Инд. авторы:	Fedotov A.P., Phedorin M.A., Suvorov A.S., Melgunov M.S., Khodzher T.V.
Заглавие:	Permafrost thawing inferred from Arctic lake sediment of the Taimyr Peninsula, East Siberia, Russia
Библ. ссылка:	Fedotov A.P., Phedorin M.A., Suvorov A.S., Melgunov M.S., Khodzher T.V. Permafrost thawing inferred from Arctic lake sediment of the Taimyr Peninsula, East Siberia, Russia // International Journal of Environmental Studies. - 2012. - Vol.69. - Iss. 1. - P.7-19. - ISSN 0020-7233. - EISSN 1029-0400.
Внешние системы:	DOI: 10.1080/00207233.2012.619879; SCOPUS: 2-s2.0-84857949472;
Реферат:	eng: The objective of this paper is to reconstruct permafrost thawing at 71°N of Arctic Siberia during the termination of the Little Ice Age and the subsequent Recent Warming. Sediment samples from Lake Dalgan of the Taimyr Peninsula were analysed by high-resolution X-ray fluorescence spectroscopy at 1 mm scan resolution, and Fourier-transform infrared techniques. Intense permafrost thawing was calculated from the level of terrigenous and leached matter supplied by meltwater into the lakes. We defined three episodes of increased permafrost thawing during the last 170 years. The first maximum of permafrost melting occurred from 1870 to 1880, the second episode was from 1900 to 1930 and the third began from 1960 and continues to date. During these periods, maxima of permafrost melting occurred with a specific time lag following temperature maxima. © 2012 Copyright Taylor and Francis Group, LLC.
Ключевые слова:	Thawing; Sedimentology; Phase transitions; Leaching; Lakes; Fourier transform infrared spectroscopy; Fluorescence spectroscopy; Anoxic sediments; XRF-SR scan; X ray fluorescence spectroscopy; Specific time; SIBERIA; Permafrost; Little Ice Age; Lake sediments; Infrared technique; High resolution; FTIR; East Siberia; Arctic Russia; XRF-SR scan; Permafrost thawing; FTIR; Arctic Russia; Sediment samples;
Издано:	2012
Физ. характеристика:	с.7-19