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  • 1
    Keywords: Forschungsbericht ; Ostsee ; Küstenmeer ; Eutrophierung ; Benthos
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (143 Seiten, 3,31 MB) , Diagramme
    Language: German
    Note: Förderkennzeichen BMBF 03F0683A. - Verbund-Nummer 01149366 , Autoren dem Berichtsblatt entnommen. - Paralleltitel dem englischen Berichtsblatt entnommen , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Zusammenfassung: Deutsch, Englisch
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  • 2
    Publication Date: 2023-06-20
    Description: Coastal waters have strong gradients in dissolved organic matter (DOM) quantity and characteristics, originating from terrestrial inputs and autochthonous production. Enclosed seas with high freshwater input therefore experience high DOM concentrations and gradients from freshwater sources to more saline waters. The brackish Baltic Sea experiences such salinity gradients from east to west and from river mouths to the open sea. Furthermore, the catchment areas of the Baltic Sea are very diverse and vary from sparsely populated northern areas to densely populated southern zones. Coastal systems vary from enclosed or open bays, estuaries, fjords, archipelagos and lagoons where the residence time of DOM at these sites varies and may control the extent to which organic matter is biologically, chemically or physically modified or simply diluted with transport off-shore. Data of DOM with simultaneous measurements of dissolved organic (DO) nitrogen (N), carbon (C) and phosphorus (P) across a range of contrasting coastal systems are scarce. Here we present data from the Roskilde Fjord, Vistula and Öre estuaries and Curonian Lagoon; four coastal systems with large differences in salinity, nutrient concentrations, freshwater inflow and catchment characteristics. The C:N:P ratios of DOM of our data, despite high variability, show site specific significant differences resulting largely from differences residence time. Microbial processes seemed to have minor effects, and only in spring did uptake of DON in the Vistula and Öre estuaries take place and not at the other sites or seasons. Resuspension from sediments impacts bottom waters and the entire shallow water column in the Curonian Lagoon. Finally, our data combined with published data show that land use in the catchments seems to impact the DOC:DON and DOC:DOP ratios of the tributaries most.
    Description: Academy of Sciences of Finland
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: BONUS COCOA and Bundesministerium für Bildung und Forschung
    Description: Academy of Finland
    Description: Danish Research Council for Independent Research
    Description: BONUS COCOA Project
    Description: Leibniz-Institut für Ostseeforschung Warnemünde (IOW) (3484)
    Keywords: ddc:551.9 ; Coastal systems ; Dissolved organic matter ; Riverine input ; Baltic Sea
    Language: English
    Type: doc-type:article
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  • 3
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    PANGAEA
    In:  Supplement to: Asmala, Eero; Haraguchi, Lumi; Markager, Stiig; Massicotte, Philippe; Riemann, Bo; Staehr, Peter A; Carstensen, Jacob (2018): Eutrophication leads to accumulation of recalcitrant autochthonous organic matter in coastal environment. Global Biogeochemical Cycles, 32(11), 1673-1687, https://doi.org/10.1029/2017GB005848
    Publication Date: 2023-03-14
    Description: Anthropogenic nutrient enrichment is changing the structure and the function of coastal ecosystems. These coastal zones are transitions between freshwater and marine systems where multiple biogeochemical processes remove, produce and transform organic matter. The extent to which the coastal zone is merely a conduit for terrestrial (allochthonous) organic matter, versus a distinct source of autochthonous organic matter fueled by eutrophication, is unclear. To address this issue, we characterized the freshwater and marine dissolved organic matter (DOM) pools in an eutrophic estuary with a long water residence time (Roskilde Fjord, Denmark) over an annual cycle. We combined elemental, optical (absorbance and fluorescence) and isotopic analyses to obtain insight about the bulk properties of the DOM pool during this period. We also used sediment traps to analyze the changes related to the exchange of organic matter between the particulate (POM) and dissolved (DOM) fractions. The results showed that labile autochthonous DOM from in situ primary production was rapidly transformed to more recalcitrant DOM that accumulated in the estuary despite continuous exchange with the open sea. Also, parts of the POM pool were degraded rapidly (within 24h) and transformed into the DOM pool. Accumulated DOM was characterized by relatively low molecular size and stable carbon isotopic value, and by high protein-like fluorescence. These results indicate that autotrophic material can be a major source of specific recalcitrant DOM in eutrophic coastal waters, contributing significantly to the flux of organic carbon to the ocean.
