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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>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/bg-5-43-2008</doi>
	<article_url>http://www.biogeosciences.net/5/43/2008/</article_url>
	<abstract_html>http://www.biogeosciences.net/5/43/2008/bg-5-43-2008.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/5/43/2008/bg-5-43-2008.pdf</fulltext_pdf>
	<start_page>43</start_page>
	<end_page>53</end_page>
	<publication_date>2008-01-24</publication_date>
	<article_title content_type="html">Short-term fate of phytodetritus in sediments across the Arabian Sea Oxygen Minimum Zone</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>J. H. Andersson</name>
			<email>han@dmi.dk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>C. Woulds</name>
		</author>
		<author numeration="3" affiliations="2,5">
			<name>M. Schwartz</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>G. L. Cowie</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>L. A. Levin</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>K. Soetaert</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>J. J. Middelburg</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Netherlands Institute of Ecology (NIOO-KNAW), Centre for Estuarine and Marine Ecology, POB 140, 4400 AC Yerseke, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">University of Edinburgh, School of Geosciences, West Mains Road, EH9 3JW, Scotland</affiliation>
		<affiliation numeration="3" content_type="html">Integrative Oceanography Division, Scripps Institution of Oceanography, La Jolla, CA 92093-0218, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark</affiliation>
		<affiliation numeration="5" content_type="html">now at: University of West Florida, 11000 University Parkway, Pensacola, FL 32514, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The short-term fate of phytodetritus was investigated across the
  Pakistan margin of the Arabian Sea at water depths ranging from 140
  to 1850 m, encompassing the oxygen minimum zone
  (~100&amp;ndash;1100 m). Phytodetritus sedimentation events were
  simulated by adding ~44 mmol &lt;sup&gt;13&lt;/sup&gt;C-labelled algal material
  per m&lt;sup&gt;2&lt;/sup&gt; to surface sediments in retrieved cores. Cores were
  incubated in the dark, at in situ temperature and oxygen concentrations.
  Overlying waters were sampled periodically, and cores were recovered
  and sampled (for organisms and sediments) after durations of two and
  five days. The labelled carbon was subsequently traced into
  bacterial lipids, foraminiferan and macrofaunal biomass, and
  dissolved organic and inorganic pools.  The majority of the label
  (20 to 100%) was in most cases left unprocessed in the sediment at
  the surface. The largest pool of processed carbon was found to be
  respiration (0 to 25% of added carbon), recovered as dissolved
  inorganic carbon. Both temperature and oxygen were found to
  influence the rate of respiration.  Macrofaunal influence was most
  pronounced at the lower part of the oxygen minimum zone where it
  contributed 11% to the processing of phytodetritus.</abstract>
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</article>

