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  • PANGAEA  (149)
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  • 1
    facet.materialart.
    Unknown
    (Table 1) Hydrochemical parameters of water and ice from the North Dvina River and its tributaries (2010)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Alkalinity, total; Archive of Ocean Data; ARCOD; Belaya River (tributary of Pinega); Carbon, organic, dissolved; Chloride; Creek from the llasskoe bog; Date; Event label; Ilasskoe bog; Karasozero Lake; Karelka River; Karmozero Lake; Karst depression; Kelda River; Latitude of event; Location of event; Longitude of event; North Dvina River; North Dvina River, Maimaksa Channel; North Dvina River at Lapominka; North Dvina River at Myudyug Island; North Dvina River at Ust-Pinega; Period; pH; pH meter (Orion); Pinega River; Pinega River at Golubino; Polta River; Saint Spring; Sample comment; Sotka River; Sulfate; Temperature, water; Thermometer; Titration; VSh-A-1; VSh-A-10; VSh-A-11-12; VSh-A-13; VSh-A-14; VSh-A-15; VSh-A-16; VSh-A-17; VSh-A-18; VSh-A-19; VSh-A-2; VSh-A-20; VSh-A-21; VSh-A-22; VSh-A-23; VSh-A-24; VSh-A-25; VSh-A-26; VSh-A-27; VSh-A-28; VSh-A-29; VSh-A-3; VSh-A-30; VSh-A-31; VSh-A-32; VSh-A-33; VSh-A-34; VSh-A-35; VSh-A-36; VSh-A-37; VSh-A-38; VSh-A-39; VSh-A-3-F; VSh-A-3-J; VSh-A-4; VSh-A-40; VSh-A-41; VSh-A-42; VSh-A-43; VSh-A-44; VSh-A-5; VSh-A-6; VSh-A-7; VSh-A-8; VSh-SD; Water sample; Wet combustion; WS
    Type: Dataset
    Format: text/tab-separated-values, 466 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    (Table 2) Concentrations of chemical elements in water of the North Dvina River and its tributaries (2010)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Aluminium; Antimony; Archive of Ocean Data; ARCOD; Arsenic; Barium 2+; Belaya River (tributary of Pinega); Bismuth; Boron; Cadmium; Caesium; Calcium; Cerium; Chromium; Cobalt; Copper; Creek from the llasskoe bog; Date; Dysprosium; Erbium; Europium; Event label; Gadolinium; Gallium; Germanium; Hafnium; Holmium; Ilasskoe bog; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; Karasozero Lake; Karelka River; Karmozero Lake; Karst depression; Kelda River; Lanthanum; Latitude of event; Lead; Lithium; Location of event; Longitude of event; Lutetium; Magnesium; Manganese 2+; Molybdenum; Neodymium; Nickel; North Dvina River; North Dvina River, Maimaksa Channel; North Dvina River at Lapominka; North Dvina River at Myudyug Island; North Dvina River at Ust-Pinega; Period; Pinega River; Pinega River at Golubino; Polta River; Potassium; Praseodymium; Rubidium; Saint Spring; Samarium; Sample comment; Selenium; Silicon; Sodium; Sotka River; Strontium 2+; Terbium; Thallium; Thorium; Thulium; Titanium; Tungsten; Uranium; Vanadium; VSh-A-1; VSh-A-10; VSh-A-11-12; VSh-A-13; VSh-A-14; VSh-A-15; VSh-A-16; VSh-A-17; VSh-A-18; VSh-A-19; VSh-A-2; VSh-A-20; VSh-A-21; VSh-A-22; VSh-A-23; VSh-A-24; VSh-A-25; VSh-A-26; VSh-A-27; VSh-A-28; VSh-A-29; VSh-A-3; VSh-A-30; VSh-A-31; VSh-A-32; VSh-A-33; VSh-A-34; VSh-A-35; VSh-A-36; VSh-A-37; VSh-A-3-F; VSh-A-4; VSh-A-40; VSh-A-41; VSh-A-42; VSh-A-43; VSh-A-44; VSh-A-6; VSh-A-7; VSh-A-8; VSh-SD; Water sample; WS; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 2784 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
    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
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 4
    facet.materialart.
