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  • Springer Nature  (33,743)
  • Institute of Physics  (7,656)
  • Blackwell Publishing Ltd  (2,995)
  • University of Chicago Press  (2,736)
  • American Chemical Society (ACS)
  • American Institute of Physics (AIP)
  • PANGAEA
  • 1950-1954  (25,353)
  • 1935-1939  (21,831)
Collection
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Year
  • 1
    Publication Date: 2023-07-09
    Keywords: Achnanthes brevipes var. intermedia; Achnanthes clevei; Achnanthes delicatula; Achnanthes exigua; Achnanthes exilis; Achnanthes flexella; Achnanthes hauckiana; Achnanthes hungarica; Achnanthes lanceolata; Achnanthes lanceolata var. elliptica; Achnanthes longipes; Achnanthes microcephala; Actinocyclus ehrenbergi; Amphora commutata; Amphora holsatica; Amphora normani; Amphora ovalis; Amphora ovalis var. pediculus; Amphora perpusilla; Amphora robusta; Anomoeoneis sphaerophora; Asterionella formosa; Biddulphia levis; Biddulphia subaequa; Caloneis amphisbaena; Caloneis bacillum; Caloneis ladogensis; Caloneis obtusa; Caloneis permagna; Caloneis schumanniana; Caloneis schumanniana var. biconstricta; Caloneis silicula; Caloneis zachariasi; Campylodiscus bicostatus; Campylodiscus clypeus; Campylodiscus echeneis; Campylodiscus noricus var. hibernica; Chaetoceros spores; Cocconeis clandestina; Cocconeis diminuta; Cocconeis disculus; Cocconeis pediculus; Cocconeis placentula; Cocconeis scutellum; Coscinodiscus asteromphalus; Coscinodiscus commutatus; Coscinodiscus denarius; Coscinodiscus excentricus; Coscinodiscus kuetzingii; Coscinodiscus lacustris; Coscinodiscus radiatus; Coscinodiscus rothi var. subsala; Cyclotella antiqua; Cyclotella comta; Cyclotella kuetzingiana; Cyclotella meneghiniana; Cyclotella ocellata; Cyclotella striata var. ambigua; Cymatopleura elliptica; Cymatopleura solea; Cymbella affinis; Cymbella aspera; Cymbella cistula; Cymbella cuspidata; Cymbella cymbiformis; Cymbella ehrenbergi; Cymbella helvetica; Cymbella lanceolata; Cymbella leptoceros; Cymbella naviculiformis; Cymbella parva; Cymbella prostrata; Cymbella tumida; Cymbella ventricosa; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoma vulgaris; Didymosphenia geminata; Diploneis didyma; Diploneis domblittensis; Diploneis domblittensis var. subconstricta; Diploneis elliptica; Diploneis fusca; Diploneis interrupta; Diploneis oculata; Diploneis ovalis; Diploneis smithii; Epithemia argus; Epithemia hyndmanni; Epithemia intermedia; Epithemia muelleri; Epithemia sorex; Epithemia sorex var. gracilis; Epithemia turgida; Epithemia zebra; Epithemia zebra var. porcellus; Epithemia zebra var. saxonica; Eunotia gracilis; Eunotia lunaris; Eunotia pectinalis; Eunotia praerupta; Event label; FH_III-8; FH_IX-14; FH_VI-10; FH_VII-15; FH_VII-35; FH_VII-9; FH_VIII-11; FH_X-18; FH_X-8; FH_XI-6; FH_XII-12; FH_XII-9; FH_XIII-5; FH_XIV-5; FH_XVI-14; FH_XVII-18; FH_XVII-a1; Fragilaria brevistriata; Fragilaria capucina var. mesolepta; Fragilaria construens; Fragilaria inflata; Fragilaria leptostauron; Fragilaria pinnata; Frustulia rhomboides; Geological sample; GEOS; Gomphocymbella ancyli; Gomphonema acuminatum; Gomphonema angustatum; Gomphonema augur; Gomphonema constrictum; Gomphonema intricatum; Gomphonema longiceps; Gomphonema longiceps var. montana; Gomphonema olivaceum; Grammatophora oceanica; Gyrosigma acuminatum; Gyrosigma attenuatum; Hantzschia amphioxys; Hyalodiscus scoticus; Mastogloia elliptica; Mastogloia elliptica var. dansei; Mastogloia grevillei; Mastogloia smithi; Mastogloia smithi var. amphicephala; Mastogloia smithi var. lacustris; Melosira ambigua; Melosira arenaria; Melosira binderiana; Melosira distans; Melosira granulata; Melosira islandica; Melosira italica; Melosira varians; Meridion circulare; Navicula abrupta; Navicula americana; Navicula amphibola; Navicula anglica; Navicula bacilliformis; Navicula bacillum; Navicula binodis; Navicula cari; Navicula cincta; Navicula costulata; Navicula crucicula; Navicula cryptocephala; Navicula cuspidata; Navicula cuspidata var. ambigua; Navicula dicephala; Navicula digito-radiata; Navicula exigua; Navicula gastrum; Navicula gracilis; Navicula gracilloides; Navicula humerosa; Navicula hungarica; Navicula hungarica var. capitata; Navicula integra; Navicula jentzschi; Navicula lacustris; Navicula lanceolata; Navicula latissima; Navicula menisculus; Navicula oblonga; Navicula peregrina; Navicula