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  • 1
    Online-Ressource
    Online-Ressource
    Stuttgart :Schweizerbart,
    Schlagwort(e): Ecology. ; Lake ecology. ; Limnology. ; Electronic books.
    Materialart: Online-Ressource
    Seiten: 1 online resource (290 pages)
    Ausgabe: 1st ed.
    ISBN: 9783510654482
    DDC: 574.5
    Sprache: Deutsch
    Anmerkung: Cover -- Title -- Impressum -- Inhalt -- Vorwort -- 1 Ein See mit langer Untersuchungstradition -- 2 Bodenseeeinzugsgebiet -- 2.1 Landschaftselemente -- 2.2 Klima -- 2.2.1 Temperatur -- 2.2.2 Wind -- 2.2.3 Niederschlag -- 2.3 Zufl üsse -- 2.4 Landnutzung im Einzugsgebiet -- 2.4.1 Die natürliche Vegetation -- 2.4.2 Die heutige sekundäre Naturlandschaft -- 3 Abiotische Strukturen und Prozesse -- 3.1 Beckenmorphologie und Sedimente -- 3.1.1 Seeteile und Seebecken -- 3.1.2 Zusammensetzung und regionale Verteilung der Sedimente -- 3.1.3 Regionale Muster der Sedimentation -- 3.1.4 Jahreszeitliche Sedimentationsmuster -- 3.2 Wasserstände und Wasserhaushalt -- 3.2.1 Wasserstände -- 3.2.2 Wasserbilanz -- 3.2.3 Austausch- und Verweilzeiten -- 3.3 Schichtungsentwicklung und Durchmischungs prozesse -- 3.3.1 Wärmehaushalt des Sees -- 3.3.2 Thermische Schichtung des Sees -- 3.3.3 Oberflächenschwingungen und interne Wellen -- 3.3.4 Strömungen und turbulente Durchmischungen -- 3.3.5 Dichteströmungen -- 3.3.6 Einschichtung und Transport von Flusswasser -- 3.4 Wasserchemismus -- 3.4.1 Jahreszeitliche Änderungen der Tiefenverteilungen der Stoffe -- 4 Die Lebensgemeinschaften des Bodensees -- 4.1 Die Lebensgemeinschaft der Freiwasserzone -- 4.1.1 Pflanzliches Plankton -- 4.1.2 Die tierische Planktongemeinschaft (Zooplankton) -- 4.1.3 Bakterienplankton -- 4.1.4 Die Fische -- 4.1.5 Vertikalverteilung und vertikale Wanderungen von Plankton und Fischen -- 4.1.6 Horizontale Verteilungsmuster -- 4.1.7 Der Bodensee als Modellsystem für die pelagische Planktonsukzession -- 4.2 Die Lebensgemeinschaft der Ufer- und Flachwasserzone -- 4.2.1 Zonierung der Flachwasserzone -- 4.2.2 Pfl anzliche Lebensgemeinschaften der Ufer- und Flachwasserzone -- 4.2.3 Mikrobielle Lebensgemeinschaften -- 4.2.4 Tierische Lebensgemeinschaften -- 4.3 Die Lebensgemeinschaft des tiefen Seebodens. , 4.3.1 Die Besonderheiten des profundalen Lebensraums -- 4.3.2 Raumzeitliche Verteilungsmuster der Lebensgemeinschaften -- 4.3.3 Die wichtigsten Organismengruppen -- 4.4 Biotische Stoff- und Energieflüsse -- 4.4.1 Erfassung von Stoffkreisläufen -- 4.4.2 Schematische Darstellung der wichtigsten Stoff-Flüsse im See -- 4.4.3 Kohlenstoff- und Nährstoff-Flüsse in der Freiwasserzone des Obersees -- 4.4.4 Litorale Stoffumsätze und Sediment-Wasser-Austausch -- 4.4.5 Profundale Stoffumsätze und Sediment-Wasser-Austausch -- 4.4.6 Besonderheiten der biotischen Stoff-Flüsse des Untersees -- 5 Anthropogene Belastungen -- 5.1 Die IGKB als