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  • 1
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    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad | Supplement to: Emelyanov, Emelyan M; Kravtsov, Victor A (2007): Cause of elevated As concentrations in the Baltic Sea and Vistula Lagoon. Geochemistry International, 45(8), 798-815, https://doi.org/10.1134/S001670290708006X
    Publication Date: 2023-05-12
    Description: As is less toxic than Hg, Cd, Pb, Se, Zn, and Cu. The As clarke for clays and shales is 10 ppm. Our samples of bottom sediments from Kurshskii Bay were determined to contain from 15 to 26 ppm As and up to 34 ppm As in the vicinity of the Neman River mouth. Elevated As concentrations (50-114 ppm) were detected in four columns of subsurface bottom sediments (at depths of 10-65 cm) from the Vistula Lagoon. Elevated As concentrations (50-180 ppm) were also found in a few surface samples of sand from the Gdansk Deep near oil platform D-6. These sediments are either partly contaminated with anthropogenic As or contain Fe sulfides and glauconite, which can concentrate As and contain its elevated concentrations. The As concentration in columns of bottom sediments from the Gulf of Finland were at the natural background level (throughout the columns) typical of the area (9-34 ppm). We repeatedly detected very high As concentrations (up to 227 ppm As) in politic ooze from Bornholm Deep, in the vicinity of the sunken vessel with chemical weapons. The sources of elevated As concentrations in the Baltic Sea are the following: (1) chemical weapon (CW) material buried in the floor of the Baltic Sea; (2) As-bearing pesticides, agricultural mineral fertilizers, and burned coal and other fuels; (3) kerogen-bearing Ordovician rocks exposed on the bottom; and (4) As-rich Fe sulfides brought to the area together with construction sand and gravel. This mixture was used in paper production and for the construction of hydraulic engineering facilities in the Vistula Lagoon in the early 20th century and later caused the so-called lagoon disease.
    Keywords: Archive of Ocean Data; ARCOD; Baltic Sea, Bornholm Deep; Baltic Sea, Gdansk Deep; Baltic Sea, Gulf of Finland; Baltic Sea, northern part; GC; GF-2; GF-4; GRAB50; Gravity corer; Kas; NC; Niemistoe corer; Ocean-50 grab; PSH-4027; PSH-4803; PV-1
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-05-12
    Keywords: AAK_1950-99; AK1-1; AK1-10; AK1-11; AK1-12; AK1-2; AK1-3; AK1-5; AK1-7; AK1-8; AK3-100; AK3-101-2; AK3-108; AK3-121; AK3-130; AK3-136; AK3-137; AK3-138; AK3-140; AK3-141; AK3-142; AK3-143; AK3-143-2; AK3-144; AK3-145; AK3-147; AK3-150-3; AK3-151; AK3-152; AK3-153; AK3-156; AK3-157; AK3-158; AK3-159; AK3-160; AK3-161; AK3-161-2; AK3-163; AK3-164; AK3-166; AK3-167; AK3-168; AK3-170-2; AK3-171; AK3-175; AK3-185; AK3-203; AK3-205; AK3-208; AK3-209; AK3-210; AK3-211-3; AK3-39; AK3-50; AK3-51; AK3-52; AK3-53-2; AK3-53-3; AK3-54; AK3-55; AK3-56; AK3-59-2; AK3-68; AK3-87-2; AK3-95; AK3-97; AK3-98; AK3-99; AK5-327-1; AK5-328-2; AK5-332-2; AK5-333-2; AK5-337-2; AK5-340-2; AK5-345; AK5-351; AK5-352-2; AK5-356; AK5-362; AK5-366-2; AK5-375; AK5-376-2; AK5-377-2; AK5-378; AK5-400-2; AK5-402; AK5-403; AK5-405; AK5-414; AK5-416-2; AK5-419; AK5-421-2; AK5-421-3; AK6-431-1; AK6-431-3; AK6-432-5; AK6-434; AK6-434-2; AK6-435; AK6-436; AK6-439; AK6-440; AK6-441; AK6-441-2; AK6-441-4; AK6-441-6b; AK6-441-8; AK6-441-D-2; AK6-441-D-3; AK6-443-D-9; AK6-445-2; AK6-447-3; AK6-448; Akademik A Kovalyevskiy; Akademik Kurchatov; Akademik Vavilov; AKov_1960-353K; AKov_1960-356K; AKov_1960-357K; AKov_1960-363K; AKov_1960-364K; AKov_1960-366K; AKov_1960-367K; AKov_1960-368K; AKov_1960-369K; AKov_1960-370K; AKov_1960-373K; AKov_1960-376K; AKov_1960-377K; AKov_1960-378K; AKov_1960-414K; AKov_1960-415K; AKov_1960-4K; AKov_1960-5K; AKov_1960-6K; AKov_1960-798K; AKov_1960-799K; AKov_1960-800K; AKov_1960-8K; AKU1; AKU3; AKU5; AKU6; AkV-1; AkV-1-293; AkV-1-294; AkV-1-296; AkV-1-299; AkV-1-303; AkV-1-304; AkV-1-307; AkV-1-308; AkV-1-310; AkV-1-311; AkV-1-313; AkV-1-316; AkV-1-317; AkV-1-318; AkV-1-319; AkV-1-320; AkV-1-323; AkV-1-325; AkV-1-328; AkV-1-332; AkV-1-334; AkV-1-336; AkV-1-340; AkV-1-341; AkV-1-342; AkV-1-343; AkV-1-345; AkV-1-346; AkV-1-347; AkV-1-348; AkV-1-349; AkV-1-350; AkV-1-351; AkV-1-352; AkV-1-354; AkV-1-355; AkV-1-356; AkV-1-359; AkV-1-360; AkV-1-362; AkV-1-363; AkV-1-366; AkV-1-368; AkV-1-370; AkV-1-373; AkV-1-374; AkV-1-375; AkV-1-376; AkV-1-378; AkV-1-380; AkV-1-381; AkV-1-384; AkV-1-385; AkV-1-387; AkV-1-389; AkV-1-390; AkV-1-391; AkV-1-393; AkV-1-394; AkV-1-395; AkV-1-396; AkV-1-397; AkV-1-398; AkV-1-399; AkV-1-400; AkV-1-402; AkV-1-403; AkV-1-405; AkV-1-406; AkV-1-408; AkV-1-410; AkV-1-411; AkV-1-412; AkV-1-415; AkV-1-416; AkV-1-417; AkV-1-418; AkV-2; AkV-2-429; AkV-2-437; AkV-2-446; AkV-2-448; AkV-2-452; AkV-2-453; AkV-2-454; AkV-2-457; AkV-2-460; AkV-2-463; AkV-2-464; AkV-2-466; AkV-2-467; AkV-2-468; AkV-2-469; AkV-2-470; AkV-2-471; AkV-2-473; AkV-2-474; AkV-2-475; AkV-2-478; AkV-2-479; AkV-2-480; AkV-2-482; AkV-2-487; AkV-2-489; AkV-2-490; AkV-2-491; AkV-3; AkV-3-514; AkV-3-515; AkV-3-516; AkV-3-517; AkV-3-518; AkV-3-519; AkV-3-521; AkV-3-522; AkV-3-527; AkV-3-529; AkV-3-531; AkV-3-535; AkV-3-536-1; AkV-3-536-2; AkV-3-536-3; AkV-3-538; AkV-3-539; AkV-3-540; AkV-3-541; AkV-3-548; AkV-3-551; AkV-3-552; AkV-3-553; AkV-3-554; AkV-3-555; AkV-3-556; AkV-3-557; AkV-3-558; AkV-3-561; AkV-3-562; AkV-3-568; AkV-3-569; AkV-3-571; AkV-3-576-1; AkV-3-576-2; AkV-3-576-3; AkV-3-577; AkV-3-578-1; AkV-3-578-2; AkV-3-578-3; AkV-3-578-4; AkV-3-582; AkV-3-583; AkV-3-584; AkV-3-594; AkV-3-595; AkV-3-596; AkV-3-598; AkV-3-599; AkV-3-601; AkV-3-602; AkV-4; AkV-4-703; AkV-4-707; AkV-4-711; AkV-4-715; AkV-4-722; AkV-4-724; AkV-4-725; AkV-4-726; AkV-4-727; AkV-4-729; AkV-4-735; AkV-4-739; AkV-4-741; AkV-4-742; AkV-4-743; AkV-4-752; AkV-4-756; AkV-4-759; AkV-4-764; AkV-4-764a; AkV-4-765; AkV-4-767; AkV-4-771; AkV-4-778; AkV-4-779; AkV-4-782; AkV-4-784; AkV-4-789; AkV-4-794; AkV-4-795; AkV-4-797; AkV-4-804; AkV-4-805; AkV-4-807; AkV-4-808; AkV-4-809; AkV-4-811; AkV-4-812; AkV-4-813; AkV-4-814; AkV-4-815; AkV-4-816; AkV-4-817; AkV-4-818; AkV-4-819; AkV-4-824; AkV-4-825a; AkV-4-828; AkV-4-829; AkV-4-833; AkV-4-834; AkV-4-835; AkV-4-837; AkV-4-839; AkV-4-840; AkV-4-841; AkV-4-842; AkV-4-844; AkV-4-846; AkV-4-847; AkV-5; AkV-5-1000; AkV-5-1006; AkV-5-1007; AkV-5-1008; AkV-5-1009; AkV-5-1010; AkV-5-1011; AkV-5-1012; AkV-5-1013; AkV-5-1015; AkV-5-1016; AkV-5-1017; AkV-5-1018; AkV-5-1021; AkV-5-1023; AkV-5-1024; AkV-5-1025; AkV-5-1026; AkV-5-1027; AkV-5-1028; AkV-5-1032; AkV-5-1033; AkV-5-1034; AkV-5-1035; AkV-5-1036; AkV-5-1037; AkV-5-1038; AkV-5-1039; AkV-5-1040; AkV-5-1042; AkV-5-1046; AkV-5-1047; AkV-5-1048; AkV-5-1049; AkV-5-1052; AkV-5-1053; AkV-5-1056; AkV-5-1058; AkV-5-1059; AkV-5-1060; AkV-5-1062; AkV-5-1065; AkV-5-1069; AkV-5-1070; AkV-5-1072; AkV-5-907; AkV-5-952; AkV-5-954; AkV-5-956; AkV-5-959; AkV-5-960; AkV-5-961; AkV-5-973; AkV-5-979; AkV-5-981; AkV-5-982; AkV-5-996; AkV-8; AkV-8-1319; AkV-8-1320; AkV-8-1321; AkV-8-1328; AkV-8-1330; AkV-8-1331; AkV-8-1334; AkV-8-1338; AkV-8-1339; AkV-8-1340; AkV-8-1342; AkV-8-1344; AkV-8-1346; AkV-8-1347; AkV-8-1348; AkV-8-1351; AkV-8-1352; AkV-8-1353; AkV-8-1357; AkV-8-1358; AkV-8-1359; AkV-8-1360; AkV-8-1361; AkV-8-1362; AkV-8-1363; AkV-8-1364; AkV-8-1366; AkV-8-1367; AkV-8-1368; AkV-8-1370; AkV-8-1371; AkV-8-1372; AkV-8-1374; AkV-8-1375; AkV-8-1376; AkV-8-1377; AkV-8-1378; AkV-8-1379; AkV-8-1380; AkV-8-1381; AkV-8-1383; AkV-8-1384; AkV-8-1386; AkV-8-1387; AkV-8-1388; AkV-9; AkV-9-1417; AkV-9-1419; AkV-9-1423; AkV-9-1437; AkV-9-1439; AkV-9-1443; AkV-9-1444; AkV-9-1450; AN4177-M-1965; AN4177-M-2002; AN4177-M-2003; AN4177-M-2026; AN4177-M-2062; AN4177-M-2123; AN4177-M-2124; AN4177-M-2125; AN4177-M-2137; AN4177-M-2138; AN4177-M-2176; AN4177-M-2183; AN4177-M-2189; AN4177-M-2204; AN4177-M-2206; AN4177-M-2207; AN4177-M-2208; AN4177-M-2209; AN4177-M-2213; AN4177-M-2224; AN4177-M-2236; AN4177-M-2248; AN4177-M-2249; AN4177-M-2254; AN4177-M-2255; AN4177-M-2264; AN4177-M-2289; AN4177-M-2290; AN4177-M-2292; AN4177-M-2293; AN4177-M-2294; AN4177-M-2326; AN4177-M-2331; AN4177-M-2332; AN4177-M-2334; AN4177-M-2336; AN4177-M-2352; AN4177-M-2358; AN4177-M-2359; AN4177-M-2360; AN4177-M-2361; AN4178-M-1005; AN4178-M-1007; AN4178-M-1009; AN4178-M-1010; AN4178-M-1011; AN4178-M-1012; AN4178-M-1021; AN4178-M-1022; AN4178-M-1023; AN4178-M-1024; AN4178-M-1026; AN4178-M-1027; AN4178-M-1030; AN4178-M-1031; AN4178-M-1071; AN4178-M-1072; AN4178-M-1073; AN4178-M-1074; AN4178-M-1075; AN4178-M-1077; AN4178-M-1080; AN4178-M-1083; AN4178-M-1096; AN4178-M-1097; AN4178-M-1098; AN4178-M-1099; AN4178-M-1105; AN4178-M-1105a; AN4178-M-1108; AN4178-M-1112; AN4178-M-1113; AN4178-M-1114; AN4178-M-1115; AN4178-M-1117; AN4178-M-1119; AN4178-M-1121; AN4178