<?xml version="1.0" encoding="UTF-8" standalone="no"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v2.3 20070202//EN" "journalpublishing.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Mar. Sci.</journal-id>
<journal-title>Frontiers in Marine Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Mar. Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-7745</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.3389/fmars.2016.00156</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Marine Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Phytoplankton Virus Production Negatively Affected by Iron Limitation</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name><surname>Slagter</surname> <given-names>Hans A.</given-names></name>
<xref ref-type="aff" rid="aff1"><sup>1</sup></xref>
<xref ref-type="author-notes" rid="fn001"><sup>&#x0002A;</sup></xref>
<uri xlink:href="http://loop.frontiersin.org/people/337735/overview"/>
</contrib>
<contrib contrib-type="author">
<name><surname>Gerringa</surname> <given-names>Loes J. A.</given-names></name>
<xref ref-type="aff" rid="aff1"><sup>1</sup></xref>
<uri xlink:href="http://loop.frontiersin.org/people/236549/overview"/>
</contrib>
<contrib contrib-type="author">
<name><surname>Brussaard</surname> <given-names>Corina P. D.</given-names></name>
<xref ref-type="aff" rid="aff2"><sup>2</sup></xref>
<uri xlink:href="http://loop.frontiersin.org/people/329672/overview"/>
</contrib>
</contrib-group>
<aff id="aff1"><sup>1</sup><institution>Department of Ocean Systems, NIOZ Royal Institute for Sea Research, Utrecht University</institution> <country>Den Burg, Netherlands</country></aff>
<aff id="aff2"><sup>2</sup><institution>Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Institute for Sea Research, Utrecht University</institution> <country>Den Burg, Netherlands</country></aff>
<author-notes>
<fn fn-type="edited-by"><p>Edited by: Sylvia Gertrud Sander, University of Otago, New Zealand</p></fn>
<fn fn-type="edited-by"><p>Reviewed by: Jessica Nicole Fitzsimmons, Texas A&#x00026;M University, USA; Aridane G. Gonzalez, University of Western Brittany, France</p></fn>
<fn fn-type="corresp" id="fn001"><p>&#x0002A;Correspondence: Hans A. Slagter <email>hans.slagter&#x00040;nioz.nl</email></p></fn>
<fn fn-type="other" id="fn002"><p>This article was submitted to Marine Biogeochemistry, a section of the journal Frontiers in Marine Science</p></fn>
</author-notes>
<pub-date pub-type="epub">
<day>30</day>
<month>08</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="collection">
<year>2016</year>
</pub-date>
<volume>3</volume>
<elocation-id>156</elocation-id>
<history>
<date date-type="received">
<day>29</day>
<month>03</month>
<year>2016</year>
</date>
<date date-type="accepted">
<day>16</day>
<month>08</month>
<year>2016</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#x000A9; 2016 Slagter, Gerringa and Brussaard.</copyright-statement>
<copyright-year>2016</copyright-year>
<copyright-holder>Slagter, Gerringa and Brussaard</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/"><p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p></license>
</permissions>
<abstract><p>Fe-limited monocultures of the ubiquitous algae <italic>Micromonas pusilla</italic> and <italic>Phaeocystis globosa</italic> were infected with their respective viruses (MpV and PgV) to ascertain the effect of Fe-limitation on phytoplankton host-virus dynamics. The effect of the viral shunt on Fe concentrations and bioavailability is starting to gain attention, since not only is Fe released through lysis, but also its solubility is increased by the simultaneous release of Fe-binding dissolved organic ligands. However, the effect of Fe-limitation on the process of viral lysis itself is poorly understood. In this study fine adjustment of a seawater-based culture medium including the use of ultra-clean trace metal conditions and protocols allowed for Fe-limited growth at nanomolar amounts as opposed to micromolar amounts typically employed in culturing. Viral lysates derived from Fe-limited and Fe-replete (for comparison) hosts were cross-inoculated in hosts of both Fe treatments, to judge the quality of the resulting lysate as well as the effect of Fe introduction after initial infection. For both phytoplankton host-virus systems, the virus burst size reduced strongly under Fe stress, i.e., on average 28 &#x000B1; 1% of replete. Moreover, the MpV virus progeny showed highly reduced infectivity of 30 &#x000B1; 7%, whereas PgV infectivity was not affected. A small addition of Fe to Fe-limited cultures coming from the Fe-replete lysate counteracted the negative effect of Fe-limitation on phytoplankton virus production to some extent (but still half of replete), implying that the physiological history of the host at the moment of infection was an important underlying factor. These results indicate that Fe-limitation has the strong potential to reduce the loss of phytoplankton due to virus infection, thereby affecting the extent of Fe-cycling through the viral shunt. To what extent this affects the contribution of viral lysis-induced organic ligand release needs further study.</p></abstract>
<kwd-group>
<kwd>algae</kwd>
<kwd>marine phytoplankton</kwd>
<kwd>marine viruses</kwd>
<kwd>iron</kwd>
<kwd>Fe speciation</kwd>
<kwd>Fe limitation</kwd>
</kwd-group>
<contract-num rid="cn001">822.01.018</contract-num>
<contract-num rid="cn002">311975</contract-num>
<contract-sponsor id="cn001">Nederlandse Organisatie voor Wetenschappelijk Onderzoek<named-content content-type="fundref-id">10.13039/501100003246</named-content></contract-sponsor>
<contract-sponsor id="cn002">Seventh Framework Programme<named-content content-type="fundref-id">10.13039/501100004963</named-content></contract-sponsor>
<counts>
<fig-count count="2"/>
<table-count count="3"/>
<equation-count count="0"/>
<ref-count count="77"/>
<page-count count="11"/>
<word-count count="8530"/>
</counts>
</article-meta>
</front>
<body>
<sec sec-type="intro" id="s1">
<title>Introduction</title>
<p>Phytoplankton form the base of most marine pelagic food webs and are important in sequestering atmospheric carbon dioxide (CO<sub>2</sub>) through photosynthesis. The production of phytoplankton is controlled by physicochemical variables (bottom-up) as well as by biological factors (top-down). Main bottom-up controls of phytoplankton are light and nutrient availability (Behrenfeld et al., <xref ref-type="bibr" rid="B6">2006</xref>). The latter can be subdivided into major (nitrate, phosphate, and silicate) and micro-nutrients (e.g., iron; de Baar et al., <xref ref-type="bibr" rid="B19">1990</xref>; Martin et al., <xref ref-type="bibr" rid="B41">1990</xref>). Top-down factors, e.g., grazing and viral infection, influence the organic matter flux differently (Wilhelm and Suttle, <xref ref-type="bibr" rid="B75">1999</xref>; Weitz and Wilhelm, <xref ref-type="bibr" rid="B74">2012</xref>). While grazing transfers photosynthetically fixed carbon and organic nutrients up the food chain (Calbet and Landry, <xref ref-type="bibr" rid="B17">2004</xref>), viral lysis results in the release of the hosts&#x00027; cellular content into the surrounding water (Gobler et al., <xref ref-type="bibr" rid="B27">1997</xref>; Wilhelm and Suttle, <xref ref-type="bibr" rid="B75">1999</xref>). Thereupon, the flow of nutrients through the microbial food web is stimulated by bacterial recycling of the dissolved and dead particulate matter (Brussaard et al., <xref ref-type="bibr" rid="B12">2005</xref>; Suttle, <xref ref-type="bibr" rid="B64">2005</xref>; Brussaard and Mart&#x000ED;nez, <xref ref-type="bibr" rid="B13">2008</xref>). Virally-induced mortality of various different natural phytoplankton groups was found to be at least an equally important loss factor as microzooplankton grazing (Baudoux et al., <xref ref-type="bibr" rid="B4">2007</xref>; Mojica et al., <xref ref-type="bibr" rid="B48">2016</xref>).</p>
<p>In order to understand and predict changes in phytoplankton community composition, it is important to elucidate how bottom-up and top-down factors interact and affect phytoplankton population dynamics. Several studies using phytoplankton host-virus culture systems showed that major nutrient availability influences viral production (Maat and Brussaard, <xref ref-type="bibr" rid="B37">2016</xref> and see review by Mojica and Brussaard, <xref ref-type="bibr" rid="B47">2014</xref>). For example, phosphorus (P) limitation of the virally infected phytoplankton host results in a prolonged latent period, i.e., the time between infection and the initial release of progeny viruses from the host cell, for the infecting viruses (Maat et al., <xref ref-type="bibr" rid="B38">2014</xref>). Moreover, P-stress resulted in reduced viral burst size, i.e., the number of newly formed viruses released per lysed host cell (Bratbak et al., <xref ref-type="bibr" rid="B9">1998</xref>; Maat et al., <xref ref-type="bibr" rid="B38">2014</xref>). These studies proposed shortage of phosphorus as a viral production substrate as well as possible host energy deficiency as reasons for the lower and delayed viral particle yield. There is, however, virtually nothing known on the effect of micronutrient limitation on phytoplankton host-virus interactions.</p>
<p>Furthermore, as iron (Fe) solubility in seawater is low (Millero, <xref ref-type="bibr" rid="B46">1998</xref>; Liu and Millero, <xref ref-type="bibr" rid="B36">2002</xref>), marine phytoplankton depend on Fe-binding ligands to increase solubility and therefore bioavailability (Gledhill and van den Berg, <xref ref-type="bibr" rid="B26">1994</xref>; Rue and Bruland, <xref ref-type="bibr" rid="B59">1995</xref>). The redox state of Fe is an important factor in Fe bioavailability. The oxidized Fe(III) state is the more stable and thus prevalent state in marine conditions, while the reduced Fe(II) state is the more bioavailable (Breitbarth et al., <xref ref-type="bibr" rid="B10">2010</xref>; Shaked and Lis, <xref ref-type="bibr" rid="B61">2012</xref>). Release of reactive oxygen species during phytoplankton growth has been shown to contribute to bioavailability of Fe by facilitating reduction of Fe(III) (Kustka et al., <xref ref-type="bibr" rid="B34">2005</xref>; Garg et al., <xref ref-type="bibr" rid="B20">2007</xref>). Furthermore, organic exudates have been connected to lowered Fe(II) oxidation rates experimentally (Gonz&#x000E1;lez et al., <xref ref-type="bibr" rid="B29">2014</xref>). Part of the Fe-binding ligand pool is thought to be of marine biological origin. Strong Fe-binding organic ligands called siderophores are purposefully produced by bacteria (Butler, <xref ref-type="bibr" rid="B16">2005</xref>; Mawji et al., <xref ref-type="bibr" rid="B44">2011</xref>). Humic acids and polysaccharide excretions are other recognized Fe chelators with a biological origin (Hassler et al., <xref ref-type="bibr" rid="B31">2011</xref>; Laglera et al., <xref ref-type="bibr" rid="B35">2011</xref>). The highest Fe-binding ligand concentrations generally correlate with biological activity (Rue and Bruland, <xref ref-type="bibr" rid="B59">1995</xref>; Gerringa et al., <xref ref-type="bibr" rid="B25">2006</xref>; Ibisanmi et al., <xref ref-type="bibr" rid="B32">2011</xref>). Viral lysis, releasing organic substances in seawater, may well be an important contributor to the ligand pool (Gobler et al., <xref ref-type="bibr" rid="B27">1997</xref>; Poorvin et al., <xref ref-type="bibr" rid="B54">2004</xref>, <xref ref-type="bibr" rid="B55">2011</xref>). In these studies by Poorvin and others, it was found that bacterial and cyanobacterial lysates provided organically bound Fe in a form more bioavailable than supplied inorganic, ethylenediaminetetraacetic acid (EDTA) bound or desferrioxamine B (DFB) bound Fe. In comparison to the studied bacteria&#x00027;s self-produced siderophores, lysates were also found to contain more bioavailable Fe.</p>
<p>Fe-limitation negatively affects phytoplankton physiology and growth (de Baar et al., <xref ref-type="bibr" rid="B19">1990</xref>; Martin et al., <xref ref-type="bibr" rid="B41">1990</xref>; Behrenfeld et al., <xref ref-type="bibr" rid="B5">1996</xref>; Timmermans et al., <xref ref-type="bibr" rid="B66">2001b</xref>). Besides energetic consequences of Fe-limitation in terms of the cell&#x00027;s ability to harvest light energy (Geider and La Roche, <xref ref-type="bibr" rid="B21">1994</xref>), Fe is also found to be an essential micronutrient for DNA replication (Netz et al., <xref ref-type="bibr" rid="B50">2012</xref>; Zhang, <xref ref-type="bibr" rid="B77">2014</xref>). As parasites viruses are dependent on the metabolism of their host for the production of their progeny. We hypothesize that viral production depends on the degree of Fe-stress of the host. Viral lysis in turn affects the production of Fe-binding organic ligands and thus the solubility of the limiting Fe. Thus far, in terms of impact on Fe cycling, studies focussed solely on the release of Fe or Fe-binding organic ligands upon viral lysis and not on the virus growth cycle (Gobler et al., <xref ref-type="bibr" rid="B27">1997</xref>; Poorvin et al., <xref ref-type="bibr" rid="B54">2004</xref>, <xref ref-type="bibr" rid="B55">2011</xref>). Here we examine virus production characteristics under Fe-limitation for two key ecologically relevant phytoplankton hosts: the nanoeukaryotic bloom-forming Prymnesiophyte <italic>Phaeocystis globosa</italic> and the picoeukaryotic Prasinophyte <italic>Micromonas pusilla</italic>. <italic>Phaeocystis</italic> is a globally occurring, bloom-forming genus (Vaulot et al., <xref ref-type="bibr" rid="B72">1994</xref>), with <italic>P. globosa</italic> ecologically relevant in temperate marine waters (Schoemann et al., <xref ref-type="bibr" rid="B60">2005</xref>). Viruses have been found to drive <italic>P. globosa</italic> bloom decline (Brussaard, <xref ref-type="bibr" rid="B11">2004</xref>; Brussaard et al., <xref ref-type="bibr" rid="B12">2005</xref>; Baudoux et al., <xref ref-type="bibr" rid="B3">2006</xref>). <italic>M. pusilla</italic> is a common species that is distributed globally (Not et al., <xref ref-type="bibr" rid="B51">2004</xref>, <xref ref-type="bibr" rid="B52">2005</xref>; Vaulot et al., <xref ref-type="bibr" rid="B73">2008</xref>). It has been speculated that viral control of this species is continuous (Cottrell and Suttle, <xref ref-type="bibr" rid="B18">1995</xref>). As model species for diverse regions and ecological niches, these species were chosen in this study to offer a broad insight in the response to Fe-limitation of phytoplankton host-virus systems in world oceans subject to changing conditions. Limiting concentrations were of ecological relevance to represent a natural context.</p>
