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  • PANGAEA  (56,379)
  • 2005-2009  (56,379)
  • 2007  (56,379)
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  • 2005-2009  (56,379)
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  • 1
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    Oxygen respiration and metabolic enzyme malate dehydrogenase of Euphasia superba in the South Atlantic Ocean (2007)
    PANGAEA
    In:  Supplement to: Pape, Carsten; Teschke, Mathias; Meyer, Bettina (2008): Melatonin and its possible role in mediating seasonal metabolic changes of Antarctic krill, Euphausia superba. Comparative Biochemistry and Physiology - Part A: Molecular & Integrative Physiology, 149(4), 426-434, https://doi.org/10.1016/j.cbpa.2008.02.001
    Details
    Publication Date: 2024-06-26
    Description: Melatonin, the chief secretory product of the vertebrate pineal gland is suspected to be a ubiquitous molecule principally involved in the transduction of photoperiodic information. Besides vertebrates, melatonin has been detected throughout phylogeny in numerous non-vertebrate taxa. In the present study, the occurrence of melatonin in Antarctic krill Euphausia superba and its possible role in mediating seasonal metabolic changes was evaluated. Melatonin was quantified by enzyme linked immunosorbent assay (ELISA) in high performance liquid chromatography (HPLC) purified extracts of eyestalks and hemolymph of krill sampled in the Lazarev Sea during the Antarctic winter and summer. In addition, oxygen uptake rates and the activities of the metabolic enzyme malate dehydrogenase (MDH) were recorded to assess the metabolic status of krill. Validation of melatonin measurements was carried out on the basis of three different extraction methods with parallel determination of melatonin by ELISA in crude extracts and in HPLC purified extracts, and after derivatization of melatonin under alkaline conditions in the presence of hydrogen peroxide. A significantly higher respiration rate and MDH activity was found in summer krill than in winter krill indicating that krill was in a state of reduced metabolic activity during winter. However, neither during winter nor during summer there were detectable melatonin concentrations in the visual system or hemolymph of krill. Based on these results, we question a mediating role of melatonin in the control of seasonal metabolic changes in Antarctic krill in particular and its physiological significance in krill in general.
    Keywords: ANT-XXIII/2; ANT-XXIII/6; AWI_BioOce; Biological Oceanography @ AWI; Polarstern; PS69; PS69/043-2; PS69/046-1; PS69/078-1; PS69/092-1; PS69/474-1; PS69/489-1; PS69/497-1; PS69/506-7; PS69/518-1; PS69/520-1; PS69/534-1; Rectangular midwater trawl; RMT
    Type: Dataset
    Format: application/zip, 14 datasets
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    DATA PANGAEA
  • 2
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    Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean (2007)
    PANGAEA
    In:  Supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551, https://doi.org/10.1016/j.quascirev.2005.07.024
    Details
    Publication Date: 2024-06-26
    Description: New geochronometers are needed for sediments of the Arctic Ocean spanning at least the last half million years, largely because oxygen-isotope stratigraphy is relatively ineffective in this ocean, and because other dating techniques require significant assumptions about sedimentation rates. Multi-aliquot luminescence sediment-dating procedures were applied to polymineral, fine-silt samples from 9 core-top and 37 deeper samples from 20 cores representing 19 sites across the Arctic Ocean. Most samples have independent age assignments and other known properties (e.g., % coarse fraction, % carbonate, U-Th isotopes). Thick-source alpha-particle counting indicates that for most regions the contribution of measured unsupported 230Th and 231Pa to calculated dose rates is 〈ca+5–11%. IR-PSL dating of polymineral fine-silt fractions from core-top and near-core-top samples indicates that three sites (mainly from the western Arctic Ocean) have long-bleach inherited ages of only 3–7 kyr, suggesting potential for accurate PSL and TL dating without an inherited correction when older interglacial samples are selected. Samples from a giant gravity core from the western region (Northwind Ridge) yield acceptable long-bleach TL and IR-PSL ages up to 100 kyr. A sample from the eastern region (near Gakkel Ridge) gives a long-bleach age of ca 60 kyr, agreeing with an independent age assignment. Several samples in the 10–40 kyr 14C range from other sites produce large long-bleach age overestimates, indicating the variable effects of ice-rafting and other depositional and bottom-currentreworking (re-suspension) processes during glacial stages. Short-bleach dating tests provide IR-PSL age estimates for core tops that appear to penetrate the 'reworking veil' of inherited ages, and not only suggest a procedure to greatly reduce long-bleach inherited ages but also have implications for the 14C reservoir correction. This study identifies the most promising regions for future luminescence dating, and suggests that for several regions of the Arctic Ocean, interglacial-stage (foram-'rich') sediments from ridge tops are preferred for the fine-grain luminescence dating methods.
