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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-5-891-2008</doi>
	<article_url>http://www.biogeosciences.net/5/891/2008/</article_url>
	<abstract_html>http://www.biogeosciences.net/5/891/2008/bg-5-891-2008.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/5/891/2008/bg-5-891-2008.pdf</fulltext_pdf>
	<start_page>891</start_page>
	<end_page>911</end_page>
	<publication_date>2008-06-02</publication_date>
	<article_title content_type="html">Predicting the global distribution of planktonic foraminifera using a dynamic ecosystem model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. Fraile</name>
			<email>igaratza@palmod.uni-bremen.de</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Schulz</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>S. Mulitza</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>M. Kucera</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Faculty of Geosciences, University of Bremen, P.O. Box 330440, 28334 Bremen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">MARUM &amp;ndash; Center For Marine Environmental Sciences, University of Bremen, P.O. Box 330440, 28334 Bremen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Geosciences, Eberhard Karls University of Tübingen, Sigwartstrasse 10, 72076 Tübingen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">We present a new planktonic foraminifera model developed for the global ocean mixed-layer. The main purpose of the model is to explore the response
of planktonic foraminifera to different boundary conditions in the geological past, and to quantify
the seasonal bias in foraminifera-based paleoceanographic proxy records.
This model is forced with hydrographic data and with
biological information taken from an ecosystem model to predict monthly concentrations of the most common
planktonic foraminifera species used in paleoceanography: &lt;i&gt;N. pachyderma&lt;/i&gt;
(sinistral and dextral varieties), &lt;i&gt;G. bulloides, G. ruber&lt;/i&gt;
(white variety) and &lt;i&gt;G. sacculifer&lt;/i&gt;. The sensitivity of each species
with respect to temperature (optimal temperature and range of tolerance) is
derived from previous sediment-trap studies.

&lt;br&gt;&lt;br&gt;
Overall, the spatial distribution patterns of most of the species are
in agreement with core-top data. &lt;i&gt;N. pachyderma&lt;/i&gt; (sin.) is limited to
polar regions, &lt;i&gt;N. pachyderma&lt;/i&gt; (dex.) and &lt;i&gt;G. bulloides&lt;/i&gt; are
the most common species in high productivity zones,
while &lt;i&gt;G. ruber&lt;/i&gt; and &lt;i&gt;G. sacculifer&lt;/i&gt; are more abundant in
tropical and subtropical oligotrophic waters. For
&lt;i&gt;N. pachyderma&lt;/i&gt; (sin) and &lt;i&gt;N. pachyderma&lt;/i&gt; (dex.),
the season of maximum production coincides with that observed in sediment-trap records.
Model and sediment-trap data for &lt;i&gt;G. ruber&lt;/i&gt; and &lt;i&gt;G. sacculifer&lt;/i&gt; show, in
general, lower concentrations and less seasonal variability at all sites. A sensitivity experiment suggest that,
within the temperature-tolerance range of a species, food availability may be the main
parameter controlling its abundance.</abstract>
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</article>

