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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Andreev, Andrei A; Manley, William F; Ingólfsson, Ólafur; Forman, Steven L (2001): Environmental changes on Yugorski Peninsula, Kara Sea, Russia, during the last 12,800 radiocarbon years. Global and Planetary Change, 31(1-4), 255-264, https://doi.org/10.1016/S0921-8181(01)00123-0
    Publication Date: 2024-07-05
    Description: New pollen and radiocarbon data from an 8.6-m coastal section, Cape Shpindler (69°43' N; 62°48' E), Yugorski Peninsula, document the latest Pleistocene and Holocene environmental history of this low Arctic region. Twelve AMS 14C dates indicate that the deposits accumulated since about 13,000 until 2000 radiocarbon years BP. A thermokarst lake formed ca. 13,000-12,800 years BP, when scarce arctic tundra vegetation dominated the area. By 12,500 years BP, a shallow lake existed at the site, and Arctic tundra with Poaceae, Cyperaceae, Salix, Saxifraga, and Artemisia dominated nearby vegetation. Climate was colder than today. Betula nana became dominant during the Early Preboreal period about 9500 years BP, responding to a warm event, which was one of the warmest during the Holocene. Decline in B. nana and Salix after 9500 years BP reflects a brief event of Preboreal cooling. A subsequent increase in Betula and Alnus fruticosa pollen percentages reflects amelioration of environmental conditions at the end of Preboreal period (ca. 9300 years BP). A decline in arboreal taxa later, with a dramatic increase in herb taxa, reflects a short cold event at about 9200 years BP. The pollen data reflect a northward movement of tree birch, peaking at the middle Boreal period, around 8500 years BP. Open Betula forest existed on the Kara Sea coast of the Yugorski Peninsula during the Atlantic period (8000-4500 years BP), indicating that climate was significantly warmer than today. Deteriorating climate around the Atlantic-Subboreal boundary (ca. 4500 years BP) is recorded by a decline in Betula percentages. Sedimentation slowed at the site, and processes of denudation and/or soil formation started at the beginning of the Subatlantic period, when vegetation cover on Yugorski Peninsula shifted to near-modern assemblages.
    Keywords: AWI_PerDyn; Cape Shpindler, Yugorski Peninsula, Russia; CS98-10; Geological profile sampling; GEOPRO; Permafrost Research (Periglacial Dynamics) @ AWI; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
    Publication Date: 2024-07-05
    Keywords: Alnus; Alnus fruticosa; Artemisia; Asteraceae; AWI_PerDyn; Betula sect. Albae; Betula sect. Nanae; Brassicaceae; Bryales; Cape Sabler, Taymyr Lake, Taymyr Peninsula, Krasnoyarsk, northern Russia; Caryophyllaceae; Chenopodiaceae; Cichoriaceae; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Ericales; Fabaceae; Geological profile sampling; GEOPRO; Indeterminata; Larix; Liliaceae; Lycopodium; Lycopodium alpinum; Lycopodium complanatum; Lycopodium pungens; Onagraceae; Papaver; Permafrost Research (Periglacial Dynamics) @ AWI; Pinus; Plantago; Poaceae; Polemonium; Polygonum aviculare-type; Polygonum bistorta-type; Polypodiaceae; Primulaceae; Ranunculaceae; Rosaceae; Rubus chamaemorus; Rumex/Oxyria; Salix; SAO4; Saxifraga; Scrophulariaceae; Sphagnum; Valerianaceae
    Type: Dataset
    Format: text/tab-separated-values, 560 data points
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  • 3
    Publication Date: 2024-07-05
    Keywords: Abies; Akademik Boris Petrov; Alnus fruticosa; Anthemis-type; Armeria maritima-type; Artemisia; Asteraceae; Betula; BP99; BP99-04/06; Brassicaceae; Cariophyllaceae; cf. Carpinus betulus; cf. Potamogeton; cf. Pterocarya; Chenopodiaceae; Cirsium; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Drosera; Ephedra distachya-type; Epilobium-type; Ericaceae; Filipendula; Galium-type; GC; Gentianaceae; Gravity corer; Helianthemum; Ilex-type; Illecebrum verticillatum; Juniperus-type; Larix; Limonium; Lycopodiaceae; Lycopodium spike; Menyanthes trifoliata; Myriophyllum verticillatum; Nymphaea; Onagraceae; Picea obovata; Pinguicula; Pinus diploxylon; Pinus haploxylon; Plantago; Poaceae; Polemonium; Pollen, reworked; Pollen indeterminata; Polypodiales; Populus; Quercus; Ranunculaceae; Ribes rubrum-type; Rumex; Salix; Saxifraga; Selaginella selaginoides; Serratula-type; Siberian River Run-Off; SIRRO; Sphagnum; Thalictrum; Tilia; Typha angustifolia; Typha latifolia; Ulmus; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 3172 data points
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  • 4
    Publication Date: 2024-07-05
    Keywords: Abies; Alnus fruticosa; Apiaceae; Artemisia; Asteraceae; AWI_PerDyn; Betula sect. Albae; Betula sect. Nanae/Fruticosae; Botrychium; Botryococcus; Brassicaceae; Bryales; Calluna; Cape Sabler, Taymyr Lake, Taymyr Peninsula, Krasnoyarsk, northern Russia; Caryophyllaceae; Castilleja; Chenopodiaceae; Cichoriaceae; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Dryas; Epilobium; Equisetum; Ericales undifferentiated; Fabaceae; Gentianaceae; Geological profile sampling; GEOPRO; Helianthemum-type; Indeterminata; Juniperus; Lamiaceae; Larix; Ledum; Liliaceae; Lloydia; Lycopodium complanatum; Lycopodium selago; Lycopodium sp.; Menyanthes; Nuphar; Nymphaea; Nymphoides; Oxyria; Papaver; Pediastrum kawraiskyi; Pediastrum sp.; Pedicularis; Permafrost Research (Periglacial Dynamics) @ AWI; Picea; Pinus subgen. Haploxylon; Pinus sylvestris; Poaceae; Polemonium; Polipodiaceae; Pollen, redeposited; Polygonum bistorta; Polypodium; Potamogeton; Primulaceae; Ranunculaceae; Rosaceae undifferentiated; Rumex; Salix; Sanguisorba officinalis; SAO1; Saxifraga nivalis-type; Saxifraga undifferentiated; Scrophulariaceae undifferentiated; Selaginella rupestris; Selaginella selaginoides; Sieversia-type; Sparganium-type; Sphagnum; Thalictrum; Valerianaceae; Varia
    Type: Dataset
    Format: text/tab-separated-values, 3550 data points
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  • 5
    Publication Date: 2024-07-05
    Keywords: Alnus; Alnus fruticosa; Androsace; Apiaceae; Artemisia; Asteraceae; AWI_PerDyn; AWI Arctic Land Expedition; Betula sect. Albae; Betula sect. Nanae; Boraginaceae; Botrychium; Botryococcus; Brassicaceae; Bryales; Caryophyllaceae; Chenopodiaceae; Chichoriaceae; COMPCORE; Composite Core; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Dipsacaceae; Dryas; Ephedra distachya; Epilobium; Equisetum; Ericales undifferentiated; Fabaceae; Gentianaceae; Hippophae rhamnoides; Huperzia selago-type; Indeterminata; Juniperus; Lamiaceae; Larix; Ledum; Liliaceae; Lycopodium annotinum-type; Lycopodium complanatum-type; Lycopodium inundatum; Lycopodium sp.; Papaver; Pediastrum; Permafrost Research (Periglacial Dynamics) @ AWI; PG1228; Picea obovata; Pinus sibirica; Pinus sylvestris; Plantago; Poaceae; Polemonium; Pollen, redeposited; Polygonum; Polypodiaceae; Populus; Primulaceae; Ranunculaceae; Rosaceae undifferentiated; Rubiaceae; RU-Land_1995_Taymyr; Rumex/Oxyria-type; Salix; Saxifragaceae; Scrophulariaceae; Selaginella selaginoides; Sparganium/Potamogeton-type; Sphagnum; Taymyr; Taymyr95; Labaz_Lake_Expedition; Thalictrum; Valeriana
    Type: Dataset
    Format: text/tab-separated-values, 5579 data points
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  • 6
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    PANGAEA
    In:  Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky Universität Oldenburg, Germany
    Publication Date: 2024-07-02
    Keywords: Aussenjade1; Biogeochemistry of Tidal Flats; CTD; CTD/Rosette; CTD-RO; DEPTH, water; Filtration; Graphite furnace atomic absorption spectrometer (GF-AAS); Manganese; Salinity; Senckenberg; Suspended matter, particulate/solids; WATT; WATT1998
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Ravizza, Gregory E; Peucker-Ehrenbrink, Bernhard (2003): Chemostratigraphic Evidence of Deccan Volcanism from the Marine Osmium Isotope Record. Science, 302(5629), 1392-1395, https://doi.org/10.1126/science.1089209
    Publication Date: 2024-07-02
    Description: Continental flood basalt (CFB) volcanism is hypothesized to have played a causative role in global climate change and mass extinctions. Uncertainties associated with radiometric dating preclude a clear chronological assessment of the environmental consequences of CFB volcanism. Our results document a 25% decline in the marine 187Os/188Os record that predates the Cretaceous-Tertiary boundary (KTB) and coincides with late Maastrichtian warming. We argue that this decline provides a chemostratigraphic marker of Deccan volcanism and thus constitutes compelling evidence that the main environmental consequence of Deccan volcanism was a transient global warming event of 3° to 5°C that is fully resolved from the KTB mass extinction.
