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A Comparison of Holocene with Pleistocene Interglacial Periods Similarities and Differences

机译:全新世与先生外夹时段相似性和差异的比较

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The Dome C ice core records indicate there have been eight cycles of ice ages and nine interglacial periods over the past 800,000 years, is approximately the second half of the Pleistocene. They appear to be occurring over approximately 100,000 years cycles due to the three Milankovitch cycles: (1) eccentricity measuring how elliptical the earth's orbital path is; (2) tilt of rotational axis; and (3) axial precession/wobble. It is thought that anthropogenic activities have caused the Holocene, the current interglacial period, to be different from the others. Is that so? If it is true in what way is the Holocene different from past interglacial periods? There is ice core record data with respect to concentration of greenhouse gases and other ion records, and by compiling the distribution of results we can compare the interglacial periods with each other. In addition to comparison to the full intervals, there are data regarding temperature, gas and ion concentrations, and rate of change throughout previous interglacial periods that can be used as a comparison with the Holocene. Methane concentrations vary throughout each interglacial period and in a manner that differs from each other with peaks either near the start or middle of an interglacial period; only the Holocene has a peak concentration towards end of period, as a result of anthropogenic influences.
机译:圆顶C冰核心记录表明过去80万年的冰龄和九个中间峡期时期都有八个周期,大约是优秀滋卵剂的下半部分。由于三个米兰科接收周期,它们似乎发生在大约100,000年周期中:(1)偏心测量地球的轨道路径如何椭圆形; (2)倾斜旋转轴; (3)轴向预防/摆动。据认为,人为的活动导致全新世,目前的中间夹峰期,与其他人不同。是这样吗?如果它是真实的,全新女与过去的中间夹次时期不同?关于温室气体的浓度和其他离子记录的浓度有冰核记录数据,并通过编制结果的分布,我们可以比较彼此的中间尖端时期。除了与全间隔进行比较之外,还有关于温度,气体和离子浓度的数据,以及在先前的间冰片时期的变化率,可用作与全茂的比较。甲烷浓度在每个屏幕周期内变化,并且以彼此不同的方式,峰值靠近侧面的开始或中间的峰值;由于人为的影响,只有全茂的峰值浓度朝向时期的峰值浓度。

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