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  • PANGAEA  (199)
  • AMER SOC LIMNOLOGY OCEANOGRAPHY  (1)
  • Elsevier B.V.  (1)
  • INTER-RESEARCH  (1)
  • Institut für Meereskunde  (1)
Document type
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Years
  • 11
    Publication Date: 2023-03-10
    Keywords: Atlantic Ocean; Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; FGGE_EQ1; FGGE_EQ2; FGGE-Equator 79 - First GARP Global Experiment; HOBS; Howaldt-Bathysonde; Latitude of event; Longitude of event; M51; 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_114-1; M51_115-1; M51_116-2; M51_117-2; M51_122-1; M51_123-1; 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_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_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_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; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 998682 data points
    Location Call Number Limitation Availability
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  • 12
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    PANGAEA
    In:  Supplement to: Kraft, Angelina; Bauerfeind, Eduard; Nöthig, Eva-Maria; Klages, Michael; Beszczynska-Möller, Agnieszka; Bathmann, Ulrich (2013): Amphipods in sediment traps of the eastern Fram Strait with focus on the life-history of the lysianassoid Cyclocaris guilelmi. Deep Sea Research Part I: Oceanographic Research Papers, 73, 62-72, https://doi.org/10.1016/j.dsr.2012.11.012
    Publication Date: 2023-03-16
    Description: Life-cycle characteristics of the free-swimming lysianassoid amphipod Cyclocaris guilelmi were investigated and compared to those of other regularly appearing amphipods in the Arctic deep-sea community. In this context we analysed time-series data of meso- and bathypelagic amphipods collected as swimmers in moored sediment traps from 2004 to 2008 at the deep-sea long-term observatory HAUSGARTEN (79°N/4°E) in the eastern Fram Strait, Arctic Ocean. Six mesopelagic and three bathypelagic deep-sea amphipod species regularly occurred in the traps. The lysianassoid C. guilelmi showed a stable interannual population size and seasonal peaks in its occurrence from August to February during the five-year sampling period. The investigation of its population structure and reproduction ecology indicated year-round breeding behavior of this species. Up to 4 cohorts consisting mainly of juvenile and female C. guilelmi were observed. We conclude that C. guilelmi plays an important role within the Arctic amphipod deep water community.
    Keywords: Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
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  • 13
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    PANGAEA
    In:  Supplement to: von Bodungen, Bodo; Antia, Avan N; Bauerfeind, Eduard; Haupt, Olaf; Koeve, Wolfgang; Machado, E; Peeken, Ilka; Peinert, Rolf; Reitmeier, Sven; Thomsen, C; Voss, Maren; Wunsch, M; Zeller, Ute; Zeitzschel, Bernt (1995): Pelagic processes and vertical flux of particles: an overview of a long-term comparative study in the Norwegian Sea and Greenland Sea. Geologische Rundschau, 84(1), 11-27, https://doi.org/10.1007/BF00192239
    Publication Date: 2023-05-12
    Description: Pelagic processes and their relation to vertical flux have been studied in the Norwegian and Greenland Seas since 1986. Results of long-term sediment trap deployments and adjoining process studies are presented, and the underlying methodological and conceptional background is discussed. Recent extension of these investigations at the Barents Sea continental slope are also presented. With similar conditions of input irradiation and nutrient conditions, the Norwegian and Greenland Seas exhibit comparable mean annual rates of new and total production. Major differences can be found between these regions, however, in the hydrographic conditions constraining primary production and in the composition and seasonal development of the plankton. This is reflected in differences in the temporal patterns of vertical particle flux in relation to new production in the euphotic zone, the composition of particles exported and in different processes leading to their modification in the mid-water layers. In the Norwegian Sea heavy grazing pressure during early spring retards the accumulation of phytoplankton stocks and thus a mass sedimentation of diatoms that is often associated with spring blooms. This, in conjunction with the further seasonal development of zooplankton populations, serves to delay the annual peak in sedimentation to summer or autumn. Carbonate sedimentation in the Norwegian Sea, however, is significantly higher than in the Greenland Sea, where physical factors exert a greater control on phytoplankton development and the sedimentation of opal is of greater importance. In addition to these comparative long-term studies a case study has been carried out at the continental slope of the Barents Sea, where an emphasis was laid on the influence of resuspension and across-slope lateral transport with an analysis of suspended and sedimented material.
