HUNTING FOR ANTARCTICA'S OLDEST ICE

• Published in: Ice and Snow
• Main Authors: V. Ya. Lipenkov, A. A. Ekaykin
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: Nauka 2018
• Subjects: антарктида; гидраты; глубокое бурение; датирование льда; древний лёд; климатическая перестройка; палеоклиматическая реконструкция; плейстоцен; Science; Q; Antarctic; The Antarctic; Austral; East Antarctic Ice Sheet; Vostok Station; Antarc*; EPICA; ice core; Ice Sheet; Антарктида
• Online Access: https://doi.org/10.15356/2076-6734-2018-2-255-260; https://doaj.org/article/210c9601129d43c58b482651ec890433

One of the key priority tasks for the international Antarctic community is drilling and studying old Antarctic ice with age exceeding 1 million years in order to investigate possible reasons for the Mid-Pleistocene Transition. During the 2017–2018 austral season at Vostok Station, we carried out microscopic study of geometrical properties of the crystalline inclusions of air hydrates in ice core samples from boreholes 5G‑3 (Vostok) and DC2 (EPICA DC) in depth intervals where the age of the ice exceeded 400,000 years. The obtained data confirmed the existence of a robust linear relationship between the mean radius of the hydrates and the age of the ice in the bottom part of the East Antarctic ice sheet, and will be useful for further development of the new dating technique based on the phenomena of hydrate growth in polar ice. Preliminary, the age of the atmospheric ice bedded at Vostok at a depth of3538 m, inferred from the data on the size of the hydrates, amounts to 1.3±0.17 million years. The existence of ice older than 1 million years in the vicinity of Vostok implies that in the area of Ridge B, where the ice flow line which passes through Vostok Station originates, even older ice, with undisturbed stratigraphy, may exist. It would be desirable therefore to carry out a glacio-geophysical traverse to Ridge B in order to implement a detailed study of Dome B area aimed at identifying the most suitable site for a new deep drilling of the Antarctic ice sheet.