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  • Blackwell Publishing Ltd  (4,825)
  • Oxford University Press  (3,775)
  • Copernicus
  • PANGAEA
  • 1955-1959  (8,856)
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  • 1
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    PANGAEA
    In:  EPIC3Veröffentlichungen des Geobotanischen Institutes Rübel in Zürich, Bremerhaven, PANGAEA, 34, pp. 150-158
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 2
    Publication Date: 2016-02-18
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2015-10-28
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 5
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2016-01-27
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 6
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2016-04-07
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 8
    Publication Date: 2023-07-09
    Keywords: Abra antwerpiensis; Acamptpgenotia escheri; Acera bellardii; Acirsa lanceolata; Aclaeon inflatus; Actaeonidea terebelloides; Actaeon semistriatus; Admete fusiformis; Alvania antwerpiensis; Alvania belgica; Amusium woodi; Anadara diluvii; Anadara suessi; Ancilla obsoleta; Ancistrosyrinx cometi; Angulus fallax; Angulus posterus; Anomia epphippium; Aphinotoma debilis; Aporrhais alata; Aporrhais speciosa margerini; Aquilofusus beyrichi; Aquilofusus oppenheimi; Aquilofusus virgineus; Arca pectunculoides; Architectonica carocollatum; Architectonica simplex; Astarle triangularis; Astarte goldfussi; Astarte gracilis; Astarte pygmaea; Astarte radiata; Astenotoma pannus; Asthenotoma basteroti; Asthenotoma colus; Asthenotoma festiva; Asthenotoma pannoides; Aturia aturi; Bathytoma cataphracta; Bathytoma mioturbida; Bittium spina; Borsonia uniplicata; Cadulus gadus; Calliostoma laureatum; Calliostoma muelleri; Calyptraea chinensis; Cancellaria aperta; Cancellaria behmi; Cancellaria beyrichi; Cancellaria calais; Cancellaria cancellata praecedens; Cancellaria contorta; Cancellaria mitraeformis parvula; Cancellaria umbilicaris pluricostata; Cancellaria varicosa; Capulus striatulus; Capulus ungaricus; Cardita chamaeformis; Cardita squamulosa; Cardium danubianum; Cardium hanseatum; Cardium papillosum; Cardium straeleni; Cerithella genei; Cerithiopsis subsoluta; Chama gryphaeoides; Chlamys angelonii; Chlamys edegemensis; Chlamys ercolanianus; Chlamys lilli; Chlamys radians; Chlamys spinulosus duwelzi; Chlamys tigerinus; Chrysallida pygmaea; Cingula proxima; Circulus hennei; Circulus praecedens; Circulus striatus; Clavatula boreointerrupta; Clavatula boreoromana; Clavatula hemmoorensis; Clavatula obliquiplicatula; Clavatula olgae; Clavus bicingulatus; Clavus borealis; Clavus diensti; Clavus hannoveranus; Clavus obtusangulus; Clavus selenkae; Clavus terebra intermedia; Conus dujardini; Corbula basteroti; Corbula gibba; Corbulamya donaciformis; Crepidula cvepidula; Cuspidaria costellata; Cuspidaria cuspidata; Cylichna cylindracea; Cymatium tarbellianum; Daphnella anceps; Daphnella grippi; Daphnella rappardi; Daphnella scabra; Daphnella zetes; Dentalium dollfussi; Dentalium entale; Dentalium michelotti; Dentalium novemcostatum mutabile; Dentalium vitreum; Distorsio tortuosum; Donax intermedius; Dorsanum boreobaccatum; Dosinia basteroti; Ensis ensis; Ervilia pusilla; Erycina degrangii; Eulimella acicula; Eulimella hoernesi; Eulimella neumayri; Exilia contigua; Genota ramosa elisae; Genota ramosa parvicarinata; Globularia compressa; Glycimeris pilosa; Gouldia minima; Haedropleura maitreja; Hydrobia antwerpiensis; Isocardia lunulata; Isocardia punctata; Laevicardium cyprium; Lathyrus rothi; Leda emarginata; Leda pygmaea; Leda westendorpi; Lepton transversarium; Lienardia boehmi; Lienardia elatior; Lienardia luisae; Lienardia textilis; Lima subauriculata; Limopsis aradasi; Limopsis aurita; Limopsis lamellata; Liomesus pompeckyi; Lucina fragilis; Lutetia nitida; Mangilia g¸richi; Mangilia miorugulosa; Mangilia roemeri; Mangilia tenella; Martesia rugosa; Melanella lactea; Melanella polita; Mitra bellardii; Mitra grateloupi; Mitra planicosta; Modiolus phaseolinus; Momtacuta truncata; Montacuta coarctata; Murex delbosianus scalariformis; Murex inornatus; Murex nysti; Murex spinicosta; Musculus sp.; Mytilus fuscus; Nassa cavata; Nassa cymbrica; Nassa facki; Nassa holsatica; Nassa polsensis; Nassa prismatica; Nassa schroederi; Nassa scklotheimi; Nassa serraticosta; Nassa tenuistriata; Nassa tumida crassispiralis; Nassa turbinella; Natica beyrichi; Natica hayiseata; Niso terebellum acarinatoconica; Nucula haesendoncki; Nucula jeffreysi; Nucula laevigata; Nucula nucleus; Odostomia conoidea; Oliva dufresnei procera; Opalia pertusa; Opalia straeleni; Opalia torulosa perconica; Ostrea cochlear; Ostrea digitalina; Pandora inaequivalvis; Panopaea menardi; Pecten brummeIi; Pecten subbenedictus; Peratotoma hosiusi; Phacoides borealis; Phacoides dentatus laevigatas; Phacoides droueti; Phalium bicoronatum; Phalium miolaevigatum; Philbertia reticulata; Phos decussatus; Pinna pectinata; Pirula condita; Pirula simplex; Pitar chionoides; Pitar cimbrica; Pitar incrassata nysti; Pitar rudis; Polynices catena helicina; Polynices catena johannae; Polynices miopusilla; Polynices olla; Polynices submamillaris dertomamilla; Polynices varians protractus; Potamides tricinctus; Pteria phalaenacea; Pyramidella plicosa; Pyrene corrugata; Pyrene nassoides; Pyrgulina cimbrica; Raphitoma plicatella; Retusa elongata; Retusa truncatula; Ringicula auriculata buccinea; Ringicula auriculata ventricosa; Ringicula costata; Sabatia utricula; Sample comment; Sandbergeria wolffi; Saxicava arctica; Scacchia cimbrica; Scala amoena subreticula; Scala crassicostata; Scala crebricostellata; Scala frondicula; Scala procomitalis; Scala sallomacensis nordica; Scala weyersi; Scaphander grateloupi; Scaphella bolli; Schleswig-Holstein, Germany; Scurria compressiuscula; Seila trilineata; S-H; Sigaretus aquensis deshayesi; Sipho grippi; Solariella miosuturalis; Solariella straeleni; Solariella tournoueri; Solenocurtus basteroti; Spiratella atlanta; Spisula subtruncata triangula; Streptochetus sexcostatus; Strombiformis taurinensis; Taras trigonulus; Teinostoma hanseata; Terebra acuminata; Terebra basteroti; Terebra hoernesi; Terebra neglecta; Thapsiella costulata; Thracia ventricosa; Thyasira flexuosa; Tornus dollfussi; Triphora fritschi; Trophon vaginatus semperi; Turbonilla amoena; Turbonilla densecostata; Turbonilla elegantissima gastaldi; Turbonilla miomutinensis; Turbonilla miostriatula edegemensis; Turbonilla pseudoauricula; Turbonilla pseudoterebralis; Turricula steinvorthi; Turris boreoturricula; Turris coronata; Turris denticula borealis; Turris duchasteli flexiplicata; Turris inermis; Turris stoffelsi; Turris zimmermanni; Turritella eryna; Turritella geinitzi; Turritella subangulata; Typhis fistulosus; Vaginella depressa; Venus multilamella; Venus ovata; Vermetus intortus woodi; Vexillum aciculum; Vexillum cimbricum; Volvula acuminata; Xenophora deshayesi; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 294 data points
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  • 9
    Publication Date: 2023-07-09
    Keywords: Acamptogenotia straeleni; Admete subangulosa; Anadara diluvii; Aporrhais alata; Aquilofusus semiglaber; Arca pectunculoides; Astarte fusca; Astarte reimersi; Astarte waeli; Asthenotoma festiva; Bathytoma cataphracta; Bathytoma mioturbida; Cancellaria rothi; Cardita orbicularis; Cardium papillosum; Chlamys radians; Clavus obeliscus; Clavus obtusangulus; Clavus staringi; Conus antediluvianus; Corbula gadus; Corbula gibba; Counting; Cylichna cylindracea; Drillia modiola; Gauss-Krueger Hochwert; Gauss-Krueger Rechtswert; Gauss-Krueger Streifen; Isocardia forchhammeri; Leda pygmaea; Mangelia sp.; Murex spinicosta; Nassa prismatica; Nassa syltensis; Natica koeneni; Nucula jeffreysi; Nucula laevigata; Phalium miolaevigatum; Philbertia reticulata; Pyramidella plicosa; Pyrene nassoides; Ringicula auriculata; Sabatia utricula; Sample ID; Scala frondicula; Schleswig-Holstein, Germany; Sipho distinctus; Spisula subtruncata triangula; Streptochetus sexcostatus; Terebra forchhammeri; Trophon vaginatus semperi; Turbonilla densecostata; Turris annae; Turris aquensis; Turris badensis; Turris helena; Turritella tricarinata; Turritella triplicata; Typhis fistulosus; Uetersen; Venus multilamella; Xenophora testigera; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 10
    Publication Date: 2023-07-09
