Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)
Identifieur interne : 000F48 ( Istex/Corpus ); précédent : 000F47; suivant : 000F49Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)
Auteurs : R. Casotti ; A. Landolfi ; C. Brunet ; F. D'Ortenzio ; O. Mangoni ; M. Ribera D'Alcalà ; M. DenisSource :
- Journal of Geophysical Research: Oceans [ 0148-0227 ] ; 2003-09.
Abstract
The relationship between phytoplankton distribution and dynamics, and the resident water masses in the Ionian Sea was investigated in the spring of 1999 by flow cytometry, HPLC, microscopy, 14C incorporation, and serial dilutions. More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl−1 h−1). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl−1 h−1) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m−2 d−1), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d−1 at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d−1) Picoeukaryote growth was tightly coupled with grazing (0.80 d−1), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.
Url:
DOI: 10.1029/2002JC001541
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More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl−1 h−1). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl−1 h−1) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m−2 d−1), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d−1 at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d−1) Picoeukaryote growth was tightly coupled with grazing (0.80 d−1), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>R. 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More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl−1 h−1). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl−1 h−1) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m−2 d−1), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d−1 at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d−1) Picoeukaryote growth was tightly coupled with grazing (0.80 d−1), indicating efficient biomass recycling. 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More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl−1 h−1). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl−1 h−1) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m−2 d−1), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d−1 at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d−1) Picoeukaryote growth was tightly coupled with grazing (0.80 d−1), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>ultraplankton</term></item><item><term>flow cytometry</term></item><item><term>primary productivity</term></item><item><term>Mediterranean Sea</term></item><item><term>mixing</term></item><item><term>photoacclimation</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>Physical and Biochemical Evolution of the Eastern Mediterranean in the 1990s (PBE)</term></item><item><term>BIOGEOSCIENCES</term></item><item><term>Ecosystems, structure and dynamics</term></item><item><term>Food webs and trophodynamics</term></item><item><term>OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</term></item><item><term>Ecosystems, structure, dynamics, and modeling</term></item><item><term>Food webs, structure, and dynamics</term></item><item><term>Phytoplankton</term></item><item><term>Zooplankton</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2002-07-16">Received</change><change when="2003-02-19">Registration</change><change when="2003-09">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><original>false</original><mimetype>text/plain</mimetype><extension>txt</extension><uri>https://api.istex.fr/document/A9C4BCDB45BAA02633B67A45CB0251FC2509E354/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component type="serialArticle" version="2.0" xml:lang="en" xml:id="jgrc9160"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2156-2202c</doi><issn type="print">0148-0227</issn><issn type="electronic">2156-2202</issn><idGroup><id type="product" value="JGRC"></id><id type="coden" value="JGREA2"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS">Journal of Geophysical Research: Oceans</title><title type="short">J. 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Res.</title></titleGroup></publicationMeta><publicationMeta level="part" position="90"><doi>10.1002/jgrc.v108.C9</doi><idGroup><id type="focusSection" value="3"></id></idGroup><titleGroup><title type="focusSection" xml:lang="en">Journal of Geophysical Research: Oceans</title></titleGroup><numberingGroup><numbering type="journalVolume" number="108">108</numbering><numbering type="journalIssue">C9</numbering></numberingGroup><coverDate startDate="2003-09">September 2003</coverDate></publicationMeta><publicationMeta level="unit" position="170" type="article" status="forIssue"><doi>10.1029/2002JC001541</doi><idGroup><id type="editorialOffice" value="2002JC001541"></id><id type="society" value="8116"></id><id type="unit" value="JGRC9160"></id></idGroup><countGroup><count type="pageTotal" number="19"></count></countGroup><copyright ownership="thirdParty">Copyright 2003 by the American Geophysical Union.