    Keywords: 25-245; 74-525A; 86-577_Site; AGE; COMPCORE; Composite Core; Deep Sea Drilling Project; Depth, relative; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Indian Ocean//BASIN; Leg25; Leg74; Leg86; Negative-thermal ionization mass spectrometry (N-TIMS); North Pacific; Osmium; Osmium-187/Osmium-188, error; Osmium-187/Osmium-188 ratio; Sample code/label; South Atlantic/CREST
    Type: Dataset
    Format: text/tab-separated-values, 109 data points
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  • 8
    Publication Date: 2024-07-01
    Keywords: 30; 31; 33; 35; AGSO Cruise 147; BC; Box corer; Campbell Plateau; Counting 〉150 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; ELT36; ELT36.001-PH; ELT36.005-PC; ELT36.006-PC; ELT53; ELT53.013-PC; ELT53.014-PC; Eltanin; Event label; Foraminifera, planktic; Foraminifera, planktic indeterminata; GC; Globigerina bulloides; Globigerina falconensis; Globigerina quinqueloba; Globigerinella aequilateralis; Globigerinella calida; Globigerinita glutinata; Globigerinita uvula; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia scitula; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Gravity corer; IMAGES III - IPHIS; Latitude of event; Longitude of event; Marion Dufresne (1995); MD106; MD972106G; MD97-2106G; MD972108BX; MD97-2108BX; MD972110G; MD97-2110G; Neogloboquadrina dutertrei; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Orbulina universa; PC; Piston corer; Rig Seismic; RS147; RS147-GC14; RS147-GC17; RS147-GC20; RS147-GC31; SO136; SO136_147BX; SO136_153BX; SO136_161BX; SO136_165BX; Sonne; South Tasman Rise; Tasman Sea; TASQWA
    Type: Dataset
    Format: text/tab-separated-values, 334 data points
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  • 9
    Publication Date: 2024-07-01
    Keywords: Age, 14C milieu/reservoir corrected; Age, dated; Age, dated standard deviation; Amundsen Basin; ARK-VIII/3; AWI_Paleo; Calendar age; Comment; Depth, reference; DEPTH, sediment/rock; Elevation of event; Event label; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Latitude of event; Lomonosov Ridge, Arctic Ocean; Longitude of event; Makarov Basin; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/157; PS19/165; PS19/181; PS19/186; PS19 ARCTIC91; PS2163-1; PS2170-4; PS2180-1; PS2185-3
    Type: Dataset
    Format: text/tab-separated-values, 75 data points
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  • 10
    Publication Date: 2024-07-01
    Keywords: Amundsen Basin; ARK-VIII/3; AWI_Paleo; DEPTH, sediment/rock; Event label; Lignin; Lomonosov Ridge, Arctic Ocean; Long-chain n-alkanes, C27+C29+C31, per unit mass total organic carbon; Long-chain n-alkanes, C27H56+C29H60+C31H64 per unit sediment mass; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/165; PS19/186; PS19 ARCTIC91; PS2170-4; PS2185-4
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 11
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    PANGAEA
    In:  Supplement to: Ragueneau, Olivier; Gallinari, Morgane; Corrin, Lydie; Grandel, Sibylle; Hall, Per; Hauvespre, Anne; Lampitt, Richard Stephen; Rickert, Dirk; Ståhl, Henrik; Tengberg, Anders; Witbaard, Rob (2001): The benthic silica cycle in the Northeast Atlantic: annual mass balance, seasonality, and importance of non-steady-state processes for the early diagenesis of biogenic opal in deep-sea sediments. Progress in Oceanography, 50(1-4), 171-200, https://doi.org/10.1016/S0079-6611(01)00053-2
    Publication Date: 2024-07-01
    Description: Within the framework of the EU-funded BENGAL programme, the effects of seasonality on biogenic silica early diagenesis have been studied at the Porcupine Abyssal Plain (PAP), an abyssal locality located in the northeast Atlantic Ocean. Nine cruises were carried out between August 1996 and August 1998. Silicic acid (DSi) increased downward from 46.2 to 213 µM (mean of 27 profiles). Biogenic silica (BSi) decreased from ca. 2% near the sediment-water interface to 〈1% at depth. Benthic silicic acid fluxes as measured from benthic chambers were close to those estimated from non-linear DSi porewater gradients. Some 90% of the dissolution occurred within the top 5.5 cm of the sediment column, rather than at the sediment-water interface and the annual DSi efflux was close to 0.057 mol Si/m**2/yr. Biogenic silica accumulation was close to 0.008 mol Si/m**2/yr and the annual opal delivery reconstructed from sedimentary fluxes, assuming steady state, was 0.065 mol Si/m**2/yr. This is in good agreement with the mean annual opal flux determined from sediment trap samples, averaged over the last decade (0.062 mol Si/m**2/yr). Thus ca. 12% of the opal flux delivered to the seafloor get preserved in the sediments. A simple comparison between the sedimentation rate and the dissolution rate in the uppermost 5.5 cm of the sediment column suggests that there should be no accumulation of opal in PAP sediments. However, by combining the BENGAL high sampling frequency with our experimental results on BSi dissolution, we conclude that non-steady state processes associated with the seasonal deposition of fresh biogenic particles may well play a fundamental role in the preservation of BSi in these sediments. This comes about though the way seasonal variability affects the quality of the biogenic matter reaching the seafloor. Hence it influences the intrinsic dissolution properties of the opal at the seafloor and also the part played by non-local mixing events by ensuring the rapid transport of BSi particles deep into the sediment to where saturation is reached.
    Keywords: 12925-008; 12926-002; 12930-040; 12930-045; 12930-075; 12930-082; 12930-087; 13077-018; 13077-021; 13077-035; 13077-057; 13078-019; 13200-012; 13200-024; 13200-026; 13200-032; 13200-059; 13200-074; 13201-005; 13368-040; 362; 54301-002; 54301-010; 54301-023; ALBEX lander; Bengal; BENGAL; Benthic Biology and Geochemistry of a North-eastern Atlantic Abyssal Locality; CH135; Challenger; D222/1; D222/2; D226; D229; D231; D236; DI236_11-1; Discovery (1962); GBGL; GBGL-01; GBGL-02; Göteborg lander; M36/6; M36/6_MC33; M42/2; M42/2_365; M42/2_367; M42/2_377-6; M42/2_381; M42/2_397-1; M42/2_422; M42/2_425; M42/2_432-1; M42/2_433; M42/2_MC2; M42/2_MC28; M42/2_MC30; M42/2_MC32; M42/2_MC34; M42/2_MC5; M42/2_MC9; MCB57; MCS; Meteor (1986); MUC; MultiCorer; MultiCorer, small; MultiCorer Barnett pattern (12-57); NIOZL
    Type: Dataset
    Format: application/zip, 33 datasets
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  • 12
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    PANGAEA
    In:  Supplement to: Volkmann, Renate; Mensch, Manfred (2001): Stable isotope composition (d18O, d13C) of living planktic foraminifers in the outer Laptev Sea and Fram Strait. Marine Micropaleontology, 42(3-4), 163-188, https://doi.org/10.1016/S0377-8398(01)00018-4
    Publication Date: 2024-07-01
    Description: The upper water column in the Fram Strait and the outer Laptev Sea was sampled for water column isotopes and living planktic foraminifer species Neogloboquadrina pachyderma (sinistral coiling) (Ehrenberg), 1861 and Turborotalita quinqueloba (Natland),1938. Their shell delta18O and delta13C values are compared to water oxygen and dissolved inorganic carbon isotope data to determine the environmental influence on the foraminifers' isotopic ratio. Major controls on the oxygen isotope composition of both species are the shallow depth habitat under permanent ice coverage, the low salinity surface layer, and the rate of metabolic activity. None of the specimens precipitated its shell in isotopic equilibrium with the ambient sea water. They are all depleted in 13C and 18O, attributed to a species-specific vital effect. For nonencrusted N. pachyderma (sin.) in the 125-250 µm size class, this vital effect amounts to 1.3 per mil in delta18O and 2.0 per mil in delta13C. It increases to higher values in waters under permanent ice cover. T. quinqueloba reveals a mean vital effect of about 1.3 per mil in delta18O and 2.6 per mil in delta13C. The general isotopic trends are similar for N. pachyderma (sin.) and T. quinqueloba. Differences in the species' isotope ratio at the same sites are caused by different calcification depths and metabolic activity. The oxygen isotope composition of N. pachyderma (sin.) shows a relationship to salinity measurements and indicates that it is a good quantitative proxy for salinity reconstructions, while no relationship exists in this region between N. pachyderma (sin.) oxygen isotopes and water temperature.
