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  • Other Sources  (54)
  • Conseil de l'Europe  (22)
  • ASLO (Association for the Sciences of Limnology and Oceanography)  (19)
  • American Meteorological Society
  • IFM-GEOMAR
  • MDPI Publishing
  • 2000-2004  (54)
  • 1
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 23, no. 50, pp. 131-136, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Publication Date: 2004
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; USA
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  • 2
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 23, no. 6, pp. 165-168, pp. L24314, (ISSN: 1340-4202)
    Publication Date: 2004
    Keywords: Earthquake hazard ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; leveling ; Geodesy ; El ; Asnam ; Algeria
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  • 3
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 23, no. B11, pp. 111-123, pp. 1892
    Publication Date: 2004
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; Tectonics
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  • 4
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 23, no. 3, pp. 143-148, pp. 1006, (ISSN: 1340-4202)
    Publication Date: 2004
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; Error analysis ; TIDES ; Spectrum ; Soehne, ; Sohne
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  • 5
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 23, no. 10, pp. 125-129, pp. 1370, (ISSN 0343-5164)
    Publication Date: 2004
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; Error analysis
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  • 6
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 49 . pp. 1435-1445.
    Publication Date: 2019-09-23
    Description: Microzooplankton have received increased attention as an important trophic link between the microbial loop and calanoid copepods. On the basis of food size spectra overlap in some microzooplankton groups and calanoid copepods, however, such microzooplankton could function as competitors rather than as food for calanoid copepods (intraguild prey). Mixotrophic flagellates presumably represent a link between the microbial loop and the micro and mesozooplankton. We investigated the effects of microzooplankton and mixotrophy by altering the presence of a heterotrophic dinoflagellate and of a mixotrophic nanoflagellate in artificial food webs with calanoid copepods as terminal consumers. Overall system productivity was manipulated by two levels of nutrient enrichment. The heterotrophic dinoflagellate drastically reduced the nanophytoplankton and enhanced the reproduction of the copepods, suggesting that its role as a competitor is negligible compared to its function as a trophic link. In spite of the presence of heterotrophic nanoflagellates, the mixotroph had a strong negative effect on the picophytoplankton and (presumably) on bacterial biomass. At the same time, the mixotroph enhanced the atomic C:N ratio of the seston biomass, indicating a higher efficiency in overall primary production. Copepod reproduction was enhanced in the presence of the mixotrophic nanoflagellate. Results did not support predictions of the intraguild predation theory: The ratios of the intraguild predators and their preys were not affected by overall system productivity
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  • 7
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    IFM-GEOMAR
    In:  Alkor-Berichte, AL247 . IFM-GEOMAR, Kiel, Germany, 26 pp.
    Publication Date: 2021-01-28
    Description: Dates of Cruise: 11.10. to 14.10.2004 Projects: BASEWECS and Student course in physical oceanography; Port Call: Warnemünde (11.10.)
    Type: Report , NonPeerReviewed
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  • 8
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    IFM-GEOMAR
    In:  Alkor-Berichte, AL240 . IFM-GEOMAR, Kiel, Germany, 21 pp.
    Publication Date: 2021-01-28
    Description: Dates of Cruise: 29.06. to 02.07.2004 Projects: BASEWECS and Student course in physical oceanography Port Calls: Warnemünde (29.06.; 01.07) and Sassnitz (30.06.)
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  • 9
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    IFM-GEOMAR
    In:  IFM-GEOMAR Report, 01 . IFM-GEOMAR, Kiel, Germany, 206 pp.
    Publication Date: 2018-02-27
    Type: Report , PeerReviewed
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  • 10
    Publication Date: 2012-04-20
    Description: The overall objective of the subproject A3 of SFB 460* (1996 - 2003) was to observe the water mass transformation in the eastern basin of the subpolar gyre with direct methods including RAFOS floats. Our floats populated the 1500 m depth range of the Iceland Basin occupied by low salinity Labrador Sea Water and higher salinity Overflow Water. The first water mass reaches the Basin through the Charlie-Gibbs Fracture Zone. Its source region is in the Labrador Sea where it is generated on a yearly basis by deep reaching winter time convection. The second intermediate water mass of the eastern basin enters the region as Iceland Scotland Overflow Water with its perpetual source in the Norwegian Seas. At the southeastern margin of our region of interest remainders of Mediterranean Water mix with the other two characteristic water masses. A smaller number of floats was deployed in the lower deep water of the Iceland Basin at nominally 2600m depth. Data for the presented gallery of intermediate float trajectories were collected between summer 1997 and summer 2003. We have tracked 57 RAFOS floats. These neutrally buoyant in-situ drifters were launched during six research cruises. Their average underwater missions exceeded one year. The Lagrangian experiment lasted until 2003 when all four sound sources were completely recovered. The data set comprises also trajectories from float parks. These ensembles of floats enable repeated Lagrangian time series with identical initial conditions allowing estimates of the representativeness of individual trajectories. *SFB (Sonderforschungsbereich) stands for an accelerated research initiative comprising intensive observations and modelling efforts of fluctuations in the thermohaline circulation in the subpolar gyre of the North Atlantic.