    Keywords: Abra antwerpiensis; Acamptpgenotia escheri; Acera bellardii; Acirsa lanceolata; Aclaeon inflatus; Actaeonidea terebelloides; Actaeon semistriatus; Admete fusiformis; Alvania antwerpiensis; Alvania belgica; Amusium woodi; Anadara diluvii; Anadara suessi; Ancilla obsoleta; Ancistrosyrinx cometi; Angulus fallax; Angulus posterus; Anomia epphippium; Aphinotoma debilis; Aporrhais alata; Aporrhais speciosa margerini; Aquilofusus beyrichi; Aquilofusus oppenheimi; Aquilofusus virgineus; Arca pectunculoides; Architectonica carocollatum; Architectonica simplex; Astarle triangularis; Astarte goldfussi; Astarte gracilis; Astarte pygmaea; Astarte radiata; Astenotoma pannus; Asthenotoma basteroti; Asthenotoma colus; Asthenotoma festiva; Asthenotoma pannoides; Aturia aturi; Bathytoma cataphracta; Bathytoma mioturbida; Behrendorf; Bittium spina; Borsonia uniplicata; Cadulus gadus; Calliostoma laureatum; Calliostoma muelleri; Calyptraea chinensis; Cancellaria aperta; Cancellaria behmi; Cancellaria beyrichi; Cancellaria calais; Cancellaria cancellata praecedens; Cancellaria contorta; Cancellaria mitraeformis parvula; Cancellaria umbilicaris pluricostata; Cancellaria varicosa; Capulus striatulus; Capulus ungaricus; Cardita chamaeformis; Cardita squamulosa; Cardium danubianum; Cardium hanseatum; Cardium papillosum; Cardium straeleni; Cerithella genei; Cerithiopsis subsoluta; Chama gryphaeoides; Chlamys angelonii; Chlamys edegemensis; Chlamys ercolanianus; Chlamys lilli; Chlamys radians; Chlamys spinulosus duwelzi; Chlamys tigerinus; Chrysallida pygmaea; Cingula proxima; Circulus hennei; Circulus praecedens; Circulus striatus; Clavatula boreointerrupta; Clavatula boreoromana; Clavatula hemmoorensis; Clavatula obliquiplicatula; Clavatula olgae; Clavus bicingulatus; Clavus borealis; Clavus diensti; Clavus hannoveranus; Clavus obtusangulus; Clavus selenkae; Clavus terebra intermedia; Conus dujardini; Corbula basteroti; Corbula gibba; Corbulamya donaciformis; Crepidula cvepidula; Cuspidaria costellata; Cuspidaria cuspidata; Cylichna cylindracea; Cymatium tarbellianum; Daphnella anceps; Daphnella grippi; Daphnella rappardi; Daphnella scabra; Daphnella zetes; Dentalium dollfussi; Dentalium entale; Dentalium michelotti; Dentalium novemcostatum mutabile; Dentalium vitreum; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Distorsio tortuosum; Donax intermedius; Dorsanum boreobaccatum; Dosinia basteroti; Ensis ensis; Ervilia pusilla; Erycina degrangii; Eulimella acicula; Eulimella hoernesi; Eulimella neumayri; Event label; Exilia contigua; Gauss-Krueger Hochwert; Gauss-Krueger Rechtswert; Gauss-Krueger Streifen; Genota ramosa elisae; Genota ramosa parvicarinata; Globularia compressa; Glycimeris pilosa; Gouldia minima; Großenwiehe; Haedropleura maitreja; Hydrobia antwerpiensis; Isocardia lunulata; Isocardia punctata; Laevicardium cyprium; Lathyrus rothi; Leda emarginata; Leda pygmaea; Leda westendorpi; Lepton transversarium; Lienardia boehmi; Lienardia elatior; Lienardia luisae; Lienardia textilis; Lima subauriculata; Limopsis aradasi; Limopsis aurita; Limopsis lamellata; Liomesus pompeckyi; Lucina fragilis; Lutetia nitida; Mangilia g¸richi; Mangilia miorugulosa; Mangilia roemeri; Mangilia tenella; Martesia rugosa; Melanella lactea; Melanella polita; Mitra bellardii; Mitra grateloupi; Mitra planicosta; Modiolus phaseolinus; Momtacuta truncata; Montacuta coarctata; Murex delbosianus scalariformis; Murex inornatus; Murex nysti; Murex spinicosta; Musculus sp.; Mytilus fuscus; Nassa cavata; Nassa cymbrica; Nassa facki; Nassa holsatica; Nassa polsensis; Nassa prismatica; Nassa schroederi; Nassa scklotheimi; Nassa serraticosta; Nassa tenuistriata; Nassa tumida crassispiralis; Nassa turbinella; Natica beyrichi; Natica hayiseata; Niso terebellum acarinatoconica; Nucula haesendoncki; Nucula jeffreysi; Nucula laevigata; Nucula nucleus; Odderade; Odostomia conoidea; Oliva dufresnei procera; Opalia pertusa; Opalia straeleni; Opalia torulosa perconica; Ostrea cochlear; Ostrea digitalina; Oxlund; Pandora inaequivalvis; Panopaea menardi; Pecten brummeIi; Pecten subbenedictus; Peratotoma hosiusi; Phacoides borealis; Phacoides dentatus laevigatas; Phacoides droueti; Phalium bicoronatum; Phalium miolaevigatum; Philbertia reticulata; Phos decussatus; Pinna pectinata; Pirula condita; Pirula simplex; Pitar chionoides; Pitar cimbrica; Pitar incrassata nysti; Pitar rudis; Polynices catena helicina; Polynices catena johannae; Polynices miopusilla; Polynices olla; Polynices submamillaris dertomamilla; Polynices varians protractus; Potamides tricinctus; Pteria phalaenacea; Pyramidella plicosa; Pyrene corrugata; Pyrene nassoides; Pyrgulina cimbrica; Raphitoma plicatella; Retusa elongata; Retusa truncatula; Ringicula auriculata buccinea; Ringicula auriculata ventricosa; Ringicula costata; Sabatia utricula; Sample ID; Sandbergeria wolffi; Saxicava arctica; Scacchia cimbrica; Scala amoena subreticula; Scala crassicostata; Scala crebricostellata; Scala frondicula; Scala procomitalis; Scala sallomacensis nordica; Scala weyersi; Scaphander grateloupi; Scaphella bolli; Schleswig-Holstein, Germany; Scurria compressiuscula; Seila trilineata; Sigaretus aquensis deshayesi; Sipho grippi; Solariella miosuturalis; Solariella straeleni; Solariella tournoueri; Solenocurtus basteroti; Spiratella atlanta; Spisula subtruncata triangula; Streptochetus sexcostatus; Strombiformis taurinensis; Suederhastedt; Taras trigonulus; Teinostoma hanseata; Terebra acuminata; Terebra basteroti; Terebra hoernesi; Terebra neglecta; Thapsiella costulata; Thracia ventricosa; Thyasira flexuosa; Tornus dollfussi; Triphora fritschi; Trophon vaginatus semperi; Turbonilla amoena; Turbonilla densecostata; Turbonilla elegantissima gastaldi; Turbonilla miomutinensis; Turbonilla miostriatula edegemensis; Turbonilla pseudoauricula; Turbonilla pseudoterebralis; Turricula steinvorthi; Turris boreoturricula; Turris coronata; Turris denticula borealis; Turris duchasteli flexiplicata; Turris inermis; Turris stoffelsi; Turris zimmermanni; Turritella eryna; Turritella geinitzi; Turritella subangulata; Typhis fistulosus; Vaginella depressa; Venus multilamella; Venus ovata; Vermetus intortus woodi; Vexillum aciculum; Vexillum cimbricum; Vioel; Volvula acuminata; Xenophora deshayesi; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 3574 data points
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  • 11
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    PANGAEA
    In:  Supplement to: Niino, Hiroshi (1955): On a manganese nodule and Perotrochus beyrichii dredged from the banks near the Izu Islands. Records of Oceanographic works in Japan, 2(2), 120-126, hdl:10013/epic.47489.d001
    Publication Date: 2023-08-28
    Description: Manganese nodules have been found by the author in the shallow waters of the Hyotan-se bank west of Shikime-jima, an island of the Izu archipelago in the Sea of Japan. The slopes around the bank are steep and rocks are exposed; gravels and coarse material cover the broad and flat plain on its top; andesite and basalt, which are very common in the bedrock, are found mingled with liparite gravels together with a number of manganese concretions from the bank.
    Keywords: Dredge; DRG; Hakuho-Maru; HAM_1968-1976; JAPAN_B; Japan Sea; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 12
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    PANGAEA
    In:  Supplement to: Goldberg, Edward D; Arrhenius, Gustaf (1958): Chemistry of Pacific pelagic sediments. Geochimica et Cosmochimica Acta, 13(2-3), 153-212, https://doi.org/10.1016/0016-7037(58)90046-2
    Publication Date: 2023-08-28
    Description: The chemical and mineralogical composition of pelagic sediments from the East Pacific Ocean has been determined with the aim of defining the ultimate sources and the mechanisms of formation of the solid phases. The distribution of elements between sea-water, the pore solution and the various solid components of the sediments permits interpretations of the variations in time and space of the gross chemical composition of pelagic clays. For example, manganese, present in sea-water in a divalent form, is apparently oxidized at the sediment-water interface to tetravalent species which subsequently become a part of the group of ferromanganese oxide minerals which are found in the marine environment. It is suggested the rate of manganese accumulation in sediments is some function of the length of time the sediment surface is in contact with sea-water. The contribution of chemical species from the different geospheres is considered. The quantitative importance of pelagic clays in the major sedimentary cycle is studied on the basis of the distribution of the weathered igneous rock products between continental and pelagic deposits and sea-water. These analyses of a wide variety of pelagic clays allow a reformulation of the geochemical balance and it is concluded that pelagic clays account for approximately 13 per cent of the total mass of sediments produced over geologic time.