-M-1124; AN4178-M-1127; AN4178-M-1129; AN4178-M-1130; AN4178-M-1133; AN4178-M-1134; AN4178-M-1139; AN4178-M-1140; AN4178-M-1141; AN4178-M-1142; AN4178-M-1143; AN4178-M-1145; AN4178-M-1148; AN4178-M-1149; AN4178-M-1150; AN4178-M-1151; AN4178-M-1152; AN4178-M-1153; AN4178-M-1154; AN4178-M-1155; AN4178-M-1156; AN4178-M-1157; AN4178-M-1158; AN4178-M-1160; AN4178-M-1161; AN4178-M-1162; AN4178-M-1163; AN4178-M-1164; AN4178-M-1165; AN4178-M-1166; AN4178-M-1170; AN4178-M-1171; AN4178-M-1172; AN4178-M-1173; AN4178-M-1174; AN4178-M-1175; AN4178-M-1186; AN4178-M-1187; AN4178-M-1188; AN4178-M-1189; AN4178-M-1964; AN8002-1965; AN8002-566; AN8002-581; AN8002-587; AN8002-591; AN8002-592; AN8002-602; AN8002-603; AN8002-604; AN9013-9; AN9013-9-509; AN9013-9-511; AN9013-9-512; AN9013-9-517; AN9013-9-520; AN9013-9-531; AN9013-9-533; AN9013-9-545; AN9013-9-550; AN9086-8; AN9086-8-129; AN9086-8-13; AN9086-8-14; AN9086-8-166; AN9086-8-18; AN9086-8-19; AN9086-8-21; AN9086-8-22; AN9086-8-24; AN9086-8-28; AN9086-8-287; AN9086-8-33; AN9086-8-398; AN9086-8-415; AN9086-8-469; AN9086-8-525; AN9086-8-558; AN9086-8-6; AN9086-8-660; AN9086-8-661; AN9086-8-663; AN9086-8-665; AN9086-8-667; AN9086-8-669; AN9086-8-7; AN9086-8-703; AN9086-8-705; AN9086-8-711; AN9086-8-712; AN9086-8-729; AN9086-8-730; AN9086-8-737; AN9086-8-739; AN9086-8-743; AN9086-8-744; AN9086-8-780; AN9086-8-781; AN9086-8-782; AN9086-8-783; AN9086-8-784; AN9086-8-785; AN9086-8-786; AN9086-8-787; AN9086-8-788; AN9086-8-789; AN9086-8-790; AN9086-8-792; AN9086-8-820; AN9086-8-842; AN9086-8-9; AN-Bel-1; AN-
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Emelyanov, Emelyan M; Trimonis, Egidius S; Boström, Kurt; Yuspina, L F; Vaikutene, G; Lei, G (2001): Sedimentation in the West Gotland Basin, Baltic Sea (from the data of Core PSh-2537). Translated from Okeanologiya, 2001, 41(6), 910-923, Oceanology, 41(6), 873-885
    Publication Date: 2023-05-12
    Description: We studied the grain-size, mineral and chemical compositions, physical properties, radiocarbon age, spore-pollen spectra, and diatom composition in sediments from Core PSh24-2537 sampled in the West Gotland Basin. Four lithological-stratigraphic units were distinguished: varved clays of the Baltic Ice Lake, black and black-gray (sulfide) clays of the Yoldian Sea, gray clays of Ancylus Lake, and greenish-gray sapropel-like littorine and post-littorine silts of the marine stage of Holocene. These units differ from each other both in their matter composition and in plant remains. In the littorine silts organic carbon concentra¬tion reached from 1.5 to 10.35%. Conditions of sediment accumulation and the stages of evolution of the West Gotland Basin over the post-glacial time are characterized.
    Keywords: Archive of Ocean Data; ARCOD; GC; Gotland Basin, Baltic Sea; Gravity corer; PSh24-2537
