907 datasets found

The short monolith (19 cm of peat and 10 cm of the mineral soil beneath), CF Ib, was taken at 40 m NW of the Visitor Centre (VC), immediately to the north of a transverse...

The sampling site was in an extensive blanket bog, 16 km south of Céide Fields Visitor Centre, where peat cutting had revealed many pine timbers and also oak timbers. This...

The sampling site was in a small basin-bog (ca. 300 x 100 m). The basin is surrounded by blanket bog that has preserved a pre-peat, extensive stone-wall, regular field system,...

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...

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...

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)

In 2008, a 404 cm long sediment core (2008-3) was recovered from 8 m depth in the southern part of Lake Big Yarovoe. It consists mostly of striated black, grey and greenish-grey...