2001/01/01 by Yurij K Vasil’chuk, Yurij K Vasil'chuk, Alla C Vasil'chuk +6 · 5 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Climate change and permafrost #Methane Hydrates and Related Phenomena
paper · pdf · doi:10.1017/s0033822200041199
The Duvanny Yar cross-section located in the Lower Kolyma River valley of Northern Yakutia (69°N, 158°E, height above the Kolyma River level 55 m), has been studied and dated in detail by radiocarbon. The sequence mainly consists of sandy loam sediments with large syngenetic ice wedges. Their width at the top is 1–3.5 m. Allochthonous organic material occurs in high content, concentrating as 0.5–0.7 m lenses. Shrub fragments, twigs, and mammoth bones are accumulated in peaty layers. Through interpolation based on a series of 14 C dates, dating of the host sediments provides an approximate age for the ice wedges. The 14 C dates of various types of organic material are sometimes very close, but not all in agreement. Therefore, the dates do not accurately show the age of the δ 18 O and δD plots. A new approach is developed to a 14 C dating strategy of syncryogenic sediments with high admixture of allochthonous organic material. The main purpose of this study is to consider detection of inversions or disturbances in the syngenetic permafrost sediment at the Duvanny Yar cross-section by 14 C date series. Direct accelerator mass spectrometry (AMS) dating of the ice confirmed the relatively young age of ice wedges.