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  • 1985-1989  (12)
  • 2011  (566,988)
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  • 1
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    PANGAEA
    In:  Supplement to: Dupont, Lydie M; Caley, Thibaut; Kim, Jung-Hyun; Castañeda, Isla S; Malaizé, Bruno; Giraudeau, Jacques (2011): Glacial-interglacial vegetation dynamics in South Eastern Africa coupled to sea surface temperature variations in the Western Indian Ocean. Climate of the Past, 7(4), 1209-1224, https://doi.org/10.5194/cp-7-1209-2011
    Publication Date: 2024-05-27
    Description: Glacial-interglacial fluctuations in the vegetation of South Africa might elucidate the climate system at the edge of the tropics between the Indian and Atlantic Oceans. However, vegetation records covering a full glacial cycle have only been published from the eastern South Atlantic. We present a pollen record of the marine core MD96-2048 retrieved by the Marion Dufresne from the Indian Ocean ~120 km south of the Limpopo River mouth. The sedimentation at the site is slow and continuous. The upper 6 m (spanning the past 342 Ka) have been analysed for pollen and spores at millennial resolution. The terrestrial pollen assemblages indicate that during interglacials, the vegetation of eastern South Africa and southern Mozambique largely consisted of evergreen and deciduous forests. During glacials open mountainous scrubland dominated. Montane forest with Podocarpus extended during humid periods was favoured by strong local insolation. Correlation with the sea surface temperature record of the same core indicates that the extension of mountainous scrubland primarily depends on sea surface temperatures of the Agulhas Current. Our record corroborates terrestrial evidence of the extension of open mountainous scrubland (including fynbos-like species of the high-altitude Grassland biome) for the last glacial as well as for other glacial periods of the past 300 Ka.
    Keywords: Acacia; Acalypha; Acanthaceae; Afraegle; Afrormosia; Afzelia; Age model; Aizoaceae; Alchornea; Alismataceae; Allophylus; Aloe-type; Amaranthaceae/Chenopodiaceae; Anemia-type; Anthoceros; Anthospermum; Artemisia (Africa); Avicennia; Balanites; Baphia-type; Blighia-type; Borassus-type; Borreria; Boscia-type; Brachystegia; Bridelia; Burkea; Butyrospermum; Buxus-type madagascaria; Caesalpinioideae; CALYPSO; Calypso Corer; Campanulaceae; Canthium; Caperonia; Capparis; Caryophyllaceae; Cassia-type; Casuarina; Celastraceae/Hippocrateaceae; Celtis; Center for Marine Environmental Sciences; Cephalosphaera; Chrysophyllum; Cissus; Clematis-type; Cleome; Cliffortia; Cnestis-type; Coffea-type; Cola cordifolia; Combretaceae/Melastomataceae; Commelinaceae; Commiphora; Compositae Liguliflorae; Compositae Tubuliflorae; Compositae Vernonieae; Cotula-type; Counting, palynology; Crossopteryx; Crotalaria; Croton-type; Cucumis; Cussonia; Cuviera; Cynometra-type; Cyperaceae (africa); Daisy-type; Daniellia-type; Deinbollia-type; DEPTH, sediment/rock; Dialium-type; Dicliptera-type; Diospyros; Dodonaea villosa; Dombeya-type; Dracaena; Elaeis guineensis; Erica (Africa); Erythrina; Euclea; Eugenia; Euphorbia; Euphorbiaceae undifferentiated; Evolvulus-type; Fadogia-type; Fagonia; Fern spores; Flabellaria; Gaertnera; Galium; Garcinia; Gazania-type; Grewia; Gunnera perpensa; Haplocoelum; Heritiera-type; Hermannia; Hymenocardia; Hyphaene; Hypoestes type; Ilex cf.. mitis; Indigofera-type; Isoberlinia-type; Justicia-type; Khaya; Kigelia-type; Klaineanthus; Lannea; Leea; Leonotis; Liliaceae; Limnophyton-type; Lobelia (Africa); Lonchocarpus; Lophira; Luffa; Lumnitzera racemosa; Lycopodium (Africa); Lycopodium cernuum; Macaranga; Mallotus; Manilkara; Marion Dufresne (1995); Marker, added; Marker, found; MARUM; MD104; MD96-2048; Melochia; Millettia; Mimosoideae; Mitragyna; Moraceae; Morelia senegalensis; Myrica; Myrsine africana; Nyctaginaceae; Nymphaea; Ochna; Ocimum; Olea; Ormocarpum; Oxygonum; Pandanus; Papilionoideae; Parinari; Passerina montana; PEGASE; Pelargonium; Peltophorum africanum; Pentabrachion-type reticulatum; Pentzia-type; Petalidium; Petersianthus