    Type: Report , NonPeerReviewed
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  • 11
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    IFM-GEOMAR
    In:  IFM-GEOMAR, Kiel, p. 82, 17 pp.
    Publication Date: 2012-11-23
    Type: Book , NonPeerReviewed
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  • 12
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    IFM-GEOMAR
    In:  IFM-GEOMAR, Kiel, p. 82, 17 pp.
    Publication Date: 2012-11-23
    Type: Book , NonPeerReviewed
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  • 13
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 49 (1). pp. 168-179.
    Publication Date: 2019-03-06
    Description: We assess population dynamics of picophytoplankton groups (≤2 μm diameter; Prochlorococcus, Synechococcus, and picoeukaryote) at a Pacific Ocean coastal site in the Southern California Bight. Weekly sampling (August 2000 to January 2002), dilution experiments, and flow cytometric analysis were combined with an instrument-specific calibration for cell size determination, allowing biovolume and carbon biomass estimation. Synechococcus was almost always numerically dominant, accounting for 60 ± 12 of the total picoplankton cells over time. It had moderately high growth rates (0.52-0.86 d-1) and was subject to low grazing mortality (-0.14 to -0.39 d-1). Prochlorococcus growth and mortality rates were roughly balanced (0.33 ± 0.14 d-1 and -0.36 ± 0.06 d-1, respectively). Picoeukaryotes had the highest growth rates (0.71-1.29 d-1) and were responsible for, on average, 76 of net carbon production (NCP), amounting in up to 32.05 ± 1.31 μg C L-1 d-1 produced and 28.31 ± 2.61 μg C L-1 d-1 consumed. In order to better define the eukaryotic component of these populations, an isolate was characterized via small subunit rRNA gene sequencing, transmission electron microscopy, and growth experiments and was identified as the prasinophyte Ostreococcus, not previously known to the Pacific Ocean. Our results show that although picoeukaryotes do not stand out as particularly important players in this system on the basis of cell abundance, they dominate in terms of picophytoplankton biomass and trophic transfer potential of carbon in this size class.
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  • 14
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 37 (6). pp. 1146-1163.
    Publication Date: 2018-03-20
    Description: Denitrification was investigated in the Baltic proper at two stations with different conditions in the deep water. The Gotland Deep was examined as an example of a basin with anoxic, H2S‐containing deep water and station T was taken as an example of low‐oxygen (〈0.2 ml liter−1), sulfide‐free deep water. Denitrification was measured by the acetylene blockage method; in addition, N2O reduction was followed in samples without acetylene. To shed light on the factors limiting denitrification, we compared in situ rates to denitrification after adding nitrate or electron donors. Denitrification was restricted to the layer of the oxic‐anoxic interface in the Gotland Deep and to the water layer near the sediment of station T. For both stations it could be shown that denitrification was not limited by nitrate availability. A lack of available organic C seemed to limit denitrification rates and growth of denitrifiers. As a result of C limitation in the water column, denitrification was restricted to energy‐rich interfaces. In the low‐oxygen water away from energy‐rich interfaces, the less C‐demanding nitrification‐denitrification coupling (NH4+ → N2O → N2) seemed to be favored. Denitrification in the water of the central Baltic seems to be subjected to strong variability due to changing C supply during the course of the year. However, limitation by C availability can be assumed for most of the year and should be taken into account in calculating the N budget of the Baltic.
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  • 15
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 48 (5). pp. 1825-1830.