    Unknown
    Composition of phosphate containing sediments and phosphatic grains from the Namibian shelf
    PANGAEA
    In:  Supplement to: Baturin, Gleb N; Zhegallo, E A; Isaeva, Alexandra B (1998): Formation of phosphatic grains in the sediments of the Namibian Shelf. Translated from Okeanologiya, 1998, 38(2), 260-269, Oceanology, 38(2), 235-243
    Details
    Publication Date: 2023-05-12
    Description: Recent phosphatic grains from diatomaceous oozes, as well as Pliocene grains from phosphatic sands of the Namibian shelf were studied by a scanning electron microscopy coupled with microprobe analysis. Lithification of the grains occurred together with changes in their composition and structure resulting from progressive phosphatization of biogenic material and partial crystallization of phosphatic matter, which is presented by three predominant forms: colloform, globular, and microcrystalline. Recent grains and associated nodules are authigenic. Their structure and composition related to Pliocene redeposited grains, which might be generated under similar conditions.
    Keywords: Archive of Ocean Data; ARCOD; Atlantic Ocean; Dredge; DRG; Grab; GRAB; Mikhail Lomonosov; ML26; ML26_2048; Namibian shelf; PL4-12
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Composition and fluxes of sinking particulate material and bottom sediments in the northeast Black Sea in 1998-1999
    PANGAEA
    In:  Supplement to: Rusakov, Valery Yu; Shimkus, Kazimir M; Zernova, Valentina V; Isaeva, Alexandra B; Serova, Valentina V; Karpenko, Alexandra A; Demina, Lyudmila V (2003): Distribution and composition of sedimentary matter in the northeast Black Sea. Translated from Oceanology, 2003, 43(3), 459-468, Oceanology, 43(3), 434-442
    Details
    Publication Date: 2023-05-12
    Description: For the first time deep-sea mooring stations with sediment traps were deployed in the northeast Black Sea. One sediment trap for long-term studies was located at Station 1 (44°15'N, 37°43'E, deployment depth 1800 m, depth 1900 m). The trap collected sinking sedimentary material from January to May 1998. Material collectors were changed every 15 days. Other stations with sediment traps for short-term studies (September-October 1999) were located on the shelf: Station 2 (44°16'N, 38°37'E, deployment depth 45 m, depth 50 m) and on the bottom of the canyon: Station 3 (44°16'N, 38°22'E, deployment depth 1145 m, depth 1150 m), Station 4 (44°11'N, 38°21'E, deployment depths 200, 1550, 1650 m, depth 1670 m). Collected material indicates that vertical particle fluxes are controlled by seasonal changes of in situ production and by dynamics of terrigenous matter input. Higher vertical particle flux of carbonate and biogenic silica was in spring due to bloom of plankton organisms. Maximum of coccolith bloom is in April-May. Bloom of diatoms begins in March. In winter and autumn lithogenic material dominates in total flux. Its amount strongly depends on storms and river run-off. Suspended particle material differs from surface shelf sediments by finer particles (mainly clay fraction) and high content of clay minerals and biogenic silica. This material may form lateral fluxes with higher concentration of particles transported along the bottom of deep-sea canyons from the shelf to the deep basin within the nepheloid layer. In winter such transportation of sedimentary material is more intensive due to active vertical circulation of water masses.
    Keywords: Archive of Ocean Data; ARCOD; Black Sea; ST-RSh-1; ST-RSh-2; ST-RSh-3; ST-RSh-4; Trap; TRAP
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
    facet.materialart.
    Unknown
    Lignin and chemical elements in the surface layer of bottom sediments from the Kandalaksha Bay of the White Sea
    PANGAEA
    In:  Supplement to: Peresypkin, Valery I; Lukashin, Vyacheslav N; Isaeva, Alexandra B; Prego, Ricardo (2004): Lignin and chemical elements in the sediments of Kandalaksha Bay (White Sea). Translated from Okeanologiya, 2004, 44(5), 743-755, Oceanology, 44(5), 698-709
    Details
    Publication Date: 2023-05-12
    Description: Chemical composition of the upper layer of sediments (0-1 cm) in the Kolvits and Knazhaya inlets, and also in the deep-water part of the Kandalaksha Bay is considered. It is shown that silts are richer in Fe, TOC, and heavy metals, than sands. The highest concentration of these elements is found in sediments under mixing zones of riverine and sea waters. Correlations of P, Zn, Cd, and Cu with iron are high, and correlations of Pb and Cu with organic carbon are also high. Very high concentration of Pb in the Kandalaksha Bay indicate technogenic pollution of sediments. Lignin makes significant contribution to formation of organic matter in the sediments. Composition of lignin in bottom sediments of the Kandalaksha Bay is defined by composition of lignin in soils and aerosols. Vanillin and syringyl structures prevail in molecular composition of lignin in bottom sediments. Their sources are coniferous vegetations, soils, and mosses. Ratios of certain types of phenol compounds indicate pollution of the upper layer of sediments by technogenic lignin. Lead and copper correlate well with this technogenic lignin.
