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  • Forschungsdaten  (683)
  • PANGAEA  (683)
  • Springer Science + Business Media
  • 1970-1974  (683)
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  • PANGAEA  (683)
  • Springer Science + Business Media
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  • 1
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Vinogradov, Mikhail E (1973): New data on the quantitative distribution of plankton in the deep layers of the Sea of Japan. Oceanology, 13, 904-907
    Publikationsdatum: 2023-07-10
    Beschreibung: Vertical distribution of zooplankton biomass from the surface to bottom layers (3400 m) is examined. Material was collected layer by layer by a BR 113/140 net at 41°59' N and 133°37' E on July 2 and 3, 1970. Quantity of plankton below 1000 m was found to be much less than at corresponding depths in the adjacent regions of the ocean. This impoverishment is due to absence of oceanic bathypelagic animals in deep layers of the Sea of Japan. Absence of specialized predators (plankton-feeders) deep in the Sea of Japan results in underconsumption of interzonal animals that sink to great depths. Upon dying they should reach the floor in larger quantities than in the ocean.
    Schlagwort(e): Amphipoda, biomass; Archive of Ocean Data; ARCOD; Chaetognatha, biomass; Copepoda, biomass; Depth, bottom/max; Depth, top/min; DEPTH, water; Euphausiacea, biomass; Mysidacea, biomass; North Pacific; Ostracoda, biomass; PLA; Plankton net; VITYAZ; Vityaz (ex-Mars); VITYAZ6674; Zooplankton, biomass
    Materialart: Dataset
    Format: text/tab-separated-values, 129 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Simonsen, R (1974): The Diatom Plankton of the Indian Ocean Expedition of RV "Meteor" 1964 - 1965. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D19, 1-107
    Publikationsdatum: 2023-07-09
    Beschreibung: During the Indian Ocean Expedition of R/V METEOR phytoplankton samples were taken with a multiple closing net (Multinet) at 103 stations. In this material the diatoms were investigated. In all 247 taxa could be identified which belong to 242 species and 5 varieties of formae of 80 genera. Of these 1 variety, 15 pecies, and 3 genera are newly described. New combinations were made for 18 species, and a number of old combinations was reinstated.
    Schlagwort(e): Abundance estimate; Actinocyclus curvatulus; Actinocyclus elongatus; Actinocyclus octonarius; Actinocyclus subtilis; Actinoptychus annulatus; Actinoptychus senarius; Actinoptychus splendens; Amphiprora alata; Amphiprora sulcata; Amphora angusta; Amphora bigibba; Amphora crassa; Amphora decussata; Amphora graffeana; Amphora granulata; Amphora robusta; Amphora spectabilis; Amphora wisei; Area/locality; Asterionella glacialis; Asterionella notata; Asterolampra grevillei; Asterolampra marylandica; Asteromphalus arachne; Asteromphalus elegans; Asteromphalus flabellatus; Asteromphalus heptactis; Asteromphalus imbricatus; Asteromphalus ingens; Asteromphalus petterssonii; Asteromphalus roperianus; Asteromphalus sarcophagus; Auricula insecta; Bacillaria paradoxa; Bacteriastrum furcatum; Bacteriastrum furcatum-hispida; Biddulphia pulchella; Biddulphia tuomeyi; Caloneis elongata; Cerataulina bergonii; Cerataulus smithii; Chaetoceros atlanticus; Chaetoceros bacteriastroides; Chaetoceros buceros; Chaetoceros coarctatus; Chaetoceros compressus; Chaetoceros curvisetus; Chaetoceros decipiens; Chaetoceros denticulatus; Chaetoceros didymus; Chaetoceros diversus; Chaetoceros lorenzianus; Chaetoceros messanensis; Chaetoceros peruvianus; Chaetoceros radicans; Chaetoceros rostratus; Chaetoceros seychellarum; Chaetoceros sumatranus; Chaetoceros tetratichon; Climacodium frauenfeldianum; Cocconeis dirupta; Cocconeis dirupta-flexella; Cocconeis distans; Cocconeis placentula; Cocconeis scutellum; Corethron criophilum; Coscinodiscus africanus; Coscinodiscus asteromphalus; Coscinodiscus centralis; Coscinodiscus concinniformis; Coscinodiscus concinnoides; Coscinodiscus crenulatus; Coscinodiscus gigas; Coscinodiscus granii; Coscinodiscus jonesianus; Coscinodiscus lineatus; Coscinodiscus nodulifer; Coscinodiscus oculus-iridis; Coscinodiscus perforatus; Coscinodiscus plicatoides; Coscinodiscus radiatus; Coscinodiscus reniformis; Coscinodiscus stellaris; Coscinodiscus thorii; CT; Cyclotella striata; Cyclotella stylorum; Cymatonitzschia marina; Cymatotheka weissflogii; Dactyliosolen mediterraneus; DEPTH, water; Detonula pumila; Diploneis bomboides; Diploneis didyma; Diploneis papula; Diploneis smithii; Ditylum sol; Ethmodiscus gazellae; Ethmodiscus rex; Ethmodiscus spp. fragments; Eucampia cornuta; Eucampia zodiacus; Fragilaria intermedia; Glyphodesmis rhombica; Gomphonema pseudexiguum; Gossleriella tropica; Grammatophora marina; Guinardia flaccida; Hantzschia amphioxys; Haslea gigantea; Haslea gretharum; Haslea hyalinissima; Haslea wawrikae; Hemiaulus hauckii; Hemiaulus membranaceus; Hemiaulus sinensis; Hemidiscus cuneiformis; Hemidiscus kanayanus; IIOE - International Indian Ocean Expedition; Indian Ocean; Lauderia annulata; Licmophora communis; Licmophora flabellata; M1; M1-track; Mastogloia minuta; Mastogloia rostrata; Mastogloia woodiana; Melosira granulata; Meteor (1964); Navicula abrupta; Navicula comoides; Navicula crucifera; Navicula directa; Navicula distantepunctata; Navicula durandii; Navicula humerosa; Navicula lorenzii; Navicula mutica; Navicula mutica forma cohnii; Navicula nivalis; Navicula protracta; Navicula salinarum; Nitzschia aequatorialis; Nitzschia bicapitata; Nitzschia braarudii; Nitzschia capuluspalae; Nitzschia closterium; Nitzschia constricta; Nitzschia cuspidata; Nitzschia dietrichii; Nitzschia distans; Nitzschia heimii; Nitzschia hybrida; Nitzschia inflatula; Nitzschia inflatula-capitata; Nitzschia interruptestriata; Nitzschia kolaczeckii; Nitzschia lineola; Nitzschia longa; Nitzschia longicollum; Nitzschia longissima; Nitzschia lorenziana; Nitzschia marina; Nitzschia maxima; Nitzschia ossiformis; Nitzschia panduriformis; Nitzschia pungens; Nitzschia pungiformis; Nitzschia sicula; Nitzschia sigma; Nitzschia sigmaformis; Nitzschia socialis; Nitzschia subfraudulenta; Nitzschia subpacifica; Number; Odontella aurita; Odontella mobiliensis; Odontella regia; Odontella rhombus; Odontella sinensis; Oestrupia musca; Pachyneis gerlachii; Palmeria hardmaniana; Paralia sulcata; Pinnularia borealis; Pinnularia cuneatoundulata; Plagiogramma staurophorum; Planktoniella sol; Pleurosigma directum; Pleurosigma indicum; Pleurosigma naviculaceum; Pleurosigma planctonicum; Podocystis spathulata; Podosira stelliger; Porosira denticulata; Protoraphis hustedtiana; Pseudoeunotia doliolus; Pseudohimantidium pacificum; Pseudotriceratium punctatum; Rhabdonema adriaticum; Rhaphoneis amphiceros; Rhaphoneis surirella; Rhaphoneis surirelloides; Rhizosolenia alata; Rhizosolenia alata-indica; Rhizosolenia bergonii; Rhizosolenia calcar-avis; Rhizosolenia castracanei; Rhizosolenia cochlea; Rhizosolenia cylindrus; Rhizosolenia hebetata; Rhizosolenia imbricata; Rhizosolenia robusta; Rhizosolenia setigera; Rhizosolenia styliformis; Roperia tesselata; Sample code/label; Skeletonema costatum; Stauroneis amphioxys; Stauroneis membranacea; Stephanopyxis palmeriana; Stephanopyxis turris; Stictodiscus californicus; Surirella fastuosa; Synedra hennedyana; Synedra indica; Thalassionema bacillaris; Thalassionema nitzschioides; Thalassiosira diporocyclus; Thalassiosira eccentrica; Thalassiosira lineata; Thalassiosira minuscula; Thalassiosira oestrupii; Thalassiosira punctigera; Thalassiosira spinosa; Thalassiosira subtilis; Thalassiosira symmetrica; Thalassiothrix delicatula; Thalassiothrix frauenfeldii; Thalassiothrix longissima; Thalassiothrix mediterranea; Thalassiothrix vanhoeffenii; Trachyneis antillarum; Trachyneis aspera; Trachyneis debyi; Triceratium broeckii; Triceratium dubium; Triceratium favus; Triceratium pentacrinus; Triceratium robertsianum; Trigonium alternans; Trigonium reticulum; Tropidoneis maxima; Tropidoneis sp.; Tropidoneis subulata; Underway cruise track measurements
    Materialart: Dataset
    Format: text/tab-separated-values, 1337 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Counting 〉400 µm fraction; Date/Time of event; DEPTH, water; Euphausia brevis; Euphausia hemigibba; Event label; HAI; Josephine Seamount; Latitude of event; Longitude of event; M9; M9c_NET023; M9c_NET026; M9c_NET027; M9c_NET030; M9c_NET031; Meganyctiphanes norvegica; Meteor (1964); Nematoscelis megalops; Stylocheiron carinatum; Stylocheiron longicorne; Stylocheiron suhmii; Thysanoessa gregaria; Thysanopoda subaequalis; Towed zooplankton net
    Materialart: Dataset
    Format: text/tab-separated-values, 45 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Cape Blanc/Meteor Bank/Portugal; Counting 〉400 µm fraction; Date/Time of event; DEPTH, water; Euphausia brevis; Euphausia hemigibba; Euphausia mutica; Event label; HAI; Latitude of event; Longitude of event; M9; M9a_NET003; M9a_NET005; M9a_NET006; M9a_NET007; M9a_NET010; M9a_NET014; M9a_NET016; M9a_NET019; M9a_NET023; M9a_NET025; M9a_NET026; M9a_NET027; M9c_NET053; M9c_NET055; M9c_NET057; M9c_NET062; M9c_NET063; M9c_NET071; M9c_NET078; M9c_NET079; Meteor (1964); Nematobrachion flexipes; Nematoscelis megalops; Stylocheiron abbreviatum; Stylocheiron affine; Stylocheiron carinatum; Stylocheiron longicorne; Stylocheiron suhmii; Thysanoessa gregaria; Thysanopoda obtusifrons; Thysanopoda subaequalis; Towed zooplankton net
    Materialart: Dataset
    Format: text/tab-separated-values, 260 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Calculated after Simpson-Index; Cape Blanc/Meteor Bank/Portugal; Counting 〉500 µm fraction; DEPTH, water; Diversity; Euphausia brevis; Euphausiacea, larvae; Euphausia hemigibba; Euphausia mutica; Euphausia sp.; Event label; Latitude of event; Longitude of event; M19; M19_NET001; M19_NET004; M19_NET005; M19_NET008; M19_NET009; M19_NET010; M19_NET011; M19_NET012; M19_NET013; M19_NET016; M19_NET026; M19_NET027; M19_NET028; M19_NET030; M19_NET037; M19_NET041; M19_NET042; M19_NET043; M19_NET044; M19_NET046; M19_NET047; M19_NET048; M19_NET049; M19_NET050; Meteor (1964); Nematobrachion flexipes; Nematobrachion sexspinosus; Nematoscelis atlantica; Nematoscelis megalops; Nematoscelis sp.; Nematoscelis tenella; Ring trawl; Rossbreiten-Expedition 1970; RTR; Stylocheiron abbreviatum; Stylocheiron carinatum; Stylocheiron elongatum; Stylocheiron longicorne; Stylocheiron sp.; Stylocheiron suhmii; Thysanoessa sp.; Thysanopoda obtusifrons; Thysanopoda subaequalis; Thysanopoda tricuspidata
    Materialart: Dataset
    Format: text/tab-separated-values, 575 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; DEPTH, water; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Larvae net; LN; M9; M9_C; Meteor (1964); Northeast Atlantic; Number; Pterosagitta draco; Sagitta decipiens; Sagitta enflata; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta planctonis; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 108 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Depth, bottom/max; Depth, top/min; DEPTH, water; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Larvae net; LN; M9; M9_A; Meteor (1964); Northeast Atlantic; Pterosagitta draco; Sagitta decipiens; Sagitta enflata; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta planctonis; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 78 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Unbekannt
    PANGAEA
    In:  Supplement to: Weigmann, Renate (1970): Zur Ökologie und Ernährungsbiologie der Euphausiaceen (Crustacea) im Arabischen Meer. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D5, 11-52
    Publikationsdatum: 2023-07-09
    Beschreibung: In the present paper, the ecology and feeding habits of euphausiids are described. The samples were taken at the time of the NE-monsoon (1964/65) by R. V. "Meteor" in the Arabian Sea and adjacent waters. 24 species were determined. According to distribution of the species, the following marine areas can be distinguished: Arabian Sea: 24 species, dominant are Euphausia diomedeae, E. tenera, E. distinguenda, Stylocheiron carinatum. Gulf of Aden: 10 species, dominant are Euphausia diomedeae, E. distinguenda. Red Sea: 6 species, dominant are Euphausia diomedeae, E. distinguenda. Gulf of Oman : 5 Species, dominant are Euphausia distinguenda, Pseudeupbaufia latifrons. Persian Gulf: 1 species - Pseudeuphausia latifrons. The total number of euphausiids indicate the biomass of this group. High densities of euphausiids (200-299 and 〉 300 individuals/100 m**3) occur in the innermost part of the Gulf cf Aden, in the area south of the equator near the African east coast, near Karachi (Indian west coast) and in the Persian Gulf. Comparison with data relating to production biology confirms that these are eutrophic zones which coincide with areas in which upwelling occurs at the time of the NE-monsoon. The central part of the Arabian Sea differs from adjacent waters by virtue of less dense euphausiid populations (〉 199 individuals/100 m**3). Measurements relating to production biology demonstrate a relatively low concentration of primary food sources. Food material was ascertained by analysis of stomach content. The following omnivorous species were examined: Euphausia diomedeae, E. distinguenda, E. tenera, Pseudeuphausia latifrons and Thysanopoda tricuspidata. Apart from crustacean remains large numbers of Foraminifera, Radiolaria, tintinnids, dinoflagellates were found in the stomachs. Quantitatively crustaceans form the most important item in the diet. Food selection on the basis of size and form appears to be restricted to certain genera of tintinnids. The genera Stylocheiron and Nematoscelis are predators. Only crustacean remains were found in the stomachs of Stylocheiron abbreviatum, whereas Radiolaria, Foraminifera and tintinnids occurred to some extent in Nematasceli sp. Different euphausiids in the food chain in the Arabian Sea. In omnivorous species the position is variable, since they not only feed by filtering autotrophic and heterotrophic Protista, but also by predation on zooplankton. Carnivorous species without filtering apparatus feed exclusively on zooplankton of the size of copepods. Only these species are well established as occupying a higher position in the food chain. The parasitic protozoan Tbalassomyces fagei was found on Euphausia diomedeae, E. fenera, E. distinguenda and E. sanzoi.