macrocarpus; Phaeoceros; Phoenix; Piliostigma; Piptadeniastrum-type africanum; Plantago; Poaceae undifferentiated; Podocarpus; Pollen, total; Polycarpaea-type; Polygonum aviculare-type; Polygonum senegalense-type; Protea; Pseudolachnostylis-type; Psychotria; Psydrax-type subcordata; Pteris; Pterocarpus; Raphia; Rauvolfia; Restionaceae; Rhamnaceae; Rhizophora; Rhus-type; Rhynchosia-type; Rubiaceae monade; Ruellia; Rumex; Sapotaceae; Sapotaceae/Meliaceae; Scabiosa-type; Schefflera; Schrebera; Scrophulariaceae (Africa); Securinega; Selago-type; Solanum; Sorindeia-type juglandifolia; Spirostachys africana; Stephanocolporate striatoreticulate; Sterculia-type; Stereospermum; Stipularia africana; Stoebe-type; Strophanthus-type; Strychnos; Sutera-type; Tamarindus-type indica; Tapinanthus; Teclea-type; Tephrosia-type; Tetrorchidium; Thymelaeaceae; Tribulus; Trichilia; Typha angustifolia-type; Uapaca; Urticaceae; Volume; Waltheria; Zaluzianskya-type; Zanthoxylum; Ziziphus-type; Zygophyllum
    Type: Dataset
    Format: text/tab-separated-values, 24360 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Borchard, Corinna; Borges, Alberto Vieira; Händel, Nicole; Engel, Anja (2011): Biogeochemical response of Emiliania huxleyi (PML B92/11) to elevated CO2 and temperature under phosphorous limitation: A chemostat study. Journal of Experimental Marine Biology and Ecology, 410, 61-71, https://doi.org/10.1016/j.jembe.2011.10.004
    Publication Date: 2024-05-27
    Description: The present study investigates the combined effect of phosphorous limitation, elevated partial pressure of CO2 (pCO2) and temperature on a calcifying strain of Emiliania huxleyi (PML B92/11) by means of a fully controlled continuous culture facility. Two levels of phosphorous limitation were consecutively applied by renewal of culture media (N:P = 26) at dilution rates (D) of 0.3 d- and 0.1 d-1. CO2 and temperature conditions were 300, 550 and 900 µatm pCO2 at 14 °C and 900 µatm pCO2 at 18 °C. In general, the steady state cell density and particulate organic carbon (POC) production increased with pCO2, yielding significantly higher concentrations in cultures grown at 900 µatm pCO2 compared to 300 and 550 µatm pCO2. At 900 µatm pCO2, elevation of temperature as expected for a greenhouse ocean, further increased cell densities and POC concentrations. In contrast to POC concentration, C-quotas (pmol C cell-1) were similar at D = 0.3 d-1 in all cultures. At D = 0.1 d-1, a reduction of C-quotas by up to 15% was observed in the 900 µatm pCO2 at 18 °C culture. As a result of growth rate reduction, POC:PON:POP ratios deviated strongly from the Redfield ratio, primarily due to an increase in POC. Ratios of particulate inorganic and organic carbon (PIC:POC) ranged from 0.14 to 0.18 at D = 0.3 d-1, and from 0.11 to 0.17 at D = 0.1 d-1, with variations primarily induced by the changes in POC. At D = 0.1 d-1, cell volume was reduced by up to 22% in cultures grown at 900 µatm pCO2. Our results indicate that changes in pCO2, temperature and phosphorus supply affect cell density, POC concentration and size of E. huxleyi (PML B92/11) to varying degrees, and will likely impact bloom development as well as biogeochemical cycling in a greenhouse ocean.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated, see reference(s); Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, organic, particulate; Carbon, organic, particulate, production per cell; Carbon, organic, particulate/Nitrogen, organic, particulate ratio; Carbon, organic, particulate/Phosphorus, organic, particulate ratio; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Colorimetry; Element analyser CNS, EURO EA; Emiliania huxleyi; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Experiment day; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Haptophyta; Infrared gas analyzer (LI-COR LI-6252); Laboratory experiment; Laboratory strains; Light:Dark cycle; Macro-nutrients; Measured; Nitrate; Nitrogen, inorganic, dissolved; Nitrogen, organic; Nitrogen, organic, particulate/Phosphorus, organic, particulate ratio; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate organic carbon, per cell; Particulate