    Publication Date: 2018-06-25
    Description: Environmental evidence suggests that Aureococcus anophagefferens (Pelagophyceae), a eukaryotic picoplankton that blooms in coastal seawaters, can outcompete other organisms because of its ability to use abundant dissolved organic nitrogen (DON). To test this hypothesis, we isolated A. anophagefferens in axenic culture and monitored its growth on high-molecular weight (HMW) DON collected from sediment pore waters, a putative source for DON in bays where blooms occur. HMW DON originating from pore water had a substantially higher protein content than surface seawater DON. We found that A. anophagefferens could deplete 25-36% of the available nitrogen in cultures with HMW DON as the sole source of nitrogen and that this corresponded well with the protein fraction in pore-water HMW DON. High rates of cell surface peptide hydrolysis and no detectable N-acetyl polysaccharide hydrolysis, together with the high percentage of hydrolyzable amino acids compared to hydrolyzable aminosugars present in the HMW DON, pointed to the protein fraction as the more likely source of nitrogen used for growth. Whether or not nitrogen scavenging from protein is a common mechanism in phytoplankton is at present unknown but needs to be investigated
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  • 16
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 48 (5). pp. 1903-1912.
    Publication Date: 2014-01-30
    Description: According to a recent dynamical model, the depth of a well-mixed water column should have contrasting effects on the abundances of sinking and nonsinking phytoplankton taxa. Because of increasing light limitation, nonsinking taxa should decline monotonically with increasing mixing depth, and because of sinking loss limitation at low mixing depths, sinking taxa should peak at intermediate mixing depths. Along a gradient of mixing depths, the position of this maximum should increase with increasing taxon-specific sinking velocity and decrease with increasing background turbidity. In two field-enclosure experiments, we investigated the effects of mixing depth and background turbidity on a variety of sinking and nonsinking phytoplankton taxa. We exposed the natural, 100-µm screened phytoplankton community of a clear, unproductive, but silica-rich lake to a gradient of mixing depths (1.5- 15 m) during 4-6 weeks. To mimic two different background turbidities, the transparent enclosure walls were surrounded by either white or black foliage. Although diatoms suffered from high sedimentation losses at low mixing depths, they dominated biomass at all mixing depths throughout both experiments. Results were largely in accordance with model predictions. Specific gross growth rates of most common taxa were negatively related to mixing depth. In both experiments, the abundances of most sinking taxa showed a unimodal pattern along the mixing depth gradient, while two of three motile taxa declined monotonically with mixing depth. The depths where these taxa reached their maximal abundances were positively related to taxon-specific sinking velocity and negatively related to background turbidity.
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  • 17
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 48 (1). pp. 179-188.
    Publication Date: 2014-01-30
    Description: The uptake and efflux of 64Cu was studied in the marine cyanobacterium Synechoccous strain WH7803 (DC2). Uptake followed classical Michaelis-Menten type kinetics in metal-buffered seawater. The maximum uptake rate, Vmax, was 0.236 ± 0.016 × 10-18 mol Cu cell-1 h-1, with the half-saturation constant, KS, of 10-10.81±0.11 mol L-1. An efflux mechanism was also observed in WH7803, whose growth was inhibited by high internal Cu concentrations. Efflux of Cu enabled WH7803 to maintain homeostasis for Cu at typical seawater ambient free copper concentrations ([Cu2+]f). The sensitivity of WH7803 growth to Cu was related to a simple inability to regulate internal Cu concentrations when external concentrations were 〉10-11 mol L-1.
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  • 18
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    IFM-GEOMAR
    In:  IFM-GEOMAR, Kiel, Germany, 4 pp.
    Publication Date: 2021-01-29
    Description: 19.02.-21.02.2003
    Type: Report , NonPeerReviewed
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  • 19
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 38 (8). pp. 1803-1812.
    Publication Date: 2019-09-23
    Description: Sediments from the River Elbe estuary and incubated sediments were extracted with 1 N HCI for 24 h at room temperature. The extracted ferric and ferrous iron was determined with DC and AC polarography. Acid-volatile sulfide was determined from H2S trapped in aqueous zinc acetate solution. Analysis of sediment samples and extraction residues with Mossbauer spectroscopy demonstrated that the Fe oxidation state was conserved during extraction and polarographic determination, siderite and vivianite were completely dissolved, and Fe(II) in chlorite was partially extracted with HCl. Incubation experiments showed that extractable Fe was almost completely oxidized to Fe(III) at the oxic sediment surface and reduced to Fe(II) in deeper anoxic layers within a few weeks. Reactive Fe(III), i.e. that fraction of Fe which was reducible on the time scale of the incubation experiment, was completely extracted with HCl.
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  • 20
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 48 . pp. 55-67.
