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  • 2020-2024  (6)
  • 1980-1984  (14)
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Year
  • 1
    Online Resource
    Online Resource
    Untersuchungen zur Primärproduktion und Ökologie des Phytoplanktons im zentralen äquatorialen Atlantik : Ergebnisse der Meteor-Expedition "FGGE-Äquator 79" (1983)
    Kiel
    Details Availability
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (165 Seiten = 28 MB) , Diagramme, Illustrationen
    URL: https://oceanrep.geomar.de/42046/
    Language: German
    Location Call Number Limitation Availability
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    GEOMAR CATALOGUE
    Link to Library Catalog
    get availability status
  • 2
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    Unknown
    Effects of Atlantification and changing sea‐ice dynamics on zooplankton community structure and carbon flux between 2000 and 2016 in the eastern Fram Strait (2022)
    John Wiley & Sons, Inc. | Hoboken, USA
    Details
    Publication Date: 2023-12-14
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉The collection of zooplankton swimmers and sinkers in time‐series sediment traps provides unique insight into year‐round and interannual trends in zooplankton population dynamics. These samples are particularly valuable in remote and difficult to access areas such as the Arctic Ocean, where samples from the ice‐covered season are rare. In the present study, we investigated zooplankton composition based on swimmers and sinkers collected by sediment traps at water depths of 180–280, 800–1320, and 2320–2550 m, over a period of 16 yr (2000–2016) at the Long‐Term Ecological Research observatory HAUSGARTEN located in the eastern Fram Strait (79°N, 4°E). The time‐series data showed seasonal and interannual trends within the dominant zooplankton groups including copepoda, foraminifera, ostracoda, amphipoda, pteropoda, and chaetognatha. Amphipoda and copepoda dominated the abundance of swimmers while pteropoda and foraminifera were the most important sinkers. Although the seasonal occurrence of these groups was relatively consistent between years, there were notable interannual variations in abundance, suggesting the influence of various environmental conditions such as sea‐ice dynamic and lateral advection of water masses, for example, meltwater and Atlantic water. Statistical analyses revealed a correlation between the Arctic dipole climatic index and sea‐ice dynamics (i.e., ice coverage and concentration), as well as the importance of the distance from the ice edge on swimmer composition patterns and carbon export.〈/p〉
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Federal Ministry of Education and Research (BMBF)
    Description: Helmholtz‐Gemeinschaft
    Keywords: ddc:577.7 ; eastern Fram Strait ; sea ice dynamics ; zooplankton population dynamics
    Language: English
    Type: doc-type:article
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    CITATION GEO-LEO
  • 3
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    Unknown
    Untersuchungen zur Primärproduktion und Ökologie des Phytoplanktons im zentralen äquatorialen Atlantik : Ergebnisse der Meteor-Expedition "FGGE-Äquator 79" (1983)
    In:  (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 141 pp
    Details
    Publication Date: 2018-02-28
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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    OceanRep: Thesis - not published by a publisher
  • 4
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    Unknown
    Planktological and chemical data from the equatorial Atlantic at 22o W obtained in February to June 1979 : ("FGGE - equator '79") (1983)
    Institut für Meereskunde
    Details
    Publication Date: 2023-09-19
    Type: Report , NonPeerReviewed
    Format: text
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    OceanRep: Report - other report
  • 5
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    Unknown
    Effects of Atlantification and changing sea‐ice dynamics on zooplankton community structure and carbon flux between 2000 and 2016 in the eastern Fram Strait (2023)
    Wiley
    Details
    Publication Date: 2024-02-07
    Description: The collection of zooplankton swimmers and sinkers in time-series sediment traps provides unique insight into year-round and interannual trends in zooplankton population dynamics. These samples are particularly valuable in remote and difficult to access areas such as the Arctic Ocean, where samples from the ice-covered season are rare. In the present study, we investigated zooplankton composition based on swimmers and sinkers collected by sediment traps at water depths of 180–280, 800–1320, and 2320–2550 m, over a period of 16 yr (2000–2016) at the Long-Term Ecological Research observatory HAUSGARTEN located in the eastern Fram Strait (79°N, 4°E). The time-series data showed seasonal and interannual trends within the dominant zooplankton groups including copepoda, foraminifera, ostracoda, amphipoda, pteropoda, and chaetognatha. Amphipoda and copepoda dominated the abundance of swimmers while pteropoda and foraminifera were the most important sinkers. Although the seasonal occurrence of these groups was relatively consistent between years, there were notable interannual variations in abundance, suggesting the influence of various environmental conditions such as sea-ice dynamic and lateral advection of water masses, for example, meltwater and Atlantic water. Statistical analyses revealed a correlation between the Arctic dipole climatic index and sea-ice dynamics (i.e., ice coverage and concentration), as well as the importance of the distance from the ice edge on swimmer composition patterns and carbon export.
