On the possibility to restore the climatic signal in the disturbed record of stable water isotope content in the old (0.4–1.2 Ma) Vostok ice (Central Antarctica)

• Published in: Ice and Snow
• Main Authors: A. Ekaykin A., V. Lipenkov Ya., A. Veres N., A. Kozachek V., A. Skakun A., А. Екайкин А., В. Липенков Я., А. Верес Н., А. Козачек В., А. Скакун А.
• Other Authors: The authors thank Russian Science Foundation for the financial support (grant 18-17-00110)., Авторы благодарят Российский научный фонд за финансовую поддержку (грант 18-17-00110).
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: IGRAS 2019
• Subjects: Antarctica; ice cores; Mid-Pleistocene Transition; old ice; paleoclimate; stable water isotopes; Vostok station; Антарктида; древний лёд; ледяные керны; палеоклимат; среднеплейстоценовый переход; стабильные изотопы воды; станция Восток; Antarctic; Vostok Station; Annals of Glaciology; Antarc*; ice core; The Cryosphere
• Online Access: https://ice-snow.igras.ru/jour/article/view/592; https://doi.org/10.15356/2076-6734-2019-4-463

In this work we have presented new detailed (with the resolution of 10 cm) stable water isotope (δD and δ18O) profile measured in the central Antarctic Vostok ice core section that contains old ice with the age from 0.4 to 1.2 million years. To interpret these data we have developed a model of molecular diffusion in ice and determined the value of so-called «diffusion length». We have demonstrated that the climatic signal in this ice interval is disturbed by a combination of two processes, ice layer folding (that is accompanied by layer overturning and mixing) and molecular diffusion. The whole old ice interval can be divided in 5 zones that differ in terms of character and intensity of these two processes. In three of these zones the climatic signal is partly preserved and could be restored to some extent. However, in the most interesting and old zone 5 (0.75–1.2 Ma) the climatic signal is nearly completely erased and could hardly be reconstructed. At the same time, the isotopic records obtained from the Vostok old ice have preserved the information on the mean level of the isotopic content of ice in glacial and interglacial stages. This gives an opportunity to reveal and study long-term climatic trends with typical duration longer than main climatic cycles (40–100 ka). Представлены новые детальные данные (с разрешением 10 см) об изотопном составе (δD и δ18O) керна со станции Восток в интервале 3318–3537 м, содержащего древний лёд возрастом 0,4–1,2 млн лет. Показано, что климатический сигнал в этом интервале льда сильно искажён совместным действием стратиграфических нарушений в залегании ледяных слоёв и молекулярной диффузии. Сделана попытка частично восстановить климатический сигнал в отдельных интервалах древнего льда.