    Keywords: 08995002-SC11; Barium; Boron; Calcium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; File name; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; San Clemente Basin, Pacific ocean; Strontium; Tin; Titanium; Uniform resource locator/link to image; Vanadium; X-ray microanalyzer analysis (XMA); Ytterbium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 13
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    PANGAEA
    In:  Supplement to: Tatsumoto, M; Goldberg, Edward D (1959): Some aspects of the marine geochemistry of uranium. Geochimica et Cosmochimica Acta, 17(3-4), 201-208, https://doi.org/10.1016/0016-7037(59)90094-8
    Publication Date: 2023-08-28
    Description: The uranium concentrations in marine calcareous material of a biological origin varied between 0.0X and 0.X p.p.m. with the exception of corals which had concentrations of several p.p.m. The aragonitic oolites and aragonite precipitated from sea-water had values similar to those of the corals. A geochronology based on the growth of ionium (thorium-230) from uranium is applicable not only to corals, as previous investigators have pointed out, but also to oolites. Several examples of "oolite ages" are given. The uranium content of ferromanganese minerals from pelagic deposits is of the order of from 4 to 5 p.p.m.
    Keywords: Atlantic Ocean; DEPTH, sediment/rock; DNWB0BBD; DNWB0BBD-047G; DNWB0BBD-052G; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG47; DWBG52; DWHD55; Event label; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Spencer F. Baird; TH1; TH1-TR4; Theta; Uranium; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 14
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1957): MUKLUK Expedition, July-August, 1957: Cores and Dredge Samples. SIO Reference Series, 57-53, 6 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described are taken during the MUKLUK expedition of the R/V Spencer Baird in July-August 1957 by the Scripps Institute of Oceanography. A total of 31 cores and dredges were recovered and are available at Scripps Institute of Oceanography for sampling and study.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Latitude of event; Longitude of event; MKLK02BD; MKLK03BD-029D; MKLK03BD-030D; MUKLUK-B; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 21 data points
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  • 15
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    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1958): Drift Station Alpha - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2023-08-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) on the Drift Station Alpha in the Arctic Ocean from August 1957 until June 1958. A total of 16 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Arctic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DSA-10; DSA-12; DSA-5; DSA-9; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to metadata file
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 16
    Publication Date: 2023-08-28
    Description: Deposits of manganese ore have been found in five of the six provinces of Cuba and have been reported from the sixth. Only Oriente and Pinar del Rio provinces have more than a few known deposits and only the deposits of Oriente have yielded any appreciable amount of ore. In this area the Cobre formation, of late Cretaceous(?) to middle Eocene age, overlies the Vinent formation but their stratigraphie relations are unknown. The Cobre overlies unconformably the Habana(?) formation. The Cobre formation consists of andesitic, basaltic, and dacitic tuff, agglomerate, and lavas with minor amounts of marine clastic and limestone deposits, and a prominent limestone bed, the Charco Redondo limestone member, at the top of the formation. All productive manganese deposits of Oriente are in the Cobre formation, usually within a few tens of meters above or below the base of the Charco Redondo limestone member.
    Keywords: Charco_Redondo_S; Comment; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Guanaba_S; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Ponupo_S; Position; Quantity of deposit; Quinto_S; Sample ID; Sediment type; Size; Substrate type; Taratana_S
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 17
    Publication Date: 2023-08-28
    Description: Saipan, situated about 15° N. and 146° E., is one of the larger and more southerly of the Mariana Islands. The 15 small islands of this chain are strung along an eastwardly convex ridge for more than 400 miles north to south, midway between Honshu and New Guinea and about 1,200 miles east of the Philippines. Paralleling this ridge 60 to 100 miles further east is a deep submarine trench, beyond which lies the Pacific Basin proper. To the west is the Philippine Sea, generally deeper than 2,000 fathoms. The trench coincides with a zone of negative gravity anomalies, earthquake foci occur at increasing depths westward from it, and silica- and alumina-rich volcanic rocks characterize the emergent island chain itself. The contrast between these features and those of the Pacific Basin proper to the east is held to favor the conclusion that the Mariana island arc and trench define the structural and petrographic front of Asia.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Mariana Islands; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Papago_C; Position; Quantity of deposit; Sample ID; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 18
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    In:  Supplement to: Jones, L H P; Milne, Angela A (1956): Birnessite, a new manganese oxide mineral from Aberdeenshire, Scotland. Mineralogical Magazine, 31(235), 283-288, https://doi.org/10.1180/minmag.1956.031.235.01
    Publication Date: 2023-08-28
    Description: A manganese pan near Birness contains grains of an optically uniaxial negative mineral near (Na0.7Ca0.3)Mn7O14·2·8H2O, giving an X-ray powder pattern similar to that of synthetic materials described as 'manganous manganite' and delta-MnO2. Material giving a similar pattern has been described from a natural occurrence in Canada, but no mineral name was assigned; the name birnessite is now proposed. The mineral is probably formed by air-oxidation of manganous oxides under alkaline conditions.
    Keywords: Aluminium oxide; Birness_J; Calcium oxide; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese dioxide; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Scotland; Sediment type; Silicon dioxide; Sodium oxide; Titanium dioxide; Water in rock
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 19
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    In:  Supplement to: Dietz, Robert S (1955): Manganese deposits on the northeast Pacific sea floor. California Journal of Mines and Geology, 51(3), 209-220, https://archive.org/details/californiajourna53cali
    Publication Date: 2023-08-28
    Description: Sea floor dredging by the H.M.S. Challenger, the U.S.S. Albatross, the U.S.S. EPC(R) 857, and vessels of the Scripps Institution of Oceanography shows that extensive deposits of manganese nodules are on the deep sea floor and that crusts of manganese dioxide cover many seamounts. Sea floor photography reveals that in some places these crusts are quite continuous and the nodules are closely packed. These crusts and nodules are fully oxidized and hydrated mixtures of man¬ganese and iron plus earthy impurities. Also, relatively high concen¬trations of the trace elements nickel, copper, and cobalt are present.
    Keywords: DICH-SS; Dredge; Dredge, rock; DRG; DRG_R; Erben Seamount, Pacific Ocen; GOLDHW1; Horizon; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MDPC02HO-MP-037A; MIDPAC; MPC-25F-2; MPC-26A-3; MPC-37A; NEL-667; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; Sylvania Seamount, Pacific Ocean; Wired profile sonde; WP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 20
    Publication Date: 2023-08-28
    Description: The Kara scientific expedition of 1945, using the fishing trawler M. Gorkiy and survey vessel Osetr, took sediment samples in the Kara Sea in addition to other oceanographic work. The investigations of sediments composition was compared with biological and hydrological data obtained in the same areas. The sediments sampled were subjected to mechanical, mineralogical, chemical and faunistic analyses. During this survey iron-manganese concretions were recovered.
    Keywords: Deposit type; DEPTH, sediment/rock; Description; EG; Ekman grab; Elevation of event; Event label; GORK45-10; GORK45-11; GORK45-14; GORK45-16; GORK45-17; GORK45-18; GORK45-19; GORK45-20; GORK45-21; GORK45-30; GORK45-32; GORK45-37; GORK45-39; GORK45-4; GORK45-7; GORK45-8; Gorkiy1945; Identification; Kara Sea; Latitude of event; Longitude of event; Maxim Gorkiy; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Peterson grab; PETG; Position; Quantity of deposit; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 21
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    In:  Supplement to: Hurley, RJ (1956): Expedition CHINOOK I, Lowering log, June-August 1956. University of California, Scripps Institution of Oceanography, Unpublished, hdl:10013/epic.46558.d001
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the CHINOOK Expedition in July to August 1956 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 20 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: CHIN02BD; CHIN02BD-013GA; CHIN02BD-016G; CHIN0ABD-001G; CHIN0ABD-002G; CHIN0ABD-004G; CHIN0ABD-006G; CHIN0ABD-007G; CHINOOK; CHNK-13G; CHNK-16G; CHNK-18G; CHNK-1G; CHNK-2G; CHNK-4G; CHNK-6G; CHNK-7G; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 22
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    In:  Supplement to: Bruun, Anton F (1959): General introduction to the reports and list of deep-sea stations. in: Galathea Report - Scientific Results of the Danish Deep Sea Expedition Round the World. 1950-1952, Danish Science Press, Copenhagen, Denmark, 7-48
    Publication Date: 2023-08-28
    Description: The Danish Expedition of the "Galathea II" around the world brought important results concerning the marine organisms in the deep sea. The "Galathea II" showed not only different organisms of the Abyssal but for the first time of the deepest trenches of the western Pacific. Anton Bruun coined the term Hadal for the region below the Abyssal under 6000 m. Although the "Galathea II" aimed to investigate new deep sea regions beside the routes of former expeditions and to widen the horizon of knowledge relating marine organisms the technical equipment and the methodological approach had partly been developed earlier. The expedition of the "Galathea II" is part of a long tradition of cruises such as that of the British "Challenger", the German "Valdivia" and the Swedish "Albatross" and especially the Danish cruises of the "Dana I" and "Dana II" which happened some years before.
    Keywords: Banda Sea; Comment; Core; CORE; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GAL_1950-1952_Denmark; Galathea; GALT-179; GALT-182; GALT-435; GALT-469; GALT-494; GALT-574; GALT-658; GALT-724; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Philippine Sea; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Tasman Sea
    Type: Dataset
    Format: text/tab-separated-values, 73 data points
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  • 23
    Publication Date: 2023-08-28
    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
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  • 24
    Publication Date: 2023-08-28
    Description: The cores described in this list were taken on the THETA-1 (TH1) Expedition in June to September 1956 from the R/V Theta. A total of 19 cores and dredges were recovered and are archived at Scripps for sampling and study.