    Publication Date: 2014-01-30
    Description: Carbon acquisition in relation to CO2 supply was investigated in three marine bloom-forming microalgae, the diatom Skeletonema costatum, the flagellate Phaeocystis globosa, and the coccolithophorid Emiliania huxleyi. In vivo activities of extracellular (eCA) and intracellular (iCA) carbonic anhydrase activity, photosynthetic O2 evolution, CO2 and HCO uptake rates were measured by membrane inlet mass spectrometry in cells acclimated to pCO2 levels of 36, 180, 360, and 1,800 ppmv. Large differences were obtained between species both with regard to the efficiency and regulation of carbon acquisition. While eCA activity increased with decreasing CO2 concentration in S. costatum and P. globosa, consistently low values were obtained for E. huxleyi. No clear trends with pCO2 were observed in iCA activity for any of the species tested. Half saturation concentrations (K1/2) for photosynthetic O2 evolution, which were highest for E. huxleyi and lowest for S. costatum, generally decreased with decreasing CO2 concentration. In contrast, K1/2 values for P. globosa remained unaffected by pCO2 of the incubation. CO2 and HCO3- were taken up simultaneously by all species. The relative contribution of HCO3- to total carbon uptake generally increased with decreasing CO2, yet strongly differed between species. Whereas K1/2 for CO2 and HCO3- uptake was lowest at the lowest pCO2 for S. costatum and E. huxleyi, it did not change as a function of pCO2 in P. globosa. The observed taxon-specific differences in CO2 sensitivity, if representative for the natural environment, suggest that changes in CO2 availability may influence phytoplankton species succession and distribution. By modifying the relative contribution of different functional groups, e.g., diatomaceous versus calcareous phytoplankton, to the overall primary production this could potentially affect marine biogeochemical cycling and air-sea gas exchange.
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  • 21
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 48 (2). pp. 764-776.
    Publication Date: 2014-01-30
    Description: The chemical speciation of dissolved Cu was investigated by voltammetric methods in Gullmar Fjord, Sweden, over the course of a year from September 1996 until August 1997. Sampling was carried out on a roughly monthly basis, with an intensive survey carried out in May 1997. Surface water temperatures ranged from 21 to 22°C, whereas bottom waters in the fjord were approximately 6°C throughout. Macronutrient concentrations in the fjord during the period of the survey were investigated independently by the Göteborgs och Bohus läns Vattenvårdsförbund (Water Quality Association of Göteborg and Bohus). Surface phosphate concentrations were highest in early spring with low levels (〈0.1 mmol kg-1) over the late spring and summer. Nitrate and silicate showed a similar pattern to phosphate with the exception of high concentrations encountered in surface waters when low salinity plumes caused by runoff were encountered. A period of calm, sunny weather in January 1997 saw the initiation of the spring bloom some 2 months earlier than usual. Dissolved Cu speciation was dominated by organic complexation (over 99.8%) throughout this study. Strong Cu binding ligands (log K 〉 12.5) were not detected during the winter or early spring and could be related to the temperature-related seasonal appearance of the cyanobacterium Synechoccocus in these waters. The appearance of the strong Cu ligands led to a decrease in the concentration of free copper, resulting in a seasonal cycle for free copper in the fjord. This is the first study to examine Cu speciation over an annual cycle in a coastal environment
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  • 22
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 47 . pp. 1324-1335.
    Publication Date: 2014-01-30
    Description: EisenEx�the second in situ iron enrichment experiment in the Southern Ocean�was performed in the Atlantic sector over 3 weeks in November 2000 with the overarching goal to test the hypothesis that primary productivity in the Southern Ocean is limited by iron availability in the austral spring. Underwater irradiance, chlorophyll a (Chl a), photochemical efficiency, and primary productivity were measured inside and outside of an iron-enriched patch in order to quantify the response of phytoplankton to iron fertilization. Chl a concentration and photosynthetic rate (14C uptake in simulated in situ incubations) were measured in pico-, nano-, and microphytoplankton. Photochemical efficiency was studied with fast repetition rate fluorometry and xenon-pulse amplitude modulated fluorometry. The high-nutrient low-chlorophyll waters outside the Fe-enriched patch were characterized by deep euphotic zones (63-72 m), low Chl a (48-56 mg m-2), low photosynthetic efficiency (Fv/Fm ~ 0.3), and low daily primary productivity (130-220 mg C m-2 d-1). Between 70 and 90% of Chl a was found in pico- and nanophytoplankton. During the induced bloom, Fv/Fm increased up to ;0.55, primary productivity and Chl a reached the maximum values of 790 mg C m-2 d-1 and 231 mg Chl a m-2, respectively. As a consequence, the euphotic depth decreased to ~41 m. Picophytoplankton biomass hardly changed. Nano- and microphytoplankton biomass increased. In the first 2 weeks of the experiment, when the depth of the upper mixed layer was mostly 〈40 m, primary productivity was highly correlated with Chl a. In the third week, productivity was much lower than predicted from Chl a, probably because of a reduction in photosynthetic capacity as a consequence of increased physical variability in the upper water column. These results provide unequivocal evidence that iron supply is the central factor controlling phytoplankton primary productivity in the Southern Ocean, even if the mixing depth is 〉80 m.
