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  • 1990-1994  (28)
  • 1965-1969  (25)
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  • 21
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (99 Seiten = 12 MB) , Graphen, Karten
    Language: German
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  • 22
    Electronic Resource
    Electronic Resource
    Springer
    Helgoland marine research 15 (1967), S. 589-601 
    ISSN: 1438-3888
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Description / Table of Contents: Zusammenfassung 1. Viele Tintinnenarten sind kosmopolitisch verbreitet. Gebiete des Weltmeeres mit ähnlichen Lebensbedingungen beherbergen gleiche Tintinnen. Sie leben in der lichtdurchfluteten Zone des Meeres, wo das Angebot an Nahrung am größten ist. Tägliche vertikale Wanderungen wurden nachgewiesen. 2. Die jahreszeitliche Verbreitung richtet sich nach der geographischen Breite. Bei der ozeanischen Wetterschiffstation India liegt das Maximum mit 4 000 000 Exemplaren unter 1 m2 im Mai bis Juli; das entspricht einer Biomasse von etwa 300 mm3. 3. Der begrenzende Faktor für die Entwicklung und Verbreitung von Tintinnen ist vor allem die Wassertemperatur. Der Einfluß von Salzgehalt und Sauerstoffsättigung ist offensichtlich weniger bedeutsam. 4. Die Nahrung der Tintinnen besteht aus Detritus, Bakterien, nackten Flagellaten, Coccolithophoriden, Peridineen, Diatomeen und Silicoflagellaten. Die Tintinnen selbst werden von Euphausiaceen, Copepoden, Tunicaten und Fischlarven gefressen. 5. Tintinnen bilden eines der ersten Glieder in der Nahrungskette. Man sollte in Zukunft dieser interessanten Giliatengruppe bei produktionsbiologischen Untersuchungen mehr Beachtung schenken.
    Notes: Abstract Tintinnids are shell building Protozoa regarded as heterotrich ciliates. Most of them are marine; less than 2% of the 800 known species occur in fresh water. Tintinnids live almost exclusively free-swimming pelagic and occur at all latitudes, in all seas, predominantly in the upper illuminated water layers. Their geographical distribution is primarily controlled by temperature and so is their development; salinity and oxygen seem of little importance. Tintinnids are one of the first links in the food chain. They feed on detritus, bacteria, naked flagellates, coccolithophores, peridineans and diatoms. The tintinnids themselves are eaten by copepods, euphausiids, tunicates and fish larvae.
    Type of Medium: Electronic Resource
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  • 23
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    Elsevier
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 40 (1-2). pp. 495-519.
    Publication Date: 2018-03-05
    Description: Productivity regime and phytoplankton size structure are described for two different epipelagic systems in the tropical/subtropical Northeast Atlantic Ocean investigated during 9–11 day drift studies in spring 1989 in the JGOFS North Atlantic Bloom Experiment, 18°N, 30°W and 33°N, 20°W. At the 18°N study site, an oligotrophic system was encountered. The water column above the main pycnocline at about 50–60 m depth was nutrient-depleted, and both chlorophyll and primary production displayed subsurface maxima at the nutricline. Picoplankton was the dominant size fraction, accounting for 78–90% of chlorophyll and 83–98% of primary production. Synechococcus-type coccoid cyanobacteria were the dominant picoplankters. The hydrographic situation was characterized by high small-scale variability; the most interesting feature was the intrusion of nutrient-depleted Subtropical Salinity Maximum Water into the euphotic zone, whose impacts on the productivity regime are discussed. At 33°N study site, a post-bloom situation was encountered. Although the euphotic zone was nutrient-depleted, higher amounts of larger phytoplankton were present, the contribution of picoplankton being 42–53% of chlorophyll and 42–86% of primary production. Over the course of the drift study, subsurface maxima of chlorophyll and productivity evolved, the contribution of picoplankton having increased. Picocyanobacteria again were the dominant picoplankters. At both study sites the profiles of abundance ratios of picocyanobacteria to picoeucaryotes cell numbers proved to be a useful tool to characterize water masses.
