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δ¹⁸O values of Holocene and modern ice‐wedge ice on the Chukotka Peninsula an...
Stable oxygen isotopes composition (δ¹⁸O) in modern syngenetic ice wedges (recent ice veinlets - i.e. modern ice veins formed during the last 60-100 years and penetrated into... -
δ¹⁸O values for Holocene and modern ice‐wedges at Sites 2 and 3
Stable isotope ratios (δ¹⁸O and δ²H) were analyzed at the stable isotope laboratory of the Faculty of Geography in the Lomonosov Moscow State University (headed by Prof. Yu.... -
Stable isotope (δ¹⁸O, δ²H and d) values, standard deviations, slopes and inte...
Stable isotope ratios (δ¹⁸O and δ²H) were analyzed at the stable isotope laboratory of the Faculty of Geography in the Lomonosov Moscow State University (headed by Prof. Yu.... -
Radiocarbon ages of peat and wood from the sediment adjacent to the ice‐wedge...
14C ages of bulk samples were obtained at the Institute of Geology RAS (lab code GIN) and in the Institute for the History of Material Culture, St. Petersburg (lab code Le).... -
Air temperature data from weather stations in Eastern Chukotka (for 1965–2015)
This dataset has no description
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Isotopic evidence for Holocene January air temperature variability on the Eas...
Ice‐wedge ice can provide a valuable record of past winter climate variability at high latitudes yet to date this proxy has been applied only sparsely across the Chukotka region...
