphere and replaces it with O2. Respiration takes O2 from the atmosphere and replaces it with CO2. However, these processes are not in balance. Not all organic matter is oxidized. Some is buried in sedimentary rocks. The result is that over geologic time, there has been more oxygen put into the atmosphere and carbon dioxide removed by photosynthesis than the reverse.

 

Weathering

Carbon dioxide and the other atmospheric gases dissolve in surface waters. Dissolved gases are in equilibrium with the gas in the atmosphere. Carbon dioxide reacts with water in solution to form the weak acid, carbonic acid. Carbonic acid disassociates into hydrogen ions and bicarbonate ions. The hydrogen ions and water react with most common minerals (silicates and carbonates) altering the minerals. The products of weathering are predominantly clays (a group of silicate minerals) and soluble ions such as calcium, iron, sodium, and potassium. Bicarbonate ions also remain in solution; a remnant of the carbonic acid that was used to weather the rocks.

 

 

Carbonate Rocks

1. Carbon dioxide is removed from the atmosphere by dissolving in water and forming carbonic acid

CO2 + H2O -> H2CO3 (carbonic acid)

2. Carbonic acid is used to weather rocks, yielding bicarbonate ions, other ions, and clays

H2CO3 + H2O + silicate minerals -> HCO3- + cations (Ca++, Fe++, Na+, etc.) + clays

3. Calcium carbonate is precipitated from calcium and bicarbonate ions in seawater by marine organisms like coral

Ca++ + 2HCO3- -> CaCO3 + CO2 + H2O

the carbon is now stored on the seafloor in layers of limestone


 

Metamorphism of Carbonates

Some of this carbon is returned to the atmosphere via metamorphism of limestone at depth in subduction zones or in orogenic belts

CaCO3 + SiO2 -> CO2 + CaSiO3

followed by outgassing at the volcanic arc.

 

 

The Greenhouse Effect

Most of the sun's energy that falls on the Earth's surface is in the visible light portion of the electromagnetic spectrum. This is in large part because the Earth's atmosphere is transparent to these wavelengths (we all know that with a functioning ozone layer, the higher frequencies like ultraviolet are mostly screened out). Part of the sunlight is reflected back into space, depending on the albedo or reflectivity of the surface. Part of the sunlight is changed into infrared (lower frequency than visible light). While the dominant gases of the atmosphere (nitrogen and oxygen) are transparent to infrared, the so-called greenhouse gasses, primarily water vapor (H2O), carbon dioxide, and methane (CH4), absorb the infrared radiation. They collect this heat energy and hold it in the atmosphere. While we worry about possible global warming from the additional CO2 we put into the atmosphere by burning fossil fuels, if there was no CO2 in the atmosphere the global climate would be significantly cooler.

 

 

The Climate Buffer

Because of the role of CO2 in climate, feedbacks in the carbon cycle act to maintain global temperatures within certain bounds so that the climate never gets too hot or too cold to support life on Earth. The process is a large-scale example of LeChatelier's Principle. This chemical principle states that if a reaction at equilibrium is perturbed by the addition or removal of a product or reactant, the reaction will adjust so as to attempt to bring that chemical species back to its original concentration. For example, as carbonic acid is removed from solution by weathering of rocks, the reaction will adjust by producing more carbonic acid. And since the dissolved CO2 is in equilibrium with atmospheric CO2, more CO2 is removed from the atmosphere to replace that removed from solution by weathering.


some examples:

If CO2 concentration increases in the atmosphere because of an increased rate of outgassing, global temperature will rise. Rising temperature and more dissolved CO2 will lead to increased weathering of crustal rocks as a result of faster reaction rates (temperature effect) and greater acidity. Enhanced weathering will use up the excess CO2 thereby cooling the climate.

If global temperature cools as a result of some astronomical forcing or tectonic/ocean circulation effect, the lower temperatures will result in lower rates of chemical weathering. Decreased weathering means less CO2 being drawn from the atmosphere by weathering reactions, leaving more CO2 in the atmosphere to increase temperatures.

If more rocks become available for rapid weathering as a result of mountain uplift the enhanced weathering will draw down atmospheric CO2 and decrease global temperatures. But the decreased temperatures will slow reaction rates, thereby using less CO2, thus allowing temperatures to moderate.

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