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Volcanic synchronization of Dome Fuji and Dome C Antarctic deep ice cores over the past 216 kyr

机译:过去216年的富士圆顶和C圆顶南极深层冰芯的火山同步

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Two deep ice cores, Dome Fuji (DF) and EPICA Dome C (EDC), drilled at remotedome summits in Antarctica, were volcanically synchronized to improve ourunderstanding of their chronologies. Within the past 216 kyr, 1401 volcanictie points have been identified. DFO2006 is the chronology for the DF corethat strictly follows O2 / N2 age constraints with interpolationusing an ice flow model. AICC2012 is the chronology for five cores, includingthe EDC core, and is characterized by glaciological approaches combining iceflow modelling with various age markers. A precise comparison between thetwo chronologies was performed. The age differences between them are within2 kyr, except at Marine Isotope Stage (MIS) 5. DFO2006 gives ages older thanAICC2012, with peak values of 4.5 and 3.1 kyr at MIS 5dand MIS 5b, respectively. Accordingly, the ratios of duration(AICC2012 / DFO2006) range between 1.4 at MIS 5e and 0.7 at MIS 5a. Whenmaking a comparison with accurately dated speleothem records, the age ofDFO2006 agrees well at MIS 5d, while the age of AICC2012 agrees well atMIS 5b, supporting their accuracy at these stages. In addition, we found thatglaciological approaches tend to give chronologies with younger ages andwith longer durations than age markers suggest at MIS 5d–6. Therefore, wehypothesize that the causes of the DFO2006–AICC2012 age differences at MIS 5are (i) overestimation in surface mass balance at around MIS 5d–6 in theglaciological approach and (ii) an error in one of the O2 / N2 ageconstraints by ~ 3 kyr at MIS 5b. Overall, we improved ourknowledge of the timing and duration of climatic stages at MIS 5. This newunderstanding will be incorporated into the production of the next commonage scale. Additionally, we found that the deuterium signals of ice, δDice, at DF tends to lead the one at EDC, with the DF lead being morepronounced during cold periods. The lead of DF is by +710 years (maximum)at MIS 5d, ?230 years (minimum) at MIS 7a and +60 to +126 years on average.
机译:在南极洲的远程穹顶处钻探的两个深冰芯,富士穹顶(DF)和EPICA穹顶C(EDC),在火山上进行了同步,以提高我们对它们年代的理解。在过去的216年中,已经确定了1401个火山点。 DFO2006是DF核心的年代,严格遵循O 2 / N 2 年龄限制,并使用冰流模型进行插值。 AICC2012是包括EDC核心在内的五个核心的时间顺序,其特征在于结合冰流建模和各种年龄标记的冰川学方法。两种时间顺序之间进行了精确的比较。除海洋同位素阶段(MIS)5之外,它们之间的年龄差异在2年之内。DFO2006给出的年龄比AICC2012年长,MIS 5d和MIS 5b的峰值分别为4.5和3.1 kyr。因此,持续时间的比率(AICC2012 / DFO2006)在MIS 5e时为1.4,在MIS 5a时为0.7。当与准确标明日期的脾疫记录进行比较时,DFO2006的年龄与MIS 5d一致,而AICC2012的年龄与MIS 5b一致,从而支持了这些阶段的准确性。此外,我们发现冰川学方法倾向于提供年龄比MIS 5d–6所建议的年龄标记年轻得多且持续时间更长的年代学。因此,我们假设MIS 5的DFO2006–AICC2012年龄差异的原因是(i)用冰川学方法高估了MIS 5d-6周围的表面质量平衡,以及(ii)O 2之一存在误差。 sub> / N 2 的年龄受MIS 5b约束〜3 kyr。总体而言,我们提高了对MIS 5的气候阶段的时间和持续时间的了解。这一新的认识将被纳入下一个通用级别的生产中。此外,我们发现在DF处,冰的氘信号δ D ice 倾向于在EDC处领先,而在寒冷时期,DF铅的发音更为明显。 MIS 5d DF的领先时间最长为+710年,MIS 7a DF的领先时间最短为+230年,平均为+60到+126年。

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