perpusilla; Navicula placentula; Navicula platystoma; Navicula protracta; Navicula pupula; Navicula pusilla; Navicula pygmaea; Navicula radiosa; Navicula reinhardtii; Navicula rhynchocephala; Navicula scutelloides; Navicula tuscula; Navicula tuscula var. minor; Navicula viridula; Navicula vulpina; Neidium affine; Neidium affine var. amphirhynchus; Neidium bisulcatum; Neidium hitchcockii; Neidium iridis; Neidium kozlowi; Neidium productum; Nitzschia amphibia; Nitzschia angustata; Nitzschia capitellata; Nitzschia circumsuta; Nitzschia dissipata; Nitzschia gracilis; Nitzschia interrupta; Nitzschia punctata; Nitzschia scalaris; Nitzschia sigmoidea; Nitzschia sinuata var. tabellaria; Nitzschia tryblionella; Number; Opephora martyi; Pinnularia cardinalis; Pinnularia divergens; Pinnularia episcopalis; Pinnularia esox; Pinnularia gibba; Pinnularia globiceps; Pinnularia interrupta; Pinnularia leptosoma; Pinnularia macilenta; Pinnularia major; Pinnularia mesolepta; Pinnularia microstauron; Pinnularia microstauron var. ambigua; Pinnularia microstauron var. brebissoni; Pinnularia nobilis; Pinnularia streptoraphe; Pinnularia viridis; Rhabdonema arcuatum; Rhizosolenia calcar-avis; Rhoicosphenia curvata; Rhopalodia gibba; Rhopalodia gibba var. ventricosa; Rhopalodia gibberula; Rhopalodia musculus; Sample code/label; Stauroneis acuta; Stauroneis anceps; Stauroneis phoenicenteron; Stauroneis smithi; Stephanodiscus astraea; Surirella bifida; Surirella biseriata; Surirella biseriata var. bifrons; Surirella biseriata var. bifrons forma punctata; Surirella biseriata var. rostrata; Surirella caproni; Surirella elegans; Surirella linearis; Surirella linearis var. constricta; Surirella linearis var. helvetica; Surirella ovata; Surirella robusta; Surirella robusta var. splendida; Surirella striatula; Surirella tenera; Surirella tenera var. nervosa; Synedra capitata; Synedra pulchella; Synedra tabulata var. fasciculata; Synedra ulna; Synedra vaucheriae; Tabellaria fenestrata; Tabellaria flocculosa; Terpsinoe americana; Thalassiosira baltica; Vistula Lagoon, Baltic Sea
    Type: Dataset
    Format: text/tab-separated-values, 17584 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-07-09
    Keywords: Achnanthes clevei; Achnanthes dispar; Achnanthes exigua; Achnanthes hauckiana; Achnanthes hungarica; Achnanthes lanceolata; Achnanthes lanceolata var. elliptica; Achnanthes microcephala; Actinocyclus ehrenbergi; Amphora holsatica; Amphora normani; Amphora ovalis; Amphora ovalis var. pediculus; Amphora robusta; Anomoeoneis sphaerophora; Biddulphia levis; Biddulphia subaequa; Caloneis amphisbaena; Caloneis bacillum; Caloneis ladogensis; Caloneis obtusa; Caloneis permagna; Caloneis schumanniana; Caloneis schumanniana var. biconstricta; Caloneis silicula; Caloneis zachariasi; Campylodiscus bicostatus; Campylodiscus clypeus; Campylodiscus echeneis; Campylodiscus noricus var. hibernica; Chaetoceros sp.; Cocconeis diminuta; Cocconeis disculus; Cocconeis pediculus; Cocconeis placentula; Coscinodiscus asteromphalus; Coscinodiscus commutatus; Coscinodiscus excentricus; Coscinodiscus lacustris; Coscinodiscus radiatus; Coscinodiscus rothii var. subsalsa; Cyclotella antiqua; Cyclotella comta; Cyclotella kuetzingiana; Cyclotella meneghiniana; Cyclotella striata var. ambigua; Cymatopleura elliptica; Cymatopleura solea; Cymbella affinis; Cymbella aspera; Cymbella cistula; Cymbella cuspidata; Cymbella cymbiformis; Cymbella ehrenbergi; Cymbella lanceolata; Cymbella leptoceros; Cymbella naviculiformis; Cymbella prostrata; Cymbella tumida; Cymbella ventricosa; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoma elongatum; Diatoma vulgaris; Didymosphenia geminata; Diploneis didyma; Diploneis domblittensis; Diploneis domblittensis var. subconstricta; Diploneis elliptica; Diploneis interrupta; Diploneis marginestriata; Diploneis oculata; Diploneis ovalis; Diploneis puella; Diploneis smithii; Epithemia argus; Epithemia hyndmanni; Epithemia intermedia; Epithemia muelleri; Epithemia sorex; Epithemia sorex var. gracilis; Epithemia turgida; Epithemia zebra; Epithemia zebra var. porcellus; Epithemia zebra var. saxonica; Eucocconeis flexella; Eunotia gracilis; Eunotia pectinalis; Eunotia praerupta; Event label; Fragilaria brevistriata; Fragilaria construens; Fragilaria inflata; Fragilaria intermedia; Fragilaria lapponica; Fragilaria leptostauron; Fragilaria pinnata; Fragilaria