River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons

Inshore massive corals often display bright luminescent lines that have been linked to river flood plumes into coastal catchments and hence have the potential to provide a long-term record of hinterland precipitation. Coral luminescence is thought to result from the incorporation of soil-derived hum...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Coral reefs 2010-09, Vol.29 (3), p.579-591
Hauptverfasser: Grove, C. A, Nagtegaal, R, Zinke, J, Scheufen, T, Koster, B, Kasper, S, McCulloch, M. T, van den Bergh, G, Brummer, G. Jan A
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 591
container_issue 3
container_start_page 579
container_title Coral reefs
container_volume 29
creator Grove, C. A
Nagtegaal, R
Zinke, J
Scheufen, T
Koster, B
Kasper, S
McCulloch, M. T
van den Bergh, G
Brummer, G. Jan A
description Inshore massive corals often display bright luminescent lines that have been linked to river flood plumes into coastal catchments and hence have the potential to provide a long-term record of hinterland precipitation. Coral luminescence is thought to result from the incorporation of soil-derived humic acids transported to the reef during major flood events. Corals far from terrestrial sources generally only exhibit dull relatively broad luminescence bands, which are attributed to seasonal changes in coral density. We therefore tested the hypothesis that spectral ratios rather than conventional luminescence intensity provide a quantitative proxy record of river runoff without the confounding effects of seasonal density changes. For this purpose, we have developed a new, rapid spectral luminescence scanning (SLS) technique that splits emission intensities into red, green and blue domains (RGB) for entire cores with an unprecedented linear resolution of 71.4 μm. Since humic acids have longer emission wavelength than the coral aragonite, normalisation of spectral emissions should yield a sensitive optical humic acid/aragonite ratio for humic acid runoff, i.e., G/B ratio. Indeed, G/B ratios rather than intensities are well correlated with Ba/Ca, a geochemical coral proxy for sediment runoff, and with rainfall data, as exemplified for coral records from Madagascar. Coral cores also display recent declining trends in luminescence intensity, which are also reported in corals elsewhere. Such trends appear to be associated with a modern decline in skeletal densities. By contrast, G/B spectral ratios not only mark the impact of individual cyclones but also imply that humic acid runoff increased in Madagascar over the past few decades while coral skeletal densities decreased. Consequently, the SLS technique deconvolves the long-term interplay between humic acid incorporation and coral density that have confounded earlier attempts to use luminescence intensities as a proxy for river runoff.
doi_str_mv 10.1007/s00338-010-0629-y
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_851467701</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>762270996</sourcerecordid><originalsourceid>FETCH-LOGICAL-a629t-2fe7378eb9ea426ce14d03b911b632aac52d89f1bb2cd02ce21cec9a3d1e58cf3</originalsourceid><addsrcrecordid>eNqNkU-L1TAUxYso-JzxA7gyCOKqzs1N2yRLGfwHA8LorEOad_Po2CbPpB14335SOii40FklkN89OfecqnrF4T0HkBcZQAhVA4caOtT16Um1443AGrRsn1Y7kIh1A6ieVy9yvgWAttViV9nr4Y4SS0uI3rNELoY8p8XNQ7kwn-LEQryjkeUjuTnZkY3LNATKjoIjlp0NYQgHFj2bbM5FjLm4YvknjTQXkfPqmbdjppcP51l18-njj8sv9dW3z18vP1zVtvida_QkhVTUa7INdo54swfRa877TqC1rsW90p73Pbo9oCPkjpy2Ys-pVc6Ls-rdpntM8ddCeTbTUFyOow0Ul2xUy5tOSuD_JWWHKDVKfBypZMn-USRo3RXyzV_kbVxSKNEYWSrslGrXj_kGuRRzTuTNMQ2TTSfDwayFm61wUwo3a-HmVGbePgjbUsvokw1uyL8HUXAhtV7Xx43L5SkcKP0x8C_x19uQt9HYQyrCN9-xhAm87C-L5Xs7KMWX</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>733868852</pqid></control><display><type>article</type><title>River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons</title><source>SpringerLink Journals</source><creator>Grove, C. A ; Nagtegaal, R ; Zinke, J ; Scheufen, T ; Koster, B ; Kasper, S ; McCulloch, M. T ; van den Bergh, G ; Brummer, G. Jan A</creator><creatorcontrib>Grove, C. A ; Nagtegaal, R ; Zinke, J ; Scheufen, T ; Koster, B ; Kasper, S ; McCulloch, M. T ; van den Bergh, G ; Brummer, G. Jan A</creatorcontrib><description>Inshore massive corals often display bright luminescent lines that have been linked to river flood plumes into coastal catchments and hence have the potential to provide a long-term record of hinterland precipitation. Coral luminescence is thought to result from the incorporation of soil-derived humic acids transported to the reef during major flood events. Corals far from terrestrial