    Type: Article , PeerReviewed
    Format: text
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  • 24
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    Elsevier
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 40 (3). pp. 711-735.
    Publication Date: 2018-03-05
    Description: The productivity regime and size structure of phytoplankton are described for three different epipelagic systems in the Arabian Sea during the inter-monsoon period in spring 1987: (1) the coast of Oman; (2) the central Arabian Sea; and (3) the shelf off Pakistan. These results are related to the functioning of the specific ecosystem. Off the coast of Oman, the transition from a surface maximum of autotrophic biomass and production to a more oligotrophic system, with a chlorophyll subsurface maximum, was observed. Concomitantly, the size spectrum changed towards a higher significance of picoplankton. In the central Arabian Sea, a typical oligotrophic system with a pronounced subsurface maximum of autotrophic biomass and primary production was encountered. Here, the epipelagic system could be divided into two distinct sub-systems: the surface layer “regenerated” production, the predominance of picophytoplankton and minor losses due to sedimentation, thus a “closed” system; and the subsurface maximum layer at the nutricline characterized by higher sedimentation losses and more diatoms. Both sub-systems showed about the same productivity, the turnover in the surface layer having been much greater than in the subsurface maximum. The system on the shelf off Pakistan is seen as a decay stage of the open ocean system when water from offshore is transported onto the shelf during the onset of monsoon winds.
    Type: Article , PeerReviewed
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  • 25
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    Pergamon Press
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 40 (1-2). pp. 537-557.
    Publication Date: 2020-08-05
    Description: During leg 1 of Meteor cruise 10 in March/April 1989 at 18 circ N, 30 circ W, the high spatial and temporal resolution of hydrographic CTD-stations indicated that the study site was in a hydrographically complex region in the transition zone between the Canary Current and the North Equatorial Current at the southern boundary of the subtropical gyre. Strong variability was found within the upper 120 m due to interleavings of warmer and saltier subtropical salinity maximum water with colder and less saline upper thermocline water. The interleavings caused unexpected nose-like temperature, salinity, nitrate and oxygen profiles yet not described in the literature. A second variability source was found in the Central Water area, because the study area was situated in the vicinity of the Central Water Boundary dividing North and South Atlantic Central Water. Hydrographic analysis of the study shows that interpretations of biological and chemical data can only be done in conjunction with high resolution CTD-profiling
    Type: Article , PeerReviewed
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  • 26
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    Elsevier
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 40 (1-2). pp. 521-536.
    Publication Date: 2019-01-21
    Description: During a R.V. Meteor JGOFS-NABE cruise to a tropical site in the northeast Atlantic in spring 1989, three different vertical regimes with respect to nitrate distribution and availability within the euphotic zone were observed. Besides dramatic variations in the depth of the nitracline, a previously undescribed nose-like nitrate maximum within the euphotic zone was the most prominent feature during this study. Both the vertical structure of phytoplankton biomass and the degree of absolute and relative new production were related to the depth of the nitracline, which in turn was dependent on the occurrence/non-occurrence of the subsurface subtropical salinity maximum (S(max)). The mesoscale variability of the nitracline depth, as indicated from a pre-survey grid, and published data on the frequent occurrence of the S(max) in tropical waters suggest higher variability of new production and F-ratio than usually expected for oligotrophic oceans. The importance of salt fingering and double diffusion for nitrate transport into the euphotic zone is discussed.
