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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (104 Seiten = 4 MB) , Diagramme
    Edition: 2021
    Language: German
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  • 2
    Type of Medium: Online Resource
    Pages: Online-Ressource (94 Seiten, 7 MB) , Diagramme
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 141
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 416 (2002), S. 168-171 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The oceanic carbon cycle is mainly determined by the combined activities of bacteria and phytoplankton, but the interdependence of climate, the carbon cycle and the microbes is not well understood. To elucidate this interdependence, we performed high-frequency sampling of sea water along a ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2022-06-03
    Description: Between 28 August and 5 September 1982 thirty water samples (5 m depth) were taken on a transect between the Bothnian Bay and the Kiel Bight. Despite substantially differing hydrographical situations within the different subregions of the Baltic Sea, the total bacterial numbers showed a remarkable regional uniformity. Bacterial numbers fluctuated between 3 and 4 x 106 cells ml-1. A distinct pattern was observed: mean bacterial cell volumes were high in the Bothnian Bay (0.145 µm3) and low in the Gotland- and Bornholm Sea (0.094 and 0.091 µm3, respectively). The bacterial biomass fell in the range of 184 - 117 µg C 1-1. The activity parameters were somewhat more variable than bacterial numbers and biomass.
    Type: Article , NonPeerReviewed
    Format: text
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  • 5
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    Wiley
    In:  Internationale Revue der gesamten Hydrobiologie und Hydrographie, 79 (4). pp. 605-619.
    Publication Date: 2018-06-19
    Description: Studies on the Mediterranean Undercurrent in the Gulf of Cádiz showed that bacterial abundance and biomass as well as heterotrophic activity were higher in the water of Mediterranean origin in 500–800 m depth than in the adjacent Atlantic water. Upwelling processes off Mauretania and Portugal were accompanied by high bacterial numbers (bacterial plate counts) in the mixed surface layer. Changes in the qualitative composition of the bacterial flora in the waters off West Africa and in the Arabian Gulf were explained by the introduction of dust from desert regions into the sea by aeolian transport. In the Western Baltic migration of fish was detected by the presence of special bacteria, which normally live on or in these animals. Regions with complex hydrographic structures such as the Western and Central Baltic Sea revealed interesting relationships between bacteriological abundance and activity on the one hand and characteristic physical and chemical properties, such as origin, salinity and O2/H2S‐content, on the other. The importance of bacteriological variables for the characterization of different water bodies is discussed.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2013-07-17
    Description: Phytoplankton and bacteria are sensitive indicators of environmental change. The temporal development of these key organisms was monitored from 1988 to the end of 2007 at the time series station Boknis Eck in the western Baltic Sea. This period was characterized by the adaption of the Baltic Sea ecosystem to changes in the environmental conditions caused by the conversion of the political system in the southern and eastern border states, accompanied by the general effects of global climate change. Measured variables were chlorophyll, primary production, bacteria number, -biomass and -production, glucose turnover rate, macro-nutrients, pH, temperature and salinity. Negative trends with time were recorded for chlorophyll, bacteria number, bacterial biomass and bacterial production, nitrate, ammonia, phosphate, silicate, oxygen and salinity while temperature, pH, and the ratio between bacteria numbers and chlorophyll increased. Strongest reductions with time occurred for the annual maximum values, e.g. for chlorophyll during the spring bloom or for nitrate during winter, while the annual minimum values remained more stable. In deep water above sediment the negative trends of oxygen, nitrate, phosphate and bacterial variables as well as the positive trend of temperature were similar to those in the surface while the trends of salinity, ammonia and silicate were opposite to those in the surface. Decreasing oxygen, even in the surface layer, was of particular interest because it suggested enhanced recycling of nutrients from the deep hypoxic zones to the surface by vertical mixing. The long-term seasonal patterns of all variables correlated positively with temperature, except chlorophyll and salinity. Salinity correlated negatively with all bacterial variables (as well as precipitation) and positively with chlorophyll. Surprisingly, bacterial variables did not correlate with chlorophyll, which may be inherent with the time lag between the peaks of phytoplankton and bacteria during spring. Compared to the 20-yr averages of the environmental and microbial variables, the strongest negative deviations of corresponding annual averages were measured about ten years after political change for nitrate and bacterial secondary production (~ −60%), followed by chlorophyll (−50%) and bacterial biomass (−40%). Considering the circulation of surface currents in the Baltic Sea we interpret the observed patterns of the microbial variables at the Boknis Eck time series station as a consequence of the improved management of water resources after 1989 and – to a minor extent – the trends of the climate variables salinity and temperature.
    Type: Article , PeerReviewed
    Format: text
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  • 7
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    Bundesanstalt für Gewässerkunde
    In:  Hydrologie und Wasserbewirtschaftung, 55 (4). pp. 188-198.
