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  • Data  (84)
  • 1965-1969  (84)
  • 1955-1959
  • 1950-1954
  • 1945-1949
  • 1969  (84)
Collection
Keywords
Publisher
Years
  • 1965-1969  (84)
  • 1955-1959
  • 1950-1954
  • 1945-1949
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Cronan, David S; Tooms, J S (1969): The geochemistry of manganese nodules and associated pelagic deposits from the Pacific and Indian Oceans. Deep Sea Research and Oceanographic Abstracts, 16(4), 335-359, https://doi.org/10.1016/0011-7471(69)90003-5
    Publication Date: 2024-07-01
    Description: Chemical and mineralogical analyses of manganese nodules from a large number of widely spaced localities in the Pacific and Indian Oceans have shown that their mineralogy and chemical composition varies both areally and with depth of formation. This is considered to result from a number of factors, important among which are: (a) their proximity to continental or volcanic sources of elements; (b) the chemical environment of deposition, including the degree of oxygenation; and (c) local factors such as the upward migration of reduced manganese in sediments from certain areas. Sub-surface nodules appear to share the chemical characteristics of their surface counterparts, especially those from volcanic areas where sub-surface sources of elements are probably important.
    Keywords: 2P-50; 2P-52; AMP3P; AMPH-009D; AMPH01AR; AMPH02AR-009D; AMPH03AR-080G; AMPH03AR-085P; AMPH03AR-086G; AMPH03AR-100G; AMPH03AR-124C; AMPH03AR-125PG; AMPH-080G; AMPH-085P; AMPH-086G; AMPH-100G; AMPH-116P; AMPH-124C; AMPH-125PG; AMPHITRITE; Argo; Barium; CAP-24HG; CAPH0BHO-024G; CAPRICORN-H; Central Pacific; CHA-160; CHA-289; CHA-297; Challenger1872; Chromium; Cobalt; Copper; Core; CORE; D2; D5106; D5123; D5175; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discovery (1962); DNWB0ABD; DNWB0ABD-007G; DNWB0BBD; DNWB0BBD-046G; DNWH0BHO-031G; DODO; DODO-020C; DODO-025PG; DODO-027P; DODO-060P; DODO-062D; DODO-066DA; DODO-075P; DODO-084G; DODO-110P; DODO-113D; DODO-125D; DODO-127D; DODO-130G; DODO-132P; DODO-232D; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWBD1; DWBD4; DWBG46; DWBG-59; DWBG7; DWH48; DWHD15; DWHD16; DWHG31; Elevation of event; Event label; FANB01BD; FANBD-20D; FANFARE-B; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); HILO; HILO01ST-004G; HILO01ST-005G; HILO-04G; HILO-05G; Horizon; Indian Ocean; Iron; JAPANYON; John_Murray_Expedition; JPYN02BD-009G; JPYN04BD-011G; JPYN05BD-013G; JPYN05BD-015P; JPYN05BD-017G; JPYN05BD-031PG; JPYN05BD-048PG; JPYN05BD-050PG; JYN2; JYN2-008G; JYN2-009G; JYN4-011G; JYN5-013G; JYN5-015P; JYN5-015PG; JYN5-017G; JYN5-031PG; JYN5-048PG; JYN5-050PG; Latitude of event; Lead; Longitude of event; Loss on ignition; LSDA; LSDA-122G; LSDA-126G; LSDH; LSDH-045G; LSDH-087P; LSDH-089PG; LSDH-090P; LSDH-090PG; LSDH-093PG; LUSIAD-A; LUSIAD-H; MABAH-166; Mabahiss (1933); Mag_Bay; MAGBAY-A35; Magdalena_Bay; Manganese; Marine_Vertebrates_65-1; MDPC02HO-MP-025F-1; MDPC02HO-MP-026A-3; MDPC02HO-MP-033K; MDPC02HO-MP-037C; MDPC03HO-MP-043A; MIDPAC; Molybdenum; Monegasque Trawl; MONS01AR-MONS08AR; MONSOON; MPC-25F-1; MPC-26A-3; MPC-33K; MPC-37C; MPC-43A; MSN-128G; MTRW; MV65-1; MV65-1-38; MV65-1-41; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Optical