    Keywords: Arctic Ocean; ARK-XI/1; ARK-XIII/2; AWI_Paleo; Barents Sea; CTD/Rosette; CTD-RO; East Greenland continental slope; gcmd1; Laptev Sea; MSN; Multiple opening/closing net; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS36; PS36/021-1; PS36/022-1; PS36/023-1; PS36/024-1; PS36/024-4; PS36/025-1; PS36/031-1; PS36/032-1; PS36/033-1; PS36/044-1; PS36/047-1; PS44; PS44/039-1; PS44/052-1; PS44/058-1; PS44/060-1; PS44/063-1; PS44/064-1; PS44/069-1; PS44/072; PS44/072-2; PS44/074-1; PS44/076-1; PS44/077-1; PS44/079-1; PS44/084-1; PS44/089-1; PS44/091-1; PS44/094-1; PS44/096-1; PS44/098-1; PS44/099-1; W Spitzbergen; Yermak Plateau
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 13
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    PANGAEA
    In:  Supplement to: Steinke, Stephan; Kienast, Markus; Pflaumann, Uwe; Weinelt, Mara; Stattegger, Karl (2001): A High-Resolution Sea-Surface Temperature Record from the Tropical South China Sea (16,500–3000 yr B.P.). Quaternary Research, 55(3), 352-362, https://doi.org/10.1006/qres.2001.2235
    Publication Date: 2024-07-01
    Description: The timing and magnitude of sea-surface temperature (SST) changes in the tropical southern South China Sea (SCS) during the last 16,500 years have been reconstructed on a high-resolution, 14C-dated sediment core using three different foraminiferal transfer functions (SIMMAX28, RAM, FP-12E) and geochemical (Uk'37) SST estimates. In agreement with CLIMAP reconstructions, both the FP-12E and the Uk'37 SST estimates show an average late glacial-interglacial SST difference of 2.0°C, whereas the RAM and SIMMAX28 foraminiferal transfer functions show only a minor (0.6°C) or no consistent late glacial-interglacial SST change, respectively. Both the Uk'37 and the FP-12E SST estimates, as well as the planktonic foraminiferal delta18O values, indicate an abrupt warming (ca. 1°C in 〈200 yr) at the end of the last glaciation, synchronous (within dating uncertainties) with the Bølling transition as recorded in the Greenland Ice Sheet Project 2 (GISP2) ice core, whereas the RAM-derived deglacial SST increase appears to lag during this event by ca. 500 yr. The similarity in abruptness and timing of the warming associated with the Bølling transition in Greenland and the southern SCS suggest a true synchrony of the Northern Hemisphere warming at the end of the last glaciation. In contrast to the foraminiferal transfer function estimates that do not indicate any consistent cooling associated with the Younger Dryas (YD) climate event in the tropical SCS, the Uk'37 SST estimates show a cooling of ca. 0.2-0.6°C compared to the Bølling-Allerød period. These Uk'37 SST estimates from the southern SCS argue in favor of a Northern Hemisphere-wide, synchronous cooling during the YD period.
    Keywords: GIK/IfG; GIK18287-3; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; SL; SO115; SO115_40; Sonne; SUNDAFLUT; Sunda Shelf
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 14
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    PANGAEA
    In:  Supplement to: Knies, Jochen; Vogt, Christoph (2003): Freshwater pulses in the eastern Arctic Ocean during Saalian and Early Weichselian ice-sheet collapse. Quaternary Research, 60(3), 243-251, https://doi.org/10.1016/j.yqres.2003.07.008
    Publication Date: 2024-07-01
    Description: Improved multiparameter records from the northern Barents Sea margin show two prominent freshwater pulses into the Arctic Ocean during MIS 5 that significantly disturbed the regional oceanic regime and probably affected global climate. Both pulses are associated with major iceberg-rafted debris (IRD) events, revealing intensive iceberg/sea ice melting. The older meltwater pulse occurred near the MIS 5/6 boundary (~131,000 yr ago); its ~2000 year duration and high IRD input accompanied by high illite content suggest a collapse of large-scale Saalian Glaciation in the Arctic Ocean. Movement of this meltwater with the Transpolar Drift current into the Fram Strait probably promoted freshening of Nordic Seas surface water, which may have increased sea-ice formation and significantly reduced deep-water formation. A second pulse of freshwater occurred within MIS 5a (~77,000 yr ago); its high smectite content and relatively short duration is possibly consistent with sudden discharge of Early Weichselian ice-dammed lakes in northern Siberia as suggested by terrestrial glacial geologic data. The influence of this MIS 5a meltwater pulse has been observed at a number of sites along the Transpolar Drift, through Fram Strait, and into the Nordic Seas; it may well have been a trigger for the North Atlantic cooling event C20.
    Keywords: ARK-VIII/2; AWI_Paleo; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/112; PS19 EPOS II; PS2138-1; Quaternary Environment of the Eurasian North; QUEEN; SL; Svalbard
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 15
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    PANGAEA
    In:  Supplement to: Sauter, Eberhard-Jürgen; Schlüter, Michael; Suess, Erwin (2001): Organic carbon flux and remineralization in surface sediments from the northern North Atlantic derived from pore-water oxygen microprofiles. Deep Sea Research Part I: Oceanographic Research Papers, 48(2), 529-553, https://doi.org/10.1016/S0967-0637(00)00061-3
    Publication Date: 2024-07-01
    Description: Organic carbon fluxes through the sediment/water interface in the high-latitude North Atlantic were calculated from oxygen microprofiles. A wire-operated in situ oxygen bottom profiler was deployed, and oxygen profiles were also measured onboard (ex situ). Diffusive oxygen fluxes, obtained by fitting exponential functions to the oxygen profiles, were translated into organic carbon fluxes and organic carbon degradation rates. The mean Corg input to the abyssal plain sediments of the Norwegian and Greenland Seas was found to be 1.9 mg C/m**2/d. Typical values at the seasonally ice-covered East Greenland continental margin are between 1.3 and 10.9 mg C/m**2/d (mean 3.7 mg C/m**2/d), whereas fluxes on the East Greenland shelf are considerably higher, 9.1-22.5 mg C/m**2/d. On the Norwegian continental slope Corg fluxes of 3.3-13.9 mg C/m**2/d (mean 6.5 mg C/m**2/d) were found. Fluxes are considerably higher here compared to stations on the East Greenland slope at similar water depths. By repeated occupation of three sites off southern Norway in 1997 the temporal variability of diffusive O2 fluxes was found to be quite low. The seasonal signal of primary and export production from the upper water column appears to be strongly damped at the seafloor. Degradation rates of 0.004-1.1 mg C/cm**3/a at the sediment surface were calculated from the oxygen profiles. First-order degradation constants, obtained from Corg degradation rates and sediment organic carbon content, are in the range 0.03-0.6/a. Thus, the corresponding mean lifetime of organic carbon lies between 1.7 and 33.2 years, which also suggests that seasonal variations in Corg flux are small. The data presented here characterize the Norwegian and Greenland Seas as oligotrophic and relatively low organic carbon deep-sea environments.
    Keywords: 12; 13; 14; 16; 20; 25; 26; 30; ARK-X/1; ARK-XI/2; ARK-XIII/1b; Giant box corer; GKG; Global Environmental Change: The Northern North Atlantic; M36/3; M36/3_201; M36/3_246-2; M36/3_249-2; Meteor (1986); MOOR; Mooring; MUC; MULT; MultiCorer; Multiple investigations; North Greenland Sea; Norwegian continental margin; O2PRO; Oxygen profiler; Polarstern; PS31; PS31/007-4; PS31/014-13; PS31/017-8; PS31/089-5; PS31/092-1; PS37; PS37/012; PS37/013; PS37/014; PS37/016; PS37/020; PS37/025; PS37/026; PS37/030; PS44; PS44/022-4; PS44/023-5; SFB313; SVT12; SVT14; SVT15; SVT8; Voering Plateau; VP6
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 16
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    PANGAEA
    In:  Supplement to: Diekmann, Bernhard; Fütterer, Dieter K; Grobe, Hannes; Hillenbrand, Claus-Dieter; Kuhn, Gerhard; Michels, Klaus; Petschick, Rainer; Pirrung, Michael (2004): Terrigenous sediment supply in the polar to temperate South Atlantic: land-ocean links of environmental changes during the late Quaternary. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budget and Current Systems. Springer-Verlag, Berlin, Heidelberg, New York, 375-399, hdl:10013/epic.15597.d001
    Publication Date: 2024-07-01
    Description: Terrigenous sediment parameters in modern sea-bottom samples and sediment cores of the South Atlantic are used to infer variations in detrital sources and modes of terrigenous sediment supply in response to environmental changes through the late Quaternary climate cycles. Massaccumulation rates of terrigenous sediment and fluxes of ice-rafted detritus are discussed in terms of temporal variations in detrital sediment input from land to sea. Grain-size parameters ofterrigenous mud document the intensity of bottom-water circulation, whereas clay-mineral assemblages constrain the sources and marine transport routes of suspended fine-grained particulates, controlled by the modes of sediment input and patterns of ocean circulation. The results suggest low-frequency East Antarctic ice dynamics with dominant 100-kyr cycles and high rates of Antarctic Bottom Water formation and iceberg discharge during interglacial times. In contrast, the more subpolar ice masses of the Antarctic Peninsula also respond to short-term climate variability with maximum iceberg discharges during glacial terminations related to the rapid disintegration of advanced ice masses. In the northern Scotia Sea, increased sediment supply from southern South America points to extended ice masses in Patagonia during glacial times. In the southeastern South Atlantic, changes in regional ocean circulation are linked to global thermohaline ocean circulation and are in phase with northern-hemispheric processes of ice build-up and associated formation of North Atlantic Deep Water, which decreased during glacial times and permitted a wider extension of southern-source water masses in the study area.