</copyright><eventGroup><event type="manuscriptReceived" date="2002-07-16"></event><event type="manuscriptRevised" date="2003-01-23"></event><event type="manuscriptAccepted" date="2003-02-19"></event><event type="firstOnline" date="2003-09-24"></event><event type="publishedOnlineFinalForm" date="2003-09-24"></event><event type="xmlConverted" agent="SPi Global Converter:AGUv3.42_TO_WileyML3Gv1.0.3 version:1.2; WileyML 3G Packaging Tool v1.0; AGU2WileyML3G Final Clean Up v1.0" date="2012-12-17"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:4.0.1" date="2014-03-20"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-30"></event></eventGroup><numberingGroup><numbering type="pageFirst">n/a</numbering><numbering type="pageLast">n/a</numbering></numberingGroup><subjectInfo><subject href="http://psi.agu.org/specialSection/PBEMD1">Physical and Biochemical Evolution of the Eastern Mediterranean in the 1990s (PBE)</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0439">Ecosystems, structure and dynamics</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0491">Food webs and trophodynamics</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/4815">Ecosystems, structure, dynamics, and modeling</subject><subject href="http://psi.agu.org/taxonomy5/4817">Food webs, structure, and dynamics</subject><subject href="http://psi.agu.org/taxonomy5/4855">Phytoplankton</subject><subject href="http://psi.agu.org/taxonomy5/4890">Zooplankton</subject></subjectInfo></subjectInfo><selfCitationGroup><citation xml:id="jgrc9160-cit-0000" type="self"><author><familyName>Casotti</familyName>, <givenNames>R.</givenNames></author>, <author><givenNames>A.</givenNames> <familyName>Landolfi</familyName></author>, <author><givenNames>C.</givenNames> <familyName>Brunet</familyName></author>, <author><givenNames>F.</givenNames> <familyName>D'Ortenzio</familyName></author>, <author><givenNames>O.</givenNames> <familyName>Mangoni</familyName></author>, <author><givenNames>M.</givenNames> <familyName>Ribera d'Alcalà</familyName></author>, and <author><givenNames>M.</givenNames> <familyName>Denis</familyName></author> (<pubYear year="2003">2003</pubYear>), <articleTitle>Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)</articleTitle>, <journalTitle>J. Geophys. Res.</journalTitle>, <vol>108</vol>, 8116, doi:<accessionId ref="info:doi/10.1029/2002JC001541">10.1029/2002JC001541</accessionId>, <issue>C9</issue>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:JGRC.JGRC9160.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="7"></count><count type="tableTotal" number="5"></count></countGroup><titleGroup><title type="main">Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)</title><title type="short">PHYTOPLANKTON OF THE IONIAN SEA</title><title type="shortAuthors">Casotti <i>et al</i>.</title></titleGroup><creators><creator creatorRole="author" xml:id="jgrc9160-cr-0001" affiliationRef="#jgrc9160-aff-0001"><personName><givenNames>R.</givenNames> <familyName>Casotti</familyName></personName><contactDetails><email normalForm="raffa@szn.it">raffa@szn.it</email></contactDetails></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0002" affiliationRef="#jgrc9160-aff-0001 #jgrc9160-aff-0003"><personName><givenNames>A.</givenNames> <familyName>Landolfi</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0003" affiliationRef="#jgrc9160-aff-0001"><personName><givenNames>C.</givenNames> <familyName>Brunet</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0004" affiliationRef="#jgrc9160-aff-0001"><personName><givenNames>F.</givenNames> <familyName>D'Ortenzio</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0005" affiliationRef="#jgrc9160-aff-0001 #jgrc9160-aff-0004"><personName><givenNames>O.</givenNames> <familyName>Mangoni</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0006" affiliationRef="#jgrc9160-aff-0001"><personName><givenNames>M.</givenNames> <familyName>Ribera d'Alcalà</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc9160-cr-0007" affiliationRef="#jgrc9160-aff-0002"><personName><givenNames>M.</givenNames> <familyName>Denis</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="IT" type="organization" xml:id="jgrc9160-aff-0001"><orgName>Stazione Zoologica “A. Dohrn” di Napoli</orgName><address><city>Naples</city><country>Italy</country></address></affiliation><affiliation countryCode="FR" type="organization" xml:id="jgrc9160-aff-0002"><orgName>Laboratoire d'Océanographie et de Biogéochimie</orgName><address><city>Marseille</city><country>France</country></address></affiliation><affiliation type="organization" xml:id="jgrc9160-aff-0003"><unparsedAffiliation>Now at School of Ocean and Earth Science, University of Southampton, Southampton Oceanography Centre, Southampton, UK.</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="jgrc9160-aff-0004"><unparsedAffiliation>Now at University of Naples “Federico II”, Dipartimento di Zoologia, Naples, Italy.</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="jgrc9160-kwd-0001">ultraplankton</keyword><keyword xml:id="jgrc9160-kwd-0002">flow cytometry</keyword><keyword xml:id="jgrc9160-kwd-0003">primary productivity</keyword><keyword xml:id="jgrc9160-kwd-0004">Mediterranean Sea</keyword><keyword xml:id="jgrc9160-kwd-0005">mixing</keyword><keyword xml:id="jgrc9160-kwd-0006">photoacclimation</keyword></keywordGroup><supportingInformation></supportingInformation><abstractGroup><abstract type="main"><p xml:id="jgrc9160-para-0001" label="1">The relationship between phytoplankton distribution and dynamics, and the resident water masses in the Ionian Sea was investigated in the spring of 1999 by flow cytometry, HPLC, microscopy, <sup>14</sup>C incorporation, and serial dilutions. More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). <i>Synechococcus</i> sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of <i>Synechococcus</i> sp. and <i>Prochlorococcus</i> sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (<i>P</i>/<i>B</i> of 11.40 mg C mg chl<sup>−1</sup> h<sup>−1</sup>). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (<i>P</i>/<i>B</i> of 20.47 mg C mg chl<sup>−1</sup> h<sup>−1</sup>) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chl<i>a</i>, and productivity (208.0 mg C m<sup>−2</sup> d<sup>−1</sup>), but also the most variable in terms of mesoscale features. Growth of <i>Synechococcus</i> sp. and <i>Prochlorococcus</i> sp. was slow (0.36 d<sup>−1</sup> at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d<sup>−1</sup>) Picoeukaryote growth was tightly coupled with grazing (0.80 d<sup>−1</sup>), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>PHYTOPLANKTON OF THE IONIAN SEA</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean)</title></titleInfo><name type="personal"><namePart type="given">R.</namePart><namePart type="family">Casotti</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><affiliation>E-mail: raffa@szn.it</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A.</namePart><namePart type="family">Landolfi</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><affiliation>Now at School of Ocean and Earth Science, University of Southampton, Southampton Oceanography Centre, Southampton, UK.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">C.</namePart><namePart type="family">Brunet</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">F.</namePart><namePart type="family">D'Ortenzio</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">O.</namePart><namePart type="family">Mangoni</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><affiliation>Now at University of Naples “Federico II”, Dipartimento di Zoologia, Naples, Italy.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Ribera d'Alcalà</namePart><affiliation>Stazione Zoologica “A. Dohrn” di Napoli, Naples, Italy</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Denis</namePart><affiliation>Laboratoire d'Océanographie et de Biogéochimie, Marseille, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2003-09</dateIssued><dateCaptured encoding="w3cdtf">2002-07-16</dateCaptured><dateValid encoding="w3cdtf">2003-02-19</dateValid><edition>Casotti, R., A. Landolfi, C. Brunet, F. D'Ortenzio, O. Mangoni, M. Ribera d'Alcalà, and M. Denis (2003), Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean), J. Geophys. Res., 108, 8116, doi:10.1029/2002JC001541, C9.</edition><copyrightDate encoding="w3cdtf">2003</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">7</extent><extent unit="tables">5</extent></physicalDescription><abstract>The relationship between phytoplankton distribution and dynamics, and the resident water masses in the Ionian Sea was investigated in the spring of 1999 by flow cytometry, HPLC, microscopy, 14C incorporation, and serial dilutions. More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area (“Italian Side”) was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl−1 h−1). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area (“Greek Side,” GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl−1 h−1) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m−2 d−1), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d−1 at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d−1) Picoeukaryote growth was tightly coupled with grazing (0.80 d−1), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.</abstract><subject><genre>keywords</genre><topic>ultraplankton</topic><topic>flow cytometry</topic><topic>primary productivity</topic><topic>Mediterranean Sea</topic><topic>mixing</topic><topic>photoacclimation</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Geophysical Research: Oceans</title></titleInfo><titleInfo type="abbreviated"><title>J. Geophys. Res.</title></titleInfo><genre type="journal">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/specialSection/PBEMD1">Physical and Biochemical Evolution of the Eastern Mediterranean in the 1990s (PBE)</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0439">Ecosystems, structure and dynamics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0491">Food webs and trophodynamics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4815">Ecosystems, structure, dynamics, and modeling</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4817">Food webs, structure, and dynamics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4855">Phytoplankton</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4890">Zooplankton</topic></subject><identifier type="ISSN">0148-0227</identifier><identifier type="eISSN">2156-2202</identifier><identifier type="DOI">10.1002/(ISSN)2156-2202c</identifier><identifier type="CODEN">JGREA2</identifier><identifier type="PublisherID">JGRC</identifier><part><date>2003</date><detail type="volume"><caption>vol.</caption><number>108</number></detail><detail type="issue"><caption>no.</caption><number>C9</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>19</total></extent></part></relatedItem><identifier type="istex">A9C4BCDB45BAA02633B67A45CB0251FC2509E354</identifier><identifier type="DOI">10.1029/2002JC001541</identifier><identifier type="ArticleID">2002JC001541</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2003 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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