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Chizhova, Julia N.
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δ¹⁸O values of Holocene and modern ice‐wedge ice on the Chukotka Peninsula and w...
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Isotopic evidence for Holocene January air temperature variability on the East C...
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¹⁴C AMS ages of organic matter from ice wedges and host sediments from Adventdal...
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δ¹⁸O values in the ice wedge from the Adventdalen valley, Svalbard
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δ¹⁸O values for Holocene and modern ice‐wedges at Sites 2 and 3
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Oxygen stable isotope variation in Late Holocene ice wedges in Yamal Peninsula a...
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Oxygen stable isotope variation in Late Holocene ice wedges in Yamal Peninsula a...
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Isotopic evidence for Holocene January air temperature variability on the East C...
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Air temperature data from weather stations in Eastern Chukotka (for 1965–2015)
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Isotopic evidence for Holocene January air temperature variability on the East C...
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Depth of massive ice bodies near the Sabettayakha River mouth, Yamal Peninsula,...
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Pollen and spores in massive ice, snow, sea ice and ice wedges
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Stable isotopes in the closed-system Weather Pingo, Alaska and Pestsovoye Pingo,...
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Lithalsas in the Sentsa River Valley, Eastern Sayan Mountains, Southern Russia
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Isotope composition of snow cover on a long transzonal profile of Western Siberi...
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Isotope composition of snow cover on a long transzonal profile of Western Siberi...
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Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in the core of larg...
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Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in the core of a sm...
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Oxygen and Hydrogen Isotope Compositions of Lithalsa Frozen Core: A Case Study f...
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Oxygen and Hydrogen Isotope Compositions of Lithalsa Frozen Core: A Case Study f...
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Related Subjects
Location
Sample ID
Holocene
Event label
Latitude of event
Longitude of event
permafrost
Sample comment
Sample type
radiocarbon
Russia
δ18O
ice‐wedge
stable water isotopes
Yamal Peninsula
DEPTH
DEPTH, sediment/rock
sediment/rock
Deuterium excess
massive ice
Comment
Multiple investigations
Mires
North-Eastern Europe
Oxygen isotopes
Palsa
Chukotka
Mass spectrometer Finnigan Delta-V
Reference/source
Site
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