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  • Diatom  (2)
  • 14C-leucine incorporation; Alkalinity, total; Aragonite saturation state; Bacteria, production as carbon; Bacterial cell multiplication; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cell density; Cell density, standard deviation; Chondroitin sulfate hydrolysis; Coast and continental shelf; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Experiment day; Field experiment; Fucoidan hydrolysis; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Laminarin hydrolysis; Measured; Mesocosm or benthocosm; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Other metabolic rates; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Proportion of total bacteria attached to particles; Salinity; Sample ID; see reference(s); Temperate; Temperature, water; Thymidine incorporation; Time, incubation; Xylan hydrolysis  (1)
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  • 1
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    Unbekannt
    PANGAEA
    In:  Supplement to: Arnosti, Carol; Grossart, Hans-Peter; Mühling, M; Joint, Ian; Passow, Uta (2011): Dynamics of extracellular enzyme activities in seawater under changed atmospheric pCO2: a mesocosm investigation. Aquatic Microbial Ecology, 64(3), 285-298, https://doi.org/10.3354/ame01522
    Publikationsdatum: 2024-03-15
    Beschreibung: As part of the PeECE II mesocosm project, we investigated the effects of pCO2 levels on the initial step of heterotrophic carbon cycling in the surface ocean. The activities of microbial extracellular enzymes hydrolyzing 4 polysaccharides were measured during the development of a natural phytoplankton bloom under pCO2 conditions representing glacial (190 µatm) and future (750 µatm) atmospheric pCO2. We observed that (1) chondroitin hydrolysis was variable throughout the pre-, early- and late-bloom phases, (2) fucoidanase activity was measurable only in the glacial mesocosm as the bloom developed, (3) laminarinase activity was low and constant, and (4) xylanase activity declined as the bloom progressed. Concurrent measurements of microbial community composition, using denaturing-gradient gel electrophoresis (DGGE), showed that the 2 mesocosms diverged temporally, and from one another, especially in the late-bloom phase. Enzyme activities correlated with bloom phase and pCO2, suggesting functional as well as compositional changes in microbial communities in the different pCO2 environments. These changes, however, may be a response to temporal changes in the development of phytoplankton communities that differed with the pCO2 environment. We hypothesize that the phytoplankton communities produced dissolved organic carbon (DOC) differing in composition, a hypothesis supported by changing amino acid composition of the DOC, and that enzyme activities responded to changes in substrates. Enzyme activities observed under different pCO2 conditions likely reflect both genetic and population-level responses to changes occurring among multiple components of the microbial loop.
    Schlagwort(e): 14C-leucine incorporation; Alkalinity, total; Aragonite saturation state; Bacteria, production as carbon; Bacterial cell multiplication; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cell density; Cell density, standard deviation; Chondroitin sulfate hydrolysis; Coast and continental shelf; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Experiment day; Field experiment; Fucoidan hydrolysis; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Laminarin hydrolysis; Measured; Mesocosm or benthocosm; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Other metabolic rates; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Proportion of total bacteria attached to particles; Salinity; Sample ID; see reference(s); Temperate; Temperature, water; Thymidine incorporation; Time, incubation; Xylan hydrolysis
    Materialart: Dataset
    Format: text/tab-separated-values, 664 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    Unbekannt
    Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
    Publikationsdatum: 2022-05-26
    Beschreibung: The presented data suggest that acclimatization times of exponentially growing diatoms to environmental perturbations may be weeks to months, rather than days to weeks. The response of acclimatized T. weissflogii to pCO2 depended on irradiance and temperature and was highly interactive, non-linear, and non-uniform. A very significant negative effect of pCO2 was observed under growth conditions that were light-, and temperature-limited; a smaller, but still significant negative response was seen under light-limiting growth conditions, whereas pCO2 did not affect growth rates of T. weissflogii under light-saturated growth conditions. Cell quotas of organic carbon, nitrogen, or chlorophyll a were linked to growth rate. The cell-normalized production of transparent exopolymer particles (TEP) was positively correlated with POC cell quotas, with some minor impact of irradiance and pCO2 on the relationship. This correlation of TEP production with carbon cell quotas is consistent with the hypothesis that extracellular release is an inherent component of cell metabolism. Results suggest that elevated pCO2 functions as an (additional) metabolic stressor for T. weissflogii and that the interaction of different stressors determines growth rates and cell characteristics in a complex, non-linear relationship.
    Beschreibung: The increase in partial pressure of CO2 (pCO2) is causing ocean acidification, which impacts the growth rates and elemental composition of phytoplankton. Here, shifts in growth rates and cell quotas of Thalassiosira weissflogii grown under a variety of different temperatures, irradiances, and pCO2 conditions are discussed.
    Beschreibung: This research was supported by NSF Grant: OCE-0926711
    Schlagwort(e): Ocean Acidification ; Temperature ; Transparent exopolymer particles (TEP) ; Climate change ; Diatom ; Thalassiosira weissflogii ; Partial Pressure CO2 (pCO2) ; Growth Rates ; Cell Quotas ; Marinobacter adhaerens HP15
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Format: text/csv
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
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    Unbekannt
    Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
    Publikationsdatum: 2022-05-26
    Beschreibung: The Series 4 Experiment, Aggregation of Thalassiosira weissflogii as a function of pCO2, temperature and bacteria, is made up of 2 phases. The Acclimatisation Phase and the Aggregation Phase. The Acclimatisation Phase has two components – The Carbonate System data and the Cell Counts Data. The Aggregation Phase also has two components – The Carbonate System + TEP data and the Sinking Velocity data. Note: For a complete list of measurements, refer to the supplemental document ' Series4_Field_names.pdf' .
    Beschreibung: Increasing Transparent Exopolymer Particle (TEP) formation during diatom blooms as a result of elevated temperature and pCO2 have been suggested to result in enhanced aggregation and carbon flux, therewith potentially increasing the sequestration of carbon by the ocean. We present experimental results on TEP and aggregate formation by Thalassiosira weissflogii (diatom) in the presence or absence of bacteria under two temperature and three pCO2 scenarios. During the aggregation phase of the experiment TEP formation was elevated at the higher temperature (20ºC vs. 15ºC), as predicted. However, in contrast to expectations based on the established relationship between TEP and aggregation, aggregation rates and sinking velocity of aggregates were depressed in warmer treatments, especially under ocean acidification conditions. If our experimental findings can be extrapolated to natural conditions, they would imply a reduction in carbon flux and potentially reduced carbon sequestration after diatoms blooms in the future ocean.
    Beschreibung: This research was supported by NSF Grant: OCE-0926711
    Beschreibung: 2014-10-08
    Schlagwort(e): Ocean acidification ; Temperature ; Transparent exopolymer particles (TEP) ; Marine aggregates ; Climate change ; Diatom ; Thalassiosira weissflogii ; Marinobacter adhaerens HP15
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Format: application/pdf
    Format: text/csv
    Standort Signatur Einschränkungen Verfügbarkeit
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