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  • 23
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 47 (3). pp. 753-761.
    Publication Date: 2014-01-30
    Description: Flows of the major biogeochemical elements (C, N, P, Si) and of transparent exopolymer particles (TEP) were traced during a bloom of a natural assemblage of marine diatoms in a mesocosm (l m(3)) to determine whether the exudation and subsequent gelation of carbon-rich phytoplankton exopolymers can account for the formation and potential export of carbon in excess of that predicted by Redfield ratios. Exponential growth of the phytoplankton community in the mesocosm extended for 10 d until nitrate concentration fell below detection and concentrations of dissolved inorganic and particulate organic nitrogen and phosphorus remained stable. Tight covariation of particulate organic elements occurred as long as nutrients were replete. But, after nitrate depletion, decoupling of carbon dynamics from that of nitrogen and phosphorus was observed, with a large flow of carbon into TEP An uptake of 72% more dissolved inorganic carbon (DIC) than inferred from nitrate supply and Redfield stoichiometry (referred to as carbon overconsumption) occurred during the study, largely during the postbloom phase, and was almost entirely traced to the particulate organic matter (POM) pool. Marine snow (aggregates 〉0.5 mm) appeared at the onset of nitrate depletion and coincided with rapid increase in TEP concentrations. Elemental composition of marine snow differed from the Redfield ratio by an enrichment in carbon and a depletion in phosphorus relative to nitrogen. It is suggested that sinking of TEP-rich marine snow could be a possible mechanism for export of carbon above calculations that are based on the Redfield stoichiometry.
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  • 24
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    IFM-GEOMAR
    In:  IFM-GEOMAR, Kiel, Germany, 4 pp.
    Publication Date: 2021-01-29
    Description: 14.10.-16.10.2002
    Type: Report , NonPeerReviewed
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  • 25
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    IFM-GEOMAR
    In:  [Poster] In: 100 Jahre Kieler Meeresforschung, 07.-30.06.2002, Kiel, Germany .
    Publication Date: 2013-11-20
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  • 26
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    IFM-GEOMAR
    In:  [Poster] In: 100 Jahre Kieler Meeresforschung, 07.-30.06.2002, Kiel, Germany .
    Publication Date: 2013-11-20
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  • 27
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    IFM-GEOMAR
    In:  [Poster] In: 100 Jahre Kieler Meeresforschung, 07.-30.06.2002, Kiel, Germany .
    Publication Date: 2013-11-20
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  • 28
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    IFM-GEOMAR
    In:  [Poster] In: 100 Jahre Kieler Meeresforschung, 07.-30.06.2002, Kiel, Germany .
    Publication Date: 2013-11-20
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  • 29
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 47 . pp. 120-128.
    Publication Date: 2014-01-30
    Description: The carbon isotopic composition of marine phytoplankton varies significantly with growth conditions. Aqueous CO2 concentration [CO2] and algal growth rate (µ) have been suggested to be important factors determining isotope fractionation (ep). Here we examine ep of the coccolithophorid Emiliania huxleyi in relation to CO2 concentration and light conditions in dilute batch cultures. Cells were incubated at different irradiance cycles, photon flux densities (PFDs), and [CO2]. Isotope fractionation varied between 6.7 and 12.3‰ under 16 : 8 h light : dark cycle (L :D) and between 14.7 and 17.8‰ at continuous light. ep was largely independent of ambient [CO2], varying generally by less than 2‰ over a range of [CO2] from 5 to 34 mmol L-1. Instantaneous carbon-specific growth rates (µC) and PFDs, ranging from 15 to 150 mmol m-2 s-1, positively correlated with ep. This result is inconsistent with theoretical considerations and experimental results obtained under constant light conditions, suggesting an inverse relationship between ep and µ. In the present study the effect of PFDs on ep was stronger than that of mand thus resulted in a positive relationship between µ and ep. In addition, the L:D cycle of 16 : 8 h resulted in significantly lower ep values compared to continuous light. Since the observed offset of about 8‰ could not be related to daylength dependent changes in µC, this implies a direct influence of the irradiance cycle on ep. These findings are best explained by invoking active carbon uptake in E. huxleyi. If representative for the natural environment, these results complicate the interpretation of carbon isotope data in geochemical and paleoceanographic applications.