    Publication Date: 2019-09-24
    Description: An vier Tidenzyklus-Stationen von 21 bis 36 Std. Dauer wurde auf einem Längsschnitt von Hamburg bis zur Außenelbe untersucht, welchen Anteil die Bakterien am Abbau der organischen Substanz haben. Der Gesamt-Abbau durch die planktische Organismengemeinschaft wurde aus dem Sauerstoffverbrauch mit einem angenommenen Respirationsquotienten von 0,85 bestimmt. Der bakterielle Abbau wurde über die Biomasse-Produktion und die Wachstums-Effizienz der Bakterien ermittelt. Die Tidenzyklus-Stationen mit einer hohen zeitlichen Auflösung zeigten eine große Variabilität der Abbauprozesse während der Gezeiten. Die Mittelwerte ergaben, dass der Gesamt-Abbau im oberen noch limnischen Bereich 10,2 μg C l-1 h-1 betrug mit einem bakteriellen Anteil von 82%. Flussabwärts ging der Gesamt-Abbau auf 2,7 μg C l-1 h-1 zurück und der bakterielle Anteil belief sich auf rd. 50 %. Der Längsschnitt von Hamburg bis Neuwerk mit einer hohen räumlichen Auflösung zeigte eine grundsätzlich ähnliche regionale Verteilung. Der hohe Anteil des bakteriellen Abbaus in dem oberen limnischen Ästuarbereich geht darauf zurück, dass das hier aus dem Mittellauf der Elbe eingeschwemmte Phytoplankton infolge Lichtmangels größtenteils abstirbt. Die Ursachen liegen in der großen Wassertiefe des Hamburger Hafengebietes und der starken Gezeitendurchmischung der Wassersäule. Dadurch vermindert sich die Respiration des Phytoplanktons und die Abbautätigkeit ist daher im Wesentlichen auf die Bakterien und das Zooplankton beschränkt. Von diesen beiden verbleibenden Hauptkomponenten des Flussplanktons spielen die Bakterien die wichtigere Rolle beim Abbau der organischen Substanz im Elbe-Ästuar.
    Type: Article , PeerReviewed
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  • 8
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    In:  [Poster] In: 4. International conference Enzymes in the Environment: Activity, Ecology and Application, 17.-21.07.2011, Bad Nauheim, Germany .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
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    Bundesanstalt für Gewässerkunde
    In:  Hydrologie und Wasserbewirtschaftung, 54 (1). pp. 18-28.
    Publication Date: 2019-09-23
    Description: Der Nord-Ostsee-Kanal ist ein Brackwasserbiotop, der sich durch einen relativ hohen Salzgehalt in seinem östlichen Teil, einem fast ausgesüßten mittleren Bereich und einem leichten Salzgehaltsanstieg auf den letzten westlichen Kilometern auszeichnet. In seiner westlichen Hälfte ist die Wassertrübung deutlich höher als in der östlichen. Die Bakterienzahl lag nahe der Schleuse Kiel-Holtenau zwischen 3,6 und 7,9 x 10 hoch 9 l hoch -1 Zellen, von denen 0 bis 9,5 % an Partikeln angeheftet waren. In Richtung Westen nahmen die Bakterienzahl und der Prozentsatz der partikelgebundenen Bakterien fast linear zu und erreichten in der Nähe der Schleuse Brunsbüttel mit 11,5 bis 18,0 x 10 hoch 9 l hoch -1 Zellen und 80-94 % partikelgebundenen Bakterien ihre Maxima. Trübungsgehalt, Bakterienzahl und Prozentsatz der partikelgebundenen Bakterien waren hoch signifikant miteinander korreliert. Die Mittelwerte der bakteriellen Aktivität (gemessen als Leucin-Inkorporation), die zwischen 45 pmol l hoch -1 h hoch -1 im Januar und 383 pmol l hoch -1 h hoch -1 im Juli lagen, zeigten den großen Einfluss der sommerlichen Temperaturzunahme. Die maximalen Werte der spezifischen Leucin-Inkorporation erreichten rd. 80 pmol h hoch -1 10 hoch -9 Bakterien. Die Umsatzraten von Acetat, das als Repräsentant für die niedermolekularen gelösten organischen Verbindungen verwendet wurde, beliefen sich auf Werte zwischen 7 und 34,1 % h-1 (Mittelwerte über den gesamten NOK). Die Erneuerungszeit für den Acetat-"Pool" lag demnach zwischen rund 14 h (Januar) und 3 h (April).
    Type: Article , PeerReviewed
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  • 10
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    In:  [Invited talk] In: UNSPECIFIED, 13.04, AnSan, Korea .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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