    Keywords: Atlantic Ocean; C-58; C-60; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; TH1; TH1-57SCC; TH1-59SCC; TH1-TR4; TH1-TR6; TH1-TR7; Theta; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 25
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1959): FANFARE Expedition 1959, List of cores and dredge samples copied from shipboard logs (R/V H. M. Smith and R/V Spencer F. Baird). Scripps Institution of Oceanography, UC San Diego, unpublished, 6 pp, https://www.ngdc.noaa.gov/mgg/geology/data/1599/15995003/15995003.pdf
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken on the FANFARE Expedition in July 1959 by Scripps Institution of Oceanography from the R/V H. M. Smith and the R/V Spencer F. Baird. A total of 49 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites, all in the eastern tropical central Pacific.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, chain bag; DRG_C; Elevation of event; Event label; FANB01BD; FANB01BD-024G; FANBD-20D; FANBD-24G; FANBD-25D; FANFARE-B; FANFARE-S; FANS01HMS; FANS01HMS-016G; FANS-16G; GC; Gravity corer; H.M. Smith; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Size; Spencer F. Baird; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 26
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    In:  Supplement to: Bramlette, M; Faughn, James L; Hurley, RJ (1959): Anomalous sediment deposition on the flank of Eniwetok Atoll. Geological Society of America Bulletin, 70(12), 1549-1552, https://doi.org/10.1130/0016-7606(1959)70%5B1549:ASDOTF%5D2.0.CO;2
    Publication Date: 2023-08-28
    Description: Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
    Keywords: 10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 341 data points
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  • 27
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1959): Expedition VEMA 15. Lamont Geological Observatory, Columbia University, New York, unpublished, 26 pp, https://www.ngdc.noaa.gov/mgg/curator/data/vema/vm15/vm15_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 15 Expedition from October 1958 until July 1959 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 410 cores and dredges 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; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TRAWL; Trawl net; V15; V15-003PD; V15-101; V15-119SBT; V15-120SBT; V15-122SBT; V15-125SBT; V15-129; V15-130; V15-131; V15-135; V15-135SBT; V15-136; V15-138; V15-144; V15-151SBT; V15-160; V15-187; V15-188; V15-197; V15-202; V15-30; V15-40; V15-44A; V15-45; V15-47; V15-48; V15-61SBT; V15-66; V15-77SBT; V15-78SBT; V15-79SBT; V15-8; V15-80SBT; V15-81SBT; V15-82SBT; V15-95SBT; Vema
    Type: Dataset
    Format: text/tab-separated-values, 698 data points
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  • 28
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    In:  Supplement to: Ericson, D; Baker, RN; Goldstein, RF (1955): Vema Cruise 07 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 8 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm07/vm07_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 7 Expedition from May until September 1955 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 78 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; V07; V07-25; V07-61; V07-71; V07-8; Vema
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 29
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    In:  Supplement to: Hekinian, Roger; Starkes, J; Ericson, D (1956): Vema Cruise 09 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, 40 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 9 Expedition from February until April 1958 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 34 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; V09; V09-13TW; V09-15; V09-16; V09-18; V09-2; V09-21; V09-26; V09-28; V09-33; V09-9; Vema
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 30
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    In:  Supplement to: Ericson, D; Morgenstein, M; Grinnell, R (1956): Vema Cruise 10 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 145 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 10 Expedition from June until September 1956 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 95 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; V10; V10-1; V10-11; V10-19; V10-20; V10-21; V10-32; V10-42; V10-50; V10-6; V10-65; V10-72; V10-77; V10-78; V10-80; V10-82; V10-83; V10-88; V10-95; V10-97; V10-99; Vema
    Type: Dataset
    Format: text/tab-separated-values, 254 data points
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  • 31
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1957): Vema Cruise 12 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 87 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 12 Expedition from December 1956 until August 1957 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 119 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; V12; V12-1; V12-101; V12-103; V12-104; V12-107; V12-108; V12-109; V12-111; V12-114; V12-115; V12-116; V12-117; V12-120; V12-121; V12-127; V12-128; V12-14; V12-19; V12-20; V12-22; V12-52; V12-54; V12-56; V12-65; V12-72; V12-73; V12-80; V12-85; V12-93; V12-96; V12-97; V12-98; V12-99; Vema
    Type: Dataset
    Format: text/tab-separated-values, 377 data points
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  • 32
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    In:  Supplement to: Kuno, Hisashi; Fisher, Robert L; Nasu, Noriyuki (1956): Rock fragments and pebbles dredged near Jimmu Seamount, northwestern Pacific. Deep Sea Research, 3(2), 126-133, https://doi.org/10.1016/0146-6313(56)90090-9
    Publication Date: 2023-08-28
    Description: Fifty-five rock fragments and pebbles were dredged at 2,550-2,800 fathoms (4,650-5,100 metres) near Jimmu Seamount, 700 miles southeast of Kamchatka. Tuffaceous shale, andesitic and dacitic tuff, pyroxene-hornblende dacite-pumice, and augite-hypersthene andesite are the most abundant rock types. Minor constituents in the haul include augite-pigeonite basalt, augite-olivine basalt, olivine dolerite, quartz syenite porphyry, metabasalt, sandstone, and chert. Petrographic and chemical analyses indicate closer affinities with Kuril Islands and Kamchatka volcanic rocks than with Cenozoic Japanese or Pacific Basin types. Probably these rocks were dropped by Pleistocene icebergs carried south and east by ocean currents.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Substrate type; TRAN_JG; TRANSPAC; Trans-Pacific; Uniform resource locator/link to image; Western Pacific
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 33
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    In:  Supplement to: Ljunggren, P (1955): Geochemistry and radioactivity of some Mn and Fe bog ores. Geologiska Föreningens i Stockholm förhandlingar: GFF (The transactions of the Geological Society of Sweden, 77(1), 33-44, https://doi.org/10.1080/11035895509455349
    Publication Date: 2023-08-28
    Description: The trace element content of different bog ores has been measured and it appeared that most of these elements are enriched in the manganiferous bog ores as compared with the ferriferous ones. The manganiferous bog ores have also proved to have a higher radioactivity than the ferriferous ones.
    Keywords: Barium; Beryllium; Boron; Caesium; Chromium; Cobalt; DEPTH, sediment/rock; Description; Detector raw counts; Event label; Geiger counter; Identification; Iron oxide, Fe2O3; Lake Tisjoen, Sweden; Lead; Lika_L; Manganese dioxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; River Lika, Sweden; Rubidium; Strontium; Tisjoen_L; Vanadium; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 181 data points
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  • 34
    Publication Date: 2023-08-28
    Keywords: Cerium oxide; CHA-276; Challenger1872; DEPTH, sediment/rock; Description; Grab; GRAB; H.M.S. Challenger (1872); Mercury oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample code/label; Thorium oxide
    Type: Dataset
    Format: text/tab-separated-values, 5 data points
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  • 35
    Publication Date: 2023-08-28
    Keywords: 248; CHA-248; CHA-252; CHA-276; Challenger1872; DEPTH, sediment/rock; Description; Event label; Grab; GRAB; H.M.S. Challenger (1872); Insoluble material; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Sample code/label; Soluble residue; TRAWL; Trawl net
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 36
    Publication Date: 2023-08-28
    Keywords: 248; CHA-248; CHA-252; CHA-276; Challenger1872; Deposit type; DEPTH, sediment/rock; Description; Event label; Feature; Grab; GRAB; H.M.S. Challenger (1872); NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Station label; Substrate type; TRAWL; Trawl net; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 37
    Publication Date: 2023-08-28
    Keywords: ALB-13; Albatross (1882-1921); Albatross1899-1900; ALBTR-13; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 38
    Publication Date: 2023-08-28
    Keywords: Albatross (1882-1921); Albatross1904-1905; ALBTR-4658; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 39
    Publication Date: 2023-07-10
    Keywords: Batrachium; Betula; Betula nana; Betula pendula; Betula pubescens; Beug_pollen-archive; Calliergon giganteum; Calliergon sarmentosum; Calliergon stramineum; Carex rostrata; Carex sect. Eucarex; Carex sect. Vignea; Cicuta virosa; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Drepanocladus exannulatus; Drepanocladus fluitans; Eleocharis palustris; Fiberg57makro; Fichtelgebirge, Northern Germany; Helodium blandowii; Hippuris vulgaris; Juniperus; Meesea triquetra; Menyanthes trifoliata; Montia rivularis; Myriophyllum alterniflorum; Nitella; Paludella squarrosa; Pinus sp.; Pinus sylvestris; Polytrichum commune; Polytricum strictum; Potamogeton obtusifolius; Potamogeton pusillus; Potamogeton rutilus; Potentilla palustris; PROFILE; Profile sampling; Rhynchospora; Salix; Sampling on land; Sphagnum sect. Cuspidata; Sphagnum teres; Stellaria palustris
    Type: Dataset
    Format: text/tab-separated-values, 675 data points
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  • 40
    Publication Date: 2023-11-01
    Keywords: Abies; Alnus; Apiaceae; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Bupleurum; Calluna; Campanulaceae; Carpinus; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Circaea; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Fagus; Fichtelgebirge, Northern Germany; Filicinae; Filipendula; Fraxinus; Gentianaceae; Geranium; Hedera; Helianthemum alpestre; Hippophae; Juniperus; Knautia; Lamiaceae; Lycopodium annotinum; Lysimachia; Melampyrum; Onobrychis; Onosma; Picea; Pinus; Plantago lanceolata; Plantago major/media-type; Poaceae; Polygonum bistorta-type; Polypodium vulgare; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus frangula; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scrophulariaceae; SEELOH92; Seelohe; Sparganium-type; Sphagnum; Succisa; Thalictrum; Tilia cordata-type; Typha latifolia; Ulmus; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia; Viburnum
    Type: Dataset
    Format: text/tab-separated-values, 1748 data points
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  • 41
    Publication Date: 2023-11-01
    Keywords: Alnus; Apiaceae; Artemisia; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Filicinae; Filipendula; Fraxinus; Gentianaceae; Gypsophila; Hedera; Helianthemum; Hippophae; Juniperus; Kleines Rotes Moor/Rhön; Knautia; Lycopodium alpinum-type; Lysimachia; Melampyrum; Menyanthes; Montia; Onobrychis; Picea; Pinus; Plantago major/media-type; Poaceae; Polemonium; Polygonum bistorta-type; Polypodium vulgare; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus frangula; Rhinanthus; RotesMoor1; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scabiosa; Scrophulariaceae; Selaginella selaginoides; Sparganium-type; Sphagnum; Thalictrum; Tilia cordata-type; Trifolium; Ulmus; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia
    Type: Dataset
    Format: text/tab-separated-values, 2130 data points
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  • 42
    Publication Date: 2023-11-01
    Keywords: Apiaceae; Armeria; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Epilobium; Equisetum; Filicinae; Filipendula; Geranium; Harz, Germany; Helianthemum; Hippophae; Indeterminata; Juniperus; Lamiaceae; Lycopodium alpinum-type; Melampyrum; Menyanthes; Montia; Onobrychis; Pinus; Poaceae; Polygonum bistorta-type; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; RadauerBorn56; Ranunculus; Ranunculus subgen. Batrachium; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Selaginella selaginoides; Sparganium-type; Sphagnum; Thalictrum; Ulmus; Vaccinium-type; Valeriana sambucifolia; Varia
    Type: Dataset
    Format: text/tab-separated-values, 550 data points
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  • 43
    Publication Date: 2023-11-01
    Keywords: Alnus; Apiaceae; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Bupleurum; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Circaea; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cuscuta; Cyperaceae; DEPTH, sediment/rock; Drosera rotundifolia; Dryopteris filix-mas; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Fiberg57; Fichtelgebirge, Northern Germany; Filicinae; Filipendula; Fraxinus; Gentianaceae; Geranium; Hedera; Helianthemum alpestre; Helianthemum nummularium-type; Hippophae; Juniperus; Knautia; Lamiaceae; Lycopodium alpinum-type; Lycopodium inundatum; Lysimachia; Melampyrum; Menyanthes; Montia; Myriophyllum; Myriophyllum spicatum-type; Onobrychis; Picea; Pinus; Plantago lanceolata; Plantago major/media-type; Pleurospermum; Poaceae; Polemonium; Polygonum bistorta-type; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scrophulariaceae; Selaginella selaginoides; Sorbus-type; Sparganium-type; Sphagnum; Thalictrum; Thelypteris; Tilia cordata-type; Trifolium; Typha latifolia; Ulmus; Urtica; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia
    Type: Dataset
    Format: text/tab-separated-values, 6028 data points
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  • 44
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    PANGAEA
    In:  Supplement to: Riley, J P; Sinhaseni, P (1958): Chemical composition of three manganese nodules from the Pacific Ocean. Journal of Marine Research, 17, 466-482, hdl:10013/epic.46183.d001
    Publication Date: 2023-08-28
    Description: Three manganese nodules from the Pacific Ocean have been analysed for 35 elements by using mainly spectrophotometric and spectrographic methods. Cu, Co, Ni, Zn, and Pb were found in amounts approaching 1 %, which far exceeds their average concentrations in igneous rocks. On the other hand, elements having readily hydrolysable ions, such as Ga, Sc, Zr, Y, La and Ti, are present only in amounts comparable with their concentrations in igneous rocks. Sb, Bit Be, and Cr were not detected. The hydrochloric acid-insoluble fraction of nodules is practically free of the heavy metals that are characteristic of the acid-soluble fraction; it consists principally of clay minerals, together with lesser amounts of quartz, apatite, biotite and sodium and potassium felspars.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 45
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    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
    Publication Date: 2023-08-28
    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
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  • 46
    Publication Date: 2023-08-28
    Keywords: 248; Aluminium oxide; Barium oxide; Boron oxide; Cadmium oxide; Calcium oxide; Carbon dioxide; CHA-248; CHA-252; CHA-276; Challenger1872; Chromium(III) oxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; Event label; Gallium oxide; Germanium oxide; Grab; GRAB; H.M.S. Challenger (1872); Iron oxide, Fe2O3; Lanthanum oxide; Lead oxide; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Oxygen, gas; Phosphorus pentoxide; Potassium oxide; Sample code/label; Scandium oxide; Silver oxide; Sodium oxide; Spectrophotometric; Strontium oxide; Thallium(I) oxide; Tin dioxide; Titanium dioxide; TRAWL; Trawl net; Tungsten trioxide; Vanadium oxide; Water in rock; Yttrium oxide; Zinc oxide; Zirconium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
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  • 47
    Publication Date: 2023-08-28
    Keywords: ALB-173; Albatross (1882-1921); Albatross1899-1900; ALBTR-173; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 43 data points
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  • 48
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    PANGAEA
    In:  Supplement to: Pettersson, Hans (1955): Manganese nodules and oceanic radium. Deep Sea Research - Supplement to Volume 3: Papers in Marine Biology and Oceanography, Pergamon Press, London & New York, 335-345, https://archive.org/details/papersinmarinebi00lond
    Publication Date: 2023-08-28
    Description: Thanks to the courtesy of the British Museum of Natural History the author obtained from their Challenger collections two small nodules, and through a similar courtesy of the Mineralogical Department of the Riksmuseum in Stockholm one half of a much larger nodule, also from the Challenger Expedition. Results from his initial measurements of the radium contents of these samples convinced the author that the radium in the nodules is accumulated from the surrounding sediment. In the present paper the author conducted a much more thorough investigation on nodules obtained during the U.S. Albatross cruises of Dr. Agassiz. Detailed measurements of radium were conducted on individual layers and spots inside each nodule.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 49
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    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1958): Expedition VEMA 14. Lamont Geological Observatory, Columbia University, New York, unpublished, 24 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm14/vm14_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 14 Expedition from November 1957 until August 1958 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 151 cores and dredges 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; Dredge, rock; DRG_R; Elevation of event; Event label; Indian Ocean; Latitude of event; LGO-BT-57 or VM14 SBT57 (SIO); Longitude of event; Method/Device 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; V14; V14-106; V14-114; V14-132; V14-133; V14-136; V14-144; V14-16BT; V14-2; V14-28; V14-28BT; V14-46; V14-51RD; V14-57RD; V14-65; V14-69C; V14-6RD; V14-78; V14-8; V14-84A; V14-85; V14-86; V14-9; V14-91; V14-93; V14-99; Vema; VM14 51-CP (SIO); VM14 9TW (SIO)
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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  • 50
    Publication Date: 2023-08-28
    Keywords: 248; Aluminium oxide; Barium; Calcium oxide; CHA-248; CHA-252; CHA-276; Challenger1872; Cobalt; Copper; DEPTH, sediment/rock; Description; Event label; Gallium; Grab; GRAB; H.M.S. Challenger (1872); Iron oxide, Fe2O3; Lead; Magnesium oxide; Manganese oxide; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Phosphorus pentoxide; Potassium oxide; Sample code/label; Silicon dioxide; Sodium oxide; Spectrophotometric; Strontium; Tin; Titanium dioxide; TRAWL; Trawl net; Vanadium; Water in rock; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 59 data points
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  • 51
    Publication Date: 2023-08-28
    Keywords: Area/locality; Cobalt; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Erben Seamount, Pacific Ocen; Event label; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-026A-3; MIDPAC; MPC-26A-3; NEL-667; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D7; Pacific Ocean; Wet chemistry; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 52
    Publication Date: 2023-08-28
    Keywords: Area/locality; Cobalt; Deposit type; DEPTH, sediment/rock; DICH-SS; Dredge; Dredge, rock; DRG; DRG_R; Event label; GOLDHW1; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-037A; MIDPAC; MPC-37A; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; Sylvania Seamount, Pacific Ocean; Wet chemistry; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 53
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Area/locality; Calcium oxide; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Horizon; Identification; Insoluble residue; Iron; Loss on ignition; Magnesium oxide; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL-D1; Phosphorus pentoxide; Silicon dioxide; Sulfur, total; Titanium dioxide; Vanadium oxide; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 54
    Publication Date: 2023-08-28
    Keywords: Description; DICH-SS; Dredge, rock; DRG_R; Event label; File name; Horizon; MDPC02HO-MP-025F-2; MIDPAC; MPC-25F-2; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Page(s); Sylvania Seamount, Pacific Ocean; Uniform resource locator/link to image; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 55
    Publication Date: 2023-08-28
    Keywords: Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Hakuho-Maru; HAM_1968-1976; Identification; Iron; JAPAN_B; Japan Sea; Lead; Manganese; Molybdenum; Nickel; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Silicon; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 56
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Hakuho-Maru; HAM_1968-1976; Identification; JAPAN_B; Japan Sea; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 57
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    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: Acapulco Trench, Pacific ocean; CHUB01BD; CHUB01BD-001G; CHUB01BD-002G; CHUB01BD-003G; CHUB01BD-009G; CHUB01BD-017G; CHUB01BD-019G; CHUB01BD-033G; CHUB01BD-034G; CHUB01BD-039G; CHUB02BD-010G; CHUB-1; CHUB-17; CHUB-19; CHUB-2; CHUB-3; CHUB-33; CHUB-34; CHUB-39; CHUB5; CHUB-9; CHUBASCO; CHUB-X; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Feature; 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, 116 data points
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  • 58
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    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: CAP-13HG; CAP-22HG; CAP-24HG; CAP-26HG; CAP-28HG; CAP-30BG; CAP-31BG; CAP-32HG; CAP-33BG; CAP-34BG; CAP-36HG; CAP-39BG-1; CAP-41BG-1; CAP-44HG; CAP-50BG-1; CAPB01BD-030BG; CAPB01BD-031BG; CAPB01BD-033BG; CAPB01BD-034BG; CAPB01BD-039BG-01; CAPB01BD-041BG-01; CAPB01BD-050BG-01; CAPH0AHO-013G; CAPH0BHO-022G; CAPH0BHO-024G; CAPH0BHO-026G; CAPH0BHO-028G; CAPH0CHO-036G; CAPH0CHO-044G; CAPRICORN-B; CAPRICORN-H; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Event label; Feature; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Visual description
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    Publication Date: 2023-11-03
    Description: Die biologischen Arbeiten der Deutschen Antarktischen Expedition 1938/39 wurden in übereinstimmung mit dem Institut für Walforschung der damaligen Reichsanstalt für Fischerei in Hamburg durchgeführt. ... Hier sollen nur die Beobachtungen über die Wale, Robben und Vögel betrachtet werden. Verbunden damit ist ein Überblick über die hydrographischen Verhältnisse sowie die Zusammenstellung der Volumina der quantitativen Oberflächenplanktonproben.