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  • 30
    Publication Date: 2018-06-25
    Description: Although N2-fixing cyanobacteria contribute significantly to oceanic sequestration of atmospheric CO2, little is known about how N2 fixation and carbon fixation (primary production) interact in natural populations of marine cyanobacteria. In a developing cyanobacterial bloom in the Baltic Sea, rates of N2 fixation (acetylene reduction) showed both diurnal and longer-term fluctuations. The latter reflected fluctuations in the nitrogen status of the cyanobacterial population and could be correlated with variations in the ratio of acetylene reduced to 15N2 assimilated. The value of this ratio may provide useful information about the release of newly fixed nitrogen by a cyanobacterial population. However, although the diurnal fluctuations in N2 fixation broadly paralleled diurnal fluctuations in carbon fixation, the longer-term fluctuations in these two processes were out of phase.
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  • 31
    Publication Date: 2020-04-24
    Type: Report , NonPeerReviewed
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 4a, pp. 53-56, pp. 2083, (ISBN 1-86239-117-3)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Geol. aspects ; paleo ; Seismicity ; Fault zone ; The ; Netherlands ; Germany ; Roermond ; GPR ; electrical ; Tomography ; Liege ; KNMI ; LGIH ; NITG-NTO
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  • 33
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 3, pp. 93-96, pp. B02405, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Fault zone ; Germany ; Juelich ; Eifel ; Niederrhein ; Bucht ; paleo ; Seismicity
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. B6, pp. 105-108, pp. B03403, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Structural geology ; Fault zone ; paleo ; Seismicity ; Basel ; Bree ; Oberrhein ; Graben ; Niederrhein ; Bucht ; PALEOSIS ; Roer ; Feldbiss ; Switzerland ; Germany ; Belgium ; Netherlands
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. B6, pp. 109-111, pp. B03403, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Structural geology ; Fault zone ; paleo ; Seismicity ; Basel ; Oberrhein ; Graben ; Switzerland
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 2, pp. 83-88, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 2001
    Keywords: Earthquake hazard ; paleo ; Seismicity ; Fault zone ; Belgium ; The ; Netherlands ; Germany ; Refraction seismics ; Reflection seismics ; GPR ; Geoelectrics ; Electromagnetic methods/phenomena ; Tomography
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 5, pp. 113-115, pp. L09603, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Strain ; paleo ; Seismicity ; Tien ; Tian ; Shan ; Bishkek ; Suusamyr ; Pamir ; lake ; Issyk ; Kul ; C14 ; Kirgisia ; Graefe, ; Grafe
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  • 38
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 19, pp. 89-92, pp. L19312, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; France ; Italy ; Project report/description ; Fault zone ; J. ; Déverchère
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  • 39
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 2, pp. 35-38, pp. 2501, (ISBN: 0-12-018847-3)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Seismicity ; Niederrhein ; Bucht ; Germany
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  • 40
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 20, pp. 39-43, pp. B04102, (ISBN: 0-12-018847-3)
    Publication Date: 2001
    Keywords: Earthquake hazard ; paleo ; Seismicity ; Project report/description ; Oberrhein ; Germany
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 1-4, pp. 147-152, pp. L12309, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Fault zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Structural geology ; paleo ; Seismicity ; Feldbiss ; Belgium
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  • 42
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 33, pp. 1-4, pp. 2163
    Publication Date: 2001
    Keywords: Earthquake hazard ; Earthquake risk ; Munich ; Re
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  • 43
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 2, pp. 31-34, pp. 2501, (ISBN: 0-12-018847-3)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Structural geology ; Fault zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Niederrhein ; Bucht
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 2, pp. 57-61, pp. B05309, (ISBN 0-471-26610-8)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Belgium ; Fault zone ; Roermond ; The ; Netherlands ; Neeroeteren
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  • 45
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 4, pp. 133-134, pp. B09402, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; paleo ; Seismicity ; Italy
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  • 46
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 1-4, pp. 153-156, pp. L12309, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; Niederrhein ; Bucht ; PALEOSIS ; paleo ; Seismicity ; Structural geology ; trenching
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 1-4, pp. 157-161, pp. L12309, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Earthquake hazard ; paleo ; Seismicity ; Structural geology ; trenching ; Belgium
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    Conseil de l'Europe
    In:  Cahiers du Centre Européen de Géodynamique et de Séismologie, Luxembourg, Conseil de l'Europe, vol. 18, no. 19, pp. 77-78, pp. 1484, (ISBN: 0534351875, 2nd edition)
    Publication Date: 2001
    Keywords: Earthquake hazard ; paleo ; Seismicity ; Chile ; South ; America
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 46 . pp. 1378-1391.
