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  • Data  (595)
  • 1975-1979  (584)
  • 1945-1949  (11)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Fechter, Rosina (1979): Gastropoden aus der Iberischen Tiefsee. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D30, 23-40
    Publication Date: 2023-07-10
    Description: During the cruises 3 and 15 of R.V. "Meteor", representatives of 7 families of benthic abyssal gastropods were collected. The prevalent group was the Turridae; the Naticidae are represented by 2 species, the remaining families by a single species each. A survey of the frequency and distribution of the species within the study area is given. A systematic part deals with the individual species in detail, including notes on taxonomy, material and distribution. Concerning the composition of the abyssal gastropod fauna of the present material, Neogastropoda are 4 times as many as Archaeogastropoda and 6 times as many as Mesogastropoda and Opisthobranchia. 89 % of all specimens are Neogastropoda. Usually deep-sea organisms have a non-pelagic development, but many of the Iberian deep-sea Turrids have a planktotrophic protoconch, that means a long pelagic larval period. Among the 19 species, 2 are cosmopolitan, 9 show a transatlantic distribution and 8 are confined to East-Atlantic basins.
    Keywords: Agassiz Trawl; AGT; Belomitra quadrunplex; Benthomangelia sp.; Cocculina aff. C. pusilla; Cyclostrema richardi; Cylichnium oliviformis; DEPTH, water; Event label; Gymnobela engonia; Iberian deep sea; Latitude of event; Longitude of event; M15; M15_024; M15_025; M3; M3/1_024; M3/1_030; M3/1_037; M3/1_038; Meteor (1964); Neverita cf. nana; Number of species; Phymorhynchus alberti; Pleurotomella (Theta) bathyiberica; Pleurotomella (Theta) lyronuclea; Pleurotomella bruneri; Pleurotomella catherinae; Pleurotomella packardi; Pleurotomella phyxanor; Pleurotomella sandersoni; Pleurotomella tincta; Polinices (Euspira) aff. P. agujanus; Seguenzia elegans; Shannon Diversity Index; Turbonilla sp.
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Wood, D A; Tarney, J; Varet, J; Saunders, Andrew D; Bougault, Henri; Joron, Jean Louis; Treuil, M; Cann, Joe R (1979): Geochemistry of basalts drilled in the North Atlantic by IPOD Leg 49: implications for mantel heterogeneity. Earth and Planetary Science Letters, 42(1), 77-97, https://doi.org/10.1016/0012-821X(79)90192-4
    Publication Date: 2023-07-10
    Description: IPOD Leg 49 recovered basalts from 9 holes at 7 sites along 3 transects across the Mid-Atlantic Ridge: 63°N (Reykjanes), 45°N and 36°N (FAMOUS area). This has provided further information on the nature of mantle heterogeneity in the North Atlantic by enabling studies to be made of the variation of basalt composition with depth and with time near critical areas (Iceland and the Azores) where deep mantle plumes are thought to exist. Over 150 samples have been analysed for up to 40 major and trace elements and the results used to place constraints on the petrogenesis of the erupted basalts and hence on the geochemical nature of their source regions. It is apparent that few of the recovered basalts have the geochemical characteristics of typical "depleted" midocean ridge basalts (MORB). An unusually wide range of basalt compositions may be erupted at a single site: the range of rare earth patterns within the short section cored at Site 413, for instance, encompasses the total variation of REE patterns previously reported from the FAMOUS area. Nevertheless it is possible to account for most of the compositional variation at a single site by partial melting processes (including dynamic melting) and fractional crystallization. Partial melting mechanisms seem to be the dominant processes relating basalt compositions, particularly at 36°N and 45°N, suggesting that long-lived sub-axial magma chambers may not be a consistent feature of the slow-spreading Mid-Atlantic Ridge. Comparisons of basalts erupted at the same ridge segment for periods of the order of 35 m.y. (now lying along the same mantle flow line) do show some significant inter-site differences in Rb/Sr, Ce/Yb, 87Sr/86Sr, etc., which cannot be accounted for by fractionation mechanisms and which must reflect heterogeneities in the mantle source. However when hygromagmatophile (HYG) trace element levels and ratios are considered, it is the constancy or consistency of these HYG ratios which is the more remarkable, implying that the mantle source feeding a particular ridge segment was uniform with respect to these elements for periods of the order of 35 m.y. and probably since the opening of the Atlantic. Yet these HYG element ratios at 63°N are very different from those at 45°N and 36°N and significantly different from the values at 22°N and in "MORB". The observed variations are difficult to reconcile with current concepts of mantle plumes and binary mixing models. The mantle is certainly heterogeneous, but there is not simply an "enriched" and a "depleted" source, but rather a range of sources heterogeneous on different scales for different elements - to an extent and volume depending on previous depletion/enrichment events. HYG element ratios offer the best method of defining compositionally different mantle segments since they are little modified by the fractionation processes associated with basalt generation.
    Keywords: 49-407; 49-408; 49-409; 49-410; 49-410A; 49-411; 49-412A; 49-413; Aluminium oxide; Caesium; Calcium oxide; Carbon dioxide; Cerium; Chromium; Cobalt; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Europium; Event label; Gadolinium; Glomar Challenger; Hafnium; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Latitude of event; Leg49; Longitude of event; Lutetium; Magnesium number; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Niobium; North Atlantic/BASIN; North Atlantic/FRACTURE ZONE; North Atlantic/RIDGE; Phosphorus pentoxide; Potassium oxide; Rubidium; Samarium; Sample code/label; Sample code/label 2; Scandium; Silicon dioxide; Sodium oxide; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Water in rock; X-ray fluorescence (XRF); Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 722 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Andres, Hans Georg (1977): Gammaridea (Crustacea, Amphipoda) aus dem Iberischen Tiefseebecken. Auswertung des Materials der Fahrten 3 und 15 von F.S. "Meteor". Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D25, 54-67
    Publication Date: 2023-07-10
    Description: Four species of gammaridean Amphipoda are recorded from the Iberian deep sea basin at about 5000 m depth: Bathyceradocus iberiensis sp. n., Paracallisoma platepistomum sp. n., Parandaniexis cf. mirabilis Schellenberg, 1929, and Paragissa galatheae Barnard, 1961. The biology of the four species is discussed.
    Keywords: Agassiz Trawl; AGT; Bathyceradocus iberiensis; Counting; Date/Time of event; DEPTH, water; Event label; Iberian deep sea; Latitude of event; Longitude of event; M15; M15_025; M3; M3/1_024; M3/1_030; M3/1_037; M3/1_038; Meteor (1964); Paracallisoma platepistomum; Parandaniexis cf. mirabilis; Parargissa galathea
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Riegraf, Wolfgang (1978): Benthonische Schelf-Foraminiferen aus dem Valanginium-Hauterivium (Unterkreide) des Indischen Ozeans südwestlich Madagaskar (Deep Sea Drilling Project Leg 25, Site 249). Geologische Rundschau, 78(3), 1047-1061, https://doi.org/10.1007/BF01829334
    Publication Date: 2023-07-10
    Description: From 12 radiolarian-rich claystone samples of the DSDP-Leg 25, Site 249, situated in the western Indian Ocean southwest of Madagascar 4 species of agglutinated and 38 species of calcareous benthonic foraminifera are described, 13 of them in open nomenclature. As a lot of Valanginian species and Gavelinella barremiana occur in the foraminiferal faunas described here a Valanginian-Hauterivian age is assigned to them. These microfaunas investigated here yield some index species characteristic in the Lower Cretaceous deposits of Northern Germany and also from the near-by Madagascar. Nodosariids dominate in a striking way with 36 species, especially of Astacolus, Citharina, Lenticulina, Lingulina, Marginulinopsis, Nodosaria, Saracenaria, and Vaginulina. Important Neocomian species well-known from other DSDP sites, namely Praedorothia ouachensis (SIGAL) and planktonic foraminifers, are missing. The microfaunas of Site 249 have to be derived from shelf areas.
    Keywords: 25-249; Ammobaculites sp.; Astacolus cephalotes; Astacolus microdictyotus; Citharina harpa; Citharina sp.; Citharina truncata; Deep Sea Drilling Project; Dentalina debilis; Dentalina sp.; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eoguttulina bilocularis; Fish remains; Foraminifera, benthic; Gavelinella barremiana; Globulina bucculenta; Glomar Challenger; Glomospirella gaultina; Indian Ocean//RIDGE; Leg25; Lenticulina nodosa; Lenticulina roemeri; Lenticulina saxonica; Lingulina biformis; Lingulina lamellata; Lingulina semiornata; Lingulina sp.; Lithologic unit/sequence; Marginulina caelata; Marginulina inaequalis; Marginulinopsis bettenstaedti; Marginulinopsis matutina; Nodosaria obscura; Nodosaria sp.; Ophiuroidea remains; Ostracoda; Paalzowella feifeli; Palmula crepidularis; Palmula malakialinensis; Palmula sp.; Porifera spiculae; Pseudonodosaria humilis; Radiolarians abundance; Ramulina tappanae; Reophax aff. eckernex; Reophax sp.; Sample code/label; Saracenaria crassicosta; Saracenaria lutanata; Tristix acutangulus; Vaginulina recta
    Type: Dataset
    Format: text/tab-separated-values, 600 data points
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Ellis, C Howard; Lohman, William H (1979): Neogene calcareous nannoplankton biostratigraphy in eastern Mediterranean deep-sea sediments (DSDP Leg 42A, Sites 375 and 376). Marine Micropaleontology, 4, 61-84, https://doi.org/10.1016/0377-8398(79)90006-9
    Publication Date: 2023-07-10
    Description: Calcareous nannoplankton biostratigraphy has been worked out in the eastern Mediterranean utilizing deep-sea sediments recovered from DSDP Leg 42A Sites 375 and 376. These two drill sites were located approximately 55 km west of Cyprus on the Florence Rise. Sediments, ranging in age from early Miocene (Helicosphaera ampliaperta Zone) through Holocene, contain sufficient age-diagnostic species to recognize essentially all of the lowlatitude nannoplankton zones described by Bukry, although regional, secondary marker species are needed to define some zonal boundaries. Reworked Cretaceous and Paleogene nannoplankton occur throughout the stratigraphic interval studied, but not in quantities large enough to mask indigenous species. Sedimentation rates at Sites 375 and 376 were highest in the late Miocene and late Pleistocene. Open-marine, warm-water species of discoasters are present in significant numbers throughout the Miocene and Pliocene. Earliest Pliocene assemblages contain numerous specimens of ceratoliths. Nannoplankton in post-Messinian sediments at the drill sites and the Zanclean stratotype at Capo Rossello, Sicily, indicate that the base of the Amaurolithus tricorniculatus Zone (base of Triquetrorhabdulus rugosus Subzone) corresponds with the Miocene-Pliocene boundary.