    Schlagwort(e): Arabian Sea; DEPTH, water; Eastern Arabian Sea; Euphauaia diomedeae; Euphausia brevis; Euphausiacea; Euphausia distinguenda; Euphausia mutica; Euphausia paragibba; Euphausia pseudogibba; Euphausia sanzoi; Euphausia similis; Euphausia tenera; Event label; Golf of Aden, Arabian Sea; Gulf of Oman; IIOE - International Indian Ocean Expedition; Indian Ocean Standard Net; IOSN; Latitude of event; Longitude of event; M1; M1_042; M1_049; M1_052; M1_062; M1_066; M1_071; M1_073; M1_077; M1_093; M1_094; M1_101; M1_104; M1_106; M1_109; M1_113; M1_114; M1_115; M1_124; M1_126; M1_129; M1_132; M1_134; M1_135; M1_136; M1_137; M1_139; M1_141; M1_145; M1_146; M1_147; M1_149; M1_150; M1_151; M1_153; M1_157; M1_158; M1_167; M1_173; M1_175; M1_180; M1_181; M1_182; M1_183; M1_184; M1_186; M1_194; M1_195; M1_197; M1_199; M1_200; M1_205; M1_209; M1_210; M1_214; M1_218; M1_220; M1_222; M1_225; M1_233; M1_234; M1_235; M1_236; M1_238; M1_239; M1_243; M1_244; M1_245; M1_247; M1_248; M1_253; M1_275; M1_277; M1_293; M1_294; M1_373; M1_379; M1_380; M1_381; M1_NET042; M1_NET049; M1_NET052; M1_NET062; M1_NET066; M1_NET071; M1_NET073; M1_NET077; M1_NET093; M1_NET094; M1_NET101; M1_NET104; M1_NET106; M1_NET109; M1_NET113; M1_NET114; M1_NET115; M1_NET124; M1_NET126; M1_NET129; M1_NET132; M1_NET134; M1_NET135; M1_NET136; M1_NET137; M1_NET139; M1_NET141; M1_NET145; M1_NET146; M1_NET147; M1_NET149; M1_NET150; M1_NET151; M1_NET153; M1_NET157; M1_NET158; M1_NET167; M1_NET173; M1_NET175; M1_NET180; M1_NET181; M1_NET182; M1_NET183; M1_NET184; M1_NET186; M1_NET194; M1_NET195; M1_NET197; M1_NET199; M1_NET200; M1_NET205; M1_NET209; M1_NET210; M1_NET214; M1_NET218; M1_NET220; M1_NET222; M1_NET225; M1_NET233; M1_NET234; M1_NET235; M1_NET236; M1_NET238; M1_NET239; M1_NET243; M1_NET244; M1_NET245; M1_NET247; M1_NET248; M1_NET253; M1_NET275; M1_NET277; M1_NET293; M1_NET294; M1_NET373; M1_NET379; M1_NET380; M1_NET381; Meteor (1964); Nematobrachion flexipes; Nematoscelis sp.; Nematoscelis tenella; Northern Arabian Sea; Number of species; Persian Gulf; Pseudeuphausia latifrons; Red Sea; Stylocheiron abbreviatum; Stylocheiron affine; Stylocheiron carinatum; Stylocheiron longicorne; Stylocheiron microphthalma; Stylocheiron suhmii; Thysanopoda aequalis; Thysanopoda monacantha; Thysanopoda obtusifrons; Thysanopoda tricuspidata; Western Arabian Sea
    Materialart: Dataset
    Format: text/tab-separated-values, 2440 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Hesthagen, Ivar H (1970): On the near-bottom plankton and benthic invertebrate fauna of the Josephine Seamount and the Great Meteor Seamount. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D8, 61-70
    Publikationsdatum: 2023-07-09
    Beschreibung: 15 samples obtained with Beyer's epibenthic closing net were studied quantitatively. The numbers of epi- and endobenthic animals were found to be correlated with the volume of sediment in the samples. Among the planktonic components, calanoid copepodes were strongly predominant. In the samples obtained on the Great Meteor Seamount, very much larger numbers of these animals were caught in the daytime than at night. Possible explanations for this difference are suggested.
    Schlagwort(e): Amphipoda; Anthozoa, larvae; Appendicularia; Ascidiacea; Asteroidea; Atlantische Kuppenfahrten 1967/4-7; Bivalvia; Bryozoa; Cape Blanc/Meteor Bank/Portugal; Cephalopoda; Chaetognatha; Cirripedia; Copepoda; Counting 〉500 µm fraction; Crinoidea; Cumacea; Decapoda; Decapoda, larvae; DEPTH, sediment/rock; EBS; Echinoidea; Echiurida; Elevation of event; Epibenthic sledge; Euphausiacea; Event label; Gastropoda; Hydrozoa; IFM-GEOMAR; Josephine Seamount; Latitude of event; Leibniz-Institut für Meereswissenschaften, Kiel; Longitude of event; M9; M9_BSN007; M9_BSN008; M9_BSN009; M9_BSN010; M9_BSN012; M9_BSN013; M9_BSN014; M9_BSN015; M9_BSN018; M9_BSN019; M9_BSN020; M9_BSN021; M9_BSN022; M9_BSN023; M9_BSN024; Meteor (1964); Mysidacea; Nematoda; Ophiuroidea; Ostracoda; Pisces; Polychaeta; Porifera; Pycnogonida; Sample comment; Sample volume; Scyphozoa; Seriocarpa rhizoides; Sipunculida; Solenogastres; Thaliacea
    Materialart: Dataset
    Format: text/tab-separated-values, 600 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Depth, bottom/max; Depth, top/min; DEPTH, water; Eukrohnia bathypelagica; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Krohnitta subtilis; Larvae net; LN; M9; M9_C; Meteor (1964); Northeast Atlantic; Pterosagitta draco; Sagitta bipunctata; Sagitta decipiens; Sagitta enflata; Sagitta friderici; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta minima; Sagitta planctonis; Sagitta scrippsae; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 38 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 11
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Depth, bottom/max; Depth, top/min; DEPTH, water; Eukrohnia bathypelagica; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Krohnitta subtilis; Larvae net; LN; M9; M9_A; Meteor (1964); Northeast Atlantic; Pterosagitta draco; Sagitta bipunctata; Sagitta decipiens; Sagitta enflata; Sagitta friderici; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta minima; Sagitta planctonis; Sagitta scrippsae; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 38 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 12
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; Depth, bottom/max; Depth, top/min; DEPTH, water; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Larvae net; LN; M9; M9_C; Meteor (1964); Northeast Atlantic; Pterosagitta draco; Sagitta decipiens; Sagitta enflata; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta planctonis; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 78 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 13
    Publikationsdatum: 2023-07-09
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; DEPTH, water; Eukrohnia fowleri; Eukrohnia hamata; Krohnitta pacifica; Larvae net; LN; M9; M9_A; Meteor (1964); Northeast Atlantic; Number; Pterosagitta draco; Sagitta decipiens; Sagitta enflata; Sagitta hexaptera; Sagitta lyra; Sagitta marcocephala; Sagitta planctonis; Sagitta serratodentata
    Materialart: Dataset
    Format: text/tab-separated-values, 180 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 14
    Publikationsdatum: 2023-07-07
    Schlagwort(e): Actinolite; Aegirine; Allanite; Anatase; Apatite; Augite; Biotite; Biotite, light; Biotite and green micas; Brookite; Chlorite; Chloritoid; Chromite; Clinopyroxene; Clinozoisite; DEPTH, sediment/rock; Diopside; Epidote; Garnet; Glaucophane; Hornblende, brown; Hornblende, green; Indeterminata; Kyanite; LATITUDE; LONGITUDE; Minerals, altered; Monazite; Muscovite; Olivine; Opaque minerals; Orthopyroxene; Rutile; Sample code/label; Size fraction 3.0-3.5 phi; Sphene; Spinel; Staurolite; Tourmaline; Tremolite; Vesuvianite; Xenotime; Zircon; Zoisite
    Materialart: Dataset
    Format: text/tab-separated-values, 751 data points
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  • 15
    Publikationsdatum: 2023-07-10
    Schlagwort(e): ADEPDCruises; Archiannelida; Counting 44-500 µm fraction; Cumacea; DEPTH, sediment/rock; Echiurida; Elevation of event; Event label; Foraminifera; Gastrotricha; GC; Gnathostomulida; Gravity corer; Halicaridae; Harpacticoidea; Hydrozoa; Kinorhyncha; Lamellibranchiata; Latitude of event; LB#1; LB#2; LB#3; LB#4; LC#1; LC#2; Longitude of event; LSL#1; LSL#2; LSL#3; LSL#4; Meiofauna, metazoa per volume; Nauplii; NE-America, Hatteras Abyssal Plain; Nematoda; Nemertea; Ostracoda; Polychaeta; Rotifera; Tardigrada; Turbellaria
    Materialart: Dataset
    Format: text/tab-separated-values, 200 data points
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  • 16
    facet.materialart.
    Unbekannt
    PANGAEA
    Publikationsdatum: 2023-07-10
    Schlagwort(e): ADEPDCruises; Archiannelida; Counting 44-500 µm fraction; DEPTH, sediment/rock; Elevation of event; Event label; FB#1; FB#2; FB#3; FC#1; FC#2; Foraminifera; FSL#1; FSL#2; FSL#3; FSL#4; FSL#5; FSL#6; Gastrotricha; GC; Gravity corer; Halicaridae; Harpacticoidea; Hydrozoa; Kinorhyncha; Lamellibranchiata; Latitude of event; Longitude of event; Meiofauna, metazoa per volume; Nauplii; NE-America, Hatteras Abyssal Plain; Nematoda; Nemertea; Ostracoda; Polychaeta; Rotifera; Tardigrada; Turbellaria
    Materialart: Dataset
    Format: text/tab-separated-values, 187 data points
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  • 17
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Amyclina facki; Anadara diluvii; Antalis sp.; Aquilofusus festivus; Area/locality; Astarte goldfussi goldfussi; Astarte gracilis convexior; Babylonella fusiformis; Bittium spina; Boreodrillia hosiusi; Chrysallida pygmaea; Conolithus dujardini; Crassispira borealis; Cyclocardia chamaeformis; Cylichna cylindracea; Dentalium dollfussi; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation 2; Euspira helicina; Ficus conditus; Fusiturris flexiplicata; Gemmula boreoturricula; Gemmula denticula borealis; Gemmula stoffelsi; Gemmula zimmermanni; Glycymeris lunulata baldii; Gouldia minima; Hinia (Telasco) bocholtensis; Laevastarte angulata; LATITUDE; Lauenburg1972; Limopsis aurita; LONGITUDE; Lyrotyphis sejunctus priscus; Meiocardia harpa; Neoguraleus tenella; Nicania radiata; Nucula nucleus; Ocinebrina imbricata; Parvicardium straeleni; Pectunculina lamellata; Pterynotus (Alipurpura) nysti; Ringiculina buccinea; Saccella westendorpi; Sample ID; Schleswig-Holstein, Germany; Spiratella valvatina; Streptodictyon abruptus; Streptolathyrus contiguus; Sveltia varicosa; Turritella subangulata; Varicorbula gibba; Venus multilamella; Xenophora deshayesi; Yoldia glaberrima; Yoldiella pygmaea
    Materialart: Dataset
    Format: text/tab-separated-values, 2120 data points
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  • 18
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Abra bosqueti; Abra cf. bojei; Acamptogenotia escheri; Acamptogenotia morreni; Acanthocardia sp.; Actaeon semistriatus; Amusium sp.; Amyclina facki; Anadara diluvii; Ancilla (Baryspira) karsteni; Ancilla obsoleta; Anomia cf. asperella; Aporrhais speciosa; Aquilofusus guerichi; Aquilofusus waeli; Architectonica dumonti; Arctica islandica; Area/locality; Astarte (Digitaria) koeneni; Astarte (Digitariopsis) propinqua; Astarte (Goodallia) laevigata; Astarte (Laevastarte) angulata; Astarte goldfussi praecursor; Astarte gracilis gracilis; Astarte pygmaea; Asthenotoma festiva; Asthenotoma obliquinodosa; Atrina pectinata; Babylonella fusiformis; Bathyarca pectunculoides; Bathytoma crenata; Bathytoma jugleri; Bittium spina; Bonellitia evulsa postera; Brachytoma obtusangula; Brachytoma pannoides; Brocchinia mitraeformis parvula; Callista beyrichi xesta; Calyptraea chinensis; Cavilucina (Gonimyrtea) droueti schloenbachi; Ceratocyathus granulatus; Cerithella bitorquata; Circulus carinatus; Conolithus dujardini; Conuber submamillaris; Costoanachis guembeli; Crassispira borealis; Cuspidaria clava; Cyclocardia orbicularis tuberculata; Cylichna cylindracea; Cylichnina elongata; Cylindrophyllia duncani; Cyrtodaria angusta; Dacrydium pygmaeum; Dentalium holsaticum aff. acutum; Dentalium kickxi; Dentalium novemcostatum mutabile; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dosinia basteroti; Ecphora wiechmanni; Elaeocyma sp.; Elevation 2; Ensis cf. ensis; Eulimella neumayri; Euspira helicina; Ficus concinnus; Ficus conditus; Fusiturris aquensis; Fusiturris duchasteli; Fusiturris flexiplicata; Gemmula boreoturricula; Gemmula cf. bosqueti; Gemmula coronata; Gemmula denticula borealis; Gemmula laticlavia; Gemmula zimmermanni; Genota ramosa; Glycymeris lunulata; Habecardium subturgidum; Hastula beyrichi; Haustator goettentrupensis; Hemiacirsa cf. leunisii; Hemiacirsa lanceolata; Hiatella arctica; Hinia (Telasco) schlotheimi; Hinia (Uzita) serraticosta; Kleinella (Leucolina) nordmanni; Lamellinucula comta; LATITUDE; Lauenburg1972; Limarca retifera; Limopsis aurita; Liomesus rarus; LONGITUDE; Lucinoma borealis; Lyrotyphis sejunctus; Melanella (Polygureulina) glabella; Mitrella (Macrurella) nassoides; Modiolula phaseolina; Mormula amoena; Murex (Haustellum) inornatum globosum; Murex inornatus; Myurellina acuminata; Nassarius (Phrontis) poelsensis; Neoguraleus holzapfeli; Neoguraleus roemeri; Neoguraleus tenella; Nuculana (Saccella) westendorpi; Nucula nucleus; Nuculoma haesendoncki hanseata; Nuculoma laevigata peregrina; Odostomia conoidea; Oliva (Strephona) dufresnei; Ostrea sp.; Pagodula semperi angustevaricata; Panope angusta inflata; Parvicardium kochi; Pecten (Hilberia) hofmanni; Peronaea benedeni fallax; Peronaea benedeni nysti; Phos decussatus; Pitar rudis cimbrica; Pleurotomoides luisae; Poromya hanleyana; Pyramidella plicosa; Pyrgolampros pseudoterebralis; Pyrgolampros undulata; Ringiculina buccinea; Riuzorus acuminatus; Roxania subutriculus; Sample ID; Sassia flandrica enodis; Scaphander grateloupi; Scaphella siemsseni; Schleswig-Holstein, Germany; Semicassis bicoronata; Sigatica hantoniensis; Sinodia westendorpi; Sinum philippii; Solariella bernaysi; Solenocurtus basteroti; Species present; Spisula trinacria; Stephanophyllia nysti; Streptodictyon elongatus; Streptodictyon gottschei; Streptodictyon sexcostatus; Strioterebrum basteroti; Strioterebrum hoernesi; Surcula regularis; Sveltia varicosa; Syrnola hoernesi; Syrnola subulata; Teinostoma (Solariorbis) antwerpiense; Thracia speyeri; Trophon deshayesi capito; Trophon octonarius; Turbonilla acuticosta; Turricula steinvorthi; Turriscala pusilla; Typhis pungens; Uromitra acicula; Varicorbula gibba; Ventrilia acutangula; Venus multilamella; Xenophora deshayesi; Yoldia glaberrima; Yoldiella pygmaea; Zygochlamys ambigna; Zygochlamys cf. decussata; Zygochlamys semistriata
    Materialart: Dataset
    Format: text/tab-separated-values, 30921 data points
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  • 19
    facet.materialart.
