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  • 1
    facet.materialart.
    Unknown
    The Global Plankton Database: an inventory and data from the Former Soviet Union expeditions
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Description: At present time, there is a lack of knowledge on the interannual climate-related variability of zooplankton communities of the tropical Atlantic, central Mediterranean Sea, Caspian Sea, and Aral Sea, due to the absence of appropriate databases. In the mid latitudes, the North Atlantic Oscillation (NAO) is the dominant mode of atmospheric fluctuations over eastern North America, the northern Atlantic Ocean and Europe. Therefore, one of the issues that need to be addressed through data synthesis is the evaluation of interannual patterns in species abundance and species diversity over these regions in regard to the NAO. The database has been used to investigate the ecological role of the NAO in interannual variations of mesozooplankton abundance and biomass along the zonal array of the NAO influence. Basic approach to the proposed research involved: (1) development of co-operation between experts and data holders in Ukraine, Russia, Kazakhstan, Azerbaijan, UK, and USA to rescue and compile the oceanographic data sets and release them on CD-ROM, (2) organization and compilation of a database based on FSU cruises to the above regions, (3) analysis of the basin-scale interannual variability of the zooplankton species abundance, biomass, and species diversity.
    Keywords: AAK106; AAK62; AAK65; AAK7/1; AAK7/2; AAK7/3; AAK7/4; AAK7/5; AAK71; AAK88; AAK90; AAK95; Adriatic Sea; Aegean Sea; Akademik A Kovalyevskiy; Akademik Vernadsky; AKov_106-track; AKov_62-track; AKov_65-track; AKov_7/1-track; AKov_7/2-track; AKov_7/3-track; AKov_7/4-track; AKov_7/5-track; AKov_71-track; AKov_88-track; AKov_90-track; AKov_95-track; Arabian Sea; Aral_Sea; Atlantic Ocean; AV10; AV10_938-1; AV10_938-2; AV10_939-1; AV10_939-2; AV10_940-1; AV10_940-2; AV10_941-1; AV10_941-2; AV10_942-1; AV10_942-2; AV10_943-1; AV10_943-2; AV10_944-1; AV10_944-2; AV10_945-1; AV10_945-2; AV10_946-1; AV10_947-1; AV10_948-1; AV10_948-2; AV10_949-1; AV10_949-2; AV10_950-1; AV10_950-2; AV10_950-3; AV10_950-4; AV10_951-1; AV10_951-2; AV10_952-1; AV10_952-2; AV10_953-1; AV10_953-2; AV10_954-1; AV10_954-2; AV10_955-1; AV10_955-2; AV10_956-1; AV10_956-2; AV10_957-1; AV10_958-1; AV10_959-1; AV10_960-1; AV10_961-1; AV10_961-10; AV10_961-100; AV10_961-101; AV10_961-102; AV10_961-103; AV10_961-104; AV10_961-105; AV10_961-106; AV10_961-107; AV10_961-108; AV10_961-109; AV10_961-11; AV10_961-110; AV10_961-111; AV10_961-112; AV10_961-113; AV10_961-114; AV10_961-115; AV10_961-116; AV10_961-117; AV10_961-118; AV10_961-119; AV10_961-12; AV10_961-120; AV10_961-121; AV10_961-122; AV10_961-123; AV10_961-124; AV10_961-125; AV10_961-126; AV10_961-127; AV10_961-128; AV10_961-129; AV10_961-13; AV10_961-130; AV10_961-131; AV10_961-132; AV10_961-133; AV10_961-134; AV10_961-135; AV10_961-136; AV10_961-137; AV10_961-138; AV10_961-139; AV10_961-14; AV10_961-140; AV10_961-141; AV10_961-142; AV10_961-143; AV10_961-144; AV10_961-145; AV10_961-146; AV10_961-147; AV10_961-148; AV10_961-149; AV10_961-15