    Keywords: Amaurolithus amplificus; Amaurolithus delicatus; Amaurolithus primus; Amaurolithus tricorniculatus; Angulolithina arca; Arkhangelskiella cymbiformis; Braarudosphaera bigelowii; Broinsonia parca; Capo_Rossello; Ceratolithus acutus; Ceratolithus rugosus; Chiasmolithus grandis; Chiasmolithus sp.; Coccolithus miopelagicus; Coccolithus pelagicus; Coronocyclus nitescens; Cretarhabdus crenulatus; Cribrosphaera ehrenbergii; Cyclicargolithus abisectus; Cyclicargolithus floridanus; Cyclococcolithus leptoporus; Cyclococcolithus macintyrei; Dictyococcites bisectus; Discoaster asymmetricus; Discoaster barbadiensis; Discoaster bellus; Discoaster binodosus; Discoaster bollii; Discoaster braarudii; Discoaster brouweri; Discoaster challengerii; Discoaster deflandrei; Discoaster divaricatus; Discoaster druggii; Discoaster intercalaris; Discoaster lautus; Discoaster lodoensis; Discoaster loeblichii; Discoaster multiradiatus; Discoaster obtusus; Discoaster pentaradiatus; Discoaster quinqueramus; Discoaster sp.; Discoaster sp. cf. D. quinquenamus; Discoaster stellulus; Discoaster surculus; Discoaster variabilis; Discolithina japonica; Discolithina multipora; Discolithina sp.; Eiffellithus eximius; Eiffellithus turriseiffelii; Gartnerago obliquum; Helicosphaera ampliaperta; Helicosphaera carteri; Helicosphaera euphratis; Helicosphaera intermedia; Helicosphaera sellii; Isthmolithus recurvus; Italy; Lithostromation perdurum; Micrantholithus entaster; Micrantholithus sp.; Microrhabdulus decoratus; Micula staurophora; Nannofossil zone; ORDINAL NUMBER; OUTCROP; Outcrop sample; Parhabdolithus embergeri; Prediscosphaera cretacea; Reticulofenestra hillae; Reticulofenestra pseudoumbilicus; Reticulofenestra umbilicus; Rhabdosphaera procera; Rhabdosphaera sp.; Scapholithus fossilis; Scyphosphaera apsteinii; Scyphosphaera globulata; Scyphosphaera intermedia; Scyphosphaera pulcherrima; Scyphosphaera sp.; Sphenolithus abies; Sphenolithus distentus; Sphenolithus heteromorphus; Sphenolithus moriformis; Sphenolithus neoabies; Sphenolithus predistentus; Sphenolithus radians; Tetralithus aculeus; Tetralithus nitidus; Tetralithus trifidus; Thoracosphaera sp.; Triquetrorhabdulus carinatus; Triquetrorhabdulus rugosus; Triquetrorhabdulus sp.; Umbilicosphaera cricota; Vagalapilla octoradiata; Watznaueria barnesae; Watznaueria gronosa; Zygodiscus deflandrei; Zygodiscus sp.; Zygrhablithus bijugatus
    Type: Dataset
    Format: text/tab-separated-values, 2254 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Mostafavi, Nasser (1978): Die Gattung Hinia (Nassariidae, Gastropoda) im Tertiär NW-Deutschlands. Meyniana, 30, 29-53, https://doi.org/10.2312/meyniana.1978.30.29
    Publication Date: 2023-07-10
    Description: The genus Hinia is divided in 4 subgenera; other subgenera are not represented in the area studied. It was possible to find criteria for a better discrimination of the highly variable species H. (Hinia) schlotheimi and H. (Hinia) turbinella. The species "fuchsi" has been placed in the synonymy of H. (Hinia) turbinella. The species H. (Hinia) schlotheimi (BEYRICH) and H. (Telasco) schroederi (KAUTSKY) have been united under the name H. (Hinia) schlotheimi. The easily distinguishable species H. (Tritonella) tenuistriata and H. (Hinia) sulcata belong to two different genera. H. (Tritonella) cimbrica andersoni of the Viol- and Katzheide-Beds (Reinbek-stage) is separable from the population found in the Hemmoor-stage, it turned out to be a valuable guide subspecies for the Reinbek-stage. The species H. (Tritonella) serraticosta, H. (Tritonella) catulli, H. (Hinia) holsatica, and H. (Telasco) syltensis are all similar in respect to shape and ornamentation. Criteria have been found for a better discrimination of these species. The species contabulata, effusa and seminodifera described by SPEYER (1864), turned out to be contogenetic stages of H. (Tritonella) pygmaea. H. (Tritonella) cavata, previously described from the Tertiary of the North sea area, was proven to be absent from the area investigated. The forms described under that name, belong to H. (Tritonella) woodwardi.
    Keywords: Area/locality; Behrendorf; Elevation of event; Event label; Germany; Großenwiehe; HAND; Hemmoor; Island of Sylt, Germany; Katzheide; Latitude of event; Longitude of event; Long-term time series Sylt; Mittelholstein; Odderade; ORDINAL NUMBER; Oxlund; Pinneberg; PROFILE; Profile sampling; Sample amount; Sampling by hand; Schenefeld; Schleswig-Holstein, Germany; Shell, angle from apex; Shell, angle from apex, standard deviation; Shell, angle of protoconch; Shell, angle of protoconch, standard deviation; Shell, number of ribs; Shell, number of ribs, standard deviation; Shell, number of whorls; Shell, number of whorls, standard deviation; Species; Sylt_Morsum; Twistringen; Vaale; Vioel
    Type: Dataset
    Format: text/tab-separated-values, 391 data points
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  • 7
    Publication Date: 2023-07-10
    Keywords: Amphipoda; BCR; Box corer (Reineck); Calculated; Copepoda; Counting 〉50 µm fraction; Cumacea; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Indeterminata; Isopoda; Kinorhyncha; Lithology/composition/facies; M23; M23_122; Meiofauna, biomass, wet mass; Meteor (1964); Nauplii; Nematoda; Nordost-Atlantik-Expedition 1971; Ostracoda; Polychaeta; South Atlantic Ocean; Tanaidacea; Tardigrada
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
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  • 8
    Publication Date: 2023-07-10
    Keywords: Amphipoda; BCR; Box corer (Reineck); Calculated; Copepoda; Counting 〉50 µm fraction; Cumacea; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Indeterminata; Isopoda; Kinorhyncha; Lithology/composition/facies; M23; M23_149; Meiofauna, biomass, wet mass; Meteor (1964); Nauplii; Nematoda; Nordost-Atlantik-Expedition 1971; Ostracoda; Polychaeta; South Atlantic Ocean; Tanaidacea; Tardigrada
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 9
    Publication Date: 2023-07-10
    Keywords: Amphipoda; BCR; Box corer (Reineck); Calculated; Copepoda; Counting 〉50 µm fraction; Cumacea; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Indeterminata; Isopoda; Kinorhyncha; Lithology/composition/facies; M23; M23_122; Meiofauna, biomass, wet mass; Meteor (1964); Nauplii; Nematoda; Nordost-Atlantik-Expedition 1971; Ostracoda; Polychaeta; South Atlantic Ocean; Tanaidacea; Tardigrada
    Type: Dataset
    Format: text/tab-separated-values, 106 data points
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  • 10
    Publication Date: 2023-07-10
    Keywords: Campanularia (Clytia) gravieri; Cuspidella humilis; DEPTH, water; Diphasia mutulata; DIVER; Dynamena cornicina; Dynamena quadridentata; Edendrium ramosum; Event label; Gymnangium eximium; Gymnangium hians; Halecium sp.; Halocordyle disticha; Hebella parasitica; Hebella venusta; Hydropolyp; IIOE - International Indian Ocean Expedition; Laomedea (Obelia) dichotoma; Latitude of event; Longitude of event; Lytocarpus philippinus; Plumularia setacea; Red_Sea; Red_Sea_001; Red_Sea_003; Red_Sea_005; Red_Sea_006; Red_Sea_007; Red_Sea_008; Red_Sea_010; Red_Sea_028; Red_Sea_029; Red Sea; Sampling by diver; Sertularella mediterranea; Solanderia minima; Solanderia secunda; Synthecium elegans; Thyroscyphus fruticosus
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 11
    Publication Date: 2023-07-10
    Keywords: Abylopsis tetragona; Auftrieb 72; Bargmannia elongata; Bassia bassensis; BONGO; Bongo net; Chelophyes appendiculata; Counting 〉500 µm fraction; Depth, bottom/max; Depth, top/min; DEPTH, water; Halistemma rubrum; IFM-GEOMAR; Leibniz-Institut für Meereswissenschaften, Kiel; Lensia achilles; M26; M26_NET012; Meteor (1964); Nanomia bijuga; Nectopyramis thetis; off Northwest Africa; Physophora hydrostatica; Praya dubia; Rosacea spp.; Sulculeolaria quadrivalvis; Vogtia glabra; Vogtia pentacantha; Vogtia serrata
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 12
    Publication Date: 2023-07-10
    Keywords: Abylopsis tetragona; Auftrieb 72; Bargmannia elongata; Bassia bassensis; BONGO; Bongo net; Chelophyes appendiculata; Counting 〉500 µm fraction; Depth, bottom/max; Depth, top/min; DEPTH, water; Halistemma rubrum; IFM-GEOMAR; Leibniz-Institut für Meereswissenschaften, Kiel; Lensia achilles; M26; M26_NET013; Meteor (1964); Nanomia bijuga; Nectopyramis thetis; off Northwest Africa; Physophora hydrostatica; Praya dubia; Rosacea spp.; Sulculeolaria quadrivalvis; Vogtia glabra; Vogtia pentacantha; Vogtia serrata
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 13
    Publication Date: 2023-07-10
    Keywords: 11-100; Aluminium; Aluminium oxide; Calcium; Calcium oxide; Chromium; Chromium(III) oxide; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg11; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Minerals; North Atlantic/BASIN; Number of oxygens; Potassium; Potassium oxide; Sample code/label; Sample comment; Silicon; Silicon dioxide; Sodium; Sodium oxide; Titanium; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 14
    Publication Date: 2023-07-10
    Keywords: 11-100; Barium; Boron; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Emission spectrometry; Europium; Gallium; Gas chromatography; Glomar Challenger; Hafnium; Holmium; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Iron oxide, Fe2O3/Iron oxide, FeO ratio; Lanthanum; Leg11; Lithium; Lutetium; Neodymium; Nickel; North Atlantic/BASIN; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Vanadium; Water in rock; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 85 data points
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  • 15
    Publication Date: 2023-07-09
    Keywords: Agassiz Trawl; Aglaophenia latecarinata; AGT; Antenella secundaria; BC; BD; Box corer; Campanularia (Clytia) gravieri; Campanularia (Clytia) hemisphaerica; Campanularia (Clytia) latitheca; Campanularia (Clytia) paulensis; Cnidoscyphus aequalis; DEPTH, sediment/rock; Diphasia digitalis; Diphasia mutulata; Dredge, benthos; Dynamena cornicina; Eastern Basin; Edendrium ramosum; Elevation of event; Eudendrium deciduum; Event label; Filellum sp.; Grab (Shipek); Gulf of Aden; Gymnangium eximium; Gymnangium gracilicaulis; Gymnangium hians; Halecium beanii; Halocordyle disticha; Halopteris glutinosa; Hebella parasitica; Hebella venusta; Hydractinata echinata; Hydropolyp; IIOE - International Indian Ocean Expedition; Indian Ocean Standard Net; IOSN; Laomedea (Obelia) bicuspidata; Latitude of event; Longitude of event; Lytocarpus balei; Lytocarpus philippinus; M1; M1_008; M1_019; M1_021; M1_031; M1_054; M1_063; M1_065; M1_067; M1_068; M1_070; M1_075; M1_076; M1_NET021; Meteor (1964); Nemertesia ramosa; Plumularia setacea; Plumularia wasini; Pycnothea mirabilis; Red Sea; Sertularella campanulata; Sertularella mediterranea; Sertularella natalensis; Sertularella polyzonias; Sertularia ligulata; Sertularia trigonostoma; SHIPEK; Spaerocoryne bedoti; Synthecium elegans; Thecocarpus flexuosus; Thyroscyphus fruticosus; TRAWL; Trawl net; Zygophylax armata
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Vinogradov, Mikhail E; Shushkina, Elvira A; Kukina, Irina N (1976): Functional characteristics of a planktonic community in an equatorial upwelling region. Oceanology, 16, 67-76
    Publication Date: 2023-07-09
    Description: An analysis was made of composition and content of nutrients, salts, particulate and dissolved organic matter, and various plankton groups in a series of samples collected by a 140-liter sampling bottle to depth up to 150 m at 4 equatorial stations between 97° and 154°W. Large and small phytoplankton, bacteria (aggregated and dispersed), heterotrophic flagellates, infusorians, radiolarians, foraminifers, fine filter-feeders, small and large, mostly herbivorous copepods, cyclopoids, predatory calanoids, and other predators were investigated separately. Trophic relations between these elements are established from personal and published data, and rate of their metabolism and some other physiological parameters are determined. Such functional characteristics as extent of satisfaction of food requirements of organisms belonging to various trophic groups, intensity of trophic relations, balance between production and consumption by individual elements of the community, ecological efficiency, and net and specific production of the groups distinguished, of individual trophic levels, of total zooplankton, and of the community as a whole are calculated. Variations of these characteristics along the equator with decreasing upwelling intensity are examined and their possible causes and mechanisms are discussed.