    Unbekannt
    PANGAEA
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Alismataceae; Carex subgen. Eucarex; Carex subgen. Vignea; Compositae; Counting, palynology; Cyperaceae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Illinois, United States of America; Larix; Livingstone piston sampler; LPS; Lycopus; Lysimachia; Niantic; Picea; Picea, cones; Typha; Viola
    Materialart: Dataset
    Format: text/tab-separated-values, 154 data points
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  • 20
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Calculated; Cephalopoda; Cephalopoda, mass; Decapoda; Decapoda, mass; DEPTH, water; Euphausiacea; Euphausiacea, mass; Fish larvae; Fish larvae, mass; Hyperiidae, mass; Hyperiidea; Macroplankton; Macroplankton, mass; Macroplankton, wet weighted; Myctophidae; Myctophidae, mass; Mysidacea; Mysidacea, mass; Pteropoda; Pteropoda, mass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6469; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 162 data points
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  • 21
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Decapoda, biomass; DEPTH, water; Euphausiacea, biomass; Fishes, biomass; Invertebrata, biomass; Macroplankton, biomass; Myctophidae, biomass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6469; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 22
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Calculated; Cephalopoda; Cephalopoda, mass; Decapoda; Decapoda, mass; DEPTH, water; Euphausiacea; Euphausiacea, mass; Fish larvae; Fish larvae, mass; Hyperiidae, mass; Hyperiidea; Macroplankton; Macroplankton, mass; Macroplankton, wet weighted; Myctophidae; Myctophidae, mass; Mysidacea; Mysidacea, mass; Pteropoda; Pteropoda, mass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6490; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 162 data points
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  • 23
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Decapoda, biomass; DEPTH, water; Euphausiacea, biomass; Fishes, biomass; Invertebrata, biomass; Macroplankton, biomass; Myctophidae, biomass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6429; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 24
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Decapoda, biomass; DEPTH, water; Euphausiacea, biomass; Fishes, biomass; Invertebrata, biomass; Macroplankton, biomass; Myctophidae, biomass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6490; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 25
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Calculated; Cephalopoda; Cephalopoda, mass; Decapoda; Decapoda, mass; DEPTH, water; Euphausiacea; Euphausiacea, mass; Fish larvae; Fish larvae, mass; Hyperiidae, mass; Hyperiidea; Macroplankton; Macroplankton, mass; Macroplankton, wet weighted; Myctophidae; Myctophidae, mass; Mysidacea; Mysidacea, mass; Pteropoda; Pteropoda, mass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6493; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 198 data points
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  • 26
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Archive of Ocean Data; ARCOD; Decapoda, biomass; DEPTH, water; Euphausiacea, biomass; Fishes, biomass; Invertebrata, biomass; Macroplankton, biomass; Myctophidae, biomass; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ6493; Western Pacific
    Materialart: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 27
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Aporrhais alata; Aquilofusus luneburgensis; Aquilofusus semiglaber; Archimediella cochlias; Astarte (Ashtarotha) anus; Astarte (Carinastarte) reimersi; Astarte (Carinastarte) vetula; Astarte (Nicania) radiata gleuei; Astarte radiata; Babylonella fusiformis; Bathytoma jugleri; Brachytoma obtusangula; Calliostoma sp.; Conolithus antediluvianus; Cyclocardia orbicularis; Dentalium badense; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dolicholatirus rothi; Elevation of event; Euspira helicina; Event label; Fusiturris helena; Gemmula annae; Gemmula badensis; Haedropleura maitreja; Heide_T1; Hinia (Uzita) prismatica; Hinia (Zeuxis) holsatica; Katzheide; Kiel_KH; Laevidentalium sp.; Lamellinucula georgiana; Latitude of event; Layer description; Limopsis aurita; Longitude of event; Lyrotyphis sp.; Microdrillia crispata; Narona lyrata parvicarinata; Parvicardium straeleni; Phalium (Semicassis) sp.; Pleurotomoides luisae; Pyramidella plicosa; Pyrgolampros pseudoterebralis; Ringiculina buccinea; Schleswig-Holstein, Germany; Schulensee; Sipho distinctus; Sipho gregarius; Spiratella atlanta; Spirotropis modiola; Streptodictyon sexcostatus; Strombiformis glaber; Turbonilla pseudocostellata; Turritella tricarinata; Uromitra wirtzi; Xenophora sp.; Yoldia glaberrima; Yoldiella pygmaea
    Materialart: Dataset
    Format: text/tab-separated-values, 302 data points
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  • 28
    facet.materialart.
    Unbekannt
    PANGAEA
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Ammonia beccarii; Ammoscalaria runiana; Ammotium cassis; Bulimina marginata; Bulimina sp.; Buliminella elegantissima; Cibicides lobatulus; Cribrononion albiumbilicatum; Cribrononion asklundi; Cribrononion excavatum; Cribrononion incertum; Cribrononion pauciloculum; Dentalina sp.; Eggerella scabra; Fursenkoina fusiformis; Globigerina sp.; Great_Belt; Group; Guembelina globulosa; Lagena semilineata; Lagena sp.; Lagena sulcata laevicostata; MULT; Multiple investigations; Nonionella cf. grateloupi; Nonionella sp.; Protelphidium cf. anglicum; Reophax dentaliniformis regularis; Reophax subfusiformis; Sediment type; Spiroplectammina biformis; Western Baltic Sea
    Materialart: Dataset
    Format: text/tab-separated-values, 196 data points
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  • 29
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Abra sorgenfreii; Acamptogenotia escheri; Acanthocardia hanseata; Aequipecten radians; Amaea (Acrilla) amoena subreticula; Amyclina facki; Anadara diluvii; Ancilla obsoleta; Angulus (Moerella) donacina; Angulus fallax; Aporrhais alata; Aquilofusus beyrichi; Aquilofusus siebsi; Architectonica (Pseudotorinia) obtusa; Arctica sp.; Aspella (Favartia) sp.; Astarte (Digitaria) beyschlagi; Astarte (Goodallia) triangularis; Astarte (Isocrassina) angulata; Astarte goldfussi; Astarte gracilis convexior; Astarte radiata; Asthenotoma festiva; Babylonella fusiformis; Barlohe; Bathytoma mioturbida; Bittium spina; Boreodrillia hosiusi; Brachytoma obtusangula; Brachytoma pannoides; Brocchinia parvula; Cadulus gadus; Calliostoma (Ampullotrochus) elegantulum muelleri; Calyptraea chinensis; Cancellaria contorta; Cavilucina (Mesomiltha) droueti; Ceratocyathus granulatus; Cerithiella genei; Cerithiopsis vignali; Circulus hennei; Clavatula boreointerrupta; Clavatula boreoromana; Conolithus dujardini; Costoanachis corrugata; Crassispira borealis; Cuspidaria cuspidata; Cyclocardia chamaeformis; Cylichna cylindracea; Cylichnina elongata; Cylindrophyllia duncani; Delve_1; Dentalium dollfussi; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Ditrupa cornea; Dolicholatirus rothi; Donax stoffelsi; Dorsanum boreobaccatum; Elaeocyma diensti; Elevation of event; Epalxis hinschi; Ervilia pusilla; Erycina (Hemilepton) sp.; Eulimella sp.; Euspira helicina; Event label; Ficus conditus; Fusiturris aquensis; Fusiturris flexiplicata; Gemmula boreoturricula; Gemmula coronata; Gemmula denticula borealis; Gemmula stoffelsi; Gemmula zimmermanni; Glossus sp.; Glycymeris sp.; Gouldia minima; Habecardium subturgidum; Haustator eryna; Heide_T1; Hemiacirsa lanceolata; Hiatella arctica; Hinia (Telasco) bocholtensis fuchsi; Hinia (Tritonella) tenuistriata; Hinia (Uzita) serraticosta; Hinia cavata; Hinia cimbrica; Hinia subobesa; Hinia turbinella; Korobkovia woodi; Laevidentalium sp.; Lamellinucula jeffreysi; Latitude of event; Layer description; Lembulus emarginatus; Limopsis aurita; Longitude of event; Lucinoma borealis; Lutetia nitida; Lyrotyphis sejunctus priscus; Macoma elliptica; Meiocardia harpa; Melanella (Balcis) eichwaldi; Metuonella grippi; Mitrella (Macrurella) nassoides; Modiolula phaseolina; Murex inornatus; Nassarius (Phrontis) poelsensis; Nassarius (Phrontis) woodwardi; Natica cf. tigrina; Neoguraleus calais; Neoguraleus guerichi; Neoguraleus tenella; Neverita olla; Niso terebellum acarinatoconica; Nuculana (Saccella) westendorpi; Nucula nucleus; Nuculoma haesendoncki; Nuculoma laevigata; Odostomia conoidea; Oliva (Strephona) dufresnei; Parvicardium straeleni; Pecten brummeIi; Pectunculina retifera; Perrona hemmoorensis; Perrona obliquiplicatula; Phalium bicoronatum; Phalium miolaevigatum; Pharus saucatsensis; Phos decussatus; Pleurotomoides borealis; Pleurotomoides campanulata; Pleurotomoides elatior; Pleurotomoides luisae; Polinices miopusillus; Poromya neaeroides; Pyramidella plicosa; Pyrgolampros pseudoterebralis; RD_Armensee_501; Rhizorus acuminatus; Ringiculina buccinea; Ringiculina ravni; Roxania subutriculus; Scaphander grateloupi; Scaphella bolli; Schleswig-Holstein, Germany; Seila trilineata; Sipho grippi; Spisula trinacria; Splendrillia selenkae; Streptodictyon sexcostatus; Strioterebrum basteroti; Strioterebrum hoernesi; Strombiformis glaber; Sveltia varicosa; Syrnola hoernesi; Tahusyrinx corneti; Torculoidella subangulata; Trigonostoma umbilicaris pluricostata; Turricula steinvorthi; Typhis sp.; Vaginella depressa; Varicorbula gibba; Ventrilia acutangula; Venus multilamella; Xenophora deshayesi; Yoldia glaberrima; Yoldiella pygmaea
    Materialart: Dataset
    Format: text/tab-separated-values, 954 data points
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  • 30
    Publikationsdatum: 2023-07-07
    Schlagwort(e): Apatite; Archive of Ocean Data; ARCOD; Biotite; Carbonates in heavy mineral fraction; Carbonates light; Chlorite, light; Chlorite in heavy mineral fraction; Clayey aggregates; Clinopyroxene; Corundum; Counting, Stereo Microscope; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Disthene; Elevation of event; Epidote; Event label; Feldspar; Garnet; Grain size analysis after Petelin (1967, Nauka, Moscow); Gulf of Guinea; Heavy minerals; Hornblende; Latitude of event; Light minerals; Limonite; Longitude of event; Marcasite; Mikhail Lomonosov; ML10; ML10_829; ML10_846; ML10_847; ML10_848; Olivine; Ore; Organic remains; Orthopyroxene; Plagioclase; Quartz; Rock fragments; Sediment type; Separation with use of heavy (2.9) liquid; Size fraction 0.100-0.050 mm; Sphene; Staurolite; Tourmaline; Tremolite/Actinolite; Volcanic glass, heavy; Volcanic glass, light; Zircon; Zoisite
    Materialart: Dataset
    Format: text/tab-separated-values, 233 data points
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  • 31
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    Unbekannt
    PANGAEA
    In:  Supplement to: Soldatov, A V; Murdmaa, Ivar O (1970): The mineral composition of the deposits in the Romanche gap. Oceanology, 10, 375-381
    Publikationsdatum: 2023-07-11
    Beschreibung: A study was made of mineral composition of sand- and silt-sized fractions of recent clastic (riftogenic) sediments and solidified deposits collected from the bottom of the Romanche Trench during the first voyage of R/V Akademik Kurchatov. Similarity between mineral compositions of sediments and bedrocks (ultrabasites, gabbroids, diabases) was established. This similarity is a basis for considering the mineral complex of the deposits that have been derived from the bedrocks of the trench slopes, and have formed due to their submarine denudation accompanied by tectonic crushing. The same mineral composition was found in pieces of older consolidated deposits; this suggests that conditions of sedimentation similar to those at recent times have existed for a long time in the Romanche Trench.
    Schlagwort(e): AK1-08; AK1-10GC; AK1-5GR; AK1-7DRG; AK1-7GC; Akademik Kurchatov; AKU1; Anthophyllite; Apatite; Archive of Ocean Data; ARCOD; Augite-diopside; Black ore; Carbonate, authigenic; Carbonate, biogenic; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dredge; DRG; Elevation of event; Enstatite-bronzite; Epidote-zoisite; Event label; Feldspar; Fish teeh and bones; Garnet; GC; Grab; GRAB; Gravity corer; Heavy minerals; Heavy minerals, sum; Hornblende; Hornblende, basaltic; Hypersthene; Latitude of event; Leucoxene; Light minerals; Light minerals, sum; Longitude of event; Mica; Nonidentified, altered, heavy; Nonidentified, altered, light; Olivine; Opal, biogenic silica; Quartz; Red ore; Romanche Trench; Serpentine-chlorite; Size fraction; Spinel; Tremolite/Actinolite; Volcanic glass, heavy; Volcanic glass, light; Zircon
    Materialart: Dataset
    Format: text/tab-separated-values, 440 data points
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  • 32
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    PANGAEA
    In:  Supplement to: Baturin, Gleb N (1971): Formation of phosphate sediments and water dynamics. Oceanology, 11, 372-376
    Publikationsdatum: 2023-07-11
    Beschreibung: Available data on composition of sediments from the inner and outer continental shelves of the Southwest Africa, and on currents and variations of sea level in the Upper Quaternary are examined to elucidate the process of phosphate material concentration. Sand and gravel fractions in diatom oozes from the inner shelf have much higher phosphorus contents than adjoining sediments. This is due to presence of diagenetic phosphate nodules. As sea level varies, fine sediments are eroded by waves or currents that leads to formation of coarse-grained phosphate sediments.