</sec>
<sec sec-type="methods" id="s2">
<title>Methods</title>
<sec>
<title>Materials preparation</title>
<p>Cleaning of equipment and preparation of chemicals took place in a class 100 ultra-clean laboratory environment (Interflow). Culture handling and sampling were carried out in a 15&#x000B0;C climate chamber within the ultra-clean laboratory. When outside the ultra-clean environment, sample handling took place inside class 100 laminar flow hoods (Interflow). All rinsing and chemical dissolution and dilution was done using 18 M&#x003A9; deionized Milli-Q water (Merck Millipore), further referred to as MQ.</p>
<p>Prior to use, general labware of high- and low-density polyethylene (HDPE and LDPE, respectively) and fluorinated ethylene propylene (FEP) was cleaned thoroughly by pre-rinsing (5x) with MQ, followed by soaking in 6 M hydrochloric acid (HCl) for a minimum of 24 h, and a final thorough (5x) MQ rinsing. A sub-boiling quartz distillation apparatus (Savillex) was used to purify nitric acid (HNO<sub>3</sub>) in triplicate, yielding Fe free quartz distilled (3QD) HNO<sub>3</sub>. A 0.3 M 3QD-HNO<sub>3</sub> solution is used to fill stored bottles.</p>
<p>The polycarbonate (PC) culture flasks (50&#x02013;500 mL, VWR) and bottles (1&#x02013;2 L, Nalgene) were acid cleaned with 1 M HCl for a minimum of 24 h, after which they were rinsed with MQ (5x). Finally, bottles were sterilized with a 10% volume of boiling MQ, i.e., the bottle with MQ was microwaved at 900 W to boiling point and left boiling for &#x0007E;20 s. After vigorous shaking the hot MQ was poured out over the inverted lid. Culture vessels were then left to air-dry in a laminar flow bench for at least 2 h.</p>
</sec>
<sec>
<title>Culturing</title>
<p>Axenic cultures of the nanoeukaryotic Prymnesiophyte <italic>P. globosa</italic> G(A) (culture collection of the University of Groningen, the Netherlands) and the picoeukaryotic Prasinophyte <italic>M. pusilla</italic> LAC38 (Marine Research Center culture collection, G&#x000F6;teborg University, Sweden) were maintained under trace metal clean conditions.</p>
<p>A low Fe-containing medium (Low Trace: LT) based on natural seawater (DFe 0.2 nM, collected west of the Bay of Biscay, Atlantic Ocean after Rijkenberg et al., <xref ref-type="bibr" rid="B57">2012</xref>) was designed without metal chelators such as EDTA. Chelators as EDTA are used as metal buffers in culture media, and are added in 10<sup>&#x02212;6</sup>&#x02013;10<sup>&#x02212;3</sup> M concentrations to ascertain that those transition metals added as micronutrients, e.g., Cu, Co, Fe, Mn, Mo, Ni, V, Zn, are kept in the dissolved phase through complexation by EDTA (Sunda and Huntsman, <xref ref-type="bibr" rid="B62">1995</xref>). However, these high concentrations of artificial ligands completely overrule the natural chemistry of the metals, making the study of natural Fe binding organic ligands impossible (Gerringa et al., <xref ref-type="bibr" rid="B24">2000</xref>). The medium was enriched with the macronutrients NaNO<sub>3</sub> (Sigma-Aldrich) and Na<sub>2</sub>HPO<sub>4</sub> (Merck Millipore) to final concentrations of 128 and 8 &#x003BC;M, respectively. The following micronutrients were added: KBr (7.1 &#x003BC;M final concentration), NaF (3.0 &#x003BC;M), CaCl<sub>2</sub>&#x000B7;2H<sub>2</sub>O, (17.9 &#x003BC;M), SrCl<sub>2</sub>&#x000B7;6H<sub>2</sub>O (0.8 &#x003BC;M), MgCl<sub>2</sub>&#x000B7;6H<sub>2</sub>O (2.3 &#x003BC;M) and Na<sub>2</sub>SeO<sub>3</sub> (10.0 nM). Vitamins H, B1, and B12 were added to final concentrations of 2.0, 296.0, and 0.4 nM, respectively. A combined Tris(hydroxymethyl) aminomethane (Tris) and HCl buffer was added to a 4.0 &#x003BC;M final concentration. Nutrient and buffer stock solutions were cleaned of trace metal contaminations by equilibration with MnO<sub>2</sub> after van den Berg and Kramer (<xref ref-type="bibr" rid="B68">1979</xref>). The MnO<sub>2</sub> was removed using a trace metal clean 47 mm diameter 0.2 &#x003BC;m pore size PC filter (Whatman) in a polysulfone (PSU) filter tower (Nalgene) with an electric vacuum pump (Merck Millipore). This cleaning process was performed twice. To maintain constant growth for multiple generations addition of additional trace metals proved essential. These trace metal additions were kept to a minimum in order to avoid influencing Fe speciation, e.g., interactions between Cu and Fe (Gonz&#x000E1;lez et al., <xref ref-type="bibr" rid="B28">2016</xref>). <italic>P. globosa</italic> received an additional trace solution containing final concentrations of 2.0 nM ZnSO<sub>4</sub>&#x000B7;7H<sub>2</sub>O, 1.0 nM CoCl<sub>2</sub>&#x000B7;6H<sub>2</sub>O, 4.6 nM MnCl<sub>2</sub>&#x000B7;4H<sub>2</sub>O, and 0.6 nM Na<sub>2</sub>MoO<sub>4</sub>&#x000B7;2H<sub>2</sub>O. <italic>M. pusilla</italic> showed poor physiological condition and growth using this trace solution. Because it was impossible to maintain as steady state under these conditions, a slightly different trace solution was used, containing final concentrations of 4.0 nM ZnSO<sub>4</sub>&#x000B7;7H<sub>2</sub>O, 5.0 nM CoCl<sub>2</sub>&#x000B7;6H<sub>2</sub>O, 1.0 nM CuSO<sub>4</sub>&#x000B7;5H<sub>2</sub>O, 1.0 nM NiSO<sub>4</sub>&#x000B7;6H<sub>2</sub>O, 1.0 nM Na<sub>3</sub>VO<sub>4</sub>, 1.0 nM K<sub>2</sub>CrO<sub>4</sub>, 9.1 nM MnCl<sub>2</sub>&#x000B7;4H<sub>2</sub>O, 4.1 nM Na<sub>2</sub>MoO<sub>4</sub>&#x000B7;2H<sub>2</sub>O, and 1.0 nM H<sub>2</sub>SeO<sub>3</sub>. Fe was added from an acidified 3 &#x003BC;M FeCl stock solution made using a 1000 mg L<sup>&#x02212;1</sup> ICP stock (Fluka, Sigma-Aldrich). The Fe-limiting medium contained final concentrations of 1.0 and 3.0 nM Fe for <italic>P. globosa</italic> and <italic>M. pusilla</italic>, respectively. In comparison, the Fe-replete (control) medium contained 9.0 &#x003BC;M FeCl for both species.</p>
<p>Culture temperature was 15&#x000B0;C and irradiance was supplied at 90 &#x003BC;mol quanta m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup> under a 16:8 h light:dark cycle. Phytoplankton cultures were maintained semi-continuously to obtain and sustain constant and comparable physiology and growth, i.e., diluting the culture daily with new medium whereby the exact volume was determined by the maximum growth rate possible under Fe-limiting culture conditions without wash-out (Maat et al., <xref ref-type="bibr" rid="B38">2014</xref>). The limiting Fe concentration determined the maximum cell abundance, which was determined before and after dilution using flow cytometry (Marie et al., <xref ref-type="bibr" rid="B40">1999</xref>). At steady state, i.e., after at least 8 volume changes and consistent phytoplankton counts (2.1 &#x000B1; 0.4 &#x000D7; 10<sup>6</sup> and 2.1 &#x000B1; 0.7 &#x000D7; 10<sup>6</sup> for <italic>P. globosa</italic> and <italic>M. pusilla</italic>, respectively), samples were collected for dissolved macronutrients (nitrogen and phosphorus) and Fe, as well as pigment composition. Nutrient samples (5 ml after washing of filter and tube) were 0.2 &#x003BC;m filtered (25 mm diameter Acrodisk, Pall) and frozen at &#x02212;20&#x000B0;C until analysis. GF/C filtered (1.2 &#x003BC;m nominal pore size, 25 mm diameter, Whatman) algal pigment samples of 50 mL were frozen at &#x02212;80&#x000B0;C until analysis.</p>
<p>Axenic viral lysate of the double-stranded DNA viruses PgV-07T (Baudoux and Brussaard, <xref ref-type="bibr" rid="B2">2005</xref>) infecting <italic>P. globosa</italic> G(A) and MpV-08T (Mart&#x000ED;nez et al., <xref ref-type="bibr" rid="B43">2014</xref>) infecting <italic>M. pusilla</italic> LAC38 were obtained by 10% v/v inoculation to exponentially growing phytoplankton host and checked for full lysis by flow cytometry (FCM). Fe-limited lysates of both phytoplankton viruses were initiated by 1% v/v inoculations with Fe-replete lysates, after which a minimum of 5 subsequent 10% v/v inoculations followed before use for the experiment. This way the Fe concentration in the Fe-limited lysate was similar to the Fe concentration in the Fe-limited host culture. The number of infective phytoplankton viruses was determined using the most probable number (MPN) endpoint dilution assay according to Suttle (<xref ref-type="bibr" rid="B63">1993</xref>). MPN data was analyzed using the University of British Columbia Computer Science department&#x00027;s Assay Analyser software program (Passmore et al., <xref ref-type="bibr" rid="B53">2000</xref>).</p>
</sec>
<sec>
<title>Experimental design</title>
<p>Steady state exponentially growing phytoplankton cultures were subdivided per treatment (Fe-limited and Fe-replete) in 6 replicate 500 mL culture flasks. Two days later the viral infection experiment started 3 h into the light period. For each treatment, 2 replicate cultures received viruses produced on Fe-limited host culture (VL), 2 replicates received viruses produced on Fe-replete host culture (VR), and 2 replicates did not receive viruses and served as non-infected controls (C). Fe-limited lysates were added not only to the respective Fe-limited host cultures, but also to the Fe-replete host in order to test for the reduced infectivity we observed under Fe-limitation (See Results). For this reason and to still guarantee a one-step infection cycle we aimed to add 20&#x02013;25 viruses per algal cell for <italic>P. globosa</italic>. Given lower yields for <italic>M. pusilla</italic>, we endeavored to add at least 5&#x02013;10 viruses per algal cell, while still maintaining a &#x0007E;10% v/v addition. Similarly, Fe-replete lysate was also added to Fe-limited host cultures. This caused a Fe-spike of about 0.9 &#x003BC;M (10% v/v of Fe-replete medium containing lysate), which allows testing whether a spike of Fe influences virus proliferation.</p>
<p>The moment viruses were added, cultures were maintained in-batch. We examined the effect of frequent handling by taking along a control subculture per Fe-limited treatment that was only gently mixed once a day. Samples for phytoplankton and virus abundance as well as photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub>) were taken every 4 h until full lysis of the cultures (48 h for <italic>P. globosa</italic> and 96 h for <italic>M. pusilla</italic>). Phytoplankton abundance and F<sub>v</sub>/F<sub>m</sub> were determined directly upon sampling, while viral abundance samples were fixed with glutaraldehyde (EM-grade, 0.5% final concentration), flash frozen in liquid nitrogen and stored at &#x02212;80&#x000B0;C (Brussaard et al., <xref ref-type="bibr" rid="B14">2010</xref>).</p>
</sec>
<sec>
<title>Analyses</title>
<p>High Performance Liquid Chromatography (HPLC) pigment analysis was performed on steady state phytoplankton samples after Zapata et al. (<xref ref-type="bibr" rid="B76">2000</xref>). Phytoplankton cells in fresh samples were discriminated and counted based on Chlorophyll-a red autofluorescence using a FACSCanto flow cytometer (Becton Dickinson) equipped with a 17 mW 633 nm HeNe red laser. Viral abundances were also determined by flow cytometry using a FACSCalibur flow cytometer (Becton Dickinson) equipped with a 15 mW 488 nm argon-ion blue laser triggered on green fluorescence, following the protocol by Brussaard et al. (<xref ref-type="bibr" rid="B14">2010</xref>). In short, samples were diluted 200&#x02013;1000-fold using a 2 M Tris-HCl buffer at pH 8 and viruses were stained using the nucleic acid-specific fluorescent dye SYBR Green I (Molecular Probes&#x000AE;, Life Technologies, Thermo Fisher). Raw data were analyzed using Cytowin (Vaulot, <xref ref-type="bibr" rid="B71">1989</xref>; Version 4.31 available at <ext-link ext-link-type="uri" xlink:href="http://application.sb-roscoff.fr/Phyto/index.php">http://application.sb-roscoff.fr/Phyto/index.php</ext-link>), whereby PgV and MpV were easily discriminated by plotting green nucleic acid-specific fluorescence vs. side scatter (Baudoux and Brussaard, <xref ref-type="bibr" rid="B2">2005</xref>; Mart&#x000ED;nez et al., <xref ref-type="bibr" rid="B42">2015</xref>).</p>
<p>The number of infective phytoplankton viruses was determined using the endpoint dilution assay according to Suttle (<xref ref-type="bibr" rid="B63">1993</xref>). In short, 10-fold dilution series were set up in 5 replicate tubes using a dilute Fe-replete phytoplankton culture at a density of &#x0007E;10<sup>6</sup> cells mL<sup>&#x02212;1</sup>. A row of uninfected control tubes was added to each analysis. Cell lysis was regularly scored by eye and the final score after 14 days post-infection was used to calculate the number of infectious viruses. Dividing this number of infectious by the total number of PgV or MpV provided the % infectious viruses.</p>