    Keywords: AK17-1454; AK17-1456; AK17-1458; AK17-1461; Archive of Ocean Data; ARCOD; Bacteria, biomass per area, as energy; Calanoides, biomass per area, as energy; Calculated; Carnivorous animals, biomass per area, as energy; Copepoda, biomass per area, as energy; Cyclopoida, biomass per area, as energy; Date/Time of event; Depth, bottom/max; Depth, top/min; DEPTH, water; Equatorial Pacific; Event label; Filter feeder, biomass per area, as energy; Flagellates, biomass per area, as energy; Infusorians, biomass per area, as energy; Latitude of event; Longitude of event; Nonpredatory animals, biomass per area, as energy; Phytoplankton, biomass per area, as energy; PLA; Plankton, biomass per area, as energy; Plankton net; Predators, biomass per area, as energy; Protozoa; Protozoa, biomass per area, as energy; Radiolarians, biomass per area, as energy; Zooplankton, biomass per area, as energy
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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  • 17
    Publication Date: 2023-07-10
    Keywords: 42-373A; Aluminium oxide; Barium; Calcium oxide; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Dysprosium; Europium; Glomar Challenger; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Lead; Leg42; Lithium; Lutetium; Magnesium oxide; Manganese oxide; Mediterranean Sea/BASIN; Niobium; Phosphorus pentoxide; Potassium oxide; Rubidium; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; Strontium; Tantalum; Terbium; Thorium; Titanium dioxide; Uranium; Water in rock; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 696 data points
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  • 18
    Publication Date: 2023-07-10
    Keywords: Abies, needles; Age, comment; Ajuga; Alchemilla; Alnus sp., fruits; Apiaceae indeterminata; Arabis alpina/jacquini; Arenaria cf. ciliata; Armeria calyx; Betula cf. nana, fruits; Betula humilis, fruits; Betula humilis, fruit scales; Betula pubescens, fruits; Betula pubescens, fruit scales; Betula sp., fruits; Betula sp., fruit scales; Carex cf. elongatum utriculi; Carum carvi; Caryophyllaceae, seeds; Caryophyllaceae capsule; cf. Heracleum; cf. Potentilla; Cirsium arvense; Cirsium cf. arvense; Cladium; Comment; Compositae indeterminata; Coniferae, buds; Coniferae, bud scales; Coniferae, cone scales; Coniferae, seeds; Coniferae, seed wings; Counting, palynology; Cyperaceae biconvex, nuts; Cyperaceae trigonous, nuts; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Eupatorium cannabinum; Gypsophila cf. repens; Heracleum; Juniperus, needles; Labiatae indeterminata; Larix, needles; Linum alpinum; Najas flexilis; Najas marina; Picea, anthers; Picea, needles; Picea, seed wings; Picris cf. hieracioides; Picris hieracioides; Pinus, needles; Pinus, spur shoots; Poaceae; Pollen zone; Polygonum; Potamogeton alpinus; Potamogeton cf. alpinus; Potamogeton cf. natans; Potamogeton sp.; Potentilla; Quercus, bud scales; Ranunculus cf. montanus; Ranunculus sp.; Rubus; Rumex; Rumex perianth; Salix, bud scales; Sambucus; Samerberg, Bavaria, Germany; Samerberg1; Scabiosa; Silene cucubalus; Stachys cf. silvatica; Taraxacum; Thalictrum alpinum; Thalictrum minus; Viola; Wood remains; Zannichellia
    Type: Dataset
    Format: text/tab-separated-values, 9416 data points
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  • 19
    Publication Date: 2023-07-10
    Keywords: Abies, cone scales; Abies, needles; Abies, seeds; Abies, seed wings; Alnus glutinosa, fruits; Alnus sp., cones; Alnus sp., fruits; Betula cf. humilis, fruits; Betula sp., fruits; Betula sp., fruit scales; Carex cf. elongatum utriculi; Carpinus; cf. Heracleum; Cladium; Comment; Compositae indeterminata; Coniferae, buds; Coniferae, bud scales; Coniferae, cone scales; Coniferae, seeds; Coniferae, seed wings; Counting, palynology; Cyperaceae trigonous, nuts; Depth, bottom/max; Depth, top/min; Eupatorium cannabinum; Fluderbach_I; HAND; Ilex; Larix, needles; Picea, anthers; Picea, needles; Picea, seed wings; Picea omorica, needles; Pinus, needles; Pinus, spur shoots; Pollen zone; Populus tremula, bud scales; Quercus, bud scales; Rubus; Rumex; Salix, bud scales; Samerberg, Bavaria, Germany; Sampling by hand; SECTION, height; Taxus; Taxus, needles; Tilia platyphyllos; Wood remains
    Type: Dataset
    Format: text/tab-separated-values, 1505 data points
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  • 20
    Publication Date: 2023-07-10
    Keywords: Abies, cone scales; Abies, needles; Abies, seeds; Abies, seed wings; Age, comment; Ajuga; Alchemilla; Alnus glutinosa, fruits; Alnus sp., cones; Alnus sp., fruits; Apiaceae indeterminata; Arabis alpina/jacquini; Arenaria cf. ciliata; Armeria calyx; Betula cf. humilis, fruits; Betula cf. nana, fruits; Betula humilis, fruits; Betula humilis, fruit scales; Betula pubescens, fruits; Betula sp., fruits; Betula sp., fruit scales; Carex cf. elongatum utriculi; Carpinus; Carum carvi; Caryophyllaceae, seeds; Caryophyllaceae capsule; cf. Heracleum; cf. Potentilla; Cirsium arvense; Cirsium cf. arvense; Cladium; COMPCORE; Compositae indeterminata; Composite Core; Coniferae, buds; Coniferae, bud scales; Coniferae, cone scales; Coniferae, seeds; Coniferae, seed wings; Counting, palynology; Cyperaceae biconvex, nuts; Cyperaceae trigonous, nuts; Depth, bottom/max; Depth, composite; Depth, top/min; Eupatorium cannabinum; Gypsophila cf. repens; Heracleum; Ilex; Juniperus, needles; Labiatae indeterminata; Larix, needles; Linum alpinum; Najas flexilis; Najas marina; Picea, anthers; Picea, needles; Picea, seed wings; Picea omorica, needles; Picris cf. hieracioides; Picris hieracioides; Pinus, needles; Pinus, spur shoots; Poaceae; Pollen zone; Polygonum; Populus tremula, bud scales; Potamogeton alpinus; Potamogeton cf. alpinus; Potamogeton sp.; Potentilla; Quercus, bud scales; Ranunculus cf. montanus; Ranunculus sp.; Rubus; Rumex; Rumex perianth; Salix, bud scales; Sambucus; Samerberg; Samerberg, Bavaria, Germany; Sample comment; Scabiosa; Silene cucubalus; Stachys cf. silvatica; Taraxacum; Taxus; Taxus, needles; Thalictrum alpinum; Thalictrum minus; Tilia platyphyllos; Viola; Wood remains; Zannichellia
    Type: Dataset
    Format: text/tab-separated-values, 12330 data points
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  • 21
    Publication Date: 2023-07-10
    Keywords: 43-384; Biantholithus sparsus; Biscutum aff. dimorphosum; Biscutum tenuiculum; Braarudosphaera bigelowii; Braarudosphaera discula; Braarudosphaera imbricata; Bramletteius sp.; Campylosphaera eodela; Chiasmolithus bidens; Chiasmolithus californicus; Chiasmolithus consuetus; Chiasmolithus danicus; Chiasmolithus sp.; Coccolithus eopelagicus; Coccolithus pelagicus; Crepidolithus spp.; Cruciplacolithus primus; Cruciplacolithus subrotundus; Cruciplacolithus tenuis; Cyclolithella robusta; Deep Sea Drilling Project; DEPTH, sediment/rock; Discoaster lenticularis; Discoaster mohleri; Discoaster multiradiatus; Discoaster nobilis; Discoaster sp.; Discolithina plana; Discolithina rimosa; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ellipsolithus distichus; Ellipsolithus macellus; Epoch; Ericsonia subpertusa; Etching index; Fasciculithus aff. richardii; Fasciculithus alanii; Fasciculithus clinatus; Fasciculithus hayi; Fasciculithus pileatus; Fasciculithus sp.; Fasciculithus tympaniformis; Fasciculithus ulii; Glomar Challenger; Goniolithus fluckigeri; Heliolithus cantabriae; Heliolithus conicus; Heliolithus kleinpellii; Heliolithus riedelii; Leg43; Markalius astroporus; Markalius sp.; Nannofossil abundance; Nannofossils preservation; Nannofossil zone; Neochiastozygus concinnus; Neochiastozygus imbriei; Neochiastozygus junctus; North Atlantic/RIDGE; Overgrowth index; Prinsius bisulcus; Reworked; Sample code/label; Sphenolithus anarrhopus; Sphenolithus moriformis; Thoracosphaera deflandrei; Thoracosphaera operculata; Thoracosphaera saxea; Toweius craticulus; Toweius eminens; Toweius tovae; Zygodiscus plectopons; Zygodiscus sigmoides; Zygodiscus simplex
    Type: Dataset
    Format: text/tab-separated-values, 5286 data points
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  • 22
    Publication Date: 2023-07-10
    Keywords: 43-384; Arkhangelskiella cymbiformis; Biscutum constans; Braarudosphaera spp.; Broinsonia enormis; Broinsonia parca; Broinsonia signata; Chiasmolithus danicus; Chiastozygus litterarius; Corollithion exiguum; Crepidolithus spp.; Cretarhabdus conicus; Cretarhabdus coronadventis; Cretarhabdus surirellus; Cribrosphaera ehrenbergii; Cyclagelosphaera margerelii; Cylindralithus spp.; Deep Sea Drilling Project; DEPTH, sediment/rock; Discorhabdus rotatorius; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eiffellithus trabeculatus; Eiffellithus turriseiffelii; Epoch; Etching index; Gartnerago obliquum; Glomar Challenger; Kamptnerius magnificus; Leg43; Lithastrinus floralis; Lithraphidites carniolensis; Lithraphidites helicoideus; Lithraphidites quadratus; Lucianorhabdus cayeuxii; Manivitella pemmatoidea; Markalius astroporus; Marthasterites furcatus; Microrhabdulus decoratus; Micula mura; Micula staurophora; Nannofossil abundance; Nannofossils preservation; Nephrolithus frequens; North Atlantic/RIDGE; Octopodorhabdus decussatus; Overgrowth index; Parhabdolithus angustus; Parhabdolithus embergeri; Parhabdolithus splendens; Podorhabdus decorus; Prediscosphaera cretacea; Prediscosphaera spinosa; Pseudoemiliania regularis; Reinhardtites anthophorus; Sample code/label; Staurolithites laffittei; Tegumentum stradneri; Tetracolporopollenites obscurus; Tetralithus aculeus; Thoracosphaera spp.; Tranolithus gabalus; Tranolithus orionatus; Vagalapilla aachena; Vagalapilla compacta; Vagalapilla matalosa; Vagalapilla octoradiata; Vekshinella stradneri; Watznaueria barnesae; Watznaueria communis; Zeugrhabdotus diplogrammus; Zeugrhabdotus elegans; Zygodiscus sigmoides; Zygodiscus spiralis