    Keywords: 88-BC22; 88-GGC23; 89-BC11; 92-BC17; 94-BC16; 94-BC17; 94-BC19; 94-BC20; 94-BC28; Amundsen Basin; Antarctic Ocean; Arctic Ocean; ARK-IV/3; ARK-VIII/3; BC; Box corer; Gakkel Ridge, Arctic Ocean; GGC; Giant box corer; Giant gravity corer; Giant piston corer; GIK21524-2 PS11/364-2; GIK21533-3 PS11/412; GKG; GPC; Gravity corer (Kiel type); KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Morris Jesup Rise; Polarstern; PS11; PS1524-2; PS1533-3; PS19/157; PS19/160; PS19/165; PS19/175; PS19/186; PS19/206; PS19/218; PS19/222; PS19/228; PS19 ARCTIC91; PS2163-2; PS2166-2; PS2170-1; PS2177-1; PS2185-3; PS2195-4; PS2200-2; PS2202-2; PS2206-3; SL; Svalbard
    Type: Dataset
    Format: application/zip, 18 datasets
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    DATA PANGAEA
  • 3
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    Meiobenthos investigations in the Black Sea during Poseidon cruise POS317/3 (2007)
    PANGAEA
    In:  Supplement to: Sergeeva, Nelly G; Gulin, Maksim (2007): Meiobenthos from an active methane seepage area in the NW Black Sea. Marine Ecology, 28(1), 152-159, https://doi.org/10.1111/j.1439-0485.2006.00143.x
    Details
    Publication Date: 2024-06-26
    Description: Meiobenthos densities and higher taxon composition were studied in an active gas seepage area at depths from 182 to 252 m in the submarine Dnieper Canyon located in the northwestern part of the Black Sea. The meiobenthos was represented by Ciliata, Foraminifera, Nematoda, Polychaeta, Bivalvia, Gastropoda, Amphipoda, and Acarina. Also present in the sediment samples were juvenile stages of Copepoda and Cladocera which may be of planktonic origin. Nematoda and Foraminifera were the dominant groups. The abundance of the meiobenthos varied between 2397 and 52593 Ind./m**2. Maximum densities of Nematoda and Foraminifera were recorded in the upper sediment layer of a permanent H2S zone at depths from 220 to 250 m. This dense concentration of meiobenthos was found in an area where intense methane seeps were covered by methane-oxidizing microbial mats. Results suggest that methane and its microbial oxidation products are the factors responsible for the presence of a highly sulfidic and biologically productive zone characterized by specially adapted benthic groups. At the same time, an inverse correlation was found between meiofauna densities and methane concentrations in the uppermost sediment layers. The hypothesis is that the concentration of Nematoda and Foraminifera within the areas enriched with methane is an ecological compromise between the food requirements of these organisms and their adaptations to the toxic H2S.
    Keywords: GC; Gravity corer; HERMES; Hotspot Ecosystem Research on the Margins of European Seas; MUC; MultiCorer; P14; P4; P5; P6; P7; P8; P9; POS317/3; POS317/3_790MUC; POS317/3_796GC; POS317/3_802MUC; POS317/3_803MUC; POS317/3_804MUC; POS317/3_805MUC; POS317/3_815MUC; POS317/3_827MUC; Poseidon; Western Black Sea
    Type: Dataset
    Format: application/zip, 8 datasets
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    DATA PANGAEA
  • 4
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    Carbonate sedimentology of the Propeller Mound, Northeast Atlantic (2007)
    PANGAEA
    In:  Supplement to: Dorschel, Boris; Hebbeln, Dierk; Rüggeberg, Andres; Dullo, Wolf-Christian (2007): Carbonate budget of a cold-water coral carbonate mound: Propeller Mound, Porcupine Seabight. International Journal of Earth Sciences, 96(1), 73-83, https://doi.org/10.1007/s00531-005-0493-0
    Details
    Publication Date: 2024-06-26
    Description: High resolution studies from the Propeller Mound, a cold-water coral carbonate mound in the NE Atlantic, show that this mound consists of 〉50% carbonate justifying the name "carbonate mound". Through the last ~300,000 years approximately one third of the carbonate has been contributed by cold-water corals, namely Lophelia pertusa and Madrepora oculata. This coral bound contribution to the carbonate budget of Propeller Mound is probably accompanied by an unknown portion of sediments buffered from suspension by the corals. However, extended hiatuses in Propeller Mound sequences only allow the calculation of a net carbonate accumulation. Thus, net carbonate accumulation for the last 175 kyr accounts for only 〈0.3 g/cm2/kyr, which is even less than for the off-mound sediments. These data imply that Propeller Mound faces burial by hemipelagic sediments as has happened to numerous buried carbonate mounds found slightly to the north of the investigated area.