    Schlagwort(e): AK3-140; AK3-143; AK3-151; AK3-152; AK3-157; AK3-160; AK3-161; AK3-163; Akademik Kurchatov; AKU3; Archive of Ocean Data; ARCOD; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Grab; GRAB; Latitude of event; Longitude of event; Phosphorus pentoxide; Size fraction; Wet chemistry
    Materialart: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 33
    Publikationsdatum: 2023-07-11
    Schlagwort(e): Atlantische Kuppenfahrten 1967/4-7; BC; BCR; Box corer; Box corer (Reineck); Bryozoa; Cape Blanc/Meteor Bank/Portugal; Coral; Counting; Crinoidea; Decapoda; DEPTH, sediment/rock; Dredge; DRG; Echinoidea; Elevation of event; Event label; Foraminifera, benthic recent; Foraminifera, benthic reworked; Foraminifera, planktic; Foraminifera, planktic recent; Foraminifera, planktic reworked; Fragments; Gastropoda; Gastropoda, planktic; Gastropoda, planktic recent; Gastropoda, planktic reworked; Grab; GRAB; Grains, relict; Indeterminata; Latitude of event; Longitude of event; M19; M19_211; M19_215-2; M19_217-2; M9; M9_101; M9_101b; M9_110; M9_117; M9_118; M9_119; M9_121; M9_122; M9_123; M9_124; M9_125; M9_127; M9_128; M9_129; M9_130; M9_131; M9_132; M9_133; Median, grain size; Meteor (1964); Mode, grain size; North Atlantic; Ophiuroidea; Ostracoda; Pelecypods; Quartz; Rossbreiten-Expedition 1970; Serpulidae; Size fraction; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 2 mm, gravel; Size fraction 2.000-0.630 mm, coarse sand; South Atlantic Ocean; Sponge spiculae; van Veen Grab; VGRAB; Volcanic glass
    Materialart: Dataset
    Format: text/tab-separated-values, 625 data points
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  • 34
    Publikationsdatum: 2023-07-11
    Schlagwort(e): Atlantis_II_1969; Atlantis II (1963); Calcite/Dolomite ratio; Calculated; Carbonates; Coruh; Feldspar; Plagioclase/Kalifeldspar ratio; Quartz; Quartz/Feldspar ratio; SESAME; Size fraction; Southern European Seas: Assessing and Modelling Ecosystem Changes; Water sample; WS
    Materialart: Dataset
    Format: text/tab-separated-values, 49 data points
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  • 35
    Publikationsdatum: 2023-07-11
    Schlagwort(e): 804; Calcite/Dolomite ratio; Calculated; Carbonates; Feldspar; Global River Discharge; Inozu; Kizilirmak, Turkey, Asia; Plagioclase/Kalifeldspar ratio; Quartz; Quartz/Feldspar ratio; RGS; River gauging station; SESAME; Size fraction; Southern European Seas: Assessing and Modelling Ecosystem Changes
    Materialart: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 36
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    PANGAEA
    In:  Geological Institute, Russian Academy of Sciences, Moscow
    Publikationsdatum: 2023-07-11
    Schlagwort(e): Archive of Ocean Data; ARCOD; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Grain size analysis after Petelin (1967, Nauka, Moscow); Gravity corer; Iron; Latitude of event; Longitude of event; Northwest Pacific; PC; Percentage; Piston corer; Size fraction; VITYAZ; Vityaz (ex-Mars); VITYAZ6158-GC; VITYAZ6161-PC; Wet chemistry
    Materialart: Dataset
    Format: text/tab-separated-values, 79 data points
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  • 37
    Publikationsdatum: 2023-09-03
    Schlagwort(e): Aotea Seamount, Eastern Tasman Sea; CSM-HG4D; CSM-HG6C; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; ELT36; ELT36.024-BT; ELT36.039-BT; Eltanin; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Philippine Sea; Position; Quantity of deposit; Sample code/label; Size; Southern Basin, Pacific Ocean; Southern Ocean; Substrate type; TAR_1968; TAR_1968_E-902; Taranui; TRAWL; Trawl net; Uniform resource locator/link to image; Visual description; Vityaz (ex-Mars); Vityaz-48; VITYAZ6298-30-TR
    Materialart: Dataset
    Format: text/tab-separated-values, 241 data points
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  • 38
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    PANGAEA
    In:  Supplement to: Cronan, David S; Thomas, R L (1972): Geochemistry of ferromanganese oxide concretions and associated deposits in Lake Ontario. Geological Society of America Bulletin, 83(5), 1493-1502, https://doi.org/10.1130/0016-7606(1972)83%5B1493:GOFOCA%5D2.0.CO;2
    Publikationsdatum: 2023-08-28
    Beschreibung: A large deposit of ferromanganese oxide coated sands and scattered manganese nodules occurs in the northern portion of Lake Ontario. The Mn and Fe contents of the concretions are similar to those in concretions from other environments, while their Ni, Cu, and Co contents are lower than in deep-sea nodules, but higher than in most previously described lacustrine concretions. Pb and Zn are high in the coatings and exceed the concentrations found in many previously analyzed Mn deposits. Within the deposit, Mn, Ni, Co, and Zn contents are correlated, and they vary inversely with Fe. Mn, Fe, Ni, Cu, and Pb are present in the interstitial waters of the sediments underlying the deposit in higher concentrations than in the overlying lake waters, thus providing a potential source of metals for concretion formation.The origin and compositional variations in the deposit possibly can be explained in terms of the fractionation and precipitation of Fe and Mn as a result of redox variations in the lake sediments. Eh increases from south to north across the deposit in such a way that iron may be selectively oxidized and precipitated in the south and manganese, in the north. The upward diffusion of Mn, Fe, and associated elements from the underlying sediments probably provides the principal source of the metals in the south of the deposit, while metal-enriched bottom waters are probably the principal source in the north.
    Schlagwort(e): Lake Ontario; Lake-Ontario_K2; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Materialart: Dataset
    Format: application/zip, 2 datasets
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  • 39
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    PANGAEA
    In:  Supplement to: Scott, Robert B; Rona, Peter A; Butler, Louis W; Nalwalk, Andrew J; Scott, Martha R (1972): Manganese Crusts of the Atlantis Fracture Zone. (see erratum for this paper: Nature Phys. Sci. 242, 95, 1973), Nature Physical Science, 239(92), 77-79, https://doi.org/10.1038/physci239077a0
    Publikationsdatum: 2023-08-28
    Beschreibung: Summaries of the transition element chemistry of oceanic ferro-manganese deposits report compositional trends related to water depth and to geographic proximity to continental margins1-4. Explanations of compositional variations include continental source influence3, 5, 6, diagenetic environmental control of manganese mineralogy that regulates the trace metal composition1, 3, 7, ionic mobility in interstitial solutions during diagenesis3, 8-10, and volcanic or hydrothermal influence3, 11-14. Glasby15 rejects a significant pressure control on manganese oxide mineralogy on thermodynamic grounds.
    Schlagwort(e): Atlantic Ocean; Atomic absorption spectrometry (AAS); Chromium; Cobalt; Copper; Discoverer (1966); DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Event label; Iron; Manganese; Mercury; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; T3-71D 148-2B; T3-71D 160-10G; TAG1971; TAG1971-10G; TAG1971-2B; Trans-Atlantic Geotraverse 1971; Vanadium; Zinc
    Materialart: Dataset
    Format: text/tab-separated-values, 146 data points
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  • 40
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    PANGAEA
    In:  Supplement to: Varentsov, Igor M (1972): On the main aspects of formation of ferromanganese ores in recent basins (lakes). In: Proc. 24th Intl. Geol. Congr., presented at the Mineral Deposits Symposium, 24th International Geological Congress (Montreal), Sect 4, 395-403, hdl:10013/epic.46330.d001
    Publikationsdatum: 2023-08-28
    Beschreibung: The distribution of Mn and Fe in water, sediments, hydroxide nodules and crusts of Eningi-Lampi ore-bearing lake is regular, and concordant from the source to the areas of accumulation of these components. Mn-Fe hydroxide nodules and crusts occur at the water-sediment interface, and more rarely in the upper (0-5 cm) film of brown watery mud. The leading role in the formation of Mn-Fe nodules and crusts is played by the chemosorption and auto-catalytic oxidation in the course of interaction of component-bearing solutions with active surfaces. This is considered to be the basic process for the model of ferromanganese ore formation in recent basins. Despite the differences in the physico-geographical and geochemical characteristics of lakes, mediterranean seas and oceans, the formation of ferromanganese hydroxide nodules and crusts in these basins may be explained by this model.
    Schlagwort(e): DEPTH, sediment/rock; Dredge; DRG; Elevation of event; EningiLampi_104; EningiLampi_116; EningiLampi_117; EningiLampi_118; EningiLampi_119; EningiLampi_121; EningiLampi_123; EningiLampi_127; EningiLampi_128; EningiLampi_133; EningiLampi_137; EningiLampi_141; EningiLampi_150; EningiLampi_152; EningiLampi_154; EningiLampi_158; EningiLampi_99; Event label; Iron; Lake Eningi-Lampi, Russia; Latitude of event; Longitude of event; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Spectrophotometric
    Materialart: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 41
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Harriss, Robert C; Troup, Arthur G (1970): Chemistry and origin of freshwater ferromanganese concretions. Limnology and Oceanography, 15(5), 702-712, https://doi.org/10.4319/lo.1970.15.5.0702
    Publikationsdatum: 2023-08-28
    Beschreibung: Ferromanganese concretions from Grand Lake and Ship Harbour Lake in Nova Scotia and Mosque Lake in Ontario are most common in water 0.5 to 2 m deep. X-ray diffraction studies show the ferromanganese portions of the concretions to he amorphous. Petrographic and electron probe studies of the ferromanganese material reveal chemical banding of iron and manganese. Bulk chemical analyses indicate that the Fe:Mn ratios of concretions from different sites within a single lake are similar, whereas concretions from different lakes have characteristic Fe:Mn ratios. Trace element concs are different in different lakes and are generally several orders of magnitude less than those of oceanic nodules.
    Schlagwort(e): Canada; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Grab; GRAB; Grand_Lake-H; Identification; Lake_Charlotte-S; Lake_Mosque-H; Mercury; Mercury vapor detector; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nova Scotia, Canada; Ontario, Canada
    Materialart: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 42
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    PANGAEA
    In:  Supplement to: Bertrand, Wayne Gerrard (1972): A geological reconnaissance of the Dellwood seamount area, northeast Pacific Ocean, and its relation to plate tectonics (MS thesis). University of British Columbia, Vancouver, Canada, 166 pp, https://open.library.ubc.ca/cIRcle/collections/ubctheses/831/items/1.0053141
    Publikationsdatum: 2023-08-28
    Beschreibung: The Dellwood Seamount Area, an area of approximately 10,000 square km., about 185 km. west of the northern tip of Vancouver Island is located at or near the northernmost end of the Juan de Fuca plate. The main purpose of the study was to test the hypothesis that the Dellwood Knolls mark the site of a short spreading segment connected to the Explorer Spreading Segment at one end by a transform fault trending along the southwestern slope of Paul Revere Ridge; and meeting the Queen Charlotte right lateral transform fault at the other end. An analysis of more than 950 km. of continuous seismic reflection profiles, in conjunction with other geophysical data, shows that (i) the Revere -Dellwood fault zone is a dextral transform fault zone connecting the Explorer and Dellwood spreading segments. (ii) The Queen Charlotte transform fault dies out at the southeastern end of the Scott Channel near the northeastern end of the Dellwood Spreading Segment. (iii) In the channel between the Dellwood Knolls (one of two possible locations of the Dellwood Spreading Segment), the sediments and volcanic basement are cut by normal faults, a feature which is characteristic of spreading centres with median valleys. The heat flow in this channel and in the Revere - Dellwood fault zone is high. (iv) The lower continental slope sediments west of Queen Charlotte Sound is faulted and crumpled and may be the northerly extension of the Scott Islands fault, zone and a site of slow contemporaneous or recently ceased subduction. The deformation of the thick turbidite sequence in the Winona Basin may also be due to subduction. Basalt from the area is chemically intermediate between tholeiitic and alkalic types. That from the Northwest Dellwood Knolls, however, is least differentiated and less than 1 myr. old in contrast to basalt from the sediment-draped Southeast Dellwood Knolls, the latter basalt having Mn-coating up to 50 mm. thick and is thus relatively old. This suggests that spreading may be occurring at the Northwest Dellwood Knolls and not in the channel between the knolls. The texture of basalts from the Dellwood Seamount Range vary depending on size of pillow and depth below pillow surface, but the mineralogy is essentially similar. An unusual rock probably best described as a plagio-clase-olivine basalt porphyry was also recovered from the Dellwood Seamount Range. Non-volcanic rocks recovered include glacial erratics, an authigenic sandstone comprising glacial fragments in an iron-rich cement, a laminated limonitic sediment and manganese nodules. The Dellwood Spreading Segment may have originated by left lateral transcurrent offset from the Explorer Spreading Segment, the offset caused by a change in the direction of motion of the Juan de Fuca plate.
    Schlagwort(e): 70025-5837; 70025-5842; Aluminium; Atomic absorption spectrometry (AAS); Calcium; CNAV Endeavour; Cobalt; Copper; Date/Time of event; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; EN70-025; EN70-025-3D; EN70-025-9D; Event label; HUDSON 70 PHASE VII; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Potassium; Sample ID; Silicon; Sodium; Titanium; Zinc
    Materialart: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 43
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    Unbekannt
    PANGAEA
    In:  Supplement to: Edgington, David N; Callender, Edward (1970): Minor element geochemistry of Lake Michigan ferromanganese nodules. Earth and Planetary Science Letters, 8(2), 97-100, https://doi.org/10.1016/0012-821X(70)90157-3
    Publikationsdatum: 2023-08-28
    Beschreibung: Samples of ferromanganese nodules from several localities in Lake Michigan have been analyzed for their minor element content utilizing neutron activation techniques. The thorium and uranium levels in Lake Michigan nodules exhibit marked dissimilarities with marine nodules. The radium content of these freshwater nodules is substantially higher than the reported marine values. The concentrations of barium in the Lake Michigan nodules appear to be abnormally high. Although barium could be present as minute segregations of the mineral barite, patterns obtained using the electron microprobe suggest it is evently dispersed throughout the nodules. The average arsenic content of these freshwater nodules is at least twice as great as that reported for highly oxidized marine sediments. If all this arsenic is dissolved and released into Green Bay as a result of changing environmental conditions (eutrophication), the concentration in the water of Green Bay would be several times the maximum permissible level for drinking water.