    Keywords: Absorption coefficient, 230 nm; Absorption coefficient, 254 nm; Absorption coefficient, 275 nm; Absorption coefficient, 295 nm; Absorption coefficient, 300 nm; Absorption coefficient, 350 nm; Absorption coefficient, 355 nm; Absorption coefficient, 375 nm; Absorption coefficient, 400 nm; Absorption coefficient, 440 nm; Ammonium; Biological index; Carbon, organic, dissolved; Carbon, organic, total; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Event label; Fluorescence, peak A; Fluorescence, peak C; Fluorescence, peak M; Fluorescence, peak T; Fluorescence index; Humification index; LATITUDE; LONGITUDE; Molecular mass; MULT; Multiple investigations; Nitrate; Nitrate and Nitrite; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen, organic, dissolved; Nitrogen, total; Nitrogen, total dissolved; PDZ Europa ANCA-GSL elemental analyser; pH; Phosphate; Phosphorus, inorganic, dissolved; Phosphorus, organic, dissolved; Phosphorus, total; Phosphorus, total dissolved; Ratio; Roskilde_fjord_RF01; Roskilde_fjord_RF02; Roskilde_fjord_RF03; Roskilde_fjord_RF04; Roskilde_fjord_RF05; Roskilde_fjord_RF06; Roskilde_fjord_RF07; Roskilde_fjord_RF08; Salinity; Sample ID; SEC analyser; Silicate; Specific ultraviolet absorbance normalized to DOC, 254 nm; Spectral slope, 275-295 nm; Spectral slope, 300-650 nm; Spectral slope, 350-400 nm; Spectrophotometer UV/VIS (Shimadzu 2401PC); Temperature, water; Varian Cary Eclipse fluorometer (Agilent); Wet oxidation total organic carbon analyzer Shimadzu; δ13C, dissolved organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 7907 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Asmala, Eero; Kaartokallio, Hermanni; Carstensen, Jacob; Thomas, David N (2016): Variation in riverine inputs affect dissolved organic matter characteristics throughout the estuarine gradient. Frontiers in Marine Science, 2, 125, https://doi.org/10.3389/fmars.2015.00125
    Publication Date: 2023-02-15
    Description: Terrestrial dissolved organic matter (DOM) undergoes significant changes during the estuarine transport from river mouths to the open sea. These include transformations and degradation by biological and chemical processes, but also the production of fresh organic matter. Since many of these processes occur simultaneously, properties of the DOM pool represent the net changes during the passage along the hydrological path. We examined changes in multiple DOM characteristics across three Finnish estuarine gradients during spring, summer and autumn: Dissolved organic carbon (DOC) concentration, coloured DOM absorbance and fluorescence, stable carbon isotope signal of DOC and molecular size distribution. Changes in these DOM characteristics with salinity were analysed in relation to residence time (i.e. freshwater transit time), since increased residence time is likely to enhance DOM degradation while stimulating autochthonous DOM production at the same time. Our results show that the investigated DOM characteristics are highly correlated, indicating common physico-chemical transformations along the salinity continuum. Residence time did not explain variations in the DOM characteristics any better than salinity. Due to large variations in DOM characteristics at the river end-member, conservative mixing models do not seem to be able to accurately describe the occurrence and extent of deviations in DOM properties in the estuaries we investigated.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2023-02-15
    Keywords: Absorption coefficient, 230 nm; Absorption coefficient, 254 nm; Absorption coefficient, 275 nm; Absorption coefficient, 295 nm; Absorption coefficient, 300 nm; Absorption coefficient, 350 nm; Absorption coefficient, 355 nm; Absorption coefficient, 375 nm; Absorption coefficient, 400 nm; Absorption coefficient, 440 nm; Aluminium, dissolved; Ammonium; Automated analysis following alkaline persulfate oxidation; Bacteria; Carbon, organic, dissolved; DATE/TIME; Depth, description; Depth of Secchi Disk; Event label; Fluorescence, peak A; Fluorescence, peak C; Fluorescence, peak M; Fluorescence, peak T; Fluorescence index; High nucleic acid bacteria; ICP-OES; Iron, dissolved; Kyronjoki_00; Kyronjoki_01; Kyronjoki_02; Kyronjoki_03; Kyronjoki_04; Kyronjoki_XX; Lachat QuickChem 8000 flow injection autoanalyzer; LATITUDE; Leucine incorporation rate; LONGITUDE; Low nucleic acid bacteria; Manganese, dissolved; Manually after Grasshoff et al. (1983); Molecular mass; MULT; Multiple investigations; Nitrate; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen, organic, dissolved; Nitrogen, total; Nitrogen, total dissolved; PDZ Europa ANCA-GSL elemental analyser; Ratio; Salinity; Sample ID; SEC analyser; Silicate; Specific ultraviolet absorbance normalized to DOC; Spectral slope, 275-295 nm; Spectral slope, 300-650 nm; Spectral slope, 350-400 nm; Spectrophotometer UV/VIS (PerkinElmer Lambda 650); Subtracting combined inorganic nitrogen from total dissolved nitrogen; Temperature, water; Thymidine incorporation rate; TOC analyser, MQ1000; Varian Cary Eclipse fluorometer (Agilent); δ13C, dissolved inorganic carbon; δ15N, total dissolved nitrogen