<p>Photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub>) measurements were performed using a Chlorophyll Fluorometer with a red emitter-detector unit (Water-PAM, Waltz). Samples were kept in the dark for 30 min at culturing temperature, after which chlorophyll autofluorescence was measured in duplicate in the dark adapted state (F<sub>0</sub>) and after a saturation pulse of 2.5 s (F<sub>m</sub>). F<sub>v</sub> is defined as the difference between F<sub>m</sub> and F<sub>0</sub> (Genty et al., <xref ref-type="bibr" rid="B23">1989</xref>). Concentrations of dissolved inorganic macronutrients nitrate and orthophosphate were verified colorimetrically using a trAAcs 800 auto analyser (Murphy and Riley, <xref ref-type="bibr" rid="B49">1962</xref>; Grasshoff, <xref ref-type="bibr" rid="B30">1983</xref>), and were non-limiting at all times (&#x0003E;128 &#x003BC;M nitrate and &#x0003E;8 &#x003BC;M phosphate). Verification of the dissolved Fe concentration was done using flow injection analysis after Klunder et al. (<xref ref-type="bibr" rid="B33">2011</xref>), the detection limit of this method was 0.01 nM.</p>
</sec>
</sec>
<sec id="s3">
<title>Results and discussion</title>
<sec>
<title>Steady state</title>
<p>Exponential growth rate (&#x003BC;<sub>max</sub>) for both Fe-limited and Fe-replete <italic>P. globosa</italic> and Fe-replete <italic>M. pusilla</italic> was 0.99 &#x000B1; 0.11 d<sup>&#x02212;1</sup>. <italic>M. pusilla</italic> showed, however, reduced growth under Fe-limitation (0.63 &#x000B1; 0.07 d<sup>&#x02212;1</sup>). Initial difficulties encountered with consistent semi-continuous culturing of <italic>M. pusilla</italic> required us to increase the Fe concentration to 3 nM as compared to the 1 nM for <italic>P. globosa.</italic> Still, the lower steady state &#x003BC;<sub>max</sub> found for <italic>M. pusilla</italic> under Fe-limitation suggests a less efficient Fe-uptake or utilization of <italic>M. pusilla</italic> as compared to <italic>P. globosa</italic>. However, the photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub>) of the Fe-limited <italic>M. pusilla</italic> remained high around 0.6. Thus, the smaller-sized <italic>M. pusilla</italic> requires more Fe to grow, albeit at a lower &#x003BC;<sub>max</sub>, while it is capable of retaining F<sub>v</sub>/F<sub>m</sub> at a value similar to Fe-replete conditions. Reduced F<sub>v</sub>/F<sub>m</sub> and growth rate under Fe-limitation has been reported for a small diatom species (Timmermans et al., <xref ref-type="bibr" rid="B65">2001a</xref>); however, both variables were reduced for the same species and not one or the other as found in present study. Our result do not support the earlier reports that small phytoplankton (diatoms and cyanobacteria) are growing better under Fe-limitation than larger phytoplankton (Price et al., <xref ref-type="bibr" rid="B56">1994</xref>; Timmermans et al., <xref ref-type="bibr" rid="B66">2001b</xref>, <xref ref-type="bibr" rid="B67">2004</xref>). Whether the differences are due to species-specific or phytoplankton group related responses is currently unclear.</p>
<p>The cellular Chlorophyll-a concentration at steady state was lower under Fe-limitation compared to the Fe-replete control cultures for both algal species (Tables <xref ref-type="table" rid="T1">1</xref>, <xref ref-type="table" rid="T2">2</xref>). For <italic>M. pusilla</italic> the reduction was larger, i.e., Chlorophyll-a concentration was only 40% of Fe-replete concentration, compared to 63% for <italic>P. globosa</italic>. In the Fe-limited <italic>P. globosa</italic> cultures, cellular Chlorophyll-c concentration was reduced (to a similar extent; Table <xref ref-type="table" rid="T1">1</xref>), whereas for <italic>M. pusilla</italic> the Chlorophyll-b concentration also decreased compared to Fe-replete (Table <xref ref-type="table" rid="T2">2</xref>). Furthermore, Fe-limitation led to a different distribution of light-harvesting xanthophylls in <italic>P. globosa</italic> (Table <xref ref-type="table" rid="T1">1</xref>). Cellular 19&#x00027;-hexafucoxanthin concentration was found 5-fold higher in the Fe-limited cultures as compared to Fe-replete <italic>P. globosa</italic> (4.8 &#x000D7; 10<sup>&#x02212;12</sup> g cell<sup>&#x02212;1</sup>), while 19&#x02032;-butanoyloxyfucoxanthin and fucoxanthin concentrations were 0 and 89% of Fe-replete, respectively. The photoprotective xanthophyll derivatives in Fe-limited <italic>P. globosa</italic> are increased relative to Chlorophyll-a, i.e., the diadinoxanthin concentration over Chlorophyll-a is 162% of Fe-replete (0.58 and 0.57 &#x000D7; 10<sup>&#x02212;11</sup> g &#x000D7; cell <sup>&#x02212;1</sup>, respectively) and the diatoxanthin concentration is 181% of Fe-replete (0.08 and 0.07 &#x000D7; 10<sup>&#x02212;11</sup> g &#x000D7; cell<sup>&#x02212;1</sup>, respectively). Fe-limited <italic>M. pusilla</italic> cultures (Table <xref ref-type="table" rid="T2">2</xref>) had lower cellular Chlorophyll-b and light-harvesting xanthophyll concentrations. Relative to the Chlorophyll-a concentration, photoprotective xanthophyll derivatives antheraxanthin, zeaxanthin, and lutein were present in higher amounts. Only violaxanthin remains lower both in absolute and relative terms.</p>
<table-wrap position="float" id="T1">
<label>Table 1</label>
<caption><p><bold>Steady state phytoplankton pigment composition in non-infected Fe-limited (first column) and Fe-replete (second column) <italic>P. globosa</italic> cultures</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>Pigments</bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>Treatment</bold></th>
</tr>
<tr>
<th/>
<th valign="top" align="center"><bold>Limited</bold></th>
<th valign="top" align="center"><bold>Replete</bold></th>
<th valign="top" align="center"><bold>Ratio</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Chlorophyll a<xref ref-type="table-fn" rid="TN1"><sup>a</sup></xref></td>
<td valign="top" align="center">1.31</td>
<td valign="top" align="center">2.08</td>
<td valign="top" align="center">0.63</td>
</tr>
<tr>
<td valign="top" align="left">Chlorophyll c2<xref ref-type="table-fn" rid="TN1"><sup>a</sup></xref></td>
<td valign="top" align="center">0.31</td>
<td valign="top" align="center">0.37</td>
<td valign="top" align="center">0.86</td>
</tr>
<tr>
<td valign="top" align="left">Chlorophyll c3<xref ref-type="table-fn" rid="TN1"><sup>a</sup></xref></td>
<td valign="top" align="center">0.23</td>
<td valign="top" align="center">0.48</td>
<td valign="top" align="center">0.47</td>
</tr>
<tr>
<td valign="top" align="left">19&#x00027;-hexafucoxanthin<xref ref-type="table-fn" rid="TN2"><sup>b</sup></xref></td>
<td valign="top" align="center">0.48</td>
<td valign="top" align="center">0.09</td>
<td valign="top" align="center">5.16</td>
</tr>
<tr>
<td valign="top" align="left">19&#x00027;-butanoyloxyfucoxanthin<xref ref-type="table-fn" rid="TN2"><sup>b</sup></xref></td>
<td valign="top" align="center">0.00</td>
<td valign="top" align="center">0.20</td>
<td valign="top" align="center">0.00</td>
</tr>
<tr>
<td valign="top" align="left">Fucoxanthin<xref ref-type="table-fn" rid="TN2"><sup>b</sup></xref></td>
<td valign="top" align="center">1.13</td>
<td valign="top" align="center">2.01</td>
<td valign="top" align="center">0.56</td>
</tr>
<tr>
<td valign="top" align="left">Diadinoxanthin<xref ref-type="table-fn" rid="TN3"><sup>c</sup></xref></td>
<td valign="top" align="center">0.58</td>
<td valign="top" align="center">0.57</td>
<td valign="top" align="center">1.02</td>
</tr>
<tr>
<td valign="top" align="left">Diatoxanthin<xref ref-type="table-fn" rid="TN3"><sup>c</sup></xref></td>
<td valign="top" align="center">0.08</td>
<td valign="top" align="center">0.07</td>
<td valign="top" align="center">1.07</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Concentrations of pigments are expressed in 10<sup>&#x02212;11</sup> g cell<sup>&#x02212;1</sup>. The third column shows the ratio of Fe-limited over Fe-replete cultures, serving to indicate relative shifts in pigment composition</italic>.</p>
<fn id="TN1">
<label>a</label>
<p><italic>Chlorophylls</italic>,</p></fn>
<fn id="TN2">
<label>b</label>
<p><italic>light harvesting xanthophyll derivatives and</italic></p></fn>
<fn id="TN3">
<label>c</label>
<p><italic>photoprotective xanthophyll derivatives are grouped together</italic>.</p></fn>
</table-wrap-foot>
</table-wrap>
<table-wrap position="float" id="T2">
<label>Table 2</label>
<caption><p><bold>Steady state phytoplankton pigment composition in non-infected Fe-limited (first column) and Fe-replete (second column) <italic>M. pusilla</italic> cultures</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>Pigments</bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>Treatment</bold></th>
</tr>
<tr>
<th/>
<th valign="top" align="center"><bold>Limited</bold></th>
<th valign="top" align="center"><bold>Replete</bold></th>
<th valign="top" align="center"><bold>Ratio</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Chlorophyll a<xref ref-type="table-fn" rid="TN4"><sup>a</sup></xref></td>
<td valign="top" align="center">2.70</td>
<td valign="top" align="center">6.78</td>
<td valign="top" align="center">0.40</td>
</tr>
<tr>
<td valign="top" align="left">Chlorophyll b<xref ref-type="table-fn" rid="TN5"><sup>b</sup></xref></td>
<td valign="top" align="center">2.06</td>
<td valign="top" align="center">4.50</td>
<td valign="top" align="center">0.46</td>
</tr>
<tr>
<td valign="top" align="left">Neoxanthin<xref ref-type="table-fn" rid="TN5"><sup>b</sup></xref></td>
<td valign="top" align="center">0.44</td>
<td valign="top" align="center">0.88</td>
<td valign="top" align="center">0.50</td>
</tr>
<tr>
<td valign="top" align="left">Prasinoxanthin<xref ref-type="table-fn" rid="TN5"><sup>b</sup></xref></td>
<td valign="top" align="center">0.71</td>
<td valign="top" align="center">1.52</td>
<td valign="top" align="center">0.47</td>
</tr>
<tr>
<td valign="top" align="left">Antheraxanthin<xref ref-type="table-fn" rid="TN6"><sup>c</sup></xref></td>
<td valign="top" align="center">0.27</td>
<td valign="top" align="center">0.12</td>
<td valign="top" align="center">2.33</td>
</tr>
<tr>
<td valign="top" align="left">Zeaxanthin<xref ref-type="table-fn" rid="TN6"><sup>c</sup></xref></td>
<td valign="top" align="center">0.17</td>
<td valign="top" align="center">0.10</td>
<td valign="top" align="center">1.75</td>
</tr>
<tr>
<td valign="top" align="left">Lutein<xref ref-type="table-fn" rid="TN6"><sup>c</sup></xref></td>
<td valign="top" align="center">0.13</td>
<td valign="top" align="center">0.29</td>
<td valign="top" align="center">0.44</td>
</tr>
<tr>
<td valign="top" align="left">Violaxanthin<xref ref-type="table-fn" rid="TN6"><sup>c</sup></xref></td>
<td valign="top" align="center">0.29</td>
<td valign="top" align="center">1.14</td>
<td valign="top" align="center">0.25</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Concentrations of pigments are expressed in 10<sup>&#x02212;11</sup> g cell<sup>&#x02212;1</sup>. The third column shows the ratio of Fe-limited over Fe-replete cultures, serving to indicate relative shifts in pigment composition</italic>.</p>
<fn id="TN4">
<label>a</label>
<p><italic>Chlorophylls</italic>,</p></fn>
<fn id="TN5">
<label>b</label>
<p><italic>light harvesting xanthophyll derivatives and</italic></p></fn>
<fn id="TN6">
<label>c</label>
<p><italic>photoprotective xanthophyll derivatives are grouped together</italic>.</p></fn>
</table-wrap-foot>
</table-wrap>
<p>Overall, the pigment analysis shows that for both phytoplankton species the photosystem shifted toward a more photoprotective character under Fe-limited conditions. The lower concentrations of chlorophyll and most light-harvesting xanthophylls furthermore indicated that the Fe-limited cells suffered a lower light-harvesting capacity. Fe is essential for all life and earlier studies showed that Fe-deficiency can lead to anemia in mammals, the dysfunction of Fe-dependent enzymes in yeast, the reduction of the amount of electron-transferring complexes and induction of chlorosis in plants, and a decrease in Fe-intensive light harvesting pigment synthesis and increased photoprotective pigments in phytoplankton (Geider et al., <xref ref-type="bibr" rid="B22">1993</xref>; Mengel, <xref ref-type="bibr" rid="B45">1994</xref>; van Leeuwe and Stefels, <xref ref-type="bibr" rid="B70">2007</xref>; van de Poll et al., <xref ref-type="bibr" rid="B69">2009</xref>; Zhang, <xref ref-type="bibr" rid="B77">2014</xref>). In line with the fact that the Fe concentrations in the Fe-limited cultures were always below the limit of detection, these results confirm that both phytoplankton cultures were indeed Fe-limited, despite that <italic>M. pusilla</italic> showed healthy F<sub>v</sub>/F<sub>m</sub>. The more pronounced shift to photoprotective pigment production relative to light-harvesting Chlorophyll-a in <italic>M. pusilla</italic> compared to <italic>P. globosa</italic> is in agreement with the strong decline in steady state <italic>M. pusilla</italic> cell abundance with Fe-limitation while F<sub>v</sub>/F<sub>m</sub> was unaffected. However, <italic>M. pusilla</italic> was unable to grow at 1 nM Fe while <italic>P. globosa</italic> grew well. Our results imply that <italic>P. globosa was</italic> more affected energetically by Fe-limitation, while <italic>M. pusilla</italic> suffered instead in overall cellular production.</p>
</sec>
<sec>
<title>Viral infection characteristics</title>