virescens; Frustulia rhomboides; Frustulia vulgaris; Geological sample; GEOS; Gomphocymbella ancyli; Gomphonema acuminatum; Gomphonema angustatum; Gomphonema constrictum; Gomphonema intricatum; Gomphonema olivaceum; Gomphonema parvulum; Grammatophora oceanica; Gyrosigma acuminatum; Gyrosigma attenuatum; Hantzschia amphioxys; KH_II-1; KH_II-2; KH_III-12; KH_III-3; KH_III-5; KH_III-8; KH_Memeler-Tief; KH_V-5; KH_VI-3; KH_VII-10; KH_VII-18N; KH_VII-19N; KH_VII-2; KH_X-7a; KH_XIII-13; KH_XIII-19; Mastogloia elliptica; Mastogloia elliptica var. dansei; Mastogloia grevillei; Mastogloia smithi; Mastogloia smithi var. amphicephala; Mastogloia smithi var. lacustris; Melosira ambigua; Melosira arenaria; Melosira binderiana; Melosira distans; Melosira granulata; Melosira italica; Melosira varians; Meridion circulare; Navicula amphibola; Navicula anglica; Navicula bacillum; Navicula binodis; Navicula cari; Navicula costulata; Navicula crucicula; Navicula cryptocephala; Navicula cuspidata; Navicula cuspidata var. ambigua; Navicula dicephala; Navicula exigua; Navicula forcipata; Navicula gastrum; Navicula gracilis; Navicula gracilloides; Navicula humerosa; Navicula hungarica; Navicula hungarica var. capitata; Navicula integra; Navicula jentzschi; Navicula lacustris; Navicula lanceolata; Navicula laterostrata; Navicula latissima; Navicula menisculus; Navicula oblonga; Navicula optima; Navicula peregrina; Navicula placentula; Navicula platystoma; Navicula protracta; Navicula pseudotuscula; Navicula pupula; Navicula pusilla; Navicula pygmaea; Navicula radiosa; Navicula reinhardtii; Navicula rhynchocephala; Navicula schoenfeldii; Navicula scutelloides; Navicula tuscula; Navicula viridula; Navicula vulpina; Neidium affine; Neidium affine var. amphirhynchus; Neidium bisulcatum; Neidium dubium; Neidium dubium var. constricta; Neidium iridis; Neidium kozlowi; Neidium productum; Nitzschia amphibia; Nitzschia angustata; Nitzschia capitellata; Nitzschia circumsuta; Nitzschia denticula var. ancyli; Nitzschia gracilis; Nitzschia scalaris; Nitzschia sigma; Nitzschia sigmoidea; Nitzschia sinuata var. tabellaria; Nitzschia tryblionella; Number; Opephora martyi; Pinnularia cardinalis; Pinnularia divergens; Pinnularia episcopalis; Pinnularia esox; Pinnularia gentilis; Pinnularia gibba; Pinnularia interrupta; Pinnularia major; Pinnularia mesolepta; Pinnularia microstauron; Pinnularia microstauron var. ambigua; Pinnularia microstauron var. brebissoni; Pinnularia nobilis; Pinnularia streptoraphe; Pinnularia subcapitata; Pinnularia viridis; Rhabdonema arcuatum; Rhoicosphenia curvata; Rhopalodia gibba; Sample code/label; Stauroneis acuta; Stauroneis anceps; Stauroneis phoenicenteron; Stauroneis smithi; Stephanodiscus astraea; Surirella bifida; Surirella biseriata; Surirella biseriata var. bifrons; Surirella biseriata var. bifrons forma punctata; Surirella biseriata var. rostrata; Surirella caproni; Surirella elegans; Surirella linearis; Surirella linearis var. constricta; Surirella linearis var. helvetica; Surirella ovata; Surirella robusta; Surirella robusta var. splendida; Surirella striatula; Surirella tenera; Surirella tenera var. nervosa; Synedra capitata; Synedra pulchella; Synedra tabulata; Synedra ulna; Synedra vaucheriae; Tabellaria fenestrata; Tabellaria flocculosa; Terpsinoe americana; Thalassiosira baltica; Vavicula cincta; Vistula Lagoon, Baltic Sea
    Type: Dataset
    Format: text/tab-separated-values, 2555 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2023-07-09
    Keywords: Achnanthes brevipes var. intermedia; Achnanthes clevei; Achnanthes delicatula; Achnanthes hungarica; Achnanthes lanceolata; Achnanthes longipes; Actinocyclus ehrenbergi; Amphora ovalis; Amphora ovalis var. pediculus; Anomoeoneis sphaerophora; Biddulphia aurita; Biddulphia levis; Caloneis amphisbaena var. subsalina; Caloneis bacillum; Caloneis silicula; Campylodiscus bicostatus; Campylodiscus clypeus; Campylodiscus echeneis; Campylodiscus noricus var. hibern; Chaetoceros sp.; Cocconeis diminuta; Cocconeis disculus; Cocconeis pediculus; Cocconeis placentula; Cocconeis scutellum; Coscinodiscus asteromphalus; Coscinodiscus commutatus; Coscinodiscus excentricus; Coscinodiscus lacustris; Coscinodiscus oculus-iridis; Coscinodiscus radiatus; Cyclotella comta; Cyclotella meneghiniana; Cyclotella striata var. ambigua; Cymatopleura elliptica; Cymatopleura solea; Cymbella aspera; Cymbella