    Type: Dataset
    Format: text/tab-separated-values, 2185 data points
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  • 6
    Publication Date: 2023-12-12
    Keywords: Absorption coefficient, 230 nm; Absorption coefficient, 254 nm; Absorption coefficient, 275 nm; Absorption coefficient, 295 nm; Absorption coefficient, 300 nm; Absorption coefficient, 350 nm; Absorption coefficient, 355 nm; Absorption coefficient, 375 nm; Absorption coefficient, 400 nm; Absorption coefficient, 440 nm; Aluminium, dissolved; Ammonium; Automated analysis following alkaline persulfate oxidation; Bacteria; Carbon, organic, dissolved; DATE/TIME; Depth, description; Depth of Secchi Disk; Event label; Fluorescence, peak A; Fluorescence, peak C; Fluorescence, peak M; Fluorescence, peak T; Fluorescence index; High nucleic acid bacteria; ICP-OES; Iron, dissolved; Kiiminkijoki_00; Kiiminkijoki_01; Kiiminkijoki_02; Kiiminkijoki_03; Kiiminkijoki_04; Kiiminkijoki_05; Lachat QuickChem 8000 flow injection autoanalyzer; LATITUDE; Leucine incorporation rate; LONGITUDE; Low nucleic acid bacteria; Manganese, dissolved; Manually after Grasshoff et al. (1983); Molecular mass; MULT; Multiple investigations; Nitrate; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen, organic, dissolved; Nitrogen, total; Nitrogen, total dissolved; PDZ Europa ANCA-GSL elemental analyser; Ratio; Salinity; Sample ID; SEC analyser; Silicate; Specific ultraviolet absorbance normalized to DOC; Spectral slope, 275-295 nm; Spectral slope, 300-650 nm; Spectral slope, 350-400 nm; Spectrophotometer UV/VIS (PerkinElmer Lambda 650); Subtracting combined inorganic nitrogen from total dissolved nitrogen; Temperature, water; Thymidine incorporation rate; TOC analyser, MQ1000; Varian Cary Eclipse fluorometer (Agilent); δ13C, dissolved inorganic carbon; δ15N, total dissolved nitrogen
    Type: Dataset
    Format: text/tab-separated-values, 2536 data points
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  • 7
    Publication Date: 2023-12-12
    Keywords: Absorption coefficient, 230 nm; Absorption coefficient, 254 nm; Absorption coefficient, 275 nm; Absorption coefficient, 295 nm; Absorption coefficient, 300 nm; Absorption coefficient, 350 nm; Absorption coefficient, 355 nm; Absorption coefficient, 375 nm; Absorption coefficient, 400 nm; Absorption coefficient, 440 nm; Aluminium, dissolved; Ammonium; Automated analysis following alkaline persulfate oxidation; Bacteria; Carbon, organic, dissolved; DATE/TIME; Depth, description; Depth of Secchi Disk; Event label; Fluorescence, peak A; Fluorescence, peak C; Fluorescence, peak M; Fluorescence, peak T; Fluorescence index; High nucleic acid bacteria; ICP-OES; Iron, dissolved; Karjaanjoki_00; Karjaanjoki_01; Karjaanjoki_02; Karjaanjoki_03; Karjaanjoki_04; Lachat QuickChem 8000 flow injection autoanalyzer; LATITUDE; Leucine incorporation rate; LONGITUDE; Low nucleic acid bacteria; Manganese, dissolved; Manually after Grasshoff et al. (1983); Molecular mass; MULT; Multiple investigations; Nitrate; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen, organic, dissolved; Nitrogen, total; Nitrogen, total dissolved; PDZ Europa ANCA-GSL elemental analyser; Ratio; Salinity; Sample ID; SEC analyser; Silicate; Specific ultraviolet absorbance normalized to DOC; Spectral slope, 275-295 nm; Spectral slope, 300-650 nm; Spectral slope, 350-400 nm; Spectrophotometer UV/VIS (PerkinElmer Lambda 650); Subtracting combined inorganic nitrogen from total dissolved nitrogen; Temperature, water; Thymidine incorporation rate; TOC analyser, MQ1000; Varian Cary Eclipse fluorometer (Agilent); δ13C, dissolved inorganic carbon; δ15N, total dissolved nitrogen
    Type: Dataset
    Format: text/tab-separated-values, 1971 data points
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  • 8
    Publication Date: 2024-04-24