<p>Infection of both phytoplankton species resulted in one-step infection cycles with full lysis of the cultures whereas the non-infected controls grew or maintained constant cell number (Figures <xref ref-type="fig" rid="F1">1A,B</xref>, <xref ref-type="fig" rid="F2">2A,B</xref>). Cell growth in the non-infected Fe-replete cultures reflects the synchronized cell division during the dark period (Brussaard et al., <xref ref-type="bibr" rid="B15">1999</xref>). In the Fe-limited cultures growth of <italic>P. globosa</italic> halted, which was due to stress from the frequent sampling, since the Fe-limited subcultures that were sampled only once a day did show some growth (data not shown). The F<sub>v</sub>/F<sub>m</sub> of the uninfected Fe-replete phytoplankton cultures remained constant (Figures <xref ref-type="fig" rid="F1">1C,D</xref>, <xref ref-type="fig" rid="F2">2C,D</xref>), whereby the small variations observed in the Fe-replete <italic>P. globosa</italic> cultures relate to the light:dark cycle (Figure <xref ref-type="fig" rid="F1">1D</xref>). The Fe-limited non-infected control cultures showed a decline in F<sub>v</sub>/F<sub>m</sub> over time as a result of the Fe deprivation, but to a lesser extent than the infected cultures.</p>
<fig id="F1" position="float">
<label>Figure 1</label>
<caption><p><bold>Temporal dynamics of <italic>P. globosa</italic> viral infections: host cell abundance over time (h) in Fe-limited (A) and Fe-replete cultures (B); photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub>) over time (h) of Fe-limited (C) and Fe-replete cultures (D); viral abundance in Fe-limited (E) and Fe-replete (F) cultures</bold>. Circles represent non-infected controls, black triangles represent infections with Fe-replete host derived viruses (VR) and white triangles represent infections with Fe-limited host derived viruses (VL). Error bars indicate deviation of replicates (<italic>n</italic> &#x0003D; 2); when not visible they fall within the symbols. Shaded areas indicate dark periods, explaining the slight declines in F<sub>v</sub>/F<sub>m</sub> for the Fe-replete non-infected host. Furthermore, the dark period illustrates the onset of the synchronized cell division. Inlay in <bold>(E)</bold> magnifies the first 20 h post-infection.</p></caption>
<graphic xlink:href="fmars-03-00156-g0001.tif"/>
</fig>
<fig id="F2" position="float">
<label>Figure 2</label>
<caption><p><bold>Temporal dynamics of <italic>M. pusilla</italic> viral infections: host cell abundance over time (h) in Fe-limited (A) and Fe-replete cultures (B); photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub>) over time (h) of Fe-limited (C) and Fe-replete cultures (D); viral abundance in Fe-limited (E) and Fe-replete (F) cultures</bold>. Circles represent non-infected controls, black triangles represent infections with Fe-replete host derived viruses (VR) and white triangles represent infections with Fe-limited host derived viruses (VL). Error bars indicate deviation of replicates (<italic>n</italic> &#x0003D; 2); when not visible these fall within the symbols. Shaded areas indicate dark periods, explaining the slight declines in F<sub>v</sub>/F<sub>m</sub> for the Fe-replete non-infected host. Furthermore, the dark period illustrates the onset of the synchronized cell division. Inlay in <bold>(B)</bold> shows off scale host control growth, inlays in <bold>(E,F)</bold> magnify the first 20 h post-infection.</p></caption>
<graphic xlink:href="fmars-03-00156-g0002.tif"/>
</fig>
<p>When infected with the corresponding Fe-treatment virus (i.e., Fe-limited host with VL and Fe-replete host with VR), Fe-limitation resulted for the infected <italic>P. globosa</italic> in slightly delayed (about 4 h) and slower cell lysis than for the Fe-replete cultures (full lysis occurring about a day later; Figures <xref ref-type="fig" rid="F1">1A,B</xref>). F<sub>v</sub>/F<sub>m</sub> showed similar differences in temporal dynamics between the Fe-limited and Fe-replete infected cultures upon infection with these viruses (Figures <xref ref-type="fig" rid="F1">1C,D</xref>). At large, the infected <italic>M. pusilla</italic> cultures showed similar results (Figure <xref ref-type="fig" rid="F2">2</xref>). The alterations in host physiological condition in the Fe-limited cultures resulted for both phytoplankton species in slower release of virus progeny and reduced virus yield when infected with VL as compared to Fe-replete cultures (Figures <xref ref-type="fig" rid="F1">1E,F</xref>, <xref ref-type="fig" rid="F2">2E,F</xref>). The latent period, e.g., the time period to extracellular release of newly produced viruses, was however unaffected by Fe-limitation of the host. Experiments with the same strain of <italic>M. pusilla</italic> did show prolonged latent periods when under phosphorus (P) and nitrogen (N) limitation (Maat et al., <xref ref-type="bibr" rid="B38">2014</xref>; Maat and Brussaard, <xref ref-type="bibr" rid="B37">2016</xref>). These were suggested to be due to reduced substrate and host energy availability resulting from impaired photophysiology under major nutrient limitation. In our study Chlorophyll-a concentration was comparably reduced but F<sub>v</sub>/F<sub>m</sub> of Fe-limited steady state <italic>M. pusilla</italic> was not impaired. Then again, F<sub>v</sub>/F<sub>m</sub> of <italic>P. globosa</italic> cells prior to infection was reduced compared to Fe-replete, still not prolonging the latent period. We cannot be sure of the exact underlying mechanism from the here presented data, but the proliferation of DNA viruses is directly dependent on Fe due to the essential role Fe plays in the catalytic center of ribonucleotide reductase, produced early in infection to support dNTPs production needed for viral DNA synthesis (Romeo et al., <xref ref-type="bibr" rid="B58">2001</xref>). As such, it can be speculated that not the time to produce a virus is affected but instead the number of viruses that can be produced before cell lysis occurs. The burst size of MpV and PgV indeed decreased strongly under Fe-limitation, i.e., to 24 and 29% of the burst size produced under Fe-replete conditions (20 and 196 viruses lysed host cell<sup>&#x02212;1</sup>; Table <xref ref-type="table" rid="T3">3</xref>). In comparison to <italic>P. globosa</italic>, the reduced growth rate of Fe-limited steady state <italic>M. pusilla</italic> did not significantly affect the extent of reduction in virus burst size. Nonetheless, <italic>M. pusilla</italic> required a higher cellular Fe concentration. This implies that Fe-limited <italic>P. globosa</italic>, able to grow at the lower Fe concentration, displays a more efficient virus proliferation (despite the low F<sub>v</sub>/F<sub>m</sub> at the start of infection).</p>
<table-wrap position="float" id="T3">
<label>Table 3</label>
<caption><p><bold>Burst sizes (number of virus progeny per lysed host cell) of PgV-07T and MpV-08T infecting Fe-replete and Fe-limited <italic>P. globosa</italic> (Pg) and <italic>M. pusilla</italic> (Mp), respectively</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>Treatment</bold></th>
<th valign="top" align="center"><bold>Burst size</bold></th>
<th valign="top" align="center"><bold>% of replete</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Pg replete &#x0002B; VR</td>
<td valign="top" align="center">671 &#x000B1; 62</td>
<td/>
</tr>
<tr>
<td valign="top" align="left">Pg replete &#x0002B; VL</td>
<td valign="top" align="center">679 &#x000B1; 5</td>
<td/>
</tr>
<tr>
<td valign="top" align="left">Pg limited &#x0002B; VL</td>
<td valign="top" align="center">196 &#x000B1; 35</td>
<td valign="top" align="center">29 &#x000B1; 0.2</td>
</tr>
<tr>
<td valign="top" align="left">Pg limited &#x0002B; VR</td>
<td valign="top" align="center">308 &#x000B1; 4</td>
<td valign="top" align="center">46 &#x000B1; 2.3</td>
</tr>
<tr>
<td valign="top" align="left">Mp replete &#x0002B; VR</td>
<td valign="top" align="center">84 &#x000B1; 14</td>
<td/>
</tr>
<tr>
<td valign="top" align="left">Mp replete &#x0002B; VL</td>
<td valign="top" align="center">83 &#x000B1; 6</td>
<td/>
</tr>
<tr>
<td valign="top" align="left">Mp limited &#x0002B; VL</td>
<td valign="top" align="center">20 &#x000B1; 0</td>
<td valign="top" align="center">24 &#x000B1; 5.2</td>
</tr>
<tr>
<td valign="top" align="left">Mp limited &#x0002B; VR</td>
<td valign="top" align="center">46 &#x000B1; 2</td>
<td valign="top" align="center">54 &#x000B1; 0.5</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Viruses were derived from a Fe-replete host (VR) or a Fe-limited host (VL). Burst sizes for Fe-limited cultures are also expressed as a percentage of the corresponding infections in Fe-replete cultures.</italic></p>
</table-wrap-foot>
</table-wrap>
<p>Noteworthy, the higher Fe concentration needed to allow for sustainable growth of <italic>M. pusilla</italic> under Fe-limitation did not prevent the loss of infectivity of the virus progeny. Infectivity of the Fe-limited MpV lysate was reduced to 30 &#x000B1; 7%, while in contrast PgV did not show decreased infectivity for Fe-limited hosts. Our results signify that a stronger Fe-stress experienced by the Fe-limited <italic>M. pusilla</italic> (expressed in reduced growth rate) is more likely responsible for the production of impaired virus progeny than a changed photosynthetic capacity (F<sub>v</sub>/F<sub>m</sub> 0.2 for <italic>P. globosa</italic> compared to 0.6 for <italic>M. pusilla</italic>). The fact that total virus abundance, as measured after staining with a nucleic acid dye, was higher than the infective abundance indicates that (i) virus particles and (ii) viral nucleic acids were produced. Still, impaired capsid proteins or host receptors may explain a loss of infectivity. Alternatively, processes known to be Fe-intensive are DNA replication and repair (Netz et al., <xref ref-type="bibr" rid="B50">2012</xref>; Zhang, <xref ref-type="bibr" rid="B77">2014</xref>). Failure of DNA repair could indeed explain the result of reduced percentage infective viruses. Future research should not only focus on the causal aspects <italic>per se</italic> but also study what causes the dissimilarities in loss of infectivity between the algal viruses since different responses will directly regulate community composition. Furthermore, future studies should screen if and how other marine taxa and different viruses are affected by virus proliferation under Fe-limitation. For example, non-marine tailed bacteriophages have been found to contain iron ions in the tail proteins that can utilize the siderophore-bound iron receptors on the host cell membrane for attachment of the phage and subsequent infection of the bacterial host (Bartual et al., <xref ref-type="bibr" rid="B1">2010</xref>). It is likely that similar interactions also exists for marine bacteriophages (Bonnain et al., <xref ref-type="bibr" rid="B7">2016</xref>). Still open questions are whether such phages will obtain fewer iron ions in their tail under Fe-deprivation, and if this will negatively affect their infectivity. Furthermore, the recently proposed &#x0201C;Ferrojan Horse Hypothesis&#x0201D; by Bonnain et al. (<xref ref-type="bibr" rid="B7">2016</xref>) posits that introduction of phage-attached Fe may aid the host. More study is needed to test this theory and its potential interference with siderophore-specific uptake mechanisms and effect on Fe cycling.</p>
<p>For all Fe-replete cultures (i.e., high Fe concentration and consequently high F<sub>v</sub>/F<sub>m</sub> of around 0.6) and the Fe-limited <italic>M. pusilla</italic> the lysis dynamics and decline in F<sub>v</sub>/F<sub>m</sub> for the VR- and VL-infected cultures were largely comparable (Figures <xref ref-type="fig" rid="F1">1D</xref>, <xref ref-type="fig" rid="F2">2D</xref>). However, the Fe-treatment history of the virus (VL or VR) did matter in combination with Fe-limited <italic>P. globosa</italic> cells, i.e., infection with VR did delay the decline in F<sub>v</sub>/F<sub>m</sub> with more than a day (Figure <xref ref-type="fig" rid="F1">1C</xref>). Infection with a VR lysate is analogous to a relief in Fe-limitation at the time of infection. When the Fe-limited <italic>P. globosa</italic> cultures were infected with a VR lysate, they were effectively spiked with an Fe increase of &#x0007E;10% relative to Fe-replete conditions (0.9 &#x003BC;M). The 100&#x02013;300-fold increase of Fe with the addition of an Fe-replete lysate (0.9 &#x003BC;M vs. 1&#x02013;3 nM) takes the culture Fe concentration well out of limitation ranges which are generally considered to be in nano- to picomolar ranges (de Baar et al., <xref ref-type="bibr" rid="B19">1990</xref>; Martin et al., <xref ref-type="bibr" rid="B41">1990</xref>; Brand, <xref ref-type="bibr" rid="B8">1991</xref>). The concentration increase in our experiment is comparatively drastic to assure lifting of Fe-limitation to levels nearer normal replete cultures. This cross-inoculation provides insight in the potential effects of sudden introduction of Fe, e.g., with (seasonal) dust deposition or terrestrial runoff. The effect of this spike with Fe was apparently enough to prevent instant loss of photosynthetic capacity in the Fe-limited <italic>P. globosa</italic> cells. For both phytoplankton species, the improved physiological condition upon infection of Fe-limited host with VR virus resulted in enhanced viral production compared to Fe-limited infected with VL virus (by 1.6 and 2.3-fold for PgV and MpV, respectively; Table <xref ref-type="table" rid="T3">3</xref>). The effect on burst size is thus stronger for the more Fe-sensitive <italic>M. pusilla</italic>, indicating that <italic>M. pusilla</italic> is more capable of mobilizing the Fe added for viral production. Utilization of the limiting macronutrient P when added post infection was also found to stimulate virus production of <italic>M. pusilla</italic> (Maat et al., <xref ref-type="bibr" rid="B39">2016</xref>). Although, our results indicate that an infected host is capable of mobilizing the limiting Fe for viral production upon addition post infection, it did not lead to a complete recovery of virus production as compared to Fe-replete conditions (around 50% of the replete treatment; Table <xref ref-type="table" rid="T2">2</xref>).</p>