cistula; Cymbella cuspidata; Cymbella cymbiformis; Cymbella ehrenbergi; Cymbella lanceolata; Cymbella prostrata; Cymbella tumida; Cymbella ventricosa; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoma elongatum; Diatoma vulgaris; Diploneis didyma; Diploneis domblittensis; Diploneis elliptica; Diploneis fusca; Diploneis interrupta; Diploneis ovalis; Diploneis smithii var. rhombica; Epithemia argus; Epithemia intermedia; Epithemia sorex; Epithemia turgida; Epithemia zebra; Eucocconeis flexella; Eunotia lunaris; Eunotia pectinalis; Eunotia praerupta; Event label; FN_III; FN_IV-0; FN_IX; FN_IX-a1; FN_V; FN_V-100; FN_V-300; FN_VIII-2a; FN_X-20; FN_XII-300; FN_XIII-14a; FN_XIV-18; FN_XVI-22; Fragilaria capucina; Fragilaria construens; Fragilaria inflata; Fragilaria intermedia; Fragilaria leptostauron; Fragilaria pinnata; Fragilaria schulzi; Fragilaria virescens; Frustulia vulgaris; Geological sample; GEOS; Gomphonema acuminatum; Gomphonema angustatum; Gomphonema constrictum; Grammatophora oceanica; Gyrosigma acuminatum; Gyrosigma attenuatum; Hantzschia amphioxys; Hyalodiscus scoticus; Melosira ambigua; Melosira arenaria; Melosira granulata; Melosira italica; Melosira juergensi; Melosira moniliformis; Melosira varians; Meridion circulare; Navicula bacillum; Navicula cincta; Navicula costulata; Navicula cryptocephala; Navicula cuspidata; Navicula dicephala; Navicula elegans; Navicula gastrum; Navicula humerosa; Navicula hungarica; Navicula laterostrata; Navicula latissima; Navicula menisculus; Navicula oblonga; Navicula peregrina; Navicula platystoma; Navicula pseudotuscula; Navicula pupula; Navicula pusilla; Navicula pygmaea; Navicula radiosa; Navicula reinhardtii; Navicula rhynchocephala; Navicula schoenfeldii; Navicula scutelloides; Navicula tuscula; Navicula viridula; Neidium affine; Neidium bisulcatum; Neidium iridis; Nitzschia amphibia; Nitzschia angustata; Nitzschia apiculata; Nitzschia circumsuta; Nitzschia denticula var. ancyli; Nitzschia hungarica; Nitzschia scalaris; Nitzschia sigma; Nitzschia spectabilis; Nitzschia tryblionella; Opephora martyi; Pinnularia cardinalis; Pinnularia gentilis; Pinnularia interrupta; Pinnularia maior; Pinnularia nobilis; Pinnularia subcapitata; Pinnularia viridis; Rhabdonema arcuatum; Rhabdonema minutum; Rhizosolenia calcar-avis; Rhoicosphenia curvata; Rhopalodia gibba; Rhopalodia gibba var. ventricosa; Rhopalodia gibberula; Sample code/label; Stauroneis acuta; Stauroneis anceps; Stauroneis phoenicenteron; Stephanodiscus astraea; Surirella biseriata; Surirella caproni; Surirella elegans; Surirella linearis; Surirella ovata; Surirella robusta var. splendida; Surirella striatula; Surirella tenera; Surirella tenera var. nervosa; Synedra capitata; Synedra pulchella; Synedra tabulata; Synedra ulna; Synedra vaucheriae; Tabellaria fenestrata; Tabellaria flocculosa; Terpsinoe americana; Thalassiosira baltica; Vistula Lagoon, Baltic Sea
    Type: Dataset
    Format: text/tab-separated-values, 1541 data points
    Location Call Number Expected Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 3. Lamont Geological Observatory, Columbia University, New York, unpublished, 11 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm03/vm03_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 3 Expedition from January 1957 until June 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 160 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V03; V03-137; V03-140; V03-157; V03-21; V03-27; V03-29; V03-3; Vema
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
    Location Call Number Expected Availability
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 4. Lamont Geological Observatory, Columbia University, New York, unpublished, 8 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm04/vm04_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 4 Expedition from July until September 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 54 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V04; V04-20; V04-35; V04-51; V04-53; Vema
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
    Location Call Number Expected Availability
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 5. Lamont Geological Observatory, Columbia University, New York, unpublished, 7 pp, https://www.ngdc.noaa.gov/mgg/curator/data/vema/vm05/vm05_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 5 Expedition from November until December 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 48 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TC; Trigger corer; V05; V05-11; V05-24; V05-27; V05-40; V05-42; V05-7; V05-7TW; Vema