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: El'tsina, Galina N; Emelyanov, Emelyan M (1975): Relationship between mineral, chemical and grain size composition of recent biogenic carbonate sediments (on example of the Atlantic Ocean). Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 10(5), 3-15
    Publication Date: 2023-05-12
    Description: This work was based on a study of the upper layer of recent carbonate bottom sediments of the Atlantic Ocean. Biogenic carbonate of recent sediments is represented by metastable and stable minerals. In the ocean metastable phases can exist indefinitely long, but the structure of polymorphism determines inevitability of transformation of metastable phases into stable ones. This transformation occurs in the solid phase. In the absence of a critical point between the two phases of the transition process is not available for study by microscopic methods. It is estimated indirectly by studying the nature and extent of changes in mineral and chemical compositions. With aging of sediments their mineral composition alters in direction of increasing contents of resistant minerals. Fine grained sediments and fractions are subject to more intensive effects of early diagenesis processes, rather than coarse ones; this is reflected in their mineral composition. Regularities of distribution of carbonate minerals in size fractions consistent with the direction of polymorphic transformations in calcium carbonate. Such transformations can occur in a particular dimension of grains. Concrete grain size depends on environmental conditions. This situation explains presence of metastable biogenic carbonates at different depths of the ocean and suggests presence of diagenetic calcite in sediments occurring below expected for each case depth of the transition.
    Keywords: AK3-144; AK3-210; AK3-99; Akademik Kurchatov; AKU3; AN9086-8; AN9086-8-469; Archive of Ocean Data; ARCOD; AtlantNIRO-SRTR-9086; Bel2; Bel2-1; Bel2-12; Bel2-13; Bel2-18; Bel2-19; Bel2-2; Bel2-36; Bel2-4; Bel2-49; Bel2-52; Bel2-54; Bel2-69; Bel2-75; Bel2-8; Belogorsk; Grab; GRAB
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Kuptsov, Vladimir M; Emelyanov, Emelyan M; Shimkus, Kazimir M; Grakova, Irina V; Chabashvili, Sergey V (1981): New radiocarbon age determinations of bottom sediments and the sedimentation rates in the Mediterranean Sea. Oceanology, 21(3), 365-370
    Publication Date: 2023-05-12
    Description: Bottom sediment samples were collected in the Central Mediterranean, Southern Adriatic, Tyrrhenian, Algerian-Provencal, and Alboran basins of the Mediterranean Sea. Fifty-six datings were done for 12 sediment cores. The lowest sedimentation rates during Holocene were found on the abyssal plain of the Algerian-Provencal basin (2.4-4.0 cm/ky). In the Southern Adriatic, Tyrrhenian, and Alboran basins sedimentation rates were somewhat higher (6-12 cm/ky). On slopes of the Southern Adriatic and Tyrrhenian basins during Late Würm glaciation rates of "normal" sedimentation were within the range 11.8-26.8 cm/ky.