organic carbon production; Particulate organic nitrogen per cell; Particulate organic nitrogen production; Particulate organic phosphorus per cell; Particulate organic phosphorus production; Pelagos; pH; Phosphate; Phosphorus, inorganic; Phosphorus, organic, particulate; Phosphorus, organic, particulate, production per cell; Phytoplankton; Primary production/Photosynthesis; Production of particulate organic nitrogen; Radiation, photosynthetically active; Revelle factor; Salinity; Salinometer - Tropic Marin Sea Salt, Dr. Biener GmbH, Germany; Sample ID; Single species; Spectrophotometry; Temperature; Temperature, water; WTW 340i pH-analyzer and WTW SenTix 81-electrode
    Type: Dataset
    Format: text/tab-separated-values, 1068 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Krug, Sebastian; Schulz, Kai Georg; Riebesell, Ulf (2011): Effects of changes in carbonate chemistry speciation on Coccolithus braarudii: a discussion of coccolithophorid sensitivities. Biogeosciences, 8(3), 771-777, https://doi.org/10.5194/bg-8-771-2011
    Publication Date: 2024-05-27
    Description: Ocean acidification and associated shifts in carbonate chemistry speciation induced by increasing levels of atmospheric carbon dioxide (CO2) have the potential to impact marine biota in various ways. The process of biogenic calcification, for instance, is usually shown to be negatively affected. In coccolithophores, an important group of pelagic calcifiers, changes in cellular calcification rates in response to changing ocean carbonate chemistry appear to differ among species. By applying a wider CO2 range we show that a species previously reported insensitive to seawater acidification, Coccolithusbraarudii, responds both in terms of calcification and photosynthesis, although at higher levels of CO2. Thus, observed differences between species seem to be related to individual sensitivities while the underlying mechanisms could be the same. On this basis we develop a conceptual model of coccolithophorid calcification and photosynthesis in response to CO2-induced changes in seawater carbonate chemistry speciation.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calculated, see reference(s); Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, production per cell; Carbon, organic, particulate/Nitrogen, organic, particulate ratio; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Coccolithus braarudii; Coccolithus braarudii, size; Coccolithus braarudii, size, standard deviation; Coulter counter; 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; Haptophyta; Identification; Laboratory experiment; Laboratory strains; Light:Dark cycle; Measured; Nitrate; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon/particulate organic carbon ratio; Pelagos; pH; Phosphate; Photometrically using autoanalyzer QUAATRO; Phytoplankton; Primary production/Photosynthesis; Radiation, photosynthetically active; Salinity; Single species; South Atlantic; Temperature, water; Thermal conductivity meter; Titration potentiometric, 794 Basic Titrino (Metrohm)
    Type: Dataset
    Format: text/tab-separated-values, 930 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Langer, Gerald; Bode, Maya (2011): CO2 mediation of adverse effects of seawater acidification in Calcidiscus leptoporus. Geochemistry, Geophysics, Geosystems, 12(5), Q05001, https://doi.org/10.1029/2010GC003393
    Publication Date: 2024-05-27
    Description: The coccolithophore Calcidiscus leptoporus (strain RCC1135) was grown in dilute batch culture at CO2 levels ranging from ~200 to ~1600 µatm. Increasing CO2 concentration led to an increased percentage of malformed coccoliths and eventually (at ~1500 µatm CO2) to aggregation of cells. Carbonate chemistry of natural seawater was manipulated in three ways: first, addition of acid; second, addition of a HCO3/CO3 solution; and third, addition of both acid and HCO3/CO3 solution. The data set allowed the disentangling of putative effects of the different parameters of the carbonate system. It is concluded that CO2 is the parameter of the carbonate system which causes both aberrant coccolithogenesis and aggregation of cells.