    Type: Article , PeerReviewed
    Format: text
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 6
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    Carbon, silicon, carbonate, seston, and biogenic and lithogenic export fluxes from sediment traps deployed in the Eurasian Arctic Ocean (2020)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: AWI_BioOce; Biogenic, flux; Biological Oceanography @ AWI; Calcium carbonate, flux; Carbon, organic, particulate, flux; DATE/TIME; DEPTH, water; Duration, number of days; Elevation of event; Event label; FRAM; FRontiers in Arctic marine Monitoring; Gakkel_A1-1; Gakkel_N1-1; Latitude of event; Lithogenic, flux; Longitude of event; MOOR; Mooring; PS78/255-1; PS78/262-3; Seston, flux; Silicon, dissolved + particulate, flux
    Type: Dataset
    Format: text/tab-separated-values, 518 data points
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    DATA PANGAEA
  • 7
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    Biomarker fluxes from sediment traps deployed in the Eurasian Arctic Ocean (2020)
    PANGAEA
    Details
    Publication Date: 2023-11-30
    Keywords: 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane, flux; 24-Methylcholest-5-en-3beta-ol and 24-Ethylcholest-5-en-3beta-ol, flux; 24-Methylcholesta-5,22E-dien-3beta-ol, flux; AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Duration; Duration, number of days; Elevation of event; Event label; FRAM; FRontiers in Arctic marine Monitoring; Gakkel_A1-1; Gakkel_N1-1; Latitude of event; Longitude of event; MOOR; Mooring; PS78/255-1; PS78/262-3
    Type: Dataset
    Format: text/tab-separated-values, 295 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 8
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    Current meter measurements in the equatorial Atlantic (1984)
    PANGAEA
    In:  Supplement to: Bauerfeind, Eduard; Brockmann, Christian; Fahrbach, Eberhard; Meincke, Jens; Panitz, Hans Jürgen; Rohardt, Gerd; Sy, Alexander (1984): A compendium of the oceanographic data obtained during FGGE-Equator '79, Cruise No. 51 of R.V. Meteor. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A/B Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A/B25, 1-108
    Details
    Publication Date: 2024-02-03
    Description: From 27 January to 23 June 1979 R.V. „Meteor“ surveyed the central equatorial Atlantic on a section along 22° W from 3° N to 2° S. During the observation period, a hydrographic section down to 600 m was repeated ten times with a continous „Howaldt-Bathysonde“ CTD and a rosette sampler. The station distance was 10 to 15 nm. The water samples were used to recalibrate salinity and to determine oxygen, nutrients and chlorophyll a. An undulating CTD system („Delphin“) was towed on 11 sections. A profiling distance of one to two nautical miles and a profile depth of 90 m was obtained. Five current meter arrys were moored along 22° W between 3° N and 1°S from January to March 1979. In May and June two moorings were installed at 2° N and at the equator. On the buoys measurements of wind speed and direction were obtained. At 43 stations a wire-guided Aanderaa profiling current meter was successfully lowered. Drifting buoy experiments were repeated three times with clusters of 5 to 10 buoys. A fourth experiment took place in 1978 in the Gulf of Guinea. On the way from and to XBT sections were carried out. The data sets obtained by these instruments are presented in this data report.