    Schlagwort(e): Antimony; Arsenic; Atomic absorption spectrometry (AAS); Barium; Bromine; Cadmium; Cerium; Cobalt; Comment; Copper; Dredge; DRG; EDGI1970_11; EDGI1970_2; EDGI1970_35; EDGI1970_37; EDGI1970_43; EDGI1970_6; Europium; Event label; Gallium; Green Bay - Lake Michigan; Iron; Lake Michigan; Lanthanum; Manganese; Maximum; Neutron activation analysis; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Radium; ROSS1969_25; Samarium; Sample ID; Scandium; Soluble residue; Strontium; Thorium; Uranium; Zinc
    Materialart: Dataset
    Format: text/tab-separated-values, 241 data points
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  • 44
    Publikationsdatum: 2023-08-28
    Beschreibung: The Atlantic Advisory Panel proposed that Site 8 should be drilled on the rise between the Hatteras and Sohm Abyssal Plains (lat 35° 2l'N., long 67° 3l'W.) This location was considered to offer the best opportunity for realizing two primary objectives. The first of these objectives was to sample and date the oldest available rock in a region adjacent to the North American continent and as far as possible from the Mid-Atlantic Ridge. The second objective relates to the potential paleobiological and paleoecological information that could be derived from the sedimentary column in this general area.
    Schlagwort(e): 2-8; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg2; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Substrate type
    Materialart: Dataset
    Format: text/tab-separated-values, 17 data points
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  • 45
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 12 of this report formerly was designated 14 by the Atlantic Advisory Panel. It was drilled in the Cape Verde Basin (latitude 19° 42'N, longitude 26° 01'W), which is underlain by 2000 to 2100 feet (0.9 to 1.1 seconds reflection time) of sediment. The bottom topography of the basin is fairly smooth but not to the degree of an abyssal plain. Site 12 was selected to provide material for paleontological investigations.
    Schlagwort(e): 2-12C; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Glomar Challenger; Latitude of event; Leg2; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/BASIN; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type
    Materialart: Dataset
    Format: text/tab-separated-values, 53 data points
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  • 46
    Publikationsdatum: 2023-08-28
    Beschreibung: The preliminary planning and approach to site 13 were taken from the JOIDES Atlantic Advisory Panel Report and from a previous detailed survey of the site by R/V Vema of the Lamont Geological Observatory. Several CSP profiles crossing the selected site in various directions show an uplifted portion of the sea floor roughly circular in shape of about 10 kilometers in diameter. In contrast to the smooth bottom of the surrounding abyssal plain, the topography of the small rise selected for the site has a small-scale roughness of amplitude of 40 to 80 meters. The work reported here is a biostratigraphic summary of available samples. Only the most important and biostratigraphically significant components of the faunas have been noted. No attempt has been made to give an exhaustive faunal analysis of the samples seen.
    Schlagwort(e): 3-13; 3-15; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg3; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; South Atlantic/HILL
    Materialart: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 47
    Publikationsdatum: 2023-08-28
    Beschreibung: The Atlantic Advisory Panel proposed that Site 9 should be drilled on the northeastern flank of the Bermuda Rise (lat. 32° 37' N., long. 59° 10' W.), which is about 100 miles west of the Sohm Abyssal Plain. The bottom of this region consists of low linear ridges that are roughly parallel and oriented in a northwest-southeasterly direction. Scattered seamounts, some of which have peaks 2000 fathoms (3660 meters) below sea level, arise from the otherwise featureless sea floor between the ridges. The primary purpose in drilling Site 9 was to examine a sedimentary column where seismic reflectors were largely absent and to determine the age of sediments overlying acoustical basement in the examination of sea floor spreading.
    Schlagwort(e): 2-9A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Glomar Challenger; Latitude of event; Leg2; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Size
    Materialart: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 48
    Publikationsdatum: 2023-08-28
    Beschreibung: Prior to arrival on this site, the only survey data available was from the Vema-20 crossing of the area. The recommended site location was over a relatively smooth valley in the bottom topography at about 4750 meters (15,580 feet) depth (uncorrected), about 10 kilometers wide E-W between peaks (or ridges) on either side. Sediment thickness was unknown. The center of the valley is near the peak of a wide (40 to 50 kilometers) positive magnetic anomaly, identified as Magnetic Anomaly 30 in the hypothesized geomagnetic time scale with an age of 72 million years.
    Schlagwort(e): 3-20; 3-20A; 3-20C; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg3; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; South Atlantic/VALLEY; Substrate type
    Materialart: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 49
    Publikationsdatum: 2023-08-28
    Beschreibung: The drilling objectives at this site were to complete the cored section begun at Site 23 in accordance with the recommendations of the JOIDES Atlantic Advisory Panel, presented in the Site 23 report. The location coincides with a position on the southeastern side of the elevated portion of basement in this area.
    Schlagwort(e): 4-24; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Glomar Challenger; Latitude of event; Leg4; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; South Atlantic/CONT RISE
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 50
    Publikationsdatum: 2023-08-28
    Beschreibung: At the Leg 4 pre-cruise meeting in Miami, Florida, in January 1969, the Ridge site was proposed as an additional site to be investigated, if possible. Since the water depth and sediment thickness at this site were both minimal (2000 meters and less than 100 meters, respectively) and the location was not far from the track between initially planned sites, the shipboard party decided, upon completion of work at Site 24, to make a 24-hour drilling effort on the North Brazilian Ridge. The drilling objectives at this location were to sample and date the sediments atop the Ridge crest and to determine the nature, age and origin of the consolidated material beneath the thin mantle of sediment.
    Schlagwort(e): 4-25A; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Glomar Challenger; Latitude of event; Leg4; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Size; South Atlantic/RIDGE; Substrate type
    Materialart: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 51
    Publikationsdatum: 2023-08-28
    Beschreibung: The northern margin of the Demerara Abyssal Plain is bordered by a low ESE-WNW trending rise known as the Barracuda Ridge. North of South America, the eastern margin of the Demerara Abyssal Plain is formed by the Barbados Ridge. An extensive sedimentary section of the Barbados Ridge is exposed on the island of Barbados and consists of a series of radiolarian to planktonic foraminiferal and calcareous nannofossil biogenic sediments interlayered with ash beds. To determine the nature of the sediments and "basement," Site 27 was selected on the northern margin of the Demerara Abyssal Plain, south of the Barracuda Ridge.
    Schlagwort(e): 4-27; 4-27A; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg4; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/RIDGE; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type
    Materialart: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 52
    Publikationsdatum: 2023-08-28
    Beschreibung: The southern Caribbean basins are thought to be part of a relatively old and geologically stable crustal plate. Although surrounded by belts of high earthquake activity, the central Caribbean is seismically quiet. The region also constitutes a quiet magnetic zone and appears to have resisted all of the surrounding forces related to ocean floor spreading. In addition to providing considerable information on the general geologic history of the Caribbean region, paleontologic studies on cores at Site 29 were expected to provide valuable data on phylogenetic trends within the planktonic foraminifera and calcareous nannoplankton, furnishing more accurate criteria for intercontinental stratigraphic correlation. The work reported here is a biostratigraphic summary of available samples. only the most important and biostratigraphically significant components of the faunas have been noted. No attempt has been made to give an exhaustive faunal analysis of the samples seen.
    Schlagwort(e): 4-29B; Caribbean Sea/BASIN; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Glomar Challenger; Latitude of event; Leg4; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 53
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 26 was selected on the crest of the Mid-Atlantic Ridge between 15°N and 5°S is offset to the east nearly 4000 kilometers through a series of fracture zones. One of the most prominent of these is the Vema Fracture Zone, a narrow east-west trending trough which cuts through the Mid-Atlantic Ridge at latitude 11°N.
    Schlagwort(e): 4-26; Comment; Date/Time of event; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Glomar Challenger; Latitude of event; Leg4; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/TROUGH; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Size
    Materialart: Dataset
    Format: text/tab-separated-values, 18 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 54
    Publikationsdatum: 2023-08-28
    Schlagwort(e): Barium oxide; Calcium oxide; Charco_Redondo_S; Comment; Cuba; Deposit type; DEPTH, sediment/rock; Iron oxide, Fe2O3; Magnesium oxide; Manganese dioxide; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium oxide; Sample ID; Silicon dioxide; Sodium oxide; Water in rock; Wet chemistry
    Materialart: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 55
    Publikationsdatum: 2023-08-28
    Beschreibung: The cores and dredges described in this report were taken on the ARIES Expedition from November 1970 until October 1971 by the Scripps Institution of Oceanography from the R/V Thomas Washington. A total of 65 cores and dredges were recovered and are available at Scripps for sampling and study.
    Schlagwort(e): ARIES; ARIES-002D; ARIES-003D; ARIES-005D; ARIES-007D; ARIES-009D; ARIES-010D; ARIES-011D; ARIES-012D; ARIES-013D; ARIES-014D; ARIES-015D; ARIES-016D; ARIES-019D; ARIES-020D; ARIES-021D; ARIES-022D; ARIES-023D; ARIES-024D; ARIES-025D; ARIES-026D; ARIES-027D; ARIES-028D; ARIES-029D; ARIES-030D; ARIES-031D; ARIES-032D; ARIES-033D; ARIES-035D; ARIES-036D; ARIES-037D; ARIES-038D; ARIES-039D; ARIES-041D; ARIES-044D; ARIES-045PG; ARIES-047G; ARIES-049G; ARIES-051D; ARIES-055D; ARIES-056D; ARIES-057D; ARIES-058D; ARIES-059D; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; 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; Substrate type; Thomas Washington; Uniform resource locator/link to image
    Materialart: Dataset
    Format: text/tab-separated-values, 426 data points
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  • 56
    Publikationsdatum: 2023-08-28
    Beschreibung: The BLM-OCS (Bureau of Land Management-Outer Continental Shelf) program was designed to establish chemical, biological, and geological baseline on the South Texas Continental Shelf. The focus for the geological program was to establish the nature and amount of the suspended sediment in the water column, of the Holocene sediments on the shelf, and to identify and locate regions of geology conditions which may be hazardous to OCS operations. To accomplish these goals three cruises were planned. The report constitutes results of the first cruise. The results of these cruises associated with the subsequent laboratory analysis, enabled to establish a detailed baseline in order to provide significant geologic and biologic data for environmental assessment. Dredges recovered are available at University of Texas (see: BLM/OCS South Texas Outer Continental Shelf (STOCS) Project Sediment Data http://www.ngdc.noaa.gov/docucomp/page?xml=NOAA/NESDIS/NGDC/MGG/Geology/iso/xml/G02888.xml&view=getDataView&header=none).
    Schlagwort(e): 1974-012-FA; BLMSTG-55G; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Gulf of Mexico; Kana Keoki; KNKE BLM-Leg Alpha; CORPUS 22/28; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Size; Substrate type
    Materialart: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 57
    Publikationsdatum: 2023-08-28
    Beschreibung: The BLM-OCS (Bureau of Land Management-Outer Continental Shelf) program was designed to establish chemical, biological, and geological baseline on the South Texas Continental Shelf. The focus for the geological program was to establish the nature and amount of the suspended sediment in the water column, of the Holocene sediments on the shelf, and to identify and locate regions of geology conditions which may be hazardous to OCS operations. To accomplish these goals three cruises were planned. The report constitutes results of the second cruise. The results of these cruises associated with the subsequent laboratory analysis, enabled to establish a detailed baseline in order to provide significant geologic and biologic data for environmental assessment. Dredges recovered are available at University of Texas (see: BLM/OCS South Texas Outer Continental Shelf (STOCS) Project Sediment Data http://www.ngdc.noaa.gov/docucomp/page?xml=NOAA/NESDIS/NGDC/MGG/Geology/iso/xml/G02888.xml&view=getDataView&header=none).
    Schlagwort(e): 1974-014-FA; BLMSTG-191G; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Gulf of Mexico; Kana Keoki; KNKE BLM-Leg Bravo; CORPUS 23/29; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Substrate type
    Materialart: Dataset
    Format: text/tab-separated-values, 6 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 58
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Fischer, A G; Boyce, Robert E; Bukry, David; Douglas, Robert G; Garrison, Robert E; Kling, S A; Krasheninnikov, Valery A; Lisitzin, Alexander P; Pimm, Anthony C (1971): Site 49. In: Fischer, A.G.; et al., Initial Reports of the Deep Sea Drilling Project, 6, Initial Reports of the Deep Sea Drilling Project, 6, U.S. Government Printing Office, VI, 171-194, https://doi.org/10.2973/dsdp.proc.6.107.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: At Sites 47 and 48, impenetrable and cherty Upper Cretaceous chalks were found. The upper part of what infer to be lower Cretaceous is even more reflective, and likely to be very cherty (and was found to be cherty in the Vema core). It became clear that basement could only be reached where the Upper Cretaceous and the upper part of the lower Cretaceous are absent. However, west of Site 48, the R/V Argo record showed an area in which the Upper Cretaceous has wedged out down dip, and the Lower Cretaceous is thinning out by loss of the strongly reflective beds at the top. This area appeared to offer the best chance for sampling the lowermost transparent layer. Two holes were drilled: Hole 49.0 and Hole 49.1 after Hole 49.0 stopped at 18 m. Beds near the base of sedimentary sequence revealed by the seismic profiles are found to be of early Cretaceous (Neocomian) or latest Jurassic (Tithonian) age, and of pelagic facies. The crust under the Shatsky Rise is latest Jurassic or older.
    Schlagwort(e): 6-49; 6-49A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg6; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 59
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Fischer, A G; Boyce, Robert E; Bukry, David; Douglas, Robert G; Garrison, Robert E; Kling, S A; Krasheninnikov, Valery A; Lisitzin, Alexander P; Pimm, Anthony C (1971): Site 50. In: Fischer, A.G.; et al., Initial Reports of the Deep Sea Drilling Project, 6, Initial Reports of the Deep Sea Drilling Project, 6, U.S. Government Printing Office, VI, 195-222, https://doi.org/10.2973/dsdp.proc.6.108.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 49 had been selected to investigate the basal part of the sedimentary sequence as revealed by the acoustic profiles, and to sample the underlying opaque material. However, the cherty nature of the sediments prevented penetration of the section at Site 49, and the only recourse appeared to be to move to a spot of even thinner sedimentary cover. Such a place existed, just downslope from Site 49, where Horizon B' comes very close to the surface, this is where Site 50 was selected.
    Schlagwort(e): 6-50; 6-50A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg6; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 28 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 60
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Fischer, A G; Boyce, Robert E; Bukry, David; Douglas, Robert G; Garrison, Robert E; Kling, S A; Krasheninnikov, Valery A; Lisitzin, Alexander P; Pimm, Anthony C (1971): Site 48. In: Fischer, A.G.; et al., Initial Reports of the Deep Sea Drilling Project, 6, Initial Reports of the Deep Sea Drilling Project, 6, U.S. Government Printing Office, VI, 145-169, https://doi.org/10.2973/dsdp.proc.6.106.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Having been stopped by chert in the Maestrichtian at Site 47, a site was looked for which would give an adequate Cenozoic thickness for satisfactory spudding-in, yet promised to lead from this into an older part of the section. This is the first record of Middle Maestrichtian in pelagic carbonate facies from the Northwest Pacific and surrounding lands, a matter of paleontologic-biostratigraphic importance.