    Keywords: Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; VITYAZ; Vityaz_14712; Vityaz (ex-Mars); Vityaz-65; VITYAZ7908; VITYAZ7910; VITYAZ7912; VITYAZ7917; VITYAZ7918; VITYAZ7927; VITYAZ7928; VITYAZ7930; VITYAZ7931; VITYAZ7935; VITYAZ7937
    Type: Dataset
    Format: application/zip, 11 datasets
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Emelyanov, Emelyan M (1992): The sediments of the anoxic basins of the Mediterranean Sea. Oceanology, 32(3), 382-388
    Publication Date: 2023-05-12
    Description: Biomass and size structure of planktic infusoria communities were investigated in March 1987 at nine stations on a 370 mile transect across the coastal upwelling zone, the California current, and subtropical waters. Infusoria compose up to 71-92% of total biomass of heterotrophic micro- and nannoplankton; their biomass was 0.6-2.0 g/m**2 in the 0-200 m layer. Distinctive characteristics of taxonomic and size structures were of great diversity of microplanktic Stormbilidiwn forms, comparatively low abundance of tintinnids, and high abundance of nannoplanktic infusoria that accounted for 26-54% of biomass.
    Keywords: AMK20-2127; AMK20-2128; AMK20-2129; AMK20-2130; AMK20-2132; Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; OKEAN; Okean Grab
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Lisitzin, Alexander P; Bogdanov, Yury A; Emelyanov, Emelyan M; Maksimov, A N; Pustelnikov, Oleg S; Serova, Valentina V; Lukoshevitchus, L S; Soldatov, A V; Ilin, Alexander V; Koshelev, V A; Litvin, Vladimir M; Senin, YuM; Svirenko, Inna P; Shurko, Y I (1975): Osadkonakoplenie v Atlanticheskom Okeane (Sedimentation in the Atlantic Ocean). Kaliningradskaya Pravda (Kaliningrad), 462 pp
    Publication Date: 2023-05-12
    Description: The book summarizes data on distribution and composition of sedimentary material suspended in waters of the Atlantic Ocean and its seas. Results of observations of Soviet and foreign expeditions are given. Distribution of suspended matter in sections across the ocean, as well as in the most studied seas are shown. New data on grain size, mineral and chemical composition of suspended matter are published. Summary of history of investigation of bottom sediments from the Atlantic Ocean from the first scientific cruises to the present is done. A brief description of sediment types in the ocean and a detailed description of Mediterranean Sea sediments are given.