spectrographic analysis; Pacific Ocean; Page(s); PC; Piston corer; PROA; PROA-011PG; PROA-079P; PROA-101G; PROA-105G; PROA-108P; PROA-108PG; PROA-113P; PROA-113PG; PROA-116P; PROA-137G; PROA-139G; PROA-147G; PROA-148G; PROA-151G; PROA-156G; PROA-157G; PROA-159G; PROA-160G; PROA-161G; PROA-162G; PROA-169G; Prospector; Prospector-63; RISEPAC; RISP-14V; RISP-45V; RISP-5V; RISP-8V; Sample comment; Sample ID; Sediment type; Size; SOB; SOB-010D; SOB-013D; SOB-020D; SOB-025D; SOB-027D; SOBO03BD-010D; SOBO03BD-013D; SOBO04BD-020D; SOBO04BD-025D; SOBO04BD-027D; Southern Borderland; Spencer F. Baird; Stranger; TC; TET-27G-B-CC; TETH02BD; TETH02BD-027G-B-CC; TETHYS_2; Titanium; Trigger corer; Vanadium; Vit 5200; Vit 5202; Vit 5270; Vityaz (ex-Mars); Vityaz-35; VITYAZ5193; VITYAZ5200; VITYAZ5202; VITYAZ5270; Volumetric; WAH-24FF8; WAH-2P; WAH-2PG; WAH-4P; WAH-4PG; WAHI01BD; WAHINE
    Type: Dataset
    Format: text/tab-separated-values, 2463 data points
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1969): QUEBRADA(1969) Expedition, Dredge List, R/V T. Washington. Scripps Institution of Oceanography, UC San Diego, unpublished, 8 pp, https://www.ngdc.noaa.gov/mgg/curator/data/thomas_washington/quebrada/quebrada_log.pdf
    Publication Date: 2024-07-01
    Description: The dredges described in this report were taken on the QUEBRADA Expedition from November until December 1969 by the Scripps Institution of Oceanography from the R/V T. Washington. A total of 26 dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; QBR-10D; QBR-1D; QBR-22D; QBR-26D; QBR-2D; QBR-7A; QBR-8B; Quantity of deposit; QUEBRADA; Sample ID; Size; Substrate type; Thomas Washington
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-06-26
    Description: In the summer of 1966 (1966-06-20 to 1966-07-08), during approximately one month, research vessels from Finland, Germany, Norway, Sweden and UK-Scotland made hydrographical investigations in the Skagerrak, parts of the NE North Sea Proper and N Kattegat. Germany also deployed recording current meters, 16 instruments at 10 positions, with some 20 days' data collection. Finally, there were current measurements from research vessels drifting or at anchor. One of the aims was to estimate the average water transport and its origin. The data has been quality controlled.
    Keywords: AL01_01; AL01_02; AL01_03; AL01_04; AL01_05; AL01_06; AL01_07; AL01_08; AL01_09; AL01_10; AL01_11; AL01_12; AL01_13; AL01_14; AL01_15; AL01_16; AL01_17; AL01_18; AL01_19; AL01_20; AL01_21; AL01_22; AL01_23; Alkor (1965); Alkor66; Aranda (1989); Aranda66/1; Aranda66/1_131; Aranda66/1_132; Aranda66/1_133; Aranda66/1_134; Aranda66/1_135; Aranda66/1_136; Aranda66/1_137; Aranda66/1_138; Aranda66/1_139; Aranda66/1_140; Aranda66/1_141; Aranda66/1_142; Aranda66/1_143; Aranda66/1_144; Aranda66/1_145; Aranda66/1_146; Aranda66/1_147; Aranda66/1_148; Aranda66/1_149; Aranda66/1_150; Aranda66/1_151; Aranda66/1_152; Aranda66/1_153; Aranda66/1_154; Aranda66/1_155; Aranda66/1_156; Aranda66/1_157; Aranda66/1_158; Aranda66/1_159; Aranda66/1_160; Aranda66/1_161; Aranda66/1_162; Aranda66/1_163; Aranda66