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<article language="en">
	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/bg-5-1057-2008</doi>
	<article_url>http://www.biogeosciences.net/5/1057/2008/</article_url>
	<abstract_html>http://www.biogeosciences.net/5/1057/2008/bg-5-1057-2008.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/5/1057/2008/bg-5-1057-2008.pdf</fulltext_pdf>
	<start_page>1057</start_page>
	<end_page>1072</end_page>
	<publication_date>2008-07-28</publication_date>
	<article_title content_type="html">Modeling the marine aragonite cycle: changes under rising carbon dioxide and its role in shallow water CaCO&lt;sub&gt;3&lt;/sub&gt; dissolution</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>R. Gangstø</name>
			<email>gangsto@climate.unibe.ch</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Gehlen</name>
		</author>
		<author numeration="3" affiliations="1,5">
			<name>B. Schneider</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>L. Bopp</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>O. Aumont</name>
		</author>
		<author numeration="6" affiliations="2,4">
			<name>F. Joos</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">LSCE/IPSL, Laboratoire des Sciences du Climat et de l&apos;Environnement, CEA-CNRS-UVSQ, Orme des Merisiers, Bât. 712, CEA/Saclay, 91198 Gif-sur-Yvette Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstr. 5, 3012 Bern, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">LOCEAN/IPSL, Centre IRD de Bretagne, BP 70, 29280 Plouzané, France</affiliation>
		<affiliation numeration="4" content_type="html">Oeschger Centre for Climate Change Research, University of Bern, Erlachstrasse 9a, 3012 Bern, Switzerland</affiliation>
		<affiliation numeration="5" content_type="html">now at: Institute of Geosciences, University of Kiel, Luedwig-Meyn-Str. 10, 24098 Kiel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The marine aragonite cycle has been included in the global biogeochemical
model PISCES to study the role of aragonite in shallow water CaCO&lt;sub&gt;3&lt;/sub&gt;
dissolution. Aragonite production is parameterized as a function of
mesozooplankton biomass and aragonite saturation state of ambient waters.
Observation-based estimates of marine carbonate production and dissolution
are well reproduced by the model and about 60% of the combined CaCO&lt;sub&gt;3&lt;/sub&gt;
water column dissolution from aragonite and calcite is simulated above 2000
m. In contrast, a calcite-only version yields a much smaller fraction. This
suggests that the aragonite cycle should be included in models for a
realistic representation of CaCO&lt;sub&gt;3&lt;/sub&gt; dissolution and alkalinity. For the
SRES A2 CO&lt;sub&gt;2&lt;/sub&gt; scenario, production rates of aragonite are projected to
notably decrease after 2050. By the end of this century, global aragonite
production is reduced by 29% and total CaCO&lt;sub&gt;3&lt;/sub&gt; production by 19%
relative to pre-industrial. Geographically, the effect from increasing
atmospheric CO&lt;sub&gt;2&lt;/sub&gt;, and the subsequent reduction in saturation state, is
largest in the subpolar and polar areas where the modeled aragonite
production is projected to decrease by 65% until 2100.</abstract>
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</article>