    Schlagwort(e): 6-48; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg6; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/PLATEAU; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 61
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Karig, Dan (1971): Site Surveys in the Mariana Area (Scan IV). In: Fischer, A.G.; et al., Initial Reports of the Deep Sea Drilling Project, 6, Initial Reports of the Deep Sea Drilling Project, 6, U.S. Government Printing Office, VI, 681-689, https://doi.org/10.2973/dsdp.proc.6.120.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: During the fourth and fifth legs of Scan Expedition, drill Sites 53 and 60 were surveyed and Site 59 was traversed. In addition to the drill site surveys, several other areas across the Mariana Arc System were investigated in some detail, guided by reconnaissance work aboard the R/V Argo from the previous year. The remarkable similarities in the occurrence and relative positions of a wide range of structural features in western Pacific arc systems strongly suggest a common mechanism of origin. The area in which crustal deformation related to island arc tectonism is occurring, more extensive and complex than generally recognized, is defined as the active island arc system; this includes not only the trench and volcanic chain, but also the deep basin and submarine ridge on the concave side of the active volcanoes.
    Schlagwort(e): Argo; CAME; Camera; Comment; Deposit type; DEPTH, sediment/rock; Description; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; SCAN; SCAN-STA39C; Sediment type; Uniform resource locator/link to image; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 9 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 62
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 61. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 27-47, https://doi.org/10.2973/dsdp.proc.7.103.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: The results at Site 59 suggested that Mesozoic sediments are present beneath a thin Tertiary cover in the region north of the Caroline Ridge near the Mariana Trench. Since one of the principal objectives of the drilling program was to find old Pacific crust, and since the section at Site 59 was not fully penetrated, it seemed worth a determined effort to go beyond the level reached at Site 59, somewhere in the same general area, in an attempt to reach basement. As the reflection profile taken by Argo (SCAN Leg V) through Site 59 shows the section above thesmooth basement reflector (Horizon B?) thinning northwestward from about 0.3 to 0.15 second, by loss of part of the lower "transparent" layer, this is were Site 61 was located.
    Schlagwort(e): 7-61; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 9 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 63
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 63. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 323-472, https://doi.org/10.2973/dsdp.proc.7.105.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: The sedimentary section at Site 62 on Eauripik Ridge can be traced eastward into the East Caroline Basin. It was decided to drill a hole to basement in the eastern part of East Caroline Basin to determine the age of the upper strong reflectors and to test the hypothesis that sediments older than any at Site 62 are present. A nearly complete section was obtained from middle Oligocene to Quaternary, unconformably overlying basalt containing middle Oligocene chalk xenoliths. The sediments consist of chalk and chalk ooze in the Oligocene and Miocene, and of marl ooze and calcareous clay in the Pliocene and Quaternary.
    Schlagwort(e): 7-63; 7-63A; 7-63B; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 33 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 64
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Presley, Bobby J; Kaplan, I R (1971): Interstitial Water Chemistry: Deep Sea Drilling Project, Leg 7. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 883-887, https://doi.org/10.2973/dsdp.proc.7.113.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: The interstitial water received at UCLA from Leg 7 (Guam to Hawaii) consisted of forty-two samples of approximately 5 milliliters each, three samples of approximately 10 milliliters each, and three samples of approximately 100 milliliters each. These pore waters had been squeezed from sediments consisting primarily of biogenic ooze, and had been collected at five different drilling sites along the route. High cobalt value were observed at Site 66 and were accompanied by a relatively high manganese concentration, but more normal iron, nickel and copper concentrations. This apparent cobalt enrichment could not be explained at the time of procedure. The line Islands area were Site 66 is situated was later notoriously known for its high Co values in manganese crust deposits (see, He, G., Ma, W., Song, C., Yang, S., Zhu, B., Yao, H., Jiang, X., Cheng, Y., 2011. Distribution characteristics of seamount cobalt-rich ferromanganese crusts and the determination of the size of areas for exploration and exploitation. Acta Oceanologica Sinica 30, 63–75. doi:10.1007/s13131-011-0120-9).
    Schlagwort(e): 7-62A; 7-65; 7-66; Atomic absorption spectrometry (AAS); Cobalt; Comment; Copper; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg7; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/RIDGE; Sample code/label; Sediment type; Silicon
    Materialart: Dataset
    Format: text/tab-separated-values, 30 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 65
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 67. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 821-841, https://doi.org/10.2973/dsdp.proc.7.109.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 67 is on the Hawaiian Arch, in the general region selected for one of the Mohole Project sites. Therefore, intensive geophysical surveys have been made in the area. The objectives were to penetrate the entire sedimentary sequence to basement in order to learn the petrology and ages of the sediments and of the seismic reflectors, and to obtain samples of the underlying basement rocks. Well consolidated and bedded volcanic sandstone and mudstone, and claystone were found to extend from the sea floor to a depth of 60 meters, where a layer of hard brown porcelanite stopped the bit. Displaced radiolarians in mud from a core at 60 meters indicate sediments of early Eocene or late Paleocene age are present somewhere above that depth.
    Schlagwort(e): 7-67; 7-67A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 15 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 66
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 65. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 607-723, https://doi.org/10.2973/dsdp.proc.7.107.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: An acoustically very transparent layer is present over much of the deep basin—here termed the Central Basin—between the Gilbert and Marshall Islands on the west and the Line Islands on the east. The Pacific Panel recommended drilling in this region to sample at least the upper transparent layer, and the first opaque layer beneath. Several possible sites were considered by the panel and by the shipboard party. Of paramount importance in choosing a particular site was a concern that sufficient sediments be present to bury the bottom-hole assembly (the drill collars and bumper subs) before the bit struck hard rock. A set of nearly continuous cores of an apparently uninterrupted section of radiolarian ooze ranging in age from middle Eocene to Recent was obtained, but the bit did not reach the deepest seismic reflector. Below depths of 127 meters, in the Oligocene and Eocene, thin chert and turbidite beds are sparsely interbedded with ooze.
    Schlagwort(e): 7-65; 7-65A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 41 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 67
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 66. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VII, 725-819, https://doi.org/10.2973/dsdp.proc.7.108.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: One of the principal objectives in the Central Pacific Basin was to elucidate the Paleobathymetric history of the region, which is located amidst groups of atolls and guyots that have subsided as much as 2 kilometers since mid-Cretaceous times. After failure to penetrate the entire sedimentary section and to sample basement at Site 65, on the west side of the Central Basin another site in the Basin where basement rocks might be sampled was searched. Likely places were known from unpublished reflection profiles on the east side of the Basin near the Line Islands by the Hawaii Institute of Geophysics. Finally it was decided to drill a transparent section once again in this area acoiding turbidites formations.
    Schlagwort(e): 7-66; 7-66A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 67 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 68
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Tracey, J I; Sutton, George H; Nesteroff, Wladimir D; Galehouse, J S; von der Borch, Christopher C; Moore, T; Lipps, J; Haq, Bilal U; Beckmann, Jean-Pierre (1971): Site 70. In: Tracey, J.I.Jr.; et al., Initial Reports of the Deep Sea Drilling Project, 8, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VIII, 135-284, https://doi.org/10.2973/dsdp.proc.8.105.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 70 is located about 20 miles north of the northern boundary of the Clipperton Fracture Zone near 140° W. It is the northernmost of the N-S line of sites drilled during Leg 8 to investigate the east-west trending accumulation of sediment centered at about 2°N near 140°W. It lies about 500 miles south of Site 42 of Leg 5, the southernmost of a line of sites continuing to the north. The R/V Argo SCAN survey indicated that the area was one of low, broad abyssal hills, 2 to 10 miles in width on E-W profiles, with relatively thick sediment cover.
    Schlagwort(e): 8-70; 8-70A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg8; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 26 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 69
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Tracey, J I; Sutton, George H; Nesteroff, Wladimir D; Galehouse, J S; von der Borch, Christopher C; Moore, T; Lipps, J; Haq, Bilal U; Beckmann, Jean-Pierre (1971): Site 74. In: Tracey, J.I.Jr.; et al., Initial Reports of the Deep Sea Drilling Project, 8, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VIII, 621-674, https://doi.org/10.2973/dsdp.proc.8.109.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 74 is located 250 miles northeast of the Marquesas Islands and lies 270 miles south of Site 73 and 400 miles north of Site 75. It is one of the sites along the N-S line drilled during Leg 8 to investigate the east-west trending accumulation of sediments centered about 2°N near 140°W. Site 74 is located near the center of a relatively flat area about 3 miles across. There is some indication of minor deformation at the site.
    Schlagwort(e): 8-74; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg8; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Pacific/BASIN; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 9 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 70
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    PANGAEA
    In:  Supplement to: Tracey, J I; Sutton, George H; Nesteroff, Wladimir D; Galehouse, J S; von der Borch, Christopher C; Moore, T; Lipps, J; Haq, Bilal U; Beckmann, Jean-Pierre (1971): Site 75. In: Tracey, J.I.Jr.; et al., Initial Reports of the Deep Sea Drilling Project, 8, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VIII, 675-709, https://doi.org/10.2973/dsdp.proc.8.110.1971
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 75 is located 300 miles southeast of the Marquesas Islands; 400 miles south of Site 74. It is the southernmost of the sites along the N-S line drilled during Leg 8 to investigate the east-west trending accumulation of sediments centered about 2°N near 140°W. This site is a replacement for the site at 31°S originally chosen by the JOIDES Pacific Advisory Panel (PAP Site 27). The original site was not drilled since a preliminary R/V Argo SCAN survey indicated insufficient sediment thickness.
    Schlagwort(e): 8-75; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg8; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Pacific/CONT RISE; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 71
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    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 76. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 21-41, https://doi.org/10.2973/dsdp.proc.9.102.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 76 was selected in order to core a thick sequence of sediments north of the Tuamotu ridge that had been crossed by Glomar Challenger justprior to the termination of Leg 8 in Tahiti. Two holes at this site continuously cored 27 meters of lower Pliocene to Recent phillipsitic clay and calcareous nannofossil ooze interbedded with calcareous turbidites. The drill bit was stopped by a silicified calcareous turbidite of Early Pliocene age.
    Schlagwort(e): 9-76; 9-76A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Pacific/PLAIN; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 72
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    PANGAEA
    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 79. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 317-400, https://doi.org/10.2973/dsdp.proc.9.105.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 79 is located on the crest of the equatorial Pacific sediment belt (Ewing and others, 1968) and is the westernmost of a series of sites (79, 81, 82 and 83) that follow the crest of this belt eastward to and across the crest of the oceanic ridge, locally known as the East Pacific Rise. The purpose of these sites is two-fold: 1) to study variations in biostratigraphy and sediment type from west to east across the Pacific and 2) to paleontologically date basement and determine the rate of spreading of the Pacific plate since the time of deposition of the oldest sediments at Site 77.
    Schlagwort(e): 9-79; 9-79A; Comment; Deep Sea Drilling Project; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/VALLEY; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 36 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 73
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    In:  Supplement to: Worzel, J Lamar; Bryant, W R; Beall, A O; Dickinson, K; Laury, R; Smith, L A; McNeely, B; Foreman, H P; Capo, R (1973): Site 86. In: Worzel, J.L.; Bryant, W.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, X, 25-47, https://doi.org/10.2973/dsdp.proc.10.103.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The origin of the Campeche Escarpment in the Gulf of Mexico has been attributed to several causes. Some suggest that the scarp represents a fault scarp, others suggest that its origin is a function of upbuilding and outbuilding likened, in some cases, to that of delta building. Still others suggest that the scarp represents the detrital accumulation seaward of a barrier or reef complex. In order to clarify these possible interpretations, Site 86 was located on a bench at a depth of 780 fathoms in the vicinity of the Campeche Escarpment.
    Schlagwort(e): 10-86; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Gulf of Mexico/BENCH; Identification; Leg10; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 32 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 74
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    PANGAEA
    In:  Supplement to: Hollister, Charles D; Ewing, John I; Habib, Daniel; Lancelot, Yves; Luterbacher, Hanspeter; Paulus, F J; Poag, C Wylie; Wilcoxon, James A; Worstell, Paula J (1972): Site 99: Cat Gap. In: Hollister, C.D.; Ewing, J.I.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XI, 51-73, https://doi.org/10.2973/dsdp.proc.11.102.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: The principal objective at this site was the recovery of Mesozoic sediment and a sample of Horizon B (or basement). The location chosen for drilling is about 40 nautical miles southeast of San Salvador in 4914 meters of water. Aside from the possibility of recovering the oldest Atlantic sediment, drilling at this site was expected to produce interesting samples for comparison stratigraphically and lithologically with those of Holes 4 and 5 of Leg 1.
    Schlagwort(e): 11-99A; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg11; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CHANNEL; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 34 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 75
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    PANGAEA
    In:  Supplement to: Hollister, Charles D; Ewing, John I; Habib, Daniel; Hathaway, James; Lancelot, Yves; Luterbacher, Hanspeter; Paulus, F J; Poag, C Wylie; Wilcoxon, James A; Worstell, Paula J (1972): Site 105: Lower Continental Rise Hills. In: Hollister, C.D.; Ewing, J.I.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XI, 219-312, https://doi.org/10.2973/dsdp.proc.11.106.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: In view of the fact that thick sections of Neocomian and Jurassic limestone were found in the region off the Bahama Islands (Holes 99A, 100 and 101) a hole was selected for drilling between New York and Bermuda at a position where knowledge might be gained about the structure and composition of the lower continental rise hills. In addition, such a hole would ascertain the age of the crust.
    Schlagwort(e): 11-105; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg11; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/HILL; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 76
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    In:  Supplement to: Laughton, Anthony S; Berggren, William A; Benson, Richard N; Davies, Thomas A; Franz, A; Musich, L F; Perch-Nielsen, Katharina; Ruffman, A; van Hinte, Jan E; Whitmarsh, Robert B (1972): Site 111. In: Laughton, A.S.; Berggren, W.A.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 33-159, https://doi.org/10.2973/dsdp.proc.12.103.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: Orphan Knoll is a pronounced submarine feature at the foot of the continental rise and bounded on its northeast side by the 4000-meter deep abyssal plain of the Labrador Basin. It lies isolated on the ocean floor some 550 kilometers northeast of Newfoundland and 350 kilometers north of Flemish Cape. The DSDP drilling site 111 was originally chosen by the Atlantic Advisory Panel on the basis of Charcot's Flexotir continuous seismic profile provided by CNEXO.
    Schlagwort(e): 12-111; 12-111A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg12; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/KNOLL; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 20 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 77
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    PANGAEA
    In:  Supplement to: Laughton, Anthony S; Berggren, William A; Benson, Richard N; Davies, Thomas A; Franz, Ulrich; Musich, L F; Perch-Nielsen, Katharina; Ruffman, A; van Hinte, Jan E; Whitmarsh, Robert B; Bukry, David (1972): Site 113. In: Laughton, A.S.; Berggren, W.A.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 255-311, https://doi.org/10.2973/dsdp.proc.12.105.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: Seismic reflection profiles across the Labrador Sea by Vema-19 and Charcot-S had revealed a rugged basement topography almost entirely buried by sediments up to 2000 meters thick. It was first suggested that this was the median valley of a mid-Labrador Sea ridge where oceanic crust was generated during the last phase of opening of the Labrador Sea but which is now virtually inactive and covered by sediment. The choice of a site where basement could be dated by sampling sediments that were believed to be the same age as the basement was difficult. Site 113 was eventually chosen in a local valley 8 kilometers south of a small knoll believed, from the Vema-ll record, to be a basement high.