; AV10_961-150; AV10_961-151; AV10_961-152; AV10_961-153; AV10_961-154; AV10_961-155; AV10_961-156; AV10_961-157; AV10_961-158; AV10_961-159; AV10_961-16; AV10_961-160; AV10_961-161; AV10_961-162; AV10_961-163; AV10_961-164; AV10_961-165; AV10_961-166; AV10_961-167; AV10_961-168; AV10_961-169; AV10_961-17; AV10_961-170; AV10_961-171; AV10_961-172; AV10_961-173; AV10_961-174; AV10_961-175; AV10_961-176; AV10_961-177; AV10_961-178; AV10_961-179; AV10_961-18; AV10_961-180; AV10_961-181; AV10_961-182; AV10_961-183; AV10_961-184; AV10_961-185; AV10_961-186; AV10_961-187; AV10_961-188; AV10_961-189; AV10_961-19; AV10_961-190; AV10_961-191; AV10_961-192; AV10_961-193; AV10_961-194; AV10_961-195; AV10_961-196; AV10_961-197; AV10_961-198; AV10_961-199; AV10_961-2; AV10_961-20; AV10_961-200; AV10_961-201; AV10_961-202; AV10_961-203; AV10_961-204; AV10_961-205; AV10_961-206; AV10_961-207; AV10_961-208; AV10_961-209; AV10_961-21; AV10_961-210; AV10_961-211; AV10_961-212; AV10_961-213; AV10_961-214; AV10_961-215; AV10_961-216; AV10_961-217; AV10_961-218; AV10_961-219; AV10_961-22; AV10_961-220; AV10_961-221; AV10_961-222; AV10_961-223; AV10_961-224; AV10_961-225; AV10_961-226; AV10_961-227; AV10_961-228; AV10_961-229; AV10_961-23; AV10_961-230; AV10_961-231; AV10_961-232; AV10_961-233; AV10_961-234; AV10_961-235; AV10_961-236; AV10_961-237; AV10_961-238; AV10_961-239; AV10_961-24; AV10_961-240; AV10_961-241; AV10_961-242; AV10_961-243; AV10_961-244; AV10_961-245; AV10_961-246; AV10_961-247; AV10_961-248; AV10_961-249; AV10_961-25; AV10_961-250; AV10_961-251; AV10_961-252; AV10_961-253; AV10_961-254; AV10_961-255; AV10_961-256; AV10_961-257; AV10_961-258; AV10_961-259; AV10_961-26; AV10_961-260; AV10_961-261; AV10_961-262; AV10_961-263; AV10_961-264; AV10_961-265; AV10_961-266; AV10_961-267; AV10_961-268; AV10_961-269; AV10_961-27; AV10_961-270; AV10_961-271; AV10_961-272; AV10_961-273; AV10_961-274; AV10_961-275; AV10_961-276; AV10_961-277; AV10_961-2771; AV10_961-278; AV10_961-279; AV10_961-28; AV10_961-280; AV10_961-281; AV10_961-282; AV10_961-283; AV10_961-284; AV10_961-285; AV10_961-286; AV10_961-287; AV10_961-288; AV10_961-289; AV10_961-29; AV10_961-290; AV10_961-291; AV10_961-292; AV10_961-293; AV10_961-294; AV10_961-295; AV10_961-296; AV10_961-297; AV10_961-298; AV10_961-299; AV10_961-3; AV10_961-30; AV10_961-300; AV10_961-301; AV10_961-302; AV10_961-303; AV10_961-304; AV10_961-305; AV10_961-306; AV10_961-307; AV10_961-308; AV10_961-309; AV10_961-31; AV10_961-310; AV10_961-311; AV10_961-312; AV10_961-313; AV10_961-314; AV10_961-315; AV10_961-316; AV10_961-317; AV10_961-318; AV10_961-319; AV10_961-32; AV10_961-320; AV10_961-321; AV10_961-322; AV10_961-323; AV10_961-324; AV10_961-325; AV10_961-326; AV10_961-327; AV10_961-328; AV10_961-329; AV10_961-33; AV10_961-330; AV10_961-331; AV10_961-332; AV10_961-333; AV10_961-334; AV10_961-34; AV10_961-35; AV10_961-36; AV10_961-37; AV10_961-38; AV10_961-39; AV10_961-4; AV10_961-40; AV10_961-41; AV10_961-42; AV10_961-43; AV10_961-44; AV10_961-45; AV10_961-46; AV10_961-47; AV10_961-48; AV10_961-49; AV10_961-5; AV10_961-50; AV10_961-51; AV10_961-52; AV10_961-53; AV10_961-54; AV10_961-55; AV10_961-56; AV10_961-57; AV10_961-58; AV10_961-59; AV10_961-6; AV10_961-60; AV10_961-61; AV10_961-62; AV10_961-63; AV10_961-64; AV10_961-65; AV10_961-66; AV10_961-67; AV10_961-68; AV10_961-69; AV10_961-7; AV10_961-70; AV10_961-71; AV10_961-72; AV10_961-73; AV10_961-74; AV10_961-75; AV10_961-76; AV10_961-77; AV10_961-78; AV10_961-79; AV10_961-8; AV10_961-80; AV10_961-81; AV10_961-82; AV10_961-83; AV10_961-84; AV10_961-85; AV10_961-86; AV10_961-862; AV10_961-87; AV10_961-88; AV10_961-89; AV10_961-9; AV10_961-90; AV10_961-91; AV10_961-92; AV10_961-93; AV10_961-94; AV10_961-95; AV10_961-96; AV10_961-97; AV10_961-98; AV10_961-99; AV10_962-1; AV10_963-1; AV10_964-1; AV10_965-1; AV10_966-1; AV10_967-1; AV10_968-2; AV10_969-2; AV10_970-1; AV10_970-2; AV10_971-2; AV10_974-1; AV11; AV11_1000-2; AV11_1001-2; AV11_1002-2; AV11_1003-1; AV11_1005-1; AV11_1006-1; AV11_1006-10; AV11_1006-11; AV11_1006-12; AV11_1006-13; AV11_1006-15; AV11_1006-16; AV11_1006-17; AV11_1006-18; AV11_1006-19; AV11_1006-2; AV11_1006-20; AV11_1006-21; AV11_1006-22; AV11_1006-23; AV11_1006-24; AV11_1006-25; AV11_1006-26; AV11_1006-27; AV11_1006-28; AV11_1006-29; AV11_1006-3; AV11_1006-30; AV11_1006-31; AV11_1006-32; AV11_1006-33; AV11_1006-34; AV11_1006-35; AV11_1006-36; AV11_1006-37; AV11_1006-38; AV11_1006-39; AV11_1006-4; AV11_1006-40; AV11_1006-41; AV11_1006-42; AV11_1006-43; AV11_1006-44; AV11_1006-45; AV11_1006-46; AV11_1006-47; AV11_1006-48; AV11_1006-49; AV11_1006-5; AV11_1006-50; AV11_1006-51; AV11_1006-52; AV11_1006-6; AV11_1006-7; AV11_1006-8; AV11_1006-9; AV11_1007-10; AV11_1007-11; AV11_1007-12; AV11_1007-13; AV11_1007-14; AV11_1007-15; AV11_1007-16; AV11_1007-17; AV11_1007-18; AV11_1007-19; AV11_1007-2; AV11_1007-20; AV11_1007-21; AV11_1007-22; AV11_1007-23; AV11_1007-24; AV11_1007-25; AV11_1007-26; AV11_1007-27; AV11_1007-28; AV11_1007-29; AV11_1007-3; AV11_1007-30; AV11_1007-31; AV11_1007-32; AV11_1007-33; AV11_1007-34; AV11_1007-35; AV11_1007-36; AV11_1007-37; AV11_1007-38; AV11_1007-39; AV11_1007-4; AV11_1007-40; AV11_1007-41; AV11_1007-42; AV11_1007-43; AV11_1007-44; AV11_1007-45; AV11_1007-46; AV11_1007-47; AV11_1007-48; AV11_1007-49; AV11_1007-5; AV11_1007-50; AV11_1007-51; AV11_1007-52; AV11_1007-53; AV11_1007-54; AV11_1007-55; AV11_1007-56; AV11_1007-57; AV11_1007-58; AV11_1007-59; AV11_1007-6; AV11_1007-60; AV11_1007-61; AV11_1007-62; AV11_1007-63; AV11_1007-7; AV11_1007-8; AV11_1007-9; AV11_1008-1; AV11_1010-1; AV11_1010-2; AV11_1011-1; AV11_1011-2; AV11_1012-1; AV11_1013-1; AV11_1013-2; AV11_1014-1; AV11_1014-2; AV11_1015-1; AV11_1015-2; AV11_1016-1; AV11_1016-2; AV11_1017-1; AV11_1017-2; AV11_1018-1; AV11_1018-2; AV11_1019-1; AV11_1019-2; AV11_1021-2; AV11_1022-2; AV11_1023-2; AV11_1024-2; AV11_1025-2; AV11_1026-2; AV11_1027-2; AV11_1028-2; AV11_1029-2; AV11_1030-2; AV11_1032-2; AV11_1033-2; AV11_1034-2; AV11_1035-2; AV11_1036-2; AV11_1037-2; AV11_1038-2; AV11_1039-2; AV11_1040-2; AV11_1041-2; AV11_1042-2; AV11_1043-2; AV11_1044-2; AV11_1045-2; AV11_1046-2; AV11_1051-1; AV11_1051-10; AV11_1051-11; AV11_1051-12; AV11_1051-13; AV11_1051-14; AV11_1051-15; AV11_1051-16; AV11_1051-17; AV11_1051-18;
    Type: Dataset
    Format: application/zip, 752 datasets
