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  • 1
    Schlagwort(e): Forschungsbericht ; Meerwasser ; Kohlendioxid ; Versauerung ; Biogeochemie
    Materialart: Buch
    Seiten: 23 S. , Ill., graph. Darst.
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMBF 03F0608 A-O. - Verbund-Nr. 01073496
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Schlagwort(e): Forschungsbericht ; Meerwasser ; Kohlendioxid ; Versauerung ; Biogeochemie
    Materialart: Buch
    Seiten: 23 Seiten , Illustrationen, Diagramme
    Sprache: Englisch
    Anmerkung: Förderkennzeichen BMBF 03F0608 A-O. - Verbund-Nr. 01073496
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Schlagwort(e): Hochschulschrift ; Coccolithophoridae ; Verkalkung ; Photosynthese
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (112 Seiten = 9 MB) , Illustrationen, Graphen
    Ausgabe: Online-Ausgabe 2021
    Sprache: Englisch
    Anmerkung: Zusammenfassung in deutscher und englischer Sprache
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Schlagwort(e): Hochschulschrift
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (66 Seiten = 3,6 MB) , Illustrationen, Graphen
    Ausgabe: 2022
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Schlagwort(e): Hochschulschrift
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (57 Seiten = 2 MB) , Illustrationen, Graphen, Karte
    Ausgabe: Online-Ausgabe 2023
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Schlagwort(e): Hochschulschrift
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (34 Seiten = 1 MB) , Illustrationen, Graphen
    Ausgabe: Online-Ausgabe 2023
    Sprache: Englisch
    Anmerkung: Zusammenfassung in deutscher und englischer Sprache
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-02-07
    Beschreibung: As one of Earth's most productive marine ecosystems, the Peruvian upwelling system transports large amounts of biogenic matter from the surface to the deep ocean. Whilst particle sinking velocity is a key factor controlling the biological pump, thereby affecting carbon sequestration and O2-depletion, it has not yet been measured in this system. During a 50 d mesocosm experiment in the surface waters off the coast of Peru, we assessed particle sinking velocities and their biogeochemical and physical drivers. We further characterized the general properties of exported particles under different phytoplankton communities and nutritional states. Average sinking velocities varied between size classes and ranged from 12.8 ± 0.7 m d−1 (particles 40–100 µm) to 19.4 ± 0.7 m d−1 (particles 100–250 µm) and 34.2 ± 1.5 m d−1 (particles 250–1000 µm) (± 95 % CI). Despite a distinct plankton succession from diatoms to dinoflagellates with concomitant 5-fold drop in opal ballasting, substantial changes in sinking velocity were not observed. This illustrates the complexity of counteracting factors driving the settling behaviour of marine particles. In contrast, we found higher sinking velocities with increasing particle size and roundness and decreasing porosity. Size had by far the strongest influence among these physical particle properties, despite a high amount of unexplained variability. Our study provides a detailed analysis of the drivers of particle sinking velocity in the Peruvian upwelling system, which allows modellers to optimize local particle flux parameterization. This will help to better project oxygen concentrations and carbon sequestration in a region that is subject to substantial climate-driven changes.
