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  • 1
    Keywords: Hochschulschrift ; Zooplankton ; Verkalkung
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (72 Seiten = 10 MB) , Illustrationen, Graphen
    Edition: 2021
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 2
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource
    DDC: 570
    Language: English
    Note: Kiel, Univ., Diss., 2010
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  • 3
    Publication Date: 2021-02-08
    Description: Long-term time series data show that ocean acidification is occurring in the subtropical oceans. As a component of an in situ mesocosm experiment carried out offGran Canaria in the subtropical North Atlantic, we examined the influence of ocean acidification on the net production of dimethylsulfide (DMS). Over 23 days under oligotrophic conditions, time-integrated DMS concentrations showed an inverse relationship of -0.21 ± 0.02 nmol DMS nmol-1 H+ across the gradient of H+ concentration of 8.8-23.3 nmol l-1, equivalent to a range of pCO2 of 400-1,252 atm. Proportionally similar decreases in the concentrations of both dissolved and particulate dimethylsulfoniopropionate (DMSP) were observed in relation to increasing H+ concentration between the mesocosms. The reduced net production of DMSP with increased acidity appeared to result from a decrease in abundance of a DMSP-rich nanophytoplankton population. A 35S-DMSP tracer approach was used to determine rates of dissolved DMSP catabolism, including DMS production, across the mesocosm treatments. Over a phase of increasing DMS concentrations during the experiment, the specific rates of DMS production were significantly reduced at elevated H+ concentration. These rates were closely correlated to the rates of net DMS production indicating that transformation of dissolved DMSP to DMS by bacteria was a major component of DMS production. It was not possible to resolve whether catabolism of DMSP was directly influenced by H+ concentrations or was an indirect response in the bacterial community composition associated with reduced DMSP availability. There is a pressing need to understand how subtropical planktonic communities respond to the predicted gradual prolonged ocean acidification, as alterations in the emission of DMS from the vast subtropical oceans could influence atmospheric chemistry and potentially climate, over a large proportion of the Earth's surface.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2017-06-29
    Type: Article , NonPeerReviewed
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  • 5
    Publication Date: 2019-09-23
    Description: To understand the influence of changing surface ocean pH and carbonate chemistry on the coccolithophore Emiliania huxleyi, it is necessary to characterize mechanisms involved in pH homeostasis and ion transport. Here, we measured effects of changes in seawater carbonate chemistry on the fluorescence emission ratio of BCECF (2',7'-bis-(2-carboxyethyl)-5-(and-6)-carboxyfluorescein) as a measure of intracellular pH (pH(i)). Out of equilibrium solutions were used to differentiate between membrane permeation pathways for H+, CO(2) and HCO(3)-. Changes in fluorescence ratio were calibrated in single cells, resulting in a ratio change of 0.78 per pH(i) unit. pH(i) acutely followed the pH of seawater (pH(e)) in a linear fashion between pH(e) values of 6.5 and 9 with a slope of 0.44 per pH(e) unit. pH(i) was nearly insensitive to changes in seawater CO(2) at constant pH(e) and HCO(3)-. An increase in extracellular HCO(3)- resulted in a slight intracellular acidification. In the presence of DIDS (4,4'-diisothiocyanatostilbene-2,2'-disulfonic acid), a broad-spectrum inhibitor of anion exchangers, E. huxleyi acidified irreversibly. DIDS slightly reduced the effect of pH(e) on pH(i). The data for the first time show the occurrence of a proton permeation pathway in E. huxleyi plasma membrane. pH(i) homeostasis involves a DIDS-sensitive mechanism.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2012-07-06
    Description: Microzooplankton grazing and algae growth responses to increasing pCO2 levels (350, 700 and 1050 μatm) were investigated in nitrate and phosphate fertilized mesocosms during the PeECE III experiment 2005. Grazing and growth rates were estimated by the dilution technique combined with taxon specific HPLC pigment analysis. Microzooplankton composition was determined by light microscopy. Despite a range of up to 3 times the present CO2 levels, there were no clear differences in any measured parameter between the different CO2 treatments. During days 3–9 of the experiment the algae community standing stock, measured as chlorophyll a (Chl-a), showed the highest instantaneous grow rates (k=0.37–0.99 d−1) and increased from ca. 2–3 to 6–12 μg l−1, in all mesocosms. Afterwards the phytoplankton standing stock decreased in all mesocosms until the end of the experiment. The microzooplankton standing stock, that was mainly constituted by dinoflagellates and ciliates, varied between 23 and 130 μg C l−1 (corresponding to 1.9 and 10.8 μmol C l−1), peaking on day 13–15, apparently responding to the phytoplankton development. Instantaneous Chl-a growth rates were generally higher than the grazing rates, indicating only a limited overall effect of microzooplankton grazing on the most dominant phytoplankton. Diatoms and prymnesiophytes were significantly grazed (12–43% of the standing stock d−1) only in the pre-bloom phase when they were in low numbers, and in the post-bloom phase when they were already affected by low nutrients and/or viral lysis. The cyanobacteria populations appeared more affected by microzooplankton grazing which generally removed 20–65% of the standing stock per day.
