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  • 1
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    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
  • 2
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    Unknown
    Organic nitrogen and organic phosphorus concentrations bays of the White Sea
    PANGAEA
    In:  Supplement to: Chugaynova, V A; Nesterova, G I; Konnov, Vitaly A; Maksimova, M P (1993): Organic nitrogen and phosphorus forms in White Sea bays. Oceanology, 33(2), 167-174
    Details
    Publication Date: 2023-05-12
    Description: Concentrations of organic and mineral nitrogen and phosphorus in waters from different types of bays were determined during summer of 1987. Content of organic nitrogen in surface waters reached 80-97% of total; content of mineral phosphorus was 60-100%. Concentrations of N_org and P_org in deep waters decreased to 70 and 40%, respectively. Distribution of organic matter in the bays was controlled by river run-off.
    Keywords: Archive of Ocean Data; ARCOD; ChC1; ChC2; ChC3; KemC1; KemC2; KemC3; KolC1; KolC2; KolC3; SorC1; SorC2; SorC3; SumiC1; SumiC2; SumiC3; VSC1; VSC2; VSC3; Water sample; White Sea; WS
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
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    Hydrochemistry measured on water bottle samples during Mikhail Lomonosov cruise ML16 (2011)
    PANGAEA
    In:  Marine Hydrophysical Institute, National Academy of Sciences of Ukraine
    Details
    Publication Date: 2023-01-13
    Keywords: Alkalinity, total; Black Sea; Bottle, Niskin; Calculated; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Event label; Hydrogen sulfide; Latitude of event; Longitude of event; Mikhail Lomonosov; ML16; ML16_1293; ML16_1294; ML16_1295; ML16_1296; ML16_1297; ML16_1298; ML16_1299; ML16_1300; ML16_1301; ML16_1302; ML16_1307; ML16_1308; ML16_1309; ML16_1310; ML16_1311; ML16_1312; ML16_1313; ML16_1314; ML16_1315; ML16_1316; ML16_1317; ML16_1318; ML16_1319; ML16_1320; ML16_1321; ML16_1321-2; ML16_1321-3; ML16_1322; ML16_1322-2; ML16_1323; ML16_1324; ML16_1325; ML16_1326; ML16_1327; ML16_1328; ML16_1329; ML16_1330; ML16_1331; ML16_1332; ML16_1333; ML16_1334; MULT; Multiple investigations; NIS; Oxygen; Oxygen, Winkler (Culberson, 1991, WOCE Report 68/91); Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2724 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 4
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    (Table 2) Salinity in bays of the White Sea
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Description: Analysis of contribution of micronodules of sand and silt size to chemical composition of various types of pelagic sediments, as well as use of published data indicate that in some types of bottom sediments micronodules are the principal carriers of manganese and nickel. These elements appear to constitute smaller fractions of colloidal iron and manganese hydroxides, as well as terrigenous material.
    Keywords: Archive of Ocean Data; ARCOD; DEPTH, water; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; MV-CB-1; MV-CB-2; MV-CB-3; MV-CB-4; MV-KeB-1; MV-KeB-2; MV-KoB-1; MV-KoB-2; MV-KoB-3; MV-PB-1; MV-PB-2; MV-SoB-1; MV-SoB-2; MV-SuB-1; MV-SuB-2; MV-SuB-3; MV-VSB-1; MV-VSB-2; MV-VSB-3; MV-VSB-4; MV-VSB-5; Salinity; White Sea, Chupa Bay; White Sea, Kem Bay; White Sea, Kolezhma Bay; White Sea, Pongoma Bay; White Sea, Soroka Bay; White Sea, Suma Bay; White Sea, Velikaya Salma Bay
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 5
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    (Table 3) Organic nitrogen and organic phosphorus concentrations the Sumi and Kolezhma coves of the White Sea
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Archive of Ocean Data; ARCOD; DEPTH, water; Elevation of event; Event label; KolC1; KolC2; KolC3; Latitude of event; Longitude of event; Nitrogen, organic; Phosphorus, organic; SumiC1; SumiC2; SumiC3; Titration; Water sample; White Sea; WS
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
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    (Table 1) Concentrations of organic carbon in bays of the White Sea
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Description: Analysis of contribution of micronodules of sand and silt size to chemical composition of various types of pelagic sediments, as well as use of published data indicate that in some types of bottom sediments micronodules are the principal carriers of manganese and nickel. These elements appear to constitute smaller fractions of colloidal iron and manganese hydroxides, as well as terrigenous material.