    Type: Dataset
    Format: text/tab-separated-values, 2442 data points
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  • 23
    Publication Date: 2023-07-10
    Keywords: 43-385; Arkhangelskiella cymbiformis; Biscutum constans; Broinsonia enormis; Chiastozygus litterarius; Cretarhabdus conicus; Cretarhabdus surirellus; Cribrosphaerella ehrenbergii; Cyclagelosphaera margerelii; Cylindralithus spp.; Deep Sea Drilling Project; DEPTH, sediment/rock; Discorhabdus rotatorius; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eiffellithus turriseiffelii; Epoch; Etching index; Glomar Challenger; Leg43; Lithraphidites carniolensis; Lithraphidites quadratus; Manivitella pemmatoidea; Microrhabdulus decoratus; Micula mura; Micula staurophora; Nannofossil abundance; Nannofossils preservation; North Atlantic/SEAMOUNT; Overgrowth index; Parhabdolithus splendens; Prediscosphaera cretacea; Prediscosphaera spinosa; Pseudoemiliania regularis; Sample code/label; Staurolithites laffittei; Tetralithus aculeus; Tetralithus trifidus; Vekshinella stradneri; Watznaueria barnesae; Zeugrhabdotus diplogrammus; Zygodiscus spiralis
    Type: Dataset
    Format: text/tab-separated-values, 272 data points
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  • 24
    Publication Date: 2023-07-10
    Keywords: Aluminium; Archive of Ocean Data; ARCOD; Arsenic; Calcium carbonate; Calculated from skeletal dry weight; Carbon, organic, total; Chromium; Cobalt; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-611; DM9-612; DM9-613; DM9-615; DM9-625; DM9-626; DM9-627; DM9-628; DM9-629; DM9-641; DM9-643; DM9-645; DM9-647; DM9-649; DM9-651; DM9-653; DM9-655; DM9-668; DM9-669; DM9-670; DM9-671; DM9-672; DM9-673; DM9-674; DM9-675; DM9-677; DM9-678; DM9-685; DM9-686; Dmitry Mendeleev; Elevation of event; Event label; Gallium; GC; Germanium; Grab; GRAB; Gravity corer; Iron; Latitude of event; Lead; Longitude of event; Manganese; Molybdenum; MULT; Multiple investigations; Nickel; Niobium; Northeast Pacific; North Pacific; Northwest Pacific; Opal, biogenic silica; PC; Phosphorus; Piston corer; Quantitative emission spectral analysis; Selenium; Sulfur, total; Tantalum; Titanium; Vanadium; VITYAZ; Vityaz (ex-Mars); VITYAZ6158-GC; VITYAZ6159-GC; VITYAZ6160-PC; VITYAZ6161-PC; VITYAZ6162-GC; VITYAZ6163-GC; VITYAZ6164-GC; VITYAZ6165-GR-2; VITYAZ6166-GC; VITYAZ6167-GC; VITYAZ6168-GC; VITYAZ6169-GC; VITYAZ6171-GC; VITYAZ6172-GC; VITYAZ6173-GC; VITYAZ6174-PC; VITYAZ6175-GC; VITYAZ6176-GC; Water in rock; Wet chemistry; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 10509 data points
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  • 25
    Publication Date: 2023-07-10
    Keywords: 10-86; 10-94; 10-95; Acarinina collactea, δ13C; Acarinina collactea, δ18O; Acarinina mckannai, δ13C; Acarinina mckannai, δ18O; Acarinina nitida, δ13C; Acarinina nitida, δ18O; Chiloguembelina midwayensis, δ13C; Chiloguembelina midwayensis, δ18O; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Gavelinella spp., δ13C; Gavelinella spp., δ18O; Glomar Challenger; Gulf of Mexico/BENCH; Gulf of Mexico/SCARP; Leg10; Morozovella subbotinae, δ13C; Morozovella subbotinae, δ18O; Morozovella uncinata, δ13C; Morozovella uncinata, δ18O; Morozovella velascoensis, δ13C; Morozovella velascoensis, δ18O; Nuttallides spp., δ13C; Nuttallides spp., δ18O; Planktic foraminifera zone; Planorotalites compressus, δ13C; Planorotalites compressus, δ18O; Planorotalites pseudomenardii, δ13C; Planorotalites pseudomenardii, δ18O; Robulus spp., δ13C; Robulus spp., δ18O; Sample code/label; Subbotina trilocularis, δ13C; Subbotina trilocularis, δ18O; Subbotina triloculinoides, δ13C; Subbotina triloculinoides, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
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  • 26
    Publication Date: 2023-07-10
    Keywords: 39-356; 39-357; Acarinina spp., δ13C; Acarinina spp., δ18O; Chiloguembelina midwayensis, δ13C; Chiloguembelina midwayensis, δ18O; Cibicides spp., δ13C; Cibicides spp., δ18O; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Gavelinella spp., δ13C; Gavelinella spp., δ18O; Globoconusa daubjergensis, δ13C; Globoconusa daubjergensis, δ18O; Glomar Challenger; Guembelitria cretacea, δ13C; Guembelitria cretacea, δ18O; Lagena spp., δ13C; Lagena spp., δ18O; Leg39; Morozovella aff. trinidadensis, δ13C; Morozovella aff. trinidadensis, δ18O; Morozovella angulata, δ13C; Morozovella angulata, δ18O; Morozovella conicotruncata, δ18O; Morozovella inconstans, δ13C; Morozovella inconstans, δ18O; Morozovella trinidadensis, δ13C; Morozovella trinidadensis, δ18O; Morozovella uncinata, δ13C; Morozovella uncinata, δ18O; Morozovella velascoensis, δ18O; Nuttallides spp., δ13C; Nuttallides spp., δ18O; Planktic foraminifera zone; Planorotalites compressus, δ13C; Planorotalites compressus, δ18O; Planorotalites eugubinus, δ13C; Planorotalites eugubinus, δ18O; Pulleniatina spp., δ13C; Pulleniatina spp., δ18O; Robulus spp., δ13C; Robulus spp., δ18O; Sample code/label; South Atlantic/CONT RISE; South Atlantic/PLATEAU; Subbotina fringa, δ13C; Subbotina fringa, δ18O; Subbotina pseudobulloides, δ13C; Subbotina pseudobulloides, δ18O; Subbotina triloculinoides, δ13C; Subbotina triloculinoides, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 179 data points
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  • 27
    Publication Date: 2023-07-10
    Keywords: Archive of Ocean Data; ARCOD; Depth, bottom/max; Depth, top/min; DEPTH, water; North Pacific; PLA; Plankton net; Sample comment; Thysanoessa longipes, biomass; VITYAZ; Vityaz (ex-Mars); VITYAZ7519
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
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  • 28
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Stanley, Daniel Jean; Sheng, Harrison; Kholief, Mahmoud M (1979): Sand on the southern Mediterranean Ridge: proximal basement and distal African-Nile provenance. Nature, 279(5714), 594-598, https://doi.org/10.1038/279594a0
    Publication Date: 2023-07-07
    Description: Petrographic analysis of Quaternary terrigenous sand layers in eastern Mediterranean cores reveals distinct mineralogical differences between the Egyptian Shelf–Nile Cone region and the southern part of the Mediterranean Ridge. A compositionally and texturally immature suite in Ridge cores, mixed with a Nile-derived assemblage, identifies a fresh non-recycled mineral component derived from proximal igneous and metamorphic surface or near-surface exposures, probably in the south–central Ridge area rather than from distal African sources. The presence of such basement terrains would be consistent with a compressive thrust-belt origin for this part of the Mediterranean Ridge.
    Keywords: 13-130; 13-131; Amphibole; Apatite; Area/locality; CHN119-11; Clinopyroxene; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Epidote; Event label; Garnet; GC; Glomar Challenger; Grab; GRAB; Gravity corer; Heavy minerals; Heavy minerals, opaque; Heavy minerals, sum; Leg13; Mediterranean Sea; Mediterranean Sea/CONE; Mediterranean Sea/RIDGE; Orthopyroxene; P6508-42; P6508-45; P6510-10; P6510-5; P6510-6; P6510-8; P6510-P14; P6510-P17; P6510-P4; PC; Piston corer; Sample code/label; Sphene; V10; V10-53; Vema; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 533 data points
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  • 29
    Publication Date: 2023-07-07
    Keywords: 43-382; 43-383; 43-384; 43-385; 43-386; 43-387; 44-388A; 44-390; 44-391A; Anatase; Apatite; Barite; Biotite; Calculated; Chlorite; Clinopyroxene; Counting, Stereo Microscope; Deep Sea Drilling Project; Disthene; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epidote; Event label; Formation; Garnet; Glomar Challenger; Hornblende; Iron hydroxides; Latitude of event; Leg43; Leg44; Leucoxene; Longitude of event; Magnetite; Minerals; Minerals, other; Monazite; North Atlantic; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/RIDGE; North Atlantic/SEAMOUNT; Orthopyroxene; Palagonite; Pyrite, FeS2; Rutile; Sample code/label; Siderite; Sillimanite; Sphene; Spinel; Staurolite; Sum; Tourmaline; Tremolite/Actinolite; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 2604 data points
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  • 30
    Publication Date: 2023-07-07
    Keywords: 22-211; 22-214; 22-218; 23-221; 23-222; 24-232; 24-232A; 25-240; 25-248; 26-250A; Aegirine; Andalusite; Apatite; Augite-diopside; Biotite; Carbonates; Chlorite; Clinopyroxene; Clinozoisite; Collophane; Counting 63-125 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epidote; Event label; Fragments; Garnet; Glauconite; Glomar Challenger; Heavy minerals; Hornblende; Indeterminata; Indian Ocean//BASIN; Indian Ocean//FAN; Indian Ocean//RIDGE; Indian Ocean/Arabian Sea/CONE; Indian Ocean/Arabian Sea/PLAIN; Indian Ocean/Gulf of Aden/TRENCH; Kyanite; Leg22; Leg23; Leg24; Leg25; Leg26; Minerals, altered; Monazite; Muscovite; Opaque minerals; Orthopyroxene; Riebeckite; Rutile; Sample code/label; Sillimanite; Sphene; Staurolite; Topaz; Total; Tourmaline; Tremolite/Actinolite; Volcanic glass; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 663 data points
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  • 31
    facet.materialart.
    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publication Date: 2023-07-11
    Keywords: 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; Grain size, pipette analysis; Grain size, sieving; Latitude of event; Longitude of event; Phosphorus pentoxide; Size fraction; Size fraction 〈 0.010 mm; Size fraction 〉 0.100 mm; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 68 data points
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  • 32
    facet.materialart.
