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  1. Article ; Online: Stimulated bacterial growth under elevated p CO₂: results from an off-shore mesocosm study.

    Endres, Sonja / Galgani, Luisa / Riebesell, Ulf / Schulz, Kai-Georg / Engel, Anja

    PloS one

    2014  Volume 9, Issue 6, Page(s) e99228

    Abstract: Marine bacteria are the main consumers of freshly produced organic matter. Many enzymatic processes involved in the bacterial digestion of organic compounds were shown to be pH sensitive in previous studies. Due to the continuous rise in atmospheric CO2 ... ...

    Abstract Marine bacteria are the main consumers of freshly produced organic matter. Many enzymatic processes involved in the bacterial digestion of organic compounds were shown to be pH sensitive in previous studies. Due to the continuous rise in atmospheric CO2 concentration, seawater pH is presently decreasing at a rate unprecedented during the last 300 million years but the consequences for microbial physiology, organic matter cycling and marine biogeochemistry are still unresolved. We studied the effects of elevated seawater pCO2 on a natural plankton community during a large-scale mesocosm study in a Norwegian fjord. Nine Kiel Off-Shore Mesocosms for Future Ocean Simulations (KOSMOS) were adjusted to different pCO2 levels ranging initially from ca. 280 to 3000 µatm and sampled every second day for 34 days. The first phytoplankton bloom developed around day 5. On day 14, inorganic nutrients were added to the enclosed, nutrient-poor waters to stimulate a second phytoplankton bloom, which occurred around day 20. Our results indicate that marine bacteria benefit directly and indirectly from decreasing seawater pH. During the first phytoplankton bloom, 5-10% more transparent exopolymer particles were formed in the high pCO2 mesocosms. Simultaneously, the efficiency of the protein-degrading enzyme leucine aminopeptidase increased with decreasing pH resulting in up to three times higher values in the highest pCO2/lowest pH mesocosm compared to the controls. In general, total and cell-specific aminopeptidase activities were elevated under low pH conditions. The combination of enhanced enzymatic hydrolysis of organic matter and increased availability of gel particles as substrate supported up to 28% higher bacterial abundance in the high pCO2 treatments. We conclude that ocean acidification has the potential to stimulate the bacterial community and facilitate the microbial recycling of freshly produced organic matter, thus strengthening the role of the microbial loop in the surface ocean.
    MeSH term(s) Bacterial Proteins/metabolism ; Carbon Dioxide/chemistry ; Carbon Dioxide/physiology ; Cyanobacteria/growth & development ; Cyanobacteria/metabolism ; Hydrogen-Ion Concentration ; Leucyl Aminopeptidase/metabolism ; Norway ; Phytoplankton/growth & development ; Phytoplankton/metabolism ; Seawater/chemistry ; Seawater/microbiology ; Water Microbiology
    Chemical Substances Bacterial Proteins ; Carbon Dioxide (142M471B3J) ; Leucyl Aminopeptidase (EC 3.4.11.1)
    Language English
    Publishing date 2014-06-18
    Publishing country United States
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ISSN 1932-6203
    ISSN (online) 1932-6203
    DOI 10.1371/journal.pone.0099228
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  2. Article ; Online: Effects of increasing seawater carbon dioxide concentrations on chain formation of the diatom Asterionellopsis glacialis.

    Barcelos e Ramos, Joana / Schulz, Kai Georg / Brownlee, Colin / Sett, Scarlett / Azevedo, Eduardo Brito

    PloS one

    2014  Volume 9, Issue 3, Page(s) e90749

    Abstract: Diatoms can occur as single cells or as chain-forming aggregates. These two strategies affect buoyancy, predator evasion, light absorption and nutrient uptake. Adjacent cells in chains establish connections through various processes that determine ... ...

    Abstract Diatoms can occur as single cells or as chain-forming aggregates. These two strategies affect buoyancy, predator evasion, light absorption and nutrient uptake. Adjacent cells in chains establish connections through various processes that determine strength and flexibility of the bonds, and at distinct cellular locations defining colony structure. Chain length has been found to vary with temperature and nutrient availability as well as being positively correlated with growth rate. However, the potential effect of enhanced carbon dioxide (CO2) concentrations and consequent changes in seawater carbonate chemistry on chain formation is virtually unknown. Here we report on experiments with semi-continuous cultures of the freshly isolated diatom Asterionellopsis glacialis grown under increasing CO2 levels ranging from 320 to 3400 µatm. We show that the number of cells comprising a chain, and therefore chain length, increases with rising CO2 concentrations. We also demonstrate that while cell division rate changes with CO2 concentrations, carbon, nitrogen and phosphorus cellular quotas vary proportionally, evident by unchanged organic matter ratios. Finally, beyond the optimum CO2 concentration for growth, carbon allocation changes from cellular storage to increased exudation of dissolved organic carbon. The observed structural adjustment in colony size could enable growth at high CO2 levels, since longer, spiral-shaped chains are likely to create microclimates with higher pH during the light period. Moreover increased chain length of Asterionellopsis glacialis may influence buoyancy and, consequently, affect competitive fitness as well as sinking rates. This would potentially impact the delicate balance between the microbial loop and export of organic matter, with consequences for atmospheric carbon dioxide.
    MeSH term(s) Carbon Dioxide/chemistry ; Carbon Dioxide/pharmacology ; Carbonates/chemistry ; Carbonates/metabolism ; Cell Division ; Diatoms/drug effects ; Diatoms/growth & development ; Diatoms/metabolism ; Seawater/chemistry
    Chemical Substances Carbonates ; Carbon Dioxide (142M471B3J)
    Language English
    Publishing date 2014-03-11
    Publishing country United States
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ZDB-ID 2267670-3
    ISSN 1932-6203 ; 1932-6203
    ISSN (online) 1932-6203
    ISSN 1932-6203
    DOI 10.1371/journal.pone.0090749
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  3. Article: An approach for particle sinking velocity measurements in the 3–400 μm size range and considerations on the effect of temperature on sinking rates