    Keywords: Atlantic Ocean; CTD/Rosette; CTD-RO; FGGE_1N; FGGE_1S; FGGE_2N1; FGGE_2N2; FGGE_3N; FGGE_ATK2N1; FGGE_ATK3N; FGGE_EQ1; FGGE_EQ2; FGGE_EQ3; FGGE_MET1N1; FGGE_MET1S; FGGE_MET2N1; FGGE_MET2N2; FGGE_MET3N; FGGE_METEQ1; FGGE_METEQ2; FGGE_METEQ3; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; HOBS; Howaldt-Bathysonde; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_004-1; M51_006-1; M51_007-1; M51_008-1; M51_009-1; M51_010-1; M51_011-1; M51_012-1; M51_013-1; M51_014-1; M51_015-1; M51_016-1; M51_017-1; M51_018-1; M51_019-1; M51_020-1; M51_021-1; M51_022-1; M51_023-1; M51_024-1; M51_025-1; M51_026-1; M51_027-1; M51_028-1; M51_029-1; M51_030-1; M51_031-1; M51_032-1; M51_033-1; M51_034-1; M51_035-1; M51_042-1; M51_043-2; M51_044-1; M51_045-1; M51_046-1; M51_047-1; M51_048-1; M51_049-2; M51_050-1; M51_051-1; M51_052-1; M51_053-1; M51_054-1; M51_055-1; M51_056-1; M51_057-1; M51_058-1; M51_059-1; M51_060-1; M51_061-1; M51_062-1; M51_063-1; M51_064-1; M51_065-1; M51_066-1; M51_071-1; M51_072-2; M51_073-2; 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_084-1; M51_085-1; M51_086-1; M51_087-1; M51_088-1; M51_090-2; M51_091-1; M51_092-1; M51_093-1; M51_094-1; M51_095-1; M51_096-1; M51_097-1; M51_098-2; M51_099-1; M51_100-1; M51_101-1; M51_102-1; M51_102-2; M51_103-1; M51_104-1; M51_105-1; M51_106-1; M51_107-1; M51_108-2; M51_109-1; M51_110-1; M51_111-1; M51_112-1; M51_113-2; M51_115-1; M51_116-2; M51_117-2; M51_122-1; M51_124-1; M51_125-1; M51_126-2; M51_127-1; M51_128-1; M51_129-1; M51_130-1; M51_131-1; M51_132-1; M51_134-2; M51_135-1; M51_136-1; M51_137-1; M51_138-1; M51_139-1; M51_140-1; M51_141-1; M51_142-1; M51_143-2; M51_144-1; M51_145-1; M51_146-1; M51_147-1; M51_148-1; M51_149-1; M51_150-2; M51_151-2; M51_152-2; M51_153-2; M51_154-2; M51_160-1; M51_161-1; M51_162-1; M51_163-1; M51_164-1; M51_165-1; M51_166-1; M51_167-1; M51_168-1; M51_169-1; M51_170-1; M51_171-1; M51_172-1; M51_173-1; M51_174-1; M51_175-1; M51_176-1; M51_177-1; M51_178-1; M51_179-1; M51_180-1; M51_181-2; M51_182-1; M51_183-1; M51_184-1; M51_185-1; M51_186-1; M51_190-1; M51_192-1; 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_200-1; M51_201-1; M51_202-1; M51_203-1; M51_204-1; M51_205-1; M51_206-1; M51_207-1; M51_208-1; M51_209-1; M51_210-1; M51_211-1; M51_212-2; M51_213-2; M51_214-2; M51_215-2; M51_216-1; M51_217-2; M51_218-1; M51_219-1; M51_220-1; M51_221-2; M51_222-1; M51_223-1; M51_224-2; M51_225-1; M51_226-1; 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_229-1; M51_229-2; M51_231-2; M51_232-1; M51_233-1; M51_234-1; M51_235-1; M51_235-2; M51_236-2; M51_237-1; M51_238-2; M51_240-1; M51_241-1; M51_242-2; M51_243-1; M51_244-1; M51_245-1; M51_246-1; M51_246-2; M51_247-2; M51_248-1; M51_249-1; M51_250-1; M51_251-1; M51_252-1; M51_253-1; M51_254-1; M51_255-2; M51_256-1; M51_257-1; M51_258-2; M51_260-1; M51_261-2; M51_262-1; M51_263-1; M51_264-1; M51_265-1; M51_266-1; M51_267-2; M51_268-1; M51_269-1; M51_270-1; M51_271-1; M51_272-1; M51_273-2; M51_274-1; M51_275-1; M51_276-1; M51_277-1; M51_278-1; M51_279-1; M51_280-1; M51_286-2; M51_286-4; M51_291-1; M51_292-2; M51_293-1; M51_294-2; M51_295-1; M51_296-1; M51_297-1; M51_298-1; M51_299-1; M51_300-1; M51_301-2; M51_302-1; M51_305-1; M51_306-1; M51_307-1; M51_308-1; M51_309-2; M51_310-1; M51_311-1; M51_312-1; M51_313-1; M51_314-1; M51_315-1; M51_316-1; M51_317-1; M51_318-4; M51_320-2; M51_321-1; M51_322-1; M51_323-2; M51_324-1; M51_325-1; M51_326-1; M51_329-4; M51_330-1; M51_331-1; M51_333-2; M51_334-1; M51_335-1; M51_336-1; M51_337-1; M51_338-1; M51_339-1; M51_341-1; M51_342-1; M51_343-1; M51_344-2; M51_345-1; M51_346-1; M51_B0105N; M51_B0105S; M51_B0110N; M51_B0110S; M51_B0115N; M51_B0115S; M51_B0120N; M51_B0120S; M51_B0125N; M51_B0130N; M51_B0205N; M51_B0205S; M51_B0210N; M51_B0210S; M51_B0215N; M51_B0215S; M51_B0220N; M51_B0220S; M51_B0230N