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)

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)

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 molec...

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Bibliographic Details
Main Authors: A. A. Ekaykin, V. Ya. Lipenkov, A. N. Veres, A. V. Kozachek, A. A. Skakun
Format: Article
Language:Russian
Published: Nauka 2019-12-01
Series:Lëd i Sneg
Subjects:
antarctica
ice cores
mid-pleistocene transition
old ice
paleoclimate
stable water isotopes
vostok station
Online Access:https://ice-snow.igras.ru/jour/article/view/592

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