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
    Location Call Number Expected Availability
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  • 7
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    PANGAEA
    In:  Supplement to: Goldberg, Edward D (1954): Marine Geochemistry 1. Chemical Scavengers of the Sea. The Journal of Geology, 62(3), 249-265, http://www.jstor.org/stable/30080120
    Publication Date: 2023-08-28
    Description: The ability of the hydrated oxides of manganese and iron to adsorb ions from solution (scavenging) is considered in relation to some problems in marine geology, chemistry, and biology. In the ferruginous sediments of the Pacific Ocean, iron oxides are accompanied by titanium, cobalt, and zirconium in amounts proportional to the iron content. Similarly, copper and nickel are linearly related to the manganese content. These observations are explained on the basis of scavenging. An electrochemical theory for the formation of manganese nodules is presented. Marine sediments are classified on the basis of the geosphere in which the solid phases originate. The distribution of certain ionic species in sea water between the solid and aqueous phases is considered on the basis of scavenging and co-ordination compound theory. The concentration of minor elements by members of the marine biosphere is explained either by the direct uptake of the element or by the uptake of iron or manganese oxides with the accompanying scavenged element.
    Keywords: Aluminium; CHA-160; Challenger1872; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Event label; GC; GOLDHW1; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Henderson Seamount, Pacific Ocean; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-026A-3; MDPC02HO-MP-037A; MDPC03HO-043K; MIDPAC; MPC-26A-3; MPC-37A; MPC-43J; MPC-43K; NEL-HEND; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North Pacific Ocean; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; PAS-19121; Phosphorus; Spectrophotometer, Beckmann DU; Titanium; Wired profile sonde; WP; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 118 data points
    Location Call Number Expected Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Young, Edward J (1954): Studies of trace elements in sediments. Massachusetts Intitute of Technology, Boston, Massachusetts, U.S.A., Dissertation, 137 pp, hdl:1721.1/58047
    Publication Date: 2023-08-28
    Description: By means of spectrographic analysis 96 samples of marine sediments were analyzed quantitatively for V, Ti, Zr, Co, Ni, Sc, Cr, and La, and semi-quantitatively for Ba and Sr. Ca has been estimated by visual comparison of spectrographic plates, and several Fe values have also been determined in the same way. Geographically 40 of these samples are from the Pacific Ocean basin, one of which is a manganese nodule, 21 from the Gulf of Mexico, 11 from Atchafalaya Bay, 8 from American Devonian to Miocene sedimentary rocks, 4 from the Mississippi Delta, 3 from the San Diego trough, 3 from off Grand Isle, 3 from Lake Pontchartrain, from Bay Rambour, 1 from Laguna Madre off the Texas coast, and 1 from the Guadalupe River, Texas. The afore-mentioned elements were sought using PdCl2 as an internal standard, after the method developed by Ahrens (1950) and his co-workers. Samples were run in duplicate, and standard deviations varied from 5 to 14 percent. Working curves, from which final values were obtained, were constructed with the use of standard granite, G1, and the standard diabase, W1, as standards. See Fairbairn and others (1951). An experiment was carried out to determine the effect of matrix change, involving CaCO3, on the spectral line intensities of the quantitatively analyzed elements. The distribution of each of the elements is discussed separately, and particular emphasis is given to oceanic "red clay", in which many elements are enriched. A general discussion is given to mineralogy of the sediments, cation exchange in its bearing on this thesis, and a brief recount of the two hypotheses of origin of oceanic "red clay". An application of the findings of this thesis to aid in the choice of the more likely hypothesis is made.
