2006
DOI: 10.1080/03009480600690886
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Holocene environmental history on the eastern slope of the Polar Ural Mountains, Russia

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Cited by 7 publications
(10 citation statements)
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“…The reconstructed forest tundra/boreal woodland vegetation is indicated by the presence of Larix pollen in low but significant proportions (0.5-3%). This interpretation is supported by studies on surface pollen representation across the Russian Arctic (e.g., Jankovská et al, 2006) indicating strong underrepresentation of Larix pollen compared to its occurrence on the landscape. The presence of Larix treesa taxon that was, and still is, confined to Kamchatka's more continental interior (Dirksen et al, 2013) -suggests that the climate of Kamchatka's eastern seaboard at this time was more continental than during the Holocene.…”
Section: Cal Yr Bp)mentioning
confidence: 69%
“…The reconstructed forest tundra/boreal woodland vegetation is indicated by the presence of Larix pollen in low but significant proportions (0.5-3%). This interpretation is supported by studies on surface pollen representation across the Russian Arctic (e.g., Jankovská et al, 2006) indicating strong underrepresentation of Larix pollen compared to its occurrence on the landscape. The presence of Larix treesa taxon that was, and still is, confined to Kamchatka's more continental interior (Dirksen et al, 2013) -suggests that the climate of Kamchatka's eastern seaboard at this time was more continental than during the Holocene.…”
Section: Cal Yr Bp)mentioning
confidence: 69%
“…Larch and birch began to penetrate the Polar Urals and northern parts of western Siberia at c . 9800 yr BP (Andreev et al 2001; Forman et al 2002; Jankovská et al 2006). Peat accumulation in the arctic region of West Siberia started at c .…”
Section: Resultsmentioning
confidence: 99%
“…This was a time of transition from open dry tundra-steppe landscapes to the emergence of foresttundra and peat bogs. Larch and birch began to penetrate the Polar Urals and northern parts of western Siberia at c. 9800 yr BP (Andreev et al 2001;Forman et al 2002;Jankovsk´a et al 2006). Peat accumulation in the arctic region of West Siberia started at c. 11 600-10 700 yr BP, while it intensified in the early Holocene, c. 9500 yr BP (Peteet et al 1998: p. 122).…”
Section: Environmental Situation At the Time Of Mammoth Extinction Inmentioning
confidence: 99%
“…Àíàëèç ëèòåðàòóðû ïî ïàëèíîëîãèè ïîçâîëÿåò ïîäâåðãíóòü ñîìíåíèþ ðåëèêòîâóþ ïðèðîäó ñîâðåìåííûõ ìåñòîíàõîaeäåíèé L. inundata íà Åâðîïåéñêîì Ñåâåðå è ñ÷èòàòü ýòîò âèä àëëîõòîííûì ýëåìåíòîì ôëîðû.  ïîëüçó ýòîãî ãîâîðÿò è íàøè ìíîãîëåòíèå èññëåäîâàíèÿ ñïîðîâî-ïûëüöåâûõ ñïåêòðîâ ïîçäíåëåäíèêîâüÿ è ãîëîöåíà, ïðîâåäåííûå â ëàáîðàòîðèè ãåîëîãèè êàéíîçîÿ Èíñòèòóòà ãåîëîãèè Êîìè ÍÖ ÓðÎ ÐÀÍ [1,6,8]. Ïî÷òè âî âñåõ ôîññèëüíûõ ïàëèíîñïåêòðàõ ñïîðû ýòîãî âèäà îáíàðóaeåíû íå áûëè, çà èñêëþ÷åíèåì ðàçðåçà ×åðíàÿ Ãîðêà íà Ïîëÿðíîì Óðàëå [26].…”
Section: çàêëþ÷åíèåunclassified
“… ïîëüçó ýòîãî ãîâîðÿò è íàøè ìíîãîëåòíèå èññëåäîâàíèÿ ñïîðîâî-ïûëüöåâûõ ñïåêòðîâ ïîçäíåëåäíèêîâüÿ è ãîëîöåíà, ïðîâåäåííûå â ëàáîðàòîðèè ãåîëîãèè êàéíîçîÿ Èíñòèòóòà ãåîëîãèè Êîìè ÍÖ ÓðÎ ÐÀÍ [1,6,8]. Ïî÷òè âî âñåõ ôîññèëüíûõ ïàëèíîñïåêòðàõ ñïîðû ýòîãî âèäà îáíàðóaeåíû íå áûëè, çà èñêëþ÷åíèåì ðàçðåçà ×åðíàÿ Ãîðêà íà Ïîëÿðíîì Óðàëå [26]. Çäåñü, âåðîÿòíî, íà ñêëîíàõ þaeíûõ ýêñïîçèöèé îí ïðèñóòñòâóåò â êà÷åñòâå ðåëèêòà.…”
Section: çàêëþ÷åíèåunclassified