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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>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-791-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/791/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/791/2008/cpd-4-791-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/791/2008/cpd-4-791-2008.pdf</fulltext_pdf>
	<start_page>791</start_page>
	<end_page>807</end_page>
	<publication_date>2008-06-25</publication_date>
	<article_title content_type="html">Revisiting the absolute calibration of the Greenland ice-core age-scales</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Skinner</name>
			<email>luke00@esc.cam.ac.uk</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Recently, an absolute &quot;calibration&quot; was proposed for the GRIP and GISP2
Greenland ice-core time scales (Shackleton et al., 2004). This calibration attempted to reconcile the stratigraphic
integration of ice-core, marine and speleothem archives with the absolute
age constraints that marine and speleothem records incorporate. Here we
revisit this calibration in light of the new layer-counted chronology of the
NGRIP ice-core (GICC05). The GICC05 age-scale differs from the proposed
absolute calibration by up to 1200 years late in the last glaciation, with
implications both for radiocarbon cycling and the inferred timing of North
Atlantic climate events relative to absolutely dated archives (e.g. relative
sea-level). By precisely aligning the stratigraphy of Iberian Margin marine
cores with that of the Greenland ice-cores, it appears that either: 1) the
radiocarbon content of mid-latitude Atlantic surface-waters was extremely
depleted (resulting in average surface reservoir ages up to 1700 years
prior to ~22 ka BP); or 2) the GICC05 age-scale includes too few
years (is up to 1200 years too young). It is shown here that both of these
possibilities are in fact correct to some degree. Northeast Atlantic surface
reservoir ages should be revised upward by ~350 years, while the
NGRIP age-scale appears to be &quot;missing&quot; time. These findings illustrate the
importance of integrated stratigraphy as a test for our chronologies, which
are rarely truly &quot;absolute&quot;. This is an important point, since probably the
worst error that we can make is to entrench and generalise a precise
stratigraphical relationship on the basis of erroneous absolute age
assignations.</abstract>
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</article>

