Heading for New Shores: Projecting Marine Distribution Ranges of Selected Larger Foraminifera
Identifieur interne : 000084 ( Pmc/Checkpoint ); précédent : 000083; suivant : 000085Heading for New Shores: Projecting Marine Distribution Ranges of Selected Larger Foraminifera
Auteurs : Anna E. Weinmann [Allemagne] ; Dennis Rödder [Allemagne] ; Stefan Lötters [Allemagne] ; Martin R. Langer [Allemagne]Source :
- PLoS ONE [ 1932-6203 ] ; 2013.
Abstract
The distribution of modern symbiont-bearing larger foraminifera is confined to tropical and subtropical shallow water marine habitats and a narrow range of environmental variables (e.g. temperature). Most of today's taxa are restricted to tropical and subtropical regions (between 30°N and 30°S) and their minimum temperature limits are governed by the 14 to 20°C isotherms. However, during times of extensive global warming (e.g., the Eocene and Miocene), larger foraminifera have been found as far north as 50°N (North America and Central Europe) as well as towards 47°S in New Zealand. During the last century, sea surface temperatures have been rising significantly. This trend is expected to continue and climate change scenarios for 2050 suggest a further increase by 1 to 3°C. We applied Species Distribution Models to assess potential distribution range changes of three taxa of larger foraminifera under current and future climate. The studied foraminifera include
Url:
DOI: 10.1371/journal.pone.0062182
PubMed: 23620810
PubMed Central: 3631173
Affiliations:
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a" type="main">Heading for New Shores: Projecting Marine Distribution Ranges of Selected Larger Foraminifera</title>
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<front><div type="abstract" xml:lang="en"><p>The distribution of modern symbiont-bearing larger foraminifera is confined to tropical and subtropical shallow water marine habitats and a narrow range of environmental variables (e.g. temperature). Most of today's taxa are restricted to tropical and subtropical regions (between 30°N and 30°S) and their minimum temperature limits are governed by the 14 to 20°C isotherms. However, during times of extensive global warming (e.g., the Eocene and Miocene), larger foraminifera have been found as far north as 50°N (North America and Central Europe) as well as towards 47°S in New Zealand. During the last century, sea surface temperatures have been rising significantly. This trend is expected to continue and climate change scenarios for 2050 suggest a further increase by 1 to 3°C. We applied Species Distribution Models to assess potential distribution range changes of three taxa of larger foraminifera under current and future climate. The studied foraminifera include <italic>Archaias angulatus</italic>
, <italic>Calcarina</italic>
spp., and <italic>Amphistegina</italic>
spp., and represent taxa with regional, superregional and global distribution patterns. Under present environmental conditions, <italic>Amphistegina</italic>
spp. shows the largest potential distribution, apparently due to its temperature tolerance. Both <italic>Archaias angulatus</italic>
and <italic>Calcarina</italic>
spp. display potential distributions that cover currently uninhabited regions. Under climate conditions expected for the year 2050, all taxa should display latitudinal range expansions between 1 to 2.5 degrees both north- and southward. The modeled range projections suggest that some larger foraminifera may colonize biogeographic regions that so far seemed unsuitable. <italic>Archaias angulatus</italic>
and <italic>Calcarina</italic>
spp. also show an increase in habitat suitability within their native occurrence ranges, suggesting that their tolerance for maximum temperatures has yet not been fully exploited and that they benefit from ocean warming. Our findings suggest an increased role of larger foraminifera as carbonate producers and reef framework builders in future oceans.</p>
</div>
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<pmc article-type="research-article"><pmc-dir>properties open_access</pmc-dir>
<front><journal-meta><journal-id journal-id-type="nlm-ta">PLoS One</journal-id>
<journal-id journal-id-type="iso-abbrev">PLoS ONE</journal-id>
<journal-id journal-id-type="publisher-id">plos</journal-id>
<journal-id journal-id-type="pmc">plosone</journal-id>
<journal-title-group><journal-title>PLoS ONE</journal-title>
</journal-title-group>
<issn pub-type="epub">1932-6203</issn>
<publisher><publisher-name>Public Library of Science</publisher-name>
<publisher-loc>San Francisco, USA</publisher-loc>
</publisher>
</journal-meta>
<article-meta><article-id pub-id-type="pmid">23620810</article-id>
<article-id pub-id-type="pmc">3631173</article-id>
<article-id pub-id-type="publisher-id">PONE-D-12-21819</article-id>
<article-id pub-id-type="doi">10.1371/journal.pone.0062182</article-id>
<article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject>
</subj-group>
<subj-group subj-group-type="Discipline-v2"><subject>Biology</subject>
<subj-group><subject>Ecology</subject>
<subj-group><subject>Ecological Environments</subject>
<subj-group><subject>Marine Environments</subject>
</subj-group>
</subj-group>
<subj-group><subject>Ecosystems</subject>
<subj-group><subject>Ecosystem Modeling</subject>
</subj-group>
</subj-group>
<subj-group><subject>Marine Ecology</subject>
<subj-group><subject>Coral Reefs</subject>
</subj-group>
</subj-group>
<subj-group><subject>Global Change Ecology</subject>
</subj-group>
</subj-group>
<subj-group><subject>Paleontology</subject>
<subj-group><subject>Biogeography</subject>
<subject>Micropaleontology</subject>
</subj-group>
</subj-group>
</subj-group>
<subj-group subj-group-type="Discipline-v2"><subject>Earth Sciences</subject>
<subj-group><subject>Atmospheric Science</subject>
<subj-group><subject>Climatology</subject>
<subj-group><subject>Climate Modeling</subject>
</subj-group>
</subj-group>
</subj-group>
</subj-group>
</article-categories>
<title-group><article-title>Heading for New Shores: Projecting Marine Distribution Ranges of Selected Larger Foraminifera</article-title>
<alt-title alt-title-type="running-head">Distribution Ranges of Larger Foraminifera</alt-title>
</title-group>
<contrib-group><contrib contrib-type="author"><name><surname>Weinmann</surname>
<given-names>Anna E.</given-names>
</name>
<xref ref-type="aff" rid="aff1"><sup>1</sup>
</xref>
<xref ref-type="corresp" rid="cor1"><sup>*</sup>
</xref>
</contrib>
<contrib contrib-type="author"><name><surname>Rödder</surname>
<given-names>Dennis</given-names>
</name>
<xref ref-type="aff" rid="aff2"><sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author"><name><surname>Lötters</surname>
<given-names>Stefan</given-names>
</name>
<xref ref-type="aff" rid="aff3"><sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author"><name><surname>Langer</surname>
<given-names>Martin R.</given-names>
</name>
<xref ref-type="aff" rid="aff1"><sup>1</sup>
</xref>
</contrib>
</contrib-group>
<aff id="aff1"><label>1</label>
<addr-line>Steinmann-Institut für Geologie, Mineralogie und Paläontologie, Universität Bonn, Bonn, Germany</addr-line>
</aff>
<aff id="aff2"><label>2</label>
<addr-line>Zoologisches Forschungsmuseum Alexander Koenig, Bonn, Germany</addr-line>
</aff>
<aff id="aff3"><label>3</label>
<addr-line>Institut für Biogeographie, Universität Trier, Trier, Germany</addr-line>
</aff>
<contrib-group><contrib contrib-type="editor"><name><surname>Andrew</surname>
<given-names>Andrew</given-names>
</name>
<role>Editor</role>
<xref ref-type="aff" rid="edit1"></xref>
</contrib>
</contrib-group>
<aff id="edit1"><addr-line>Bangor University, United Kingdom</addr-line>
</aff>
<author-notes><corresp id="cor1">* E-mail: <email>weinmann@uni-bonn.de</email>
</corresp>
<fn fn-type="conflict"><p><bold>Competing Interests: </bold>
The authors have declared that no competing interests exist.</p>
</fn>
<fn fn-type="con"><p>Conceived and designed the experiments: AW ML. Performed the experiments: AW ML. Analyzed the data: AW ML DR SL. Contributed reagents/materials/analysis tools: AW ML DR. Wrote the paper: AW ML.</p>
</fn>
</author-notes>
<pub-date pub-type="collection"><year>2013</year>
</pub-date>
<pub-date pub-type="epub"><day>19</day>
<month>4</month>
<year>2013</year>
</pub-date>
<volume>8</volume>
<issue>4</issue>
<elocation-id>e62182</elocation-id>
<history><date date-type="received"><day>19</day>
<month>7</month>
<year>2012</year>
</date>
<date date-type="accepted"><day>20</day>
<month>3</month>
<year>2013</year>
</date>
</history>
<permissions><copyright-year>2013</copyright-year>
<copyright-holder>Weinmann et al</copyright-holder>
<license><license-p>This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<abstract><p>The distribution of modern symbiont-bearing larger foraminifera is confined to tropical and subtropical shallow water marine habitats and a narrow range of environmental variables (e.g. temperature). Most of today's taxa are restricted to tropical and subtropical regions (between 30°N and 30°S) and their minimum temperature limits are governed by the 14 to 20°C isotherms. However, during times of extensive global warming (e.g., the Eocene and Miocene), larger foraminifera have been found as far north as 50°N (North America and Central Europe) as well as towards 47°S in New Zealand. During the last century, sea surface temperatures have been rising significantly. This trend is expected to continue and climate change scenarios for 2050 suggest a further increase by 1 to 3°C. We applied Species Distribution Models to assess potential distribution range changes of three taxa of larger foraminifera under current and future climate. The studied foraminifera include <italic>Archaias angulatus</italic>
, <italic>Calcarina</italic>
spp., and <italic>Amphistegina</italic>
spp., and represent taxa with regional, superregional and global distribution patterns. Under present environmental conditions, <italic>Amphistegina</italic>
spp. shows the largest potential distribution, apparently due to its temperature tolerance. Both <italic>Archaias angulatus</italic>
and <italic>Calcarina</italic>
spp. display potential distributions that cover currently uninhabited regions. Under climate conditions expected for the year 2050, all taxa should display latitudinal range expansions between 1 to 2.5 degrees both north- and southward. The modeled range projections suggest that some larger foraminifera may colonize biogeographic regions that so far seemed unsuitable. <italic>Archaias angulatus</italic>
and <italic>Calcarina</italic>
spp. also show an increase in habitat suitability within their native occurrence ranges, suggesting that their tolerance for maximum temperatures has yet not been fully exploited and that they benefit from ocean warming. Our findings suggest an increased role of larger foraminifera as carbonate producers and reef framework builders in future oceans.</p>
</abstract>
<funding-group><funding-statement>This work was supported by German Science Foundation (DFG) Grant number: LA 884/10-1 (<ext-link ext-link-type="uri" xlink:href="http://www.dfg.de/index.jsp">http://www.dfg.de/index.jsp</ext-link>
). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.</funding-statement>
</funding-group>
<counts><page-count count="14"></page-count>
</counts>
</article-meta>
</front>
</pmc>
<affiliations><list><country><li>Allemagne</li>
</country>
<region><li>District de Cologne</li>
<li>Rhénanie-du-Nord-Westphalie</li>
</region>
<settlement><li>Bonn</li>
</settlement>
</list>
<tree><country name="Allemagne"><region name="Rhénanie-du-Nord-Westphalie"><name sortKey="Weinmann, Anna E" sort="Weinmann, Anna E" uniqKey="Weinmann A" first="Anna E." last="Weinmann">Anna E. Weinmann</name>
</region>
<name sortKey="Langer, Martin R" sort="Langer, Martin R" uniqKey="Langer M" first="Martin R." last="Langer">Martin R. Langer</name>
<name sortKey="Lotters, Stefan" sort="Lotters, Stefan" uniqKey="Lotters S" first="Stefan" last="Lötters">Stefan Lötters</name>
<name sortKey="Rodder, Dennis" sort="Rodder, Dennis" uniqKey="Rodder D" first="Dennis" last="Rödder">Dennis Rödder</name>
</country>
</tree>
</affiliations>
</record>
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