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  • PANGAEA  (145)
  • Kiel : Inst. für Meereskunde, Abt. Marine Planktologie  (3)
  • Kiel : IFM  (2)
  • Oxford Univ. Press  (2)
Document type
Keywords
Language
  • 1
    Type of Medium: Book
    Pages: 105 S , graph. Darst , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 140
    Language: English
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  • 2
    Type of Medium: Book
    Pages: 200 S , Kt
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 180
    Language: English
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  • 3
    Type of Medium: Book
    Pages: 108 S , graph. Darst.
    Language: Undetermined
    Note: Enth.: Prophylaxe und Therapie von Fischkrankheiten in arinen Intensivkulturen (Abschlußbericht) ; Transformation von Nährstoffen bei Fischen unter unterschiedlichen physiologischen Ausgangszuständen (2. Statusbericht)
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  • 4
    Book
    Book
    Kiel : Inst. für Meereskunde, Abt. Marine Planktologie
    Type of Medium: Book
    Pages: 167 S. , graph. Darst., Kt. , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 205
    Language: German
    Note: Literaturverz. S. 151 - 167
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  • 5
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 54 Blatt , Illustrationen, Diagramme
    Edition: Online-Ausgabe 2020 1 Online-Ressource (58 Seiten = 2,5 MB)
    Language: German
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  • 6
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    Unknown
    Oxford Univ. Press
    In:  Journal of Plankton Research, 26 (3). pp. 357-369.
    Publication Date: 2019-09-23
    Description: The so-called ‘turbulence incubator’ overcomes an essential disadvantage of static in situ incubations where at high irradiances an artificial photoinhibition is caused by neglecting turbulent mixing in the upper water column. It is operated on deck and simulates the changing light conditions for vertically mixed phytoplankton cells by moving the sample bottles horizontally through a circular water bath covered by a glass lid of neutral optical density filters. In this way the exponentially decreasing irradiance within the euphotic zone is simulated and photoinhibition near the surface is avoided. A crucial point is the choice of revolution rate for simulating turbulent mixing under natural conditions. The incubator is characterized by its handy size, a relatively simple and inexpensive construction and a battery-driven motor. It can thus even be operated on small vessels without an electric generator. The incubator is especially suited for vertically mixed waters such as shallow bays, tidal estuaries and rivers. Its reliability was successfully tested by a simultaneous comparison with in situ measurements at various stations representing different water types and environmental conditions, ranging from the turbid River Elbe to the clear open Baltic Sea. In 9 out of 11 experiments, higher primary production rates were obtained in the turbulence incubator than in static in situ incubations. The majority of the latter were characterized by a pronounced photoinhibition in the upper two incubation depths representing the 100 and 50% light levels. The average rate increase amounted to 22%, with a range between 11 and 53% depending on light attenuation and irradiance.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2018-05-30
    Description: In an assessment of non-indigenous species transported by international ship traffic to German waters, commissioned by the German Federal Environmental Agency, the survival of tropical plankton organisms in ballast water was studied by accompanying a container vessel on its 23-day voyage from Singapore to Bremerhaven in Germany. Two tanks, one filled off Singapore and the other off Colombo, Sri Lanka, were monitored for their phyto- and zooplankton content by daily sampling. As already reported in previous studies, species abundance and diversity, especially of zooplankton, decreased sharply during the first days, and only a few specimens survived the whole cruise. The contents of the Colombo tank, however, changed dramatically during the last week. The harpacticoid copepod, Tisbe graciloides, increased its abundance by a factor of 100 from 0.1 to 10ind. l–1 within a few days. This is the first time that a ballast water organism has been found to multiply at such a high rate. Opportunistic species such as Tisbe are apparently able to thrive and propagate in ballast water tanks under certain conditions. Ballast water tanks may thus serve as incubators for certain species depending on their characteristics.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Krey, Johannes; Bole, R; Gillbricht, Max; Lenz, Jürgen (1971): Planktologisch-chemische Daten der "Meteor"- Expedition in den Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D9, 1-120
    Publication Date: 2024-07-19
    Description: The present volume contains the planktological data collected during the expedition of the "Meteor" to the Indian Ocean in 1964/65. It was the main objective of the expedition to study the up- and downwelling conditioned along the western and eastern coasts of the Arabian Sea by the northeastern monsoon. It is from these areas that the greater part of the data here presented was obtained. A few values from the Red Sea have been added. As the title „Planktological-Chemical Data" implies, it was chiefly with the help of chemical methods that the planktological investigations, with the exception of the particle size analysis and phytoplankton counting conducted optically, were carried out. These investigations were above all devoted to a quantitative survey of particulate matter and plankton, the latter being sampled by water-bottle and net. The zooplankton hauls were taken with the Indian Ocean Standard Net according to the international guidelines laid down for the expedition. As a rule, double catches were made at every station, one sample being intended for laboratory analysis at the Indian Ocean Biological Centre in Ernakulam, South India, and the other for the Institut für Meereskunde in Kiel. In addition to determining the standing stock, the production rate of phytoplankton was measured by the 14C method. These experiments were mainly conducted during the latter half of the expedition. The planktological studies primarily covered the euphotic zone, extending into the underlying water layers up to a depth of 600 m. The investigations were above all directed towards ascertaining the quantity of organic substance, formed by primary production, in its relation to environmental conditions and determining whether or not organic substance is actively transported from the surface into the deeper layers by the periodically migration organisms of the deep scattering layers. Depending on the station time available, a few samples could now and then be taken from deeper layers. The present volume of planktological-chemical data addresses itself to all those concerned processing the extensive material collected during the International Indian Ocean Expedition. As a readily accessible work of reference, it hopes to serve as an aid in the evaluation and interpretation of the expedition results. The complementary ecological data such as temperature, salinity, and oxygen content as well as the figures obtained on abundance and distribution in depth of the nutrients essential for primary production may be found in the volume of physical-chemical data published in Series A of the "Meteor“-Forschungsergebnisse No. 2, 1966 (Dietrich et al., 1966).
