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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>3</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-1235-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/1235/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/1235/2007/cpd-3-1235-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/1235/2007/cpd-3-1235-2007.pdf</fulltext_pdf>
	<start_page>1235</start_page>
	<end_page>1260</end_page>
	<publication_date>2007-11-08</publication_date>
	<article_title content_type="html">A 60 000 year Greenland stratigraphic ice core chronology</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. K. Andersen</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Bigler</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. B. Clausen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. Dahl-Jensen</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>S. J. Johnsen</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>S. O. Rasmussen</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>I. Seierstad</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>J. P. Steffensen</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>A. Svensson</name>
		</author>
		<author numeration="10" affiliations="1,6">
			<name>B. M. Vinther</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>S. M. Davies</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>R. Muscheler</name>
		</author>
		<author numeration="13" affiliations="4">
			<name>F. Parrenin</name>
		</author>
		<author numeration="14" affiliations="5">
			<name>R. Röthlisberger</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen, Denmark</affiliation>
		<affiliation numeration="2" content_type="html">Depart. of Geography, Univ. of Wales Swansea, Singleton Park, Swansea, SA2 8PP, UK</affiliation>
		<affiliation numeration="3" content_type="html">GeoBiosphere Science Centre, Quaternary Sciences, Lund University, Sölvegatan 12, 22362 Lund, Sweden</affiliation>
		<affiliation numeration="4" content_type="html">Laboratoire de Glaciologie et Géophysique de l&apos;Environnement, CNRS and Joseph Fourier University, Grenoble, France</affiliation>
		<affiliation numeration="5" content_type="html">British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK</affiliation>
		<affiliation numeration="6" content_type="html">Climate Research Unit, School of Environmental Sciences, Univ. of East Anglia, NR47TJ, Norwich, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on
annual layer counting of high-resolution records from Greenland ice cores.
Whereas the Holocene part of the time scale is based on various records from
the DYE-3, the GRIP, and the NorthGRIP ice cores, the glacial part is solely
based on NorthGRIP records. Here we present an 18 kyr extension of the time
scale such that GICC05 continuously covers the past 60 kyr. The new section
of the time scale places the onset of Greenland Interstadial 12 (GI-12) at
46.9&amp;plusmn;1.0 kyr b2k (before year AD 2000), the North Atlantic Ash Zone 2
layer in GI-15 at 55.4&amp;plusmn;1.2 kyr b2k, and the onset of GI-17 at 59.4&amp;plusmn;1.3 kyr b2k.
The error estimates are derived from the accumulated
number of uncertain annual layers and can be regarded as 1&amp;sigma;
uncertainties. In the 40&amp;ndash;60 kyr interval the new time scale has a
discrepancy with the Meese-Sowers GISP2 time scale of up to 2.4 kyr, whereas
GICC05 compares well to the dating of the Hulu Cave record with absolute age
differences of less than 800 years throughout the 60 kyr period. The new
time scale is generally in close agreement with other independently dated
records and reference horizons, such as the Laschamp geomagnetic excursion
and the Kleegruben speleothem record from the Austrian Alps, suggesting high
accuracy of both event durations and absolute age estimates.</abstract>
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</article>