    Keywords: Alkalinity, Gran titration (Gran, 1950); Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcidiscus leptoporus; Calcidiscus leptoporus, morphology; Calcidiscus leptoporus, morphology, standard deviation; Calcification/Dissolution; Calcite saturation state; Calculated; Calculated, see reference(s); Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, per cell; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, per cell; Carbon, organic, particulate, production per cell; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Conductivity meter (WTW, Weilheim, Gemany); 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); Gas chromatography (EURO EA Elemental Analyser, EUROVECTOR); Growth/Morphology; Growth rate; Growth rate, standard deviation; Haptophyta; Identification; Laboratory experiment; Laboratory strains; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon, production, standard deviation; Particulate inorganic carbon/particulate organic carbon ratio; Particulate inorganic carbon/particulate organic carbon ratio, standard deviation; Particulate inorganic carbon per cell, standard deviation; Particulate organic carbon, production, standard deviation; Particulate organic carbon content per cell, standard deviation; Pelagos; pH; Photometrically using autoanalyzer QUAATRO; Phytoplankton; Primary production/Photosynthesis; Salinity; Single species; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 246 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Hoppe, Clara Jule Marie; Langer, Gerald; Rost, Björn (2011): Emiliania huxleyi shows identical responses to elevated pCO2 in TA and DIC manipulations. Journal of Experimental Marine Biology and Ecology, 406(1-2), 54-62, https://doi.org/10.1016/j.jembe.2011.06.008
    Publication Date: 2024-05-27
    Description: With respect to their sensitivity to ocean acidification, calcifiers such as the coccolithophore Emiliania huxleyi have received special attention, as the process of calcification seems to be particularly sensitive to changes in the marine carbonate system. For E. huxleyi, apparently conflicting results regarding its sensitivity to ocean acidification have been published (Iglesias-Rodriguez et al., 2008a; Riebesell et al., 2000). As possible causes for discrepancies, intra-specific variability and different effects of CO2 manipulation methods, i.e. the manipulation of total alkalinity (TA) or total dissolved inorganic carbon (DIC), have been discussed. While Langer et al. (2009) demonstrate a high degree of intra-specific variability between strains of E. huxleyi, the question whether different CO2 manipulation methods influence the cellular responses has not been resolved yet. In this study, closed TA as well as open and closed DIC manipulation methods were compared with respect to E. huxleyi's CO2-dependence in growth rate, POC- and PIC-production. The differences in the carbonate chemistry between TA and DIC manipulations were shown not to cause any differences in response patterns, while the latter differed between open and closed DIC manipulation. The two strains investigated showed different sensitivities to acidification of seawater, RCC1256 being more negatively affected in growth rates and PIC production than NZEH.
    Keywords: Alkalinity, Gran titration (Gran, 1950); Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, per cell; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, per cell; Carbon, organic, particulate, production per cell; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Comment; Emiliania huxleyi; 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; Haptophyta; Laboratory experiment; Laboratory strains; Mass spectrometer ANCA-SL 20-20 Europa Scientific; Mediterranean Sea Acidification in a Changing Climate; MedSeA; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon/particulate organic carbon ratio; Pelagos; pH; Phytoplankton; Primary production/Photosynthesis; Salinity; Sample ID; Seal QuAAtro SFA Analyzer, Seal Analytical, 800 TM; Single species; South Pacific; Species; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1638 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Bach, Lennart Thomas; Riebesell, Ulf; Schulz, Kai Georg (2011): Distinguishing between the effects of ocean acidification and ocean carbonation in the coccolithophore Emiliania huxleyi. Limnology and Oceanography, 56(6), 2040-2050, https://doi.org/10.4319/lo.2011.56.6.2040
    Publication Date: 2024-05-27
