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<article language="en">
	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cp-6-19-2010</doi>
	<article_url>http://www.clim-past.net/6/19/2010/</article_url>
	<abstract_html>http://www.clim-past.net/6/19/2010/cp-6-19-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/6/19/2010/cp-6-19-2010.pdf</fulltext_pdf>
	<start_page>19</start_page>
	<end_page>29</end_page>
	<publication_date>2010-01-19</publication_date>
	<article_title content_type="html">Sea level ~400 000 years ago (MIS 11): analogue for present and future sea-level?</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Q. Bowen</name>
			<email>bowendq@cardiff.ac.uk</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3YE, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Comparison of the sea-level today with that of 400 000 years ago
(MIS 11), when the Earth&apos;s orbital characteristics were similar may
provide, under conditions of natural variability, indications of
future sea-level during the present interglacial. Then, as now,
orbital eccentricity was low and precession dampened. Evidence for
MIS 11 sea-level occurs on uplifting coastlines where shorelines
with geochronological ages have been preserved. The sea-level term
and the uplift term may be separated with an &quot;uplift correction&quot;
formula. This discovers the original sea-level at which the now
uplifted shoreline was fashioned. Estimates are based on average
uplift rates of the &quot;last interglacial&quot; sea-level (MIS 5.5) using
a range of estimates for sea-level and age at that time at different
locations. These, with varying secular tectonic regimes in different
ocean basins, provide a band of estimates for the MIS 11 sea-level.
They do not support the hypothesis of an MIS 11 sea-level at
~20 m, and instead show that it was closer to its present
level.</abstract>
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</article>