<p>In conclusion, viral infection of both phytoplankton species is distinctly influenced by Fe-limitation. The differences in sensitivity of the host to Fe-limitation subsequently affected the progeny virus growth properties. <italic>Phaeocystis</italic> and <italic>Micromonas</italic> occur in Fe-limited and Fe-replete conditions alike (Not et al., <xref ref-type="bibr" rid="B51">2004</xref>, <xref ref-type="bibr" rid="B52">2005</xref>; Schoemann et al., <xref ref-type="bibr" rid="B60">2005</xref>). Viral lysis has been shown to be an important mortality term for <italic>P. globosa</italic> under natural conditions, and also <italic>M. pusilla</italic> is readily infected (Cottrell and Suttle, <xref ref-type="bibr" rid="B18">1995</xref>; Brussaard, <xref ref-type="bibr" rid="B11">2004</xref>; Brussaard et al., <xref ref-type="bibr" rid="B12">2005</xref>; Baudoux et al., <xref ref-type="bibr" rid="B3">2006</xref>; Mart&#x000ED;nez et al., <xref ref-type="bibr" rid="B42">2015</xref>). Virus burst sizes became strongly reduced (on average by 70%) under Fe-limiting relative to Fe-replete conditions. Although, addition of Fe at the time of infection was utilized by the infected Fe-limited host to increase virus production, it was not to the level found under Fe-replete conditions. Thus, Fe-limitation irrevocably interfered with viral productivity. Additionally, Fe-limited <italic>M. pusilla</italic> demonstrated an evident effect on the quality of the viruses produced as only 30% were infective. The lowered virus infectivity and/or virus yield impair viral control of the specific host species under Fe-limitation. However, at the same time, reduced viral lysis may affect the productivity of remaining non-infected cells and of other phytoplankton species, because viral lysis is considered a driver of Fe cycling by releasing ligand-bound dissolved Fe-species back into the dissolved organic matter pool (Gobler et al., <xref ref-type="bibr" rid="B27">1997</xref>; Poorvin et al., <xref ref-type="bibr" rid="B54">2004</xref>, <xref ref-type="bibr" rid="B55">2011</xref>). What relative contributions different ligands have, and in how far their release is facilitated or impaired by viral lysis requires further study. Further experimental and <italic>in-situ</italic> study of phytoplankton host-virus dynamics under Fe-limitation is essential to elucidate the level of response specificity, but also the effects on the viral shunt in terms of nutrient cycling in general as well as Fe speciation.</p>
</sec>
</sec>
<sec id="s4">
<title>Author contributions</title>
<p>LG, CB, and HS were responsible for the design of this research. HS, CB analyzed and interpreted data. HS, LG, and CB wrote the paper.</p>
<sec>
<title>Conflict of interest statement</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
</sec>
</body>
<back>
<ack><p>We thank captain and crew of R.V. Pelagia and Micha Rijkenberg for their assistance in obtaining trace metal clean seawater stocks. We furthermore thank Josje Snoek for her assistance, Patrick Laan for dissolved Fe analysis, Swier Oosterhuis for pigment composition analysis, and Karel Bakker and Sharyn Ossebaar for nutrient analyses. We appreciate discussions with Douwe Maat, Klaas Timmermans and Willem van de Poll. This work was funded through a grant by the Netherlands Organization for Scientific Research (NWO) under contract number 822.01.018 to LG, and from the European Union Seventh Framework Programme (FP7/2007-2013) under grant agreement n 311975 (MaCuMBA) to CB.</p>
</ack>
<ref-list>
<title>References</title>
<ref id="B1">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Bartual</surname> <given-names>S. G.</given-names></name> <name><surname>Otero</surname> <given-names>J. M.</given-names></name> <name><surname>Garcia-Doval</surname> <given-names>C.</given-names></name> <name><surname>Llamas-Saiz</surname> <given-names>A. L.</given-names></name> <name><surname>Kahn</surname> <given-names>R.</given-names></name> <name><surname>Fox</surname> <given-names>G. C.</given-names></name> <etal/></person-group>. (<year>2010</year>). <article-title>Structure of the bacteriophage T4 long tail fiber receptor-binding tip</article-title>. <source>Proc. Natl. Acad. Sci. U.S.A.</source> <volume>107</volume>, <fpage>20287</fpage>&#x02013;<lpage>20292</lpage>. <pub-id pub-id-type="doi">10.1073/pnas.1011218107</pub-id><pub-id pub-id-type="pmid">21041684</pub-id></citation>
</ref>
<ref id="B2">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Baudoux</surname> <given-names>A. C.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2005</year>). <article-title>Characterization of different viruses infecting the marine harmful algal bloom species. <italic>Phaeocystis globosa</italic></article-title>. <source>Virology</source> <volume>341</volume>, <fpage>80</fpage>&#x02013;<lpage>90</lpage>. <pub-id pub-id-type="doi">10.1016/j.virol.2005.07.002</pub-id><pub-id pub-id-type="pmid">16081120</pub-id></citation>
</ref>
<ref id="B3">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Baudoux</surname> <given-names>A. C.</given-names></name> <name><surname>Noordeloos</surname> <given-names>A. A. M.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2006</year>). <article-title>Virally induced mortality of <italic>Phaeocystis globosa</italic> during two spring blooms in temperate coastal waters</article-title>. <source>Aquat. Microb. Ecol.</source> <volume>44</volume>, <fpage>207</fpage>&#x02013;<lpage>217</lpage>. <pub-id pub-id-type="doi">10.3354/ame044207</pub-id></citation>
</ref>
<ref id="B4">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Baudoux</surname> <given-names>A. C.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <name><surname>Witte</surname> <given-names>H. J.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2007</year>). <article-title>Viruses as mortality agents of picophytoplankton in the deep chlorophyll maximum layer during IRONAGES III</article-title>. <source>Limnol. Oceanogr.</source> <volume>52</volume>, <fpage>2519</fpage>&#x02013;<lpage>2529</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2007.52.6.2519</pub-id></citation>
</ref>
<ref id="B5">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Behrenfeld</surname> <given-names>M. J.</given-names></name> <name><surname>Bale</surname> <given-names>A. J.</given-names></name> <name><surname>Kolber</surname> <given-names>Z. S.</given-names></name> <name><surname>Aiken</surname> <given-names>J.</given-names></name> <name><surname>Falkowski</surname> <given-names>P. G.</given-names></name></person-group> (<year>1996</year>). <article-title>Confirmation of iron limitation of phytoplankton photosynthesis in the Equatorial Pacific Ocean</article-title>. <source>Nature</source> <volume>383</volume>, <fpage>508</fpage>&#x02013;<lpage>511</lpage>. <pub-id pub-id-type="doi">10.1038/383508a0</pub-id></citation>
</ref>
<ref id="B6">
<citation citation-type="thesis"><person-group person-group-type="author"><name><surname>Behrenfeld</surname> <given-names>M. J.</given-names></name> <name><surname>Worthington</surname> <given-names>K.</given-names></name> <name><surname>Sherrell</surname> <given-names>R. M.</given-names></name> <name><surname>Chavez</surname> <given-names>F. P.</given-names></name> <name><surname>Strutton</surname> <given-names>P.</given-names></name> <name><surname>McPhaden</surname> <given-names>M.</given-names></name> <etal/></person-group>. (<year>2006</year>). <article-title>Controls on tropical Pacific Ocean productivity revealed through nutrient stress diagnostics</article-title>. <source>Nature</source> <volume>442</volume>, <fpage>1025</fpage>&#x02013;<lpage>1028</lpage>. <pub-id pub-id-type="doi">10.1038/nature05083</pub-id><pub-id pub-id-type="pmid">16943835</pub-id></citation>
</ref>
<ref id="B7">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Bonnain</surname> <given-names>C.</given-names></name> <name><surname>Breitbart</surname> <given-names>M.</given-names></name> <name><surname>Buck</surname> <given-names>K. N.</given-names></name></person-group> (<year>2016</year>). <article-title>The Ferrojan Horse Hypothesis: iron-virus interactions in the ocean</article-title>. <source>Front. Mar. Sci.</source> <volume>3</volume>:<issue>82</issue>. <pub-id pub-id-type="doi">10.3389/fmars.2016.00082</pub-id></citation>
</ref>
<ref id="B8">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brand</surname> <given-names>L. E.</given-names></name></person-group> (<year>1991</year>). <article-title>Minimum iron requirements of marine phytoplankton and the implications for the biogeochemical control of new production</article-title>. <source>Limnol. Oceanogr.</source> <volume>36</volume>, <fpage>1756</fpage>&#x02013;<lpage>1771</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1991.36.8.1756</pub-id></citation>
</ref>
<ref id="B9">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Bratbak</surname> <given-names>G.</given-names></name> <name><surname>Jacobsen</surname> <given-names>A.</given-names></name> <name><surname>Heldal</surname> <given-names>M.</given-names></name> <name><surname>Nagasaki</surname> <given-names>K.</given-names></name> <name><surname>Thingstad</surname> <given-names>F.</given-names></name></person-group> (<year>1998</year>). <article-title>Virus production in <italic>Phaeocystis pouchetii</italic> and its relation to host cell growth and nutrition</article-title>. <source>Aquat. Microb. Ecol.</source> <volume>16</volume>, <fpage>1</fpage>&#x02013;<lpage>9</lpage>. <pub-id pub-id-type="doi">10.3354/ame016001</pub-id></citation>
</ref>
<ref id="B10">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Breitbarth</surname> <given-names>E.</given-names></name> <name><surname>Achterberg</surname> <given-names>E. P.</given-names></name> <name><surname>Ardelan</surname> <given-names>M. V.</given-names></name> <name><surname>Baker</surname> <given-names>A. R.</given-names></name> <name><surname>Bucciarelli</surname> <given-names>E.</given-names></name> <name><surname>Chever</surname> <given-names>F.</given-names></name> <etal/></person-group>. (<year>2010</year>). <article-title>Iron biogeochemistry across marine systems&#x02013;progress from the past decade</article-title>. <source>Biogeosciences</source> <volume>7</volume>, <fpage>1075</fpage>&#x02013;<lpage>1097</lpage>. <pub-id pub-id-type="doi">10.5194/bg-7-1075-2010</pub-id></citation>
</ref>
<ref id="B11">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2004</year>). <article-title>Viral control of phytoplankton populations - a review</article-title>. <source>J. Eukaryot. Microbiol.</source> <volume>51</volume>, <fpage>125</fpage>&#x02013;<lpage>138</lpage>. <pub-id pub-id-type="doi">10.1111/j.1550-7408.2004.tb00537.x</pub-id><pub-id pub-id-type="pmid">15134247</pub-id></citation>
</ref>
<ref id="B12">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name> <name><surname>Mari</surname> <given-names>X.</given-names></name> <name><surname>Van Bleijswijk</surname> <given-names>J. D. L.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name></person-group> (<year>2005</year>). <article-title>A mesocosm study of <italic>Phaeocystis globosa</italic> (Prymnesiophyceae) population dynamics: II. Significance for the microbial community</article-title>. <source>Harmful Algae</source> <volume>4</volume>, <fpage>875</fpage>&#x02013;<lpage>893</lpage>. <pub-id pub-id-type="doi">10.1016/j.hal.2004.12.012</pub-id></citation>
</ref>
<ref id="B13">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name> <name><surname>Mart&#x000ED;nez</surname> <given-names>J. M.</given-names></name></person-group> (<year>2008</year>). <article-title>Algal bloom viruses</article-title>. <source>Plant Virus.</source> <volume>2</volume>, <fpage>1</fpage>&#x02013;<lpage>10</lpage>. Available online at: <ext-link ext-link-type="uri" xlink:href="http://www.globalsciencebooks.info/Journals/PV.html">http://www.globalsciencebooks.info/Journals/PV.html</ext-link></citation>
</ref>
<ref id="B14">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name> <name><surname>Payet</surname> <given-names>J. P.</given-names></name> <name><surname>Winter</surname> <given-names>C.</given-names></name> <name><surname>Weinbauer</surname> <given-names>M. G.</given-names></name></person-group> (<year>2010</year>). <article-title>Quantification of aquatic viruses by flow cytometry</article-title>. <source>Man. Aquat. Viral Ecol.</source> <volume>11</volume>, <fpage>102</fpage>&#x02013;<lpage>109</lpage>. <pub-id pub-id-type="doi">10.4319/mave.2010.978-0-9845591-0-7.102</pub-id></citation>
</ref>
<ref id="B15">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name> <name><surname>Thyrhaug</surname> <given-names>R.</given-names></name> <name><surname>Marie</surname> <given-names>D.</given-names></name> <name><surname>Bratbak</surname> <given-names>G.</given-names></name></person-group> (<year>1999</year>). <article-title>Flow cytometric analyses of viral infection in two marine phytoplankton species, <italic>Micromonas pusilla</italic> (Prasinophyceae) and <italic>Phaeocystis pouchetii</italic> (Prymnesiophyceae)</article-title>. <source>J. Phycol.</source> <volume>35</volume>, <fpage>941</fpage>&#x02013;<lpage>948</lpage>. <pub-id pub-id-type="doi">10.1046/j.1529-8817.1999.3550941.x</pub-id></citation>