    Keywords: Arabian Sea; CTD/Rosette; CTD-RO; Eastern Arabian Sea; Golf of Aden, Arabian Sea; Gulf of Aden; IIOE - International Indian Ocean Expedition; Indian Ocean; Indian Ocean Standard Net; IOSN; M1; M1_042; M1_043; M1_045; M1_053; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_213; M1_215; M1_217; M1_218; M1_219; M1_220; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD053; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD213; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD220; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_NET090; M1_NET092; M1_NET094; M1_NET099; M1_NET101; M1_NET111; M1_NET112; M1_NET113; M1_NET114; M1_NET124; M1_NET128; M1_NET132; M1_NET133; M1_NET134; M1_NET135; M1_NET136; M1_NET144; M1_NET146; M1_NET149; M1_NET151; M1_NET152; M1_NET153; M1_NET154; M1_NET157; M1_NET164; M1_NET165; M1_NET166; M1_NET167; M1_NET168; M1_NET169; M1_NET170; M1_NET171; M1_NET172; M1_NET173; M1_NET174; M1_NET175; M1_NET176; M1_NET177; M1_NET178; M1_NET179; M1_NET180; M1_NET181; M1_NET182; M1_NET183; M1_NET186; M1_NET187; M1_NET188; M1_NET189; M1_NET195; M1_NET196; M1_NET198; M1_NET199; M1_NET200; M1_NET201; M1_NET202; M1_NET206; M1_NET207; M1_NET208; M1_NET209; M1_NET210; M1_NET218; M1_NET219; M1_NET220; M1_NET222; M1_NET223; M1_NET224; M1_NET226; M1_NET227; M1_NET232; M1_NET233; M1_NET234; M1_NET235; M1_NET236; M1_NET237; M1_NET238; Meteor (1964); Western Arabian Sea
    Type: dataset publication series
    Format: application/zip, 135 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Bauerfeind, Eduard; Boje, Rolf; Fahrbach, Eberhard; Lenz, Jürgen (1983): Planktological and chemica data from the equatorial Atlantic at 22°W obtained in February to June 1979 ("FGGE-Equator '79"). Berichte aus dem Institut für Meereskunde an der Christian-Albrechts Universität Kiel, 110, 157 pp, hdl:10013/epic.37779.d001
    Publication Date: 2024-08-15
    Description: The volume presents planktological and chemical data collected during cruise No. 51 of RV "Meteor" to the equatorial Atlantic (FGGE '79) from February to June 1979. A standard section along the meridian 22° W across the equator was sampled ten times between 2° S and 3° N. Together with a temperature and salinity profile, concentrations of oxygen, nutrients and chlorophyll a were analyzed in water samples down to a depth of 250 m. Solar radiation and light depths were measured for determination of primary productivity of the euphotic zone according to the simulated in situ method. Zooplankton biomass was estimated in 5 depth intervals down to 300 m by means of a multiple opening and closing net equipped with a mesh size of 100 µm.
