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  • 2000-2004  (324,712)
  • 1990-1994  (18)
  • 1970-1974  (8)
  • 1940-1944  (3)
  • 2003  (324,712)
Collection
Keywords
Publisher
Language
Years
Year
  • 1
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    Fig. 7. Pollen record of profile SAO4 (Analyst: G.N. Shilova) (2003)
    PANGAEA
    Details
    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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  • 2
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    Pollen analysis of sediment core BP99-04/06 (2003)
    PANGAEA
    Details
    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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  • 3
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    Fig. 4. Pollen record of profile SAO1 (Analyst: J. Hahne) (2003)
    PANGAEA
    Details
    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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  • 4
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    Fig. 3. Pollen record of profile PG1228 from lake Levinson-Lessing (2003)
    PANGAEA
    Details
    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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    DATA PANGAEA
  • 5
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    (Table S1) Marine Os isotope record across the Cretaceous-Tertiary boundary (2003)
    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
    Details
    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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  • 6
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    (Table S2) Planktonic foraminifera counts in surface sediment samples (2003)
    PANGAEA
    Details
    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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  • 7
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    Planktonic isotope record and clay mineralogy of sediment core PS2138-1 (2003)
    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
    Details
    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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  • 8
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    Ice rafted debris distribution in 16 sediment cores from the South Atlantic (2003)
    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
    Details
    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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  • 9
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    Age determination and stable isotope composition of sediment cores from the Arctic Ocean (2003)
    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
    Details
    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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  • 10
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    Chemical composition of tephra from the Greenland-Iceland-Norwegian-Sea (2003)
    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
    Details
    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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