Казанский (Приволжский) федеральный университет, КФУ
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HOLOCENE ICE-WEDGE POLYGON DEVELOPMENT IN NORTHERN YUKON PERMAFROST PEATLANDS (CANADA)
Форма представленияСтатьи в зарубежных журналах и сборниках
Год публикации2016
Языканглийский
  • Назарова Лариса Борисовна, автор
  • Палагушкина Ольга Викторовна, автор
  • Fritz Michael , автор
  • Библиографическое описание на языке оригинала Michael Fritz, Juliane Wolter, Natalia Rudaya, Olga Palagushkina, Lari-sa Nazarova, Jaroslav Obu, Janet Rethemeyer, Hugues Lantuit, Sebastian Wetterich Holocene ice-wedge polygon development in northern Yukon per-mafrost peatlands (Canada) Quaternary Science Reviews, Special Issue: PAST Gateways (Palaeo-Arctic Spatial and Temporal Gateways) Volume 147, 1 September 2016, Pages 279–297.- база данных Scopus и Web of Science
    Аннотация Ice-wedge polygon (IWP) mires in the Arctic and Subarctic are extremely vulnerable to climatic and environmental change. We present the results of a multidisciplinary paleoenvironmental study on IWPs in the northern Yukon, Canada. High-resolution laboratory analyses were carried out on a permafrost core and the overlying seasonally thawed (active) layer, from a low-centered IWP located in a drained lake basin on Herschel Island. In relation to 14 Accelerator Mass Spectrometry (AMS) radiocarbon dates spanning the last 5000 years, we report sedimentary data including grain size distribution and biogeochemical parameters (organic carbon, nitrogen, C/N ratio, δ13C), stable water isotopes (δ18O, δD), as well as fossil pollen, plant macrofossil and diatom assemblages. Three sediment units (SUs) correspond to the main stages of deposition (1) in a thermokarst lake (SU1: 4950 to 3950 cal yrs BP), (2) during transition from lacustrine to palustrine conditions after lake drainage (SU2: 3950 to 3
    Ключевые слова Permafrost peatland, arctic, thermokarst, talik, ice-wedge polygon, pollen, diatoms, plant macrofossils, stable water isotopes, deuterium excess
    Название журнала QUATERNARY SCI REV
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