    Keywords: Agulhas Basin; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-VIII/6; ANT-X/5; ANT-XI/2; ANT-XI/4; Atlantic Ridge; AWI_Paleo; Gravity corer (Kiel type); KL; Lazarev Sea; Meteor Rise; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS12; PS12/248; PS1575-1; PS16; PS16/271; PS16/278; PS16/284; PS16/311; PS16/321; PS16/345; PS16/534; PS1752-1; PS1754-1; PS1756-5; PS1768-8; PS1772-8; PS1778-5; PS18; PS18/238; PS1821-6; PS2082-1; PS2082-3; PS22/773; PS22/817; PS22 06AQANTX_5; PS2278-3; PS2319-1; PS2495-3; PS2498-1; PS2515-3; PS2564-3; PS28; PS28/293; PS28/304; PS28/378; PS30; PS30/048; Scotia Sea; Scotia Sea, southwest Atlantic; Shona Ridge; SL; South Atlantic; South Atlantic Ocean; South Orkney
    Type: Dataset
    Format: application/zip, 16 datasets
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  • 17
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    PANGAEA
    In:  Supplement to: Bauch, Henning A; Erlenkeuser, Helmut; Spielhagen, Robert F; Struck, Ulrich; Matthiessen, Jens; Thiede, Jörn; Heinemeier, Jan (2001): A multiproxy reconstruction of the evolution of deep and surface waters in the subarctic Nordic seas over the last 30,000 years. Quaternary Science Reviews, 20(4), 659-678, https://doi.org/10.1016/S0277-3791(00)00098-6
    Publication Date: 2024-07-01
    Description: On the basis of various lithological, mircopaleontological and isotopic proxy records covering the last 30,000 calendar years (cal kyr) the paleoenvironmental evolution of the deep and surface water circulation in the subarctic Nordic seas was reconstructed for a climate interval characterized by intensive ice-sheet growth and subsequent decay on the surrounding land masses. The data reveal considerable temporal changes in the type of thermohaline circulation. Open-water convection prevailed in the early record, providing moisture for the Fennoscandian-Barents ice sheets to grow until they reached the shelf break at ~26 cal. kyr and started to deliver high amounts of ice-rafted debris (IRD) into the ocean via melting icebergs. Low epibenthic delta18O values and small-sized subpolar foraminifera observed after 26 cal. kyr may implicate that advection of Atlantic water into the Nordic seas occurred at the subsurface until 15 cal. kyr. Although modern-like surface and deep-water conditions first developed at ~13.5 cal. kyr, thermohaline circulation remained unstable, switching between a subsurface and surface advection of Atlantic water until 10 cal. kyr when IRD deposition and major input of meltwater ceased. During this time, two depletions in epibenthic delta13C are recognized just before and after the Younger Dryas indicating a notable reduction in convectional processes. Despite an intermittent cooling at ~8 cal. kyr, warmest surface conditions existed in the central Nordic seas between 10 and 6 cal. kyr. However, already after 7 cal. kyr the present day situation gradually evolved, verified by a strong water mass exchange with the Arctic Ocean and an intensifying deep convection as well as surface temperature decrease in the central Nordic seas. This process led to the development of the modern distribution of water masses and associated oceanographic fronts after 5 cal. kyr and, eventually, to today's steep east-west surface temperature gradient. The time discrepancy between intensive vertical convection after 5 cal. kyr but warmest surface temperatures already between 10 and 6 cal. kyr strongly implicates that widespread postglacial surface warming in the Nordic seas was not directly linked to the rates in deep-water formation.
    Keywords: ARK-II/4; ARK-II/5; Fram Strait; GEOMAR; Giant box corer; GIK23230-1 PS05/416; GIK23230-2 PS05/416; GIK23243-1 PS05/431; GKG; GLAMAP; Gravity corer (Kiel type); Helmholtz Centre for Ocean Research Kiel; Norwegian Sea; Polarstern; PS05; PS1230-1; PS1230-2; PS1243-1; SL
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 18
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    PANGAEA
    In:  Supplement to: Lamy, Frank; Hebbeln, Dierk; Röhl, Ursula; Wefer, Gerold (2001): Holocene rainfall variability in southern Chile: a marine record of latitudinal shifts of the Southern Westerlies. Earth and Planetary Science Letters, 185(3-4), 369-382, https://doi.org/10.1016/S0012-821X(00)00381-2
    Publication Date: 2024-07-01
    Description: Geochemical and clay mineral parameters of a high accumulation marine sediment core from the Chilean continental slope (41°S) provide a 7700 yr record of rainfall variability in southern Chile related to the position of the Southern Westerlies. We especially use the iron content, measured with a time-resolution of ca. 10 yr on average, of 14C-accelerator mass spectrometry dated marine sediments as a proxy for the relative input of iron-poor Coastal Range and iron-rich Andean source rocks. Variations in this input are most likely induced by rainfall changes in the continental hinterland of the core position. Based on these interpretations, we find a pronounced rainfall variability on multi-centennial to millennial time-scales, superimposed on generally more arid conditions during the middle Holocene (7700 to 4000 cal yr B.P.) compared to the late Holocene (4000 to present). This variability and thus changes in the position of the Southern Westerlies are first compared to regional terrestrial paleoclimate data-sets from central and southern Chile. In order to derive possible wider implications and forcing mechanisms of the Holocene latitudinal shifts of the Southern Westerlies, we then compare our data to ice-core records from both tropical South America and coastal Antarctica. These records show similar bands of variability centered at ca. 900 and 1500 yr. Comparisons of band pass filters suggest a close connection of shifts of the Southern Westerlies to changes within the tropical climate system. The correlation to climate conditions in coastal Antarctica shows a more complicated picture with a phase shift at the beginning of the late Holocene coinciding with the onset of the modern state of El Niño-Southern Oscillation system. The presented data provide further evidence that the well known millennial-scale climate variability during the last glacial continued throughout the Holocene.
    Keywords: CHIPAL; GeoB; GeoB3313-1; Geosciences, University of Bremen; Gravity corer (Kiel type); SL; SO102/1; Sonne; South-East Pacific; XRF core scanner
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 19
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    PANGAEA
    In:  Supplement to: Nørgaard-Pedersen, Niels; Spielhagen, Robert F; Erlenkeuser, Helmut; Grootes, Pieter Meiert; Heinemeier, Jan; Knies, Jochen (2003): Arctic Ocean during the Last Glacial Maximum: atlantic and polar domains of surface water mass distribution and ice cover. Paleoceanography, 18(3), 1063, https://doi.org/10.1029/2002PA000781
    Publication Date: 2024-07-01
    Description: On the basis of 52 sediment cores, analyzed and dated at high resolution, the paleoceanography and climate of the Last Glacial Maximum (LGM) were reconstructed in detail for the Fram Strait and the eastern and central Arctic Ocean. Sediment composition and stable isotope data suggest three distinct paleoenvironments: (1) a productive region in the eastern to central Fram Strait and along the northern Barents Sea continental margin characterized by Atlantic Water advection, frequent open water conditions, and occasional local meltwater supply and iceberg calving from the Barents Sea Ice Sheet; (2) an intermediate region in the southwestern Eurasian Basin (up to 84-85°N) and the western Fram Strait characterized by subsurface Atlantic Water advection and recirculation, a moderately high planktic productivity, and a perennial ice cover that breaks up only occasionally; and (3) a central Arctic region (north of 85°N in the Eurasian Basin) characterized by a low-salinity surface water layer and a thick ice cover that strongly reduces bioproduction and bulk sedimentation rates. Although the total inflow of Atlantic Water into the Arctic Ocean may have been reduced during the LGM, its impact on ice coverage and halocline structure in the Fram Strait and southwestern Eurasian Basin was strong.
