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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>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-1089-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/1089/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/1089/2008/cpd-4-1089-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/1089/2008/cpd-4-1089-2008.pdf</fulltext_pdf>
	<start_page>1089</start_page>
	<end_page>1113</end_page>
	<publication_date>2008-10-01</publication_date>
	<article_title content_type="html">Two millennia of climate variability in the Central Mediterranean</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>C. Taricco</name>
			<email>taricco@ph.unito.it</email>
		</author>
		<author numeration="2" affiliations="3,4">
			<name>M. Ghil</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>G. Vivaldo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dipartimento di Fisica Generale, University of Torino, Torino, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Istituto di Fisica dello Spazio Interplanetario-INAF, University of Torino, Torino, Italy</affiliation>
		<affiliation numeration="3" content_type="html">Département Terre-Atmosphère-Océan &amp; Laboratoire de Météorologie Dynamique (CNRS and IPSL), Ecole Normale Supérieure, Paris, France</affiliation>
		<affiliation numeration="4" content_type="html">Department of Atmospheric and Oceanic Sciences, Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">This experimental work addresses the need for high-resolution, long and
homogeneous climatic time series that facilitate the study of climate
variability over time scales of decades to millennia. We present a
high-resolution record of foraminiferal &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O from a Central
Mediterranean sediment core that covers the last two millennia. The record
was analyzed using advanced spectral methods and shows highly significant
oscillatory components with periods of roughly 600, 350, 200, 125 and 11
years. Comparison with the spectra of composite temperature-proxy series over
the last millennium reveals that the &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O trend and 200-y
components are well correlated with the long-term Northern Hemisphere
temperature variations over the last millennium, showing a maximum at the
Medieval Optimum and a shallower local minimum at the Little Ice Age. In the
preceding millennium the same &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O components also reveal a deep
maximum (temperature minimum) at about 0 AD.</abstract>
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