    Description: This compilation gives an overview of the datasets gathered from DOM (DOC, DON, DOP) surveys in the Baltic Sea for the period 2014-2017 discussed in the paper Voss et. al. 2020 (doi:10.1007/s10533-020-00703-5). Sampling took place in the Roskilde Fjord, Vistula and Öre estuaries and Curonian Lagoon during a series of field campaigns by different research groups around the Baltic Sea and subsequently were analysed with comparable internationally standardized methods. Most DOC and DON were measured at the Technical University of Denmark, except samples from the Curonian Lagoon were measured at Klaipeda University, and DON samples from Vistula and Öre estuaries at the IOW. The pre-filtration was in most cases done with 0.2µm filters but sometimes GF/F filters with a nominal pore size of 0.7µm were used. Near bottom samples in Vistula and Öre estuaries were collected from clear water overlying the sediments but often showed elevated particulate matter concentrations. These data sets were treated separately as bottom boundary layer (BBL) data. The data collected during the surveys allows a cross-system comparison, exemplarily for the Baltic Sea, under a wide range of hydrological and environmental situations to test the hypothesis that rivers act as characteristic DOM source – depending on land use in the catchment - which is modified along a salinity gradient from the river offshore.
    Keywords: Baltic Sea; C:N:P ratios; Curonian_lagoon; Denmark; dissolved organic carbon; dissolved organic nitrogen; dissolved organic phosphorus; Ore_estuary; Poland; Roskilde_fjord; Sweden; Vistula_estuary
    Type: Dataset
    Format: application/zip, 264.6 kBytes
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  • 9
    Publication Date: 2021-03-30
    Description: Coastal global oceans are expected to undergo drastic changes driven by climate change and increasing anthropogenic pressures in coming decades. Predicting specific future conditions and assessing the best management strategies to maintain ecosystem integrity and sustainable resource use are difficult, because of multiple interacting pressures, uncertain projections, and a lack of test cases for management. We argue that the Baltic Sea can serve as a time machine to study consequences and mitigation of future coastal perturbations, due to its unique combination of an early history of multistressor disturbance and ecosystem deterioration and early implementation of cross-border environmental management to address these problems. The Baltic Sea also stands out in providing a strong scientific foundation and accessibility to long-term data series that provide a unique opportunity to assess the efficacy of management actions to address the breakdown of ecosystem functions. Trend reversals such as the return of top predators, recovering fish stocks, and reduced input of nutrient and harmful substances could be achieved only by implementing an international, cooperative governance structure transcending its complex multistate policy setting, with integrated management of watershed and sea. The Baltic Sea also demonstrates how rapidly progressing global pressures, particularly warming of Baltic waters and the surrounding catchment area, can offset the efficacy of current management approaches. This situation calls for management that is (i) conservative to provide a buffer against regionally unmanageable global perturbations, (ii) adaptive to react to new management challenges, and, ultimately, (iii) multisectorial and integrative to address conflicts associated with economic trade-offs.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 10
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    American Society of Limnology and Oceanography
    In:  Limnology and Oceanography: Methods, 7 . pp. 430-435.
    Publication Date: 2014-05-07
    Description: The estimation of biomass from body lengths to carbon regressions is a common approach in plankton research. Several different chemicals for sample preservation are in use, and conversion factors to account for shrinkage effects exist, but to our knowledge the consequences of using potassium-iodide and iodine (Lugol solution) as preservative on body sizes of different mesozooplankton groups have not been investigated. We tested the effect of 2% acidified Lugol solution on body sizes over time on two major marine mesozooplankton groups, namely larvaceans and copepods, which are representatives of gelatinous and chitineous plankton, respectively. For both, we observed a significant shrinkage effect over time (P 〈 0.0001). Larvaceans showed a reduction in body size by 20% within the first 2 min, which stabilized after 36 h at 22%, whereas copepods shrank by 17%. These differences were significant (P = 0.0324), with no further shrinkage observed over an additional 3 months. Failure to adequately account for shrinkage effects could result in significant biomass underestimation if length�weight relationships are generated from live material.
    Type: Article , PeerReviewed
    Format: text
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