    Keywords: 41; Amundsen Basin; Antarctic Ocean; Arctic Ocean; ARK-II/4; ARK-III/3; ARK-IV/3; ARK-IX/3; ARK-IX/4; ARK-VII/1; ARK-VIII/2; ARK-VIII/3; ARK-XIII/2; ARK-XIII/3; Barents Sea; Fram-I; FramI/4; FramI/7; Fram Strait; Gakkel Ridge, Arctic Ocean; GC; Giant box corer; GIK21294-4 PS07/584; GIK21295-4 PS07/586; GIK21297-4 PS07/588; GIK21308-3 PS07/601; GIK21314-3 PS07/608; GIK21527-10 PS11/371-10; GIK21528-7 PS11/372-7; GIK21533-3 PS11/412; GIK21535-5 PS11/430-5; GIK21535-8 PS11/430-8; GIK21894-7 PS17/069; GIK21906-1 PS17/081; GIK21906-2 PS17/081; GIK23230-1 PS05/416; GKG; Glacial Atlantic Ocean Mapping; GLAMAP; GLAMAP2000; Gravity corer; Gravity corer (Kiel type); Greenland Sea; Ice drift station; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Makarov Basin; Morris Jesup Rise; MUC; MultiCorer; Nansen Basin; Northeast Greenland; NP90-12; NP90-36; NP90-39; OD-009-11; OD-010-04; OD-031-03; OD-036-04; OD-041-04; Oden; ODEN-96; Polarstern; PS05; PS07; PS11; PS1230-1; PS1294-4; PS1295-4; PS1297-4; PS1308-3; PS1314-3; PS1527-10; PS1528-7; PS1533-3; PS1535-5; PS1535-8; PS17; PS1894-7; PS19/084; PS19/086; PS19/100; PS19/112; PS19/157; PS19/160; PS19/165; PS19/167; PS19/175; PS19/176; PS19/178; PS19/181; PS19/186; PS19/189; PS19/200; PS19/206; PS19/210; PS19/218; PS19/228; PS19/234; PS19/241; PS19/245; PS1906-1; PS1906-2; PS19 ARCTIC91; PS19 EPOS II; PS2122-2; PS2123-2; PS2129-1; PS2138-1; PS2163-1; PS2166-2; PS2170-4; PS2172-2; PS2177-1; PS2178-2; PS2179-1; PS2180-1; PS2185-3; PS2186-5; PS2193-2; PS2195-4; PS2196-2; PS2200-2; PS2206-4; PS2208-1; PS2210-3; PS2212-3; PS2423-4; PS2424-1; PS2446-4; PS26/148; PS26/149; PS26 NEW; PS27; PS27/020; PS2837-5; PS2837-6; PS2876-1; PS2876-2; PS2887-1; PS2887-2; PS44; PS44/065; PS45; PS45/029; PS45/058; SL; Svalbard; Yermak Plateau
    Type: Dataset
    Format: application/zip, 12 datasets
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  • 20
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    PANGAEA
    In:  Supplement to: Wallrabe-Adams, Hans-Joachim; Lackschewitz, Klas Sven (2003): Chemical composition, distribution, and origin of silicic volcanic ash layers in the Greenland–Iceland–Norwegian Sea: explosive volcanism from 10 to 300 ka as recorded in deep-sea sediments. Marine Geology, 193(3-4), 273-293, https://doi.org/10.1016/S0025-3227(02)00661-8
    Publication Date: 2024-07-01
    Description: Explosive ocean island volcanism in the Greenland-Iceland-Norwegian Sea (GIN Sea) is indicated by marine tephra layers at 10-300 ka. Peaks of explosive volcanism occurred in oxygen isotope stages 8, 7, 5 and 1. The depositional age of the tephra was estimated using the oxygen isotope stratigraphy and dating of marine records. Geochemical analyses of the tephra layers show that all originate from Iceland. Here we report the characteristics of tephra from these major Icelandic events in 30 deep-sea cores from the GIN Sea. Our findings provide constraints on the distribution of tephra from the eruption source. For the Vedde Ash (oxygen isotope stage 1) we estimate a minimum fallout area of 2*10**5 km**2, stretching from central Greenland in the west and southern Sweden in the east, to 71°N in the GIN Sea. The magnitude of the eruption and the regional wind conditions controlled the extent and concentrations of these ash fallout events. Oceanic circulation and differential settling may have affected the distribution and final deposition of ash particles such as bubble wall shards.
    Keywords: 403; ARK-II/5; ARK-VII/1; Atlantic Ocean; Giant box corer; GIK21852-2 PS17/018; GIK21857-2 PS17/024; GIK23059-3; GIK23065-3; GIK23243-1 PS05/431; GIK23244-2 PS05/449; GIK23245-1 PS05/450; GIK23359-4; GKG; Gravity corer (Kiel type); Iceland Sea; KAL; Kasten corer; Kolbeinsey Ridge; M2/2; M7/5; Meteor (1986); Norwegian Sea; PO158/A; Polarstern; POS158/1; POS158/1_0001/1; Poseidon; PS05; PS1243-1; PS1244-2; PS1245-1; PS17; PS1852-2; PS1857-2; SL
    Type: Dataset
    Format: application/zip, 11 datasets
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  • 21
    Publication Date: 2024-07-01
    Keywords: 405; Aluminium; Arsenic; Barium; BIGSET; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Calcium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; GEOMAR; Giant box corer; GKG; Helmholtz Centre for Ocean Research Kiel; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; Lead; M36/6; M36/6_KG10; Magnesium; Manganese; Meteor (1986); Nickel; Phosphorus; Potassium; Rubidium; Silicon; Sodium; Strontium; Thorium-230; Titanium; Vanadium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 614 data points
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  • 22
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-07-01
    Keywords: ARK-VIII/3; AWI_Paleo; DEPTH, sediment/rock; Giant box corer; GKG; Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); Morris Jesup Rise; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/222; PS19 ARCTIC91; PS2202-2
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 23
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-07-01
    Keywords: ARK-VIII/3; AWI_Paleo; DEPTH, sediment/rock; Gakkel Ridge, Arctic Ocean; Giant piston corer; GPC; Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/228; PS19 ARCTIC91; PS2206-3
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 24
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; AWI_Paleo; DEPTH, sediment/rock; Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); KAL; Kasten corer; Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2456-3; PS27; PS27/034
    Type: Dataset
    Format: text/tab-separated-values, 544 data points
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  • 25
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; AWI_Paleo; DEPTH, sediment/rock; Giant box corer; GKG; Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2460-3; PS27; PS27/040
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 26
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    PANGAEA
    Publication Date: 2024-07-01
    Keywords: CT; GEOMAR; Helmholtz Centre for Ocean Research Kiel; SO136; SO136-track; Sonne; Southwest Pacific Basin; TASQWA; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 12.2 kBytes
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  • 27
    Publication Date: 2024-07-01
    Keywords: ARK-VII/1; Counting 〉125 µm fraction; Counting 〉250 µm fraction; Counting 125-250 µm fraction; DEPTH, sediment/rock; Fishers alpha index of diversity; Foraminifera, benthic; gcmd1; Giant box corer; GIK/IfG; GIK21906-1 PS17/081; GKG; Greenland Sea; Institute for Geosciences, Christian Albrechts University, Kiel; Number of species; Polarstern; PS17; PS1906-1
    Type: Dataset
    Format: text/tab-separated-values, 675 data points
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  • 28
    Publication Date: 2024-07-01
    Keywords: Conductivity; CT; DATE/TIME; DEPTH, water; JGOFS; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; M36/5; M36/5-track; Meteor (1986); Northeast Atlantic; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 10811 data points
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  • 29
    Publication Date: 2024-07-01
    Keywords: ARK-VI/2; Counting 〉125 µm fraction; Counting 〉250 µm fraction; Counting 125-250 µm fraction; DEPTH, sediment/rock; Fishers alpha index of diversity; Foraminifera, benthic; gcmd1; Giant box corer; GIK/IfG; GIK21745-5 PS15/054-5; GKG; Greenland Sea; Institute for Geosciences, Christian Albrechts University, Kiel; Number of species; Polarstern; PS15; PS1745-5
    Type: Dataset
    Format: text/tab-separated-values, 666 data points
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  • 30
    Publication Date: 2024-07-01
    Keywords: AGE; ARK-VII/1; Calculated; Comment; Density, dry bulk; DEPTH, sediment/rock; gcmd1; Giant box corer; GIK/IfG; GIK21906-1 PS17/081; GKG; Greenland Sea; Institute for Geosciences, Christian Albrechts University, Kiel; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; Polarstern; PS17; PS1906-1; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 347 data points
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  • 31
    Publication Date: 2024-07-01