    Keywords: Abundance estimate; Amphipoda; Appendicularia; Auricularia; BNET; Brutnetz; Chaetognatha; Chaetopoda; Comment of event; Copepoda; Counting; Counting, Stereo Microscope; Crustacea indeterminata; Ctenophora; DAE3_1; DAE3_10; DAE3_11; DAE3_12; DAE3_13a; DAE3_13b; DAE3_14; DAE3_15; DAE3_16; DAE3_17; DAE3_18; DAE3_19; DAE3_1938/39; DAE3_2; DAE3_20; DAE3_21; DAE3_22; DAE3_23; DAE3_24; DAE3_25; DAE3_26; DAE3_27; DAE3_28; DAE3_29; DAE3_3; DAE3_30; DAE3_31; DAE3_32; DAE3_33; DAE3_34; DAE3_35; DAE3_36; DAE3_37; DAE3_38; DAE3_39; DAE3_4; DAE3_40; DAE3_41; DAE3_42; DAE3_43; DAE3_44; DAE3_45; DAE3_46; DAE3_47; DAE3_48; DAE3_49; DAE3_5; DAE3_50; DAE3_51; DAE3_52; DAE3_53; DAE3_54; DAE3_55; DAE3_56; DAE3_57; DAE3_58; DAE3_59; DAE3_6; DAE3_60; DAE3_61; DAE3_62; DAE3_63; DAE3_64; DAE3_65; DAE3_66; DAE3_67; DAE3_68; DAE3_69; DAE3_7; DAE3_70; DAE3_71; DAE3_72; DAE3_73; DAE3_74; DAE3_75; DAE3_76; DAE3_77; DAE3_78; DAE3_79; DAE3_8; DAE3_80; DAE3_81; DAE3_82; DAE3_83; DAE3_84; DAE3_9; Date/Time of event; Decapoda larvae; Depth, bottom/max; Depth, top/min; DEPTH, water; Deutsche Antarktische Expedition 1938/39; Directory of research expeditions of Germany; Estimated; Event label; EXP_GER; Fish indeterminata; KN; Krill net; Large volume water sampler; Latitude of event; Longitude of event; LVS; Medusa; Method/Device of event; Mollusca; Ostracoda; PLA; Plankton net; Radiolarians indeterminata; Rubber boat, Zodiac; Schizopoda; Schwabenland; Sediment sample; SES; Siphonophora sp.; Smear slide analysis; Southern Ocean; Thaliacea; Trawling; ZODIAC
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  • 60
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
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    Topics: Architecture, Civil Engineering, Surveying
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
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    Topics: Architecture, Civil Engineering, Surveying
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  • 63
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
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    Topics: Architecture, Civil Engineering, Surveying
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  • 64
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
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  • 65
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    The @photogrammetric record 1 (1955), S. 0 
    ISSN: 1477-9730
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    Topics: Architecture, Civil Engineering, Surveying
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  • 66
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Ten new species of colorless Eugleninae are described. One of them is the type of a new genus (Calycimonas physaloides nov. gen. nov. sp.). Especially remarkable forms are: Astasia acus, a species related to the green Euglena acus but without chromatophores and stigma and considerably smaller; Astasia edax, a species with animal-like nutrition and peculiar ecological adaptations; Petalomonas striata, a form which is not spirally but transversely striated; and finally Hyalophacus caecus, which was observed already by Klebs and Pochmann but was not sufficiently described. The new genus Calycimonas (ex fam. Peranemacearum) is related to Tropidoscyphus on the one hand (nearly the same shape as e.g. Tr. octocostatus, but possessing only a single flagellum) and to Petalomonas on the other hand (mode of nutrition and of swimming, formation of the reservoir, rigidity: however in transverse section not flattened).The Astasiae with zootrophic nutrition are collected in a new subgenus Astasiae devorantes or Phytophaga which comprises besides A. edax three species already described by Skuja.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. H. canis (James) is reported from three of 36 stray dogs at Singapore and one of 34 palm civets (Paradoxurus hermaphroditus Pallas) from Jeram, Selangor. H. muris (Balfour) was found at Singapore in 10 of 61 examples of Rattus norvegicus (Erxleben) and five of 23 of R. rattus diardi (Jentinck), and is also recorded from six of 139 examples of R. r. jarak (Bonhote) from Pulau Jarak, Straits of Malacca. Neutrophils of P. hermaphroditus containing gametocytes of H. canis exhibit pronounced karyorrhexis, while most of the parasites themselves show signs of pyknosis.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. A total of 155 clones of Stylonychia putrina collected in nature were tested for mating type. Two sexually isolated varieties were found among them: Variety I with 12 mating types and Var. II with 11. Five of the clones isolated in the laboratory belonged to 3 additional mating types of Var. I making a total of 15 mating types in this variety.Crosses were made among 6 of the mating types of Var. I, and 114 clones of progeny were raised and tested for mating type. No simple genetic explanation of the results was evident.An abnormal type of conjugation with fusion of the conjugants and subsequent fission was studied. Both parental mating types sometimes segregated during the first two fissions of a fused animal. Mating type determination in the progeny of the fused animals seemed to parallel that of the progeny of the normal conjugants in that in both cases certain mating types tended to be dominant over others.
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  • 69
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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  • 70
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. The cytochemical procedure of Sen was used to demonstrate urease activity in Tetrahymena pyriformis S.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
    ISSN: 1550-7408
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    Topics: Biology
    Notes: SYNOPSIS. The chimpanzee is shown to behave like man to infection with Babesia divergens or bovis: the intact animal is totally resistant, whereas the splenectomized animal develops a fulminating infection accompanied by blackwater. The splenectomized rhesus monkey reacts in the same way also, but splenectomized rabbits are insusceptible. In the chimpanzee the typical accolé position of the “divergens” organisms (as seen in cattle) is absent, but occurs in the rhesus. It is suggested that latent piroplasmosis in man may exist on a large scale in rural populations in infected localities.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. Studies cf 3 conjugating strains of Tetrahymena pyriformis grown in a bacterized medium indicated the presence of a system of alternative immobilizing surface antigens. Each strain was found to have the potential for the expression of 3 serologically unrelated antigens. These consisted of a “high temperature” antigen (expressed in the range of 20–35d̀C), a “low temperature” antigen (exhibited in cultures at 10d̀), and an antigen induced by growth in the presence of the above-mentioned “high temperature” antiserum. Normally, by the immobilization reaction, only one of these antigens could be detected as present on any one organism at any given time. The “high temperature” antigens of two of the strains were serclogically related while that of the 3rd strain did not cross-react with antisera to the other two. The “low temperature” antigens of the 3 strains were serologically related as were the antigens induced by growth in antiserum.Studies of inbred hybrids of two of the strains indicated a potential for still more alternative antigens as well as for the spontaneous expression of the antigen which in the parental strains could only be induced to appear by the presence of the specific antiserum.Study of the 3 strains in axenic medium indicated the existence of a more complex system and the possibility that two or more immobilizing antigens may be present simultaneously.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. The establishment of Eimeria tenella sporozoites in the cecal mucosa of the chicken is described. The invasion process was similar to that reported for E. necatrix by Van Doorninck and Becker. Sporozoites were found to pass through the surface epithelium of the cecal mucosa into the lamina propria. Within the lamina propria the sporozoites were engulfed by macrophages and transported to the cells of the glands of Lieberkühn. Development of the sporozoites ensues within the gland epithelium.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. The morphology of the vegetative phase and the sexual process in Pandorina morum have been studied in detail under controlled laboratory conditions. A number of strains from various areas of the United States, all essentially indistinguishable on morphological grounds, were analyzed for sexual compatibility. Forty-seven heterothallic clones were found to represent 15 separate pairs of mating types, or a minimum of 15 syngens (sensu Sonneborn, 1957). Two clones proved to be homothallic. Nine additional clones, which were not observed to mate with any strain, can be classified only after further collecting. The separate heterothallic pairs of mating types are sexually isolated by factors acting at the stage of gamete production; incompatible mating types produce no gametes when they are mixed together. The geographical distribution of the sets of mating types is very incompletely defined as yet, but they are not strictly endemic forms. Thirty heterothallic strains, representing each of the 15 sexually isolated sets of mating types of Pandorina morum, have been deposited with the Culture Collection of Algae maintained at Indiana University, Bloomington, Indiana, U.S.A.
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    Topics: Biology
    Notes: SYNOPSIS. When grown in CPLM medium or in a similar medium containing glucose instead of maltose as its sugar, Tritrichomonas foetus, Strain O, was much more sensitive to injury when frozen to -21d̀ C. in the presence. of 1 m glycerol during the initial and logarithmic phases of its population growth curve than at its peak and for some time thereafter. In 7 experiments in which the population peak occurred an average of 28.1 hours after inoculation, the average culture age at which the protozoa first survived freezing was 20.3 hours, at which time the population had reached 52.6% of its peak. The optimum culture age for survival after 1 day of freezing averaged 37.7 hours at which time the population averaged 75.6% of its peak. The optimum culture age for survival after 7 to 15 days of freezing averaged 32.3 hours, at which time the population averaged 82.7% of its peak. Better survival upon freezing was obtained in those experiments in which the population peak was reached relatively rapidly.
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  • 76
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. Specimens of Blepharisma undulans were transferred from young clone cultures to a rotocompressor with 3 mm3 of culture medium. The organisms were slightly compressed and photographed at various intervals with dark field illumination. The sequence of macronuclear and cytoplasmic changes was compared with similarly followed Feulgen preparations.The cycle falls into several phases: (1) an interphase (12–24 hr.) in which the organism increases in size while cytoplasmic and macronuclear appearances remain unchanged. During this phase, the macronucleus consists of 3 to 5 nodes of various sizes connected by strands. (2) a pre-condensation phase (1 hr.) in which a new posterior peristome and cytopyge appear without visible macronuclear change. (3) a condensation phase (10–20 min.) in which the macronuclear nodes coalesce into a round mass without dissolution of the central nodes or strands. (4) a postcondensation phase (1 hr.) characterized by: (a) elongation of the condensed macronucleus into a rod-like shape followed by typical nodal formation; or (b) elongation of the condensed macronucleus into a form resembling the letter “J”, followed by nodal formation, and resulting in a double row of nodes in one daughter and a single row in the other. Separation occurs at this time, initiating the new interphase. The development of the j-form macronucleus. the lack of obliteration of the central nodes, and the characteristic interphase condition distinguish this strain of B. undulans from others described elsewhere.