    Schlagwort(e): 12-113; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg12; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/VALLEY; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 48 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 78
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    In:  Supplement to: Laughton, Anthony S; Berggren, William A; Benson, Richard N; Davies, Thomas A; Franz, Ulrich; Musich, L F; Perch-Nielsen, Katharina; Ruffman, A; van Hinte, Jan E; Whitmarsh, Robert B; Aumento, Fabrizio; Clarke, A D; Ryall, J R; Cann, Joe R; Bryan, Wilfred B; Bukry, David (1972): Site 118. In: Laughton, A.S.; Berggren, W.A.; et al., Initial Reports of the Deep Sea Drilling Project, 12, Initial Reports of the Deep Sea Drilling Project, 12, U.S. Government Printing Office, XII, 673-751, https://doi.org/10.2973/dsdp.proc.12.109.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: The principle objective at Site 118 was to sample a formation in the Bay of Biscay which had been tentatively ascribed to Lower Cretaceous or older sediments. However it was not clear that this corresponding seismic layer was not in fact part of an extremely irregular igneous basement structure, at least at the western end of the bay.
    Schlagwort(e): 12-118; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg12; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/PLAIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 25 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 79
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    In:  Supplement to: Ryan, William B F; Hsü, Kenneth J; Cita, Maria Bianca; Dumitrica, Paulian; Llort, Jennifer; Maync, Wolf; Nesteroff, Wladimir D; Pautot, Guy; Stradner, Herbert; Wezel, Forese C (1973): Sites 133 and 134. In: Ryan, W.B.F.; Hsu, K.J.; et al., Initial Reports of the Deep Sea Drilling Project, 13, Initial Reports of the Deep Sea Drilling Project, 13, U.S. Government Printing Office, XIII, 465-514, https://doi.org/10.2973/dsdp.proc.13.114.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The western margin of Sardinia (had been explored in the Spring of 1970 by the R/V Jean Charcot of CNEXO. It showed that the basement ridge west of Sardinia lies at the very distal edge of the continental slope and has effectively dammed an upslope sedimentary basin which is presently isolated from the Balearic Abyssal Plain. Consequently a series of holes was contemplated along an east to west transverse of the Charcot profile.
    Schlagwort(e): 13-134E; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/PLAIN; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 9 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 80
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    PANGAEA
    In:  Supplement to: Ryan, William B F; Hsü, Kenneth J; Cita, Maria Bianca; Dumitrica, Paulian; Llort, Jennifer; Maync, Wolf; Nesteroff, Wladimir D; Pautot, Guy; Stradner, Herbert; Wezel, Forese C (1973): Site 126. In: Ryan, W.B.F.; Hsu, K.J.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 219-241, https://doi.org/10.2973/dsdp.proc.13.108.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The single "raison d'être" for selecting Site 126 was to explore the pre-evaporite history of the eastern Mediterranean and hopefully to establish the paleoenvironment which preceded the Late Miocene salinity crisis. The selcetd site is in a deep cleft in the Mediterranean Ridge in the central Ionian Sea, a cleft that cuts more than 250 meters below the level of Horizon M and at the same time is floored by flat-lying sediments. A secondary objective of the cleft site-selection was to ascertain what kind of sediment makes up the horizontal fill and hopefully to determine some details of the history and mechanics of the depression-filling process.
    Schlagwort(e): 13-126; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/RIDGE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 8 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 81
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    In:  Supplement to: Kulm, LaVerne D; von Huene, Roland; Duncan, John R; Ingle, James C; Kling, S A; Musich, L F; Piper, David J W; Pratt, Richard M; Schrader, Hans-Jürgen; Weser, Oscar E; Wise, Sherwood W (1973): Site 172. In: Kulm, L.D.; von Huene, R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVIII, 15-30, https://doi.org/10.2973/dsdp.proc.18.103.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: Site 172 was continuously cored to a depth of 24 meters in a sediment pond 140 kilometers south of the Murray fracture zone. The upper 9 meters consist of a moderate brown pelagic clay which changes to a zeolite-rich brown clay, brown clay zeolitite and zeolitite in the lower 9 to 24 meters. An Early Oligocene (35 to 38 my) nannofossil horizon occurs near an extrusive basalt encountered at 24 meters. These sediments are older than the 29 my age indicated by a recent identification of magnetic anomaly 8 in the "disturbed" zone. The age discrepancy suggests that the magnetic anomalies in the "disturbed" zone are still not identified correctly.
    Schlagwort(e): 18-172; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg18; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 25 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 82
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    In:  Supplement to: Natland, James H (1973): Basal Ferromanganoan Sediments at DSDP Site 183, Aleutian Abyssal Plain, and Site 192, Meiji Guyot, Northwest Pacific, Leg 19. In: Creager, J.S.; Scholl, D.W.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIX, 629-636, https://doi.org/10.2973/dsdp.proc.19.115.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: Basal sediments cored above alkali basalt at Site 183 beneath the Aleutian Abyssal Plain include iron-rich clays, a geothite-bearing calcareous ironstone (23.8% Fe and 4.16% Mn, CaCO3-free), and a pyrite-bearing unfossiliferous aragonitic limestone with 1.95 per cent Sr. At Hole 192A, atop Meiji Guyot, the northernmost of the Emperor Seamounts, five meters of iron and manganese-enriched clays interlayered and diluted with chalk lie on extrusive alkali basalt pillow lavas beneath almost a kilometer of silts, clays, and diatomaceous oozes.
    Schlagwort(e): 19-183; 19-192A; Atomic absorption spectrometry (AAS); Calcium carbonate; Carbon, organic, total; Chromium; Cobalt; Copper; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Lead; Leg19; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/GUYOT; North Pacific/PLAIN; Position; Sample code/label; Sediment type; Strontium; Visual description; Zinc
    Materialart: Dataset
    Format: text/tab-separated-values, 153 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 83
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    In:  Supplement to: Winterer, Edward L; Ewing, John I; Douglas, Robert G; Jarrard, Richard D; Lancelot, Yves; Moberly, Ralph; Moore, Theodore C; Roth, P H; Schlanger, Seymour O (1973): Initial Reports of the Deep Sea Drilling Project 17. U. S. Government Printing Office, XVII, https://doi.org/10.2973/dsdp.proc.17.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The main objectives of Leg 17 were to establish the regional pattern of oceanic crustal ages in the central Pacific, to obtain cores of the entire stratigraphic succession, especially from pre-Middle Eocene strata, To document the history of growth and subsidence of seamounts located along seamount chains, by drilling on the archipelagic apron of sediments near the foot of individual seamounts and to sample acoustic reflectors seen on seismic reflection profiles and to establish their physical properties and their ages.
    Schlagwort(e): 17-164; 17-165A; 17-168; 17-169; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg17; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 103 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 84
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    In:  Supplement to: Burns, Robert E; Andrews, James E; van der Lingen, Gerrit J; Churkin, M; Galehouse, J S; Packham, G H; Davies, Thomas A; Kennett, James P; Dumitrica, Paulian (1973): Initial Reports of the Deep Sea Drilling Project,. U. S. Government Printing Office, XXI, 931 pp, https://doi.org/10.2973/dsdp.proc.21.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The oceanic region between the Tonga-Kermadec Trench and New Zealand to the east and Australia to the west (see map at the back of this volume) has long been regarded as an anomalous region. Prior to development of the plate tectonic theory, it was known that the eastern boundary of the region was tectonically active, the western relatively passive. The DSDP Leg 21 overall objective was to provide initial coring data which would aid in reconstructing the tectonic history and relative plate movements of the Pacific and Indian crustal plates and determining the age of the tectonic features contained within the Tasman Sea region. In particular, the age and biostratigraphy of the oldest Pacific crustal section now being subducted into the Tonga-Kermadec Trench (Site 204) and the age and composition of the South Fiji Basin and of the basement rock (Site 205).
    Schlagwort(e): 21-204; 21-205; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg21; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Pacific/BASIN; South Pacific/TRENCH; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 36 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 85
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    In:  Supplement to: Heezen, Bruce C; MacGregor, Ian D; Foreman, H P; Forristall, G; Hekel, H; Jones, E J W; Kaneps, Ansis G; Krasheninnikov, Valery A; Okada, H; Ruef, Michael R (1973): The Post-Jurassic Sedimentary Sequence on the Pacific Plate; a Kinematic Interpretation Of Diachronous Deposits. In: Heezen, B.C.; MacGregor, I.D., Initial Reports of the Deep Sea Drilling Project, 20, Initial Reports of the Deep Sea Drilling Project, 20, U.S. Government Printing Office, XX, 725-738, https://doi.org/10.2973/dsdp.proc.20.133.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The sea floor of the western Pacific is covered by five stratigraphic units: (l)an eastward thinning wedge of late Tertiary silty clay, primarily of volcanic origin, (2) a Cretaceous to Tertiary zeolitic red clay, (3) a Late Cretaceous to Tertiary chalk/chert sequence, (4) a Cretaceous clay, and (5) a basal chalk/chert sequence. The basal chalk was deposited on the young crust at the crest of the mid-oceanic ridge, while the upper chalk was deposited beneath the equator, and the abyssal clays were deposited in abyssal depths in mid latitudes. A kinematic model has been constructed that outlines the deposition of these units on growing crust, which not only was displaced westward away from the accretion center of the mid-oceanic ridge, but northward under the equator. The average northward component of motion for the Pacific plate has been 2 cm per year from 0 to 30 m.y. and 4.4 cm per year from 30 to 100 m.y. The deep-sea deposits of the Pacific are basically and systematically time transgressive. Claims of general synchroneity for either lithostratigraphy or acoustostratigraphy are rejected as inconsistent with both the drilling data and the kinematic model of Pacific pelagic stratigraphy. A few more well sampled holes in the ancient Pacific plate combined with an appropriately refined kinematic model should yield a 'rather detailed history of the Pacific plate since the Jurassic.
    Schlagwort(e): 20-195; 20-196; 20-198A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg20; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 128 data points
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  • 86
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    In:  Supplement to: Pimm, Anthony C (1974): Sedimentology and History of the Northeastern Indian Ocean from Late Cretaceous to Recent. In: von der Borch, C.C.; Sclater, J.G.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXII, 717-803, https://doi.org/10.2973/dsdp.proc.22.139.1974
    Publikationsdatum: 2023-08-28
    Beschreibung: Eight sites were drilled on Leg 22 in the northeastern Indian Ocean. Three sites (214, 216, 217) on Ninetyeast Ridge penetrated a thick sequence of mostly Tertiary calcareous oozes passing down into shallow-water sediments with volcanogenic material in Sites 214 and 216. The age of the basal sequence increases northwards from Paleocene (214) through Maastrichtian (216) to Campanian (217). A nonmarine sequence of volcanoclastics and lignite overlies basalt at 214. Drilling terminated in a dolomite chert sequence at 217 before bsalt was encountered. Two sites (213, 215), in deep water on either side of Ninetyeast Ridge, showed calcareous ooze of Paleocene to early Eocene age overlying basalt passing up into brown clay and finally siliceous ooze of late Miocene and younger age. A major hiatus centered in the Oligocene occurs at both these sites. One site (212), drilled in the deepest part of the Wharton Basin, penetrated a brown clay sequence interbedded with several thick calcareous units, each of a very short time duration. Evidence from sedimentary structures and calcareous microfossils.
    Schlagwort(e): 22-212; 22-213; 22-215; 22-216; 22-217; 22-217A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//BASIN; Indian Ocean//RIDGE; Leg22; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 122 data points
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  • 87
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    In:  Supplement to: Berger, Wolfgang H; von Rad, Ulrich (1972): Cretaceous and Cenozoic Sediments from the Atlantic Ocean. In: Hayes, D.E.; Pimm, A.C.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIV, 787-954, https://doi.org/10.2973/dsdp.proc.14.126.1972
    Publikationsdatum: 2023-08-28
    Beschreibung: Leg 14 of the Deep Sea Drilling Project completed 9 holes; 7 were located off NW Africa, 1 in Ceara Abyssal Plain, and 1 on Demerara Rise. Quaternary and Pliocene sediments consist of nanno chalk oozes and brown clay. The facies boundary (CCD) is near 5000 meters. Sedimentation rates are between 10 and 30 meters/million years (m/My) for chalk ooze and 2 to 4 m/My for pelagic clay. Redeposition off the Amazon produces terrigenous and bioclastic turbidite sequences with rates increasing, on the average, from 50 to 150 m/My. Small manganese nodules (coarse sand and small pebbles) are common in sediments associated with hiatuses at Sites 135 (Eocene-Miocene, Core SW1), 136 (Late Cretaceous- Miocene, Cores 3 to 6), and to a lesser extent at 141 (Middle Miocene-Pliocene, Core 7). Additional occurrences were noted in the pelagic clays at Site 137 (Late Cretaceous to Miocene). At 135-8 (Cenomanian) micro-nodules occur within a mixture of siltstone fragments, compressed planktonic foraminifera, fish debris, as well as chert pebbles and other redeposited components. Manganese concretions are generally younger than Turonian and are restricted to the predominantly oxidized part of the sequences, that is, where sediments are mostly red, brown, or yellow-colored.
    Schlagwort(e): 14-135; 14-136; 14-137; 14-141; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg14; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/DIAPIR; North Atlantic/HILL; North Atlantic/PLAIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 72 data points
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  • 88
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    In:  Supplement to: Cronan, David S; Damiani, Theresa; Kinsman, D J J; Thiede, Jörn (1974): Sediments from the Gulf of Aden and Western Indian Ocean. In: Fisher, R.L.; Bunce, E.T.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXIV, 1047-1110, https://doi.org/10.2973/dsdp.proc.24.127.1974
    Publikationsdatum: 2023-08-28
    Beschreibung: During Leg 24 three drilling sites were occupied in the Gulf of Aden (231, 232, 233), two in the Somali Basin (234, 235), and three in the western Indian Ocean (236, 237, 238). The location of these sites is shown in Figure 1; latitude, water depth, and penetration depth are indicated in Table 1. Figure 2 summarizes the lithologies and stratigraphy of all eight sites cored. In this chapter are included lithologic summaries for each of the sites. The sediments are then discussed in terms of their individual biogenic, terrigenous, volcanogenic, or authigenic components and their sedimentary structures. In a series of synthesis sections the hemipelagic, pelagic, and basal metaliferous sedimentary facies are discussed.
    Schlagwort(e): 24-234; 24-238; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//FRACTURE ZONE; Indian Ocean//RIDGE; Leg24; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 57 data points
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  • 89
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    In:  Supplement to: Leclaire, Lucien (1974): Late Cretaceous and Cenozoic Pelagic DepositsPaleoenvironment and Paleooceanography of the Central Western Indian Ocean. In: Simpson, E.S.W.; Schlich, R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXV, 481-513, https://doi.org/10.2973/dsdp.proc.25.120.1974
    Publikationsdatum: 2023-08-28
    Beschreibung: Pelagic deposits are the dominant contributors to the sediment layers that blanket ridges and basaltic sea floor in deep basins. Among pelagic constituents, nannofossils undoubtedly are the predominant contributor, especially to Cenozoic chalk and ooze. Among Leg 25 sites, the most typical pelagic deposits are found in the Madagascar Basin (Site 245) including a clayey nanno chalk, bearing Fe-Mn oxides, resting directly on the basalt and overlain successively by a nanno chalk which is interlayered with chert and devitrified volcanic ash and a nearly pure nanno ooze. The lithologic sequence is capped by brown clay. Upper Cenozoic foram sand and foram nanno ooze were found on the Mozambique Ridge (Site 249) and particularly on the Madagascar Ridge (Site 246). Biogenic silica-rich facies are rare and mainly located near the top of the lowest latitude sites.
