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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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Analysis of the late Pleistocene cyclic ice wedge complexes in the Mayn River...
We studied the structure and composition of Late Pleistocene cyclic ice wedge complexes in the Mayn River Valley and syngenetic ice wedges in adjacent areas of the Southern...