    Keywords: Barium oxide; Calcium oxide; Chromium(III) oxide; Cobalt(III) oxide; Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Horizon; Iron oxide, Fe2O3; Lanthanum oxide; MDPC02HO-MP-026A-3; MIDPAC; MPC-26A-3; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Scandium oxide; Size; Spectrographic analysis; Strontium oxide; Titanium dioxide; Vanadium oxide; X-ray fluorescence (XRF)
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    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: Core; CORE; CUSP15P; CUSP1954; CUSP8P; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Event label; Feature; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Visual description
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    In:  Supplement to: Emiliani, Cesare (1954): Pleistocene temperature variations in the Mediterranean. Quarternaria, 2, 87-97
    Publication Date: 2024-06-26
    Description: For temperature investigations, a core in the Mediterranean Sea (No 189 of the Swedish Deep-Sea Expedition 1947-1948) was sampled at approximately 10 m intervals. Globigerina dubia, G. inflata and Globigerinoides rubra were seperated from each sample and their test were investigated for stable oxygen isotopic measurement. Oxygen isotopic analysis showed the following: 1) Ten stages are indicated. 2) The temperature minimum of stage 2 corresponds to a racliocarbon age of 17,200 years. 3) Temperature maxima of odd stages are about equal to the modern August mean, except that of stage 5 which is considerably higher and, probably reflects the influx of ice melt water. 4) Temperature minima of even stages are all very low, especially that of stage 2, and reflect conditions similar to those now prevailing around Newfoundland. 5) The temperature record indicates that during most of the time covered by the core, the Mediterranean was cooler than at present and that conditions similar to the present occurred only during comparatively short intervals. 6) Minor temperature fluctuations occur, especially in the warmer stages, which are of doubtful significance. 7) An average rate of sedimentation of 4.3 cm/1000 years is indicated for the whole core.
    Keywords: Albatross IV (1963); core_189; DEPTH, sediment/rock; Globigerina dubia, δ18O; Globigerina inflata, δ18O; Globigerinoides rubra, δ18O; NODC-0418; PC; Piston corer; SDSE_276; South Levantine Basin; SwedishDeepSeaExpedition
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  • 11
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    The @photogrammetric record 1 (1954), S. 0 
    ISSN: 1477-9730
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    Topics: Architecture, Civil Engineering, Surveying
    Notes: The effect of haze in vertical daylight air photography for various solar altitudes is considered. If appreciable haze is present the density of negatives exposed when the solar rays are inclined to the vertical at angles less than the lens field semi-angle may vary over the field to such an extent that the photographs will be unsuitable for survey purposes. A theoretical investigation is made and practical results analysed. Methods by which the phenomena may be avoided are suggested. The effect on negative density of the variation in shadow length across the picture is also discussed.
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    Notes: In Part I the visual processes involved in depth perception are briefly described and discussed, while in Part II their application in stereo plotting and allied observations is considered. Reference is made to the visual axis, the need for and nature of eye movements, the conception of the horopter space within which fusion of the binocular images occurs and objects are seen in three-dimensions, and the tolerances for fusion implied by the existence of Panum's areas. Monocular clues make an important contribution to the perception of depth, and the apparent location of an object in space is determined by the factors of retinal disparity, convergence, angular size, perspective, motion parallax, elevation, aerial haze, etc. The following problems are then discussed: The significance of the horopter in relation to the general contour in a stereo photograph; the fusion of the images in a stereo plotting machine; the arguments for and against some convergence of the eyepiece axes; the special problems of spectacle wearers; the functions of field stop. An analysis of the visual task in contour plotting is attempted, but a more complete analysis would be possible if records were available of the observer's eye movements while plotting. Finally, chromatic aberration in relation to the Multiplex system is considered, and also in connection with the stereoscopic effect observed with differently coloured objects lying in a plane.
