15 research outputs found

    Effect of elevated <i>p</i>CO<sub>2</sub> on gene regulation.

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    <p>Number of readings found for genes associated to ion transport and C<sub>i</sub> acquisition in the 150 µatm and 1400 µatm CO<sub>2</sub> treatments relative to the present-day (380 µatm) CO<sub>2</sub> treatment.</p

    Conceptual model of regulated proteins in a <i>T. heimii</i> cell.

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    <p>The regulated proteins involved in ion transport and C<sub>i</sub> acquisition are shown on their putative locations <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0065987#pone.0065987-Mackinder1" target="_blank">[39]</a>, <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0065987#pone.0065987-Reinfelder1" target="_blank">[49]</a>, <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0065987#pone.0065987-Taylor2" target="_blank">[57]</a><b>.</b> Proteins involved in vacuolar Ca<sup>2+</sup> and H<sup>+</sup> transport include P-type Ca<sup>2+</sup> ATPases (P-ATPase), Ca<sup>2+</sup>/Na<sup>+</sup> exchangers (NCX), Ca<sup>2+</sup>/H<sup>+</sup> antiporters (VCX), and vacuolar H<sup>+</sup> ATPases (V-ATPase). Active uptake of HCO<sub>3</sub><sup>−</sup> may occur via a SLC4 family anion exchanger (AE) or an SLC26 family SO<sub>4</sub><sup>3−/</sup>HCO<sub>3</sub><sup>−/</sup>C<sub>2</sub>O<sub>4</sub><sup>2−</sup> anion exchanger (SAT-1). Carbonic anhydrases (CA) are located intracellularly or extracellularly and enhance the interconversion between CO<sub>2</sub> and HCO<sub>3</sub><sup>−</sup>.</p

    Effect of elevated <i>p</i>CO<sub>2</sub> on cyst morphology.

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    <p>Cells grown under (A–C) 150 µatm CO<sub>2</sub> and (D–H) 1400 µatm CO<sub>2</sub>. Black arrows indicate cysts that are shown in detailed images, white arrows show collapsed cysts.</p

    Effect of increasing CO<sub>2</sub> concentrations on the stable isotope composition.

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    <p>(A) <sup>13</sup>C fractionation of organic carbon (ε<sub>p</sub>) and calcite (ε<sub>k</sub>), (B) <sup>18</sup>O composition of calcite (δ<sup>18</sup>O<sub>calcite</sub>) and DIC (δ<sup>18</sup>O<sub>DIC</sub>), and (C) relationship between the oxygen isotopic composition of calcite (δ<sup>18</sup>O<sub>calcite-water</sub>) in <i>Thoracosphaera</i> from this study (open diamonds) and from Ziveri et al. <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0065987#pone.0065987-Ziveri1" target="_blank">[9]</a> (grey diamonds). Horizontal lines in (B) indicate δ<sup>18</sup>O values for HCO<sub>3</sub><sup>−</sup> and CO<sub>3</sub><sup>2−</sup>, and dashed line indicates trend of curve. Solid lines indicate linear regressions (<i>n</i> = 12) with (A) ε<sub>p</sub>: R<sup>2</sup> = 0.75, P<0.001, and ε<sub>k</sub>: R<sup>2</sup> = 0.90, P<0.001, (B) δ<sup>18</sup>O<sub>DIC</sub>: R<sup>2</sup> = 0.76, P<0.001, and (C) This study: R<sup>2</sup> = 0.99, P<0.001, and Ziveri et al. (2012), (<i>n</i> = 7): R<sup>2</sup> = 0.95, P<0.001.</p

    Combined effect of elevated pCO<sub>2</sub> and nitrogen-limitation.

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    <p>(A, B) POC production, (C, D) Chl-a:POC ratios and (E, F) ε<sub>p</sub> versus CO<sub>2</sub> of <i>A</i>. <i>fundyense</i> (left) and <i>S</i>. <i>trochoidea</i> (right) cultured under nitrogen-replete conditions (HN; filled symbols) and nitrogen-limited conditions (LN; open symbols). Linear trend lines, R<sup>2</sup> and P-values represent statistically significant relationships. Symbols indicate means of technical replicates. Means ± SD for all treatments are provided in <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0154370#pone.0154370.t002" target="_blank">Table 2</a>. POC production and Chl-a:POC ratios have previously been published in [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0154370#pone.0154370.ref015" target="_blank">15</a>] and [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0154370#pone.0154370.ref018" target="_blank">18</a>], and ε<sub>p</sub> in the HN treatments in Hoins et al. 2015.</p

    Conceptual model of a dinoflagellate cell and processes at the thylakoid membrane of the chloroplasts.