    Keywords: AAK_1950-99; Akademik A Kovalyevskiy; Akademik Vavilov; AKov_1960-377K; AKov_1960-414K; AkV-1; AkV-1-299; AkV-1-304; AkV-1-310; AkV-1-311; AkV-1-316; AkV-1-317; AkV-1-318; AkV-1-319; AkV-1-334; AkV-1-343; AkV-1-351; AkV-1-359; AkV-1-380; AkV-1-384; AkV-1-387; AkV-1-390; AkV-1-394; AkV-1-396; AkV-1-398; AkV-1-405; AkV-1-406; AkV-1-408; AkV-1-410; AkV-1-411; AkV-1-412; AkV-1-415; AkV-1-416; AkV-1-417; AkV-3; AkV-3-518; AkV-3-536-1; AkV-3-583; AkV-3-594; AkV-3-595; AkV-4; AkV-4-726; AkV-4-741; AkV-4-742; AkV-4-764a; AkV-4-767; AkV-4-812; AkV-4-837; AkV-4-839; AkV-4-840; AkV-4-841; AkV-4-844; AkV-5; AkV-5-1065; AkV-5-1069; AkV-8; AkV-8-1321; Archive of Ocean Data; ARCOD; Atlantic Ocean; Grab; GRAB; Indian Ocean; MULT; Multiple investigations; Ob; Ob2; Ob2-13; Ob2-231WS; Ob2-232SM; Ob2-240WS; Ob2-243; Ob2-250SM; Ob2-253WS; Ob2-260SM; Ob2-261; Ob2-264WS; Ob2-s39; Ob2-s49; Ob2-s68; Ob3; Ob3-102; Ob3-110; Ob3-111; Ob3-458WS; Ob3-459WS; Ob3-464WS; Ob3-465SM; Ob3-469WS; Ob3-491WS; Ob3-499WS; Ob3-88; Ob3-89; Ob3-90; Ob3-92; Ob3-93; Ob3-95; Ob3-99; Ob4; Ob4-1; Ob4-27; Ob4-28; Ob4-29; Ob4-3; Ob4-30; Ob4-31; Ob4-32; Ob4-33; Ob4-34; Ob4-35; Ob4-38; Ob4-4; Ob4-41; Ob4-43; Ob4-44; Ob4-45; Ob4-46; Ob4-47; Ob4-48; Ob4-5; Ob4-6; Ob4-7; Ob4-8; OKEAN; Okean Grab; SAO75-1034; SAO75-1069; SAO75-1404; SAO75-344; SAO75-346; SAO75-351; SAO75-356; SAO75-735; SAO75-798; SAO75-814; SAO75-875; SAO75-988; SAO75-992; SAO75-995; SEPAR; Separator; Vityaz (ex-Mars); Vityaz-33; VITYAZ4779; Water sample; WS
    Type: Dataset
    Format: application/zip, 20 datasets
    Location Call Number Expected Availability
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  • 8
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad | Supplement to: Emelyanov, Emelyan M (1998): Bar'ernye Zony v Okeane (Barrier Zones in the Ocean). Yantarny Skaz (Kaliningrad), 416 pp
    Publication Date: 2023-05-12
    Description: Geochemical barrier zones play an important role in determining various physical systems and characteristics of oceans, e.g. hydrodynamics, salinity, temperature and light. In the book each of more than 30 barrier zones are illustrated and defined by physical, chemical and biological parameters. Among the topics discussed are processes of inflow, transformation and precipitation of the sedimentary layer of the open oceans and more restricted areas such as the Baltic, Black and Mediterranean Seas.
    Keywords: AK1-39; AK3-144; AK3-145; AK3-150-3; AK3-152; AK3-157; AK3-159; AK3-163GC; AK3-185; AK3-205; AK3-210; AK3-51; AK3-54; AK3-56; AK44-5000; AK44-5001; AK44-5002; AK44-5002-2; AK5-414; AK6-435; Akademik Kurchatov; AKU1; AKU3; AKU5; AKU6; AMK20-2129; AN8002-1965; AN8002-581; AN8002-602; AN9086-8; AN9086-8-729; AN9086-8-737; AN9086-8-739; AN9086-8-744; AN9086-8-780; AN9086-8-789; AN-Bel-1; AN-Bel-1-611; AN-Bel-1-636; AN-Bel-1-654; AN-Bel-1-657; Angola Basin; Archive of Ocean Data; ARCOD; AtlantNIRO-RTM-Belogorsk; AtlantNIRO-SRTM-8002; AtlantNIRO-SRTR-9086; Baltic Sea; Benguela Upwelling; East Atlantic; East Equatorial Atlantic; GC; Grab; GRAB; Gravity corer; Mediterranean Sea; MULT; Multiple investigations; Namibian shelf; OKEAN; Okean Grab; Vit20; Vityaz-2; Vy20-3171; Vy20-3175BC; Vy20-3180; Vy20-3180W; Vy20-3182; Vy20-3186; Vy20-3190; Vy20-3191; Vy20-3192; Vy20-3196; Vy20-3197; Vy20-3199; Vy20-3218; Vy20-3221; Vy20-3226; Vy20-3228; Vy20-3229; Water sample; WS
    Type: Dataset
    Format: application/zip, 17 datasets
    Location Call Number Expected Availability
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  • 9
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad | Supplement to: Emelyanov, Emelyan M; Blazhchishin, A I; Kharin, Gennady S (1976): On the role of endogenic sources in formation of chemical composition of bottom sediments from the North Atlantic. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 11(5), 3-21
    Publication Date: 2023-05-12
    Description: Results of study of bottom sediments near Iceland and on the Jan Mayen Island are reported. It was found that in recent sediments chemical elements are mainly associated with pyro- and volcanoclastics. In some areas adjusted to deep-seated faults ancient iron-manganese crusts and sediments occur. They are rich in Ni, Co, V, Cu, Mo, Cd and other elements associated with endogenic matter.
