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  • 21
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    PANGAEA
    In:  Supplement to: Kim, Jung-Hyun; Crosta, Xavier; Willmott, Verónica; Renssen, Hans; Bonnin, Jerome; Helmke, Peer; Schouten, Stefan; Sinninghe Damsté, Jaap S (2012): Holocene subsurface temperature variability in the eastern Antarctic continental margin. Geophysical Research Letters, 39, L06705, https://doi.org/10.1029/2012GL051157
    Publication Date: 2023-06-27
    Description: We reconstructed subsurface (~45-200 m water depth) temperature variability in the eastern Antarctic continental margin during the late Holocene, using an archaeal lipid-based temperature proxy (TEX86L). Our results reveal that subsurface temperature changes were probably positively coupled to the variability of warmer, nutrient-rich Modified Circumpolar Deep Water (MCDW, deep water of the Antarctic circumpolar current) intrusion onto the continental shelf. The TEX86L record, in combination with previously published climatic records, indicates that this coupling was probably related to the thermohaline circulation, seasonal variability in sea ice extent, sea temperature, and wind associated with high frequency climate dynamics at low-latitudes such as internal El Niño Southern Oscillation (ENSO). This in turn suggests a linkage between centennial ENSO-like variability at low-latitudes and intrusion variability of MCDW into the eastern Antarctic continental shelf, which might have further impact on ice sheet evolution.
    Keywords: AGE; Calculated from TEX86 (Kim et al., 2010); CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES X - CADO; Marion Dufresne (1995); MD032601; MD03-2601; MD130; Southern Ocean; Sub-surface temperature
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 22
    Publication Date: 2024-04-25
    Keywords: 293G; AGE; Alboran Sea; Branched and isoprenoid tetraether index; DEPTH, sediment/rock; GC; Gravity corer; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Professor Logachev; Tetraether index of 86 carbon atoms, high-temperature region; TTR-12_293G; TTR-12/3
    Type: Dataset
    Format: text/tab-separated-values, 182 data points
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  • 23
    Publication Date: 2024-04-25
    Keywords: Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Branched and isoprenoid tetraether index; Crenarchaeol, fractional abundance; Crenarchaeol regio-isomer, fractional abundance; DEPTH, water; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Event label; Latitude of event; Longitude of event; Matapan; McLane Pump; McLP; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance; Urania; Vector
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 24
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    PANGAEA
    In:  Supplement to: Stuut, Jan-Berend W; Zabel, Matthias; Ratmeyer, Volker; Helmke, Peer; Schefuß, Enno; Lavik, Gaute; Schneider, Ralph R (2005): Provenance of present-day eolian dust collected off NW Africa. Journal of Geophysical Research: Atmospheres, 110, D04202, https://doi.org/10.1029/2004JD005161
    Publication Date: 2024-06-26
    Description: Atmospheric dust samples collected along a transect off the West African coast have been investigated for their physical (grain-size distribution), mineralogical, and chemical (major elements) composition. On the basis of these data the samples were grouped into sets of samples that most likely originated from the same source area. In addition, shipboard-collected atmospheric meteorological data, modeled 4-day back trajectories for each sampling day and location, and Total Ozone Mapping Spectrometer aerosol index data for the time period of dust collection (February-March 1998) were combined and used to reconstruct the sources of the groups of dust samples. On the basis of these data we were able to determine the provenance of the various dust samples. It appears that the bulk of the wind-blown sediments that are deposited in the proximal equatorial Atlantic Ocean are transported in the lower level (〉~900 hPa) NE trade wind layer, which is a very dominant feature north of the Intertropical Convergence Zone (ITCZ). However, south of the surface expression of the ITCZ, down to 5°S, where surface winds are southwesterly, we still collected sediments that originated from the north and east, carried there by the NE trade wind layer, as well as by easterly winds from higher altitudes. The fact that the size of the wind-blown dust depends not only on the wind strength of the transporting agent but also on the distance to the source hampers a direct comparison of the dust's size distributions and measured wind strengths. However, a comparison between eolian dust and terrigenous sediments collected in three submarine sediment traps off the west coast of NW Africa shows that knowledge of the composition of eolian dust is a prerequisite for the interpretation of paleorecords obtained from sediment cores in the equatorial Atlantic.