Instrument zum grenzüberschreitenden Gewässerschutz -- 5.2 Nährstoffbelastung (Phosphor, Stickstoff) -- 5.2.1 Eutrophierung - die bislang gravierendste Belastung des Sees -- 5.2.2 Trophierelevante Entwicklungen im Einzugsgebiet -- 5.2.3 Zeitliche Entwicklung von Nährstoff-Frachten -- 5.2.4 Chemische Reaktion des Sees auf die Änderungen der Nährstoffzufuhr -- 5.2.5 Die Reaktion der Lebensgemeinschaften auf die Nährstoffänderungen -- 5.2.6 Eutrophierung und Oligotrophierung im Untersee -- 5.2.7 Zusammenfassende Betrachtung der Trophieentwicklung -- 5.3 Einfl uss des Klimawandels und von Klimavariabilität -- 5.3.1 Auswirkungen des Klimawandels -- 5.3.2 Gründe und Auswirkungen interannueller Klimavariabilität -- 5.3.3 Welche Veränderungen sind mit einer weiteren Klimaerwärmung zu erwarten? -- 5.4 Mikroverunreinigungen -- 5.4.1 Die aktuelle Belastungssituation des Bodensee-Wasserkörpers -- 5.4.2 Die aktuelle Belastung der Sedimente -- 5.4.3 Anreicherung in Nahrungsketten -- 5.4.4 Die aktuelle Belastung der Zuflüsse -- 5.4.5 Belastungsmodelle -- 5.4.6 Bewertung des Belastungszustandes -- 5.4.7 Minimierungsmaßnahmen -- 5.4.8 Zusammenfassende Betrachtung mit Ausblick -- 5.5 Eingriffe in den Wasser- und Energiehaushalt. , 5.5.1 Flussregulierungen -- 5.5.2 Die „Rheinvorstreckung" -- 5.5.3 Speicherkraftwerke im Einzugsgebiet des Bodensees -- 5.5.4 Wasserentnahme für Trinkwasser -- 5.5.5 Nutzung des Bodenseewassers für Kühlzwecke und Wärmegewinnung -- 5.5.6 Anthropogen bedingte Veränderungen der Wasserstände -- 5.6 Belastungen der Ufer- und Flachwasserzone -- 5.6.1 IGKB-Ansatz zur Erfassung und Bewertung von Defi ziten der Ufer- und Flachwasserzone -- 5.6.2 Erfassung des Ist-Zustands -- 5.6.3 Uferrenaturierungen und Uferschutz -- 5.7 Neobiota -- 5.7.1 Neophyten -- 5.7.2 Neozoen -- 5.8 Hygienische Belastungen -- 5.8.1 Aktuelle Belastungen mit Fäkalkeimen am Bodensee -- 5.8.2 Belastungsquellen -- 5.8.3 Verbleib der Keime im Gewässer -- 5.8.4 Maßnahmenkonzepte -- 6 Standortbestimmung und Ausblick -- 6.1 Lehren aus dem Fallbeispiel Eutrophierung -- 6.2 Gewässerüberwachung und Zustandsbewertung -- 6.3 Verbleibende Wissensdefi zite -- 6.4 Ausblick -- 7 Literatur -- 8 Sach- und Artenregister.
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Kunzmann, Alessandra Janina; Ehret, Harald; Yohannes, Elizabeth; Straile, Dietmar; Rothhaupt, Karl-Otto (2019): Calanoid copepod grazing affects plankton size structure and composition in a deep, large lake. Journal of Plankton Research, 41(6), 955-966, https://doi.org/10.1093/plankt/fbz067
    Publikationsdatum: 2023-01-30
    Beschreibung: The dataset compiles cell counts and biovolumes of different plankton groups (phytoplankton, ciliates, rotifers, heterotrophic nanoflagellates, and bacteria) obtained from three in situ bottle experiments conducted in September/October 1998 with the copepod Eudiaptomus gracilis as grazer.