    Keywords: 06MT15_2; 109-1; 114-1; 117-1; 120-1; 121-1; 125SGC; 358Bx; 361Cx; 361Fx; 361Jx; 362Co; 362Eo; 363Cx; 363Fx; 366Bo; 367Hx; 368Bx; 369Bo; 369Hx; 370Cx; 372Kx; 374Ao; 374Co; 375Bo; 375Fo; 379Bo; 379Bx; 385Bx; 387Eo; 388Dx; 389Bo; 389Bx; 389Fo; 390Fx; 390Jx; 390Mx; 391Ao; 391Do; 49-08; 49-13; 49-14; 49-15; 49-18; 49-20; 49-39; 49-43; 52-04; 52-09; 52-14; 52-24; 52-28; 52-33; 52-37; 52-38; 52-43; 57-04; 57-06; 57-07; 57-08; 57-09; 57-10; 57-11; 57-12; 57-13; 57-14; 57-20; 58-08; 70-1; 70KS06; 71-15; 71-17; 71-19; 76-2; 80KB11; 80KB28; 82KS01; 83-101; 83-104; 83-106; 83-109; 83-110; 83-201; 83-202; 83-203; 83-204; 83-205; A150/180; A15-558; A172-6; A181/185; A181-7; A1A2; A1A5; A1A6; AC85-4; Adriatic Sea; Aegean Sea; Agulhas Basin; Agulhas Ridge; AHF-11343; AHF-16830; AHF-16832; AHF-28181; Akademik A. Vinogradov; Alpha Ridge, Arctic Ocean; Amazon Fan; Amerasian Basin; AMPH01AR; AMPH-022G; AMPH-030PG; AMPHITRITE; Amundsen Basin; Angola Basin; Antarctic Ocean; ANTIPROD; ANT-IV/1c; ANT-IV/3; ANT-IX/4; ANT-V/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/5; ANT-X/6; ANT-XI/2; ANT-XI/4; APNAP1; APNAP11; APNAP12; APNAP13; APNAP14; APNAP15; APNAP16; APNAP17; APNAP18; APNAP19; APNAP2; APNAP20; APNAP3; APNAP4; APNAP5; APNAP6; APNAP7; APNAP9; APSARA1; APSARA2; APSARA3; APSARA4; Arabian Sea; Arctic Ocean; Argo; ARK-I/3; ARK-II/4; ARK-II/5; ARK-III/3; ARK-IV/3; ARK-IX/4; ARK-VI/2; ARK-VII/1; ARK-VIII/2; ARK-VIII/3; AT_II-107_22; AT_II-15_585; AT_II-15_586; AT_II-15_591; AT_II-15_592; AT_II-15_596; AT_II-15_597; AT_II-15_612; ATII_USA; Atka Bay; Atlantic Indik Ridge; Atlantic Ocean; Atlantic Ridge; Atlantis II (1963); AVI19-4; B_LANDER; B1A6; B34-91; Baffin Shelf; Balear Sea; Barents Sea; BC; BC42-11; BC43-15; BC44-12; BC5-5; BC79-8; BCR; BF043-003; BIOMASSE; Biscaya; BlakeP; Bottle, Niskin; Bottom lander; Bounty Trough, Southwest Pacific; Box corer; Box corer (Reineck); Brazil Basin; BWL2; C1; Cape Basin; Cape Blanc; CEPAG; CESAR; CESAR_83-101; CESAR_83-104; CESAR_83-106; CESAR_83-109; CESAR_83-110; CESAR_83-201; CESAR_83-202; CESAR_83-203; CESAR_83-204; CESAR_83-205; CH182-36; CH70-K11; CH72-101; CH73-108; CH73-110; CH73-136; CH73-139; CH73-139C; CH73-141; CH73-145; CH73-147; CH7X; CH88-11P; CHAT 10K; CHIPAL; CHN115-26PG; CHN115-27PG; CHN115-36PG; CHN155-36PG; CLIVAMPcruises; CONDOR-Ia; Continental slope off Brazil; Continental Slope off Rio Paraiba do Sul; CS70-5; CS72-37; CTD/Rosette; CTD-RO; D.St.A.2; D206; D84; DAL7-60; DED87-07; DEDALE87; DEPTH, sediment/rock; Discovery Seamount; DODO; DODO-124D; DODO-197; DODO-200V; DODO-201G; DODO-204; DW137; DWBG-137; DWHG84; DWHG-84; DWHG-85; East Atlantic; East Brazil Basin; Eastern Rio Grande Rise; eastern Romanche Fracture Zone; Ecor1Ki05; Ecor1Ki15; Ecor2Ki25; Ecor2Ki35; Ecor4Ki50; Elevation of event; ELT16; ELT16.009-PC; ELT20; ELT20.018-PC; ELT21; ELT21.011-PC; ELT34; ELT34.001-PC; ELT36; ELT36.039-PC; ELT36.040-PC; ELT36.041-PC; ELT36.042-PC; ELT45; ELT45.027-PC; ELT45.070-PC; ELT45.073-PC; ELT45.077-PC; ELT48; ELT48.011-PC; ELT48.022-PC; ELT48.027-PC; ELT50; ELT50.033-PC; Eltanin; EN06601; EN066-10GGC; EN32-PC4; EN32-PC6; Endeavor; ENXX; Equatorial Atlantic; ERDC; ERDC-079BX; ERDC-088BX; ERDC-092BX; ERDC-102BX; ERDC-108BX; ERDC-112BX; ERDC-123BX; ERDC-125BX; ERDC-129BX; ERDC-135BX; ERDC-136BX; ERDC-139BX; ETNA80; ETNA82; Event label; F104; F111; F137; F149; FAEGAS_IV; FBG; FGGE-Equator 79 - First GARP Global Experiment; Filchner Trough; FL-523; Fram-I; FramI/4; FramI/7; FramII/1; FramII/3; FramII/4; FramII/5; FramIII/1; FramIII/2; FramIII/3; FramIII/7; FramIII/8; FramIV/1; FramIV/7; FramIV/9; Fram Strait; G-1290; Gakkel Ridge, Arctic Ocean; GC; GC11; GC36; GC5; GeoB1000-1; GeoB1001-1; GeoB1005-2; GeoB1006-2; GeoB1007-2; GeoB1011-2; GeoB1013-2; GeoB1014-2; GeoB1015-2; GeoB1016-2; GeoB1017-3; GeoB1019-2; GeoB1020-1; GeoB1027-2; GeoB1027-3; GeoB1028-4; GeoB1028-5; GeoB1029-1; GeoB1029-3; GeoB1030-3; GeoB1031-1; GeoB1031-3; GeoB1032-2; GeoB1032-3; GeoB1033-1; GeoB1033-2; GeoB1034-1; GeoB1034-3; GeoB1035-3; GeoB1035-5; GeoB1039-1; GeoB1040-3; GeoB1041-1; GeoB1041-4; GeoB1046-2; GeoB1047-1; GeoB1048-1; GeoB1048-2; GeoB1101-4; GeoB1101-6; GeoB1103-3; GeoB1103-4; GeoB1104-4; GeoB1104-5; GeoB1105-3; GeoB1106-5; GeoB1108-6; GeoB1108-7; GeoB1109-3; GeoB1109-4; GeoB1110-3; GeoB1110-4; GeoB1111-3; GeoB1111-5; GeoB1112-3; GeoB1113-4; GeoB1113-7; GeoB1114-3; GeoB1114-4; GeoB1115-3; GeoB1115-4; GeoB1116-1; GeoB1116-2; GeoB1117-2; GeoB1117-3; GeoB1121-1; GeoB1203-2; GeoB1203-3; GeoB1204-3; GeoB1204-4; GeoB1207-2; GeoB1207-3; GeoB1208-1; GeoB1208-2; GeoB1209-1; GeoB1209-2; GeoB1210-2; GeoB1211-3; GeoB1216-1; GeoB1216-2; GeoB1217-1; GeoB1217-2; GeoB1218-1; GeoB1220-1; GeoB1220-2; GeoB1308-1; GeoB1309-3; GeoB1310-1; GeoB1311-2; GeoB1312-1; GeoB1313-1; GeoB1315-2; GeoB1401-1; GeoB1402-7; GeoB1403-2; GeoB1403-3; GeoB1404-8; GeoB1407-8; GeoB1413-1; GeoB1414-1; GeoB1414-2; GeoB1415-1; GeoB1417-1; GeoB1418-1; GeoB1419-1; GeoB1419-2; GeoB1420-1; GeoB1501-1; GeoB1503-2; GeoB1504-1; GeoB1505-3; GeoB1506-1; GeoB1508-1; GeoB1511-6; GeoB1512-1; GeoB1513-2; GeoB1514-5; GeoB1515-2; GeoB1516-1; GeoB1522-1; GeoB1523-2; GeoB1613-2; GeoB1701-2; GeoB1701-4; GeoB1702-7; GeoB1709-3; GeoB1715-1; GeoB1716-3; GeoB1719-7; GeoB1720-2; GeoB1721-4; GeoB1721-7; GeoB1722-3; GeoB1726-1; GeoB1728-1; GeoB1728-3; GeoB1729-1; GeoB1901-2; GeoB1903-3; GeoB1904-3; GeoB1907-2; GeoB2102-1; GeoB2104-1; GeoB2105-3; GeoB2106-1; GeoB2107-5; GeoB2109-3; GeoB2111-2; GeoB2112-1; GeoB2118-1; GeoB2118-3; GeoB2119-1; GeoB2119-2; GeoB2124-1; GeoB2124-3; GeoB2125-1; GeoB2125-2; GeoB2126-1; GeoB2126-3; GeoB2130-1; GeoB2130-3; GeoB2201-1; GeoB2202-5; GeoB2204-1; GeoB2205-4; GeoB2206-1; GeoB2207-2; GeoB2208-1; GeoB2213-1; GeoB2215-8; GeoB2216-2; GeoB3103-1; GeoB3108-4; GeoB3116-1; GeoB3117-3; GeoB3118-1; GeoB3119-1; GeoB3127-1; GeoB3137-1; GeoB3138-2; GeoB3149-2; GeoB3150-1; GeoB3151-2; GeoB3167-1; GeoB3168-1; GeoB3174-1; GeoB3201-2; GeoB3202-2; GeoB3203-3; GeoB3205-1; GeoB3206-2; GeoB3207-2; GeoB3208-2; GeoB3209-2; GeoB3211-1; GeoB3217-1; GeoB3218-1; GeoB3219-1; GeoB3220-2; GeoB3221-1; GeoB3227-1; GeoB3228-2; GeoB3229-1; GeoB3230-4; GeoB3231-2; GeoB3232-3; GeoB3301-2; GeoB3302-2; GeoB3303-1; GeoB3304-3; GeoB3305-2; GeoB3308-3; GeoB3312-2; GeoB3313-3; GeoB3314-2; GeoB3316-1; GeoB3317-6; GeoB3318-2; GeoB3323-6; GeoB3326-1; GeoB3327-6; GeoB3328-1; GeoB3331-1; GeoB3339-2; GeoB3349-4; GeoB3352-1; GeoB3353-1; GeoB3354-1; GeoB3355-4; GeoB3357-1; GeoB3359-1; GeoB3365-1; GeoB3368-4; GeoB3371-1; GeoB3372-4; GeoB3373-1; GeoB3374-1; GeoB3375-2; GeoB3376-2; GeoB3377-1; GeoB3378-2; GeoB3383-1; GeoB3387-3; GeoB3388-2; GeoB3827-2; GEOTROPEX 83, NOAMP I; GGC; GGC-15; GGC-15-2; Giant box corer; Giant gravity corer; GIK12301-5; GIK12302-3; GIK12303-3; GIK12304-3; GIK12305-2; GIK12306-2; GIK12307-3; GIK12308-2; GIK12309-1; GIK12309-2; GIK12310-1; GIK12310-4; GIK12313-2; GIK12314-2; GIK12315-2; GIK12316-1; GIK12317-1; GIK12322-2; GIK12323-1; GIK12324-1; GIK12325-4; GIK12326-2; GIK12327-2; GIK12327-5; GIK12328-1; GIK12328-5; GIK12328-6; GIK12337-5; GIK12338-1; GIK12339-2; GIK12340-3; GIK12341-2; GIK12342-1; GIK12343-1; GIK12344-2; GIK12345-3; GIK12345-5; GIK12346-1; GIK12347-1; GIK12379-1; GIK12392-1; GIK13123-1; GIK13124-1; GIK13131-1; GIK13138-1; GIK13140-3; GIK13147-1; GIK13150-1; GIK13220-1; GIK13221-1; GIK13222-1; GIK13223-3; GIK13224-2; GIK13225-2; GIK13230-1; GIK13231-1; GIK13232-1; GIK13233-1; GIK13234-1; GIK13235-2; GIK13236-1; GIK13237-1; GIK13238-1; GIK13273-1; GIK13275-1; GIK13279-3; GIK13280-1; GIK13282-1; GIK13283-2; GIK13289-1; GIK13289-3; GIK13290-1; GIK13291-1; GIK13329-2; GIK13526-4; GIK13527-1; GIK13528-2; GIK13529-1; GIK13530-1; GIK13532-2; GIK13533-1; GIK13534-1; GIK13536-2; GIK13557-1; GIK13583-1; GIK13584-2; GIK13585-1; GIK13586-1; GIK13587-1; GIK13588-2; GIK15626-1; GIK15627-2; GIK15628-4; GIK15629-1; GIK15630-1; GIK15631-1; GIK15632-1; GIK15634-1; GIK15635-2; GIK15637-1; GIK15638-2; GIK15639-1; GIK15640-1; GIK15641-2; GIK15642-1; GIK15643-1; GIK15644-1; GIK15645-1; GIK15646-1; GIK15647-1;
    Type: Dataset
    Format: text/tab-separated-values, 6915 data points
    Location Call Number Expected Availability
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  • 32
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Klages, Michael; Vopel, Kay; Bluhm, Hartmut; Brey, M; Soltwedel, Thomas; Arntz, Wolf E (2001): Deep-sea food falls: first observation of a natural event in the Arctic Ocean. Polar Biology, 24(4), 292-295, https://doi.org/10.1007/s003000000199
    Publication Date: 2024-07-01