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    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Corrected and interpolated magnetic susceptibility from the EDISTO Array (2019)
    PANGAEA
    Details
    Publication Date: 2023-01-13
    Keywords: after Woodruff & McManus (1966); Core; CORE; Core-08; Core-10; Core-12; Core-16; Core-25; Core-28; Core-29; Core-32; Core-34; Core-39; Core-44; Core-49; Core-52; Core-63; Core-69; Core-71; Core-74; Core-77; Core-82; Core-88; Core-93; EDISTO-08; EDISTO-10; EDISTO-12; EDISTO-16; EDISTO-25; EDISTO-28; EDISTO-29; EDISTO-32; EDISTO-34; EDISTO-39; EDISTO-44; EDISTO-49; EDISTO-52; EDISTO-63; EDISTO-69; EDISTO-71; EDISTO-74; EDISTO-77; EDISTO-82; EDISTO-88; EDISTO-93; Event label; Latitude of event; Longitude of event; Magnetic susceptibility; Norwegian-Greenland Sea; Optional event label; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 7804 data points
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    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Particle size specific rock magnetic and sediment texture data of core top samples from the EDISTO Array (2019)
    PANGAEA
    In:  Supplement to: Hatfield, Robert George; Wheeler, B H; Reilly, Brendan T; Stoner, Joseph S; Housen, Bernard A (2019): Particle Size Specific Magnetic Properties Across the Norwegian‐Greenland Seas: Insights Into the Influence of Sediment Source and Texture on Bulk Magnetic Records. Geochemistry, Geophysics, Geosystems, 20(2), 1004-1025, https://doi.org/10.1029/2018GC007894
    Details
    Publication Date: 2023-01-13
    Description: Location and water depth of the core tops used in this study alongside the percent sediment texture data. Magnetic hysteresis data are reported for the bulk sediment and the 5 fractions derived from the bulk sediment. Low temperature MS data are of the 10-32 Aµm fraction and have been interpolated to the nearest degree Celsius and cleaned of outliers.
    Type: Dataset
    Format: application/zip, 2 datasets
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    DATA PANGAEA
  • 4
    facet.materialart.
    Unknown
    (Table 9.3) Chemical composition of sedimentary rocks from Station VITYAZ7425
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Calcium oxide; Calculated; Carbon dioxide; Dredge; DRG; Gas volumetric; Iron oxide, Fe2O3; Iron oxide, FeO; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Potassium oxide; Sample code/label; Sample type; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); VITYAZ7425; Water in rock; Wet chemistry; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 110 data points
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  • 5
    facet.materialart.
    Unknown
    (Table 9.1) Chemical composition of sedimentary rocks from Stations VITYAZ7420 and 7421
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Calcium oxide; Calculated; Carbon dioxide; Dredge; DRG; Elevation of event; Event label; Gas volumetric; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Potassium oxide; Sample code/label; Sample type; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); VITYAZ7420; VITYAZ7421; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 173 data points
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  • 6
    facet.materialart.