    Keywords: Global Environmental Change: The Northern North Atlantic; Jan-Mayen Current; MOOR; Mooring; OG4; OG5; SFB313; SFB313Moorings; Silicon Cycling in the World Ocean; SINOPS
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 14
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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: 2023-05-12
    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; 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; South Atlantic Ocean; Water sample; WS; XBT
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 15
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    PANGAEA
    In:  Supplement to: Bauerfeind, Eduard; Nöthig, Eva-Maria; Pauls, Bendiks; Kraft, Angelina; Beszczynska-Möller, Agnieszka (2014): Variability in pteropod sedimentation and corresponding aragonite flux at the Arctic deep-sea long-term observatory HAUSGARTEN in the eastern Fram Strait from 2000 to 2009. Journal of Marine Systems, 132, 95-105, https://doi.org/10.1016/j.jmarsys.2013.12.006
    Publication Date: 2023-05-12
    Description: Pteropods are an important component of the zooplankton community and hence of the food web in the Fram Strait. They have a calcareous (aragonite) shell and are thus sensitive in particular to the effects of the increasing CO2 concentration in the atmosphere and the associated changes of pH and temperature in the ocean. In the eastern Fram Strait, two species of thecosome pteropods occur, the cold water-adapted Limacina helicina and the subarctic boreal species Limacina retroversa. Both species were regularly observed in year-round moored sediment traps at ~ 200-300 m depth in the deep-sea long-term observatory HAUSGARTEN (79°N, 4°E). The flux of all pteropods found in the trap samples varied from 〈 20 to ~ 870 specimen/m**2/d in the years 2000-2009, being lower during the period 2000-2006. At the beginning of the time series, pteropods were dominated by the cold-water-adapted L. helicina, whereas the subarctic boreal L. retroversa was only occasionally found in large quantities (〉 50/m**2/d). This picture completely changed after 2005/6 when L. retroversa became dominant and total pteropod numbers in the trap samples increased significantly. Concomitant to this shift in species composition, a warming event occurred in 2005/6 and persisted until the end of the study in 2009, despite a slight cooling in the upper water layer after 2007/8. Sedimentation of pteropods showed a strong seasonality, with elevated fluxes of L. helicina from August to November. Numbers of L. retroversa usually increased later, during September/October, with a maximum at the end of the season during December/January. In terms of carbonate export, aragonite shells of pteropods contributed with 11-77% to the annual total CaCO3 flux in Fram Strait. The highest share was found in the period 2007 to 2009, predominantly during sedimentation events at the end of the year. Results obtained by sediment traps occasionally installed on a benthic lander revealed that pteropods also arrive at the seafloor (~ 2550 m) almost simultaneous with their occurrence in the shallower traps. This indicates a rapid downward transport of calcareous shells, which provides food particles for the deep-sea benthos during winter when other production in the upper water column is shut down. The results of our study highlight the great importance of pteropods for the biological carbon pump as well as for the carbonate system in Fram Strait at present, and indicate modifications within the zooplankton community. The results further emphasize the importance of long-term investigation to disclose such changes.
    Keywords: Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard
    Type: Dataset
    Format: application/zip, 11 datasets
    Location Call Number Limitation Availability
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  • 16
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    PANGAEA
    In:  Supplement to: von Appen, Wilken-Jon; Schauer, Ursula; Somavilla, Raquel; Bauerfeind, Eduard; Beszczynska-Möller, Agnieszka (2015): Exchange of warming deep waters across Fram Strait. Deep Sea Research Part I: Oceanographic Research Papers, 103, 86-100, https://doi.org/10.1016/j.dsr.2015.06.003
    Publication Date: 2023-05-12
    Description: Current meters measured temperature and velocity on 12 moorings from 1997 to 2014 in the deep Fram Strait between Svalbard and Greenland at the only deep passage from the Nordic Seas to the Arctic Ocean. The sill depth in Fram Strait is 2545 m. The observed temperatures vary between the colder Greenland Sea Deep Water and the warmer Eurasian Basin Deep Water. Both end members show a linear warming trend of 0.11±0.02°C/decade (GSDW) and 0.05±0.01°C/decade (EBDW) in agreement with the deep water warming observed in the basins to the north and south. At the current warming rates, GSDW and EBDW will reach the same temperature of -0.71°C in 2020. The deep water on the approximately 40 km wide plateau near the sill in Fram Strait is a mixture of the two end members with both contributing similar amounts. This water mass is continuously formed by mixing in Fram Strait and subsequently exported out of Fram Strait. Individual measurements are approximately normally distributed around the average of the two end members. Meridionally, the mixing is confined to the plateau region. Measurements less than 20 km to the north and south have properties much closer to the properties in the respective basins (Eurasian Basin and Greenland Sea) than to the mixed water on the plateau. The temperature distribution around Fram Strait indicates that the mean flow cannot be responsible for the deep water exchange across the sill. Rather, a coherence analysis shows that energetic mesoscale flows with periods of approximately 1-2 weeks advect the deep water masses across Fram Strait. These flows appear to be barotropically forced by upper ocean mesoscale variability. We conclude that these mesoscale flows make Fram Strait a hot spot of deep water mixing in the Arctic Mediterranean. The fate of the mixed water is not clear, but after the 1990s, it does not reflect the properties of Norwegian Sea Deep Water. We propose that it currently mostly fills the deep Greenland Sea.