    Keywords: Center for Marine Environmental Sciences; ECOMOUND; Environmental controls on mound formation along the european margin; GeoB6718-2; GeoB6719-1; GeoB6725-1; GeoB6728-1; GeoB6729-1; GeoB6730-1; Gravity corer (Kiel type); MARUM; Porcupine Seabight; POS265; POS478-2; POS479-1; POS485-1; POS488-1; POS489-1; POS490-1; Poseidon; SL
    Type: Dataset
    Format: application/zip, 16 datasets
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    DATA PANGAEA
  • 5
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    Terrigenous sedimentation of sediment core GeoB6007-2 (2007)
    PANGAEA
    In:  Supplement to: Holz, Christine; Stuut, Jan-Berend W; Henrich, Rüdiger; Meggers, Helge (2007): Variability in terrigenous sedimentation processes off northwest Africa and its relation to climatic changes: inferrence from grain-size distributions of a Holocene marine sediment record. Sedimentary Geology, 202(3), 499-508, https://doi.org/10.1016/j.sedgeo.2007.03.015
    Details
    Publication Date: 2024-06-26
    Description: Variations in deposition of terrigenous fine sediments and their grain-size distributions from a high-resolution marine sediment record offshore northwest Africa (30°51.0'N; 10°16.1'W) document climate changes on the African continent during the Holocene. End-member grain-size distributions of the terrigenous silt fraction, which are related to fluvial and aeolian dust transport, indicate millennial-scale variability in the dominant transport processes at the investigation site off northwest Africa as well as recurring periods of dry conditions in northwest Africa during the Holocene. The terrigenous record from the subtropical North Atlantic reflects generally humid conditions before the Younger Dryas, during the early to mid-Holocene, as well as after 1.3 kyr BP. By contrast, continental runoff was reduced and arid conditions were prevalent at the beginning of the Younger Dryas and during the mid- and late Holocene. A comparison with high- and low-latitude Holocene climate records reveals a strong link between northwest African climate and Northern Hemisphere atmospheric circulation throughout the Holocene. Due to its proximal position, close to an ephemeral river system draining the Atlas Mountains as well as the adjacent Saharan desert, this detailed marine sediment record, which has a temporal resolution between 15 and 120 years, is ideally suited to enhance our understanding of ocean-continent-atmosphere interactions in African climates and the hydrological cycle of northern Africa after the last deglaciation.
    Keywords: GeoB; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M45/5a; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
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    Chemical and isotopic compositions of sediments and some minerals from the Derugin Basin, Sea of Okhotsk (2007)
    PANGAEA
    In:  Supplement to: Derkachev, A N; Nikolaeva, N A; Mozherovsky, A V; Grigorieva, T N; Ivanova, E D; Pletnev, S P; Barinov, N N; Chubarov, Valerii M (2007): Mineralogical and geochemical indicators of anoxic sedimentation conditions in local depressions within the Sea of Okhotsk in Late Pleistocene-Holocene. Tikhookeanskaya Geologiya, No 3, 3-33
    Details
    Publication Date: 2024-06-26
    Description: The paper reports specific mineralogical and geochemical characteristics of deposits from local depressions of the Derugin Basin. They were formed in an environment with periodic changes from oxic to anoxic conditions and show evidence for presence of hydrogen sulfide in bottom waters. Deposits of this type can be considered as a modern model for ancient ore-bearing black shale associations. Compared with typical metalliferous black shale sequences, which are characterized by high contents of organic matter, the sediments described here are depleted in elements of the organophilic association (Mo, Ni, Cu, Zn, V, and U), but have higher Mn contents.
    Keywords: Akademik M.A. Lavrentyev; Archive of Ocean Data; ARCOD; Derugin Basin; GC; Gravity corer; Gravity corer (Russian type); KOL; KOMEX; KOMEX I; KOMEX II; LV28; LV28-37-1; LV29-103-2; LV29-104-2; LV29-2; Piston corer (Kiel type); RGC; Sakhalin shelf and slope; Sea of Okhotsk; SO178; SO178-13-4; SO178-78-1; Sonne
    Type: Dataset
    Format: application/zip, 3 datasets
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    DATA PANGAEA
  • 7
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    Benthic foraminifera, stable isotope ratios and carbon concentrations of sediment cores from Propeller Mound and Porcupine Srabight (2007)
    PANGAEA
    In:  Supplement to: Rüggeberg, Andres; Dullo, Wolf-Christian; Dorschel, Boris; Hebbeln, Dierk (2007): Environmental changes and growth history of a cold-water carbonate mound (Propeller Mound, Porcupine Seabight). International Journal of Earth Sciences, 96(1), 57-72, https://doi.org/10.1007/s00531-005-0504-1
    Details
    Publication Date: 2024-06-26
    Description: On- and off-mound sediment cores from Propeller Mound (Hovland Mound province, Porcupine Seabight) were analysed to understand better the evolution of a carbonate mound. The evaluation of benthic foraminiferal assemblages from the off-mound position helps to determine the changes of the environmental controls on Propeller Mound in glacial and interglacial times. Two different assemblages describe the Holocene and Marine Isotope Stage (MIS) 2 and late MIS 3 (~31 kyr BP). The different assemblages are related to changes in oceanographic conditions, surface productivity and the waxing and waning of the British Irish Ice Sheet (BIIS) during the last glacial stages. The interglacial assemblage is related to a higher supply of organic material and stronger current intensities in water depth of recent coral growth. During the last glaciation the benthic faunas showed high abundances of cassidulinid species, implying cold bottom waters and a reduced availability of organic matter. High sedimentation rates and the domination of Elphidium excavatum point to shelf erosion related to sea-level lowering (~50 m) and the progradation of the BIIS onto the shelf. A different assemblage described for the on-mound core is dominated by Discanomalina coronata, Gavelinopsis translucens, Planulina ariminensis, Cibicides lobatulus and to a lower degree by Hyrrokkin sarcophaga. These species are only found or show significantly higher relative abundances in on-mound samples and their maximum contribution in the lower part of the record indicates a higher coral growth density on Propeller Mound in an earlier period. They are less abundant during the Holocene, however. This dataset portrays the boundary conditions of the habitable range for the cold-water coral Lophelia pertusa, which dominates the deep-water reefal ecosystem on the upper flanks of Propeller Mound. The growth of this ecosystem occurs during interglacial and interstadial periods, whereas a retreat of corals is documented in the absence of glacial sediments on-mound. Glacial conditions with cold intermediate waters, a weak current regime and high sedimentation rates provide an unfavourable environmental setting for Lophelia corals to grow. A Late Pleistocene decrease is observed in the mound growth for Propeller Mound, which might face its complete burial in the future, as it already happened to the buried mounds of the Magellan Mound province further north.