    Unknown
    (Table 2) Absolute age of Magellan Seamount Guyots
    PANGAEA
    In:  Supplement to: Rashidov, V A; Nevretdinov, E B; Selyangin, O B; Nevretdinov, Er B (2003): Geologic-geophysical investigations of Magellan Seamount Guyots, Pacific Ocean. Vestnik KRAUNC (Bulletin of Kamchanka Regional Association "Educational-Scientific Center"). Earth Sciences, No 1, 103-126
    Details
    Publication Date: 2023-05-12
    Description: This paper generalizes both original data and all available materials obtained by home and foreign researchers when studying guyots of the Magellan seamounts. The Magellan seamounts represent an extended arc-like chain of seamounts, mainly guyots within the middle part of the East-Mariana Trough. The guyots rise above the relatively flat floor of the East-Mariana Trough with depths about 5500-6000 m to the height up to 4500-4800 m and reach depth level from 1300 to 1200 m. In 1980s-1990s the Magellan seamounts become objects of permanent studies for both home and foreign researchers. First of all it is connected with the fact that considerable accumulations of Fe/Mn crusts and nodules were found at slopes and tops of the Magellan seamounts. Though having some similar features, the guyots of the Magellan seamounts differ considerably in their geological structure, time of formation and duration of volcanic activity. They were studied rather non-uniformly. The Ita-Maitai, Dalmorgeo, Roskomnedra, Vulkanolog, TIG, Hemler guyots and the Himu seamount were studied in detail, while the Nakhodka, IMGiG, TOI, DVGI guyots and the D-4 and Golden Dragonseamounts are less studied. The MA-3, MA-4, MA-10, MA-11, MA-27, MA-29, MA-31 and MA-38 guyots are very poorly studied.
    Keywords: Age, error; Age, mineral; Analytical method; Archive of Ocean Data; ARCOD; Area/locality; D-4 Seamount; Dalmorgeo Guyot; Dredge; DRG; Elevation of event; Elevation of event 2; Event label; Golden Dragon Seamount; Hemler Guyot; Himu Seamount; IOAN Guyot; Ita-Maitai Guyot; Latitude of event; Longitude of event; Nakhodka Guyot; Number of observations; Oma Vlinder Guyot; RNSN-03-01; RNSN-03-02; RNSN-03-03; RNSN-03-04; RNSN-03-05; RNSN-03-06; RNSN-03-07; RNSN-03-08; RNSN-03-09; RNSN-03-09a; RNSN-03-10; RNSN-03-11; RNSN-03-12; RNSN-03-13; RNSN-03-14; RNSN-03-15; Rock type
    Type: Dataset
    Format: text/tab-separated-values, 244 data points
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    DATA PANGAEA
  • 7
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    Unknown
    Tab. 1: Meerfelder Maar Drilling B4, stratigraphy and sequence of the lake sediments (pdf 215 kB)
    PANGAEA
    In:  Supplement to: Negendank, Jörg F W; Büchel, Georg; Hansen, R B; Hofmann, W; Irion, G; Haverkamp, B; Lorenz, V; Scharf, B; Sonne, V; Usinger, H; Weiler, H (1985): The Meerfelder Maar lake deposits. Zeitschrift für Gletscherkunde und Glazialgeologie, 21, 67-70, hdl:10013/epic.42900.d002
    Details
    Publication Date: 2023-05-12
    Description: A core from Meerfelder Maar, with a basal age of 29,000 years, provides a continuous sedimentary sequence from Late-Glacial times to the present. It includes the stratigraphical marker of the Laach Pumice Tuff. Sedimentological, geochemical, palynological, palaeobiological, palaeomagnetic and palaeontological analyses permit reconstructions of the history of the lake and its catchment area, and hence of the climate of the region, to be made. The discovery of Middle Oligocene marine, detrital fossils in the maar sediments provides insights into the palaeogeography of the Eifel region during Tertiary times.
