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	<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>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/bg-5-707-2008</doi>
	<article_url>http://www.biogeosciences.net/5/707/2008/</article_url>
	<abstract_html>http://www.biogeosciences.net/5/707/2008/bg-5-707-2008.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/5/707/2008/bg-5-707-2008.pdf</fulltext_pdf>
	<start_page>707</start_page>
	<end_page>718</end_page>
	<publication_date>2008-05-06</publication_date>
	<article_title content_type="html">Build-up and decline of organic matter during PeECE III</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. G. Schulz</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>U. Riebesell</name>
		</author>
		<author numeration="3" affiliations="2,3">
			<name>R. G. J. Bellerby</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H. Biswas</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. MeyerhÃ¶fer</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. N. MÃ¼ller</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>J. K. Egge</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>J. C. Nejstgaard</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>C. Neill</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>J. Wohlers</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>E. ZÃ¶llner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz Institute for Marine Sciences (IFM-GEOMAR), DÃ¼sternbrooker Weg 20, 24105 Kiel, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Bjerknes Centre for Climate Research, University of Bergen, AllÃ©gaten 55, 5007 Bergen, Norway</affiliation>
		<affiliation numeration="3" content_type="html">Geophysical Institute, University of Bergen, AllÃ©gaten 70, 5007 Bergen, Norway</affiliation>
		<affiliation numeration="4" content_type="html">University of Bergen, Department of Biology, Box 7800, 5020 Bergen, Norway</affiliation>
	</affiliations>
	<abstract content_type="html">Increasing atmospheric carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) concentrations due to
anthropogenic fossil fuel combustion are currently changing the ocean&apos;s
chemistry. Increasing oceanic [CO&lt;sub&gt;2&lt;/sub&gt;] and consequently
decreasing seawater pH have the potential to significantly impact
marine life. Here we describe and analyze the build-up and decline of a
natural phytoplankton bloom initiated during the 2005 mesocosm
Pelagic Ecosystem CO&lt;sub&gt;2&lt;/sub&gt; Enrichment study (PeECE III). The draw-down
of inorganic  nutrients in the upper surface layer of the mesocosms was
reflected by a concomitant increase of organic matter until day
&lt;i&gt;t&lt;/i&gt;&lt;sub&gt;11&lt;/sub&gt;, the peak of the bloom. From then on, biomass standing stocks
steadily decreased as more and more particulate organic matter was
lost into the deeper layer of the mesocosms. We show that organic
carbon export to the deeper layer was significantly enhanced at
elevated CO&lt;sub&gt;2&lt;/sub&gt;. This phenomenon might have impacted organic matter
remineralization leading to decreased oxygen concentrations in the
deeper layer of the high CO&lt;sub&gt;2&lt;/sub&gt; mesocosms as indicated by
deep water ammonium concentrations. This would have
important implications for our understanding of pelagic ecosystem
functioning and  future carbon cycling.</abstract>
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</article>