sources generally only exhibit dull relatively broad luminescence bands, which are attributed to seasonal changes in coral density. We therefore tested the hypothesis that spectral ratios rather than conventional luminescence intensity provide a quantitative proxy record of river runoff without the confounding effects of seasonal density changes. For this purpose, we have developed a new, rapid spectral luminescence scanning (SLS) technique that splits emission intensities into red, green and blue domains (RGB) for entire cores with an unprecedented linear resolution of 71.4 μm. Since humic acids have longer emission wavelength than the coral aragonite, normalisation of spectral emissions should yield a sensitive optical humic acid/aragonite ratio for humic acid runoff, i.e., G/B ratio. Indeed, G/B ratios rather than intensities are well correlated with Ba/Ca, a geochemical coral proxy for sediment runoff, and with rainfall data, as exemplified for coral records from Madagascar. Coral cores also display recent declining trends in luminescence intensity, which are also reported in corals elsewhere. Such trends appear to be associated with a modern decline in skeletal densities. By contrast, G/B spectral ratios not only mark the impact of individual cyclones but also imply that humic acid runoff increased in Madagascar over the past few decades while coral skeletal densities decreased. Consequently, the SLS technique deconvolves the long-term interplay between humic acid incorporation and coral density that have confounded earlier attempts to use luminescence intensities as a proxy for river runoff.</description><identifier>ISSN: 0722-4028</identifier><identifier>EISSN: 1432-0975</identifier><identifier>DOI: 10.1007/s00338-010-0629-y</identifier><identifier>CODEN: CORFDL</identifier><language>eng</language><publisher>Berlin/Heidelberg: Berlin/Heidelberg : Springer-Verlag</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Biological and medical sciences ; Biomedical and Life Sciences ; Brackish ; Coral carbonate ; Coral reefs ; Core scanning ; Cores ; Emissions ; Fresh water ecosystems ; Freshwater ; Freshwater &amp; Marine Ecology ; Fundamental and applied biological sciences. Psychology ; Geochemistry ; Humic acids ; Hydrologic data ; Life Sciences ; Luminescence ; Luminescence spectra ; Luminosity ; Marine biology ; Oceanography ; Porites ; River flow ; Rivers ; Runoff ; Sea water ecosystems ; Soil runoff ; Spectrum analysis ; Synecology</subject><ispartof>Coral reefs, 2010-09, Vol.29 (3), p.579-591</ispartof><rights>The Author(s) 2010</rights><rights>2015 INIST-CNRS</rights><rights>Springer-Verlag 2010</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a629t-2fe7378eb9ea426ce14d03b911b632aac52d89f1bb2cd02ce21cec9a3d1e58cf3</citedby><cites>FETCH-LOGICAL-a629t-2fe7378eb9ea426ce14d03b911b632aac52d89f1bb2cd02ce21cec9a3d1e58cf3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00338-010-0629-y$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00338-010-0629-y$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=23137991$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Grove, C. A</creatorcontrib><creatorcontrib>Nagtegaal, R</creatorcontrib><creatorcontrib>Zinke, J</creatorcontrib><creatorcontrib>Scheufen, T</creatorcontrib><creatorcontrib>Koster, B</creatorcontrib><creatorcontrib>Kasper, S</creatorcontrib><creatorcontrib>McCulloch, M. T</creatorcontrib><creatorcontrib>van den Bergh, G</creatorcontrib><creatorcontrib>Brummer, G. Jan A</creatorcontrib><title>River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons</title><title>Coral reefs</title><addtitle>Coral Reefs</addtitle><description>Inshore massive corals often display bright luminescent lines that have been linked to river flood plumes into coastal catchments and hence have the potential to provide a long-term record of hinterland precipitation. Coral luminescence is thought to result from the incorporation of soil-derived humic acids transported to the reef during major flood events. Corals far from terrestrial sources generally only exhibit dull relatively broad luminescence bands, which are attributed to seasonal changes in coral density. We therefore tested the hypothesis that spectral ratios rather than conventional luminescence intensity provide a quantitative proxy record of river runoff without the confounding effects of seasonal density changes. For this purpose, we have developed a new, rapid spectral luminescence scanning (SLS) technique that splits emission intensities into red, green and blue domains (RGB) for entire cores with an unprecedented linear resolution of 71.4 μm. Since humic acids have longer