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地球气候系统过去的变化均被“写入岩石”。尘土和冰堆积物的性质与特征、湖泊和大洋沉积物,沙丘原和河流台地,植物和动物化石组合序列、古海岸线、珊瑚生长线、树木的年轮与碳酸盐洞穴沉积层,以及古代社会的古生态和文字记录,都包含了这一历史的元素。人类的历史与文化在很大程度上归功于过去的气候多变性。了解过去的气候就是向了解我们从古至今的演变历史迈进了一步。毫无疑问,我们的将来也将受到气候的强烈影响。关于长期气候记录的新观点对于现代社会是很重要的,因为它为我们了解近期的趋向及其可能的原因提供了基础。全新世初期(大约10.000年前)人类对气候系统基本
Past changes in the Earth’s climate system have been “written into the rock.” The nature and characteristics of dust and ice deposits, lake and ocean sediments, dune and river stations, sequences of plant and animal assemblages, ancient coastlines, coral growth lines, tree-ring and carbonate cave deposits, The paleoecology and written records of society all contain this element of history. Human history and culture owe much to past climate variability. Understanding the past climate is one step closer to understanding the evolution we have made since ancient times. There is no doubt that our future will also be strongly influenced by the climate. New perspectives on long-term climate records are important to modern society because they provide the basis for our understanding of recent trends and their possible causes. In the early Holocene (about 10,000 years ago), mankind had a basic climate system