    Description: Concentrations of scavengers attracted by bait in the deep sea are documented by time-lapse photography and results of baited traps. During a remotely operated vehicle deployment in the Molloy Deep, the deepest depression of the Fram Strait, the carcass of a natant decapod, Pasiphaea tarda Krøyer, 1845, was discovered at 79°08.4'N and 002°49.85'E in a depth of 5,551 m. The carcass was covered by hundreds of individuals of Uristes sp., a scavenging lysianassoid amphipod. After documentation of this event, both the carcass and the majority of amphipods were collected. This is the first reported observation and sampling of an ongoing feeding process of scavengers on a natural food fall in the deep sea.
    Keywords: ARK-XV/1; AWI_BPP; Bentho-Pelagic Processes @ AWI; Image analysis; MUC; MultiCorer; Polarstern; PS55; PS55/003; Uristes sp., length
    Type: Dataset
    Format: text/tab-separated-values, 693 data points
    Location Call Number Expected Availability
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  • 33
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Romero, Oscar E; Hebbeln, Dierk (2003): Biogenic silica and diatom thanatocoenosis in surface sediments below the Peru-Chile Current: controlling mechanisms and relationship with productivity of surface waters. Marine Micropaleontology, 48(1-2), 71-90, https://doi.org/10.1016/S0377-8398(02)00161-5
    Publication Date: 2024-07-01
    Description: Based on 76 surface sediment samples collected between ca. 22° and 44°S along the Chilean coast in the southeast Pacific Ocean, we report on the north-south distribution of opal content and diatom concentration, and the quantitative and qualitative composition of the preserved diatom community. Latitudinal differences in the siliceous signal reflect the influence of two main mechanisms of surface water production: coastal upwelling off northern and central Chile till ca. 38°S, and nutrient enrichment by the input of cold, southern, non-upwelling-associated waters south of ca. 38°S. The poleward increase in biogenic opal and diatom values parallels well the north-south increase of pigment concentration in surface waters as recorded by satellites. Between 22° and 33°S, where low pigment concentrations are measured, opal content and diatom concentration are mostly low (except at 22°-23°S). In contrast, both higher opal and diatom values at 34°-38°S and 41°-42°S correspond well with higher pigment estimations. Preserved diatom populations document the present-day dominant hydrographical conditions. Nutrient enrichment of surface waters due to coastal upwelling results in intensive production of diatoms off northern and central Chile, reflected by the predominance of the richly-composed association of Chaetoceros spores north of ca. 38°S. The diatom association shows that the area between 35° and 38°S is transitional. The abrupt decrease of Chaetoceros spores south of not, vert, similar38°S off Chile coupled with the enhanced contribution of Thalassiosira spp., representatives of high-productivity, low-temperature waters, points to the presumed high nutrient supply by the iron-limited, nutrient-rich Antarctic Circumpolar Water. The contribution of benthic diatoms reflects some lateral transport from the near-shore area into deeper positions south of 38°S.
    Keywords: Achnanthes sp.; Actinocyclus curvatulus; Actinocyclus exiguus; Actinocyclus octonarius; Actinoptychus senarius; Actinoptychus vulgaris; Adoneis pacifica; Amphora ostrearia; Amphora sp.; Asteromphalus arachne; Asteromphalus flabellatus; Asteromphalus heptactis; Asteromphalus hyalinus; Asteromphalus sarcophagus; Aulacoseira granulata; Aulacoseira islandica; Azpeitia africana; Azpeitia barronii; Azpeitia neocrenulata; Azpeitia nodulifera; Azpeitia tabularis; Bacteriastrum elongatum; Bacteriastrum furcatum; Bacteriastrum hyalinum; Biddulphia alternans; Catacombas gailloni; Chaetoceros affinis; Chaetoceros affinis, resting spores; Chaetoceros bacteriastroides; Chaetoceros cinctus, resting spores; Chaetoceros compresus, resting spores; Chaetoceros concavicornis; Chaetoceros constrictus, resting spores; Chaetoceros coronatus, resting spores; Chaetoceros debilis, resting spores; Chaetoceros decipiens; Chaetoceros diadema; Chaetoceros diadema, resting spores; Chaetoceros didymus; Chaetoceros didymus, resting spores; Chaetoceros didymus var. protuberans; Chaetoceros lorenzianus, resting spores; Chaetoceros messanensis; Chaetoceros radicans, resting spores; Chaetoceros socialis, resting spores; Chaetoceros sp., resting spores; Chaetoceros vanheurckii, resting spores; CHIPAL; Cocconeis britannica; Cocconeis californica var. lengana; Cocconeis costata var. costata; Cocconeis costata var. hexagona; Cocconeis decipiens; Cocconeis dirupta; Cocconeis pelta; Cocconeis placentula; Cocconeis pseudomarginata; Cocconeis speciosa; Cocconeis stauroneiformis; CONDOR-Ia; Corethron sp.; Coscinodiscus argus; Coscinodiscus centralis; Coscinodiscus coculus-iridis; Coscinodiscus janischii; Coscinodiscus radiatus; Coscinodiscus thorii; Counting, diatoms; Ctenophora sp.; Cyclophora sp.; Cyclotella litoralis; Cyclotella meneghiniana; Cyclotella stelligera; Cymbella sp.; Delphineis surirella; Denticula sp.; DEPTH, sediment/rock; Diatoma sp.; Diploneis bombus; Diploneis constricta; Dytilum brightwelli, resting spores; Elevation of event; Epithemia sp.; Eunotia sp.; Event label; Fallacia nyella; Fragilariopsis doliolus; GeoB; GeoB3303-1; GeoB3311-2; GeoB3312-2; GeoB3316-1; GeoB3317-6; GeoB3349-4; GeoB3355-4; GeoB3357-1; GeoB3359-1; GeoB3365-1; GeoB3373-1; GeoB3374-1; GeoB3376-2; GeoB7103-3; GeoB7106-1; GeoB7108-3; GeoB7112-1; GeoB7114-1; GeoB7115-1; GeoB7116-1; GeoB7118-1; GeoB7119-1; GeoB7121-1; GeoB7122-2; GeoB7123-1; GeoB7127-1; GeoB7129-1; GeoB7130-1; GeoB7131-1; GeoB7133-1; GeoB7134-1; GeoB7135-1; GeoB7137-2; GeoB7138-1; GeoB7142-2; GeoB7144-1; GeoB7148-1; GeoB7150-1; GeoB7152-1; GeoB7153-1; GeoB7154-2; GeoB7155-1; GeoB7156-1; GeoB7157-1; GeoB7158-1; GeoB7159-1; GeoB7162-3; GeoB7163-4; GeoB7166-2; GeoB7167-3; GeoB7170-1; GeoB7171-2; GeoB7174-2; GeoB7175-3; GeoB7177-2; GeoB7179-1; GeoB7181-1; GeoB7186-1; GeoB7187-1; GeoB7189-1; GeoB7191-1; GeoB7192-1; GeoB7195-1; GeoB7197-1; GeoB7198-1; GeoB7199-2; GeoB7201-1; GeoB7202-1; GeoB7207-1; GeoB7209-2; GeoB7211-1; GeoB7212-1; GeoB7213-1; GeoB7214-1; GeoB7215-1; GeoB7218-1; Geosciences, University of Bremen; Gomphonema sp.; Grammatophora marina; Hannaea sp.; Hantzschia amphyoxis; Haslea hyalinissima; Hemialus sinensis; Hemidiscus cuneiformis; Latitude of event; Leptocylindrus mediterraneus; Lioloma elongatum; Longitude of event; Luticola mutica; Mastogloia rostrata; MUC; MultiCorer; Navicula cryptotenella; Navicula distans; Navicula sp.; Neidium sp.; Nitzschia bicapitata; Nitzschia interruptestriata; Nitzschia sicula; Nitzschia sp.; Nitzschia sp. Nitzschia cf. sicula; Odontella longicruris; off Chile; Opephora sp.; Paralia sulcata; Pinnularia borealis; Pinnularia microstauron; Planktoniella sol; Pleurosigma directum; Pleurosigma planctonicum; Proboscia alata; Proboscia alata forma indica; Psammodictyon panduriforme; Pseudohimantidium pacificum; Pseudo-nitzschia inflatula var. capitata; Pseudosolenia calcar-avis; Pseudostaurosira brevistriata var. inflata; Pseudotriceratium punctatum; PUCK; Rhizosolenia acuminata; Rhizosolenia bergonii; Rhizosolenia borealis; Rhizosolenia pungens; Rhizosolenia styliformis; Rhopalodia sp.; Roperia tessellata; Skeletonema costatum; SO101; SO101/3_3-1; SO102/1; SO102/2; SO156/1; SO156/2; SO156/3; Sonne; South-East Pacific; Stauroneis anceps; Stellarima stellaris; Stephanodiscus astraea; Stephanopyxis sp.; Surirella sp.; Synedra ulna; Tabularia sp.; Thalassionema bacillare; Thalassionema frauenfeldii; Thalassionema nitzschioides var. inflata; Thalassionema nitzschioides var. nitzschioides; Thalassionema nitzschioides var. parva; Thalassionema pseudonitzschioides; Thalassiosira aestivalis; Thalassiosira anguste-lineata; Thalassiosira bioculata; Thalassiosira conferta; Thalassiosira delicatula; Thalassiosira eccentrica; Thalassiosira endoseriata; Thalassiosira ferelineata; Thalassiosira gerloffii; Thalassiosira gravida; Thalassiosira lineata; Thalassiosira mendiolana; Thalassiosira minuscula; Thalassiosira nanolineata; Thalassiosira oestrupii var. oestrupii; Thalassiosira oestrupii var. venrickae; Thalassiosira pacifica; Thalassiosira plicata; Thalassiosira poro-irregulata; Thalassiosira punctifera; Thalassiosira rotula; Thalassiosira sackettii forma plana; Thalassiosira sp.; Thalassiosira subtilis; Thalassiosira symmetrica; Thalassiosira tumida; Trachyneis aspera
    Type: Dataset
    Format: text/tab-separated-values, 12996 data points
    Location Call Number Expected Availability
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  • 34