    Unknown
    PANGAEA
    In:  Geological Institute, Russian Academy of Sciences, Moscow | Supplement to: Lisitzina, Nadezhda A; Butuzova, Galina Yu (1976): Zeolites in sediments of the lithological profile across the Pacific Ocean. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 11(2), 9-21
    Publication Date: 2023-07-11
    Description: Results of petrographic, chemical and X-ray studies of zeolites in sediments in the Transpacific lithological profile from the coast of Japan to the coast of Mexico are reported. For ocean phillipsites constancy of Si/Al ratio (2.44-2.87) and unstable cation composition in quantitative predominance of potassium over sodium are characteristic. Two groups of ocean phillipsites are distinguished: of deep-water basins and of submarine rises. The first spread over broad areas of the pelagic zone, and are formed by diagenetic transformation of fine dispersed pyroclastic material in minimum sedimentation rates, the latter occur locally - in areas of basaltic volcanism manifestations.
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Barium oxide; Calcium oxide; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-612; DM9-643; Dmitry Mendeleev; Elevation of event; Event label; GC; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Northeast Pacific; Northwestern Basin, Pacific Ocean; Northwest Pacific; OKEAN; Okean Grab; Phosphorus pentoxide; Potassium oxide; Ratio; Silicon/Aluminium ratio; Silicon dioxide; Size fraction; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ4362-GR-1; VITYAZ6176-GC; VITYAZ6177-GR; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 33
    facet.materialart.
    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad
    Publication Date: 2023-07-11
    Keywords: AK3-144; AK3-210; AK3-99; Akademik Kurchatov; AKU3; AN9086-8; AN9086-8-469; Aragonite; Archive of Ocean Data; ARCOD; AtlantNIRO-SRTR-9086; Calcium carbonate; Counting 100-250 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Grab; GRAB; Latitude of event; Longitude of event; Low magnesium calcite; Magnesium-Calcite; Magnesium carbonate, magnesite; Size fraction; Volumetric; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 135 data points
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  • 34
    Publication Date: 2023-07-11
    Keywords: 19-183; Chert; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Feldspar; Fragments; Glomar Challenger; Kalifeldspar; Leg19; North Pacific/PLAIN; Plagioclase; Quartz; Quartz, polycrystalline; Ratio; Rock fragments; Sample code/label; Size fraction
    Type: Dataset
    Format: text/tab-separated-values, 782 data points
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  • 35
    Publication Date: 2023-07-11
    Keywords: 19-183; Amphibole; Amphibole group minerals; Apatite; Clinopyroxene; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epidote; Garnet; Glomar Challenger; Hornblende, basaltic; Hornblende, common; Kyanite; Leg19; North Pacific/PLAIN; Orthopyroxene; Pumpellyite; Pyroxene group minerals; Sample code/label; Size fraction; Sphene; Staurolite; Tourmaline; Tremolite/Actinolite; Zircon; Zoisite
    Type: Dataset
    Format: text/tab-separated-values, 965 data points
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  • 36
    Publication Date: 2023-07-11
    Keywords: 38-336; Aluminium oxide; Archive of Ocean Data; ARCOD; Calcium oxide; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Iron oxide, Fe2O3; Iron oxide, FeO; Leg38; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; North Atlantic/Norwegian Sea; Phosphorus pentoxide; Potassium oxide; Sample code/label; Silicon dioxide; Size fraction; Sodium oxide; Titanium dioxide; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 74 data points
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  • 37
    Publication Date: 2023-07-11
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Barium oxide; Calcium oxide; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-612; DM9-643; Dmitry Mendeleev; Elevation of event; Event label; GC; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Northeast Pacific; Northwest Pacific; OKEAN; Okean Grab; Phosphorus pentoxide; Potassium oxide; Silicon dioxide; Size fraction; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ4362-GR-2; VITYAZ6176-GC; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 38
    Publication Date: 2023-07-11
    Keywords: Archive of Ocean Data; ARCOD; Cerium; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dysprosium; Erbium; Gadolinium; GC; Gravity corer; Holmium; Lanthanum; Neodymium; Northwest Pacific; Praseodymium; Samarium; Size fraction; Terbium; Thulium; VITYAZ; Vityaz (ex-Mars); VITYAZ6176-GC; Wet chemistry; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 39
    Publication Date: 2023-07-11
    Keywords: 38-337; 38-345; Aluminium oxide; Archive of Ocean Data; ARCOD; Calcium oxide; Calculated; Carbon dioxide; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Leg38; Longitude of event; Magnesium oxide; Manganese oxide; North Atlantic/Norwegian Sea/BASIN; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample type; Silicon dioxide; Size fraction; Sodium oxide; Sulfur, total; Sum; Titanium dioxide; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 82 data points
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  • 40
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Rutkovsky, V M (1977): Constants of calcium, magnesium, zinc, cobalt, copper, and nickel exchange for sodium in iron-manganese nodules from the Pacific Ocean. Oceanology, 17(1), 46-47
    Publication Date: 2023-08-28
    Description: Constants of calcium, magnesium, zinc, cobalt, copper, and nickel exchange for sodium in iron-manganese nodules taken from different parts of the Pacific Ocean were determined under static conditions at constant ionic strength (?=0.05). These determinations revealed high capacity of nodules for sorbing the referred ions (their exchange constants range from 1.93 to 20.85). Obtained data demonstrate the major role of MnO and Fe2O3 in sorption processes in iron-manganese nodules.
    Keywords: Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Eastern Basin, Pacific Ocean; OKEAN; Okean Grab; Southern Basin, Pacific Ocean; TRAWL; Trawl net; Vityaz (ex-Mars); Vityaz-43; Vityaz-48; VITYAZ5965-3-GR; VITYAZ5965-5-GR; VITYAZ5988-4-TR; VITYAZ5996-2-TR; VITYAZ6298-2-GR
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 41
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Skornyakova, Nadezhda S; Bezrukov, Panteleimon L; Bazilevskaya, Elena S; Gordeev, Viacheslav V (1979): Fe-Mn nodules from the western Indian Ocean (zonal and local variability). Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 14(3), 3-18
    Publication Date: 2023-08-28
    Description: Regional variations in abundance, morphology, and chemical composition of Fe-Mn nodules have a zonal character. Due to circumcontinental zonality of terrigenous sedimentation the main mass of the nodules occurs in the pelagic part of the ocean, in areas of minimal sedimentation rates. In spatial variations in morphology and chemical composition of the nodules the latitudinal zonality is very clear and associated with latitudinal changes in facial conditions of sedimentation. Elevated contents of Mn, Ni, and Cu and of Mn/Fe ratio occur in nodules from the radiolarian belt. Changes of chemical composition of the nodules with depth (vertical zonality of mineralization) are confirmed. Local variations in abundance, morphology and chemical composition of the nodules are caused by ruggedness of relief and depth variations, variations in sedimentation rate, age of ore formation, intensity of diagenetic redistribution of metals.
    Keywords: Archive of Ocean Data; ARCOD; Bottom trawl; BT; Dredge; DRG; East Indian Ocean; GC; Grab; GRAB; Gravity corer; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; SIGSBY; Sigsby trawl; VITYAZ; Vityaz (ex-Mars); VITYAZ6729; VITYAZ6731-5; VITYAZ6731-6; VITYAZ6732-1; VITYAZ6734; VITYAZ6736-1; VITYAZ6737-1; VITYAZ6742-11; VITYAZ6742-13; VITYAZ6742-15; VITYAZ6742-2; VITYAZ6742-21; VITYAZ6742-22; VITYAZ6742-4; VITYAZ6742-6; VITYAZ6742-8; VITYAZ6742-9; VITYAZ6744-1; VITYAZ6744-2; VITYAZ6744-37; VITYAZ6744-39; VITYAZ6744-8; VITYAZ6746-1; VITYAZ6749-1; VITYAZ6751-2; VITYAZ6753-1; VITYAZ6754-1; VITYAZ6754-10; VITYAZ6754-11; VITYAZ6754-12; VITYAZ6754-15; VITYAZ6754-16; VITYAZ6754-4; VITYAZ6754-5; VITYAZ6754-6; VITYAZ6754-7; VITYAZ6755; VITYAZ7411-1; VITYAZ7411-2; VITYAZ7413; VITYAZ7414-1; VITYAZ7430; VITYAZ7446
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 42
    facet.materialart.
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    PANGAEA
    In:  Supplement to: Bezrukov, Panteleimon L; Skornyakova, Nadezhda S; Murdmaa, Ivar O; Andrushchenko, Polina F; Zenkevich, Nikita L (1976): Ferromanganese Nodules of the Pacific Ocean. P.P. Shirshov Institute of Oceanology of the USSR Academy of Sciences, Transactions, vol. 109. Moscow, Nauka Publ. (P.L. Bezrukov, Ed.), 301 pp
    Publication Date: 2023-08-28
    Description: The monograph highlights extensive materials collected during expeditions of P.P. Shirshov Institute of Oceanology. We consider facial conditions of nodule formation, regularities of their distribution, stratigraphic position, petrography, mineral composition, textures, geochemistry of nodules and hosting sediments. Origin of iron-manganese nodules in the Pacific Ocean is considered as well.