    Publication Date: 2014-01-30
    Description: Rates of cellular uptake of CO2 and HCO3- during steady-state photosynthesis were measured in the marine diatoms Thalassiosira weissflogii and Phaeodactylum tricornutum, acclimated to CO2 partial pressures of 36, 180, 360, and 1,800 ppmv. In addition, in vivo activity of extracellular (eCA) and intracellular (iCA) carbonic anhydrase was determined in relation to CO2 availability. Both species responded to diminishing CO2 supply with an increase in eCA and iCA activity. In P. tricornutum, eCA activity was close to the detection limit at higher CO2 concentrations. Simultaneous uptake of CO2 and HCO3- was observed in both diatoms. At air-equilibrated CO2 levels (360 ppmv), T. weissflogii took up CO2 and HCO3- at approximately the same rate, whereas CO2 uptake exceeded HCO3- uptake by a factor of two in P. tricornutum. In both diatoms, CO2 :HCO3- uptake ratios progressively decreased with decreasing CO2 concentration, whereas substrate affinities of CO2 and HCO3- uptake increased. Half-saturation concentrations were always 〈=5 mM CO2 for CO2 uptake and 〈700 mM HCO3- for HCO3- uptake. Our results indicate the presence of highly efficient uptake systems for CO2 and HCO3- in both diatoms at concentrations typically encountered in ocean surface waters and the ability to adjust uptake rates to a wide range of inorganic carbon supply.
    Type: Article , PeerReviewed
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 46 . pp. 964-970.
    Publication Date: 2014-01-30
    Description: Redfield ratios of remineralization are calculated based on chemical data analysis on isopycnal surfaces. The concentrations of dissolved inorganic carbon used in this study were corrected for the anthropogenic CO2 content as estimated with a back-calculation technique. The corrections increased the apparent carbon remineralization by 25-30%, thus proving important for the reliable estimation of Redfield carbon ratios in the presence of anthropogenic CO2. Best estimates from this study largely confirm the more recently published Redfield ratios of remineralization. The following results were obtained for the latitude range 3-41°N along 20-29°W in the Northeast Atlantic Ocean: Corg: P ratio = 123 ± 10; Corg : N ratio = 7.2 ± 0.8; -O2 :Corg ratio = 1.34 ± 0.06; -O2 : P ratio = 165 ± 15; N: P ratio = 17.5 ± 2.0. These ratios are in close agreement with the average composition of phytoplankton and represent respiration of organic matter consisting on average of 52% protein, 36% polysaccharide, and 12% lipid.
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 46 . pp. 749-757.