    Keywords: AK15-1343-1; AK15-1349; AK15-1363; AK15-1364; Akademik Kurchatov; AKU15; Archive of Ocean Data; ARCOD; Dredge; DRG; GC; Gravity corer; Jan Mayen transform fracture zone; KhP-769; Kolbeinsey Ridge; North Atlantic
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Expected Availability
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  • 10
    facet.materialart.
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad | Supplement to: Emelyanov, Emelyan M (2011): Ferromanganese ore process in the Baltic Sea. Translated from Litologiya i Poleznye Iskopaemye, 2011, 3, 227-248, Lithology and Mineral Resources, 46(3), 199-219, https://doi.org/10.1134/S0024490211030035
    Publication Date: 2023-05-12
    Description: In depressions of the Baltic Sea, where the bottom is periodically marked by stagnation, silt contains as much as 5% Mn (up to 17% in some layers) and 9-10% Corg. Silt in such depressions is laminated. The marine sediment sequence is stratified due to influx of ocean water into the sea: upper layers are oxic, while lower (near-bottom) layers are hydrosulfuric. The boundary between them is represented by the transitional O2-H2S layer. This zone (redox barrier) is marked by drastic variation in Eh. The zone below this barrier is characterized by accumulation of huge amounts of dissolved manganese Mn(II) and iron Fe(II), which diffuse from the hydrosulfuric layer into the oxic layer under influence of the gradient and precipitated as suspension with as much as 15% Fe and 45% Mn. When fresh oxygenated saline water is transported to the depressions the hydrosulfuric setting gives way to oxic one and dissolved elements are transformed into particulate phases as hydroxides and geologically instantly precipitated at the bottom. After 5-10 yr setting changes; hydrogen sulfide is again delivered to water column from the bottom. This is accompanied by supply of dissolved Mn(II) and Fe(II) previously accumulated as gel-type sediment on the bottom. Thus, the cycle of elements is repeated. The latter, however, is not completely dissolved. Some portion remains on the bottom as black rhodochrosite microlayers (laminas) that contain as much as 29% Mn. The black laminas accumulated during aeration include remains of bottom foraminifers. In addition, the bottom comprises pale diatom laminas and brownish gray varieties composed of clayey and organic substances. Bulk samples of the laminated silt contain as much as 12.9% Mn or 26.9% MnCO3. Depressions in the Baltic Sea represent an unique site of the Earth marked by accumulation of carbonate-manganiferous sediments at present. We believe that Oligocene manganese carbonate-oxide ores described by N.M. Strakhov and co-authors were accumulated in the same manner. Compositions of manganiferous sediments in the Baltic region and some ancient ores in Europe are compared. The author studied five stages of Mn accumulation and sediment transformation into ores.
    Keywords: Archive of Ocean Data; ARCOD
    Type: Dataset
    Format: application/zip, 2 datasets
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