    Keywords: Center for Marine Environmental Sciences; ECOMOUND; Environmental controls on mound formation along the european margin; GeoB6725-1; GeoB6730-1; Gravity corer (Kiel type); MARUM; Porcupine Seabight; POS265; POS485-1; POS490-1; Poseidon; SL
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 8
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    Pollen analysis of sediment cores from the mouth of the river Congo to Walvis Bay and Lüderitz (2007)
    PANGAEA
    In:  Supplement to: Dupont, Lydie M; Behling, Hermann; Jahns, Susanne; Marret, Fabienne; Kim, Jung-Hyun (2007): Variability in glacial and Holocene marine pollen records offshore from west southern Africa. Vegetation History and Archaeobotany, 16, 87-100, https://doi.org/10.1007/s00334-006-0080-8
    Details
    Publication Date: 2024-06-26
    Description: The distribution of pollen in marine sediments is used to record vegetation changes over the past 30,000 years on the adjacent continent. A transect of marine pollen sequences from the mouth of the river Congo (~5°S) to Walvis Bay and Lüderitz (~25°S) shows vegetation changes in Congo, Angola and Namibia from the last glacial period into the Holocene. The comparison of pollen records from different latitudes provides information about the latitudinal shift of open forest and savannahs (Poaceae pollen), the extension of lowland forest (rain forest pollen) and Afromontane forest (Podocarpus pollen), and the position of the desert fringe (pollen of Caryophyllaceae, Chenopodiaceae and Amaranthaceae). High Cyperaceae pollen percentages in sediments from the last glacial period off the mouth of the river Congo suggest the presence of open swamps rather than savannah vegetation in the Congo Basin. Pollen from Restionaceae in combination with Stoebe-type pollen (probably from Elytropappus) indicates a possible northwards extension of winter rain vegetation during the last glacial period. The record of Rhizophora (mangrove) pollen is linked to erosion of the continental shelf and sea-level rise. Pollen influx is highest off river mouths (10-2000 grains year**-1 cm**-2), close to the coast (300-6000 grains year**-1 cm**-2), but is an order of magnitude lower at sites situated far from the continent (〈10 grains year**-1 cm**-2).
    Keywords: 175-1079A; 175-1084A; Benguela Current, South Atlantic Ocean; Center for Marine Environmental Sciences; Congo Fan; DRILL; Drilling/drill rig; GeoB6518-1; Gravity corer (Kiel type); Joides Resolution; Leg175; M47/3; MARUM; Meteor (1986); Ocean Drilling Program; ODP; SL
    Type: Dataset
    Format: application/zip, 3 datasets
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    DATA PANGAEA
  • 9
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    Relative abundance of dinoflagellate cysts in surface sediments and dinoflagellate counts from three sediment cores from the Atlantic sector of the Southern Ocean (2007)
    PANGAEA
    In:  Supplement to: Esper, Oliver; Zonneveld, Karin A F (2007): The potential of organic-walled dinoflagellate cysts for the reconstruction of past sea-surface conditions in the Southern Ocean. Marine Micropaleontology, 65(3-4), 185-212, https://doi.org/10.1016/j.marmicro.2007.07.002
    Details
    Publication Date: 2024-06-26