    Bach, Lennart Thomas / Riebesell, Ulf / Sett, Scarlett / Febiri, Sarah / Rzepka, Paul / Schulz, Kai Georg

    Marine biology. 2012 Aug., v. 159, no. 8

    2012  

    Abstract: The flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes—remineralization rates and sinking velocities. Here, we present an ... ...

    Abstract The flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes—remineralization rates and sinking velocities. Here, we present an efficient method to measure sinking velocities of particles in the size range from approximately 3–400 μm by means of video microscopy (FlowCAM®). The method allows rapid measurement and automated analysis of mixed samples and was tested with polystyrene beads, different phytoplankton species, and sediment trap material. Sinking velocities of polystyrene beads were close to theoretical values calculated from Stokes’ Law. Sinking velocities of the investigated phytoplankton species were in reasonable agreement with published literature values and sinking velocities of material collected in sediment trap increased with particle size. Temperature had a strong effect on sinking velocities due to its influence on seawater viscosity and density. An increase in 9 °C led to a measured increase in sinking velocities of ~40 %. According to this temperature effect, an average temperature increase in 2 °C as projected for the sea surface by the end of this century could increase sinking velocities by about 6 % which might have feedbacks on carbon export into the deep ocean.
    Keywords carbon ; microscopy ; oceans ; particle size ; phytoplankton ; polystyrenes ; rapid methods ; seawater ; sediments ; temperature ; traps ; viscosity
    Language English
    Dates of publication 2012-08
    Size p. 1853-1864.
    Publishing place Springer-Verlag
    Document type Article
    ZDB-ID 1117-4
    ISSN 1432-1793 ; 0025-3162
    ISSN (online) 1432-1793
    ISSN 0025-3162
    DOI 10.1007/s00227-012-1945-2
    Database NAL-Catalogue (AGRICOLA)

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  4. Article: An approach for particle sinking velocity measurements in the 3-400 μm size range and considerations on the effect of temperature on sinking rates.

    Bach, Lennart Thomas / Riebesell, Ulf / Sett, Scarlett / Febiri, Sarah / Rzepka, Paul / Schulz, Kai Georg

    Marine biology

    2012  Volume 159, Issue 8, Page(s) 1853–1864

    Abstract: The flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes-remineralization rates and sinking velocities. Here, we present an ... ...

    Abstract The flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes-remineralization rates and sinking velocities. Here, we present an efficient method to measure sinking velocities of particles in the size range from approximately 3-400 μm by means of video microscopy (FlowCAM
    Language English
    Publishing date 2012-05-22
    Publishing country Germany
    Document type Review
    ZDB-ID 1117-4
    ISSN 1432-1793 ; 0025-3162
    ISSN (online) 1432-1793
    ISSN 0025-3162
    DOI 10.1007/s00227-012-1945-2
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  5. Book ; Online: No observed effect of ocean acidification on nitrogen biogeochemistry in a summer Baltic Sea plankton community

    Paul, Allanah J. / Achterberg, Eric P. / Bach, Lennart T. / Boxhammer, Tim / Czerny, Jan / Haunost, Mathias / Schulz, Kai-Georg / Stuhr, Annegret / Riebesell, Ulf

    eISSN: 1726-4189

    2016  

    Abstract: Nitrogen fixation by filamentous cyanobacteria supplies significant amounts of new nitrogen (N) to the Baltic Sea. This balances N loss processes such as denitrification and anammox, and forms an important N source supporting primary and secondary ... ...

