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  • 1965-1969  (123,861)
  • 1966  (123,861)
Collection
Language
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2024-05-02
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; RC10; RC10-003RD; RC10-101; RC10-101C1; RC10-101C3; RC10-103C1; RC10-104C4; RC10-11; RC10-110; RC10-123; RC10-123C4; RC10-13; RC10-131; RC10-153; RC10-154; RC10-164; RC10-165; RC10-168; RC10-171; RC10-172; RC10-176; RC10-178; RC10-179; RC10-182; RC10-205; RC10-21C2; RC10-21C3; RC10-233; RC10-239; RC10-244; RC10-26C6; RC10-26C7; RC10-274; RC10-278; RC10-279; RC10-36C1; RC10-36C2; RC10-40C2; RC10-40C4; RC10-41C1; RC10-41C2; RC10-41C4; RC10-44C2; RC10-45C3; RC10-49C2; RC10-49C3; RC10-69C2; RC10-70C1; RC10-76; RC10-77; RC10-78; RC10-79; RC10-7C2; RC10-7C6; RC10-81; RC10-87C7; RC10-88; RC10-8C1; RC10-8C2; RC10-91; RC10-93; RC10-96C2; RC10-96C4; RC10-97C1; RC10-97C4; RC10-97C5; RC10-98C1; RC10-98C3; RC10-98C4; RC10-99C2; Robert Conrad; Sediment type; Size; Substrate type; Uniform resource locator/link to file; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1142 data points
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bonatti, Enrico; Joensuu, Oiva (1966): Deep-Sea Iron Deposit from the South Pacific. Science, 154(3749), 643-645, https://doi.org/10.1126/science.154.3749.643
    Publication Date: 2024-04-20
    Description: Along with specimens of manganese oxides and basalt, rocks containing more than 30 percent iron by weight and consisting mainly of poorly crystallized goethite have been dredged from the flanks of a seamount located on the East Pacific Rise. The Fe-Mn ratio varies widely among the various oxide rocks deposited at this locality and at another seamount in the same area. The deposit was probably formed by fractional precipitation of iron and manganese which had been introduced locally into the bottom water by hydrothermal solutions of volcanic origin, and by leaching from deep-sea basaltic lavas.
    Keywords: Aluminium oxide; AMPH-002D; AMPH01AR; AMPH01AR-002D; AMPHITRITE; Argo; Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Iron; Loss on drying; Magnesium oxide; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Potassium oxide; Sample ID; Silicon dioxide; Strontium
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
    Location Call Number Expected Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Cordes, Eilhard (1966): Aufbau und Bildungsbedingungen der Schwermineralseifen bei Skagen (Dänemark). Meyniana, 16, 1-35, https://doi.org/10.2312/meyniana.1966.16.1
    Publication Date: 2024-04-19
    Description: Aufbau und Ausdehnung der Schwermineral-Anreicherungen (Ilmenit, Granat, Amphibol) am Strand südlich Skagens wurden in langen Schürfgräben untersucht. Die Seifenlagen ziehen durchgehend vom Kliff-Fuß bis zur mittleren Meereshöhe hin und liegen meist diskordant auf der alten Strandschichtung. Ihre strandparallele Ausdehnung beträgt bis zu 100 m. Aufgebaut werden sie aus dünnen Schwermineral-Lamellen, die in kleinerem Umfang überall in den Strandablagerungen zu finden sind und hier das Gefüge nachzeichnen (Rippeln, Strandwallschichtung, Schichtstörungen). Die Seifenbildung geht in einem Gebiet mit verstärktem Küstenabtrag vor sich (Lee-Erosion südlich der Hafenmolen von Skagen). Dieses deutet darauf hin, daß die Schwerminerale bei Aufarbeitung bereits vorhandener Sedimente infolge ihres unterschiedlichen hydraulischen Verhaltens Zurückbleiben und schließlich angereichert werden. Die Korngrößenverteilung der Minerale in verschiedenen Sedimentproben zeigen, daß mit steigender Schwermineral-Anreicherung eine Kornverfeinerung und Zunahme der spezifisch schwersten Minerale (opake Erzminerale und Zirkon) auftritt. In ähnlicher Weise werden die Sortierungswerte besser. Die Aufbereitung des Sedimentes wird, in Anlehnung an v. ENGELHARDT (1939), mit einem doppelten Sortierungsvorgang durch die Wasserbewegung am Strand erklärt. Beim Absinken des Sandes nach dem Brecherschwall tritt eine Vorsortierung ein, die den Abtransport der leichteren und größeren Minerale im Sog begünstigt. Verbindungen zu Vorstellungen der Aufbereitungstechnik (Rundherdverfahren) und Hydrodynamik ('laminare Unterschicht') werden hergestellt. Die Dünensande Skagens sind infolge ihres hohen Schwermineralgehaltes und günstiger Äquivalentgrößen der einzelnen Minerale besonders bedeutsam für die Seifenbildung am Strand.
