859 datasets found

The sampling site lies 425 m north-west of Behy court tomb where there were peat faces available that were suitable for sampling.A relatively long monolith (BHY VI; 54 cm peat...

The sampling site lies 25 m east of chamber of Behy court tomb where a small patch of intact uncut peat remained.A monolith 44 cm long was removed. Total depth of peat at...

The sampling site lies ca. 20 m N of Behy court tomb where an intact area of uncut peat remains.A monolith 39 cm long was removed. Total depth of peat (adjusted for shrinkage)...

The sampling sites BHY III–VI are from within the stone wall field system that is covered by blanket bog. BHY III is from ca. 65 m west of Behy Court Tomb. There was fairly...

Radiocarbon dates and calibrated ages (99.7% probability) of sediments enclosing ice wedges in the northern part of Western Siberia and north-eastern part of the East European...

δ¹⁸O, δ²H and deuterium excess (dexc) values in in the ice wedge ice (IW) and segregated ice (SI) lenses of the Yun'yaga peatland, Vorkuta region, and in the ice wedge ice from...

δ¹⁸O, δ²H and deuterium excess (dexc) values in snow from a snow patch in Vorkuta town (sampled December, 2018) and in the fresh snow (sampled December, 2005) during a single...

Paleoreconstructions based on δ¹⁸Oiw data for Late Pleistocene and Holocene syngenetic ice wedges in islands of Russian East Arctic, modified and complemented after Vasil'chuk...

Stable isotopes of Kotelny Island were measured at the Isotope Laboratory of the Faculty of Geography of Moscow University. The analysis was performed on a Finnigan Delta-V...

Oxygen isotope ratios in ice wedges were determined on a Finnigan Delta-E mass spectrometer at the Isotope Laboratory of the Institute of Geology of Estonia. Measurement errors...

Stable isotopes were measured at the Isotope Laboratory of the Faculty of Geography of Moscow University. The analysis was performed on a Finnigan Delta-V Plus mass spectrometer...

Stable oxygen isotopes composition (δ¹⁸O), hydrogen (δ²H) and deuterium excess values (dexc) in ice wedges and segregated (segr.) ice in the 6–8 m Chara River terrace and in the...

Stable oxygen isotopes composition (δ¹⁸O) in ice wedges and segregated (segr.) ices in the 6–8 m Chara River terrace, water from Chara River, rain and snow. Sampling was done in...

Radiocarbon ages from the organic plant material from the ice wedge surrounding deposits in the 6-8 m Chara River terrace in 1985 and 1988 sampling years.Samples of organic...

The values of δ18О in the ice wedges of northern Chukotka and paleotemperature characteristics during the Late Pleistocene and Holocene. Winter mean (twint.mean) and January...

Values of δ18O in the ice veinlets of modern syngenetic ice wedges on Ayon Island, in northern Chukotka and on the neighboring islands of Eastern Arctic of Russia, according to...

Composition and content of water-soluble salts in the syngenetic ice wedges of the 25–30-m Late-Pleistocene yedoma and in the modern ices and the water reservoirs of Ayon...

The composition and content of water-soluble salts in the syngenetic permafrost deposits of the 25–30-m Late- Pleistocene yedoma of Ayon Island.

Variations in δ18О values in the Late-Pleistocene (pIW) and Holocene (hIW) ice wedges and segregated ice schlieres (SIS) ices of Ayon Island.# = Isotopic analyses were...

(1) = According to (Tarakanov et al., 1974)(2) = According to (Noveishie otlozheniya i paleogeografiya pleistotsena Chukotki, 1980)