    Schlagwort(e): bottle experiment; Cell biovolume; Cells, total; ciliates; DATE/TIME; Eudiaptomus_Experiment; EXP; Experiment; grazing; Lake Constance; Name; Phytoplankton; Plankton, biovolume; Replicate; rotifers; Taxon/taxa; Treatment
    Materialart: Dataset
    Format: text/tab-separated-values, 26880 data points
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  • 3
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Science Ltd
    Global change biology 6 (2000), S. 0 
    ISSN: 1365-2486
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Biologie , Energietechnik , Geographie
    Notizen: Long-term data on water temperature, phytoplankton biovolume, Bosmina and Daphnia abundance and the timing of the clear-water phase were compared and analysed with respect to the influence of the North Atlantic Oscillation (NAO) in two strongly contrasting lakes in central Europe. In small, shallow, hypertrophic Müggelsee, spring water temperatures and Daphnia abundance both increased more rapidly than in large, deep, meso/oligotrophic Lake Constance. Because of this, the clear-water phase commenced approximately three weeks earlier in Müggelsee than in Lake Constance. In Müggelsee, the phytoplankton biovolume during late winter/early spring was related to the NAO index. In Lake Constance, where phytoplankton growth was inhibited by intense downward mixing during all years studied, this was not the case. However, in both lakes, interannual variability in water temperature, in Daphnia spring population dynamics and in the timing of the clear-water phase, were all related to the interannual variability of the NAO index. The Daphnia spring population dynamics and the timing of the clear-water phase appear to be synchronized by the NAO despite large differences between the lakes in morphometry, trophic status and flushing and mixis regimes, and despite the great distance between the lakes (∼700 km). This suggests that a great variety of lakes in central Europe may possibly have exhibited similar interannual variability during the last 20 years.
    Materialart: Digitale Medien
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  • 4
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Science Ltd
    Freshwater biology 50 (2005), S. 0 
    ISSN: 1365-2427
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Biologie
    Notizen: 1. In an attempt to discern long-term regional patterns in phytoplankton community composition we analysed data from five deep peri-alpine lake basins that have been included in long-term monitoring programmes since the beginning of the 1970s. Local management measures have led to synchronous declines in phosphorus concentrations by more than 50% in all four lakes. Their trophic state now ranges from mesotrophic to oligotrophic.2. No coherence in phytoplankton biomass was observed among lakes, or any significant decrease in response to phosphorus (P)-reduction (oligotrophication), except in Lakes Constance and Walen.3. Multivariate analyses identified long-term changes in phytoplankton composition, which occurred coherently in all lakes despite the differing absolute phosphorus concentrations.4. In all lakes, the phytoplankton species benefiting from oligotrophication included mixotrophic species and/or species indicative of oligo-mesotrophic conditions.5. A major change in community composition occurred in all lakes at the end of the 1980s. During this period there was also a major shift in climatic conditions during winter and early spring, suggesting an impact of climatic factors.6. Our results provide evidence that synchronous long-term changes in geographically separated phytoplankton communities may occur even when overall biomass changes are not synchronous.