</ref>
<ref id="B16">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Butler</surname> <given-names>A.</given-names></name></person-group> (<year>2005</year>). <article-title>Marine siderophores and microbial iron mobilization</article-title>. <source>Biometals</source> <volume>18</volume>, <fpage>369</fpage>&#x02013;<lpage>374</lpage>. <pub-id pub-id-type="doi">10.1007/s10534-005-3711-0</pub-id><pub-id pub-id-type="pmid">16158229</pub-id></citation>
</ref>
<ref id="B17">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Calbet</surname> <given-names>A.</given-names></name> <name><surname>Landry</surname> <given-names>M. R.</given-names></name></person-group> (<year>2004</year>). <article-title>Phytoplankton growth, microzooplankton grazing, and carbon cycling in marine systems</article-title>. <source>Limnol. Oceanogr.</source> <volume>49</volume>, <fpage>51</fpage>&#x02013;<lpage>57</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2004.49.1.0051</pub-id></citation>
</ref>
<ref id="B18">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Cottrell</surname> <given-names>M. T.</given-names></name> <name><surname>Suttle</surname> <given-names>C. A.</given-names></name></person-group> (<year>1995</year>). <article-title>Dynamics of lytic virus infecting the photosynthetic marine picoflagellate <italic>Micromonas pusilla</italic></article-title>. <source>Limnol. Oceanogr.</source> <volume>40</volume>, <fpage>730</fpage>&#x02013;<lpage>739</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1995.40.4.0730</pub-id></citation>
</ref>
<ref id="B19">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name> <name><surname>Buma</surname> <given-names>A. G. J.</given-names></name> <name><surname>Nolting</surname> <given-names>R. F.</given-names></name> <name><surname>Cadee</surname> <given-names>G. C.</given-names></name> <name><surname>Jacques</surname> <given-names>G.</given-names></name> <name><surname>Treguer</surname> <given-names>P. J.</given-names></name></person-group> (<year>1990</year>). <article-title>On iron limitation of the southern ocean?: experimental observations in the Weddell and Scotia Seas</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>65</volume>, <fpage>105</fpage>&#x02013;<lpage>122</lpage>. <pub-id pub-id-type="doi">10.3354/meps065105</pub-id></citation>
</ref>
<ref id="B20">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Garg</surname> <given-names>S.</given-names></name> <name><surname>Rose</surname> <given-names>A. L.</given-names></name> <name><surname>Waite</surname> <given-names>T. D.</given-names></name></person-group> (<year>2007</year>). <article-title>Superoxide-mediated reduction of organically complexed iron(III): impact of pH and competing cations (Ca<sup>2&#x0002B;</sup>)</article-title>. <source>Geochim. Cosmochim. Acta</source> <volume>71</volume>, <fpage>5620</fpage>&#x02013;<lpage>5634</lpage>. <pub-id pub-id-type="doi">10.1016/j.gca.2007.08.002</pub-id></citation>
</ref>
<ref id="B21">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Geider</surname> <given-names>R. J.</given-names></name> <name><surname>La Roche</surname> <given-names>J.</given-names></name></person-group> (<year>1994</year>). <article-title>The role of iron in phytoplankton photosynthesis, and the potential for iron-limitation of primary productivity in the sea</article-title>. <source>Photosyn. Res.</source> <volume>39</volume>, <fpage>275</fpage>&#x02013;<lpage>301</lpage>. <pub-id pub-id-type="pmid">24311126</pub-id></citation>
</ref>
<ref id="B22">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Geider</surname> <given-names>R. J.</given-names></name> <name><surname>La Roche</surname> <given-names>J.</given-names></name> <name><surname>Greene</surname> <given-names>R. M.</given-names></name> <name><surname>Olaizola</surname> <given-names>M.</given-names></name></person-group> (<year>1993</year>). <article-title>Response of the photosynthetic apparatus of <italic>Phaeodactylum tricornutum</italic> (Bacillariophyceae) to nitrate, phosphate, or iron starvation</article-title>. <source>J. Phycol.</source> <volume>29</volume>, <fpage>755</fpage>&#x02013;<lpage>766</lpage>. <pub-id pub-id-type="doi">10.1111/j.0022-3646.1993.00755.x</pub-id><pub-id pub-id-type="pmid">27448791</pub-id></citation>
</ref>
<ref id="B23">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Genty</surname> <given-names>B.</given-names></name> <name><surname>Briantais</surname> <given-names>J.&#x02013;M.</given-names></name> <name><surname>Baker</surname> <given-names>N. R.</given-names></name></person-group> (<year>1989</year>). <article-title>The relationship between the quantum yield of photosynthetic electron transport and quenching of chlorophyll fluorescence</article-title>. <source>Biochim. Biophys. Acta</source> <volume>990</volume>, <fpage>87</fpage>&#x02013;<lpage>92</lpage>. <pub-id pub-id-type="doi">10.1016/S0304-4165(89)80016-9</pub-id></citation>
</ref>
<ref id="B24">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gerringa</surname> <given-names>L. J. A.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name> <name><surname>Timmermans</surname> <given-names>K. R.</given-names></name></person-group> (<year>2000</year>). <article-title>A comparison of iron limitation of phytoplankton in natural oceanic waters and laboratory media conditioned with EDTA</article-title>. <source>Mar. Chem</source>. <volume>68</volume>, <fpage>335</fpage>&#x02013;<lpage>346</lpage>. <pub-id pub-id-type="doi">10.1016/S0304-4203(99)00092</pub-id></citation>
</ref>
<ref id="B25">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gerringa</surname> <given-names>L. J. A.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>Sarthou</surname> <given-names>G.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name></person-group> (<year>2006</year>). <article-title>Co-variance of dissolved Fe-binding ligands with phytoplankton characteristics in the canary basin</article-title>. <source>Mar. Chem.</source> <volume>102</volume>, <fpage>276</fpage>&#x02013;<lpage>290</lpage>. <pub-id pub-id-type="doi">10.1016/j.marchem.2006.05.004</pub-id></citation>
</ref>
<ref id="B26">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gledhill</surname> <given-names>M.</given-names></name> <name><surname>van den Berg</surname> <given-names>C. M. G.</given-names></name></person-group> (<year>1994</year>). <article-title>Determination of complexation of iron(III) with natural organic complexing ligands in seawater using cathodic stripping voltammetry</article-title>. <source>Mar. Chem.</source> <volume>47</volume>, <fpage>41</fpage>&#x02013;<lpage>54</lpage>. <pub-id pub-id-type="doi">10.1016/0304-4203(94)90012-4</pub-id></citation>
</ref>
<ref id="B27">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gobler</surname> <given-names>C. J.</given-names></name> <name><surname>Hutchins</surname> <given-names>D. A.</given-names></name> <name><surname>Fisher</surname> <given-names>N. S.</given-names></name></person-group> (<year>1997</year>). <article-title>Release and bioavailability of C, N, P, Se, and Fe following viral lysis of a marine chrysophyte</article-title>. <source>Limnol. Oceanogr.</source> <volume>42</volume>, <fpage>1492</fpage>&#x02013;<lpage>1504</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1997.42.7.1492</pub-id></citation>
</ref>
<ref id="B28">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gonz&#x000E1;lez</surname> <given-names>A. G.</given-names></name> <name><surname>P&#x000E9;rez-Almeida</surname> <given-names>N.</given-names></name> <name><surname>Santana-Casiano</surname> <given-names>J. M.</given-names></name> <name><surname>Millero</surname> <given-names>F. J.</given-names></name> <name><surname>Gonz&#x000E1;lez-D&#x000E1;vila</surname> <given-names>M.</given-names></name></person-group> (<year>2016</year>). <article-title>Redox interactions of Fe and Cu in seawater</article-title>. <source>Mar. Chem.</source> <volume>179</volume>, <fpage>12</fpage>&#x02013;<lpage>22</lpage>. <pub-id pub-id-type="doi">10.1016/j.marchem.2016.01.004</pub-id></citation>
</ref>
<ref id="B29">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gonz&#x000E1;lez</surname> <given-names>A. G.</given-names></name> <name><surname>Santana-Casiano</surname> <given-names>J. M.</given-names></name> <name><surname>Gonz&#x000E1;lez-D&#x000E1;vila</surname> <given-names>M.</given-names></name> <name><surname>P&#x000E9;rez-Almeida</surname> <given-names>N.</given-names></name> <name><surname>Su&#x000E1;rez De Tangil</surname> <given-names>M.</given-names></name></person-group> (<year>2014</year>). <article-title>Effect of <italic>Dunaliella tertiolecta</italic> organic exudates on the Fe(II) oxidation kinetics in seawater</article-title>. <source>Environ. Sci. Technol.</source> <volume>48</volume>, <fpage>7933</fpage>&#x02013;<lpage>7941</lpage>. <pub-id pub-id-type="doi">10.1021/es5013092</pub-id><pub-id pub-id-type="pmid">24941285</pub-id></citation>
</ref>
<ref id="B30">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Grasshoff</surname> <given-names>K.</given-names></name></person-group> (<year>1983</year>). <article-title>Determination of nitrate</article-title>. in <source>Methods of Seawater Analysis</source>, eds <person-group person-group-type="editor"><name><surname>Grasshoff</surname> <given-names>K.</given-names></name> <name><surname>Erhardt</surname> <given-names>M.</given-names></name> <name><surname>Kremling</surname> <given-names>K.</given-names></name></person-group> (<publisher-loc>Weinheim</publisher-loc>: <publisher-name>Verlag Chemie</publisher-name>), <fpage>143</fpage>&#x02013;<lpage>87</lpage>.</citation>
</ref>
<ref id="B31">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hassler</surname> <given-names>C. S.</given-names></name> <name><surname>Schoemann</surname> <given-names>V.</given-names></name> <name><surname>Nichols</surname> <given-names>C. M.</given-names></name> <name><surname>Butler</surname> <given-names>E. C. V.</given-names></name> <name><surname>Boyd</surname> <given-names>P. W.</given-names></name></person-group> (<year>2011</year>). <article-title>Saccharides enhance iron bioavailability to southern ocean phytoplankton</article-title>. <source>Proc. Natl. Acad. Sci. U.S.A.</source> <volume>108</volume>, <fpage>1076</fpage>&#x02013;<lpage>1081</lpage>. <pub-id pub-id-type="doi">10.1073/pnas.1010963108</pub-id><pub-id pub-id-type="pmid">21169217</pub-id></citation>
</ref>
<ref id="B32">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Ibisanmi</surname> <given-names>E.</given-names></name> <name><surname>Sander</surname> <given-names>S. G.</given-names></name> <name><surname>Boyd</surname> <given-names>P. W.</given-names></name> <name><surname>Bowie</surname> <given-names>A. R.</given-names></name> <name><surname>Hunter</surname> <given-names>K. A.</given-names></name></person-group> (<year>2011</year>). <article-title>Vertical distributions of iron-(III) complexing ligands in the southern ocean</article-title>. <source>Deep Sea Res. II</source> <volume>58</volume>, <fpage>2113</fpage>&#x02013;<lpage>2125</lpage>. <pub-id pub-id-type="doi">10.1016/j.dsr2.2011.05.028</pub-id></citation>
</ref>
<ref id="B33">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Klunder</surname> <given-names>M. B.</given-names></name> <name><surname>Laan</surname> <given-names>P.</given-names></name> <name><surname>Middag</surname> <given-names>R.</given-names></name> <name><surname>De Baar</surname> <given-names>H. J. W.</given-names></name> <name><surname>van Ooijen</surname> <given-names>J. C.</given-names></name></person-group> (<year>2011</year>). <article-title>Dissolved iron in the southern ocean (Atlantic Sector)</article-title>. <source>Deep Sea Res. II</source> <volume>58</volume>, <fpage>2678</fpage>&#x02013;<lpage>2694</lpage>. <pub-id pub-id-type="doi">10.1016/j.dsr2.2010.10.042</pub-id></citation>
</ref>
<ref id="B34">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Kustka</surname> <given-names>A. B.</given-names></name> <name><surname>Shaked</surname> <given-names>Y.</given-names></name> <name><surname>Milligan</surname> <given-names>A. J.</given-names></name> <name><surname>King</surname> <given-names>D. W.</given-names></name> <name><surname>Morel</surname> <given-names>F. M. M.</given-names></name></person-group> (<year>2005</year>). <article-title>Extracellular production of superoxide by marine diatoms: contrasting effects on iron redox chemistry and bioavailability</article-title>. <source>Limnol. Oceanogr.</source> <volume>50</volume>, <fpage>1172</fpage>&#x02013;<lpage>1180</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2005.50.4.1172</pub-id></citation>
</ref>
<ref id="B35">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Laglera</surname> <given-names>L. M.</given-names></name> <name><surname>Battaglia</surname> <given-names>G.</given-names></name> <name><surname>van den Berg</surname> <given-names>C. M. G.</given-names></name></person-group> (<year>2011</year>). <article-title>Effect of humic substances on the iron speciation in natural waters by CLE/CSV</article-title>. <source>Mar. Chem.</source> <volume>127</volume>, <fpage>134</fpage>&#x02013;<lpage>143</lpage>. <pub-id pub-id-type="doi">10.1016/j.marchem.2011.09.003</pub-id></citation>
</ref>
<ref id="B36">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Liu</surname> <given-names>X.</given-names></name> <name><surname>Millero</surname> <given-names>F. J.</given-names></name></person-group> (<year>2002</year>). <article-title>The Solubility of iron in seawater</article-title>. <source>Mar. Chem.</source> <volume>77</volume>, <fpage>43</fpage>&#x02013;<lpage>54</lpage>. <pub-id pub-id-type="doi">10.1016/S0304-4203(01)00074-3</pub-id></citation>