    Keywords: AWI_PhyOce; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Physical Oceanography @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 17
    Publication Date: 2023-03-25
    Keywords: Counting; Cyclocaris guilelmi, abundance index; DATE/TIME; Date/time end; DEPTH, water; Duration, number of days; GREENLANDSEA_TRAP; Sample code/label; South Greenland Sea; Themisto abyssorum, abundance index; Trap; TRAP
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
    Location Call Number Limitation Availability
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  • 18
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    Unknown
    PANGAEA
    In:  Supplement to: Lalande, Catherine; Nöthig, Eva-Maria; Bauerfeind, Eduard; Hardge, Kristin; Beszczynska-Möller, Agnieszka; Fahl, Kirsten (2016): Lateral supply and downward export of particulate matter from upper waters to the seafloor in the deep eastern Fram Strait. Deep Sea Research Part I: Oceanographic Research Papers, 114, 78-89, https://doi.org/10.1016/j.dsr.2016.04.014
    Publication Date: 2023-01-13
    Description: Time-series sediment traps were deployed at 4 depths in the eastern Fram Strait from July 2007 to June 2008 to investigate variations in the magnitude and composition of the sinking particulate matter from upper waters to the seafloor. Sediment traps were deployed at 196 m in the Atlantic Water layer, at 1296 and 2364 m in the intermediate and deep waters, and at 2430 m on a benthic lander in the near-bottom layer. Fluxes of total particulate matter, particulate organic carbon, particulate organic nitrogen, biogenic matter, lithogenic matter, biogenic particulate silica, calcium carbonate, dominant phytoplankton cells, and zooplankton fecal pellets increased with depth, indicating the importance of lateral advection on fluxes in the deep Fram Strait. The lateral supply of particulate matter was further supported by the constant fluxes of biomarkers such as brassicasterol, alkenones, campesterol, beta-sitosterol, and IP25 at all depths sampled. However, enhanced fluxes of diatoms and appendicularian fecal pellets from the upper waters to the seafloor in the presence of ice during spring indicated the rapid export (15-35 days) of locally-produced large particles that likely contributed most of the food supply to the benthic communities. These results show that lateral supply and downward fluxes are both important processes influencing the transport of particulate matter to the seafloor in the deep eastern Fram Strait, and that particulate matter size dictates the prevailing sinking process.
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 19
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    Unknown
    PANGAEA
    In:  Supplement to: Peinert, Rolf; Antia, Avan N; Bauerfeind, Eduard; von Bodungen, Bodo; Haupt, Olaf; Krumbholz, Marita; Peeken, Ilka; Ramseier, René O; Voss, Maren; Zeitzschel, Bernt (2001): Particle flux variability in the polar and Atlantic biogeochemical provinces of the Nordic Seas. In: Schäfer, W; Ritzrau, M; Schlüter & J. Thiede (eds.) The Northern North Atlantic: A Changing Environment, Springer Verlag, Berlin, 500 pp, 53-68, https://doi.org/10.1007/978-3-642-56876-3_4
    Publication Date: 2023-01-13
    Description: A decade of particle flux measurements providse the basis for a comparison of the eastern and western province s of the Nordic Seas. Ice-related physical and biological seasonality as well as pelagic settings jointly control fluxes in the western Polar Province which receive s southward flowing water of Polar origin. Sediment trap data from this realm highlight a predominantly physical flux control which leads to exports of siliceous particle s within the biological marginal ice zone as a prominent contributor. In the northward flowing waters of the eastern Atlanti c Province, feeding strategies, life histories and the succession ofdominant mesozooplankters (copepods and pteropods) are central in controlling fluxes. Furthermore, more calcareous matter is exported here with a shift in flux seasonality towards summer I autumn. Dominant pelagic processes modeled numerically as to their impact on annual organic carbon exports for both provinces confirm that interannual flux variability is related to changes in the respecti ve control mechanisms. Annual organic carbon export s are strikingly similar in the Polar and Atlantic Province s (2.4 and 2.9 g/m**2/y at 500 m depth), despite major differences in flux control. The Polar and Atlantic Provinces, however, can be distinguished according to annual fluxes of opal (1.4 and 0.6 g/m**2/y) and carbonate (6.8 and 10.4 g/m**2/y). Interannual variability may blur this in single years. Thus, it is vital to use multi-annual data sets when including particle exports in general biogeochemical province descriptions. Vertical flux profiles (collections from 500 m, 1000 m in both provinces and 300-600 m above the seafloor deviate from the general vertical decline of fluxes due to particle degradation during sinking. At depths〉 1000 m secondary fluxes (laterally advectedlresuspended particles) are often juxtaposed to primary (pelagic) fluxes, a pattern which is most prominent in the Atlantic Province. Spatial variability within the Atlantic Province remains poorly understood, and the same holds true for interannual variability. No proxies are at hand for this province to quantitatively relate fluxes to physical or biological pelagic properties. For the seasonally ice-covered Polar Province a robust relationship exists between particle export and ambient ice-regime (Ramseier et al. this volume; Ramseier et al. 1999). Spatial flux patterns may be differentiated and interannual variability can be analyzed in this manner to impro ve our ability to couple pelagic export patterns with benthic and geochemical sedimentary processes in seasonally ice-covered seas.
    Keywords: Global Environmental Change: The Northern North Atlantic; SFB313
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 20
    Publication Date: 2023-01-13
    Keywords: ALTITUDE; DATE/TIME; FGGE_METEQ3; FGGE-Equator 79 - First GARP Global Experiment; M51; Meteor (1964); MOOR; Mooring; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 4835 data points
    Location Call Number Limitation Availability
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