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    The @journal of eukaryotic microbiology 6 (1959), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. Six species of astomatous Infusoria, 4 new, are described from the alimentary tract of Oligochaeta from Ochrida Lake. Two belong to Ochridanus, characterized by a cytoskeleton whose “V”-shaped basal piece bears on its branches two articulated hooks brought together by a skeletal blade. This genus found in Ochridanous Tubificidae represents the counterpart of Anthonyella in the Lumbriculidae of Lake Baïkal. The presence of Ochridanus in these worms concurs with the almost complete absence of representatives of Radiophrya of which we have found but one species. A species of Metaradiophrya, a genus unknown to date from the Lumbricidae, was noticed in Glossoscolecidae. The different species of Ochridanus, Anthonyella, Metaradiophrya, and Radiophrya compose a very homogeneous group of Radiophryinae. The study of the ciliary rows and the cytoskeleton of 2 species of Juxtaradiophrya, parasitic in the Lumbriculidae of Ochrida, shows that, in the morphology of these ciliates, as well as in the same forms from Lake Baïkal, many transition characteristics exist between the Radiophryinae and Hoplitophryinae or Mesnilellinae. These 3 sub-families, with their undeniable genetic kinship give coherence to the family Hoplitophryidae.
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    Topics: Biology
    Notes: SYNOPSIS. Histochemical techniques were used to demonstrate the intracellular distribution of some hydrases, hydrolases, oxidases, and dehydrogenases in Stylonychia pustulata. The hydrase, aconitase, was confined to the mitochondria. Zymohexase activity occurred in the cytoplasm and probably in the mitochondria. The hydrolases, acid and alkaline phosphatases, lipase, and urease, were localized in the mitochondria. Lactic and glutamic dehydrogenases were confined to the mitochondria. Peroxidase and glycerophosphate dehydrogenase were absent.
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    The @journal of eukaryotic microbiology 5 (1958), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. When two strains cf T. pyriformis that do not require exogenous pyridoxine are crossed, all progeny grow without the vitamin. Offspring from crosses of two pyridoxine requiring clones require pyridoxine with the exception of a few which will grow without pyridoxine. The ratio is approximately 3:1 favoring the pyridoxine requiring category. In matings involving the homozygous dominant pyridoxine requiring clones with the double recessive mutant, that is +/+ X p/p, all of the resulting progeny need pyridoxine. Test crossing these heterozygotes (+/p) with the parental pyridoxine non-requiring clones (p/p) gives offspring approximating a 1:1 ratio. Matings between two heterozygotes derived from breeding experiments also yield progeny in approximately 3 pyridoxine requiring: 1 pyridoxine non-requiring. All data indicate selection for the heterozygote in the population and a possible selection against either homozygote. The great abundance of heterozygotes and rarity of recessive homozygotes in natural habitats corroborates these findings. The genetic evidence supports a single gene hypothesis although the possibility of multiple closely linked genes cannot be ignored. There is also the possibility that a dominant suppressor gene may function in blocking the activity of the pyridoxine mutant genes. Moreover, if this gene exists it may be incompletely dominant since the heterozygote grows slightly on deficient media.
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    The @journal of eukaryotic microbiology 5 (1958), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. Trichodina urinicola was found in newts, Triturus cristatus and T. taeniatus, in three localities in Czechoslovakia. The ciliate populations showed important differences on the basis of which they were separated as three new forms of this species: T. urinicola f. typica, T. urinicola f. bohemica, both from Triturus cristatus, and T. urinicola f. taeniatus from Triturus taeniatus. The great variability of trichodinids is evident from the literature as well as from our own observations, so that these new forms are to be regarded as provisional ones until it is possible to decide on the basis of a large number of observations the extent of specificity and variation of individual endozoic species of Trichodina. A detailed description of these forms is given as well as a comparison with the known species of trichodinids inhabiting the urinary tract of amphibians. A brief comment on the present taxonomy of the Urceolaridae in general is outlined.The need for a uniform description of these ciliates is emphasized; in connection with this, the taxonomic value of individual body characters is discussed. Special attention is paid to the adhesive disk of Trichodina, the structure of which is of greatest importance in the taxonomy of this group. On the basis of Dogel's and Fauré-Fremiet's descriptive methods employed in study of trichodinids, a proposal of a uniform description of Trichodina is made which involves all the important features of these protozoa.
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    Notes: SYNOPSIS. Several substrains of Euglena gracilis var. bacillaris made chlorotic by treatment with pyribenzamine or streptomycin, or by growth at high temperature (35–36°C.), have been examined for their carotenoid content. They differ from the normal green strain both qualitatively and quantitatively. Some strains produce no detectable carotenoids while the carotenoid concentration in the strains producing most is at best only one-fifth that of the normal strain. In all substrains producing carotenoids, the carotene fraction consists of β-carotene accompanied by some members of the phytofluene series. In only two of these substrains, HB-G and PBZ-G3, are xanthophylls produced in significant amounts. In HB-G, the main pigment is echinenone, and in PBZ-G3 it is zeaxanthin. The significance of these findings is briefly discussed.
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    Notes: SYNOPSIS. Association of gamonts of Pyxinia crystalligera takes place in the midgut of its beetle host, Dermestes vulpinus. At 25°C. the development of gametocysts to the point of liberation of sporocysts is completed between about 15 hours and 27 hours after the gametocysts are deposited with fecal material. Dehiscence is favored by relative humidities of 0% to 90%, but is not favored by a relative humidity of 100%. During the early development of the gametocysts outside the host, the crystals and paraglycogen granules in the cytoplasm of the associated gamonts become concentrated in large masses. The gametes are formed at the periphery of the gamonts. After fusion of the gametes takes place and the sporoblasts begin to develop, the residual cytoplasm containing the inclusions moves outward to form a continuous layer next to the gametocyst envelope, so that the sporoblasts become crowded into a central core. A few hours before dehiscence is initiated a clear area appears on the upper side of the gametocyst. The contents of the gametocyst begin to shrink away from the envelope except in the region of the clear area. Eventually the sporocysts emerge through the clear area and press against the envelope of the gametocyst, causing formation of a conical papilla in the envelope. With continued pressure from the sporocysts, the papilla ruptures at its tip, and the sporocysts emerge in a continuous thread until dehiscence is completed. The thread of sporocysts may attain a length of about 11 mm.
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    Notes: SYNOPSIS. The steps leading to purine ring closure were examined in Strigomonas oncopelti. The flagellate has an obligate adenine requirement (hypoxanthine and guanine are inert) when grown without p-aminobenzoic acid. The imidazole counterpart of adenine but not the imidazole counterpart of hypoxanthine was active. A pathway for purine biosynthesis compatible with these results is sketched.
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    Notes: SYNOPSIS. The Nuttallia of the gerbil is transmitted by Rhipicephalus secundus only if the infected meal is taken by the larva, and the subsequent nymphal stage is the only one which is able to infect. There is no transovarial transmission.Infective trophozoites remain in the larval caeca for about 12 hours after gorging. The infective nymph is able to give rise to new infections at various times after it has been allowed to feed, but never later than the third day after disengagement from the host.
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    Topics: Biology
    Notes: SYNOPSIS. The process of autogamy in unassociated individuals of Paramecium polycaryum was reported by the author in 1954. In May, 1955, conjugation was first seen in this species in cultures collected by me at Annamalainagar, South India, thus removing it from the list of non-conjugating species. This appears to be the first instance in which the process of autogamy was detected prior to observation of conjugation in the same species. Autogamy occurs in singles of the Indian race and appears to be similar, cytologically, to that of American races. The details of the micronuclear behavior in conjugation parallel those of autogamy in singles. In fact, the conjugation process seems to be one of double autogamy (cytogamy), rather than of reciprocal gametic interchange. Paroral cones, often of fair size, are formed but breakdown of the cones to permit micronuclear passage has not been observed. In conjugation there are the usual three pregamic divisions; the first shows four characteristic crescents. The resulting nuclei may all participate in the second division. Fertilization occurs in the paroral cone area. Frequently, separation of the conjugants takes place immediately after the first division of the synkaryon. The old macronucleus undergoes very little change prior to the last postzygotic micronuclear division in the ex-conjugant, when it goes into a skein condition. Four macronuclear and four micronuclear anlagen are formed in the ex-conjugants at the completion of reorganization. On occasion giant individuals of P. polycaryum were observed to have ingested numbers of Tetrahymena pyriformis. The presence of an unidentified rod-like organism in the cytoplasm of the paramecia (non-conjugating) was detected in one collection from Bangalore, India.
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. The mating behavior of 16 stocks of Paramecium multimicronucleatum from 12 states has been studied. Mating always follows a decline in nutritive conditions. The evidence indicates that there exists one set of four interbreeding mating types. The period of subculture strongly influences the mating reactions, many stocks mating only long after isolation from nature and culture in the laboratory under the restricted conditions employed. Selfing was observed to occur in many races, usually after long periods of subculture. It first occurred in only a small proportion of the population, later in a larger proportion. The similarities and differences between P. multimicronucleatum and other species of protozoa showing multiple mating types are discussed.
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    Topics: Biology
    Notes: SUMMARY. A study of the temperature-pressure relationship in oxygen poisoning of Paramecium caudatum was undertaken, as the initial step in defining some of the major factors in in vivo oxygen poisoning. Paramecium was selected because it was relatively simple to culture in a pureline clone, large numbers were readily obtained, and it was large enough to be clearly visible under low magnification. The protozoa were exposed to oxygen pressures of 0 (100%), 15, 30, 45, 60, 75, 90, 105, 120 pounds/inch2 gauge pressure at each of the following temperatures: 1, 5, 10, 15, 20, and 27°C. Exposure was accomplished in a transparent, high-pressure lucite tank which permitted visual observation with aid of a dissecting microscope. It was found at temperatures above 5°C. that oxygen toxicity varied directly with pressure, but below this temperature, with oxygen tensions of 1–2 atmospheres (absolute), oxygen toxicity varied inversely as the temperature. The possibility is advanced that oxygen may be affecting two cellular processes (perhaps enzymatic), one of which is temperature-limited below 5°C. and would, therefore, decrease the death time as the temperature is decreased. Several experiments performed at 3°C. produced a death time intermediate between results obtained at 1° and 5°C.