    Description: The coccolithophore Emiliania huxleyi was cultured under a broad range of carbonate chemistry conditions to distinguish the effects of individual carbonate system parameters on growth, primary production, and calcification. In the first experiment, alkalinity was kept constant and the fugacity of CO2(fCO2) varied from 2 to 600 Pa (1Pa ~ 10 µatm). In the second experiment, pH was kept constant (pHfree = 8) with fCO2 varying from 4 to 370 Pa. Results of the constant-alkalinity approach revealed physiological optima for growth, calcification, and organic carbon production at fCO2 values of ~20Pa, ~40 Pa, and ~80 Pa, respectively. Comparing this with the constant-pH approach showed that growth and organic carbon production increased similarly from low to intermediate CO2 levels but started to diverge towards higher CO2 levels. In the high CO2 range, growth rates and organic carbon production decreased steadily with declining pH at constant alkalinity while remaining consistently higher at constant pH. This suggests that growth and organic carbon production rates are directly related to CO2 at low (sub-saturating) concentrations, whereas towards higher CO2 levels they are adversely affected by the associated decrease in pH. A pH dependence at high fCO2 is also indicated for calcification rates, while the key carbonate system parameter determining calcification at low fCO2 remains unclear. These results imply that key metabolic processes in coccolithophores have their optima at different carbonate chemistry conditions and are influenced by different parameters of the carbonate system at both sides of the optimum.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, production per cell; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a production per cell; Chromista; Emiliania huxleyi; Emiliania huxleyi, diameter; 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); Fugacity of carbon dioxide in seawater, standard deviation; Growth/Morphology; Growth rate; Haptophyta; Laboratory experiment; Laboratory strains; Light:Dark cycle; Measured; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon/particulate organic carbon ratio; Pelagos; pH; Photometry; Phytoplankton; Pigments, Turner fluorometer; Potentiometric open-cell titration; Primary production/Photosynthesis; Radiation, photosynthetically active; Salinity; Scanning electron microscope (SEM); Single species; Temperature, water; Titration potentiometric
    Type: Dataset
    Format: text/tab-separated-values, 1396 data points
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  • 7
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    PANGAEA
    In:  Laboratoire d'Océanographie de Villefranche | Supplement to: Fiorini, Sarah; Middelburg, Jack J; Gattuso, Jean-Pierre (2011): Effects of elevated CO2 partial pressure and temperature on the coccolithophore Syracosphaera pulchra. Aquatic Microbial Ecology, 64(3), 221-232, https://doi.org/10.3354/ame01520
    Publication Date: 2024-05-27
    Description: The response of three coccolithophores (Emiliania huxleyi, Calcidiscus leptoporus and Syracosphaera pulchra) to elevated partial pressure (pCO2) of carbon dioxide was investigated in batch cultures. For the first time, we also report on the response of the non calcifying (haploid) life stage of these three species. The growth rate, cell size, inorganic (PIC) and organic carbon (POC) of both life stages were measured at two different pCO2 (400and 760 ppm) and their organic and inorganic carbon production calculated. The two lifestages within the same species generally exhibited a similar response to elevated pCO2, theresponse of the haploid stage being often more pronounced than that of the diploid stage. Thegrowth rate was consistently higher at higher pCO2 but the response of other processes varied among species. The calcification rate of C. leptoporus and of S. pulchra did not change at elevated pCO2 while increased in E. huxleyi. The POC production as well as the cell size of both life stages of S. pulchra and of the haploid stage of E. huxleyi markedly decreased at elevated pCO2. It remained unaltered in the diploid stage of E. huxleyi and C. leptoporus and increased in the haploid stage of the latter. The PIC:POC ratio increased in E. huxleyi and was constant in C. leptoporus and S. pulchra. These results suggest that the non-calcifying stage, is more responsive than the calcifying stage and that the most versatile genera will proliferate in a more acidic ocean rather than all coccolithophores will decline.