    Description: In this study we investigate the potential of organic-walled dinoflagellate cysts (dinocysts) as tools for quantifying past sea-surface temperatures (SST) in the Southern Ocean. For this purpose, a dinocyst reference dataset has been formed, based on 138 surface sediment samples from different circum-Antarctic environments. The dinocyst assemblages of these samples are composed of phototrophic (gonyaulacoid) and heterotrophic (protoperidinioid) species that provide a broad spectrum of palaeoenvironmental information. The relationship between the environmental parameters in the upper water column and the dinocyst distribution patterns of individual species has been established using the statistical method of Canonical Correspondence Analysis (CCA). Among the variables tested, summer SST appeared to correspond to the maximum variance represented in the dataset. To establish quantitative summer SST reconstructions, a Modern Analogue Technique (MAT) has been performed on data from three Late Quaternary dinocyst records recovered from locations adjacent to prominent oceanic fronts in the Atlantic sector of the Southern Ocean. These dinocyst time series exhibit periodic changes in the dinocyst assemblage during the last two glacial/interglacial-cycles. During glacial conditions the relative abundance of protoperidinioid cysts was highest, whereas interglacial conditions are characterised by generally lower cyst concentrations and increased relative abundance of gonyaulacoid cysts. The MAT palaeotemperature estimates show trends in summer SST changes following the global oxygen isotope signal and a strong correlation with past temperatures of the last 140,000 years based on other proxies. However, by comparing the dinocyst results to quantitative estimates of summer SSTs based on diatoms, radiolarians and foraminifer-derived stable isotope records it can be shown that in several core intervals the dinocyst-based summer SSTs appeared to be extremely high. In these intervals the dinocyst record seems to be highly influenced by selective degradation, leading to unusual temperature ranges and to unrealistic palaeotemperatures. We used the selective degradation index (kt-index) to determine those intervals that have been biased by selective degradation in order to correct the palaeotemperature estimates. We show that after correction the dinocyst based SSTs correspond reasonably well with other palaeotemperature estimates for this region, supporting the great potential of dinoflagellate cysts as a basis for quantitative palaeoenvironmental studies.
    Keywords: Agulhas Basin; ANT-IV/4; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/6; ANT-XVIII/5a; APSARA4; Atlantic Indik Ridge; AWI_Paleo; BC; Bounty Trough, Southwest Pacific; Box corer; Brazil Basin; Cape Basin; Central South Atlantic; ELT27; ELT27.030-PC; ELT29; ELT29.001-PC; ELT29.002-PC; ELT29.070-PC; ELT34; ELT34.006-PC; ELT34.007-PC; ELT34.009-PC; ELT34.011-PC; ELT36; ELT36.023-PC; ELT36.025-TC; ELT36.027-PC; ELT36.043-PC; ELT43; ELT43.005-PC; ELT44; ELT44.005-PC; ELT44.006-PC; ELT53; ELT53.022-PC; ELT53.023-PC; ELT53.025-PC; ELT55; ELT55.001-PC; ELT55.002-PC; ELT55.003-PC; ELT55.004-PC; ELT55.005-PC; ELT55.006-PC; ELT55.007-PC; ELT55.008-PC; ELT55.009-PC; ELT55.010-PC; Eltanin; GC; GeoB2001-1; GeoB2007-1; GeoB2008-1; GeoB2009-1; GeoB2011-1; GeoB2018-1; GeoB2019-2; GeoB2021-4; GeoB2022-3; GeoB3601-1; GeoB3602-2; GeoB3603-1; GeoB3604-4; GeoB3605-1; GeoB3809-1; GeoB3810-2; GeoB3812-2; GeoB6407-2; GeoB6409-2; GeoB6413-4; GeoB6414-1; GeoB6416-2; GeoB6417-2; GeoB6418-3; GeoB6419-2; GeoB6421-1; GeoB6422-5; GeoB6423-2; GeoB6425-1; GeoB6427-1; GeoB6429-1; Giant box corer; GKG; Gravity corer; Gravity corer (Kiel type); Indian Ocean; KAL; Kasten