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<article language="en">
	<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>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-671-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/671/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/671/2009/cpd-5-671-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/671/2009/cpd-5-671-2009.pdf</fulltext_pdf>
	<start_page>671</start_page>
	<end_page>707</end_page>
	<publication_date>2009-02-24</publication_date>
	<article_title content_type="html">Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>N. Combourieu Nebout</name>
			<email>nathalie.nebout@lsce.ipsl.fr</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>O. Peyron</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>I. Dormoy</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement, UMR 1572 CNRS/CEA/UVSQ, 91198 Gif sur Yvette Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">Laboratoire de Chrono-Environnement, UMR 6249 CNRS, Université de Franche-Comté, UFR des Sciences et Techniques, 16 Route de Gray, 25030 Besançon, France</affiliation>
	</affiliations>
	<abstract content_type="html">High-temporal resolution pollen record of Alboran Sea ODP Site 976 and pollen-based
      quantitative climate reconstruction shows that changes of Mediterranean vegetation have been
      clearly modulated by short and long term variability during the last 25 000
      years. The western Mediterranean vegetation response appears nearly
      synchronous with North Atlantic variability during the last deglaciation as well as during
      the Holocene. High-resolution analyses of the ODP 976 pollen record allows to separate the
      Bölling/Alleröd period
      in two warm episodes that surround a cooling representative of the climatic succession of
      the Bölling, Older Dryas and Alleröd. A cooling trend is observed from Bölling to
      Alleröd. The ODP pollen record confirms that Mediterranean environments show rapid
      responses to the climatic fluctuations during the last termination, in particular that of
      all the climate oscillations associated with the successive steps of the deglaciation in the
      North Atlantic have been observed in the west Mediterranean region. Recurrent Holocene
      declines of the forest cover on the Alboran Sea borderlands indicate repetitive climate
      events that correlate well with several events of increased Mediterranean dryness observed
      on the continent and with alkenone SST showing Mediterranean Sea cooling. These events
      reflect clearly the response of to Mediterranean vegetation to North Atlantic Holocene cold
      events.</abstract>
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</article>