    Keywords: AK4-225-TR; AK4-227-PH; AK4-230-GR; AK4-231-GR; AK4-232-GR; AK4-232-PH; AK4-233-GR; AK4-233-TR; AK4-259-GR; AK4-259-PH; AK4-260-GR; AK4-261-GR; Akademik Kurchatov; AKU4; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Central Pacific Seamounts, Pacific Ocean; DM8; DM8-516-GR; DM8-518-GR; DM8-520-GR; DM8-521-TR; DM8-541-GR; DM8-554-GR; DM8-556-GR; DM8-568-GR; DM8-569-GR; DM8-598-GR; DM8-599-GR; DM8-600-GR; DM8-607-GR; DM8-608-GR; Dmitry Mendeleev; Dredge; DRG; Eastern Basin, Pacific Ocean; Eastern Mariana Basin, Pacific Ocean; Equatorial Pacific; GC; Grab; GRAB; Gravity corer; Manihiki Plateau, Pacific Ocean; Marcus-Necker Ridge; Mariana Basin, Pacific Ocean; MULT; Multiple investigations; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Photo/Video; PV; Southeast Pacific; Southern Basin, Pacific Ocean; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-20; Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3151-TR; VITYAZ3233-GC-2; Vityaz-34; VITYAZ3630-PH; VITYAZ3631-GR-1; VITYAZ3632-PH; VITYAZ3635-PH; VITYAZ3729-GC-1; VITYAZ3782-PH; VITYAZ3782-TR; VITYAZ3787-TR; VITYAZ3802-TR; VITYAZ3871-GR-1; VITYAZ3899-GR-1; VITYAZ3900-GR-1; VITYAZ3996-TR; VITYAZ4009-TR; VITYAZ4074-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4199-TR; VITYAZ4217-TR; VITYAZ4221-TR; VITYAZ4239-PH; VITYAZ4239-TR; VITYAZ4245-GR; VITYAZ4249-PH; VITYAZ4249-TR; VITYAZ4261-PH; VITYAZ4265-TR; VITYAZ4273-GR-1; VITYAZ4273-PH; VITYAZ4273-TR; VITYAZ4279-PH; VITYAZ4279-TR; VITYAZ4281-TR; VITYAZ4285-GR-1; VITYAZ4285-PH; VITYAZ4289-GR-1; VITYAZ4289-TR; Vityaz-43; VITYAZ4309-TR; VITYAZ4320-TR; VITYAZ4331-GR-1; VITYAZ4343-GR-1; VITYAZ4347-GR-1; VITYAZ4347-PH; VITYAZ4351-GR; VITYAZ4355-GR; VITYAZ4359-GR-1; VITYAZ4359-PH; VITYAZ4362-GR-1; VITYAZ4370-PH; VITYAZ4370-TR; Vityaz-48; VITYAZ5066-GR; VITYAZ5066-TR; VITYAZ5074-PH; VITYAZ5074-TR; VITYAZ5096-PH; VITYAZ5100-GR-1; VITYAZ5110-GR-1; VITYAZ5112-GR; VITYAZ5114-GR; VITYAZ5124-TR; VITYAZ5126-GR-1; VITYAZ5128-TR; VITYAZ5129-GR-1; VITYAZ5133-TR; VITYAZ5139-GR-1; VITYAZ5159-TR; VITYAZ5163-GR-1; VITYAZ5398-GR-1; VITYAZ5408-GR-1; VITYAZ5409-GR-1; VITYAZ5410-GR-1; VITYAZ5411-GR-1; VITYAZ5412-DR; VITYAZ5414-GR-1; VITYAZ5420-GR-1; VITYAZ5421-GR-1; VITYAZ5422-GR-1; VITYAZ5423-GR-1; VITYAZ5424-GR; VITYAZ5429-GR-1; VITYAZ5432-GR-1; VITYAZ5437-GR; VITYAZ5505-GR; VITYAZ5937A-GR; VITYAZ5937-GR; VITYAZ5955; VITYAZ5958-GR; VITYAZ5959-GR; VITYAZ5960-GR; VITYAZ5960-PH; VITYAZ5962-GR; VITYAZ5962-PH; VITYAZ5963-GC; VITYAZ5964-GR; VITYAZ5965-0-GR; VITYAZ5965-10-GR-1; VITYAZ5965-1-GR; VITYAZ5965-2-GC; VITYAZ5965-3-GR; VITYAZ5965-3-TR; VITYAZ5965-5-GR; VITYAZ5965-6-GC; VITYAZ5966-GR; VITYAZ5966-PH; VITYAZ5968-14-DR; VITYAZ5968-15-DR; VITYAZ5968-18-GC; VITYAZ5968-1-GR; VITYAZ5968-2-GC; VITYAZ5968-3-GR; VITYAZ5968-4-GR; VITYAZ5968-7-TR; VITYAZ5968-9-GR; VITYAZ5970-GR; VITYAZ5971-GR; VITYAZ5972-TR; VITYAZ5975-GR; VITYAZ5975-PH; VITYAZ5977-PH; VITYAZ5982-GR; VITYAZ5982-PH; VITYAZ5983-GR; VITYAZ5983-PH; VITYAZ5984-GR; VITYAZ5984-PH; VITYAZ5987-GR; VITYAZ5988-11-GR; VITYAZ5988-12-GR; VITYAZ5988-13-GR; VITYAZ5988-14-GC; VITYAZ5988-16-GR; VITYAZ5988-19-TR; VITYAZ5988-20-GR; VITYAZ5988-21-GR; VITYAZ5988-22-GR; VITYAZ5988-24-GR; VITYAZ5988-25-GR; VITYAZ5988-2-GC; VITYAZ5988-4-TR; VITYAZ5988-5-GR; VITYAZ5988-7-GR; VITYAZ5988-9-GR; VITYAZ5993-GR; VITYAZ5995-GR; VITYAZ5996-10-GR; VITYAZ5996-11-TR; VITYAZ5996-13-GR; VITYAZ5996-15-GR; VITYAZ5996-17-GR; VITYAZ5996-18-GR; VITYAZ5996-1-GR; VITYAZ5996-20-GR; VITYAZ5996-22-GR; VITYAZ5996-24-GC; VITYAZ5996-25-GR; VITYAZ5996-2-TR; VITYAZ5996-4-GR; VITYAZ5996-6-GR; VITYAZ6000-GC; VITYAZ6002-11-GC; VITYAZ6002-12-DR; VITYAZ6002-17-GC; VITYAZ6002-20-GC; VITYAZ6002-21-DR; VITYAZ6002-24; VITYAZ6004-GC; VITYAZ6005-GC; VITYAZ6005-GR; VITYAZ6006-GR; VITYAZ6008; VITYAZ6009-GR; VITYAZ6011-GR; VITYAZ6012-GR; VITYAZ6013-GR; VITYAZ6014-GR; VITYAZ6015-GR; VITYAZ6015-PH; VITYAZ6015-TR; VITYAZ6016-GR; VITYAZ6017-DR; VITYAZ6165-GR-1; VITYAZ6167-GR; VITYAZ6168-GR; VITYAZ6172-GR; VITYAZ6174-GR; VITYAZ6177-GR; VITYAZ6243-GR; VITYAZ6255-GR; VITYAZ6256-GR; VITYAZ6257-GR; VITYAZ6264-GR; VITYAZ6265-DR; VITYAZ6267-GR; VITYAZ6270-DR; VITYAZ6272-GR; VITYAZ6273-GR; VITYAZ6275-11-GR; VITYAZ6275-15-TR; VITYAZ6275-2-TR; VITYAZ6275-3-GR; VITYAZ6275-5-GC; VITYAZ6275-8-TR; VITYAZ6277-3-GC; VITYAZ6277-4-TR; VITYAZ6297-TR; VITYAZ6298-10-GC; VITYAZ6298-12-GR; VITYAZ6298-13-TR; VITYAZ6298-14-GC; VITYAZ6298-18-GR; VITYAZ6298-19-GC; VITYAZ6298-1-GC; VITYAZ6298-20-TR; VITYAZ6298-24-TR; VITYAZ6298-26-GR; VITYAZ6298-28-GC; VITYAZ6298-2-GR; VITYAZ6298-30-TR; VITYAZ6298-31-GC; VITYAZ6298-33-GC; VITYAZ6298-34-GR; VITYAZ6298-35-TR; VITYAZ6298-36-GR; VITYAZ6298-37-TR; VITYAZ6298-40-TR; VITYAZ6298-42-GC; VITYAZ6298-43-GR; VITYAZ6298-45-GC; VITYAZ6298-46-GR; VITYAZ6298-47-GC; VITYAZ6298-48-GR; VITYAZ6298-49-GC; VITYAZ6298-50-GR; VITYAZ6298-51-GC; VITYAZ6298-52A-TR; VITYAZ6298-53-TR; VITYAZ6298-56-TR; VITYAZ6298-57-GC; VITYAZ6298-58; VITYAZ6298-62-TR; VITYAZ6298-7-TR; VITYAZ6298-8-GR; VITYAZ6298-9-GR; VITYAZ6299-TR; VITYAZ6300-TR; VITYAZ6307-TR; VITYAZ6331; VITYAZ6332-GR; VITYAZ6333-10-TR; VITYAZ6333-11-GR; VITYAZ6333-13-TR; VITYAZ6333-20; VITYAZ6333-22-GC; VITYAZ6333-23-TR; VITYAZ6333-26-GC; VITYAZ6333-2-TR; VITYAZ6333-3-GC; VITYAZ6333-5-GC; VITYAZ6333-7-GC; VITYAZ6333-8-GC; VITYAZ6334-GR; VITYAZ6335-GC; VITYAZ6339-GC; VITYAZ6343-TR; VITYAZ6344-TR; VITYAZ6348-TR; VITYAZ6352-TR; VITYAZ6356-TR; VITYAZ6358-TR; VITYAZ6359-TR; VITYAZ6360-TR; VITYAZ6364-TR; VITYAZ6365-TR; VITYAZ6366-DR; VITYAZ6367-DR; VITYAZ6368-DR; VITYAZ6369-DR; VITYAZ6405-PH; VITYAZ6408-PH; VITYAZ6704-GC; VITYAZ6706-DR; VITYAZ6817-GR; VITYAZ6818-TR; VITYAZ6819-TR; VITYAZ6821-GR; VITYAZ6822-DR; VITYAZ6824-GR; VITYAZ6825-GR; VITYAZ6826-GR; Vityaz Trench, Pacific Ocean
    Type: Dataset
    Format: application/zip, 14 datasets
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  • 43
    Publication Date: 2023-08-28
    Description: Analysis of manganese in sediments of the equatorial Pacific.
    Keywords: BC; Box corer; Dredge, bucket; DRG_BU; FFGR; Free-fall grab; Mn-74-01-001-FFG-001; Mn-74-01-001-FFG-002; Mn-74-01-001-FFG-003; Mn-74-01-002-FFG-004; Mn-74-01-002-FFG-006; Mn-74-01-003-FFG-007; Mn-74-01-003-FFG-009; Mn-74-01-005-B2; Mn-74-01-006-FFG-016; Mn-74-01-006-FFG-017; Mn-74-01-006-FFG-018; Mn-74-01-006-FFG-019; Mn-74-01-006-FFG-020; Mn-74-01-006-FFG-021; Mn-74-01-006-FFG-022; Mn-74-01-006-FFG-023; Mn-74-01-006-FFG-025; Mn-74-01-006-FFG-026; Mn-74-01-007-FFG-028; Mn-74-01-007-FFG-029; Mn-74-01-008-FFG-032; Mn-74-01-009-FFG-036; Mn-74-01-010-FFG-037; Mn-74-01-010-FFG-038; Mn-74-01-010-FFG-039; Mn-74-01-010-FFG-042; Mn-74-01 IODE; Mn-74-02-13A-FFG-004; Mn-74-02-13B-D-001; Mn-74-02-13B-FFG-005; Mn-74-02-13B-FFG-007; Mn-74-02-13B-FFG-008; Mn-74-02-13C-D-002; Mn-74-02-13C-D-004; Mn-74-02-13C-FFG-009; Mn-74-02-13C-FFG-011; Mn-74-02-13C-FFG-012; Mn-74-02-15-FFG-021; Mn-74-02-15-FFG-025; Mn-74-02-16-FFG-030; Mn-74-02-16-FFG-037; Mn-74-02 IDOE DOMES; Moana Wave; MW7401; MW7401-01G01; MW7401-01G02; MW7401-01G03; MW7401-02G04; MW7401-02G06; MW7401-03G07; MW7401-03G09; MW7401-05B02; MW7401-06G16; MW7401-06G17; MW7401-06G18; MW7401-06G19; MW7401-06G20; MW7401-06G21; MW7401-06G22; MW7401-06G23; MW7401-06G25; MW7401-06G26; MW7401-07G28; MW7401-07G29; MW7401-08G32; MW7401-09G36; MW7401-10G37; MW7401-10G38; MW7401-10G39; MW7401-10G42; MW7402; MW7402-13D01; MW7402-13D02; MW7402-13D04; MW7402-13G04; MW7402-13G05; MW7402-13G07; MW7402-13G08; MW7402-13G09; MW7402-13G11; MW7402-13G12; MW7402-15G21; MW7402-15G25; MW7402-16G30; MW7402-16G37; MW7402D-SBT1; MW7402D-SBT2; MW7402D-SBT4; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; TRAWL; Trawl net
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 44
    facet.materialart.