emission wavelength than the coral aragonite, normalisation of spectral emissions should yield a sensitive optical humic acid/aragonite ratio for humic acid runoff, i.e., G/B ratio. Indeed, G/B ratios rather than intensities are well correlated with Ba/Ca, a geochemical coral proxy for sediment runoff, and with rainfall data, as exemplified for coral records from Madagascar. Coral cores also display recent declining trends in luminescence intensity, which are also reported in corals elsewhere. Such trends appear to be associated with a modern decline in skeletal densities. By contrast, G/B spectral ratios not only mark the impact of individual cyclones but also imply that humic acid runoff increased in Madagascar over the past few decades while coral skeletal densities decreased. Consequently, the SLS technique deconvolves the long-term interplay between humic acid incorporation and coral density that have confounded earlier attempts to use luminescence intensities as a proxy for river runoff.</description><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Biomedical and Life Sciences</subject><subject>Brackish</subject><subject>Coral carbonate</subject><subject>Coral reefs</subject><subject>Core scanning</subject><subject>Cores</subject><subject>Emissions</subject><subject>Fresh water ecosystems</subject><subject>Freshwater</subject><subject>Freshwater &amp; Marine Ecology</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Geochemistry</subject><subject>Humic acids</subject><subject>Hydrologic data</subject><subject>Life Sciences</subject><subject>Luminescence</subject><subject>Luminescence spectra</subject><subject>Luminosity</subject><subject>Marine biology</subject><subject>Oceanography</subject><subject>Porites</subject><subject>River flow</subject><subject>Rivers</subject><subject>Runoff</subject><subject>Sea water ecosystems</subject><subject>Soil runoff</subject><subject>Spectrum analysis</subject><subject>Synecology</subject><issn>0722-4028</issn><issn>1432-0975</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqNkU-L1TAUxYso-JzxA7gyCOKqzs1N2yRLGfwHA8LorEOad_Po2CbPpB14335SOii40FklkN89OfecqnrF4T0HkBcZQAhVA4caOtT16Um1443AGrRsn1Y7kIh1A6ieVy9yvgWAttViV9nr4Y4SS0uI3rNELoY8p8XNQ7kwn-LEQryjkeUjuTnZkY3LNATKjoIjlp0NYQgHFj2bbM5FjLm4YvknjTQXkfPqmbdjppcP51l18-njj8sv9dW3z18vP1zVtvida_QkhVTUa7INdo54swfRa877TqC1rsW90p73Pbo9oCPkjpy2Ys-pVc6Ls-rdpntM8ddCeTbTUFyOow0Ul2xUy5tOSuD_JWWHKDVKfBypZMn-USRo3RXyzV_kbVxSKNEYWSrslGrXj_kGuRRzTuTNMQ2TTSfDwayFm61wUwo3a-HmVGbePgjbUsvokw1uyL8HUXAhtV7Xx43L5SkcKP0x8C_x19uQt9HYQyrCN9-xhAm87C-L5Xs7KMWX</recordid><startdate>20100901</startdate><enddate>20100901</enddate><creator>Grove, C. A</creator><creator>Nagtegaal, R</creator><creator>Zinke, J</creator><creator>Scheufen, T</creator><creator>Koster, B</creator><creator>Kasper, S</creator><creator>McCulloch, M. T</creator><creator>van den Bergh, G</creator><creator>Brummer, G. Jan A</creator><general>Berlin/Heidelberg : Springer-Verlag</general><general>Springer-Verlag</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>C6C</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7T7</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7UA</scope><scope>7QH</scope><scope>H97</scope></search><sort><creationdate>20100901</creationdate><title>River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons</title><author>Grove, C. A ; Nagtegaal, R ; Zinke, J ; Scheufen, T ; Koster, B ; Kasper, S ; McCulloch, M. T ; van den Bergh, G ; Brummer, G. Jan A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a629t-2fe7378eb9ea426ce14d03b911b632aac52d89f1bb2cd02ce21cec9a3d1e58cf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Biological and medical sciences</topic><topic>Biomedical and Life Sciences</topic><topic>Brackish</topic><topic>Coral carbonate</topic><topic>Coral reefs</topic><topic>Core scanning</topic><topic>Cores</topic><topic>Emissions</topic><topic>Fresh water ecosystems</topic><topic>Freshwater</topic><topic>Freshwater &amp; Marine Ecology</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Geochemistry</topic><topic>Humic acids</topic><topic>Hydrologic data</topic><topic>Life Sciences</topic><topic>Luminescence</topic><topic>Luminescence spectra</topic><topic>Luminosity</topic><topic>Marine biology</topic><topic>Oceanography</topic><topic>Porites</topic><topic>River flow</topic><topic>Rivers</topic><topic>Runoff</topic><topic>Sea water ecosystems</topic><topic>Soil runoff</topic><topic>Spectrum analysis</topic><topic>Synecology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Grove, C. A</creatorcontrib><creatorcontrib>Nagtegaal, R</creatorcontrib><creatorcontrib>Zinke, J</creatorcontrib><creatorcontrib>Scheufen, T</creatorcontrib><creatorcontrib>Koster, B</creatorcontrib><creatorcontrib>Kasper, S</creatorcontrib><creatorcontrib>McCulloch, M. T</creatorcontrib><creatorcontrib>van