    Keywords: Europe, Denmark; HAND; Sampling by hand; Skagen1964
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Distance; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Opaque minerals; Sample ID; Sampling by hand; Skagen1964
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Epidote; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Minerals, other; Opaque minerals; Sample ID; Sampling by hand; Skagen1964; Sorting; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 300 data points
    Location Call Number Expected Availability
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dietrich, Günter; Düing, Walter; Grasshoff, Klaus; Koske, Peter H (1966): Physikalische und chemische Daten nach Beobachtungen des Forschungsschiffes Meteor im Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A2, 1-155
    Publication Date: 2024-02-03
    Description: The present volume gives the observed physical and chemical data obtained by R.V. "Meteor" in the Indian Ocean during cruise 1964/65. The tables are based on the computations made by the National Oceanographic Data Center (NODC) in Washington. In addition to the normally communicated data, the tables contain four chemical parameters: alkalinity, ammonia, fluoride, and calcium.
    Keywords: Biscaya; CTD/Rosette; CTD-RO; Eastern Arabian Sea; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_001; M1_005; M1_006; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD001; M1_CTD005; M1_CTD006; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Mediterranean Sea; Meteor (1964); Red Sea; Western Arabian Sea
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-02-03
    Keywords: Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_005; M1_006; M1_CTD005; M1_CTD006; Mediterranean Sea; Meteor (1964); Nitrate; Oxygen; Oxygen, microelectrode, ex-situ; Phosphate; Salinity; Silicate; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; Calcium; Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Eastern Arabian Sea; Elevation of event; Event label; Fluoride; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Meteor (1964); Nitrate; Nitrite; Oxygen; Oxygen, microelectrode, ex-situ; pH; Phosphate; Phosphorus, total; Red Sea; Salinity; Silicate; Temperature, water; Turnover-thermometer; Western Arabian Sea
    Type: Dataset
    Format: text/tab-separated-values, 38537 data points
    Location Call Number Expected Availability
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  • 9
    Publication Date: 2024-02-03
    Keywords: Biscaya; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_001; M1_CTD001; Meteor (1964); Oxygen; Oxygen, microelectrode, ex-situ; Salinity; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 176 data points
    Location Call Number Expected Availability
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  • 10
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 36 no. 1, pp. 3-16
    Publication Date: 2024-01-12
    Description: Da\xc3\x9f eine Tiergruppe pelagischer Anpassung, wie die Zahnwale, in den mit dem Ozean nur mittelbar, via Nordsee, in Verbindung stehenden K\xc3\xbcstenmeeren Schwedens eine weit bescheidenere Rolle spielt als an der atlantischen K\xc3\xbcste Europas, ist nat\xc3\xbcrlich und vorauszusetzen. Von 23 europ\xc3\xa4ischen Arten sind f\xc3\xbcr Schweden bis jetzt nur 14, die meisten als seltene Irrg\xc3\xa4ste, festgestellt worden. Desto mehr man sich dabei l\xc3\xa4ngs der K\xc3\xbcste von der Nordsee entfernt, desto geringer wird die Anzahl. Schon an der Westk\xc3\xbcste sinkt sie von 14 im Skagerrak bis nur 9 Arten im Kattegatt. In der Ostsee hat man an der S\xc3\xbcdk\xc3\xbcste zuerst noch 8, an der Ostk\xc3\xbcste 4 und im Bottnischen Meerbusen endlich nur 2 (Abb. 1).\nAls heimische, zu allen Jahreszeiten \xc3\xb6fters antreffbare Bewohner kann man f\xc3\xbcr die Westk\xc3\xbcste nur zwei Arten nennen \xe2\x80\x94 den ziemlich h\xc3\xa4ufigen Schweinswal (Phocaena phocoena) und den weit selteneren Langfinnendelphin ( Lagenorhynchus albirostris). Das gro\xc3\x9fe Brackwassergebiet der Ostsee hat nur den Schweinswal allein heimisch. Der gr\xc3\xb6\xc3\x9fte Teil seines Bestandes verl\xc3\xa4\xc3\x9ft jedoch in der Regel dieses Gebiet f\xc3\xbcr die Winterzeit. Seine Wanderz\xc3\xbcge von und zu der Ostsee sind den K\xc3\xbcstenbewohnern, besonders der \xc3\x96resundgegend und der S\xc3\xbcdk\xc3\xbcste seit altem wohlbekannt und wurden an dazu geeigneten Stellen, wie Ravlunda an der Ostk\xc3\xbcste von Schonen (LINNAEUS, 1751) oder Torekov und die Laholmbucht im S\xc3\xbcdostteil des Kattegattes (NILSSON, 1847), noch im vorigen Jahrhundert zum Fang dieser Kleinwale ausgenutzt (Abb. 2). Im Gegensatz zu der herbstlichen Schweinswalsjagd in den d\xc3\xa4nischen Sunden geschah dies hier haupts\xc3\xa4chlich w\xc3\xa4hrend der Fr\xc3\xbcjahrwanderung der Tiere.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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