</ref>
<ref id="B37">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Maat</surname> <given-names>D. S.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2016</year>). <article-title>Both phosphorus and nitrogen limitation constrain viral proliferation in marine phytoplankton</article-title>. <source>Aquat. Microb. Ecol.</source> <volume>77</volume>, <fpage>87</fpage>&#x02013;<lpage>97</lpage>. <pub-id pub-id-type="doi">10.3354/ame01791</pub-id></citation>
</ref>
<ref id="B38">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Maat</surname> <given-names>D. S.</given-names></name> <name><surname>Crawfurd</surname> <given-names>K. J.</given-names></name> <name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2014</year>). <article-title>Elevated CO<sub>2</sub> and phosphate limitation favor <italic>Micromonas pusilla</italic> through stimulated growth and reduced viral impact</article-title>. <source>Appl. Environ. Microbiol.</source> <volume>80</volume>, <fpage>3119</fpage>&#x02013;<lpage>3127</lpage>. <pub-id pub-id-type="doi">10.1128/AEM.03639-13</pub-id><pub-id pub-id-type="pmid">24610859</pub-id></citation>
</ref>
<ref id="B39">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Maat</surname> <given-names>D. S.</given-names></name> <name><surname>Van Bleijswijk</surname> <given-names>J. D. L.</given-names></name> <name><surname>Witte</surname> <given-names>H. J.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2016</year>). <article-title>Virus production in phosphorus limited <italic>Micromonas pusilla</italic> stimulated by a supply of naturally low concentrations of different phosphorus sources, far into the lytic cycle</article-title>. <source>FEMS Microbiol. Ecol.</source> <volume>92</volume>:<issue>fiw136</issue>. <pub-id pub-id-type="doi">10.1093/femsec/fiw136</pub-id><pub-id pub-id-type="pmid">27316561</pub-id></citation>
</ref>
<ref id="B40">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Marie</surname> <given-names>D.</given-names></name> <name><surname>Partensky</surname> <given-names>F.</given-names></name> <name><surname>Vaulot</surname> <given-names>D.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>1999</year>). <article-title>Enumeration of phytoplankton, bacteria, and viruses in marine samples</article-title>. <source>Curr. Protoc. Cytom.</source> Chapter 11, Unit 11.11. <pub-id pub-id-type="doi">10.1002/0471142956</pub-id><pub-id pub-id-type="pmid">18770685</pub-id></citation>
</ref>
<ref id="B41">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Martin</surname> <given-names>J. H.</given-names></name> <name><surname>Fitzwater</surname> <given-names>S. E.</given-names></name> <name><surname>Gordon</surname> <given-names>R. M.</given-names></name></person-group> (<year>1990</year>). <article-title>Iron deficiency limits phytoplankton growth in antarctic waters</article-title>. <source>Global Biogeochem. Cycles</source> <volume>4</volume>, <fpage>5</fpage>&#x02013;<lpage>12</lpage>.</citation>
</ref>
<ref id="B42">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mart&#x000ED;nez</surname> <given-names>J. M.</given-names></name> <name><surname>Boere</surname> <given-names>A.</given-names></name> <name><surname>Gilg</surname> <given-names>I.</given-names></name> <name><surname>van Lent</surname> <given-names>J. W. M.</given-names></name> <name><surname>Witte</surname> <given-names>H. J.</given-names></name> <name><surname>van Bleijswijk</surname> <given-names>J. D. L.</given-names></name> <etal/></person-group>. (<year>2015</year>). <article-title>New lipid envelope-containing dsDNA virus isolates infecting <italic>Micromonas pusilla</italic> reveal a separate phylogenetic group</article-title>. <source>Aquat. Microb. Ecol.</source> <volume>74</volume>, <fpage>17</fpage>&#x02013;<lpage>28</lpage>. <pub-id pub-id-type="doi">10.3354/ame01723</pub-id></citation>
</ref>
<ref id="B43">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mart&#x000ED;nez</surname> <given-names>J. M.</given-names></name> <name><surname>Swan</surname> <given-names>B. K.</given-names></name> <name><surname>Wilson</surname> <given-names>W. H.</given-names></name></person-group> (<year>2014</year>). <article-title>Marine viruses, a genetic reservoir revealed by targeted viromics</article-title>. <source>ISME J.</source> <volume>8</volume>, <fpage>1079</fpage>&#x02013;<lpage>1088</lpage>. <pub-id pub-id-type="doi">10.1038/ismej.2013.214</pub-id><pub-id pub-id-type="pmid">24304671</pub-id></citation>
</ref>
<ref id="B44">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mawji</surname> <given-names>E.</given-names></name> <name><surname>Gledhill</surname> <given-names>M.</given-names></name> <name><surname>Milton</surname> <given-names>J. A.</given-names></name> <name><surname>Zubkov</surname> <given-names>M. V.</given-names></name> <name><surname>Thompson</surname> <given-names>A.</given-names></name> <name><surname>Wolff</surname> <given-names>G. A.</given-names></name> <etal/></person-group>. (<year>2011</year>). <article-title>Production of siderophore type chelates in Atlantic Ocean Waters enriched with different carbon and nitrogen sources</article-title>. <source>Mar. Chem.</source> <volume>124</volume>, <fpage>90</fpage>&#x02013;<lpage>99</lpage>. <pub-id pub-id-type="doi">10.1016/j.marchem.2010.12.005</pub-id></citation>
</ref>
<ref id="B45">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mengel</surname> <given-names>K.</given-names></name></person-group> (<year>1994</year>). <article-title>Iron availability in plant tissues - iron chlorosis on calcareous soils</article-title>. <source>Plant Soil</source> <volume>165</volume>, <fpage>275</fpage>&#x02013;<lpage>283</lpage>. <pub-id pub-id-type="doi">10.1007/BF00008070</pub-id></citation>
</ref>
<ref id="B46">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Millero</surname> <given-names>F. J.</given-names></name></person-group> (<year>1998</year>). <article-title>Solubility of Fe (III) in seawater</article-title>. <source>Earth Planet. Sci. Lett.</source> <volume>154</volume>, <fpage>323</fpage>&#x02013;<lpage>329</lpage>.</citation>
</ref>
<ref id="B47">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mojica</surname> <given-names>K. D. A.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2014</year>). <article-title>Factors affecting virus dynamics and microbial host-virus interactions in marine environments</article-title>. <source>FEMS Microbiol. Ecol.</source> <volume>89</volume>, <fpage>495</fpage>&#x02013;<lpage>515</lpage>. <pub-id pub-id-type="doi">10.1111/1574-6941.12343</pub-id><pub-id pub-id-type="pmid">24754794</pub-id></citation>
</ref>
<ref id="B48">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mojica</surname> <given-names>K. D. A.</given-names></name> <name><surname>Huisman</surname> <given-names>J.</given-names></name> <name><surname>Wilhelm</surname> <given-names>S. W.</given-names></name> <name><surname>Brussaard</surname> <given-names>C. P. D.</given-names></name></person-group> (<year>2016</year>). <article-title>Latitudinal variation in virus-induced mortality of phytoplankton across the North Atlantic Ocean</article-title>. <source>ISME J.</source> <volume>10</volume>, <fpage>1</fpage>&#x02013;<lpage>14</lpage>. <pub-id pub-id-type="doi">10.1038/ismej.2015.130</pub-id><pub-id pub-id-type="pmid">26262815</pub-id></citation>
</ref>
<ref id="B49">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Murphy</surname> <given-names>J.</given-names></name> <name><surname>Riley</surname> <given-names>J. P.</given-names></name></person-group> (<year>1962</year>). <article-title>A modified single solution method for the determination of phosphorous in natural waters</article-title>. <source>Anal. Chim. Acta</source> <volume>27</volume>, <fpage>31</fpage>&#x02013;<lpage>36</lpage>.</citation>
</ref>
<ref id="B50">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Netz</surname> <given-names>D. J. A.</given-names></name> <name><surname>Stith</surname> <given-names>C. M.</given-names></name> <name><surname>St&#x000FC;mpfig</surname> <given-names>M.</given-names></name> <name><surname>K&#x000F6;pf</surname> <given-names>G.</given-names></name> <name><surname>Vogel</surname> <given-names>D.</given-names></name> <name><surname>Genau</surname> <given-names>H. M.</given-names></name> <etal/></person-group>. (<year>2012</year>). <article-title>Eukaryotic DNA polymerases require an iron-sulfur cluster for the formation of active complexes</article-title>. <source>Nat. Chem. Biol.</source> <volume>8</volume>, <fpage>125</fpage>&#x02013;<lpage>132</lpage>. <pub-id pub-id-type="doi">10.1038/nchembio.721</pub-id><pub-id pub-id-type="pmid">22119860</pub-id></citation>
</ref>
<ref id="B51">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Not</surname> <given-names>F.</given-names></name> <name><surname>Latasa</surname> <given-names>M.</given-names></name> <name><surname>Marie</surname> <given-names>D.</given-names></name> <name><surname>Cariou</surname> <given-names>T.</given-names></name> <name><surname>Vaulot</surname> <given-names>D.</given-names></name> <name><surname>Simon</surname> <given-names>N.</given-names></name></person-group> (<year>2004</year>). <article-title>A Single Species, <italic>Micromonas pusilla</italic> (Prasinophyceae), dominates the eukaryotic picoplankton in the Western English Channel</article-title>. <source>Appl. Environ. Microbiol.</source> <volume>70</volume>, <fpage>4064</fpage>&#x02013;<lpage>4072</lpage>. <pub-id pub-id-type="doi">10.1128/AEM.70.7.4064-4072.2004</pub-id><pub-id pub-id-type="pmid">15240284</pub-id></citation>
</ref>
<ref id="B52">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Not</surname> <given-names>F.</given-names></name> <name><surname>Massana</surname> <given-names>R.</given-names></name> <name><surname>Latasa</surname> <given-names>M.</given-names></name> <name><surname>Marie</surname> <given-names>D.</given-names></name> <name><surname>Colson</surname> <given-names>C.</given-names></name> <name><surname>Eikrem</surname> <given-names>W.</given-names></name> <etal/></person-group>. (<year>2005</year>). <article-title>Late summer community composition and abundance of photosynthetic picoeukaryotes in Norwegian and Barents Seas</article-title>. <source>Limnol. Oceanogr.</source> <volume>50</volume>, <fpage>1677</fpage>&#x02013;<lpage>1686</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2005.50.5.1677</pub-id></citation>
</ref>
<ref id="B53">
<citation citation-type="web"><person-group person-group-type="author"><name><surname>Passmore</surname> <given-names>R.</given-names></name> <name><surname>Hsu</surname> <given-names>J.</given-names></name> <name><surname>Liu</surname> <given-names>R. X.</given-names></name> <name><surname>Tam</surname> <given-names>E.</given-names></name> <name><surname>Cai</surname> <given-names>Y. W.</given-names></name> <name><surname>Su Frasca</surname> <given-names>J.</given-names></name> <etal/></person-group>. (<year>2000</year>). <source>MPN Assay Analyzer.</source> Available online at: <ext-link ext-link-type="uri" xlink:href="http://www.ocgy.ubc.ca/~suttle/">http://www.ocgy.ubc.ca/&#x0007E;suttle/</ext-link></citation>
</ref>
<ref id="B54">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Poorvin</surname> <given-names>L.</given-names></name> <name><surname>Rinta-Kanto</surname> <given-names>J. M.</given-names></name> <name><surname>Hutchins</surname> <given-names>D. A.</given-names></name> <name><surname>Wilhelm</surname> <given-names>S. W.</given-names></name></person-group> (<year>2004</year>). <article-title>Viral release of iron and its bioavailability to marine plankton</article-title>. <source>Limnol. Oceanogr.</source> <volume>49</volume>, <fpage>1734</fpage>&#x02013;<lpage>1741</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2004.49.5.1734</pub-id></citation>
</ref>
<ref id="B55">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Poorvin</surname> <given-names>L.</given-names></name> <name><surname>Sander</surname> <given-names>S. G.</given-names></name> <name><surname>Velasquez</surname> <given-names>I.</given-names></name> <name><surname>Ibisanmi</surname> <given-names>E.</given-names></name> <name><surname>LeCleir</surname> <given-names>G. R.</given-names></name> <name><surname>Wilhelm</surname> <given-names>S. W.</given-names></name></person-group> (<year>2011</year>). <article-title>A comparison of Fe bioavailability and binding of a catecholate siderophore with virus-mediated lysates from the marine bacterium <italic>Vibrio alginolyticus</italic> PWH3a</article-title>. <source>J. Exp. Mar. Biol. Ecol.</source> <volume>399</volume>, <fpage>43</fpage>&#x02013;<lpage>47</lpage>. <pub-id pub-id-type="doi">10.1016/j.jembe.2011.01.016</pub-id></citation>
</ref>
<ref id="B56">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Price</surname> <given-names>N. M.</given-names></name> <name><surname>Ahner</surname> <given-names>B. A.</given-names></name> <name><surname>Morel</surname> <given-names>F. M. M.</given-names></name></person-group> (<year>1994</year>). <article-title>The Equatorial Pacific Ocean: grazer controlled phytoplankton populations in an iron-limited ecosystem</article-title>. <source>Limnol. Oceanogr.</source> <volume>39</volume>, <fpage>520</fpage>&#x02013;<lpage>534</lpage>.</citation>
</ref>