corer; KC029; KC032; KC046; KC064; KC073; KC075; KC078; KC081; KC083; KC084; KC090; KC095; KC098; KC100; KR88-01; KR88-02; KR88-03; KR88-04; KR88-07; KR88-08; KR88-09; KR88-13; KR88-15; KR88-16; KR88-18; KR88-25; KR88-29; KR88-30; M23/1; M34/1; M34/3; M46/4; Marion Dufresne (1972); Maud Rise; MD94-02; MD94-04; MD94-06; MD94-07; Meteor (1986); Meteor Rise; MIC; Mid Atlantic Ridge; MiniCorer; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PC; Piston corer; Polarstern; PS08; PS08/621; PS12; PS12/284; PS12/549; PS12/551; PS12/557; PS1459-4; PS1585-1; PS16; PS16/284; PS16/311; PS1650-1; PS1651-2; PS1654-1; PS1756-5; PS1768-8; PS18; PS18/238; PS2082-1; PS21 06AQANTX_4; PS22; PS22/899; PS22/902; PS22/947; PS22/973; PS2230-1; PS2366-1; PS2367-1; PS2372-1; PS2376-2; PS58; PS58/251-1; PS58/254-2; PS58/256-1; PS58/258-1; PS58/265-1; PS58/266-4; PS58/267-4; PS58/268-1; PS58/269-4; PS58/270-1; PS58/272-4; PS58/274-4; PS58/276-1; PS58/280-1; PS58/290-1; PS58/291-3; PS58/292-1; Q215; Q219; Q575; Q861; R657; S924; Shona Ridge; SL; South African margin; South Atlantic; South Atlantic Ocean; Southeast Pacific; Southern Cape Basin; South Pacific; South Pacific Ocean; TAS_67GC01; TAS_67GC18; TAS_67GC44; TAS_67GC45; TAS_67GC46; TAS_67GC47; TAS_67GC49; TAS_67GC50; TAS_67GC51; TAS_67PC02; TAS_67PC03; TAS_67PC04; U938; U950
    Type: Dataset
    Format: application/zip, 4 datasets
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    DATA PANGAEA
  • 10
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    Physical, chemical and biological oceanography from the Skagerrak Experiment (SKAGEX) (2007)
    PANGAEA
    In:  International Council for the Exploration of the Sea, Copenhagen
    Details
    Publication Date: 2024-06-26
    Description: A joint international investigation in the Skagerrak area, the Skagerrak Experiment (SKAGEX) was carried out from spring 1990 to spring 1991. Four field phases (SKAGEX I-IV) were carried out, and 17 research ships from 7 countries participated with the following objectives: - to identify and quantify the various water masses entering and leaving the Skagerrak Area, and their variations over time; - to investigate the mechanisms that drive the circulation in the area, and its links with biological processes; - to investigate the pathways of contaminants through the Skagerrak. The leader of the Project was B. Dybern; the ICES Data Centre acted as the project data centre, collating most of the oceanographic data from 2896 bottle/CTD profiles. This data set is a copy from the original data at ICES, published in 2007 via the information system PANGAEA.
    Keywords: Alexander von Humboldt; Argos; Argos90/11; Argos90/11_660; Argos90/11_661; Argos90/11_662; Argos90/11_663; Argos90/11_664; Argos90/11_665; Argos90/11_666; Argos90/11_667; Argos90/11_668; Argos90/11_669; Argos90/11_670; Argos90/11_671; Argos90/11_672; Argos90/11_673; Argos90/11_674; Argos90/11_675; Argos90/11_676; Argos90/11_677; Argos90/11_678; Argos90/11_679; Argos90/11_680; Argos90/11_681; Argos90/11_682; Argos90/11_683; Argos90/11_684; Argos90/11_685; Argos90/11_686; Argos90/11_687; Argos90/11_688; Argos90/11_689; Argos90/11_690; Argos90/11_691; Argos90/11_692; Argos90/11_693; Argos90/11_694; Argos90/11_695; Argos90/8; Argos90/8_380; Argos90/8_381; Argos90/8_382; Argos90/8_383; Argos90/8_384; Argos90/8_385; Argos90/8_386; Argos90/8_387; Argos90/8_388; Argos90/8_389; Argos90/8_390; Argos90/8_391; Argos90/8_392; Argos90/8_393; Argos90/8_394; Argos90/8_395; Argos90/8_396; Argos90/8_397; Argos90/8_398; Argos90/8_399; Argos90/8_400; Argos90/8_401; Argos90/8_402; Argos90/8_403; Argos90/8_404; Argos90/8_405; Argos90/8_406; Argos90/8_407; Argos90/8_408; Argos90/8_409; Argos90/8_410; Argos90/8_411; Argos90/8_412; Argos90/8_413; Argos90/8_414; Argos90/8_415; Argos90/8_416; Argos90/8_417; Argos90/8_418; Argos90/8_419; Argos90/8_420; Argos90/8_421; Argos90/8_422; Argos90/8_423; Argos90/8_424; Argos90/8_425; Argos90/8_426; Argos90/8_427; Argos90/8_428; Argos90/8_429; Argos90/8_430; Argos90/8_431; Argos90/8_432; Argos90/8_433; Argos90/8_434; Argos90/8_435; Argos90/8_436; Argos90/8_437; Argos90/8_438; Argos90/8_439; Argos90/8_440; Argos90/8_441; Argos90/8_442; Argos90/8_443; Argos90/8_444; Argos90/8_445; Argos90/8_446; Argos90/8_447; Argos90/8_448; Argos90/8_449; Argos90/8_450; Argos90/8_451; Argos90/8_452; Argos90/8_453; Argos90/8_454; Argos90/8_455; Argos90/8_456; Argos90/8_457; Argos90/8_458; Argos90/8_459; Argos90/8_460; Argos90/8_461; Argos90/8_462; Argos90/8_463; Argos90/8_464; Argos90/8_465; Argos90/8_466; Argos90/8_467; Argos90/8_468; Argos90/8_469; Argos90/8_470; Argos90/8_471; Argos90/8_472; Argos90/8_473; Argos90/8_474; Argos90/8_475; Argos90/8_476; Argos90/8_477; Argos90/8_478; Argos90/8_479; Argos90/8_480; Argos90/8_481; Argos90/8_482; Argos90/8_483; Argos90/8_484; Argos90/8_485; Argos90/8_486; Argos90/8_487; Argos90/8_488; Argos90/8_489; Argos90/8_490; Argos90/8_491; Argos90/8_492; Argos90/8_493; Argos90/8_494; Argos90/8_495; Argos90/8_496; Argos90/8_497; Argos90/8_498; Argos90/8_499; Argos90/8_500; Argos90/8_501; Argos90/8_502; Argos90/8_503; Argos90/8_504; Argos90/8_505; Argos90/8_506; Argos90/8_507; Argos90/8_508; Argos90/8_509; Argos90/8_510; Argos90/8_511; Argos90/8_512; Argos90/8_513; Argos90/8_514; Argos90/8_515; Argos90/8_516; Argos90/8_517; Argos90/8_518; Argos90/8_519; Argos90/8_520; Argos90/8_521; Argos90/8_522; Argos90/8_523; Argos90/8_524; Argos90/8_525; Argos90/8_526; Argos90/8_527; Argos90/8_528; Argos90/8_529; Argos90/8_530; Argos90/8_531; Argos90/8_532; Argos90/8_533; Argos90/8_534; Argos90/8_535; Argos90/8_536; Argos90/8_537; Argos90/8_538; Argos90/8_539; Argos90/8_540; Argos90/8_541; Argos90/8_542; Argos90/8_543; Argos90/8_544; Argos90/8_545; Argos90/8_546; Argos90/8_547; Argos90/8_548; Argos90/8_549; Argos90/8_550; Argos90/8_551; Argos90/8_G10-1; Argos90/8_G10-2; Argos90/8_G10-3; Argos90/8_G10-4; Argos90/8_G1-1; Argos90/8_G11-1; Argos90/8_G11-2; Argos90/8_G11-3; Argos90/8_G11-4; Argos90/8_G11-5; Argos90/8_G1-2; Argos90/8_G12-1; Argos90/8_G12-2; Argos90/8_G12-3; Argos90/8_G12-4; Argos90/8_G1-3; Argos90/8_G2-1; Argos90/8_G2-2; Argos90/8_G2-3; Argos90/8_G2-4; Argos90/8_G2-5; Argos90/8_G3-1; Argos90/8_G3-2; Argos90/8_G3-3; Argos90/8_G3-4; Argos90/8_G4-1; Argos90/8_G4-2; Argos90/8_G4-3; Argos90/8_G4-4; Argos90/8_G4-5; Argos90/8_G5-1; Argos90/8_G5-2; Argos90/8_G5-3; Argos90/8_G5-4; Argos90/8_G5-5; Argos90/8_G6-1; Argos90/8_G6-2; Argos90/8_G7-1; Argos90/8_G7-2; Argos90/8_G7-3; Argos90/8_G7-4; Argos90/8_G7-5; Argos90/8_G8-1; Argos90/8_G9-1; Argos90/8_G9-2; Argos90/8_G9-3; Argos90/8_G9-4; Argos91/1; Argos91/1_10; Argos91/1_11; Argos91/1_12; Argos91/1_13; Argos91/1_14; Argos91/1_15; Argos91/1_16; Argos91/1_17; Argos91/1_18; Argos91/1_19; Argos91/1_2; Argos91/1_20; Argos91/1_21; Argos91/1_22; Argos91/1_23; Argos91/1_24; Argos91/1_25; Argos91/1_26; Argos91/1_27; Argos91/1_28; Argos91/1_29; Argos91/1_3; Argos91/1_30; Argos91/1_31; Argos91/1_32; Argos91/1_33; Argos91/1_34; Argos91/1_35; Argos91/1_36; Argos91/1_37; Argos91/1_4; Argos91/1_5; Argos91/1_6; Argos91/1_7; Argos91/1_8; Argos91/1_9; Argos91/5; Argos91/5_221; Argos91/5_222; Argos91/5_223; Argos91/5_224; Argos91/5_225; Argos91/5_226; Argos91