/1_164; Aranda66/1_165; Aranda66/1_166; Aranda66/1_167; Aranda66/1_168; Aranda66/1_169; Aranda66/1_170; Aranda66/1_171; Aranda66/1_172; Aranda66/1_173; Aranda66/1_174; Aranda66/1_175; Aranda66/1_176; Aranda66/1_177; Aranda66/1_178; Aranda66/1_179; Aranda66/1_180; Aranda66/1_181; Aranda66/1_182; Aranda66/1_183; Aranda66/1_184; Aranda66/1_185; Aranda66/1_186; Aranda66/1_187; Aranda66/1_188; Aranda66/1_189; Aranda66/1_190; Aranda66/1_191; Aranda66/1_192; Aranda66/1_193; Aranda66/1_194; Aranda66/1_195; Aranda66/1_196; Aranda66/1_197; Aranda66/1_198; Aranda66/1_199; Aranda66/1_200; Aranda66/1_201; Aranda66/1_202; Aranda66/1_203; CTD/Rosette; CTD-RO; Dannevig; G. O. Sars (1950); GMD66; GMD66_119; GMD66_120; GMD66_121; GMD66_122; GMD66_123; GMD66_124; GMD66_125; GMD66_126; GMD66_127; GMD66_128; GMD66_129; GS66; GS66_405; GS66_406; GS66_407; GS66_408; GS66_409; GS66_410; GS66_411; GS66_412; GS66_413; GS66_414; GS66_415; GS66_416; GS66_417; GS66_418; GS66_419; GS66_420; GS66_421; GS66_422; GS66_423; GS66_424; GS66_425; GS66_426; GS66_427; GS66_428; GS66_429; GS66_430; GS66_431; GS66_432; GS66_433; GS66_434; GS66_435; GS66_436; GS66_437; GS66_438; GS66_439; GS66_440; GS66_441; GS66_442; GS66_443; GS66_444; GS66_445; GS66_446; GS66_447; GS66_448; GS66_449; GS66_450; GS66_451; GS66_452; GS66_453; GS66_454; GS66_455; GS66_456; GS66_457; GS66_458; GS66_459; GS66_460; GS66_461; GS66_462; GS66_463; GS66_464; GS66_465; GS66_466; GS66_467; GS66_468; GS66_469; GS66_470; GS66_471; GS66_472; GS66_473; GS66_474; GS66_475; GS66_476; GS66_477; GS66_478; GS66_479; GS66_480; GS66_481; GS66_482; GS66_483; GS66_484; GS66_485; GS66_486; GS66_487; GS66_488; GS66_489; GS66_490; GS66_491; GS66_492; GS66_493; GS66_494; GS66_495; GS66_496; GS66_497; GS66_498; GS66_499; GS66_500; GS66_501; GS66_502; GS66_503; GS66_504; GS66_505; GS66_506; GS66_507; GS66_508; GS66_509; GS66_510; GS66_511; GS66_512; GS66_513; GS66_514; GS66_515; GS66_516; GS66_517; GS66_518; GS66_519; GS66_520; GS66_521; GS66_522; GS66_523; GS66_524; GS66_525; GS66_526; GS66_527; GS66_528; GS66_529; GS66_530; GS66_531; GS66_532; GS66_533; GS66_534; GS66_535; GS66_536; GS66_537; GS66_538; GS66_539; GS66_540; GS66_541; GS66_542; GS66_543; GS66_544; GS66_545; GS66_546; GS66_547; GS66_548; GS66_549; GS66_550; GS66_551; GS66_552; GS66_553; GS66_554; GS66_555; GS66_556; GS66_557; GS66_558; GS66_559; GS66_560; GS66_561; GS66_562; GS66_563; GS66_564; GS66_565; GS66_566; GS66_567; GS66_568; GS66_569; GS66_570; GS66_571; GS66_572; GS66_573; GS66_574; GS66_575; GS66_576; GS66_577; GS66_578; GS66_579; GS66_580; GS66_581; GS66_582; GS66_583; GS66_584; GS66_586; GS66_588; GS66_590; GS66_592; GS66_594; GS66_596; GS66_598; GS66_600; GS66_602; GS66_604; GS66_606; GS66_608; GS66_610; GS66_612; GS66_614; GS66_617; GS66_619; GS66_621; GS66_623; GS66_625; GS66_627; GS66_631; GS66_633; GS66_635; GS66_637; GS66_639; GS66_641; GS66_643; GS66_645; GS66_647; GS66_649; GS66_651; GS66_654; GS66_656; GS66_658; GS66_660; GS66_662; GS66_664; GS66_666; GS66_668; GS66_670; GS66_672; GS66_674; GS66_676; GS66_678; GS66_680; GS66_682; GS66_684; GS66_686; GS66_688; GS66_689; GS66_690; GS66_691; GS66_692; GS66_693; GS66_694; GS66_695; GS66_696; GS66_697; GS66_698; GS66_699; GS66_700; GS66_701; GS66_702; GS66_703; GS66_704; GS66_705; GS66_706; GS66_707; GS66_708; GS66_709; GS66_710; GS66_711; Kattegat; M5; M5_032; M5_033; M5_034; M5_035; M5_036; M5_037; M5_038; M5_039; M5_040; M5_041; M5_042; M5_043; M5_044; M5_045; M5_046; M5_047; M5_048; M5_049; M5_050; M5_051; M5_052; M5_053; M5_054; M5_055; M5_056; M5_057; M5_058; M5_059; M5_060; M5_061; M5_062; M5_063; M5_064; M5_065; M5_066; M5_067; M5_068; M5_069; M5_070; M5_071; M5_072; M5_073; M5_074; M5_075; M5_076; M5_077; M5_078; M5_079; M5_080; M5_081; M5_082; M5_083; M5_084; M5_085; M5_086; M5_087; M5_088; M5_089; M5_090; M5_091; M5_092; M5_093; M5_094; M5_095; M5_096; M5_097; M5_098; M5_099; M5_100; M5_101; M5_102; M5_103; M5_104; M5_105; M5_106; M5_107; M5_108; M5_109; M5_110; M5_111; M5_112; M5_113; M5_114; M5_115; M5_116; M5_117; M5_118; M5_119; M5_120; M5_121; M5_122; M5_123; M5_124; M5_125; M5_126; M5_127; M5_128; M5_129; M5_130; M5_131; M5_132; M5_133; M5_134; M5_135; M5_136; M5_137; M5_138; M5_139; M5_140; M5_141; M5_142; M5_143; M5_144; M5_145; M5_146; M5_147; M5_148; M5_149; M5_150; M5_151; M5_152; M5_153; M5_154; M5_155; M5_156; M5_157; M5_158; M5_159; M5_160; M5_161; M5_162; M5_163; M5_164; M5_165; M5_166; M5_167; M5_168; M5_169; M5_170; M5_171; M5_172; M5_173; M5_174; Meteor (1964); North Sea; Norwegian Sea; Scotia; Scotia66; Scotia66_097; Scotia66_098; Scotia66_099; Scotia66_100; Scotia66_101; Scotia66_102; Scotia66_103; Scotia66_104; Scotia66_105; Scotia66_106; Scotia66_107; Scotia66_108; Scotia66_109; Scotia66_110; Scotia66_111; Scotia66_112; Scotia66_113; Scotia66_114; Scotia66_115; Scotia66_116; Scotia66_117; Scotia66_118; Scotia66_119; Scotia66_120; Scotia66_121; Scotia66_122; Scotia66_123; Scotia66_124; Scotia66_125; Scotia66_126; Scotia66_127; Scotia66_128; Scotia66_129; Scotia66_130; Scotia66_131; Scotia66_132; Scotia66_133; Scotia66_134; Scotia66_135; Scotia66_136; Scotia66_137; Scotia66_138; Scotia66_139; Scotia66_140; Scotia66_141; Scotia66_142; Scotia66_143; Scotia66_144; Scotia66_145; Scotia66_146; Scotia66_147; Scotia66_148; Scotia66_149; Scotia66_150; Scotia66_151; Scotia66_152; Scotia66_153; Scotia66_154; Skagerrak; Skagerrak66; Skagerrak66_071; Skagerrak66_072; Skagerrak66_073; Skagerrak66_074; Skagerrak66_075; Skagerrak66_076; Skagerrak66_077; Skagerrak66_078; Skagerrak66_079; Skagerrak66_080; Skagerrak66_081; Skagerrak66_082; Skagerrak66_083; Skagerrak66_084; Skagerrak66_085; Skagerrak66_086; Skagerrak66_087; Skagerrak66_088; Skagerrak66_089; Skagerrak66_090; Skagerrak66_091; Skagerrak66_092; Skagerrak66_093; Skagerrak66_094; Skagerrak66_095; Skagerrak66_096; Skagerrak66_097; Skagerrak66_098; Skagerrak66_099; Skagerrak66_100; Skagerrak66_101; Skagerrak66_102; Skagerrak66_103; Skagerrak66_104; Skagerrak66_105; Skagerrak66_106; Skagerrak66_107; Skagerrak66_108; Skagerrak66_109; Skagerrak66_110; Skagerrak66_111; Skagerrak66_112; Skagerrak66_113; Skagerrak66_114; Skagerrak66_115; Skagerrak66_116; Skagerrak66_117; Skagerrak66_118; Skagerrak66_119; Skagerrak66_120; Skagerrak66_121; Skagerrak66_122; Skagerrak66_123; Skagerrak66_124; Skagerrak66_125; Skagerrak66_126; Skagerrak66_127; Skagerrak66_128; Skagerrak66_129; Skagerrak66_130; Skagerrak66_131; Skagerrak66_132; Skagerrak66_133; Skagerrak66_134; Skagerrak66_135; Skagerrak66_136; Skagerrak66_137; Skagerrak66_138; Skagerrak66_139; Skagerrak66_140; Skagerrak66_141; Skagerrak66_142; Skagerrak66_143; Skagerrak66_144; Skagerrak66_145; Skagerrak66_146; Skagerrak66_147; Skagerrak66_148; Skagerrak66_149; Skagerrak66_150; Skagerrak66_151; Skagerrak66_152; Skagerrak66_153; Skagerrak66_154; Skagerrak66_155; Skagerrak66_156; Skagerrak66_157; Skagerrak66_158; Skagerrak66_159; Skagerrak66_160; Skagerrak66_161; Skagerrak66_162; Skagerrak66_163; Skagerrak66_164; Skagerrak66_165; Skagerrak66_166; Skagerrak66_167; Skagerrak66_168; Skagerrak66_169; Skagerrak66_170; Skagerrak66_171; Skagerrak66_172; Skagerrak66_173; Skagerrak66_174; Skagerrak66_175; Skagerrak66_176;
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Expected Availability
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  • 4
    Publication Date: 2024-06-26
    Description: The dredges described in this report were taken on the PR II, CORPUS 4 Expedition in January 1969 by the USGS Woods Hole Coastal and Marine Science Center from the R/V Atlantic Twin. Dredges recovered and are available at USGS Woods Hole Coastal and Marine Science Center for sampling and study.
    Keywords: 1969-001-FA; Atlantic Twin; ATTW PR II; CORPUS 4; ATWPRII-2D; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Puerto Rico; Quantity of deposit; Sample ID; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-06-26
    Keywords: AL01_01; AL01_02; AL01_03; AL01_04; AL01_05; AL01_06; AL01_07; AL01_08; AL01_09; AL01_10; AL01_11; AL01_12; AL01_13; AL01_14; AL01_15; AL01_16; AL01_17; AL01_18; AL01_19; AL01_20; AL01_21; AL01_22; AL01_23; Alkor (1965); Alkor66; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma, in situ; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Salinity; Skagerrak; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 785 data points
    Location Call Number Expected Availability
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Johnson, C E; Glasby, Geoffrey P (1969): Mössbauer Effect determination of particle size in microcrystalline iron-manganese nodules. Nature, 222(5191), 376-377, https://doi.org/10.1038/222376a0
    Publication Date: 2024-03-01
    Description: Iron-manganese nodules from the ocean floor have been extensively studied. But, because of the fine grain size of the particles of the nodules, structural identification by X-ray and electron diffraction techniques is difficult and the mineralogy of the iron oxide phase has not been well characterized. The observation of the Mössbauer spectrum-in which each nucleus absorbs gamma-rays independently-is not limited by particle size in the same way as is the observation of Bragg peaks in diffraction measurements, in which radiation must be scattered coherently from a large number of atoms. The magnetic hyperfine splitting in the Mössbauer spectrum of magnetic materials is affected, however, when the particles are so small that they become superparamagnetic. We describe here an investigation using the 57Fe Mössbauer effect of two iron-manganese nodules in which the iron oxide phase could not be detected by X-ray or electron diffraction.