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    <p>(A) high-light (HL) and nitrogen-replete (HN) conditions, (B) low-light conditions (LL) and (C) nitrogen-limitation (LN). Processes potentially influencing <sup>13</sup>C fractionation ([1]–[8]) are highlighted in red, while + and − refer to an increase or decrease in <sup>13</sup>C fractionation, respectively. (A) Saturating light and nutrient-replete conditions: Light provides the energy (= photons) needed for Photosystem II (PSII; in thylakoid membrane) to oxidize water to O<sub>2</sub>, thereby producing electrons (e<sup>-</sup>) and protons (H<sup>+</sup>). Electrons are transported by plastohydroquinone (PQ), thereby pumping more protons into the lumen. The cytochrome b<sub>6</sub>f complex oxidizes PQ molecules, thereby producing electrons, which are then transported to Photosystem I (PSI) where they reduce NADP<sup>+</sup> to NADPH. Protons are transported to F-ATPase to synthesize ATP. (B) Under light-limitation, the overall decreased amount of energy arriving at PSII causes a decrease in water oxidation, thereby producing less electrons and protons, and thus also less ATP and NADPH. (C) Under nitrogen-limitation, less NADPH is needed for NO<sub>3</sub><sup>-</sup> reduction, thus the excess electrons are transported back to PSII by cyclic energy flow. Protons are still pumped by F-ATPase, thereby increasing the amount of ATP synthesized.</p

    Combined effect of elevated pCO<sub>2</sub> and light-limitation.

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    <p>(A, B) POC production, (C, D) Chl-a:POC ratios and (E, F) ε<sub>p</sub> versus CO<sub>2</sub> of <i>G</i>. <i>spinifera</i> (left) and <i>P</i>. <i>reticulatum</i> (right). Linear trend lines, R<sup>2</sup> and P-values represent statistically significant relationships. Symbols indicate means of technical replicates. Means ± SD for all treatments are provided in <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0154370#pone.0154370.t001" target="_blank">Table 1</a>. Note that the trend line for <i>G</i>. <i>spinifera</i> under HL excludes the highest <i>p</i>CO<sub>2</sub> treatment (see also [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0154370#pone.0154370.ref016" target="_blank">16</a>]). ε<sub>p</sub> in the HL treatments have previously been published in Hoins et al. 2015.</p

    Overview of the growth parameters in the HL and LL treatments.

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    <p>Growth rate (μ, d<sup>-1</sup>), POC quota (pg C cell<sup>-1</sup>), Chl-a content (pg cell<sup>-1</sup>) and <sup>13</sup>C fractionation ε<sub>p</sub> (‰) of <i>G</i>. <i>spinifera</i> and <i>P</i>. <i>reticulatum</i> grown under high-light and low-light conditions. Values represent the mean of triplicate incubations (n = 3 ±SD). Superscript letters indicate significant differences between <i>p</i>CO<sub>2</sub> treatments (P<0.05). Superscript symbols refer to earlier published data in Hoins et al. 2015 (*).</p

    Combined Effects of Ocean Acidification and Light or Nitrogen Availabilities on <sup>13</sup>C Fractionation in Marine Dinoflagellates

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    <div><p>Along with increasing oceanic CO<sub>2</sub> concentrations, enhanced stratification constrains phytoplankton to shallower upper mixed layers with altered light regimes and nutrient concentrations. Here, we investigate the effects of elevated <i>p</i>CO<sub>2</sub> in combination with light or nitrogen-limitation on <sup>13</sup>C fractionation (ε<sub>p</sub>) in four dinoflagellate species. We cultured <i>Gonyaulax spinifera</i> and <i>Protoceratium reticulatum</i> in dilute batches under low-light (‘LL’) and high-light (‘HL’) conditions, and grew <i>Alexandrium fundyense</i> and <i>Scrippsiella trochoidea</i> in nitrogen-limited continuous cultures (‘LN’) and nitrogen-replete batches (‘HN’). The observed CO<sub>2</sub>-dependency of ε<sub>p</sub> remained unaffected by the availability of light for both <i>G</i>. <i>spinifera</i> and <i>P</i>. <i>reticulatum</i>, though at HL ε<sub>p</sub> was consistently lower by about 2.7‰ over the tested CO<sub>2</sub> range for <i>P</i>. <i>reticulatum</i>. This may reflect increased uptake of (<sup>13</sup>C-enriched) bicarbonate fueled by increased ATP production under HL conditions. The observed CO<sub>2</sub>-dependency of ε<sub>p</sub> disappeared under LN conditions in both <i>A</i>. <i>fundyense</i> and <i>S</i>. <i>trochoidea</i>. The generally higher ε<sub>p</sub> under LN may be associated with lower organic carbon production rates and/or higher ATP:NADPH ratios. CO<sub>2</sub>-dependent ε<sub>p</sub> under non-limiting conditions has been observed in several dinoflagellate species, showing potential for a new CO<sub>2</sub>-proxy. Our results however demonstrate that light- and nitrogen-limitation also affect ε<sub>p</sub>, thereby illustrating the need to carefully consider prevailing environmental conditions.</p></div

    Overview of the growth parameters in the HN and LN treatments.

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    <p>Growth rate (μ, d<sup>-1</sup>), POC quota (pg C cell<sup>-1</sup>), Chl-a (pg cell<sup>-1</sup>), POC:PON ratios (molar) and ε<sub>p</sub> (‰) of <i>A</i>. <i>fundyense</i> and <i>S</i>. <i>trochoidea</i> grown under nitrogen-replete conditions and nitrogen-limitation. Values represent the mean of duplicate incubations (n = 2 ±SD). Superscript letters indicate significant differences between <i>p</i>CO<sub>2</sub> treatments (ANOVA; P<0.05; only applied when n>2). Superscript symbols refer to earlier published data in Hoins et al. 2015 (*), and Eberlein et al. 2014 (†) and 2016 (‡).</p
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