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	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>4</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-1237-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/1237/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/1237/2008/cpd-4-1237-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/1237/2008/cpd-4-1237-2008.pdf</fulltext_pdf>
	<start_page>1237</start_page>
	<end_page>1264</end_page>
	<publication_date>2008-11-26</publication_date>
	<article_title content_type="html">Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Müller</name>
			<email>stefanie.mueller@awi.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. E. Tarasov</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. A. Andreev</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>B. Diekmann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Freie Universität Berlin, Geological Sciences, Palaeontology Section, Berlin, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Alfred Wegener Institute for Polar and Marine Research, Research Unit Potsdam, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">In this study a radiocarbon-dated pollen record from Lake Billyakh
(65&amp;deg;17&apos;N, 126&amp;deg;47&apos;E; 340 m a.s.l.) in the Verkhoyansk
Mountains was used to reconstruct vegetation and climate change since about
15 kyr BP (1 kyr=1000 cal. yr). The pollen record and pollen-based biome
reconstruction suggest that open cool steppe and grass and sedge tundra
communities with Poaceae, Cyperaceae, &lt;i&gt;Artemisia&lt;/i&gt;, Chenopodiaceae,
Caryophyllaceae and &lt;i&gt;Selaginella rupestris&lt;/i&gt; dominated the area from 15
to 13.5 kyr BP. On the other hand, the constant presence of &lt;i&gt;Larix&lt;/i&gt;
pollen in quantities comparable to today&apos;s values points to the constant
presence of boreal deciduous conifer trees in the regional vegetation during
the last glaciation. A major spread of shrub tundra communities, including
birch (&lt;i&gt;Betula&lt;/i&gt; sect. &lt;i&gt;Nanae&lt;/i&gt;), alder (&lt;i&gt;Duschekia
fruticosa&lt;/i&gt;) and willow (&lt;i&gt;Salix&lt;/i&gt;) species, is dated to 13.5–12.7 kyr
BP, indicating a noticeable increase in precipitation toward the end of the
last glaciation, particularly during the Allerød Interstadial. Between
12.7 and 11.4 kyr BP pollen percentages of herbaceous taxa rapidly
increased, whereas shrub taxa percentages decreased, suggesting strengthening
of the steppe communities associated with the relatively cold and dry Younger
Dryas Stadial. However, the pollen data in hand indicate that Younger Dryas
climate was less severe than the climate during the earlier interval from 15
to 13.5 kyr BP. The onset of the Holocene is marked in the pollen record by
the highest values of shrub and lowest values of herbaceous taxa, suggesting
a return of warmer and wetter conditions after 11.4 kyr BP. Percentages of
tree taxa increase gradually and reach maximum values after 7 kyr BP,
reflecting the spread of boreal cold deciduous and taiga forests in the
region. An interval between 7 and 2 kyr BP is noticeable for the highest
percentages of Scots pine (&lt;i&gt;Pinus&lt;/i&gt; subgen. &lt;i&gt;Diploxylon&lt;/i&gt;),
spruce (&lt;i&gt;Picea&lt;/i&gt;) and fir (&lt;i&gt;Abies&lt;/i&gt;) pollen, indicating
mid-Holocene spread of boreal forest communities in response to climate
amelioration and degradation of the permafrost layer.</abstract>
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