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AMS radiocarbon ages of three massive ice bodies on the coast of Mechigmen Ba...
Radiocarbon dating of micro-inclusions of organic material extracted directly from massive ice samples was carried out at the Laboratory of Radiocarbon Dating and Electron... -
Composition and content of water soluble salts in Late Pleistocene syngenetic...
Hydrogeochemistry of ice wedges and host sediments. Determination of the content of water soluble salts in ice wedges has been performed by titration in the laboratory of PNIIIS... -
The AMS radiocarbon dating of organic microinclusions in syngenetic Late Plei...
Radiocarbon dating of organic macrofossils (mainly grass roots and shrub twigs) out of the yedoma deposits has been carried out at the Geological Institute of the Russian... -
Compiled radiocarbon dating of Late Pleistocene syngenetic ice-wedges, northe...
Radiocarbon dating of Late Pleistocene syngenetic ice-wedges, northern Eurasia (after Vasil'chuk, 1991; 1992; additional Data supplied by S. Gubin, Ye. Slagoda, A. Kotov, and S.... -
Radiocarbon dating of allochthonous organic matter in three neighbouring vert...
The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky). -
Radiocarbon dates from organic material, Sakha, Russia
The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky) and in the Radiocarbon Laboratory of Helsinki University (H.... -
Cryogenic structures of Late-Pleistocene Yedoma and Holocene peat strata of A...
The composition of deposits and cryogenic structure of Late-Pleistocene Yedoma and Holocene peat strata of Ayon Island. -
Database of Ice-Rich Yedoma Permafrost Version 2 (IRYP v2)
Ice-rich permafrost in the circum-Arctic and sub-Arctic, such as late Pleistocene Yedoma, are especially prone to degradation due to climate change or human activity. When... -
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygon...
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice... -
Minimal, average, and maximum values of δ¹⁸O in ice wedge of the sections fro...
The oxygen isotope composition of the Late Pleistocene and Holocene syngenetic ice wedges, exposed at Mamontova Gora and Syrdakh Lake, is determined. In the area of Mamontova... -
Radiocarbon dating of Late Pleistocene and Holocene ice wedges in Mamontova G...
Radiocarbon dating of the Late Pleistocene and Holocene syngenetic ice wedges, exposed at Mamontova Gora, are determined. The age of the ice wedges is shown to be younger than... -
AMS radiocarbon dating (22-27 cal Ka BP) of massive ice on the coast of Mechi...
Field studies of the Eastern Chukotka's massive ice carried out in 2016, 2017, and 2020. The three key sites of the studied massive ice bodies are located on the coast of... -
Radiocarbon Dating and Oxygen Isotope Variations in Late Pleistocene Syngenet...
The occurrence of well-preserved redeposited organic material is the main limitation for radio-carbon dating of syngenetic permafrost sediments. Only radiocarbon dating of (1)... -
Element analysis of sediment core SO217-18522 (GIK18522-3)
This dataset has no description
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Isotope record of Planulian wuellerstorfi of sediment core SO217-18522 (GIK18...
This dataset has no description
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Age determination of sediment core SO217-18522 (GIK18522-3)
This dataset has no description
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Northeastern Kalimantan hydroclimate of Core SO217-18522 over 50 kyrs
Changes in convective activity and hydroclimate over Northeastern Kalimantan are key features to understand glacial to interglacial climate evolution in the center of the West... -
Speciated mechanism in Quaternary Cervids (Cervus and Capreolus) on both side...
Cervids, and especially the red deer Cervus elaphus, are among the most regularly and abundantly recorded ungulates in Pleistocene/Paleolithic bone assemblages. Numerous... -
Relative intensity and age depostion range in the north of the South China Se...
Relative intensity (RPI) was constructed using the equation:RPI=NRM((20-60)mT)/SIRM (20-60)mTwhere SIRM were imparted with DC fields of 1000 mT, then demagnetized using 20,... -
Stacked dole effect in the north of the South China Sea from sediment core PC...
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM
