A distinct source and differentiation history for Kolumbo submarine volcano, Santorini volcanic field, Aegean arc
Identifieur interne : 000016 ( Pmc/Curation ); précédent : 000015; suivant : 000017A distinct source and differentiation history for Kolumbo submarine volcano, Santorini volcanic field, Aegean arc
Auteurs : Martijn Klaver ; Steven Carey ; Paraskevi Nomikou ; Ingrid Smet ; Athanasios Godelitsas ; Pieter VroonSource :
- Geochemistry, Geophysics, Geosystems : G(3) [ 1525-2027 ] ; 2016.
Abstract
This study reports the first detailed geochemical characterization of Kolumbo submarine volcano in order to investigate the role of source heterogeneity in controlling geochemical variability within the Santorini volcanic field in the central Aegean arc. Kolumbo, situated 15 km to the northeast of Santorini, last erupted in 1650 AD and is thus closely associated with the Santorini volcanic system in space and time. Samples taken by remotely‐operated vehicle that were analyzed for major element, trace element and Sr‐Nd‐Hf‐Pb isotope composition include the 1650 AD and underlying K2 rhyolitic, enclave‐bearing pumices that are nearly identical in composition (73 wt.% SiO2, 4.2 wt.% K2O). Lava bodies exposed in the crater and enclaves are basalts to andesites (52–60 wt.% SiO2). Biotite and amphibole are common phenocryst phases, in contrast with the typically anhydrous mineral assemblages of Santorini. The strong geochemical signature of amphibole fractionation and the assimilation of lower crustal basement in the petrogenesis of the Kolumbo magmas indicates that Kolumbo and Santorini underwent different crustal differentiation histories and that their crustal magmatic systems are unrelated. Moreover, the Kolumbo samples are derived from a distinct, more enriched mantle source that is characterized by high Nb/Yb (>3) and low 206Pb/204Pb (<18.82) that has not been recognized in the Santorini volcanic products. The strong dissimilarity in both petrogenesis and inferred mantle sources between Kolumbo and Santorini suggests that pronounced source variations can be manifested in arc magmas that are closely associated in space and time within a single volcanic field.
Url:
DOI: 10.1002/2016GC006398
PubMed: 27917071
PubMed Central: 5114867
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<front><div type="abstract" xml:lang="en"><title>Abstract</title>
<p>This study reports the first detailed geochemical characterization of Kolumbo submarine volcano in order to investigate the role of source heterogeneity in controlling geochemical variability within the Santorini volcanic field in the central Aegean arc. Kolumbo, situated 15 km to the northeast of Santorini, last erupted in 1650 AD and is thus closely associated with the Santorini volcanic system in space and time. Samples taken by remotely‐operated vehicle that were analyzed for major element, trace element and Sr‐Nd‐Hf‐Pb isotope composition include the 1650 AD and underlying K2 rhyolitic, enclave‐bearing pumices that are nearly identical in composition (73 wt.% SiO<sub>2</sub>
, 4.2 wt.% K<sub>2</sub>
O). Lava bodies exposed in the crater and enclaves are basalts to andesites (52–60 wt.% SiO<sub>2</sub>
). Biotite and amphibole are common phenocryst phases, in contrast with the typically anhydrous mineral assemblages of Santorini. The strong geochemical signature of amphibole fractionation and the assimilation of lower crustal basement in the petrogenesis of the Kolumbo magmas indicates that Kolumbo and Santorini underwent different crustal differentiation histories and that their crustal magmatic systems are unrelated. Moreover, the Kolumbo samples are derived from a distinct, more enriched mantle source that is characterized by high Nb/Yb (>3) and low <sup>206</sup>
Pb/<sup>204</sup>
Pb (<18.82) that has not been recognized in the Santorini volcanic products. The strong dissimilarity in both petrogenesis and inferred mantle sources between Kolumbo and Santorini suggests that pronounced source variations can be manifested in arc magmas that are closely associated in space and time within a single volcanic field.</p>
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<front><journal-meta><journal-id journal-id-type="nlm-ta">Geochem Geophys Geosyst</journal-id>
<journal-id journal-id-type="iso-abbrev">Geochem Geophys Geosyst</journal-id>
<journal-id journal-id-type="doi">10.1002/(ISSN)1525-2027</journal-id>
<journal-id journal-id-type="publisher-id">GGGE</journal-id>
<journal-title-group><journal-title>Geochemistry, Geophysics, Geosystems : G(3)</journal-title>
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<publisher><publisher-name>John Wiley and Sons Inc.</publisher-name>
<publisher-loc>Hoboken</publisher-loc>
</publisher>
</journal-meta>
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<article-id pub-id-type="doi">10.1002/2016GC006398</article-id>
<article-id pub-id-type="publisher-id">GGGE21078</article-id>
<article-categories><subj-group subj-group-type="article-subject-classification"><subject>Geochemistry</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subduction Zone Processes</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Radiogenic Isotope Geochemistry</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Marine Geology and Geophysics</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subduction Zone Processes</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Mineralogy and Petrology</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subduction Zone Processes</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Tectonophysics</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subduction Zone Processes</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Volcanology</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subaqueous Volcanism</subject>
</subj-group>
<subj-group subj-group-type="article-subject-classification"><subject>Subduction Zone Processes</subject>
</subj-group>
<subj-group subj-group-type="overline"><subject>Research Article</subject>
</subj-group>
<subj-group subj-group-type="heading"><subject>Research Articles</subject>
</subj-group>
</article-categories>
<title-group><article-title>A distinct source and differentiation history for Kolumbo submarine volcano, Santorini volcanic field, Aegean arc</article-title>
<alt-title alt-title-type="right-running-head">KOLUMBO SUBMARINE VOLCANO</alt-title>
<alt-title alt-title-type="left-running-head">KLAVER ET AL.</alt-title>
</title-group>
<contrib-group><contrib id="ggge21078-cr-0001" contrib-type="author" corresp="yes"><name><surname>Klaver</surname>
<given-names>Martijn</given-names>
</name>
<address><email>martijn.klaver@bristol.ac.uk</email>
</address>
<xref ref-type="aff" rid="ggge21078-aff-0001"><sup>1</sup>
</xref>
<xref ref-type="aff" rid="ggge21078-aff-0002"><sup>2</sup>
</xref>
</contrib>
<contrib id="ggge21078-cr-0002" contrib-type="author"><name><surname>Carey</surname>
<given-names>Steven</given-names>
</name>
<xref ref-type="aff" rid="ggge21078-aff-0003"><sup>3</sup>
</xref>
</contrib>
<contrib id="ggge21078-cr-0003" contrib-type="author"><name><surname>Nomikou</surname>
<given-names>Paraskevi</given-names>
</name>
<xref ref-type="aff" rid="ggge21078-aff-0004"><sup>4</sup>
</xref>
</contrib>
<contrib id="ggge21078-cr-0004" contrib-type="author"><name><surname>Smet</surname>
<given-names>Ingrid</given-names>
</name>
<xref ref-type="aff" rid="ggge21078-aff-0005"><sup>5</sup>
</xref>
</contrib>
<contrib id="ggge21078-cr-0005" contrib-type="author"><name><surname>Godelitsas</surname>
<given-names>Athanasios</given-names>
</name>
<xref ref-type="aff" rid="ggge21078-aff-0004"><sup>4</sup>
</xref>
</contrib>
<contrib id="ggge21078-cr-0006" contrib-type="author"><name><surname>Vroon</surname>
<given-names>Pieter</given-names>
</name>
<xref ref-type="aff" rid="ggge21078-aff-0001"><sup>1</sup>
</xref>
</contrib>
</contrib-group>
<aff id="ggge21078-aff-0001"><label><sup>1</sup>
</label>
<named-content content-type="organisation-division">Department of Geology and Geochemistry</named-content>
<institution>Vrije Universiteit Amsterdam</institution>
<named-content content-type="city">Amsterdam</named-content>
<country country="NL">Netherlands</country>
</aff>
<aff id="ggge21078-aff-0002"><label><sup>2</sup>
</label>
<named-content content-type="organisation-division">Now at Bristol Isotope Group, School of Earth Sciences</named-content>
<institution>University of Bristol</institution>
<named-content content-type="city">Bristol</named-content>
<country country="GB">UK</country>
</aff>
<aff id="ggge21078-aff-0003"><label><sup>3</sup>
</label>
<named-content content-type="organisation-division">Graduate School of Oceanography</named-content>
<institution>University of Rhode Island</institution>
<named-content content-type="city">Kingston</named-content>
<named-content content-type="country-part">Rhode Island</named-content>
<country country="US">USA</country>
</aff>
<aff id="ggge21078-aff-0004"><label><sup>4</sup>
</label>
<named-content content-type="organisation-division">Faculty of Geology and Geo‐Environment</named-content>
<institution>National and Kapodistrian University of Athens</institution>
<named-content content-type="city">Athens</named-content>
<country country="GR">Greece</country>
</aff>
<aff id="ggge21078-aff-0005"><label><sup>5</sup>
</label>
<named-content content-type="organisation-division">Department of Geology</named-content>
<institution>Ghent University</institution>
<named-content content-type="city">Ghent</named-content>
<country country="BE">Belgium</country>
</aff>
<author-notes><corresp id="correspondenceTo"><label>*</label>
Correspondence to: M. Klaver, <email>martijn.klaver@bristol.ac.uk</email>
</corresp>
</author-notes>
<pub-date pub-type="epub"><day>16</day>
<month>8</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="ppub"><month>8</month>
<year>2016</year>
</pub-date>
<volume>17</volume>
<issue>8</issue>
<issue-id pub-id-type="doi">10.1002/ggge.v17.8</issue-id>
<fpage>3254</fpage>
<lpage>3273</lpage>
<history><date date-type="received"><day>13</day>
<month>4</month>
<year>2016</year>
</date>
<date date-type="accepted"><day>05</day>
<month>7</month>
<year>2016</year>
</date>
</history>
<permissions><pmc-comment> © 2016. American Geophysical Union. All Rights Reserved. </pmc-comment>
<copyright-statement content-type="article-copyright">© 2016. The Authors. Geochemistry, Geophysics, Geosystems published by Wiley Periodicals, Inc. on behalf of American Geophysical Union.</copyright-statement>
<license license-type="creativeCommonsBy-nc-nd"><license-p>This is an open access article under the terms of the <ext-link ext-link-type="uri" xlink:href="http://creativecommons.org/licenses/by-nc-nd/4.0/">Creative Commons Attribution‐NonCommercial‐NoDerivs</ext-link>
License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.</license-p>
</license>
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<abstract><title>Abstract</title>
<p>This study reports the first detailed geochemical characterization of Kolumbo submarine volcano in order to investigate the role of source heterogeneity in controlling geochemical variability within the Santorini volcanic field in the central Aegean arc. Kolumbo, situated 15 km to the northeast of Santorini, last erupted in 1650 AD and is thus closely associated with the Santorini volcanic system in space and time. Samples taken by remotely‐operated vehicle that were analyzed for major element, trace element and Sr‐Nd‐Hf‐Pb isotope composition include the 1650 AD and underlying K2 rhyolitic, enclave‐bearing pumices that are nearly identical in composition (73 wt.% SiO<sub>2</sub>
, 4.2 wt.% K<sub>2</sub>
O). Lava bodies exposed in the crater and enclaves are basalts to andesites (52–60 wt.% SiO<sub>2</sub>
). Biotite and amphibole are common phenocryst phases, in contrast with the typically anhydrous mineral assemblages of Santorini. The strong geochemical signature of amphibole fractionation and the assimilation of lower crustal basement in the petrogenesis of the Kolumbo magmas indicates that Kolumbo and Santorini underwent different crustal differentiation histories and that their crustal magmatic systems are unrelated. Moreover, the Kolumbo samples are derived from a distinct, more enriched mantle source that is characterized by high Nb/Yb (>3) and low <sup>206</sup>
Pb/<sup>204</sup>
Pb (<18.82) that has not been recognized in the Santorini volcanic products. The strong dissimilarity in both petrogenesis and inferred mantle sources between Kolumbo and Santorini suggests that pronounced source variations can be manifested in arc magmas that are closely associated in space and time within a single volcanic field.</p>
</abstract>
<abstract abstract-type="short"><title>Key Points:</title>
<p><list list-type="simple" id="ggge21078-list-0001"><list-item id="ggge21078-li-0001"><p>A trace element and Sr‐Nd‐Hf‐Pb isotope study of Kolumbo submarine volcano within the Santorini volcanic field</p>
</list-item>
<list-item id="ggge21078-li-0002"><p>The magmatic systems of Kolumbo and Santorini are unrelated and Kolumbo taps a distinct enriched mantle source</p>
</list-item>
<list-item id="ggge21078-li-0003"><p>Mantle source variations can be manifested in temporally associated arc magmas within the same volcanic field</p>
</list-item>
</list>
</p>
</abstract>
<kwd-group kwd-group-type="author-generated"><kwd id="ggge21078-kwd-0001">Kolumbo submarine volcano</kwd>
<kwd id="ggge21078-kwd-0002">Aegean arc</kwd>
<kwd id="ggge21078-kwd-0003">Santorini volcanic field</kwd>
<kwd id="ggge21078-kwd-0004">mantle source</kwd>
<kwd id="ggge21078-kwd-0005">Sr‐Nd‐Hf‐Pb isotopes</kwd>
</kwd-group>
<funding-group><award-group><funding-source>the European Research Council under the European Union's Seventh Framework Program</funding-source>
<award-id>(FP7/2007‐2013)/ERC</award-id>
<award-id>319209</award-id>
</award-group>
</funding-group>
<counts><fig-count count="12"></fig-count>
<table-count count="0"></table-count>
<page-count count="20"></page-count>
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<notes><p content-type="self-citation"><mixed-citation publication-type="journal" id="ggge21078-cit-0001"><string-name><surname>Klaver</surname>
, <given-names>M.</given-names>
</string-name>
,
<string-name><given-names>S.</given-names>
<surname>Carey</surname>
</string-name>
,
<string-name><given-names>P.</given-names>
<surname>Nomikou</surname>
</string-name>
,
<string-name><given-names>I.</given-names>
<surname>Smet</surname>
</string-name>
,
<string-name><given-names>A.</given-names>
<surname>Godelitsas</surname>
</string-name>
, and
<string-name><given-names>P.</given-names>
<surname>Vroon</surname>
</string-name>
(<year>2016</year>
), <article-title>A distinct source and differentiation history for <styled-content style="fixed-case">K</styled-content>
olumbo submarine volcano, <styled-content style="fixed-case">S</styled-content>
antorini volcanic field, <styled-content style="fixed-case">A</styled-content>
egean arc</article-title>
, <source>Geochem. Geophys. Geosyst.</source>
, <volume>17</volume>
, <fpage>3254</fpage>
–<lpage>3273</lpage>
, doi:<ext-link ext-link-type="doi" xlink:href="10.1002/2016GC006398">10.1002/2016GC006398</ext-link>
.
</mixed-citation>
</p>
</notes>
</front>
</pmc>
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