<ref id="B57">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Rijkenberg</surname> <given-names>M. J. A.</given-names></name> <name><surname>Steigenberger</surname> <given-names>S.</given-names></name> <name><surname>Powell</surname> <given-names>C. F.</given-names></name> <name><surname>van Haren</surname> <given-names>H.</given-names></name> <name><surname>Patey</surname> <given-names>M. D.</given-names></name> <name><surname>Baker</surname> <given-names>A. R.</given-names></name> <etal/></person-group>. (<year>2012</year>). <article-title>Fluxes and distribution of dissolved iron in the Eastern (Sub-) Tropical North Atlantic Ocean</article-title>. <source>Global Biogeochem. Cycles</source> 26, GB3004. <pub-id pub-id-type="doi">10.1029/2011gb004264</pub-id></citation>
</ref>
<ref id="B58">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Romeo</surname> <given-names>A. M.</given-names></name> <name><surname>Christen</surname> <given-names>L.</given-names></name> <name><surname>Niles</surname> <given-names>E. G.</given-names></name> <name><surname>Kosman</surname> <given-names>D. J.</given-names></name></person-group> (<year>2001</year>). <article-title>Intracellular chelation of iron by bipyridyl inhibits DNA virus replication: ribonucleotide reductase maturation as a probe of intracellular iron pools</article-title>. <source>J. Biol. Chem.</source> <volume>276</volume>, <fpage>24301</fpage>&#x02013;<lpage>24308</lpage>. <pub-id pub-id-type="doi">10.1074/jbc.M010806200</pub-id><pub-id pub-id-type="pmid">11301321</pub-id></citation>
</ref>
<ref id="B59">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Rue</surname> <given-names>E. L.</given-names></name> <name><surname>Bruland</surname> <given-names>K. W.</given-names></name></person-group> (<year>1995</year>). <article-title>Complexation of iron(III) by natural organic ligands in the central North Pacific as determined by a new competitive ligand equilibration/adsorptive cathodic stripping voltammetric method</article-title>. <source>Mar. Chem.</source> <volume>50</volume>, <fpage>117</fpage>&#x02013;<lpage>138</lpage>. <pub-id pub-id-type="doi">10.1016/0304-4203(95)00031-L</pub-id></citation>
</ref>
<ref id="B60">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Schoemann</surname> <given-names>V.</given-names></name> <name><surname>Becquevort</surname> <given-names>S.</given-names></name> <name><surname>Stefels</surname> <given-names>J.</given-names></name> <name><surname>Rousseau</surname> <given-names>V.</given-names></name> <name><surname>Lancelot</surname> <given-names>C.</given-names></name></person-group> (<year>2005</year>). <article-title><italic>Phaeocystis</italic> blooms in the global ocean and their controlling mechanisms: a review</article-title>. <source>J. Sea Res.</source> <volume>53</volume>, <fpage>43</fpage>&#x02013;<lpage>66</lpage>. <pub-id pub-id-type="doi">10.1016/j.seares.2004.01.008</pub-id></citation>
</ref>
<ref id="B61">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Shaked</surname> <given-names>Y.</given-names></name> <name><surname>Lis</surname> <given-names>H.</given-names></name></person-group> (<year>2012</year>). <article-title>Disassembling iron availability to phytoplankton</article-title>. <source>Front. Microbiol.</source> <volume>3</volume>:<issue>123</issue>. <pub-id pub-id-type="doi">10.3389/fmicb.2012.00123</pub-id><pub-id pub-id-type="pmid">22529839</pub-id></citation>
</ref>
<ref id="B62">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Sunda</surname> <given-names>W. G.</given-names></name> <name><surname>Huntsman</surname> <given-names>S. A.</given-names></name></person-group> (<year>1995</year>). <article-title>Iron uptake and growth limitation in oceanic and coastal phytoplankton</article-title>. <source>Mar. Chem.</source> <volume>50</volume>, <fpage>189</fpage>&#x02013;<lpage>206</lpage>. <pub-id pub-id-type="doi">10.1016/0304-4203(95)00035-P</pub-id></citation>
</ref>
<ref id="B63">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Suttle</surname> <given-names>C. A.</given-names></name></person-group> (<year>1993</year>). <article-title>Enumeration and isolation of viruses</article-title>, in <source>Handbook of Methods in Aquatic Microbial Ecology, 1st Edn.</source>, eds <person-group person-group-type="editor"><name><surname>Kemp</surname> <given-names>P. F.</given-names></name> <name><surname>Sherr</surname> <given-names>B. F.</given-names></name> <name><surname>Sherr</surname> <given-names>E. B.</given-names></name> <name><surname>Cole</surname> <given-names>J. J.</given-names></name></person-group> (<publisher-loc>Boca Raton, FL</publisher-loc>: <publisher-name>CRC Press</publisher-name>), <fpage>121</fpage>&#x02013;<lpage>134</lpage>.</citation>
</ref>
<ref id="B64">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Suttle</surname> <given-names>C. A.</given-names></name></person-group> (<year>2005</year>). <article-title>Viruses in the sea</article-title>. <source>Nature</source> <volume>437</volume>, <fpage>356</fpage>&#x02013;<lpage>361</lpage>. <pub-id pub-id-type="doi">10.1038/nature04160</pub-id><pub-id pub-id-type="pmid">16163346</pub-id></citation>
</ref>
<ref id="B65">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>Davey</surname> <given-names>M. S.</given-names></name> <name><surname>van der Wagt</surname> <given-names>B.</given-names></name> <name><surname>Snoek</surname> <given-names>J.</given-names></name> <name><surname>Geider</surname> <given-names>R. J.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <etal/></person-group>. (<year>2001a</year>). <article-title>Co-Limitation by iron and light of <italic>Chaetoceros brevis, C. dichaeta and C. calcitrans (Bacillariophyceae)</italic></article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>217</volume>, <fpage>287</fpage>&#x02013;<lpage>297</lpage>. <pub-id pub-id-type="doi">10.3354/meps217287</pub-id></citation>
</ref>
<ref id="B66">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>Gerringa</surname> <given-names>L. J. A.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name> <name><surname>van der Wagt</surname> <given-names>B.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <name><surname>de Jong</surname> <given-names>J. T. M.</given-names></name> <etal/></person-group>. (<year>2001b</year>). <article-title>Growth rates of large and small southern ocean diatoms in relation to availability of iron in natural seawater</article-title>. <source>Limnol. Oceanogr.</source> <volume>46</volume>, <fpage>260</fpage>&#x02013;<lpage>266</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2001.46.2.0260</pub-id></citation>
</ref>
<ref id="B67">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>van der Wagt</surname> <given-names>B.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name></person-group> (<year>2004</year>). <article-title>Growth rates, half saturation constants, and silicate, nitrate, and phosphate depletion in relation to iron availability of four large open-ocean diatoms from the southern ocean</article-title>. <source>Limnol. Oceanogr.</source> <volume>49</volume>, <fpage>2141</fpage>&#x02013;<lpage>2151</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2004.49.6.2141</pub-id></citation>
</ref>
<ref id="B68">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>van den Berg</surname> <given-names>C. M. G.</given-names></name> <name><surname>Kramer</surname> <given-names>J. R.</given-names></name></person-group> (<year>1979</year>). <article-title>Determination of complexing capacities of ligands in natural waters and conditional stability constants of the copper complexes by means of manganese dioxide</article-title>. <source>Anal. Chim. Acta</source> <volume>106</volume>, <fpage>113</fpage>&#x02013;<lpage>120</lpage>.</citation>
</ref>
<ref id="B69">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>van de Poll</surname> <given-names>W. H.</given-names></name> <name><surname>Janknegt</surname> <given-names>P. J.</given-names></name> <name><surname>van Leeuwe</surname> <given-names>M. A.</given-names></name> <name><surname>Visser</surname> <given-names>R. J. W.</given-names></name> <name><surname>Buma</surname> <given-names>A. G. J.</given-names></name></person-group> (<year>2009</year>). <article-title>Excessive irradiance and antioxidant responses of an antarctic marine diatom exposed to iron limitation and to dynamic irradiance</article-title>. <source>J. Photochem. Photobiol. B</source> <volume>94</volume>, <fpage>32</fpage>&#x02013;<lpage>37</lpage>. <pub-id pub-id-type="doi">10.1016/j.jphotobiol.2008.09.003</pub-id><pub-id pub-id-type="pmid">18948012</pub-id></citation>
</ref>
<ref id="B70">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>van Leeuwe</surname> <given-names>M. A.</given-names></name> <name><surname>Stefels</surname> <given-names>J.</given-names></name></person-group> (<year>2007</year>). <article-title>Photosynthetic responses in <italic>Phaeocystis antarctica</italic> towards varying light and iron conditions</article-title>, in <source>Phaeocystis, Major Link in the Biogeochemical Cycling of Climate-Relevant Elements</source>, eds <person-group person-group-type="editor"><name><surname>van Leeuwe</surname> <given-names>M. A.</given-names></name> <name><surname>Stefels</surname> <given-names>J.</given-names></name> <name><surname>Belviso</surname> <given-names>S.</given-names></name> <name><surname>Lancelot</surname> <given-names>C.</given-names></name> <name><surname>Verity</surname> <given-names>P. G.</given-names></name> <name><surname>Gieskes</surname> <given-names>W. W. C.</given-names></name></person-group> (<publisher-loc>Dordrecht</publisher-loc>: <publisher-name>Springer</publisher-name>), <fpage>61</fpage>&#x02013;<lpage>70</lpage>.</citation>
</ref>
<ref id="B71">
<citation citation-type="web"><person-group person-group-type="author"><name><surname>Vaulot</surname> <given-names>D.</given-names></name></person-group> (<year>1989</year>). <source>CYTOPC: Processing Software for Flow Cytometric Data.</source> signal and noise 2:8. Available online at: <ext-link ext-link-type="uri" xlink:href="http://application.sb-roscoff.fr/Phyto/index.php">http://application.sb-roscoff.fr/Phyto/index.php</ext-link></citation>
</ref>
<ref id="B72">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Vaulot</surname> <given-names>D.</given-names></name> <name><surname>Birrien</surname> <given-names>J.-L.</given-names></name> <name><surname>Marie</surname> <given-names>D.</given-names></name> <name><surname>Casotti</surname> <given-names>R.</given-names></name> <name><surname>Veldhuis</surname> <given-names>M. J. W.</given-names></name> <name><surname>Kraay</surname> <given-names>G. W.</given-names></name> <etal/></person-group>. (<year>1994</year>). <article-title>Morphology, ploidy, pigment composition, and genome size of cultured strains of <italic>Phaeocystis</italic> (Prymnesiophyceae)</article-title>. <source>J. Phycol.</source> <volume>30</volume>, <fpage>1022</fpage>&#x02013;<lpage>1035</lpage>.</citation>
</ref>
<ref id="B73">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Vaulot</surname> <given-names>D.</given-names></name> <name><surname>Eikrem</surname> <given-names>W.</given-names></name> <name><surname>Viprey</surname> <given-names>M.</given-names></name> <name><surname>Moreau</surname> <given-names>H.</given-names></name></person-group> (<year>2008</year>). <article-title>The diversity of small eukaryotic phytoplankton (&#x02264; 3 Mm) in marine ecosystems</article-title>. <source>FEMS Microbiol. Rev.</source> <volume>32</volume>, <fpage>795</fpage>&#x02013;<lpage>820</lpage>. <pub-id pub-id-type="doi">10.1111/j.1574-6976.2008.00121.x</pub-id><pub-id pub-id-type="pmid">18564290</pub-id></citation>
</ref>
<ref id="B74">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Weitz</surname> <given-names>J. S.</given-names></name> <name><surname>Wilhelm</surname> <given-names>S. W.</given-names></name></person-group> (<year>2012</year>). <article-title>Ocean viruses and their effects on microbial communities and biogeochemical cycles</article-title>. <source>F1000 Biol. Rep.</source> <volume>8</volume>, <fpage>2</fpage>&#x02013;<lpage>9</lpage>. <pub-id pub-id-type="doi">10.3410/B4-17</pub-id></citation>
</ref>
<ref id="B75">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Wilhelm</surname> <given-names>S. W.</given-names></name> <name><surname>Suttle</surname> <given-names>C. A.</given-names></name></person-group> (<year>1999</year>). <article-title>Viruses and nutrient cycles in the sea</article-title>. <source>Bioscience</source> <volume>49</volume>, <fpage>781</fpage>. <pub-id pub-id-type="doi">10.2307/1313569</pub-id></citation>
</ref>
<ref id="B76">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Zapata</surname> <given-names>M.</given-names></name> <name><surname>Rodr&#x000ED;guez</surname> <given-names>F.</given-names></name> <name><surname>Garrido</surname> <given-names>J. L.</given-names></name></person-group> (<year>2000</year>). <article-title>Separation of chlorophylls and carotenoids from marine phytoplankton: a new hplc method using a reversed phase C8 column and pyridine-containing mobile phases</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>195</volume>, <fpage>29</fpage>&#x02013;<lpage>45</lpage>. <pub-id pub-id-type="doi">10.3354/meps195029</pub-id></citation>
</ref>
<ref id="B77">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Zhang</surname> <given-names>C.</given-names></name></person-group> (<year>2014</year>). <article-title>Essential functions of iron-requiring proteins in DNA replication, repair and cell cycle control</article-title>. <source>Protein Cell</source> <volume>5</volume>, <fpage>750</fpage>&#x02013;<lpage>760</lpage>. <pub-id pub-id-type="doi">10.1007/s13238-014-0083-7</pub-id><pub-id pub-id-type="pmid">25000876</pub-id></citation>
</ref>
</ref-list>
</back>
</article>