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    Geophysical prospecting 2 (1954), S. 0 
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    Topics: Geosciences , Physics
    Notes: When a rather extensive network of short distance refraction profiles was shot the following two observations were made. Firstly, the wave velocity in the weathered layer showed a quite considerable fluctuation in horizontal direction, the extreme values being of the order of 300 and 700 m/sec. A practical result of this scattering of the velocities is that an uncertainty of about 10% is introduced in the computation of the weathering corrections. The second observation is that, in the majority of cases, the travel time curve does not pass through the origin. It could be ascertained that this observation was not caused by errors in the method of observation. A probable explanation of the phenomenon is found in a theory that has been developed by Gassmann, who derived the velocity distribution for a hexagonal packing of spherical solid bodies. According to this theory extremely low velocities would occur in the first few centimeters of the crust of the earth. Qualitatively, our observations are in agreement with the theory of Gassmann.
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    Notes: The geophysicists who attempted to evaluate elastic anisotropy of some bedded formations most often gave but little information about recording and interpretating the measurements.May be they did not lay enough stress on the fact that any determination of the anisotropy factor is a critical operation and that, to have some certainty. it must be made under good conditions and then discussed.Due to the very favourable conditions offered: undisturbed tectonics and topography, relatively regular series the Berriane district in Northern Sahara, is rather well suited to accurate measurements and to an anisotropy study down to 1,250 meters. Since measurements have been carried out in the wildcat drilled at Berriane by S. N. Repal, it seems interesting to communicate the results obtained and to discuss them according to the influence of high velocity layers.It can be noted that in the clay and sand series which have been investigated, anisotropy coefficient amounts to 1.09 or so.To conclude, it seems desirable that determinations made by numerous operators should allow a more accurate knowledge of the anisotropy factor in the main types of rocks.
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    Notes: The aim of the present investigation is to examine the significance of the second derivative for the purpose of the prospective determination of the geological properties of the district of Offenburg, which are relatively wellknown as a result of both reflection seismic and bore profile findings.The calculation of the second derivative is carried out by means of three approximation formulae, which are compared with each other. In contrast to the isogam map the second derivative shows some additional characteristics, whose structural significance illuminates the comparison with the results of reflection seismics.A geological profile constructed on the basis of 6 wells completely confirms the geophysical findings.
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    Notes: Book review in This Article:DAWSON, R. B. Practical lawn craft and management of sports turf.
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    Notes: Book reviewed inThis Articles:BEDDOWS, A. R. The Ryegrasses in British Agriculture: a Survey
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    Notes: The formulas derived by the author in a preliminary paper for taking into consideration refraction when dealing with the problem of a vertical plane are extended to the three-dimensional case. Vector analysis is extensively applied. Among others it is shown that in the general case the 3 horizontal twodimensional vectors, i.e.〈list xml:id="l1" style="custom"〉1) the gradient of the time of reflection2) the direction of true dip3) the vector from the shot point to the projection of the reflecting point, point into 3 different directions.
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    Notes: The dependence of the apparent resistivity on the distance between the potential electrodes is examined and a numerical method is described permitting quantitative calculations. Such a numerical relation is also established for the transformation of Wenner graphs into Schlumberger graphs.In addition it is shown, in which manner the jumps in observed Schlumberger curves, that result from changing the probe spacing, must be smoothed out.
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    Geophysical prospecting 2 (1954), S. 0 
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    Notes: The luni-solar corrections are considered under the three following aspects:Quality of results: the application of tidal corrections to all stations is pointless as long as the operations do not substantially exceed two hours.Working conditions: it seems possible to increase the duration of programs without any loss of precision, but operating in such a way requires particular care.Behaviour of gravity meters: the introduction of tidal corrections allows to separate three kinds of instrumental drifts; a good knowledge of the mean operational drift enables to appreciate the quality of a given set of measurements.An example is given to show the possibility in some cases to detect small errors which are close to the limit of precision of the instrument.
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    Notes: Exploration of the Catania region was carried out for over a year by means of electrical soundings. The thickness of the overburden (lava and alluvium) was thus computed and the contour map of the blue clays basement shows the existence of several buried channels where new wells were drilled, all of them successful.