    Keywords: Alkalinity, Gran titration (Gran, 1950); Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcidiscus leptoporus; Calcification/Dissolution; Calcite saturation state; Calculated; Calculated, see reference(s); Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, per cell; Carbon, organic, particulate; Carbon, organic, particulate, per cell; Carbon, total, particulate; Carbon, total, particulate, per cell; Carbon, total, particulate, production per cell; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Coulter Counter (Beckman Coulter); Emiliania huxleyi; 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; Haptophyta; Laboratory experiment; Laboratory strains; Light:Dark cycle; Mass spectrometer Thermo Electron Flash EA 1122 Analyzer; Measured; Mediterranean Sea; Nitrogen; Nitrogen, total; Nitrogen per cell; OA-ICC; Ocean Acidification International Coordination Centre; 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; Sample ID; Single species; Skalar AutoAnalyser; Species; Suspended particulate matter; Syracosphaera pulchra; Temperature; Temperature, water; Transparent exopolymer particles; Transparent exopolymer particles per cell
    Type: Dataset
    Format: text/tab-separated-values, 1536 data points
    Location Call Number Expected Availability
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  • 8
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    PANGAEA
    In:  Supplement to: Fiorini, Sarah; Middelburg, Jack J; Gattuso, Jean-Pierre (2011): Testing the effects of elevated pCO2 on coccolithophores (Prymnesiophyceae): comparison between haploid and diploid life stages. Journal of Phycology, 47(6), 1281–1291, https://doi.org/10.1111/j.1529-8817.2011.01080.x
    Publication Date: 2024-05-27
    Description: The response of Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler, Calcidiscus leptoporus (G. Murray et V. H. Blackman) J. Schiller, andSyracosphaera pulchra Lohmann to elevated partial pressure of carbon dioxide (pCO2) was investigated in batch cultures. We reported on the response of both haploid and diploid life stages of these three species. Growth rate, cell size, particulate inorganic carbon (PIC), and particulate organic carbon (POC) of both life stages were measured at two different pCO2 (400 and 760 parts per million [ppm]), and their organic and inorganic carbon production were calculated. The two life stages within the same species generally exhibited a similar response to elevated pCO2, the response of the haploid stage being often more pronounced than that of the diploid stage. The growth rate was consistently higher at elevated pCO2, but the response of other processes varied among species. Calcification rate of C. leptoporusand of S. pulchra did not change at elevated pCO2, whereas it increased in E. huxleyi. POC production and cell size of both life stages of S. pulchra and of the haploid stage of E. huxleyi markedly decreased at elevated pCO2. It remained unaltered in the diploid stage of E. huxleyi and C. leptoporus and increased in the haploid stage of the latter. The PIC:POC ratio increased in E. huxleyi and was constant in C. leptoporus and S. pulchra. Elevated pCO2 has a significant effect on these three coccolithophore species, the haploid stage being more sensitive. This effect must be taken into account when predicting the fate of coccolithophores in the future ocean.
    Keywords: Alkalinity, Gran titration (Gran, 1950); Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcidiscus leptoporus; Calcidiscus leptoporus, standard deviation; Calcification/Dissolution; Calcite saturation state; Calculated; Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, per cell; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, per cell; Carbon, organic, particulate, production per cell; Carbon/Nitrogen ratio; Carbon/Nitrogen ratio, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Element analyser, Thermo Finnigan flash EA 1112; Emiliania huxleyi; Emiliania huxleyi, standard deviation; 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; Haptophyta; Identification; Laboratory experiment; Laboratory strains; Lemaur hemocytometer (Fisher Scientific); Light:Dark cycle; Measured; Nitrate; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon, production, standard deviation; Particulate inorganic carbon/particulate organic carbon ratio; Particulate inorganic carbon/particulate organic carbon ratio, standard deviation; Particulate inorganic carbon per cell, standard deviation; Particulate organic carbon, production, standard deviation; Particulate organic carbon content per cell, standard deviation; Pelagos; pH; pH meter (Metrohm electrodes); Phosphate; Phytoplankton; Phytoplankton, cell biovolume; Phytoplankton, cell biovolume, standard deviation; Primary production/Photosynthesis; Radiation, photosynthetically active; Salinity; Single species; South Pacific; Species; Syracosphaera pulchra; Syracosphaera pulchra, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 492 data points
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  • 9
    Publication Date: 2024-05-27
    Keywords: Alkalinity, Gran titration (Gran, 1950); Alkalinity, total; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calculated, see reference(s); Calculated using seacarb; Carbon, inorganic, dissolved; Carbon, inorganic, particulate, per cell; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, per cell; Carbon, organic, particulate, production per cell; Carbonate ion; Chromista; DATE/TIME; Emiliania huxleyi; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; FACSCalibur flow-cytometer (Becton Dickinson); Growth/Morphology; Growth rate; Haptophyta; Identification; Laboratory experiment; Laboratory strains; Mass spectrometer Thermo Electron Flash EA 1122 Analyzer; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon/particulate organic carbon ratio; Particulate inorganic carbon/particulate organic carbon ratio, standard deviation; Pelagos; pH; pH meter (Metrohm, 826 pH mobile); Phytoplankton; Primary production/Photosynthesis; Salinity; Single species; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 10
    Publication Date: 2024-05-23
    Repository Name: EPIC Alfred Wegener Institut
    Type: Other , notRev
    Format: application/pdf
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