    Keywords: AEOLD; Aeolian dust sample; Center for Marine Environmental Sciences; D1; D10; D11; D12; D13; D14; D15; D16; D17; D18; D19; D20; D21; D22; D23; D24; D25; D3; D4; D5; D6; D7; D8; D9; GeoB; Geosciences, University of Bremen; M41/1; M41/1_D1; M41/1_D10; M41/1_D11; M41/1_D12; M41/1_D13; M41/1_D14; M41/1_D15; M41/1_D16; M41/1_D17; M41/1_D18; M41/1_D19; M41/1_D2; M41/1_D20; M41/1_D21; M41/1_D22; M41/1_D23; M41/1_D24; M41/1_D25; M41/1_D3; M41/1_D4; M41/1_D5; M41/1_D6; M41/1_D7; M41/1_D8; M41/1_D9; MARUM; Meteor (1986)
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 25
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4209-2; Gravity corer (Kiel type); Intercore correlation; Iron; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL; X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 2602 data points
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  • 26
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4213-2; Gravity corer (Kiel type); Intercore correlation; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL
    Type: Dataset
    Format: text/tab-separated-values, 1590 data points
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  • 27
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4225-1; Gravity corer (Kiel type); Intercore correlation; Iron; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL; X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 2264 data points
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  • 28
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; DEPTH, sediment/rock; GeoB4226-3; Gravity corer (Kiel type); M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL
    Type: Dataset
    Format: text/tab-separated-values, 1068 data points
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  • 29
    Publication Date: 2024-06-26
    Keywords: 666; 668; 670; 671; 673; 674; 675; 676; 677; 678; 680; 681; 682; 683; 684; 685; 686; 687; 689; 690; 691; 692; 693; 694; 695; 696; 697; 699; 700; 701; 702; 703; 704; 705; 706; 707; 708; 709; 710; 712; 713; 714; 716; 717; 718; 719; Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Alboran Sea; AN10; AN33; AN83; BC; Box corer; Branched and isoprenoid tetraether index; BT-A; BT-B; BT-C; BT-D; BT-E; BT-F; BT-G; CH_S; CH51; CH67; Crenarchaeol, fractional abundance; Crenarchaeol regio-isomer, fractional abundance; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Elevation of event; Event label; Gargano Promontory; GeoB10701-4; GeoB10703-3; GeoB10704-3; GeoB10705-3; GeoB10707-4; GeoB10708-3; GeoB10709-4; GeoB10710-4; GeoB10711-3; GeoB10712-3; GeoB10713-3; GeoB10714-3; GeoB10715-3; GeoB10716-3; GeoB10717-3; GeoB10718-3; GeoB10719-3; GeoB10720-5; GeoB10721-3; GeoB10722-3; GeoB10723-3; GeoB10724-3; GeoB10725-3; GeoB10726-3; GeoB10727-3; GeoB10728-3; GeoB10729-4; GeoB10730-3; GeoB10731-3; GeoB10732-3; GeoB10733-3; GeoB10734-3; GeoB10735-3; GeoB10736-3; GeoB10737-3; GeoB10738-3; GeoB10739-3; GeoB10740-3; GeoB10741-3; GeoB10742-3; GeoB10743-3; GeoB10744-3; GeoB10746-3; GeoB10747-3; GeoB10748-3; GeoB10749-3; Gulf of Manfredonia; Gulf of Taranto; HI-A; HI-B; HI-D; HI-E; HI-F; HII-C; HII-G; HII-H; HII-I; HII-L; HII-MIN; HII-N; HII-O; HII-PLA; HI-L; HI-M; IDEA_0204_dr1; IDEA_0204_dr2; IDEA_0204_dr3; IDEA_0204_dr4; IDEA_0204_dr5; IDEA_0204_dr6; IDEA_0404_dr3; IDEA_0404_dr4; IDEA_0404_dr5; IDEA_0404_dr6; IDEA_0404_dr7; IDEA_0404_dr8; IDEA_0604_dr1; IDEA_0604_dr2; IDEA_0604_dr3; IDEA_0604_dr4; IDEA_0604_dr5; IDEA_0604_dr6; IDEA_0604_dr7; IDEA_0604_dr8; IDEA_0803_dr3; IDEA_0803_dr4; IDEA_0803_dr5; IDEA_0803_dr6; IDEA_0803_dr8; IDEA_0903_dr1; IDEA_0903_dr2; IDEA_0903_dr4; IDEA_0903_dr5; IDEA_0903_dr6; IDEA_0903_dr7; IDEA_0903_dr8; IDEA_1103_dr1; IDEA_1103_dr2; IDEA_1103_dr3; IDEA_1103_dr4; IDEA_1103_dr5; IDEA_1103_dr6; IDEA_1103_dr8; Latitude of event; Longitude of event; MC613; MC614; MC615; MC616; MC617; MC618; MC619; MC620; MC621; MC622; MC623; MC625; MC626; MC630; MC631; MC632; MC634; MC635; MC637; MC638; MC639; MC640; MC641; MC642; MC643; MC644; MC645; Method/Device of event; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; MT10; MT11; MT14; MT15; MT16; MT17; MT20; MT24; MT25; MT28; MT29bis; MT31; MT33; MT34bis; MT352; MT353; MT37bis; MUC; MultiCorer; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; OMEX_98-5; OMEX_99-15; POS339; Poseidon; Professor Logachev; Reference/source; Riomar_A; Riomar_Aa; Riomar_B; Riomar_C; Riomar_D; Riomar_E; Riomar_F; Riomar_G; Riomar_H; Riomar_I; Riomar_J; Riomar_K; Riomar_Ka; Riomar_L; Riomar_M; Riomar_N; Riomar_O; Riomar_Pbis; Riomar_R2; Riomar_T; Strait of Otranto; T1_MUC; T2_MUC; T3_MUC; T4_MUC; T5_MUC; T6_MUC; T7_MUC; T8_MUC; T9_MUC; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance; TTR-17/1; TTR-17-1_384B; TTR-17-1_436B; V1_MUC; V2_MUC; V3_MUC
    Type: Dataset
    Format: text/tab-separated-values, 1940 data points
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  • 30
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4228-3; Intercore correlation; Iron; KOL; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; Piston corer (Kiel type); X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 3732 data points
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