    Materialart: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2024-02-02
    Beschreibung: Gelatinous zooplankton are increasingly recognized to play a key role in the ocean's biological carbon pump. Appendicularians, a class of pelagic tunicates, are among the most abundant gelatinous plankton in the ocean, but it is an open question how their contribution to carbon export might change in the future. Here, we conducted an experiment with large volume in situ mesocosms (~55–60 m3 and 21 m depth) to investigate how ocean acidification (OA) extreme events affect food web structure and carbon export in a natural plankton community, particularly focusing on the keystone species Oikopleura dioica, a globally abundant appendicularian. We found a profound influence of O. dioica on vertical carbon fluxes, particularly during a short but intense bloom period in the high CO2 treatment, during which carbon export was 42%–64% higher than under ambient conditions. This elevated flux was mostly driven by an almost twofold increase in O. dioica biomass under high CO2. This rapid population increase was linked to enhanced fecundity (+20%) that likely resulted from physiological benefits of low pH conditions. The resulting competitive advantage of O. dioica resulted in enhanced grazing on phytoplankton and transfer of this consumed biomass into sinking particles. Using a simple carbon flux model for O. dioica, we estimate that high CO2 doubled the carbon flux of discarded mucous houses and fecal pellets, accounting for up to 39% of total carbon export from the ecosystem during the bloom. Considering the wide geographic distribution of O. dioica, our findings suggest that appendicularians may become an increasingly important vector of carbon export with ongoing OA.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Bach, Lennart Thomas; Hernández-Hernández, Nauzet; Taucher, Jan; Spisla, Carsten; Sforna, Claudia; Riebesell, Ulf; Arístegui, Javier (2019): Effects of Elevated CO2 on a Natural Diatom Community in the Subtropical NE Atlantic. Frontiers in Marine Science, 6, https://doi.org/10.3389/fmars.2019.00075
    Publikationsdatum: 2024-03-06
    Beschreibung: Diatoms are silicifying phytoplankton contributing about one quarter to primary 79 production on Earth. Ocean acidification (OA) could alter the competitiveness of diatoms 80 relative to other taxa and/or lead to shifts among diatom species. In spring 2016, we set 81 up a plankton community experiment at the coast of Gran Canaria (Canary Islands, 82 Spain) to investigate the response of subtropical diatom assemblages to elevated 83 84 seawater pCO2.
    Schlagwort(e): BIOACID; Biological Impacts of Ocean Acidification
    Materialart: Dataset
    Format: application/zip, 5 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Bach, Lennart Thomas; Bauke, Christine; Meier, K J Sebastian; Riebesell, Ulf; Schulz, Kai Georg (2012): Influence of changing carbonate chemistry on morphology and weight of coccoliths formed by Emiliania huxleyi. Biogeosciences, 9(8), 3449-3463, https://doi.org/10.5194/bg-9-3449-2012
    Publikationsdatum: 2024-03-06
    Beschreibung: The coccolithophore Emiliania huxleyi is a marine phytoplankton species capable of forming small calcium carbonate scales (coccoliths) which cover the organic part of the cell. Calcification rates of E. huxleyi are known to be sensitive to changes in seawater carbonate chemistry. It has, however, not yet been clearly determined how these changes are reflected in size and weight of individual coccoliths and which specific parameter(s) of the carbonate system drive morphological modifications. Here, we compare data on coccolith size, weight, and malformation from a set of five experiments with a large diversity of carbonate chemistry conditions. This diversity allows distinguishing the influence of individual carbonate chemistry parameters such as carbon dioxide (CO2), bicarbonate (HCO3- ), carbonate ion (CO32-), and protons (H+) on the measured parameters. Measurements of fine-scale morphological structures reveal an increase of coccolith malformation with decreasing pH suggesting that H+ is the major factor causing malformations. Coccolith distal shield area varies from about 5 to 11 µm2. Changes in size seem to be mainly induced by varying [HCO3- ] and [H+] although influence of [CO32-] cannot be entirely ruled out. Changes in coccolith weight were proportional to changes in size. Increasing CaCO3 production rates are reflected in an increase in coccolith weight and an increase of the number of coccoliths formed per unit time. The combined investigation of morphological features and coccolith production rates presented in this study may help to interpret data derived from sediment cores, where coccolith morphology is used to reconstruct calcification rates in the water column.
    Schlagwort(e): -; Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Calcite saturation state; Carbon, inorganic, dissolved; Carbonate ion; Carbon dioxide; Carbon dioxide, partial pressure; Cell size; Coccoliths, malformed and incomplete; Coccoliths, malformed and incomplete, standard deviation; Height/width ratio; Height/width ratio, standard deviation; Length; Length, standard deviation; Mass; Mass, standard deviation; Measured; Particulate inorganic carbon production per cell; pH; Production; Surface area; Surface area, standard deviation; Treatment; Width; Width, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 1977 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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