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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>4</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/bg-4-63-2007</doi>
	<article_url>http://www.biogeosciences.net/4/63/2007/</article_url>
	<abstract_html>http://www.biogeosciences.net/4/63/2007/bg-4-63-2007.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/4/63/2007/bg-4-63-2007.pdf</fulltext_pdf>
	<start_page>63</start_page>
	<end_page>73</end_page>
	<publication_date>2007-01-18</publication_date>
	<article_title content_type="html">The significance of nitrogen fixation to new production during early summer in the Baltic Sea</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>U. Ohlendieck</name>
			<email>ute.ohlendieck@t-online.de</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>K. Gundersen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Meyerhöfer</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. Fritsche</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>K. Nachtigall</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>B. Bergmann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz Institut für Meereswissenschaften, Düsternbrooker Weg 20, 24105 Kiel, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Department of Botany, Stockholm University, Lilla Frescativägen 5, 10691 Stockholm, Sweden</affiliation>
		<affiliation numeration="3" content_type="html">now at: Department of Marine Sience, University of Southern Mississippi, 1020 Balch Blvd., Stennis Space Center, MS 39529, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Rates of dinitrogen (N&lt;sub&gt;2&lt;/sub&gt;) fixation and primary production were measured
during two 9 day transect cruises in the Baltic proper in June&amp;ndash;July of 1998
and 1999. Assuming that the early phase of the bloom of cyanobacteria lasted
a month, total rates of N&lt;sub&gt;2&lt;/sub&gt; fixation contributed 15 mmol N m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;
(1998) and 33 mmol N m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (1999) to new production (sensu Dugdale and
Goering, 1967). This constitutes 12&amp;ndash;26% more new N than other annual
estimates (mid July&amp;ndash;mid October) from the same region. The between-station
variability observed in both total N&lt;sub&gt;2&lt;/sub&gt; fixation and primary productivity
greatly emphasizes the need for multiple stations and seasonal sampling
strategies in biogeochemical studies of the Baltic Sea. The majority of new N
from N&lt;sub&gt;2&lt;/sub&gt; fixation was contributed by filamentous cyanobacteria. On
average, cyanobacterial cells &amp;gt;20 &amp;micro;m were able to supply a major part
of their N requirements for growth by N&lt;sub&gt;2&lt;/sub&gt; fixation in both 1998 (73%)
and 1999 (81%). The between-station variability was high however,
and ranged from 28&amp;ndash;150% of N needed to meet the rate of C incorporation
by primary production. The molar C:N rate incorporation ratio
(C:N&lt;sub&gt;RATE&lt;/sub&gt;) in filamentous cyanobacterial cells was variable (range 7&amp;ndash;28) and the average almost twice as high
as the Redfield ratio (6.6) in both years. Since
the molar C:N mass ratio (C:N&lt;sub&gt;MASS&lt;/sub&gt;) in filamentous cyanobacterial cells
was generally lower than C:N&lt;sub&gt;RATE&lt;/sub&gt; at a number of stations, we suggest that
the diazotrophs incorporated excess C on a short term basis (carbohydrate ballasting
and buoyancy regulation), released nitrogen or utilized other
regenerated sources of N nutrients. Measured rates of total N&lt;sub&gt;2&lt;/sub&gt; fixation
contributed only a minor fraction of 13% (range 4&amp;ndash;24) in 1998 and 18%
(range 2&amp;ndash;45) in 1999 to the amount of N needed for the community
primary production. An average of 9 and 15% of total N&lt;sub&gt;2&lt;/sub&gt; fixation
was found in cells &amp;lt;5 &amp;micro;m. Since cells &amp;lt;5 &amp;micro;m did not show any
detectable rates of N&lt;sub&gt;2&lt;/sub&gt; fixation, the &lt;sup&gt;15&lt;/sup&gt;N-enrichment could be
attributed to regenerated incorporation of dissolved organic N (DON) and
ammonium generated from larger diazotroph cyanobacteria. Therefore, N
excretion from filamentous cyanobacteria may significantly contribute to the
pool of regenerated nutrients used by the non-diazotroph community in
summer. Higher average concentrations of regenerated N (ammonium) coincided
with higher rates of N&lt;sub&gt;2&lt;/sub&gt; fixation found during the 1999 transect and a
higher level of &lt;sup&gt;15&lt;/sup&gt;N-enrichment in cells &amp;lt;5 &amp;micro;m. A variable but
significant fraction of total N&lt;sub&gt;2&lt;/sub&gt; fixation (1&amp;ndash;10%) could be
attributed to diazotrophy in cells between 5&amp;ndash;20 &amp;micro;m.</abstract>
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</article>

