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  • 2010-2014  (4)
  • 1980-1984  (3)
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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Aquatic plants - Ecophysiology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (224 pages)
    Edition: 1st ed.
    ISBN: 9781118803448
    DDC: 572.46
    Language: English
    Note: Intro -- Photosynthesis in the Marine Environment -- Contents -- Photosynthesis in theMarine Environment -- About the authors -- Contributing authors -- Preface -- About the companion website -- Part I Plants and the Oceans -- Introduction -- Chapter 1 The evolution of photosynthetic organisms in the oceans -- Chapter 2 The different groups of marine plants -- 2.1 Cyanobacteria -- 2.2 Eukaryotic microalgae -- 2.3 Photosymbionts -- 2.4 Macroalgae -- 2.4.1 The green algae -- 2.4.2 The brown algae -- 2.4.3 The red algae -- 2.5 Seagrasses -- Chapter 3 Seawater as a medium for photosynthesis and plant growth -- 3.1 Light -- 3.2 Inorganic carbon -- 3.2.1 pH -- 3.3 Other abiotic factors -- 3.3.1 Salinity -- 3.3.2 Nutrients -- 3.3.3 Temperature -- 3.3.4 Water velocities -- Summary notes of Part I -- Part II Mechanisms of Photosynthesis, and Carbon Acquisition in Marine Plants -- Introduction to Part II -- Chapter 4 Harvesting of light in marine plants: The photosynthetic pigments -- 4.1 Chlorophylls -- 4.2 Carotenoids -- 4.3 Phycobilins -- Chapter 5 Light reactions -- 5.1 Photochemistry: excitation, de-excitation, energy transfer and primary electron transfer -- 5.2 Electron transport -- 5.3 ATP formation -- 5.4 Alternative pathways of electron flow -- Chapter 6 Photosynthetic CO2-fixation and -reduction -- 6.1 The Calvin Cycle -- 6.2 CO2-concentrating mechanisms -- Chapter 7 Acquisition of carbon in marine plants -- 7.1 Cyanobacteria and microalgae -- 7.1.1 Cyanobacteria -- 7.1.2 Eukaryotic microalgae -- 7.2 Photosymbionts -- 7.3 Macroalgae -- 7.3.1 Use of HCO3 -- 7.3.2 Mechanisms of HCO3- use -- 7.3.3 Rubisco and macroalgal photosynthesis: The need for a CO2 concentrating mechanism -- 7.4 Seagrasses -- 7.4.1 Use of HCO3- -- 7.4.2 Mechanisms of HCO3-use -- 7.5 Calcification and photosynthesis -- Summary notes of Part II. , Part III Quantitative Measurements, and Ecological Aspects, of Marine Photosynthesis -- Introduction to Part III -- Chapter 8 Quantitative measurements -- 8.1 Gas exchange -- 8.2 How to measure gas exchange -- 8.3 Pulse amplitude modulated (PAM) fluorometry -- 8.3.1 Quantum yields -- 8.3.2 Fv∕Fm -- 8.3.3 Electron transport rates -- 8.4 How to measure PAM fluorescence -- 8.4.1 Macrophytes -- 8.4.2 Microalgae -- 8.5 What method to use: Strengths and limitations -- 8.5.1 Rapid light curves -- 8.5.2 Fv∕Fm -- 8.5.3 Alpha, "uses and misuses" -- 8.5.4 Using whole plants -- Chapter 9 Photosynthetic responses, acclimations and adaptations to light -- 9.1 Responses of high and low-light plants to irradiance -- 9.2 Light responses of cyanobacteria and microalgae -- 9.3 Light effects on photosymbionts -- 9.4 Adaptations of Carbon acquisition mechanisms to light -- 9.5 Acclimations of seagrasses to high and low irradiances -- Chapter 10 Photosynthetic acclimations and adaptations to stress in the intertidal -- 10.1 Adaptations of macrophytes to desiccation -- 10.1.1 The ever-tolerant Ulva -- 10.1.2 The intertidal Fucus -- 10.1.3 The extremely tolerant Porphyra -- 10.1.4 Acclimations of seagrasses to desiccation (or not) -- 10.2 Other stresses in the intertidal -- Chapter 11 How some marine plants modify the environment for other organisms -- 11.1 Epiphytes and other 'thieves' -- 11.2 Ulva can generate its own empires -- 11.3 Seagrasses can alter environments for macroalgae and vice versa -- 11.4 Cyanobacteria and eukaryotic microalgae -- Chapter 12 Future perspectives on marine photosynthesis -- 12.1 'Harvesting' marine plant photosynthesis -- 12.2 Predictions for the future -- 12.3 Scaling of photosynthesis towards community and ecosystem production -- Summary notes of Part III -- References -- Index.