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    PANGAEA
    In:  Supplement to: Usui, Akira; Takenouchi, Sukune; Shoji, Tetsuya (1978): Mineralogy of deep sea manganese nodules and synthesis of manganese oxides: Implications to genesis and geochemistry. Mining Geology, Society of Mining Geologists of Japan, 28(152), 405-420, https://doi.org/10.11456/shigenchishitsu1951.28.405
    Publication Date: 2023-08-28
    Description: Deep sea manganese nodules from the Central Pacific Basin are mainly composed of 10Å manganite and d-MnO2 Two zones equivalent to the minerals are evidently distinguishable according to their optical properties. Microscopic and microprobe analyses revealed quite different chemical compositions and textnral characteristics of the two zones. These different feature of the two zones of nodules suggest the different conditions under which they were formed. Concentrations of 11 metal elements in the zones and inter-element relationships show that the 10Å manganite zone is a monomineralic oxide phase containing a large amount of manganese and minor amounts of useful metals, and that the d-MnO2 zone which is apparently homogeneous under the microscope is a mixture of three or more different minerals. The chemical characteristics of the two zones can explain the variation of bulk composition of deep sea manganese nodules and inter-element relationships previously reported, suggesting that the bulk compositions are attributable to the mixing of the 10Å manganite and d-MnO2 zones in various ratios. Characteristic morphology and surface structure of some types of nodules and their relationships to chemistry are also attribut able to the textural and chemical features of the above mentioned two phases. Synthesis of hydrated manganese oxides was carried out in terms of the formation of manganese minerals in the ocean. The primary product which is an equivalent to d-MnO2 was precipitated from Mn 2+ -bearing alkaline solution under oxigenated condition by air bubbling at one atmospheric pressure and room temperature. The primary product was converted to a l0Å manganite equivalent by contact with Ni 2+, Cu 2++ or CO2+ chloride solutions. This reaction caused the decrease of Ni2+, Cu2+ or CO2+ concentrations and the increase of Na+ concentration in the solution. The reaction also proceeded even in diluted solutions of nickel chloride and resulted in a complete removal of Ni2+ from the solution. Reaction products were exclusively 10Å manganite equivalents and their chemical compositions were very similar to those of 10Å manganite in manganese nodules. The maximum value of(Cu+Ni+Co)/Mn ratio of 10Å manganite zones in manganese nodules is 0.16, and the Ni/Mn ratio of synthetic 10Å manganite ranges from 0.15 to 0.18 with the average of 0.167.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 45
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Sugimura, Y; Miyake, Yasuo; Yanagawa, Hatsue (1975): Chemical composition and the rate of accumulation of ferromanganese nodules in the Western North Pacific. Papers in Meteorology and Geophysics, 26(2), 47-54, https://doi.org/10.2467/mripapers1950.26.2_47
    Publication Date: 2023-08-28
    Description: The major and some of the minor constituents and the rate of accumulation of manganese nodules in the western North Pacific were determined. Manganese concentration in the nodules ranged from 20 to 30 per cent in the acid soluble fraction. As to the rare earth concentration, enrichment of cerium was observed in the manganese nodule as compared with that in shales or sea water. Thorium to uranium ratio in the nodule ranged from 9.4 to 14.3, which was very much higher than that in sea water. From the distribution of excess ionium, excess protactinium and Io/Th ratio, a rate of accumulation of 7 mm per million years was obtained with the surface layer of several mm in thickness of the JEDS-4-E4 nodule.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 46
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    PANGAEA
    In:  Supplement to: Moore, Willard S; Vogt, Peter R (1976): Hydrothermal manganese crusts from two sites near the Galapagos spreading axis. Earth and Planetary Science Letters, 29(2), 349-356, https://doi.org/10.1016/0012-821X(76)90139-4
    Publication Date: 2023-08-28
    Description: Manganese oxide crusts similar to those reported from the Mid-Atlantic Ridge rift valley by Scott et al., 1974 (https://doi.pangaea.de/10.1594/PANGAEA.848726) were dredged at two sites near the Galapagos spreading axis on ocean floor estimated from magnetic anomalies to be 2.4 and 0.3 m.y. old. Compared to the typical ocean-floor manganese deposits attributed to precipitation from seawater, the 2-6 cm thick manganese crusts reported here exhibit very low Fe/Mn and low 232Th/238U ratios, as well as lower transition metal and higher manganese concentrations. The manganese crusts were deposited several orders of magnitude faster than the more common hydrogenous nodules; this fact together with other geochemical characteristics and the geophysical environment suggests the manganese deposits reported here are of hydrothermal origin.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 47
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    PANGAEA
    In:  Supplement to: Glockhoff, Carolyn; Helms, Phyllis B (1975): Descriptions of cores from the Tropical Central Pacific taken on Amphitrite Expedition. Scripps Institution of Oceanography Reference Series, 75-29, 110 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/amphitrite/amphitrite_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken on AMPHITRITE Expedition in Decenber 1963 - February 1964 by Scripps Institution of Oceanography from, the R/V Argo. A total of 148 cores were recovered and are available at Scripps for sampling and study. The coring sites, all in the tropical central Pacific. The AMPHITRITE cores are here briefly described to identify visually distinct units based on lithology, color, texture, or other characteristic unique to an interval of sediment. For determination of lithology, the slides prepared from samples of the cores were examined microscopically in conjuction with the visual examination.
    Keywords: AMP3P; AMPH-001P; AMPH-001PG; AMPH-002P; AMPH-003PG; AMPH-004G; AMPH-005D; AMPH-006D; AMPH-007D; AMPH-009D; AMPH-010P; AMPH01AR; AMPH01AR-001P; AMPH01AR-001PG; AMPH01AR-002P; AMPH01AR-003PG; AMPH01AR-004G; AMPH01AR-005D; AMPH01AR-006D; AMPH01AR-010P; AMPH01AR-027P; AMPH01AR-027PG; AMPH01AR-029GV; AMPH01AR-030P; AMPH01AR-032GV; AMPH01AR-033P; AMPH01AR-033PG; AMPH01AR-035GV; AMPH01AR-038P; AMPH01AR-039P; AMPH01AR-039PG; AMPH01AR-040GV; AMPH01AR-041P; AMPH-027P; AMPH-027PG; AMPH-029GV; AMPH02AR-007D; AMPH02AR-009D; AMPH02AR-048PG; AMPH-030P; AMPH-030PG; AMPH-032GV; AMPH-033P; AMPH-033PG; AMPH-035GV; AMPH-038P; AMPH-039P; AMPH-039PG; AMPH03AR-080G; AMPH03AR-084G; AMPH03AR-085P; AMPH03AR-085PG; AMPH03AR-086G; AMPH03AR-090P; AMPH03AR-091PG; AMPH03AR-092P; AMPH03AR-092PG; AMPH03AR-097P; AMPH03AR-099P; AMPH03AR-100G; AMPH03AR-110PG; AMPH03AR-111PG; AMPH03AR-113G; AMPH03AR-115GV; AMPH03AR-117P; AMPH03AR-118PG; AMPH03AR-120P; AMPH03AR-120PG; AMPH03AR-121P; AMPH03AR-121PG; AMPH03AR-122C; AMPH03AR-123G; AMPH03AR-124C; AMPH03AR-125P; AMPH03AR-125PG; AMPH03AR-126P; AMPH03AR-126PG; AMPH03AR-136GV; AMPH03AR-141G; AMPH-040GV; AMPH-041P; AMPH-048PG; AMPH-080G; AMPH-084G; AMPH-085P; AMPH-085PG; AMPH-086G; AMPH-090P; AMPH-091PG; AMPH-092P; AMPH-092PG; AMPH-097P; AMPH-099P; AMPH-100G; AMPH-110PG; AMPH-111PG; AMPH-113G; AMPH-115GV; AMPH-116P; AMPH-117P; AMPH-118PG; AMPH-120P; AMPH-120PG; AMPH-121P; AMPH-121PG; AMPH-122C; AMPH-123G; AMPH-124C; AMPH-125P; AMPH-125PG; AMPH-126P; AMPH-126PG; AMPH-130G; AMPH-131G; AMPH-132G; AMPH-135GV; AMPH-136GV; AMPH-139GV; AMPH-141G; AMPHITRITE; Argo; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 843 data points
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  • 48
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    PANGAEA
    In:  Supplement to: Frakes, Lawrence A; Exon, Neville F; Granath, J W (1977): Preliminary studies of the Cape Leeuwin manganese nodule deposit off Western Australia. BMR Journal of Australian Geology and Geophysics, 2(1), 66-69, https://pid.geoscience.gov.au/dataset/ga/80911
    Publication Date: 2023-08-28
    Description: In 1970 a large deposit of ferromanganese nodules was discovered on the floor of the Indian Ocean southwest of Cape Leeuwin by the research vessel USNS Eltanin. This discovery, which was based largely on bottom photographs from about 20 stations, was discussed by Frakes (1975) and Kennett and Watkins (1975, 1976). The photographs suggest that the deposit spreads, nearly continuously, over 900 000km^2, and cores showed that the nodules are essentially confined to the sediment surface. Kennett and Watkins (op. cit.) pointed to the abundance of ripple and scour marks and current-formed lineations on the present surface, and of extensive disconformities in the cores, as evidence of strong present and past bottom currents in the region. They suggested that the current action had resulted in very low sedimentation rates, which had allowed the nodule field, named by them (1976) the 'Southeast Indian Ocean Manganese Pavement', to develop. In early 1976 the authors used the research vessel HMAS Diamantina for a 10-day cruise in the region to sample the nodules in order to study their chemistry and mineralogy. During the cruise 9 stations were occupied, 8 of them successfully (Figure 1), and about 2000 nodules were recovered from the sea bed. The apparatus used was a light box dredge on the ships hydrowire, which had a breaking strain of about one tonne. Although an attempt was made to reoccupy Eltanin photographic stations, it should be noted that positioning was by celestial navigation, so errors of up to 10 km are possible.
    Keywords: Cobalt; Copper; DIAM76; DIAM76_NOD-2; DIAM76_NOD-3; DIAM76_NOD-4; DIAM76_NOD-5; DIAM76_NOD-6; DIAM76_NOD-7; DIAM76_NOD-8; DIAM76_NOD-9; Diamantina; Dredge; DRG; Event label; Indian Ocean; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 49
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    PANGAEA
    In:  Supplement to: Calvert, Stephen E; Price, N B (1977): Geochemical variation in ferromanganese nodules and associated sediments from the Pacific Ocean. Marine Chemistry, 5(1), 43-74, https://doi.org/10.1016/0304-4203(77)90014-7
    Publication Date: 2023-08-28
    Description: The major and minor element compositions of a suite of abyssal sea-floor ferromanganese nodules and associated sediments from the eastern central Pacific have been used to examine inter-element relationships and the mineralogy of the nodules, the relationship between the composition of nodules, and their associated sediments and regional variations in composition with respect to likely modes for formation of such deposits. Apart from Mn and Fe, significant proportions of the total Ti, Ca, Mg, K, Ba, Sr, Th and Y and almost all the P, As, Ce, Co, Cu, Mo, Ni, Pb, Zn and Zr are present in the oxide fractions of the nodules. The Mg, Ba, Cu, Mo, Ni and Zn contents are significantly correlated with the total Fe content. Nodules from the northeastern tropical Pacific have Mn/Fe ratios highter than those in the oxide fractions of their associated sediments, todorokite as the principal Mn phase and relatively high concns of minor elements associated with Mn. Nodules from the south central Pacific have Mn/Fe ratios similar to those in the oxide fractions of the associated sediments, {delta}-MnO Sub(2) as the only Mn-phase, and relatively high concns of minor elements associated with Fe. There appears to be a smooth gradation in composition in the tropical Pacific between these 2 end members. The retional compositional variation is interpreted as a reflection of different sources of metals for, and different growth mechanisms of, sea-floor nodules. The oxide precipitate from sea water consists of {delta}-MnO Sub(2), has a relatively low Mn/Fe ratio and minor element contents related to the total Fe and Mn({delta}-MnO Sub(2)) content. The oxide precipitate forming in areas of very low sedimentation as a result of diagenetic remobilisation in the surface sediment consists of todorokite, and has a high Mn/Fe ratio and enhanced metal content in the Mn-(todorokite) phase. Available information on the morphology and compositional variation of individual nodules from the tropical Pacific corroborates these contrasting metal sources and suggests that they can be resolved on the scale of an individual oxide concretion.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 50
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    PANGAEA
    In:  Supplement to: Nohara, Masato (1977): The geochemistry of manganese nodules from the Pacific Ocean. Journal of the Geological Society of Japan, 83(5), 267-276, https://doi.org/10.5575/geosoc.83.267
    Publication Date: 2023-08-28
    Description: Considerable regional variations in the chemical composition of manganese nodules from a wide range of the Pacific Ocean have been observed. These variations can be more exactly expressed in terms of inter-element relationships. In particular, Cu-Mn and Cu-Ni associations reveal that Cu content in pelagic nodules increases rapidly in proportion to those of Mn or Ni. In nodules from continental borderland and hemipelagic areas, even if Mn or Ni contents increase, that of Cu increases only slightly. It is suggested that the considerable chemical differences within individual nodules and between nodules from the same site, at a limited pelagic area where there is no marked change in depositional conditions of nodules, are due to the role of hydrolyzable trace elements in the formation of nodules.