    Materialart: Digitale Medien
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  • 5
    Digitale Medien
    Digitale Medien
    Springer
    Environmental modeling and assessment 2 (1997), S. 13-22 
    ISSN: 1573-2967
    Schlagwort(e): trophic level ; trophic position ; dead organic matter ; carbon recycling ; trophic structure ; nutrient cycling
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Energietechnik
    Notizen: Abstract 1. The importance of the recycling of organic matter for the overall carbon and nutrient flow in a food web, e.g., by the microbial loop has been recognized for pelagic and other ecosystems during the last decade. In contrast, analyses of the trophic food web structure conducted, e.g., by network analysis based on mass‐balanced flow diagrams (i.e., computation of, e.g., trophic positions and transfer efficiencies, organismal composition of trophic levels) which greatly contribute to our understanding of the flow and cycling of matter in food webs, have not yet responded adequately to this fact by developing coherent techniques with which dead organic matter and its consumers could be considered in the models. 2. At present, dead organic matter (measured in units of carbon or nutrients) is either allocated to a fixed trophic position (between zero and one), or the trophic position of dead autochthonous material depends on the trophic position of the organisms which released it. This causes partially ambiguous and inconsistent interpretations of key measures like trophic transfer efficiences and trophic positions and greatly hampers cross‐system comparisons. 3. The present paper describes and compares four different definitions of the trophic position of dead autochthonous organic material which have either been newly invented or already used. Their impact on the resulting trophic positions of individual groups is illustrated using a food web model from the pelagic zone of Lake Constance. The present analysis evaluates the partially far reaching consequences of the definition chosen, and suggests to allocate all dead organic material to the ‘zeroth’ trophic level irrespectively of its origin (allochthonous or autochthonous), chemical composition and the commodity used to quantify the food web model (e.g., units of carbon or nutrients). By this means trophic positions and trophic transfer efficiencies get a clear and consistent ecological interpretation, while inconsistencies between analyses conducted in units of carbon or nutrients and some operational problems can be overcome and cross‐system comparisons and empirical verification are facilitated.
    Materialart: Digitale Medien
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  • 6
    Publikationsdatum: 2018-10-11
    Materialart: Article , NonPeerReviewed
    Format: text
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  • 7
    Publikationsdatum: 2020-08-13
    Beschreibung: In many regions across the globe, extreme weather events such as storms have increased in frequency, intensity, and duration due to climate change. Ecological theory predicts that such extreme events should have large impacts on ecosystem structure and function. High winds and precipitation associated with storms can affect lakes via short‐term runoff events from watersheds and physical mixing of the water column. In addition, lakes connected to rivers and streams will also experience flushing due to high flow rates. Although we have a well‐developed understanding of how wind and precipitation events can alter lake physical processes and some aspects of biogeochemical cycling, our mechanistic understanding of the emergent responses of phytoplankton communities is poor. Here we provide a comprehensive synthesis that identifies how storms interact with lake and watershed attributes and their antecedent conditions to generate changes in lake physical and chemical environments. Such changes can restructure phytoplankton communities and their dynamics, as well as result in altered ecological function (e.g., carbon, nutrient and energy cycling) in the short‐ and long‐term. We summarize the current understanding of storm‐induced phytoplankton dynamics, identify knowledge gaps with a systematic review of the literature, and suggest future research directions across a gradient of lake types and environmental conditions.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 8
    Publikationsdatum: 2017-02-02
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2022-10-08
    Beschreibung: Many lake ecosystems that have been severely disturbed by eutrophication, have also experienced large human efforts to restore “natural” conditions. However, the trajectories and the extent of recovery of these lake ecosystems are still poorly understood. In many shallow lakes, recovery was often delayed and counter‐clockwise hysteretic. Here, we study recovery and ecosystem trajectories in a large and deep lake using diatom remains in sediment cores and time series of phosphorus concentrations. We identified four periods of diatom community change: slow change during early eutrophication, thereafter a short period of rapid change after the 1950s, followed by community stability from the 1960s to the mid‐1980s, and finally a recovery phase until 2010. Diatom community structure responded quickly and in a saturating way to increasing phosphorus concentrations, but also fast to phosphorus decline. Hence, diatom community dynamics did not show counter‐clockwise hysteresis but was characterized by a high degree of recovery and clock‐wise hysteresis (CWH). We suggest that CWH in response to eutrophication and recovery is a typical and previously overlooked feature of deep lakes, which results from a more rapid change of average nutrient concentrations and thus productivity in the epilimnion compared to average nutrient concentrations across the entire water column. Such nonlinear and hysteretic responses to changing nutrients need to be considered when analyzing the effects of other stressors such as climate warming on ecosystem dynamics to prevent erroneous attribution of ecosystem change to other stressors instead of nutrient change.
    Beschreibung: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Beschreibung: European Regional Development Fund http://dx.doi.org/10.13039/501100008530
    Schlagwort(e): ddc:577.63
    Sprache: Englisch
    Materialart: doc-type:article
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