/5_227; Argos91/5_228; Argos91/5_229; Argos91/5_230; Argos91/5_231; Argos91/5_232; Argos91/5_233; Argos91/5_234; Argos91/5_235; Argos91/5_236; Argos91/5_237; Argos91/5_238; Argos91/5_239; Argos91/5_240; Argos91/5_241; Argos91/5_242; Argos91/5_243; Argos91/5_244; Argos91/5_245; Argos91/5_246; Argos91/5_247; Argos91/5_248; Argos91/5_249; Argos91/5_250; Argos91/5_251; Argos91/5_252; Argos91/5_253; Argos91/5_254; Argos91/5_255; Argos91/5_256; Argos91/5_257; Argos91/5_258; Argos91/5_259; Argos91/5_260; Argos91/5_261; Argos91/5_262; Argos91/5_263; Argos91/5_264; Argos91/5_265; Argos91/5_266; Argos91/5_267; Argos91/5_268; Argos91/5_269; Argos91/5_270; Argos91/5_271; Argos91/5_272; Argos91/5_273; Argos91/5_274; Argos91/5_E10; Argos91/5_E2; Argos91/5_E4; Argos91/5_E6; Argos91/5_E8-1; Argos91/5_E8-2; Argos91/5_F1; Argos91/5_F10; Argos91/5_F12-1; Argos91/5_F12-2; Argos91/5_F3; Argos91/5_F6; Argos91/5_F8; Argos91/5_G11; Argos91/5_G5; Argos91/5_G7; Argos91/5_G9; Argos91/5_H10; Argos91/5_H12; Argos91/5_H14; Argos91/5_H15; Argos91/5_H2; Argos91/5_H4; Argos91/5_H6; Argos91/5_H7; Argos91/5_H9; Arne Tiselius; Arnold Veimer; AT90/1; AT90/1_25; AT90/1_26; AT90/1_27; AT90/1_28; AT90/1_29; AT90/1_30; AT90/1_31; AT90/1_32; AT90/1_33; AT90/1_34; AT90/1_35; AT90/1_36; AT90/1_37; AT90/1_38; AT90/1_39; AT90/1_40; AT90/1_41; AT90/1_42; AT90/1_43; AT90/1_44; AT90/1_45; AT90/1_46; AT90/1_47; AT90/1_48; AT90/1_49; AT90/1_50; AT90/1_51; AT90/1_52; AT90/1_53; AT90/1_54; AT90/1_B1-1; AT90/1_B1-2; AT90/1_B1-3; AT90/1_B1-4; AT90/1_B1-5; AT90/1_B2-1; AT90/1_B2-2; AT90/1_B2-3; AT90/1_B2-4; AT90/1_B3-1; AT90/1_B3-2; AT90/1_B3-3; AT90/1_B3-4; AT90/1_B4-1; AT90/1_B4-2; AT90/1_B4-3; AT90/1_B4-4; AT90/1_B5-1; AT90/1_B5-2; AT90/1_B5-3; AT90/1_B5-4; AT90/1_B6-1; AT90/1_B6-2; AT90/1_B6-3; AT90/1_B6-4; AT90/1_B6-5; AT90/2; AT90/2_67; AT90/2_68; AT90/2_69; AT90/2_70; AT90/2_71; AT90/2_72; AT90/2_73; AT90/2_74; AT90/2_75; AT90/2_76; AT90/2_77; AT90/2_78; AT90/2_79; AT90/2_80; AT90/2_81; AT90/2_82; AT90/2_B0-1; AT90/2_B0-2; AT90/2_B1-1; AT90/2_B1-2; AT90/2_B2-1; AT90/2_B2-2; AT90/2_B3-1; AT90/2_B3-2; AT90/2_B4-1; AT90/2_B4-2; AT90/2_B5-1; AT90/2_B5-2; AT90/2_B6-1; AT90/2_B6-2; AT91/1; AT91/1_10; AT91/1_11; AT91/1_12; AT91/1_13; AT91/1_14; AT91/1_15; AT91/1_16; AT91/1_17; AT91/1_18; AT91/1_19; AT91/1_20; AT91/1_21; AT91/1_22; AT91/1_23; AT91/1_24; AT91/1_25; AT91/1_5; AT91/1_6; AT91/1_7; AT91/1_8; AT91/1_9; AT91/1_B0-1; AT91/1_B0-2; AT91/1_B1-1; AT91/1_B1-2; AT91/1_B2-1; AT91/1_B2-2; AT91/1_B3-1; AT91/1_B3-2; AT91/1_B4-1; AT91/1_B4-2; AT91/1_B5-1; AT91/1_B5-2; AT91/1_B6-1; AT91/1_B6-2; AT91/2; AT91/2_1; AT91/2_2; AT91/2_3; AT91/2_4; AT91/2_41; AT91/2_42; AT91/2_43; AT91/2_44; AT91/2_45; AT91/2_46; AT91/2_5; AT91/2_B1; AT91/2_B2; AT91/2_B3; AT91/2_B4; AT91/2_B5; AT91/2_B6; Atair; Atair90/6; Atair90/6_1001; Atair90/6_101; Atair90/6_1101; Atair90/6_1201; Atair90/6_1301; Atair90/6_1401; Atair90/6_1501; Atair90/6_1601; Atair90/6_1701; Atair90/6_1801; Atair90/6_1901; Atair90/6_2001; Atair90/6_201; Atair90/6_2101; Atair90/6_2201; Atair90/6_2301; Atair90/6_2401; Atair90/6_2501; Atair90/6_2601; Atair90/6_2701; Atair90/6_2801; Atair90/6_2901; Atair90/6_3001; Atair90/6_301; Atair90/6_3101; Atair90/6_3201; Atair90/6_3301; Atair90/6_3401; Atair90/6_3501; Atair90/6_3601; Atair90/6_3701; Atair90/6_3801; Atair90/6_3901; Atair90/6_4001; Atair90/6_401; Atair90/6_4101; Atair90/6_4201; Atair90/6_4301; Atair90/6_4401;
    Type: Dataset
    Format: application/zip, 68 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
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