    Abstract Nitrogen fixation by filamentous cyanobacteria supplies significant amounts of new nitrogen (N) to the Baltic Sea. This balances N loss processes such as denitrification and anammox, and forms an important N source supporting primary and secondary production in N-limited post-spring bloom plankton communities. Laboratory studies suggest that filamentous diazotrophic cyanobacteria growth and N 2 -fixation rates are sensitive to ocean acidification, with potential implications for new N supply to the Baltic Sea. In this study, our aim was to assess the effect of ocean acidification on diazotroph growth and activity as well as the contribution of diazotrophically fixed N to N supply in a natural plankton assemblage. We enclosed a natural plankton community in a summer season in the Baltic Sea near the entrance to the Gulf of Finland in six large-scale mesocosms (volume ∼ 55 m 3 ) and manipulated f CO 2 over a range relevant for projected ocean acidification by the end of this century (average treatment f CO 2 : 365–1231 µatm). The direct response of diazotroph growth and activity was followed in the mesocosms over a 47 day study period during N-limited growth in the summer plankton community. Diazotrophic filamentous cyanobacteria abundance throughout the study period and N 2 -fixation rates (determined only until day 21 due to subsequent use of contaminated commercial 15 N-N 2 gas stocks) remained low. Thus estimated new N inputs from diazotrophy were too low to relieve N limitation and stimulate a summer phytoplankton bloom. Instead, regeneration of organic N sources likely sustained growth in the plankton community. We could not detect significant CO 2 -related differences in neither inorganic nor organic N pool sizes, or particulate matter N : P stoichiometry. Additionally, no significant effect of elevated CO 2 on diazotroph activity was observed. Therefore, ocean acidification had no observable impact on N cycling or biogeochemistry in this N-limited, post-spring bloom plankton assemblage in the Baltic Sea.
    Subject code 551
    Language English
    Publishing date 2016-07-07
    Publishing country de
    Document type Book ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  6. Article ; Online: Factors controlling plankton community production, export flux, and particulate matter stoichiometry in the coastal upwelling system off Peru

    Bach, Lennart T. / Paul, Allanah J. / Boxhammer, Tim / von der Esch, Elisabeth / Graco, Michelle / Schulz, Kai Georg / Achterberg, Eric P. / Aguayo, Paulina / Arístegui, Javier / Ayón, Patrizia / Baños, Isabel / Bernales, Avy / Boegeholz, Anne Sophie / Chavez, Francisco / Chavez, Gabriela / Chen, Shao-Min / Doering, Kristin / Filella, Alba / Fischer, Martin /
    Grasse, Patricia / Haunost, Mathias / Hennke, Jan / Hernández-Hernández, Nauzet / Hopwood, Mark J. / Igarza, Maricarmen / Kalter, Verena / Kittu, Leila / Kohnert, Peter / Ledesma, Jesus / Lieberum, Christian / Lischka, Silke / Löscher, Carolin / Ludwig, Andrea / Mendoza, Ursula / Meyer, Jana / Meyer, Judith / Minutolo, Fabrizio / Ortiz Cortes, Joaquin / Piiparinen, Jonna / Sforna, Claudia / Spilling, Kristian / Sanchez, Sonia / Spisla, Carsten / Sswat, Michael / Zavala Moreira, Mabel / Riebesell, Ulf

    2020  

    Abstract: Eastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The production of organic material is fueled by upwelling of nutrient-rich deep waters and high incident light at the sea surface. However, biotic and ... ...

    Abstract Eastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The production of organic material is fueled by upwelling of nutrient-rich deep waters and high incident light at the sea surface. However, biotic and abiotic factors can modify surface production and related biogeochemical processes. Determining these factors is important because EBUS are considered hotspots of climate change, and reliable predictions of their future functioning requires understanding of the mechanisms driving the biogeochemical cycles therein. In this field experiment, we used in situ mesocosms as tools to improve our mechanistic understanding of processes controlling organic matter cycling in the coastal Peruvian upwelling system. Eight mesocosms, each with a volume of ∼55 m3, were deployed for 50 d ∼6 km off Callao (12∘ S) during austral summer 2017, coinciding with a coastal El Niño phase. After mesocosm deployment, we collected subsurface waters at two different locations in the regional oxygen minimum zone (OMZ) and injected these into four mesocosms (mixing ratio ≈1.5 : 1 mesocosm: OMZ water). The focus of this paper is on temporal developments of organic matter production, export, and stoichiometry in the individual mesocosms. The mesocosm phytoplankton communities were initially dominated by diatoms but shifted towards a pronounced dominance of the mixotrophic dinoflagellate (Akashiwo sanguinea) when inorganic nitrogen was exhausted in surface layers. The community shift coincided with a short-term increase in production during the A. sanguinea bloom, which left a pronounced imprint on organic matter C : N : P stoichiometry. However, C, N, and P export fluxes did not increase because A. sanguinea persisted in the water column and did not sink out during the experiment. Accordingly, export fluxes during the study were decoupled from surface production and sustained by the remaining plankton community. Overall, biogeochemical pools and fluxes were surprisingly constant for most of the ...
    Subject code 550
    Language English
    Publishing date 2020-10-12
    Publisher Copernicus Publications (EGU)
    Publishing country de
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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