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New AMS Dates of Organic Microinclusions in Ice Wedges from the Lower Part of...
Accelerator mass spectrometry (AMS) dating of organic microinclusions was performed on eight samples from the lower part of the thick Pleistocene syngenetic ice wedges exposed... -
Ramped pyrolysis oxidation and related 14C data sets of particulate phase cre...
The data was obtained by performing ramped pyrolysis and oxidation with 14C analysis of the emitted CO2 gases using the sedimentary residue of incubated permafrost soil (Yedoma)... -
Stable isotopes and radiocarbon measurements of sediment core MD99-2220
The 51.58 m long marine sediment core MD99-2220 was raised from the Laurentian Channel in the St. Lawrence Estuary during the IMAGES-V (International Marine Past Global Change... -
δ¹⁸O in ice wedges of yedoma deposits and Late Pleistocene paleotemperatures ...
δ¹⁸O in ice wedges of yedoma deposits in Chukchi Peninsula and Late Pleistocene paleotemperatures, 38–12 Kyr BP.Winter mean (twint.mean) and January (tJ) air temperature means... -
δ¹⁸O in present growing syngenetic ice wedges in southern Chukchi Peninsula
Winter mean (twint.mean) and January (tJ) air temperature means for the Southern Chukchi Peninsula were inferred by comparing the oxygen isotope composition of present growing... -
δ²H in ice wedge, sand wedge, massive and pore ice at Rogozhny Cape, northern...
δ²H in ice wedge (IW), sand wedge (SIW), massive (MI) and pore (PI) ice at Rogozhny Cape, northern coast of Onemen Gulf, 25 km from Anadyr Town. -
δ¹⁸O, δ²H, deuterium excess and protease activity of Mikhail hill, vicinity o...
δ¹⁸O, δ²H, deuterium excess (dexc), and protease activity (PA) in snowpacks at different elevations of Mikhail hill, vicinity of Anadyr Town, Chukchi Peninsula -
δ¹⁸O in ice wedge and pore ice from vicinity of Anadyr Town
Major ions and dissolved salts in syngenetic ice wedges in the 25–30 m thick Late Pleistocene Ledovy Obryv yedoma and the 60-m thick Ust'-Algan Obryv yedoma. -
Major ions and dissolved salts in syngenetic ice wedges from Ledovy Obryv and...
Major ions and dissolved salts in syngenetic ice wedges in the 25–30 m thick Late Pleistocene Ledovy Obryv yedoma and the 60-m thick Ust'-Algan Obryv yedoma. Analysis of major... -
δ¹⁸O variations in ice wedge and pore ice from Ledovy Obryv and Ust'-Algan ou...
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Mean January air paleotemperatures and present values from different sites in...
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Spore and pollen from outcrop samples of the Plakhinskii Yar site (Kolyma River)
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Major ion chemistry of ice wedges from outcrop samples of the Plakhinskii Yar...
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Major ion chemistry of Late Pleistocene permafrost from outcrop samples of th...
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¹⁴C ages of particulate organic matter from outcrop samples of Plakhinskii Ya...
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¹⁴C ages from Late Pleistocene syngenetic permafrost outcrop samples of Plakh...
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δ¹⁸O variations in Late Pleistocene and Holocene ice wedges and in growing pr...
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(Table 3) Stable carbon isotope and radiocarbon composition of Lena Delta fir...
Soil profile samples are given in meters below surface (m b.s.).Before present (BP), i.e., before 1950.Samples were radiocarbon-dated at the National Ocean Sciences Accelerator... -
Particulate organic carbon composition, granulometric and geochemical data fo...
To study the transformation of organic carbon through long distance transport in rivers, we measured the composition of bulk organic carbon in river suspended sediment of the... -
Marine20 - the marine radiocarbon age calibration curve (0 - 55,000 cal BP), ...
The concentration of radiocarbon (14C) differs between ocean and atmosphere. Radiocarbon determinations from samples which obtained their 14C in the marine environment therefore...