den Bergh, G</creatorcontrib><creatorcontrib>Brummer, G. Jan A</creatorcontrib><collection>AGRIS</collection><collection>Springer Nature OA Free Journals</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Water Resources Abstracts</collection><collection>Aqualine</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><jtitle>Coral reefs</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Grove, C. A</au><au>Nagtegaal, R</au><au>Zinke, J</au><au>Scheufen, T</au><au>Koster, B</au><au>Kasper, S</au><au>McCulloch, M. T</au><au>van den Bergh, G</au><au>Brummer, G. Jan A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons</atitle><jtitle>Coral reefs</jtitle><stitle>Coral Reefs</stitle><date>2010-09-01</date><risdate>2010</risdate><volume>29</volume><issue>3</issue><spage>579</spage><epage>591</epage><pages>579-591</pages><issn>0722-4028</issn><eissn>1432-0975</eissn><coden>CORFDL</coden><abstract>Inshore massive corals often display bright luminescent lines that have been linked to river flood plumes into coastal catchments and hence have the potential to provide a long-term record of hinterland precipitation. Coral luminescence is thought to result from the incorporation of soil-derived humic acids transported to the reef during major flood events. Corals far from terrestrial sources generally only exhibit dull relatively broad luminescence bands, which are attributed to seasonal changes in coral density. We therefore tested the hypothesis that spectral ratios rather than conventional luminescence intensity provide a quantitative proxy record of river runoff without the confounding effects of seasonal density changes. For this purpose, we have developed a new, rapid spectral luminescence scanning (SLS) technique that splits emission intensities into red, green and blue domains (RGB) for entire cores with an unprecedented linear resolution of 71.4 μm. Since humic acids have longer emission wavelength than the coral aragonite, normalisation of spectral emissions should yield a sensitive optical humic acid/aragonite ratio for humic acid runoff, i.e., G/B ratio. Indeed, G/B ratios rather than intensities are well correlated with Ba/Ca, a geochemical coral proxy for sediment runoff, and with rainfall data, as exemplified for coral records from Madagascar. Coral cores also display recent declining trends in luminescence intensity, which are also reported in corals elsewhere. Such trends appear to be associated with a modern decline in skeletal densities. By contrast, G/B spectral ratios not only mark the impact of individual cyclones but also imply that humic acid runoff increased in Madagascar over the past few decades while coral skeletal densities decreased. Consequently, the SLS technique deconvolves the long-term interplay between humic acid incorporation and coral density that have confounded earlier attempts to use luminescence intensities as a proxy for river runoff.</abstract><cop>Berlin/Heidelberg</cop><pub>Berlin/Heidelberg : Springer-Verlag</pub><doi>10.1007/s00338-010-0629-y</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0722-4028
ispartof Coral reefs, 2010-09, Vol.29 (3), p.579-591
issn 0722-4028
1432-0975
language eng
recordid cdi_proquest_miscellaneous_851467701
source SpringerLink Journals
subjects Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Biomedical and Life Sciences
Brackish
Coral carbonate
Coral reefs
Core scanning
Cores
Emissions
Fresh water ecosystems
Freshwater
Freshwater & Marine Ecology
Fundamental and applied biological sciences. Psychology
Geochemistry
Humic acids
Hydrologic data
Life Sciences
Luminescence
Luminescence spectra
Luminosity
Marine biology
Oceanography
Porites
River flow
Rivers
Runoff
Sea water ecosystems
Soil runoff
Spectrum analysis
Synecology
title River runoff reconstructions from novel spectral luminescence scanning of massive coral skeletons
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-25T12%3A00%3A46IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=River%20runoff%20reconstructions%20from%20novel%20spectral%20luminescence%20scanning%20of%20massive%20coral%20skeletons&rft.jtitle=Coral%20reefs&rft.au=Grove,%20C.%20A&rft.date=2010-09-01&rft.volume=29&rft.issue=3&rft.spage=579&rft.epage=591&rft.pages=579-591&rft.issn=0722-4028&rft.eissn=1432-0975&rft.coden=CORFDL&rft_id=info:doi/10.1007/s00338-010-0629-y&rft_dat=%3Cproquest_cross%3E762270996%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=733868852&rft_id=info:pmid/&rfr_iscdi=true