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- W635091545 abstract "The El’gygytgyn Meteorite Crater in Chukotka holds the unique chance to trace frozen ground conditions back to the Pliocene. The basin was not glaciated in Quaternary time and terrestrial deposits accumulated on the slopes and continuously in a central lake basin. Drilling into sedimentary permafrost at the shore of the El’gygytgyn Crater Lake recovered a 141 m long core of frozen coarse-grained deposits, which belong to an alluvial fan setting entering the central lake basin from the west. The retrieved permafrost core contains ground ice throughout and largely consists of sandy gravels with volcanic clasts embedded in a sandy matrix. Pollen assemblages, ground ice hydrochemistry (i.e. stable water isotopes, major ions) and mineralogical proxies of cryogenic weathering are used as paleoenvironmental indicators for reconstructing late Cenozoic climate, landscape and permafrost dynamics. This aids understanding permafrost history on longer time scales in NE Siberia, an area yet underexposed in permafrost research." @default.
- W635091545 created "2016-06-24" @default.
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- W635091545 date "2011-01-01" @default.
- W635091545 modified "2023-09-27" @default.
- W635091545 title "Sediment move into the 3.6 Mya old Elgygytgyn Crater Lake, NE Russian Arctic, as recorded by frozen alluvial fan deposits" @default.
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