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  • 88
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    Topics: Biology
    Notes: SUMMARY. A stock of Paramecium bursaria is described in which the peniculus contains only 8 columns of cilia and associated “granules”. The gullet system is composed of organelle complexes almost exclusively, and incorporates no underlying or transecting extensions of “pellicular fibrillar systems”. A brief discussion is presented on the value of the peniculus as a taxonomic criterion in separating “aurelia” and “bursaria” groups in Paramecium.
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  • 89
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  • 90
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    The @journal of eukaryotic microbiology 4 (1957), S. 0 
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    Topics: Biology
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  • 91
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Strains E, S and W of Tetrahymena pyriformis were examined for their ability to carry out the reactions of the Krebs-Henseleit urea cycle, using growth and enzyme studies. None of the strains was able to grow on either citruliine or ornithine in place of arginine, and proline was as active as citrulline or ornithine in sparing arginine. So little citrulline or arginine was synthesized by cell-free preparations as to be of no significance in the growth or nitrogen metabolism of the ciliates. Slight arginase activity could be detected in homogenates, but no urea was found in cultures. No urease activity could be detected using urea-C14.
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  • 92
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    The @journal of eukaryotic microbiology 4 (1957), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. An eimerian coccidian is described from the flying squirrel, Glaucomys volans, in Florida. It is identified as the same eimerian described by Roudabush from the flying squirrel in Iowa as Eimeria sciurorum. Evidence is presented that Roudabush incorrectly identified the organism. It is renamed as E. parasciurorum nov. sp. Mature oocysts have mean measurements of 29 × 16°, an index of 1.82, are cylindrical with rounded ends, have a dual membrane, and no extra residual body. Oocysts are without micropyle. Four egg-shaped, mature sporocysts in the oocyst have mean measurements of 11.2 × 6.2°, an index of 1.81, contain an oval, granular, intraresidual body and two pyriform sporozoites 10 × 3.2°, index 3.11.
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  • 93
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Two centrioles, an old one and a new one, are always present in the resting cell. From prophase onward two new ones and two old ones are present. Beginning with the resting stage, five types of centriole life cycles are described and compared with one another: In type 1, both centrioles are elongate; in type 2, the old one is long and the new one, which is short, elongates in prophase; in type 3, both are short, both elongate in prophase, and both, except for their anterior tips, degenerate in late telophase; in type 4, both are long but in prophase their distal ends become free of the rest of the centrioles, these ends migrate to center or posterior end of cell, where, after they produce the achromatic figure and it completes its function in nuclear division, they degenerate; in type 5, both are short and neither elongates at any stage of its life cycle.New centrioles are produced by the anterior ends of old ones. In their first generation, centrioles produce only extranuclear organelles (flagella, parabasals, axostyles, etc.); in their second and later generations, they produce only the achromatic figure (gametogenesis in Trichonympha and reorganization in Barbulanympha and Rhynchonympha are exceptions to this rule).The distal ends of centrioles in some types of cycles are surrounded by centrosomes; in others they are not. In one type of centriole life cycle a small central spindle is present in the resting cell in two genera; in the other types this is not the case.
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. The endogenous development of the life cycle of Eimeria alabamensis Christensen, 1941, occurs in the nucleus of the intestinal cells of cattle. Calves were killed at various intervals after inoculation with infective oöcysts to study the endogenous cycle. Excysted sporozoites were found in the contents or scrapings from the walls of rumen, omasum, small intestine, cecum, and colon. They were found in the cytoplasm of intestinal epithelium at 2 days. Schizonts were found in the nuclei beginning at 2 days, but the number was low by the 8th day. Merozoite numbers usually ranged between 16 and 32. Some host nuclei contained as many as 48 or more, but these appeared to be the result of more than one schizont merging in the same host nucleus. Merozoites were slender, spindle-shaped bodies while still in the schizont walls, but were short with bluntly rounded tips when found in intracellular spaces and crypts. Gametocytes were found as early as the 4th day. Most of the stages of gametogenesis were limited to the lowest third of the small intestine, but in heavy infections some were also found in the cecum and upper colon. Microgametocytes were multinucleate and were more densely stained than the uninucleate macrogametocytes. The ratio of macrogametocytes to microgametocytes in 100 gametes was 78: 22. Oöcysis with “shells” were found in sections of the lower 20 feet of the ileum on the 6th day, which coincided with the shortest prepatent period reported previously. As many as three schizonts or microgametocytes or four or five macrogametocytes or oöcysts could be found in the same host nucleus. The variations in shape of the oöcysts appeared to be dependent on the number of oöcysts crowded into each nucleus.
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    Topics: Biology
    Notes: SUMMARY. The role of centrioles in achromatic figure production is considered when the number present varies from 1–8. Each centriole after it becomes elongate produces astral rays from its distal end. Some of these rays remain free; some, by joining centromeres, become chromosomal fibers; and some, by joining and growing along those produced by one or more other centrioles, produce the central spindle portion of the achromatic figures. Thus, one centriole may function cooperatively with one to several others in the production of central spindles. But at least two centrioles must be present, and in the proper spacial relation to each other, to form a central spindle; one by itself can form only free astral rays, no central spindle or chromosomal fibers.The flagellated areas (to which the centrioles are anchored anteriorly) play an important role in determining the position of the distal ends of the centrioles with respect to one another, and the position of these ends, in turn, in a large measure, determines the types of achromatic figures produced, particularly the number of central spindles.
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  • 96
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Observations on binary fission of Lacrymaria olor show that it is a transverse fission. It involves probable intranuclear division of the micronucleus. Both micro- and macronucleus elongate in preliminary stages. Each is ultimately divided as cytoplasmic constriction cuts the spindle fibers of the former, and the connecting, nucleoplasmic thread of the latter.Surging movements of cytoplasm after fission elongate the daughter organisms and move new nuclei to normal, central sites. The anterior proboscis of the posterior daughter regenerates suddenly, complete with coronal cilia. Metachronal waves along ciliary meridians, strongly reversed on the posterior daughter, cause an oscillating movement which pulls the two apart, except for a slender, pellicular thread, ultimately severed. Until broken, this thread connects the rear tip of the anterior animal to the forward end of the proboscis of the posterior one. The organism is semi-quiescent, with proboscis retracted (except spasmodically) throughout fission. After fission the anterior animal quickly begins feeding movements and soon swims away. The posterior animal requires about half an hour before being able to begin feeding and swimming movements.The anterior contractile vacuole of the original animal becomes the primarily active vacuole of the anterior daughter; the posterior one that of the posterior daughter. Missing vacuoles are regenerated by the daughters in about one hour after fission. The division process requires about one hour for completion at 22.4°C.
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. The multiplication rate of Tetrahymena pyriformis HS in proteose peptone medium was measured at 12 temperatures between 18.4°C. and 36.6°C. At the temperature optimum, 32.5°C., the generation time is 2.25 hours. The upper lethal temperature lies between 36.6°C. and 38.0°C. Similarly, a study of Tetrahymena pyriformis GL revealed a temperature optimum for multiplication of 29°C. with a generation time of 3.70 hours. The upper lethal temperature falls between 34.6°C. and 35.4°C. At all temperatures employed the HS strain of organisms multiplies more rapidly than strain GL. Under identical conditions, the two strains have distinctly different growth optima, upper lethal temperatures and growth rates.As measured by multiplication rate the readjustment to a sudden change in temperature (from 18.4°C. to 27.7°C.) is completed very rapidly, with an effective lag time of about 1 hour. Such a shift in temperature gives rise to a small degree of division synchrony during the first and second population doublings which follow. Subsequently, all traces of division synchrony are lost.
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Test tube cultures of Tetrahymena pyriformis GL in the early maximum stationary phase of growth were used as inocula. After the elapse of a short lag phase a rapid transition to the logarithmic phase of growth was observed in cultures grown on peptone media(4,6). During the early phase of exponential multiplication more cells (as expressed on a percentual basis of the population number) were in the visible stage of cytoplasmic fission than after the elapse of 5 to 6 generations. Analysis of comprehensive data suggests that the higher division index in the early logarithmic phase of growth is not the expression of a synchronization of cells in metabolic respects but rather indicates a prolongation of the stage of cell fission during this phase.
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  • 99
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Ochromonas malhamensis (Pringsheim strain) can be grown above 35.5°C.; below 35°, the previous chemically defined medium supports dense growth. The B12 and thiamine requirements rise steeply with temperature, and growth promotion by folic acid emerges; folic acid spares the enhanced B12 requirement. B12 is spared also, perhaps wholly bypassed, by purines + pyrimidines + amino acids (below 35°, exogenous purines, pyrimidines, and folic acid have little effect). Requirements also emerge for glycine (spared by serine), valine and isoleucine (their ratio is critical; leucine and threonine assist in maintaining a good balance), and, at very slightly higher temperatures, phenylalanine, tryptophan, cystine, and lysine. Requirements for Mg, Fe, Zn, and Mn appear to rise steeply with temperature; metal toxicities have to be circumvented carefully. The proportion of histidine + arginine to carbohydrate has to be increased, and a Krebs-cycle component such as succinic acid becomes stimulatory. At 36.3–36.7°, a further supplement of crude natural materials such as an autoclaved suspension of Ochromonas cells is needed. Relevance of these findings to fever stress in vertebrates, general mitochondrial function, and repair of radiation damage, is discussed.
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    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. According to Kahl the trichostome genus Trichopelma may be considered to include five species: T. sphagnetanim, T. eurystoma, T. euglenivora, T. opaca, and T. torpens. A sixth species is added in the present account. The following constant characteristics distinguish it from the five earlier described ones: total lack of trichocysts; differences in the morphology of the body surfaces; dissimilarity of the upper and lower surfaces in shape (one plane, the other convex), in ciliation, and in number of cuticular furrows; unique location of the contractile vacuole.
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