    Publication Date: 2024-07-01
    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2465-1; PS27; PS27/047; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
    Location Call Number Expected Availability
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  • 35
    Publication Date: 2024-07-01
    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2466-1; PS27; PS27/048; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
    Location Call Number Expected Availability
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  • 36
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hillenbrand, Claus-Dieter; Grobe, Hannes; Diekmann, Bernhard; Kuhn, Gerhard; Fütterer, Dieter K (2003): Distribution of clay minerals and proxies for productivity in surface sediments of the Bellingshausen and Amundsen seas (West Antarctica) - Relation to modern environmental conditions. Marine Geology, 193(3-4), 253-271, https://doi.org/10.1016/S0025-3227(02)00659-X
    Publication Date: 2024-07-01
    Description: Surface sediments from the Antarctic continental margin in the Bellingshausen and Amundsen seas (Pacific sector of the Southern Ocean) were investigated in order to decipher their capability to record modern environmental conditions. Spatial distribution of terrigenous sand and mud reflect regional differences in current-induced redeposition of glaciogenic debris. Clay mineral assemblages in the shelf sediments are controlled by the supply of terrigenous detritus from source rocks in the adjacent hinterland suggesting the occurrence of yet unknown sedimentary rocks in the hinterland of the Amundsen Sea. Clay mineral distribution on the continental rise in the Bellingshausen Sea points to the continuation of a bottom current from the Antarctic Peninsula rise to at least 94°W. Foraminifer-bearing and opal-poor deposits prevail on the continental margin in the western Bellingshausen Sea and the Amundsen Sea, whereas diatom-bearing and carbonate-free sediments characterize the eastern Bellingshausen Sea. Different modes of biological production, which were deduced from accumulation rates of biogenic barium during Marine Isotope Stage 1 and recent productivity measurements, obviously control the spatial pattern of opal- and carbonate-bearing sediments in the study area.
    Keywords: Adelaide Island; Amundsen Sea; Antarctic Peninsula; ANT-VI/2; ANT-XI/3; Anvers Island; Argentine Islands; AWI_Paleo; Barium; Barium, biogenic; Bellingshausen Sea; Calcium carbonate; Calculated; Carbon, organic, total; Chlorite; DEPTH, sediment/rock; Element analyser CHN, LECO; Elevation of event; Event label; Giant box corer; GKG; Grain size, sieving/settling tube; Illite; Kaolinite; Latitude of event; Longitude of event; Marguerite Bay; MUC; MultiCorer; Opal, auto analysis (Müller & Schneider, 1993); Opal, biogenic silica; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS12; PS12/185; PS12/186; PS12/193; PS12/194; PS12/195; PS12/196; PS12/199; PS12/200; PS1554-1; PS1555-1; PS1557-1; PS1558-1; PS1559-1; PS1560-1; PS1563-1; PS1564-1; PS2522-1; PS2524-1; PS2525-1; PS2526-1; PS2527-1; PS2528-1; PS2529-1; PS2531-1; PS2532-2; PS2533-1; PS2534-2; PS2537-1; PS2538-1; PS2539-2; PS2540-1; PS2541-2; PS2542-1; PS2543-3; PS2544-1; PS2545-1; PS2546-1; PS2547-2; PS2548-2; PS2550-2; PS2553-2; PS2556-1; PS29; PS29/010; PS29/012; PS29/016; PS29/018; PS29/021; PS29/022; PS29/024; PS29/033; PS29/039; PS29/040; PS29/042; PS29/045; PS29/046; PS29/047; PS29/048; PS29/049; PS29/050; PS29/051; PS29/054; PS29/057; PS29/062; PS29/063; PS29/064; PS29/066; PS29/070; PS29/075; Sand; Silt; Size fraction 〈 0.002 mm, clay; Smectite; X-ray diffraction TEXTUR, clay fraction; X-ray fluorescence (XRF)
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    Keywords: ADEPD; Amundsen Basin; ARK-VIII/3; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll pigment equivalents; DEPTH, sediment/rock; MUC; MultiCorer; Polarstern; PS19/167; PS19 ARCTIC91; PS2172-3; Quaternary Environment of the Eurasian North; QUEEN
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll a; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Polarstern; PS2450-1; PS27; PS27/028; Quaternary Environment of the Eurasian North; QUEEN; Student_s t; Vilkitsky Strait
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll a; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Polarstern; PS2451-1; PS27; PS27/029; Quaternary Environment of the Eurasian North; QUEEN; Student_s t; Vilkitsky Strait
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll a; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Polarstern; PS2452-1; PS27; PS27/030; Quaternary Environment of the Eurasian North; QUEEN; Student_s t; Vilkitsky Strait
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Barents Sea; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Phaeopigments; Polarstern; PS2440-3; PS27; PS27/006; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Phaeopigments; Polarstern; PS2475-2; PS27; PS27/060; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Phaeopigments; Polarstern; PS2451-1; PS27; PS27/029; Quaternary Environment of the Eurasian North; QUEEN; Student_s t; Vilkitsky Strait
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    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2459-1; PS27; PS27/039; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
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    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2454-1; PS27; PS27/032; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
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    Format: text/tab-separated-values, 14 data points
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  • 83
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2456-1; PS27; PS27/034; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 84
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2458-1; PS27; PS27/038; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 85
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2460-1; PS27; PS27/040; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 86
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2463-1; PS27; PS27/044; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 87
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2465-1; PS27; PS27/047; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 88
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2467-1; PS27; PS27/049; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 89
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2468-1; PS27; PS27/050; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 90
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2470-1; PS27; PS27/053; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 91
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2475-2; PS27; PS27/060; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 92
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2477-1; PS27; PS27/064; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 93
    Publication Date: 2024-07-01
    Keywords: Adenylates, total; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2478-1; PS27; PS27/065; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 94
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Polarstern; PS2451-1; PS27; PS27/029; Quaternary Environment of the Eurasian North; QUEEN; Student_s t; Vilkitsky Strait
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 95
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2454-1; PS27; PS27/032; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 96
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2459-1; PS27; PS27/039; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 97
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2458-1; PS27; PS27/038; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 98
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2463-1; PS27; PS27/044; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 99
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2460-1; PS27; PS27/040; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 100
    Publication Date: 2024-07-01
    Keywords: Adenosine 5-Triphosphate; ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Confidence; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2462-1; PS27; PS27/043; Quaternary Environment of the Eurasian North; QUEEN; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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