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  • 1980-1984  (52)
  • 1970-1974  (87)
  • 1965-1969  (138,865)
  • 1955-1959  (64,120)
  • 1969  (138,857)
  • 1958  (64,120)
Collection
Keywords
Publisher
Language
Years
Year
  • 1
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    Unknown
    (Table 1, page 1157) DOWNWIND expedition bottom photo stations showing abundant manganese nodules (1958)
    PANGAEA
    In:  Supplement to: Menard, H William; Shipek, CJ (1958): Surface concentrations of manganese nodules. Nature, 182(4643), 1156-1158, https://doi.org/10.1038/1821156b0
    Details
    Publication Date: 2024-07-01
    Description: Manganese nodules were investigated during the Downwind Expedition, a part of the International Geophysical Year programme of the Scripps Institution of Oceanography of the University of California. Attempts were made to collect bottom photographs, cores and dredge hauls in the same areas, to measure the distribution at the surface and in depth, and to obtain large samples for physical and chemical analysis.
    Keywords: Comment; Coverage; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0BBD; DOWNWIND-B1; DOWNWIND-B2; DWBP10; DWBP11; DWBP2; DWBP5; DWBP8; DWBP9; East Pacific, Austral Basin; Elevation of event; Event label; French Polynesia; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules, mass abundance; North-East Pacific Ocean; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Southwest Pacific Ocean; Spencer F. Baird; Station 10-K1253; Station 11-K1252; Station 2-K1243; Station 5-K1250; Station 8-K1248; Station 9-K1244; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Annotated record of the detailed examination of Mn deposits from DOWNWIND Expedition stations (1958)
    PANGAEA
    Details
    Publication Date: 2024-07-01
    Description: The cores described in this report were taken on the DOWNWIND Expedition in October 1957 to February 1958 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird and the R/V Horizon. A total of 201 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DNWB0ABD; DNWB0ABD-002G; DNWB0ABD-003G; DNWB0ABD-007G; DNWB0ABD-015G; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-018G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-030GA; DNWB0BBD-030GB; DNWB0BBD-031G; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-044G; DNWB0BBD-045G; DNWB0BBD-046G; DNWB0BBD-047G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0BBD-057GA; DNWB0BBD-057GB; DNWB0CBD; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-0014H; DNWH0AHO-004H; DNWH0AHO-007H; DNWH0AHO-008TB; DNWH0BHO-031G; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B3; DOWNWIND-B4; DOWNWIND-H; Dredge; DRG; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBD8; DWBG122A-C; DWBG147B; DWBG15; DWBG16; DWBG17; DWBG18; DWBG19; DWBG2; DWBG3; DWBG30A; DWBG30B; DWBG31; DWBG37; DWBG40; DWBG43; DWBG44; DWBG45; DWBG46; DWBG47; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG57A; DWBG57B; DWBG-58; DWBG-59; DWBG7; DWH48; DWHD15; DWHD16; DWHD25; DWHD42; DWHD47; DWHD55; DWHD72; DWHG31; DWHG34; DWHH14; DWHH27; DWHH32; DWHH4; DWHH7; DWHH92; DWHT8B; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Horizon; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 669 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    (Table, page 351-359) Chemical composition of manganese nodules and crusts from the Pacific and Indian Ocean (1969)
    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
    Details
    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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    DATA PANGAEA
  • 4
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    Unknown
    Annotated record of the detailed examination of Mn deposits from QUEBRADA Expedition stations (RV Thomas Washington) (1969)
    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
    Details
    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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    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Physical and chemical oceanography from the Joint Skagerrak Expedition in 1966 (1969)
    PANGAEA
    Details
    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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    DATA PANGAEA
  • 6
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    Unknown
    Annotated record of the detailed examination of Mn deposits from PR II, CORPUS 4 Cruise, R/V Atlantic Twin off the coast of Puerto Rico (1969)
    PANGAEA
    Details