    Keywords: Archive of Ocean Data; ARCOD; Grab; GRAB; Kandalaksha Bay, White Sea; Kartesh-2000-100; Kartesh-2000-101; Kartesh-2000-102; Kartesh-2000-112; Kartesh-2000-132; Kartesh-2000-141; Kartesh-2000-49; Kartesh-2000-85; Kartesh-2000-86; Kartesh-2000-91; Kartesh-2000-92; Kartesh-2000-93
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    (Table 2) Geochemistry and radionuclides of sediment core SO60-93
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AGE; Alpha spectrometry; Aluminium oxide; Beryllium-10; Beryllium-10, standard deviation; Calcium carbonate; Density, dry bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Equatorial East Pacific; HYMAS II; Iron oxide, Fe2O3; Isotope ratio mass spectrometry; KAL; Kasten corer; KLH093; Manganese oxide; Neogloboquadrina dutertrei, δ18O; Protactinium-231; Protactinium-231, standard deviation; SO60; SO60_93; Sonne; Thorium-230, supported, uncorrected; Thorium-230, supported, uncorrected standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 1426 data points
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  • 8
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    Aerosols over the East Atlantic in spring and summer 2001
    PANGAEA
    In:  Supplement to: Klyuvitkin, Alexey A; Lukashin, Vyacheslav N; Novigatsky, Alexander N; Isaeva, Alexandra B; Serova, Valentina V (2004): Mineral aerosols, their concentrations, composition and fluxes to the oceanic surface. Translated from Okeanologiya, 2004, 44(5), 756-767, Oceanology, 44(5), 710-720
    Details
    Publication Date: 2023-05-12
    Description: Data on the concentration and mineral composition of aerosols collected by nets in Cruise 18 of R/V Akadernik Fedorov on a submeridional section in the East Atlantic are presented. An empirical curve for calculating efficiency factor of a net is given for different concentrations of mineral part of aerosols. Fluxes of lithogenic part of aerosols to the sea surface are calculated. A comparison of lithogenic fluxes from the atmosphere and in the water column of the ocean showed that values of fluxes practically coincide in areas with dominating supply of dry atmospheric material. These fluxes strongly differ in the intratropical convergence zone, where deposition of aerosols depends on atmospheric precipitation, or in regions, where sedimentary material is supplied to the ocean mainly by river run-off. Residence time of aerosol lithogenic matter in the euphotic layer is calculated.
    Keywords: AF-18; AF18-A-I; AF18-A-II; AF18-A-III; AF18-A-IV; AF18-A-IX; AF18-A-V; AF18-A-VI; AF18-A-VII; AF18-A-VIII; AF18-A-X; AF18-A-XI; AF18-A-XII; AF18-A-XIII; AF18-A-XIV; AF18-A-XV; AF18-A-XVI; AF18-A-XVII; AF18-A-XVIII; Akademik Fedorov; Archive of Ocean Data; ARCOD; Atlantic Ocean; NET600; Net 600 µm 10 x 1 m**2
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 9
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    Hydrochemistry measured on water bottle samples during Akademik Vernadsky cruise AV29 (2011)
    PANGAEA
    In:  Marine Hydrophysical Institute, National Academy of Sciences of Ukraine
    Details
    Publication Date: 2023-01-13
    Keywords: Akademik Vernadsky; AV29; AV29_4265; AV29_4266; AV29_4267; AV29_4268; AV29_4269; AV29_4270; AV29_4271; AV29_4281; AV29_4282; AV29_4283; AV29_4284; AV29_4285; AV29_4286; AV29_4287; AV29_4288; AV29_4289; AV29_4290; AV29_4291; AV29_4295; AV29_4300; AV29_4314; AV29_4324; AV29_4337; Black Sea; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Event label; Hydrogen sulfide; Latitude of event; Longitude of event; Oxygen; Oxygen, Winkler (Culberson, 1991, WOCE Report 68/91); Salinity; Temperature, water; Titration
    Type: Dataset
    Format: text/tab-separated-values, 1385 data points
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  • 10
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    Biogenic Silica at niskin bottle station RSBP1995/1996-122295-12 (2004)
    PANGAEA
    Details
    Publication Date: 2023-02-24
    Keywords: Biogenic silica; Bottle, Niskin; DEPTH, water; Nathaniel B. Palmer; NBP94-06; NIS; Ross Sea; RossSeaBloomProject1995/1996; RSBP1995/1996-122295-12; Silicon Cycling in the World Ocean; SINOPS; Station#8-CTD#15
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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