想请教OG10阅读第9篇,实在不明白这一段是什么意思,请同学们帮忙看一下到底O18和O16的比例在冰河期是变大了还是变小了。。划线部分谁能给翻译一下啊,多谢了!!! To establish such a chronology it is necessary to determine the relative amounts of land ice that existed at various times in the Earth’s past. A recent discovery (10) makes such a determination possible: relative land-ice volume for a given period can be deduced from the ratio of two oxygen isotopes, 16 and 18, found in ocean sedi- ments. Almost all the oxygen in water is oxygen 16, but a few molecules out of every thousand incorporate the (15) heavier isotope 18. When an ice age begins, the conti- nental ice sheets grow, steadily reducing the amount of water evaporated from the ocean that will eventually return to it. Because heavier isotopes tend to be left behind when water evaporates from the ocean surfaces, (20) the remaining ocean water becomes progressively enriched in oxygen 18. The degree of enrichment can be determined by analyzing ocean sediments of the period, because these sediments are composed of calcium carbonate shells of marine organisms, shells that were (25) constructed with oxygen atoms drawn from the sur- rounding ocean. The higher the ratio of oxygen 18 to oxygen 16 in a sedimentary specimen, the more land ice there was when the sediment was laid down. |