    Keywords: B4; DRILL; Drilling/drill rig; Meerfelder Maar, Germany
    Type: Dataset
    Format: application/pdf, 215.7 kBytes
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  • 8
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    Unknown
    Annotated record of the detailed examination of Mn deposits from DSDP Leg 40 (Hole 361) (1978)
    PANGAEA
    In:  Supplement to: Bolli, Hans M; Ryan, William B F; Foresman, J B; Hottman, W E; Kagami, H; Longoria, J F; McKnight, B K; Melguen, M; Natland, J; Proto-Decima, F; Siesser, W G (1978): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XL, 1079 pp, https://doi.org/10.2973/dsdp.proc.40.1978
    Details
    Publication Date: 2023-08-28
    Description: From a structural and morphological point of view, the continental margin of southwestern Africa is a middle-aged "pull-apart" or "passive-type" margin which was initially created during the breakup of the supercontinent of Gondwanaland in the Mesozoic. The most important objective of the Leg 40 expedition was the attainment of strata laid down when the newly formed ocean was very young and only a few hundred kilometers wide. Site 361 was drilled at the fall of continental platform into the Cape Basin, to a sub-sea floor depth of 1314 meters and yielded sediments that range in age from upper Eocene to lower Aptian and possibly slightly older.
    Keywords: 40-361; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; File name; Glomar Challenger; Identification; Leg40; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Atlantic; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Magnetic susceptibility at different grain sizes of core top samples from the EDISTO Array (2019)
    PANGAEA
    Details
    Publication Date: 2023-07-11
    Keywords: 79US/Fr; after Woodruff & McManus (1966); CALYPSO; Calypso Corer; Coercivity; Coercivity of remanence; Core; CORE; Core-01; Core-02; Core-03; Core-05; Core-06; Core-07; Core-08; Core-10; Core-11; Core-12; Core-13; Core-14; Core-15; Core-16; Core-17; Core-18; Core-19; Core-21; Core-22; Core-24; Core-25; Core-27; Core-28; Core-29; Core-30; Core-32; Core-34; Core-35; Core-36; Core-37; Core-38; Core-39; Core-40; Core-41; Core-42; Core-44; Core-45; Core-47; Core-48; Core-49; Core-50; Core-51; Core-52; Core-53; Core-54; Core-55; Core-60; Core-61; Core-62; Core-63; Core-64; Core-67; Core-68; Core-69; Core-71; Core-72; Core-73; Core-74; Core-76; Core-77; Core-82; Core-83; Core-84; Core-86; Core-87; Core-88; Core-93; Core-94; Core-96; Core-97; DEPTH, water; EDISTO-01; EDISTO-02; EDISTO-03; EDISTO-05; EDISTO-06; EDISTO-07; EDISTO-08; EDISTO-10; EDISTO-11; EDISTO-12; EDISTO-13; EDISTO-14; EDISTO-15; EDISTO-16; EDISTO-17; EDISTO-18; EDISTO-19; EDISTO-21; EDISTO-22; EDISTO-24; EDISTO-25; EDISTO-27; EDISTO-28; EDISTO-29; EDISTO-30; EDISTO-32; EDISTO-34; EDISTO-35; EDISTO-36; EDISTO-37; EDISTO-38; EDISTO-39; EDISTO-40; EDISTO-41; EDISTO-42; EDISTO-44; EDISTO-45; EDISTO-47; EDISTO-48; EDISTO-49; EDISTO-50; EDISTO-51; EDISTO-52; EDISTO-53; EDISTO-54; EDISTO-55; EDISTO-60; EDISTO-61; EDISTO-62; EDISTO-63; EDISTO-64; EDISTO-67; EDISTO-68; EDISTO-69; EDISTO-71; EDISTO-72; EDISTO-73; EDISTO-74; EDISTO-76; EDISTO-77; EDISTO-82; EDISTO-83; EDISTO-84; EDISTO-86; EDISTO-87; EDISTO-88; EDISTO-93; EDISTO-94; EDISTO-96; EDISTO-97; Event label; Hysteresis, saturation magnetization; Hysteresis, saturation remanence; IMAGES V; Latitude of event; Longitude of event; Magnetic susceptibility; Marion Dufresne (1995); MD114; MD99-2269; N.Iceland shelf, Reykjafjardarall; Norwegian-Greenland Sea; Optional event label; Size fraction
    Type: Dataset
    Format: text/tab-separated-values, 2400 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
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    Unknown
    (Table 3) Minor element content in ODP Hole 127-797B (1992)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 127-797B; Arsenic; Barium; Copper; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Japan Sea; Joides Resolution; Layer description; Lead; Leg127; Molybdenum; Nickel; Ocean Drilling Program; ODP; Rubidium; Sample code/label; Strontium; Sulfur, total; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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