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    Notes: The paper consists of an account of a resistivity investigation into an old river valley in Coal Measure strata. This valley denuded several of the upper coal seams leaving behind unconsolidated material and it was the purpose of the work to be described to investigate how far the extent and nature of this material could be determined by resistivity methods conducted at the surface.As such the survey fits into a wider programme of research instigated by the National Coal Board.The feature, which is quite well known geologically, was surveyed by conventional methods and the results obtained are discussed in relation to the above project.Thus, the investigations succeeded in tracing the approximate centre line of the feature and in yielding some information on the nature and order of thickness of the deposits. Limitations of the method and its future application are also discussed.
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    Notes: The efficient production of “Geophysical Prospecting” depends upon the co-operation of the individual authors and this paper serves as a guide for them. Some suggestions are also made on the presentation of papers at meetings in the hope of promoting successful discussions.
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    Notes: A process is described whereby the interpretation of seismic reflection data is carried out by a preliminary two-dimensional plotting procedure followed by a three-dimensional migration. The concept of a surface of maximum convexity is introduced as an integral part of the process of migration. The procedures for deriving the necessary charts of curves are considered and a number of serviceable charts presented.
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    Notes: In the first part of the present paper we shall investigate the possibility of localising highly situated inclined faults with the aid of the vertical gradient and the second derivative in the direction of the vertical. Since these quantities have been computed from gravity values by means of formulae of approximation we shall have to study the question as to their applicability for possible quantitative interpretation. Particular caution should be exercised when making the usual comparison with theoretical test examples. For three effects have to be taken into account which result from the application of the formulae of approximation:〈list xml:id="l1" style="custom"〉1) The extreme values appear more or less smoothed out2) Extremal abscissae are being displaced3) The results are influenced by the orientation of the grid which forms the basis of the calculation.For a practical instance it was possible to locate a well under troublesome circumstances. This well is situated on the downthrown side of an inclined fault, the depth of the upthrown side being known as a result of another well.We shall show in the second part of the present paper how small, deeply situated structures may be recognised in the diagrams of the vertical gradient and of the second derivative. In the case of two practical instances the effect of these structures is rendered unrecognisable in the isogam map in view of regional influences. The results according to the formulae of Baranov, Elkins and Rosenbach are contrasted with each other.
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    Notes: It has been shown in a paper by L. Y. Faust that the wave velocity in rock depends on the depth below the ground surface according to a specified equation. It follows that the attitude of the planes of equal velocity is influenced by the topographic relief. Under these conditions the problem arises of how to place the reference plane in such a manner, that the fluctuations of the planes of equal velocity, that result from the fluctuations in the topography, shall not affect the results of the depth computations. In the present paper an analytical solution of this problem is given.
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    Notes: In a previous paper by the first author a method has been presented for computing the first vertical derivative of the gravity field or of the magnetic field. In the present paper an analysis is given of the errors in the first vertical derivative that result when the latter is computed by the above method. Two sorts of errors are considered. Firstly, the error in the first vertical derivative that results from the errors in interpolating between isogam lines on the Bouguer anomaly map. Secondly, the error in the first vertical derivative that results from the approximations upon which the computation method is based. The conclusion is reached that both sorts of error are only of minor importance.
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    Notes: The common notion, that the regional anomaly must be as regular as possible, can be translated into mathematical language by requiring that the regional anomaly shall be represented, over a not too large area, by a surface of the second or of the third degree. The residual anomaly is commonly defined by the requirement that its horizontal dimensions must be as small as possible. This implies that also its amplitude should be small. This requirement may be moulded into a mathematical form by stating that the square of the difference between the Bouguer anomaly and the regional anomaly, integrated over a certain area, must be a minimum. On these two definitions an analytic method is based for deriving the regional anomaly. Practical computation procedures are presented.
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    Notes: The different equations of elasticity concerning the departure of the behaviour of rocks from perfect elasticity are discussed. The theory of elastic afterworking and its significance for the propagation of elastic waves is studied in detail. It is found that this theory does not explain the observations on seismic waves in exploration geophysics so well as the theory of viscoelasticity suggested by Ricker.
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    Notes: The writer classifies problems of geophysical interpretation. He distinguishes four fundamental problems and indicates the methods of solving them. Among these methods he refers to classical methods and methods based on the writer's theoretical work.The geophysical examples are developed, as well as the very simple numerical examples. Methods of enumeration are also referred to. The whole object is to show that the practical application of the geophysical methods suggested will not give prospectors any difficulty.
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    Notes: The results obtained from a number of seismic velocity well-logging surveys and adjacent refraction sections are compared. The velocities derived by these two methods for a certain layer are found to differ appreciably. This is shown by presenting the time-depth relations of the well-surveys and the time-d stance relations of the refraction sections at three locations, plotted on graphs with sloping depth- and distance axes.
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    Metroeconomica 6 (1954), S. 0 
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