    Keywords: Chromium; Cobalt; Copper; D16; D6243; D6273; Description; Discovery (1962); Dredge, rock; DRG_R; Event label; Gulf of Aden; Indian Ocean, Carlsberg Ridge; Iron; Lead; Manganese; Minerals, surface area; Molybdenum; Mössbauer spectroscopy; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Silicon dioxide; Titanium; Vanadium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
    Location Call Number Expected Availability
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Manheim, Frank T; Bischoff, James L (1969): Geochemistry of pore waters from the Shell Oil Company drill holes on the continental slope of the northern Gulf of Mexico. Chemical Geology, 4, 63-82, https://doi.org/10.1016/0009-2541(69)90040-0
    Publication Date: 2024-01-09
    Description: Pore waters were analyzed from 6 holes drilled from M.V. “Eureka” as a part of the Shell Oil Co. deeper offshore study. The holes were drilled in water depths of 600-3000 ft. (approximately 180-550 m) and penetrated up to 1000 ft. (300 m) of Pliocene-Recent clayey sediments. Salt and anhydrite caprock was encountered in one diapiric structure on the continental slope. Samples from holes drilled near diapiric structures showed systematic increases of pore-water salinity with depth, suggestive of salt diffusion from underlying salt plugs. Anomalous concentrations of K and Br indicate that at least one plug contains late-stage evaporite minerals. Salinities approaching halite saturation were observed. Samples from holes away from diapiric structures showed little change in pore-water chemistry, except for loss of SO4 and other variations attributable to early-stage diagenetic reactions with enclosing sediments. Thus, increased salt concentrations in even shallow sediments from this part of the Gulf appear to provide an indicator of salt masses at depth.
    Keywords: Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Eu-26; Eu-66; Eu-70; Eu-79; Eu-80A; Eureka-65-67; Gulf of Mexico; MV Eureka; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-01-09
    Keywords: Acid titration; Bicarbonate; Calcium; Calculated; Chlorine; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Emission spectrometry; Eu-26; Eu-66; Eu-70; Eu-79; Eu-80A; Eureka-65-67; Event label; Gulf of Mexico; Latitude of event; Longitude of event; Magnesium; MV Eureka; Ocean Drilling Program; ODP; Potassium; Powers roundness, SR; Sodium; Sulfate; Sum; Weighing of precipitate of BaSO4
    Type: Dataset
    Format: text/tab-separated-values, 135 data points
    Location Call Number Expected Availability
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  • 9
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    Unknown
    PANGAEA
    In:  Bundesanstalt für Bodenforschung, Hannover
    Publication Date: 2023-12-16
    Type: Dataset
    Format: application/pdf, 1.4 MBytes
    Location Call Number Expected Availability
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  • 10
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    Unknown
    PANGAEA
    In:  Supplement to: Vinogradov, Mikhail E; Arashkevich, Elena G (1969): Vertical distribution of interzonal copepod filter feeders and their role in communities at different depths in the Northwestern Pacific. Oceanology, 9, 400-409
    Publication Date: 2023-11-25
    Description: Vertical distribution of abundance and biomass of upper interzonal copepods Calanus cristatus, C. plumchrus, Eucalanus bungii, Metridia ochotensis and M. pacifica have been studied in the whole depth range of their occurrence. These species comprise 55 per cent of total plankton biomass in the 0-4000 m layer. The major part (90% of the population) of C. cristatus inhabit depths are above 3000 m, and of the other species - above 750-1000 m. Feeding of juveniles proceeds in the surface euphotic zone, and then adolescent animals descend to deep water. At depth 1000-2000 m they make up 〉40%, and at 2000-3000 m, about 20% of total biomass of plankton inhabiting these depths. Interzonal species serve as a food reserve for predatory deep-sea animals and as a close connection between the surface and deep-water communities that makes it possible to regard these communities as parts of a single biocoenosis.
    Keywords: Archive of Ocean Data; ARCOD; JUDAY; Juday net; Northwest Pacific; Plankton net, conical; PNC; VITYAZ; Vityaz (ex-Mars); VITYAZ5603; VITYAZ5610; VITYAZ5612; VITYAZ5621; VITYAZ5626; Vityaz5627
    Type: Dataset
    Format: application/zip, 24 datasets
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