; M51_B0305N; M51_B0305S; M51_B0310N; M51_B0310S; M51_B0315N; M51_B0315S; M51_B0320N; M51_B0320S; M51_B0325N; M51_B0330N; M51_B0405N; M51_B0405S; M51_B0410N; M51_B0410S; M51_B0415N; M51_B0415S; M51_B0420N; M51_B0420S; M51_B0425N; M51_B0430N; M51_B04EQ; M51_B0505N; M51_B0505S; M51_B0510N; M51_B0510S; M51_B0515N; M51_B0515S; M51_B0520N; M51_B0520S; M51_B0525N; M51_B0530N; M51_B05EQ; M51_B0605N; M51_B0605S; M51_B0610N; M51_B0610S; M51_B0615N; M51_B0620N; M51_B0625N; M51_B0630N; M51_B06EQ; M51_B0705N; M51_B0705S; M51_B0710N; M51_B0710S; M51_B0715N; M51_B0715S; M51_B0720N; M51_B0720S; M51_B0725N; M51_B0730N; M51_B07EQ; M51_B0805N; M51_B0805S; M51_B0810N; M51_B0810S; M51_B0815N; M51_B0815S; M51_B0820N; M51_B0820S; M51_B0825N; M51_B0830N; M51_B08EQ; M51_B0905N; M51_B0905S; M51_B0910N; M51_B0910S; M51_B0915N; M51_B0915S; M51_B0920N; M51_B0920S; M51_B0925N; M51_B0930N; M51_B1005N; M51_B1005S; M51_B1010N; M51_B1010S; M51_B1015N; M51_B1015S; M51_B1020N; M51_B1025N; M51_B1030N; M51_B10EQ; M51_BFS062; M51_BFS09E; Meteor (1964); MOOR; Mooring; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 27 datasets
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    DATA PANGAEA
  • 9
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    Effects of Atlantification and changing sea-ice dynamics on zooplankton community structure and carbon flux between 2000 and 2016 in the eastern Fram Strait (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-02
    Description: The collection of zooplankton swimmers and sinkers in time-series sediment traps provides a unique insight into year-round and inter-annual trends in zooplankton population dynamics. Such samples are particularly valuable in remote and difficult to access areas such as the Arctic Ocean, where samples from the ice-covered seasons are rare. In the present study, we investigated zooplankton composition based on swimmers and sinkers collected by sediment traps at water depths of 180-280 m, 800-1320 m, and 2320-2550 m, over a period of 16 years (2000-2016) at the central station of the LTER (Long-Term Ecological Research) HAUSGARTEN observatory in the Fram Strait. The time-series data include the abundance of copepoda, foraminifera, ostracoda, amphipoda, pteropoda, and chaetognatha that were collected in the sediment trap time-series.
    Keywords: Amphipoda, flux; ARK-XVI/2; ARK-XVII/1; ARK-XVIII/1; ARK-XX/1; ARK-XXI/1b; ARK-XXII/1c; ARK-XXIII/2; ARK-XXIV/2; ARK-XXIX/2.2; ARK-XXV/2; ARK-XXVI/2; ARK-XXVII/2; ARK-XXVIII/2; Chaetognatha, flux; Copepoda, flux; DATE/TIME; DEPTH, water; Event label; FEVI1; FEVI10; FEVI13; FEVI16; FEVI18; FEVI2; FEVI20; FEVI22; FEVI24; FEVI26; FEVI28; FEVI3; FEVI30; FEVI32; FEVI7; Foraminifera, flux; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HAUSGARTEN 2013; Latitude of event; Longitude of event; Long-term Investigation at AWI-Hausgarten off Svalbard; Maria S. Merian; Mooring (long time); MOORY; MSM02/4; MSM2/787-1, HGIV; MSM29; North Greenland Sea; Ostracoda, flux; Polarstern; Position; PS57; PS57/273-1, HGIV; PS59; PS59/101-1, HGIV; PS62; PS62/179-2, HGIV; PS66; PS66/129-1, HGIV; PS68; PS68/263-1, HGIV; PS70; PS70/218-1, HGIV; PS72; PS72/155-1, HGIV; PS74; PS74/125-2, HGIV; PS76; PS76/147-1, HGIV; PS78; PS78/177-1, HGIV; PS80; PS85; PS85/462-1, HGIV; PS93.2; Pteropoda, flux; sediment trap; Sediment trap; sinkers; swimmers; Zooplankton
    Type: Dataset
    Format: text/tab-separated-values, 3488 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 10
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    Current meter profile of station M51_2N2 in the equatorial Atlantic (Table 4) (1984)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_2N2; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_235-2; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
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