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 5 (1982), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract. The role of ‘slippage’ reactions, in the form of passive H+ uniport through CF0-CF1, ATP synthetase and breakdown of the S2 and S3 intermediates of O2 evolution, is considered in relation to the growth of phototrophic organisms at low photon fluence rates. Analysis of the limited data available suggests that adaptation (phenotypic or genotypic) to low photon fluence rates is accompanied by an increase in the ratio of light-absorbing pigments to the (potentially slippage-inducing) photosystem two units and CF0-CF1 ATP synthetases. Furthermore, organisms which are genotypically adapted to high photon fluence rates do not, when grown at low photon fluence rates, achieve the same low ratio of reaction centres to total light-harvesting pigments as is found in phototrophs genotypically adapted to low photon fluence rates. The limits to, and energy costs of, such a mechanism of adaptation to low photon fluence rates are also discussed.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology letters 10 (1981), S. 0 
    ISSN: 1574-6968
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary CO2-and O2-exchange characteristics and δ13C values have been measured in a rhodophycean haptophyte (Lemanea mamillosa), a chlorophycean haptophyte (Cladophora glomerata) and a magnoliophyte rhizophyte (Ranunculus sp.) from a 5 m stretch of the Dichty Burn near Dundee. Light-and CO2-saturated rates of photosynthesis are greatest on a dry weight basis for Cladophora and lowest for Lemanea; the order is reversed on a surface area basis. The CO2 concentration at pH 6.5 at which photosynthesis is half-saturated is 25–40 μM, with Lemanea rather lower than Cladophora or Ranunculus; these half-saturation values are similar to the free CO2 concentration in the Burn water. Lemanea cannot use HCO 3 - in photosynthesis, while Cladophora and Ranunculus can. Despite being within a factor or two of saturation with free CO2 in terms of the bulk water concentration, the growth habit of Cladophora and, particularly, Ranunculus means that the high water velocity in the Burn does not necessarily prevent C depletion effects around the plants, thus providing a possible role for HCO 3 - use by these plants. Lemanea lives in the fastest-growing parts of the Burn, and its growth habit insures that it is exposed to this high water velocity, thus minimising CO2 depletion during photosynthesis despite the low surface/volume ratio for this plant. δ13C measurements on the inorganic C in the Burn water are consistent with at least part of its excess (above air-equilibrium) inorganic C levels coming from heterotrophic activity. Lemanea has the most negative δ13C value of the three plants, consistent with CO2 use and small diffusion resistances. Ranunculus has the least negative δ13C value, consistent with some CO2 depletion and/or HCO 3 - use in situ related to a high diffusion resistance in a rhizophyte which does not have to obtain all of its N and P from the bulk water but can obtain some from the sediments. Cladophora is intermediate, suggesting some CO2 depletion and/or HCO 3 - use in this densely growing haptophyte.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2018-01-19
    Description: There has been a good deal of interest in the potential of marine vegetation as a sink for anthropogenic C emissions (“Blue Carbon”). Marine primary producers contribute at least 50% of the world’s carbon fixation and may account for as much as 71% of all carbon storage. In this paper, we analyse the current rate of harvesting of both commercially grown and wild-grown macroalgae, as well as their capacity for photosynthetically driven CO2 assimilation and growth. We suggest that CO2 acquisition by marine macroalgae can represent a considerable sink for anthropogenic CO2 emissions and that harvesting and appropriate use of macroalgal primary production could play a significant role in C sequestration and amelioration of greenhouse gas emissions.