    Type: Article , PeerReviewed
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  • 27
    Publication Date: 2022-04-22
    Description: Im August 1966 wurden zwischen Cuxhaven und Edinburgh 39 Oberflachenproben in 10 sm Abstand und 17 Tiefenproben auf 5 Vertikalstationen entnommen. Es wurden die Verteilung von Temperatur, Salzgehalt, Trübung, Gelbstoff-, Chlorophyll a- und Eiweißgehalt und die Artenzusammensetzung des größeren Phytoplanktons untersucht. Folgende Wassermassen wurden beobachtet: 1. Das Wasser der Deutschen Bucht mit hohen Werten für die Trübung, den Gelbstoff-, Chlorophyll- und Eiweißgehalt. Das Phytoplankton ist durch den Reichtum an Diatomeen mit der vorherrschenden Art Rhizosolenia imbricata var. shrubsolei gekennzeichnet. 2. Das salzreiche Doggerbankwasser atlantischer Herkunft, das sehr niedrige Werte für die untersuchten biologischen Faktoren aufweist. Neben den Diatomeen werden Dinoflagellaten häufig. 3. Das Britannische Ostktüstenwasser mit einem leicht erhöhten Gelbstoffgehalt aber sonst ebenfalls sehr niedrigen Werten für Trübung, Chlorophyll a und Eiweiß. Die Kieselalgen sind von Peridineen abgelöst worden. Die Leitform ist Ceratium furca. Der Küsteneinfluß ist an der schottischen Küste sehr viel geringer als in der Deutschen Bucht. Die niedrigen Chlorophyll- und Eiweißwerte in der offenen Nordsee kennzeichnen das sommerliche Minimum in der Planktonentwicklung.
    Type: Article , NonPeerReviewed
    Format: text
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  • 28
    Publication Date: 2022-04-19
    Type: Article , NonPeerReviewed
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  • 29
    Publication Date: 2022-04-26
    Description: Anhand von zwei käuflichen Präparaten wird die Extinktion von Chlorophyll a in verschiedenen Lösungsmitteln untersucht und daraus der Extinktionskoeffizient für frisch extrahiertes, ungetrocknetes Chlorophyll a in Methanol abgeleitet. Er beträgt für das rote Extinktionsmaximum bei 665 nm 75.0 l/g cm. Die Extinktionskoeffizienten von getrocknetem Chlorophyll a sind in den untersuchten Lösungsmitteln 10-25% niedriger als die von einer frisch extrahierten Chlorophyllösung (Tabelle 2). Die Messung des Chlorophyll a-Gehaltes kann mit hinreichender Genauigkeit in einem Filterphotometer (ELKO II, Zeiss) ausgeführt werden. Hierzu werden Eichkurven für drei verschiedene Interferenzfilter angegeben. From two purchasable preparations of crystalline chlorophyll a, the extinction coefficient of undried chlorophyll a in methanol has been calculated as 75.0 l/g cm at the maximum of extinction at 665 nm. The extinction coefficients of dried chlorophyll a in the different solvents tested are 10-25% lower than those of undried chlorophyll a (table 2). Chlorophyll a can be measured in a filter photometer (ELKO II, Zeiss) with sufficient precision. Standard curves for three different interference filters are given.
    Type: Article , NonPeerReviewed
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  • 30
    Publication Date: 2022-04-25
    Description: Es wird ein Geräit beschrieben, mit dem man sechs 5-Liter-Wasserproben aus beliebigen Wassertiefen entnehmen kann. Die Schöpfer werden elektromagnetisch geschlossen. Durch Zusatzgeräte lassen sich verschiedene Parameter kontinuierlich registrieren (z. B. t° C, S ‰, Tiefe, Oberlicht, Lichtextinktion). Dies ermöglicht je nach Fragestellung eine gezielte Probennahme. An apparatus is described which makes it possible to obtain six 5-liter walersamples from arbitrary depths. The waterbottles are closed electromagnetically. By means of accessory apparatus various parameters can be registered continuously (e.g. t°, S ‰, depth, downward light, lightextinction). This will make it possible to take samples at representative depths, which are most relevant to the problem under investigation.
    Type: Article , NonPeerReviewed
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