    Keywords: Atlantic Ocean; CTD/Rosette; CTD-RO; Equatorial Atlantic; Expendable bathythermograph; FGGE-Equator 79 - First GARP Global Experiment; M51; M51_010-1; M51_011-1; M51_013-1; M51_015-1; M51_017-1; M51_018-1; M51_020-1; M51_022-1; M51_024-1; M51_027-1; M51_029-1; M51_031-1; M51_033-1; M51_035-1; M51_036-1; M51_038-1; M51_039-1; M51_041-1; M51_043-1; M51_043-2; M51_045-1; M51_047-1; M51_049-1; M51_049-2; M51_051-1; M51_053-1; M51_055-1; M51_058-1; M51_060-1; M51_062-1; M51_064-1; M51_066-1; M51_071-1; M51_073-1; M51_075-1; M51_076-1; M51_077-1; M51_078-1; M51_079-1; M51_080-1; M51_081-1; M51_082-1; M51_083-1; M51_090-1; M51_092-1; M51_094-1; M51_096-1; M51_098-1; M51_100-1; M51_102-2; M51_104-1; M51_106-1; M51_108-2; M51_110-1; M51_112-1; M51_114-1; M51_116-1; M51_117-2; M51_122-1; M51_124-1; M51_126-2; M51_128-1; M51_130-1; M51_132-1; M51_134-1; M51_134-2; M51_136-1; M51_137-1; M51_139-1; M51_141-1; M51_143-1; M51_143-2; M51_145-1; M51_147-1; M51_149-1; M51_151-2; M51_152-2; M51_153-2; M51_160-1; M51_161-1; M51_163-1; M51_165-1; M51_167-1; M51_169-1; M51_171-1; M51_173-1; M51_175-1; M51_177-1; M51_179-1; M51_181-2; M51_183-1; M51_185-1; M51_197-1; M51_197-10; M51_197-11; M51_197-12; M51_197-2; M51_197-3; M51_197-4; M51_197-5; M51_197-6; M51_197-7; M51_197-8; M51_197-9; M51_199-1; M51_199-10; M51_199-11; M51_199-12; M51_199-13; M51_199-14; M51_199-15; M51_199-2; M51_199-3; M51_199-4; M51_199-5; M51_199-6; M51_199-7; M51_199-8; M51_199-9; M51_201-1; M51_202-1; M51_203-1; M51_205-1; M51_207-1; M51_209-1; M51_211-1; M51_212-2; M51_213-2; M51_215-2; M51_217-2; M51_219-1; M51_221-2; M51_223-1; M51_225-1; M51_227-1; M51_227-10; M51_227-2; M51_227-3; M51_227-4; M51_227-5; M51_227-6; M51_227-7; M51_227-8; M51_227-9; M51_231-2; M51_232-1; M51_234-1; M51_236-2; M51_238-2; M51_240-1; M51_242-2; M51_244-1; M51_246-1; M51_247-2; M51_248-1; M51_250-1; M51_252-1; M51_254-1; M51_255-2; M51_256-1; M51_258-1; M51_261-2; M51_263-1; M51_265-1; M51_267-2; M51_269-1; M51_271-1; M51_273-2; M51_275-1; M51_277-1; M51_279-1; M51_280-1; M51_281-1; M51_283-1; M51_285-1; M51_286-1; M51_286-4; M51_291-1; M51_292-2; M51_294-2; M51_296-1; M51_298-1; M51_300-1; M51_301-2; M51_302-1; M51_304-1; M51_306-1; M51_308-1; M51_309-2; M51_310-1; M51_312-1; M51_314-1; M51_316-1; M51_317-1; M51_320-1; M51_321-1; M51_323-2; M51_325-1; M51_327-1; M51_329-2; M51_329-4; M51_331-1; M51_333-2; M51_335-1; M51_336-1; M51_337-1; M51_339-1; M51_341-1; M51_343-1; M51_344-2; M51_345-1; Meteor (1964); MOC; MOCNESS opening/closing plankton net; MSN; Multiple opening/closing net; North Atlantic Ocean; South Atlantic Ocean; Water sample; WS; XBT
    Type: dataset publication series
    Format: application/zip, 2 datasets
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  • 10
    Publication Date: 2024-07-22
    Keywords: Calculated; Carbon, organic, total per volume; Carbon, total, particulate; Colorometric analysis, manual; CTD/Rosette; CTD-RO; DEPTH, water; IFM-GEOMAR; IIOE - International Indian Ocean Expedition; Inverted microscopy; Leibniz-Institut für Meereswissenschaften, Kiel; Lithology/composition/facies; M1; M1_111; M1_CTD111; Meteor (1964); Oxidation (alkaline) with borate buffered potassium persulphate; Particle concentration; Particle total surface; Particle volume; Phytoplankton; Phytoplankton, biomass as carbon; Proteins; Seston, dry mass; Weighted; Western Arabian Sea
    Type: dataset
    Format: text/tab-separated-values, 187 data points
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