    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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    DATA PANGAEA
  • 7
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    Unknown
    Physical oceanography during ALKOR cruise Alkor66 (1969)
    PANGAEA
    Details
    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
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    DATA PANGAEA
  • 8
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    Unknown
    Determining aquifer characteristics by the tidal method (1969)
    AGU
    Details
    Publication Date: 2024-06-06
    Description: If ground‐water levels of a confined aquifer fluctuate with sea tides, individual values of hydraulic conductivity and specific storage can then be determined. Apparent tidal efficiency and time lag are first calculated from the water level data recorded at an observational device situated inland from the sea, taking into account the response characteristics of the observational device according to criteria established by Hvorslev [1951]. The true tidal efficiency of the aquifer at the seacoast is then determined from the apparent tidal efficiency and used to obtain the specific storage. This and the tidal time lag are utilized to calculate the hydraulic conductivity. The method was tested in Prince Edward Island, Canada, and yielded results compatible with pump test data. This is a simple and inexpensive way to test a confined aquifer in the coastal environment.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 9
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    Göttinger Bodenkundliche Berichte 8 (1969)
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Details
    Publication Date: 2024-03-03
    Description: research
    Keywords: Die divergierende Humus-Metabolik benachbarter Sauer-Braunerden und Rendsinen unter Wald im Licht organischer Stoffgruppen-Untersuchungen
    Language: German
    Type: doc-type:book
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    CITATION GEO-LEO
  • 10
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    Unknown
    Göttinger Bodenkundliche Berichte 9 (1969)
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Details
    Publication Date: 2024-03-03
    Description: Voruntersuchungen zu dieser Arbeit befaßten sieb mit der stoffgruppen-chemischen Auftrennung der organischen Substanz in den organo-mineralischen A -Horizonten von benachbarten und typischen Rendsinen und Sauer-Braunerden unter Laub und Coniferen-Forsten der mitteldeutschen Berg- und RUgel-Landschaften. Die Untersuchungen ergaben: Bei gleichen Baumbeständen und in einer Distanz von nur wenigen Metern war der Gleichgewichts-Humusspiegel in den Ab-Horizonten (0 - 25 cm) der Rendsinen ca. 4-mal so hoch wre der mittlere Humus-Gehalt in den oberen 15 cm der Sauer-Braunerden. Die organische Substanz der eutrophen, kalkhaltigen Rendsinen bestand zu hohen Anteilen aus höher-polymeren Huminstoffen (Huminsäuren und lluminen), während bei den stark sauren Braunerden die Fraktionen der niedermolekularen Fulvosäuren und Streustoffe den Hauptanteil der organischen Komponente bildeten. Für die Sauer-Braunerden konnte anband der Verteilung von aggres- siven Fulvosäuren, organischen Säuren (z.B. Uronsäuren) und Kohlenhydraten nachgewiesen werden, daß die Humus- Zufuhr zum Mineralkörper des Bodens zu erheblichen Teilen durch Infiltration bewerkstelligt wird. Bei den Rendsinen erfolgt dagegen die Inkorporation durch intensive biolo- gisch-mechanische Beimischung. Während bei den Rendsinen der Umsatz der organischen Sub- stanz überwiegend im oberen Abschnitt des Solums abläuft und eine Auflage-Humus-Decke fehlt, spielt sich bei den Sauer-Braunerden der Umsatz hauptsächlich in der Humus- Auflage ab. Die Mengen und das Spektrum der organischen Substanzen, die infiltrativ in das mineralische Substrat gelangen und dort fixiert oder abgebaut werden, sind im Vergleich zu den Rendsinen gering. Sie scheinen durch eine selektiv abbau-wirksame biologische (Pilz-) Sperre in der Auflage-Decke oder an deren Untergrenze bestimmt zu werden. Als Fazit dieser Untersuchungen wurde empfohlen, zur Klä- rung der unterschiedlichen Humus-Metabolik mit Hilfe standorts-biologischer Methoden das Gewicht auf die Klärung folgender beiden Fragen zu legen:
    Description: research
    Keywords: Bodenbildung ; Bodenchemie ; Humusboden ; Metabolit ; Geoökosystem
    Language: German
    Type: doc-type:book
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    CITATION GEO-LEO
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