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    PANGAEA
    In:  Supplement to: Ihnken, Sven; Roberts, Simon; Beardall, John (2011): Differential responses of growth and photosynthesis in the marine diatom Chaetoceros muelleri to CO2 and light availability. Phycologia, 50(2), 182-193, https://doi.org/10.2216/10-11.1
    Publication Date: 2024-03-15
    Description: This study investigated the impact of photon flux and elevated CO2 concentrations on growth and photosynthetic electron transport on the marine diatom Chaetoceros muelleri and looked for evidence for the presence of a CO2-concentrating mechanism (CCM). pH drift experiments clearly showed that C. muelleri has the capacity to use bicarbonate to acquire inorganic carbon through one or multiple CCMs. The final pH achieved in unbuffered cultures was not changed by light intensity, even under very low photon flux, implying a low energy demand of bicarbonate use via a CCM. In short-term pH drift experiments, only treatment with the carbonic anhydrase inhibitor ethoxyzolamide (EZ) slowed down the rise in pH considerably. EZ was also the only inhibitor that altered the final pH attained, although marginally. In growth experiments, CO2 availability was manipulated by changing the pH in closed flasks at a fixed dissolved inorganic carbon (DIC) concentration. Low-light-treated samples showed lower growth rates in elevated CO2conditions. No CO2 effect was recorded under high light exposure. The maximal photosynthetic capacity, however, increased with CO2 concentration in saturating, but not in subsaturating, light intensities. Growth and photosynthetic capacity therefore responded in opposite ways to increasing CO2 availability. The capacity to photoacclimate to high and low photon flux appeared not to be affected by CO2treatments. However, photoacclimation was restricted to growth photon fluxes between 30 and 300 µmol photons m-2 s-1. The light saturation points for photosynthetic electron transport and for growth coincided at 100 µmol photons m-2 s-1. Below 100 µmol photons m-2 s-1 the light saturation point for photosynthesis was higher than the growth photon flux (i.e. photosynthesis was not light saturated under growth conditions), whereas at higher growth photon flux, photosynthesis was saturated below growth light levels.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chaetoceros muelleri; Chromista; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Identification; Laboratory experiment; Laboratory strains; Light; Light capturing capacity; Light capturing capacity, standard devitation; Light saturation point; Light saturation point, standard deviation; Maximal electron transport rate, relative; Maximal electron transport rate, relative, standard deviation; OA-ICC; Ocean Acidification International Coordination Centre; Ochrophyta; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; pH meter (Metrohm electrodes); Phytoplankton; Primary production/Photosynthesis; Radiation, photosynthetically active; Salinity; Single species; South Pacific; Spectrofluorometry; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 981 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Li, Wei; Gao, Kunshan; Beardall, John (2012): Interactive Effects of Ocean Acidification and Nitrogen-Limitation on the Diatom Phaeodactylum tricornutum. PLoS ONE, 7(12), e51590, https://doi.org/10.1371/journal.pone.0051590
    Publication Date: 2024-05-27
    Description: Climate change is expected to bring about alterations in the marine physical and chemical environment that will induce changes in the concentration of dissolved CO2 and in nutrient availability. These in turn are expected to affect the physiological performance of phytoplankton. In order to learn how phytoplankton respond to the predicted scenario of increased CO2 and decreased nitrogen in the surface mixed layer, we investigated the diatom Phaeodactylum tricornutum as a model organism. The cells were cultured in both low CO2 (390 µatm) and high CO2 (1000 µatm) conditions at limiting (10 µmol/L) or enriched (110 µmol/L) nitrate concentrations. Our study shows that nitrogen limitation resulted in significant decreases in cell size, pigmentation, growth rate and effective quantum yield of Phaeodactylum tricornutum, but these parameters were not affected by enhanced dissolved CO2 and lowered pH. However, increased CO2 concentration induced higher rETRmax and higher dark respiration rates and decreased the CO2 or dissolved inorganic carbon (DIC) affinity for electron transfer (shown by higher values for K1/2 DIC or K1/2 CO2). Furthermore, the elemental stoichiometry (carbon to nitrogen ratio) was raised under high CO2 conditions in both nitrogen limited and nitrogen replete conditions, with the ratio in the high CO2 and low nitrate grown cells being higher by 45% compared to that in the low CO2 and nitrate replete grown ones. Our results suggest that while nitrogen limitation had a greater effect than ocean acidification, the combined effects of both factors could act synergistically to affect marine diatoms and related biogeochemical cycles in future oceans.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Bicarbonate ion; Bicarbonate ion, standard deviation; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, reciprocal of photosynthetic affinity value; Carbon, inorganic, dissolved, reciprocal of photosynthetic affinity value, standard deviation; Carbon, inorganic, dissolved, standard deviation; Carbon, organic, particulate, per cell; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, reciprocal of photosynthetic affinity value; Carbon dioxide, reciprocal of photosynthetic affinity value, standard deviation; Carbon dioxide, standard deviation; Carotenoids, standard deviation; Carotenoids per cell; Cell biovolume; Cell biovolume, standard deviation; Cell counts, percent of total; Cell counts, standard deviation; Cell size; Cell size, standard deviation; Chlorophyll a, standard deviation; Chlorophyll a per cell; Chlorophyll c, standard deviation; Chlorophyll c per cell; Chromista; Coulometric titration; Effective quantum yield; Effective quantum yield, standard deviation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Identification; Laboratory experiment; Laboratory strains; Macro-nutrients; Maximal electron transport rate, relative; Maximal electron transport rate, relative, standard deviation; Maximum photochemical quantum yield of photosystem II; Maximum photochemical quantum yield of photosystem II, standard deviation; Nitrogen, organic, particulate, per cell; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Ochrophyta; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate organic carbon content per cell, standard deviation; Particulate organic nitrogen per cell, standard deviation; pH; pH, standard deviation; Phaeodactylum tricornutum; Photochemical efficiency; Photochemical efficiency, standard deviation; Phytoplankton; Potentiometric; Primary production/Photosynthesis; Respiration; Respiration rate, oxygen, per cell; Respiration rate, oxygen, per chlorophyll a; Respiration rate, oxygen, standard deviation; Salinity; Single species; Species; Spectrophotometric; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 29292 data points
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