    Type: Article , PeerReviewed
    Format: text
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  • 7
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    In:  (Diploma thesis), Christian-Albrechts-Universität zu Kiel, Kiel, Germany, 44 pp
    Publication Date: 2021-11-19
    Description: The effects of rising pC02 on the growth of calcifying algae, grazing by microzooplankton and copepods, and differences in calcium dissolution induced by the digestion of calcifying algae were studied as part of the PeECE III experiment. The study was conducted from May 15th to June 9th 2005 at the Espegrend Marine Biological station in Bergen, Norway. The experimental setup of the study included 9 mesocosms, which were aerated with C02 enriched air to achieve target concentrations of 370, 750 and 1150 ppmV. Future C02 levels for the years 2100 and 2150 were chosen according to a 'business as usual' anthropogenic C02 emission scenario by Houghton (1995). Dilution experiments were conducted according to Landry & Hassett (1982) and data for pigment analysis, calcite analysis and microzooplankton enumeration were collected and analysed. No compelling evidence was found for a C02 effect on the data in either of the analyses. Pigment data showed the typical development over a bloom in all C02 treatments, with growth rates exceeding grazing rates during build up and peak of the bloom. The standing stock increased rapidly, too, and decreased rapidly afterwards, together with a strong decrease of specific growth and grazing rates during the decline of the bloom. In the post bloom phase we found a typical steady state recycling situation, with almost no change in the biomass. The microzooplankton developed on a similar scale of time, which shows the tight linkage between phyto- and zooplankton. In the calcium analysis we found the vast amount of the calcite to be in free coccoliths. The microzooplankton was clearly responsible for a major loss of calcite, which is shown by high Ca loss rates throughout the whole experiment.
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 8
    Publication Date: 2022-12-19
    Description: Most metabolic processes are pH dependent. If we want to understand the influence of ocean pH and carbonate chemistry on coccolithophores, it is necessary to gain a better understanding of their physiological properties and metabolic processes. Here Emiliania huxleyi and Coccolithus pelagicus were chosen to characterise some mechanisms involved in pH homeostasis and ion transport. Effects of changes in seawater carbon chemistry on intracellular pH (pHi) were measured by 2',7'-bis-(2-carboxyethyl)-5-(and-6)-carboxyfluorescein (BCECF)fluorescence. Out of equilibrium (OOE) solutions were used to differentiate between membrane permeation pathways for H+, CO2 and HCO3-. The ionophore nigericin was used to calibrate the dimension of changes in pHi measured by BCECF. pHi acutely followed the pH of seawater (pHe) in a linear fashion between pHe 6.5 and 9. No pHi change could be detected when seawater [CO2], [CO2]e, was increased at constant pHe and extracellular [HCO3-], [HCO3-]e. An increase in [HCO3-]e resulted in a slight intracellular acidification. In the presence of 4,4′-Diisothiocyanatostilbene-2,2′-disulfonic acid (DIDS) pHi in E. huxleyi acidified and the effect was not reversible. In addition, DIDS reduced the effect of pHe on pHi slightly. The data for the first time show the occurrence of a direct proton permeation pathway in E. huxleyi plasma membrane, a direct acidifying impact of increased [HCO3-]e on pHi and no detectable influence of increased [CO2]e on pHi. pH homeostasis involves a DIDS sensitive mechanism. The data suggest the involvement of ion transport mechanisms which link ocean seawater pH and metabolic processes in E. huxleyi. To further characterise these mechanisms the impact of manipulated extracellular ion concentrations on pHi was investigated. The data on increased external [K+], [K+]e , and decreased external [Cl-], [Cl-]e, i. e. the effect of decreased gradients on pHi , showed more complex relationships. Both led to a first rapid but transient acidification of pHi and a second slower, also transient acidification upon return to control conditions. The two pH reactions showed different kinetics. The results indicate coupling of H+ transport to ion gradients. Different methods to isolate pure protoplasts and perform electrophysiological measurements on E. huxleyi were applied. E. huxleyi protoplasts showed a clean cell membrane by different methods; however the cells did not form gigaseals. In C. pelagicus protoplast isolation and sealing were achieved, however, only in limited numbers of cells. A revision of E. huxleyi membrane anatomy by confocal microscopy in collaboration with M. Gutowska and N. Fischer gave first evidence for a dual protoplast outer membrane, which might explain the difficulties in dye loading and patch sealing. In summary the collected data are a first step in characterising physiological properties of coccolithophores with respect to carbon transport pathways, and pH homeostasis on a cellular level.
    Type: Thesis , NonPeerReviewed
    Format: text
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