    Publication Date: 2018-06-25
    Description: In contrast to most pelagic primary producers, benthic macrophytes pass through morphologically distinct life stages, which can be subject to different ecological controls. Using factorial field experiments, we investigated how grazing pressure (three levels) and nutrient supply (four levels) interact in controlling the passage of marine macroalgae through an apparent recruitment bottleneck at the germling stage. In comparative experiments, we asked whether relative bottom-up and top-down effects on early life stages (〈4 week germlings) vary (1) between the eutrophic Baltic Sea and the oligotrophic NW Atlantic, (2) across seasons in the NW Atlantic, and (3) among annual and perennial macroalgae. In both systems nutrient enrichment favored and grazers suppressed recruitment of green and brown annual algae; however, enrichment effects were much more pronounced in the Baltic, whereas grazer effects dominated in the NW Atlantic. Grazers induced a shift from grazer-susceptible green to more resistant brown algae in the Baltic without reducing total germling density. In the NW Atlantic, grazers strongly reduced overall recruitment rate throughout all seasons. Effects on perennials were similar in both systems with moderate losses to grazing and no effects of nutrient enrichment. Recruit densities and species composition shifted with season in the NW Atlantic. We conclude that the relative effects of grazers and nutrient enrichment depended on the nutrient status of the system, algal life history strategy, and season. Strong bottom-up and top-down controls shape benthic community composition before macroalgae reach visible size
    Type: Article , PeerReviewed
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    Publication Date: 2018-06-25
    Description: Iron supply is thought to regulate primary production in high nitrate, low chlorophyll (HNLC) regions of the sea in both the past and the present. A critical aspect of this relationship is acquisition of iron (Fe) by phytoplankton, which occurs through a complex series of extracellular reactions that are influenced by Fe chemistry and speciation. During the first in situ mesoscale Fe-enrichment experiment in the Southern Ocean (Southern Ocean iron release experiment [SOIREE]), we monitored the uptake of Fe by three size classes of plankton and their ensuing physiological response to the Fe enrichment. Rates of Fe uptake from both inorganic Fe (Fe') and organic Fe complexes (FeL) were initially fast, indicative of Fe-limitation. After Fe enrichment phytoplankton down-regulated Fe uptake and optimized physiological performance, but by day 12 they had greatly increased their capacity to acquire Fe from FeL. The increase in Fe uptake from FeL coincided with a sixfold decrease in Fe' that followed the production of Fe-binding organic ligands. Phytoplankton were able to use organically bound Fe at rates sufficient to maintain net growth for more than 42 d. Adaptation to such shifts in Fe chemistry may contribute to bloom longevity in these polar HNLC waters.
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 46 . pp. 497-504.
    Publication Date: 2014-01-30
    Description: Blooms of the marine diatom Skeletonema costatum were initiated in closed-system batch cultures with P-deficient medium under two different initial concentrations of dissolved molecular CO2([CO2,aq]: 20.6 and 4.5 µmol L-1). Algal C: N: P ratios strongly increased with decreasing P concentration. In the exponential growth phase, C: N ratios were 1.3 mol mol-1 higher in the low relative to the high [CO2,aq] treatment. There was no [CO2,aq] effect on C: N: P ratios during P-limited growth. Carbon isotope fractionation («p ) was 2-3‰ higher in the high [CO2,aq] treatment. With growth rate decreasing due to P limitation, ep increased in both [CO2,aq] treatments by 2-3‰ despite decreasing [CO2,aq]. Under these conditions the effect of decreasing growth rate on isotope fractionation strongly dominated over that of declining CO2 availability. When extrapolated to the natural environment, these results imply that systematic changes in algal growth, as occurring during the course of phytoplankton blooms, may affect algal isotope fractionation. These results severely complicate the interpretation of carbon isotope measurements in suspended and sedimentary organic matter
    Type: Article , PeerReviewed
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    ASLO (Association for the Sciences of Limnology and Oceanography)
    In:  Limnology and Oceanography, 45 (2). pp. 339-349.
    Publication Date: 2018-06-25
    Description: By factorial field experiments we analyzed the relative effects of increased nutrient (N+P) loading and natural grazing pressure on species composition, carbon storage, and nitrogen retention in the Baltic Sea littoral food web, composed of macroalgae, grazers (snails, isopods, amphipods), and predators (shrimps, crabs, fish). Nitrogen was depleted relative to phosphorus throughout most of the year. Increasing nitrogen (6–200% over ambient concentrations) enhanced algal productivity and cover of fast-growing annual algae, grazer, and predator densities, suggesting a three-level bottom-up effect. With increasing nitrogen loading, annual algae increasingly blocked perennial algal recruitment (65–98% decrease) and growth. Grazers counteracted the effects of nutrient enrichment on algal species composition through selective consumption of annual algae. Grazer exclusion had equivalent negative effects on perennial recruitment as a 85% increase in nitrogen loading. Nutrient enrichment increased algal nitrogen content and decreased tissue C: N ratios in spring and summer but not in fall. Carbon storage and nitrogen retention, measured as C and N retained in plant biomass at the end of the growth season, were increased by grazers (C: 39%, N: 24%) but decreased with increasing nitrogen loading (C: -71%, N: -74%). Our results emphasize the important role of grazers in buffering moderate eutrophication effects and illustrate how food web interactions and shifts in species composition are tightly linked to coastal ecosystem function
    Type: Article , PeerReviewed
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