    Schlagwort(e): 25-239; 25-242; 25-245; 25-245A; 25-248; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//BASIN; Indian Ocean//CHANNEL; Leg25; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 77 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 90
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    In:  Supplement to: Doyle, Patricia S; Boltovskoy, Esteban; Herb, Rene C; Thierstein, Hans R; Hyndman, Roy D; Horvath, George J; Leidy, Rosanne D; McKelvey, Barrie C; Kempe, D R C; Rodolfo, Kelvin S; Davies, Thomas A; Luyendyk, Bruce P (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVI, 1129 pp, https://doi.org/10.2973/dsdp.proc.26.1974
    Publikationsdatum: 2023-08-28
    Beschreibung: DSDP Leg 26, is the fifth cruise of D/V Glomar Challenger in the Indian Ocean, and the first cruise of Phase III of the Deep Sea Drilling Project. The Indian Ocean is the smallest of the three major ocean basins but appears to be geologically the most complex. The sites drilled on Leg 26 were selected to try to elucidate a number of specific problems of both local and broad regional significance, as well as to add to the general knowledge of the area. In particular: a) To locate the oldest sediment in the Indian Ocean and thus possibly the date of the initial breakup of Gondwanaland (Sites 250, 256, 257); b) To determine the effects of the initiation of the Circumpolar Current on southern Indian Ocean sedimentation (Sites 250, 252, 256, 257, 258); c) To determine the history of spreading of the Southwest Branch of the Indian Ocean Ridge and the history of the crust and oceanic sedimentation in that general region (Sites 250, 251, 252).
    Schlagwort(e): 26-250A; 26-252; 26-256; 26-257; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//BASIN; Leg26; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 91
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    In:  Supplement to: Robinson, Paul T; Thayer, Julie A; Cook, Peter J; McKnight, Brian K (1974): Lithology of Mesozoic and Cenozoic Sediments of the Eastern Indian Ocean, Leg 27, Deep Sea Drilling Project. In: Veevers, J.J.; Heirtzler, J.R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVII, 1001-1047, https://doi.org/10.2973/dsdp.proc.27.148.1974
    Publikationsdatum: 2023-08-28
    Beschreibung: During Leg 27 five sites were drilled in the eastern Indian Ocean, four in abyssal plains near the western margin of Australia and one in the Timor Trough. Abyssal plain sediments are divided into two major units: (1) a lower, acoustically transparent layer of relatively uniform thickness draped over basaltic basement and (2) a horizontally layered sequence of highly variable thickness filling low areas on the surface of the transparent layer. The transparent layer, ranging in age from Upper Jurassic to Upper Cretaceous, consists chiefly of dark gray, siliceous clays and claystones with minor zeolitic clay and nannofossil ooze. Sedimentation rates are between 5 and 30 m/m.y. being highest in the Lower Cretaceous. Upper Cretaceous sediment are sparse or absent. The relatively high sedimentation rates for pelagic clay are probably due to the proximity of the Australian continent. The layered unit consists of calcareous oozes and lesser zeolitic clay and radiolarian ooze, all of Cenozoic age. Many of the oozes contain shallow-water foraminifers and graded sequences suggesting deposition by mass transport.
    Schlagwort(e): 27-259; 27-261; 27-263; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//PLAIN; Leg27; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 92
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    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Matthews, J L; Catalano, Giulio; Natland, James H; Coogan, Laurence A; Tharp, Mary; Rawson, M (1973): Western Pacific Guyots. In: Heezen, B.C.; MacGregor, I.D., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XX, 653-723, https://doi.org/10.2973/dsdp.proc.20.132.1973
    Publikationsdatum: 2023-08-28
    Beschreibung: The sea floor of the western Pacific is covered by five stratigraphic units: (l) an eastward thinning wedge of late Tertiary silty clay, primarily of volcanic origin, (2) a Cretaceous to Tertiary zeolitic red clay, (3) a Late Cretaceous to Tertiary chalk/chert sequence, (4) a Cretaceous clay, and (5) a basal chalk/chert sequence. The basal chalk was deposited on the young crust at the crest of the mid-oceanic ridge, while the upper chalk was deposited beneath the equator, and the abyssal clays were deposited in abyssal depths in mid latitudes. A kinematic model has been constructed that outlines the deposition of these units on growing crust, which not only was displaced westward away from the accretion center of the mid-oceanic ridge, but northward under the equator. The average northward component of motion for the Pacific plate has been 2 cm per year from 0 to 30 m.y. and 4.4 cm per year from 30 to 100 m.y. The deep-sea deposits of the Pacific are basically and systematically time transgressive. Claims of general synchroneity for either lithostratigraphy or acoustostratigraphy are rejected as inconsistent with both the drilling data and the kinematic model of Pacific pelagic stratigraphy. A few more well sampled holes in the ancient Pacific plate combined with an appropriately refined kinematic model should yield a 'rather detailed history of the Pacific plate since the Jurassic.
    Schlagwort(e): ARIES; ARIES-005D; ARIES-019D; ARIES-022D; ARIES-025D; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Substrate type; Thomas Washington; Uniform resource locator/link to image; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 93
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    In:  Supplement to: Aumento, Fabrizio (1970): Petrological, geochemical and geophysical studies of rocks dredged from the mid-Atlantic Ridge at 45 °N. AOL Data Series, Bedford Institute of Oceanography, Canada; www.dfo-mpo.gc.ca/Library/58126_v1_pt1.pdf and www.dfo-mpo.gc.ca/Library/58126_v1_pt2.pdf, 5-D (1+2), 598 pp, https://store.pangaea.de/Projects/NOAA-MMS/58126_v1_pt2.pdf
    Publikationsdatum: 2023-08-28
    Beschreibung: The data presented in this report is the result of investigations carried out by a number of laboratories on a suite of rocks dredged from the Mid - Atlantic Ridge at 45°N by F. Aura en to and K. S. Manchester during the three Bedford Institute cruises BI 19-66 Hudson, BI 22-68 Hudson, and BI 23-68 Theta.
    Schlagwort(e): Atlantic Ocean; BI19-66-Phase2; BI22-68-Phase4; BI23-68-Phase2; BI23-68-Phase3; BI23-68-Phase5; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; File name; HUD66/19-1; HUD66/19-1C; HUD68/22-103; HUD68/22-106; HUD68/22-108; HUD68/22-112; HUD68/22-116; HUD68/22-120; HUD68/22-123; HUD68/22-128; HUD68/22-133; HUD68/22-134; Hudson; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Size; Substrate type; Theta; THT68/23-5; THT68/23-6; THT68/23-8; Uniform resource locator/link to image; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 186 data points
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  • 94
    Publikationsdatum: 2023-08-28
    Schlagwort(e): AL34200; AL34900; AL42100; AL42300; AL42700; AL43100; AL44500; ALV342; ALV-342; ALV349; ALV-349; ALV421; ALV-421; ALV423; ALV-423; ALV427; ALV-427; ALV431; ALV-431; ALV445; ALV-445; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Event label; Grab; GRAB; Gulf of Maine, Atlantic Ocean; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 95
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    In:  Supplement to: Krishnaswami, Seth; Moore, Willard S (1973): Accretion Rates of Freshwater Manganese Deposits. Nature Physical Science, 243(129), 114-116, https://doi.org/10.1038/physci243114a0
    Publikationsdatum: 2023-08-28
    Beschreibung: 2 nodules, one spherical, similar to 2 cm diameter form L. Alstern, Sweden the other saucer-shaped, similar to 2 cm thick from L. Oneida, New York were studied by using 228Ra and super(210)pb in order to measure accretion rates in the range 100-1000 mm/10 super(3) year. The deduced rates are 1.4 and 2.6 mm/ 10 super(3) year. Respectively. The author discuss the problems of how deep sea noducles stay at the sediment-water interface when the sediment around them is accumulating 1000 times faster than the nodules themselves.
    Schlagwort(e): Alstern_K; Atomic absorption spectrometry (AAS); Barium; Beta radiometer; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; DIVER; Event label; Identification; Lake Alstern, Sweden; Lead-210; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oneida Lake, NY, USA; Oneida-Lake-SP; Radium-226; Sampling by diver
    Materialart: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 96
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    In:  Supplement to: Bowles, F A; Angino, E A; Hosterman, J W; Galle, O K (1971): Precipitation of deep-sea palygorskite and sepiolite. Earth and Planetary Science Letters, 11(1-5), 324-332, https://doi.org/10.1016/0012-821X(71)90187-7
    Publikationsdatum: 2023-08-28
    Beschreibung: Five of 34 dredge hauls taken in the Atlantic Ocean recovered a material tentatively described on shipboard as a salmon-colored clay. X-ray diffraction analysis showed the clay material to consist principally of palygorskite. Occurring with the palygorskite are quartz, calcite, and dolomite. It is suggested that the palygorskite (and sepiolite) is the result of chemical precipitation brought about by the reaction of hydrothermal solutions with sea water.
    Schlagwort(e): Atlantic Ocean; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; File name; Identification; KA68J; KA68J-RD15; KA68J-RD2; KA68J-RD20; KA68J-RD34; KA68J-RD4; Kane; Latitude of event; Longitude of event; 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
    Materialart: Dataset
    Format: text/tab-separated-values, 47 data points
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  • 97
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    In:  Supplement to: Fein, Charles D; Morgenstein, Maury (1973): Microprobe analysis of manganese crusts from the Hawaiian Archipelago. In: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, IDOE, NSF, Washington D.C., USA - http://catalog.hathitrust.org/Record/005761114 (pdf 733 kB), 85-92, https://store.pangaea.de/Projects/NOAA-MMS/Fein_1973_IDOE.pdf
    Publikationsdatum: 2023-08-28
    Beschreibung: Quantitative and qualitative chemical analyses were performed on fourteen manganese nodules and crusts from the Waho Shelf. The analyses showed that submarine weathering has leached several elements, notably Si02, A1203, Na20, CaO and MnO from the hydrated glass surrounding the basaltic seeds of the nodules. The altered glass was enriched in Ti02, MgO, K2O and total Fe. The manganese bands formed on the altered glass were further depleted in Si02, Al203, and similar to the hydrated glass in Na2O and CaO content. The manganese-enriched zones also showed higher TiO2 and NiO than the basaltic seeds, and higher total Fe than pelagic nodules from the North Pacific. Qualitative measurement of Cu, Ni, and Co, showed relative enrichment in the manganese bands. A proposed model for manganese accretion in the Waho Shelf incorporates local submarine weathering of basalts, redistribution of Mn in marine sediments, and an influx of Mn "rain" on the sea floor.
    Schlagwort(e): Aluminium oxide; Calcium oxide; Calculated; Chromium(III) oxide; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Electron microprobe (EMP); Elevation of event; Event label; Hawaii islands; Identification; Iron oxide, FeO; Kauai_Sediments-Exped; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium oxide; Silicon dioxide; Sodium oxide; TE6-1RD; TE7-3RD; TE7-4RD; TE8-1RD; TE8-5RD; TE8-7RD; Teritu; Titanium dioxide; Water in rock; Zone
    Materialart: Dataset
    Format: text/tab-separated-values, 176 data points
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  • 98
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    In:  Supplement to: Landmesser, Charles W; Morgenstein, M (1973): Survey and mapping of manganese deposits in the Hawaiian archipelago. In: Symposium on the Origin and Distribution of Managanese Nodules in the Pacific and Prospects for Exploration. Seabed Assessment Program, IDOE, NSF, Washington D.C. Honolulu, Hawaï, 93-101, https://store.pangaea.de/Projects/NOAA-MMS/Landmesser_1973.pdf
    Publikationsdatum: 2023-08-28
    Beschreibung: Detailed mapping of manganese deposits in the Kauai Channel and on the Waho Shelf adjacent to the northwest corner of Oahu is near completion. Manganese crusts and nodules are concentrated on submarine terraces between 800 and 2400 meters deep. Similarities In the geomorphology and sedimentary conditions where extensive manganese deposits are present suggest that these are primary factors controlling manganese distribution in the Hawaiian Archipelago. This information may be useful for guiding future surveys, and the technology developed for studiesiIn the Hawaiian Archipelago may have application to other areas of high topographic relief and low sediment thickness (i.e., seamounts, fracture zones, fault scarps, ridges, etc.).
    Schlagwort(e): Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; File name; Hawaii islands; Identification; Kauai_Sediments-Exped; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Size; Substrate type; TE7-3RD; TE8-4RD; TE8-7RD; TE8-8RD; Teritu; Uniform resource locator/link to image; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 99
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    In:  Hawaii Institute of Geophysics & Planetology, University of Hawaii
    Publikationsdatum: 2023-08-28
    Beschreibung: This report presents barrel descriptions of deep-sea sediment cores obtained by the Hawaii Institute of Geophysics on cruises of the R/V Mahi during 1970 in the western Pacific Ocean. Many of the cores provided useful preliminary observations for later detailed surveys of drilling sites for the Deep-Sea Drilling Project in the southwest Pacific.
    Schlagwort(e): Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Event label; Identification; Mahi; Mahi-70-04-22; MAHI70-100RD; MAHI70-28RD; MAHI70-PC-89; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Size; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 21 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 100
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    PANGAEA
    In:  Hawaii Institute of Geophysics & Planetology, University of Hawaii
    Publikationsdatum: 2023-08-28
    Beschreibung: This report represents the first in a projected series reporting core descriptions and their physical properties, to be made available through routine core handling procedures instituted at the Hawaii Institute of Geophysics in 1968 to keep pace with the capability to take long (120-foot) piston cores from the University of Hawaii's R/V MAHI. The data reported herein cover sediment cores collected during 1967, 1968, and 1969 in the region of the Solomon Islands and the Darvir. Rise, and along the central portion of the Murray Fracture Zone.
    Schlagwort(e): ABHI68-PC001; ABHI68-PC002; ABHI68-PC003; ABHI68-PC004; ABHI68-PC024; ABHI68-PC025; ABHI68-PC029; ABHI68-PC031; ABHI68-PC033; ABHI68-PC034; ABHI68-RD1; ABHI68-RD2; ABHI68-RD6; ABHI68-RD8; AbyssalHills_68; Age, comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; GC; Gravity corer; Identification; Latitude of event; Longitude of event; Mahi; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; SOLI67-GC-009; SOLI68-RD24; SOLI68-RD26; SOLI68-RD27; SOLI68-RD3; SOLI68-RD32; SOLI68-RD33; SOLI68-RD6; Solomon Islands_67; Solomon Islands_68; Substrate type; Visual description
    Materialart: Dataset
    Format: text/tab-separated-values, 350 data points
    Standort Signatur Erwartet Verfügbarkeit
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