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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>7</volume_number>
		<issue_number>8</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bg-7-2327-2010</doi>
	<article_url>http://www.biogeosciences.net/7/2327/2010/</article_url>
	<abstract_html>http://www.biogeosciences.net/7/2327/2010/bg-7-2327-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/7/2327/2010/bg-7-2327-2010.pdf</fulltext_pdf>
	<start_page>2327</start_page>
	<end_page>2337</end_page>
	<publication_date>2010-08-06</publication_date>
	<article_title content_type="html">Heterotrophic denitrification vs. autotrophic anammox – quantifying collateral effects on the oceanic carbon cycle</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. Koeve</name>
			<email>wkoeve@ifm-geomar.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. Kähler</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">IFM-GEOMAR, Leibniz-Institut für Meereskunde, Düsternbrooker Weg 20, 24105 Kiel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The conversion of fixed nitrogen to N&lt;sub&gt;2&lt;/sub&gt; in suboxic waters is estimated
to contribute roughly a third to total oceanic losses of fixed nitrogen
and is hence
understood to be of major importance to global oceanic production and,
therefore, to the role of the ocean as a sink of atmospheric CO&lt;sub&gt;2&lt;/sub&gt;. At
present heterotrophic denitrification and autotrophic anammox are considered
the dominant sinks of fixed nitrogen. Recently, it has been suggested that
the trophic nature of pelagic N&lt;sub&gt;2&lt;/sub&gt;-production may have additional,
&quot;collateral&quot; effects on the carbon cycle, where heterotrophic
denitrification provides a shallow source of CO&lt;sub&gt;2&lt;/sub&gt; and autotrophic
anammox a shallow sink. Here, we analyse the stoichiometries of nitrogen and
associated carbon conversions in marine oxygen minimum zones (OMZ) focusing
on heterotrophic denitrification, autotrophic anammox, and dissimilatory
nitrate reduction to nitrite and ammonium in order to test this hypothesis
quantitatively. For open ocean OMZs the combined effects of these processes
turn out to be clearly heterotrophic, even with high shares of the
autotrophic anammox reaction in total N&lt;sub&gt;2&lt;/sub&gt;-production and including
various combinations of dissimilatory processes which provide the substrates
to anammox. In such systems, the degree of heterotrophy
(ΔCO&lt;sub&gt;2&lt;/sub&gt;:ΔN&lt;sub&gt;2&lt;/sub&gt;),
varying between 1.7 and 6.5, is a function of the
efficiency of nitrogen conversion. On the contrary, in systems like the
Black Sea, where suboxic N-conversions are supported by diffusive fluxes of
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; originating from neighbouring waters with sulphate reduction,
much lower values of ΔCO&lt;sub&gt;2&lt;/sub&gt;:ΔN&lt;sub&gt;2&lt;/sub&gt; can be found.
However, accounting for concomitant diffusive fluxes of CO&lt;sub&gt;2&lt;/sub&gt;, the ratio
approaches higher values similar to those computed for open ocean OMZs. Based on
this analysis, we question the significance of collateral effects concerning
the trophic nature of suboxic N-conversions on the marine carbon cycle.</abstract>
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