    Keywords: Archive of Ocean Data; ARCOD; Carbon, organic, total; DEPTH, water; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; MV-CB-1; MV-CB-2; MV-CB-3; MV-CB-4; MV-KeB-1; MV-KeB-2; MV-KoB-1; MV-KoB-2; MV-KoB-3; MV-PB-1; MV-PB-2; MV-SoB-1; MV-SoB-2; MV-SuB-1; MV-SuB-2; MV-SuB-3; MV-VSB-1; MV-VSB-2; MV-VSB-3; MV-VSB-4; MV-VSB-5; Organic carbon analyzer, Photochem E3600; White Sea, Chupa Bay; White Sea, Kem Bay; White Sea, Kolezhma Bay; White Sea, Pongoma Bay; White Sea, Soroka Bay; White Sea, Suma Bay; White Sea, Velikaya Salma Bay
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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    DATA PANGAEA
  • 7
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    (Table 1) Organic nitrogen and organic phosphorus concentrations the Velikaya Salma and Chupa coves of the White Sea
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Archive of Ocean Data; ARCOD; ChC1; ChC2; ChC3; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Nitrogen, organic; Phosphorus, organic; Titration; VSC1; VSC2; VSC3; Water sample; White Sea; WS
    Type: Dataset
    Format: text/tab-separated-values, 71 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 8
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    (Table 2) Organic nitrogen and organic phosphorus concentrations the Kem and Sorok coves of the White Sea
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Archive of Ocean Data; ARCOD; DEPTH, water; Elevation of event; Event label; KemC1; KemC2; KemC3; Latitude of event; Longitude of event; Nitrogen, organic; Phosphorus, organic; SorC1; SorC2; SorC3; Titration; Water sample; White Sea; WS
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 9
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    Salinity and concentrations of organic carbon in bays of the White Sea
    PANGAEA
    In:  Supplement to: Maksimova, M P; Vladimirskiy, S S (1990): Organic carbon and the generation of organic matter in bays of the White Sea. Oceanology, 30(1), 47-51
    Details
    Publication Date: 2023-05-12
    Description: Organic carbon in bays of the White Sea was studied for the first time in 1987. Bays of various types in the Kandalaksha Gulf and the Onega Gulf were investigated. Concentration of C_org ranged from 3.5 to 9 mg/l. The highest weighted-mean concentration of C_org occurred in shallow bays of the Onega Gulf (Suma Bay - 6.17 mg/l, Kolezhma Bay - 5.25 mg/1); slightly lower levels occurred in the Soroka Bay (4.85 mg/l) and Kem' Bay (4.78 mg/l). The lowest concentrations were in deep bays of the Kandalaksha Gulf (Chupa Bay - 4.35 mg/l, Velikaya Salma Bay - 4.10 mg/l). As a rule C_org concentration decreases with depth in deep-water bays (but increases slightly in the thermocline layer). The key factor governing organic matter concentration in the bays of the Onega Gulf with river runoff is allochthonous terrigenous organic matter, as indicated by negative correlation of C_org with salinity (R=-0.83+/-0.07, p=0.96) and nonsignificant correlation with primary production.
    Keywords: Archive of Ocean Data; ARCOD; MULT; Multiple investigations; MV-CB-1; MV-CB-2; MV-CB-3; MV-CB-4; MV-KeB-1; MV-KeB-2; MV-KoB-1; MV-KoB-2; MV-KoB-3; MV-PB-1; MV-PB-2; MV-SoB-1; MV-SoB-2; MV-SuB-1; MV-SuB-2; MV-SuB-3; MV-VSB-1; MV-VSB-2; MV-VSB-3; MV-VSB-4; MV-VSB-5; White Sea, Chupa Bay; White Sea, Kem Bay; White Sea, Kolezhma Bay; White Sea, Pongoma Bay; White Sea, Soroka Bay; White Sea, Suma Bay; White Sea, Velikaya Salma Bay
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
    Electronic Resource
    Electronic Resource
    Catalytic reduction of chloronitrobenzenes to chloroanilines (1966)
    Springer
    Russian chemical bulletin 15 (1966), S. 1830-1833 
    Details
    ISSN: 1573-9171
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Conclusions 1. Ruthenium on barium sulfate (5% Ru) is an active catalyst of the reduction of p-chloronitrobenzene to p-chloroaniline, catalyzing the reaction under optimum conditions with the yield of 99.5–99.7% p-chloroaniline, with very little splitting out of HCl (0.3–0.5%). 2. Decreasing the Ru content on BaSO4 to 1, 0.5, and 0.05% lowers the yield of p-chloroaniline. 3. The use of Al2O3 as a carrier led to an intensification of the side reaction of dehalogenation.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01179688
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