    Keywords: Aluminium; Atomic absorption spectrometry (AAS), Perkin-Elmer; Cobalt; Copper; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Geographical setting; GH76-2; GH76-2-D144; Hakuho-Maru; Hakurei-Maru (1974); Identification; Iron; KH67-5-34; KH67-5-40; KH-68-3; KH68-3-9-16-2; KH68-3-9-6; KH68-3-9-7; KH68-3-9-8; KH68-3-9-9; KH-68-4; KH68-4-33-2; KH68-4-41-2; KH-69-2; KH69-2-1-1; KH69-2-5-1; KH-71-1; KH71-1-3-3a; KH-71-5; KH71-5-12-3; KH71-5-15-3; KH71-5-20-3; KH-72-2; KH72-2-46; KH-76-2; KH76-32-2; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Number of subsamples; OKAD01; OKAD02; Pacific Ocean; Sediment type; SPac_1968-69_HH_170W; SPac_1971_HH_150-100W; Station 441; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 270 data points
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  • 51
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    PANGAEA
    In:  Supplement to: Heye, D (1978): Growth conditions of manganese nodules comparative studies of growth rate, magnetization, chemical composition and internal structure. Progress in Oceanography, 7(5-6), 163-239, https://doi.org/10.1016/0079-6611(78)90001-0
    Publication Date: 2023-08-28
    Description: Twenty-four manganese nodules from the surface of the sea floor and fifteen buried nodules were studied. With three exceptions, the nodules were collected from the area covered by Valdivia Cruise VA 04 some 1200 nautical miles southeast of Hawaii. Age determinations were made using the ionium method. In order to get a true reproduction of the activity distribution in the nodules, they were cut in half and placed for one month on nuclear emulsion plates to determine the alpha-activity of the ionium and its daughter products. Special methods of counting the alpha-tracks resolution to depth intervals of 0.125 mm. For the first time it was possible to resolve zones of rapid growth (impulse growth) with growth rates, s 〉 50 mm/106 yr and interruptions in growth. With few exceptions the average rate of growth of all nodules was surprisingly uniform at 4-9 mm/10 yr. No growth could be recognized radioactively in the buried nodules. One exceptional nodule has had recent impulse growth and, in the material formed, the ionium is not yet in equilibrium with its daughter products. Individual layers in one nodule from the Indian Ocean could be dated and an average time interval of t = 2600±400 yr was necessary to form one layer. The alternation between iron and manganese-rich parts of the nodules was made visible by colour differences resulting from special treatment of cut surfaces with HCl vapour. The zones of slow growth of one nodule are relatively enriched in iron. Earlier attempts to find paleomagnetic reversals in manganese nodules have been continued. Despite considerable improvement in areal resolution, reversals were not detected in the nodules studied. Comparisons of the surface structure, microstructure in section and the radiometric dating show that there are erosion surfaces and growth surfaces on the outer surfaces of the manganese nodules. The formation of cracks in the nodules was studied in particular. The model of age-dependent nodule shrinkage and cracking surprisingly indicates that the nodules break after exceeding a certain age and/or size. Consequently, the breaking apart of manganese nodules is a continuous process not of catastrophic or discontinuous origin. The microstructure of the nodules exhibits differences in the mechanism of accretion and accretion rate of material, shortly referred to as accretion form. Thus non-directional growth inside the nodules as well as a directional growth may be observed. Those nodules with large accretion forms have grown faster than smaller ones. Consequently, parallel layers indicate slow growth. The upper surfaces of the nodules, protruding into the bottom water appear to be more prone to growth disturbances than the lower surfaces, immersed in the sediment. Features of some nodules show, that as they develop, they neither turned nor rolled. Yet unknown is the mechanism that keeps the nodules at the surface during continuous sedimentation. All in all, the nodules remain the objects of their own distinctive problems. The hope of using them as a kind of history book still seems to be very remote.
    Keywords: Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Size; Substrate type; Uniform resource locator/link to graphic; VA-04/1; VA04-114; VA04-115; VA04-123; VA04-156; VA04-162; VA04-170; VA04-196; VA04-54; VA04-62; VA04-65; VA04-77; VA04-81; VA04-84; VA04-86; VA04-87; VA04-89; VA04-92; VA04-93; Valdivia (1961); Visual description
    Type: Dataset
    Format: text/tab-separated-values, 277 data points
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  • 52
    Publication Date: 2023-08-28
    Keywords: Atomic absorption spectrometry (AAS); Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge, box; DRG_B; Elevation of event; Event label; FFGR; Free-fall grab; GH76-1; GH76-1-D137(N); GH76-1-FG12-1; GH76-1-FG12-2; GH76-1-FG15-1; GH76-1-FG16-1; GH76-1-FG16-2; GH76-1-FG17-1; GH76-1-FG17-2; GH76-1-FG19-1; GH76-1-FG19-2; GH76-1-FG20-2; GH76-1-FG22-1; GH76-1-FG22-2; GH76-1-FG25-1; GH76-1-FG25-2; GH76-1-FG27-1; GH76-1-FG27-2; GH76-1-FG28-1; GH76-1-FG28-2; GH76-1-FG29-1; GH76-1-FG29-2; GH76-1-FG31-1; GH76-1-FG5-1; GH76-1-FG5-2; GH76-1-FG6-1; GH76-1-FG6-2; GH76-1-FG7-1; GH76-1-FG9-1; GH76-1-G169; GH76-1-G171; GH76-1-G172; GH76-1-G181; GH76-1-G182; GH76-1-G183; GH76-1-G187; GH76-1-G190; GH76-1-G193; GH76-1-G195; GH76-1-G196; Hakurei-Maru (1974); Identification; Iron; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; O70; Ocean 70 grab; Pacific Ocean; Station 405; Station 407; Station 407A; Station 408; Station 409; Station 411; Station 414; Station 414A; Station 414A-2; Station 417; Station 418; Station 419; Station 423; Station 424; Station 426; Station 429; Station 430; Station 431; Station 433; Water content, wet mass; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 679 data points
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  • 53
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge, box; DRG_B; Elevation of event; Event label; FFGR; Free-fall grab; GH77-1; GH77-1-C11; GH77-1-C12; GH77-1-D211; GH77-1-D212; GH77-1-FG33-1; GH77-1-FG33-1C; GH77-1-FG33-2; GH77-1-FG33-2C; GH77-1-FG34-2; GH77-1-FG34-2C; GH77-1-FG37-1; GH77-1-FG37-1C; GH77-1-FG37-2; GH77-1-FG37-2C; GH77-1-FG39-1; GH77-1-FG39-1C; GH77-1-FG39-2; GH77-1-FG39-2C; GH77-1-FG40-1; GH77-1-FG40-1C; GH77-1-FG40-2; GH77-1-FG40-2C; GH77-1-FG41-1; GH77-1-FG41-1C; GH77-1-FG41-2; GH77-1-FG41-2C; GH77-1-FG42-1; GH77-1-FG42-1C; GH77-1-FG42-2; GH77-1-FG42-2C; GH77-1-FG43-1; GH77-1-FG43-1C; GH77-1-FG43-2; GH77-1-FG43-2C; GH77-1-FG44-1; GH77-1-FG44-1C; GH77-1-FG44-2; GH77-1-FG44-2C; GH77-1-FG45-1; GH77-1-FG45-1C; GH77-1-FG45-2; GH77-1-FG45-2C; GH77-1-FG46-1; GH77-1-FG46-1C; GH77-1-FG46-2; GH77-1-FG46-2C; GH77-1-FG48-1; GH77-1-FG48-1C; GH77-1-FG48-2; GH77-1-FG48-2C; GH77-1-FG49-1; GH77-1-FG49-1C; GH77-1-FG49-2; GH77-1-FG49-2C; GH77-1-FG50-1; GH77-1-FG50-1C; GH77-1-FG50-2; GH77-1-FG50-2C; GH77-1-FG51-1; GH77-1-FG51-1C; GH77-1-FG51-2; GH77-1-FG51-2C; GH77-1-FG52-1; GH77-1-FG52-1C; GH77-1-FG52-2; GH77-1-FG52-2C; GH77-1-FG53-1; GH77-1-FG53-1C; GH77-1-FG53-2; GH77-1-FG53-2C; GH77-1-FG54-1; GH77-1-FG54-1C; GH77-1-FG54-2; GH77-1-FG54-2C; GH77-1-FG55-1; GH77-1-FG55-1C; GH77-1-FG55-2; GH77-1-FG55-2C; GH77-1-FG60-1; GH77-1-FG60-1C; GH77-1-FG60-2; GH77-1-FG61-1; GH77-1-FG61-1C; GH77-1-FG61-2; GH77-1-FG61-2C; GH77-1-FG62-1; GH77-1-FG62-1C; GH77-1-FG62-2; GH77-1-FG62-2C; GH77-1-FG64-1; GH77-1-FG64-2; GH77-1-FG64-2C; GH77-1-FG65-1; GH77-1-FG65-2; GH77-1-FG65-2C; GH77-1-FG66-1; GH77-1-FG66-1C; GH77-1-FG66-2; GH77-1-FG67-1; GH77-1-FG67-1C; GH77-1-FG67-2; GH77-1-FG67-2C; GH77-1-FG68-1; GH77-1-FG68-1C; GH77-1-FG68-2; GH77-1-FG69-1; GH77-1-FG69-1C; GH77-1-FG69-2; GH77-1-FG69-2C; GH77-1-FG70-1; GH77-1-FG70-1C; GH77-1-FG70-2; GH77-1-FG70-2C; GH77-1-FG71-1; GH77-1-FG71-2; GH77-1-FG71-2C; GH77-1-FG71-3; GH77-1-FG71-4; GH77-1-FG71-4C; GH77-1-FG71-5; GH77-1-FG71-6; GH77-1-FG71-7; GH77-1-FG71-7C; GH77-1-FG71-8; GH77-1-FG72-1; GH77-1-FG72-1C; GH77-1-FG72-2; GH77-1-FG72-2C; GH77-1-G373; GH77-1-G376; GH77-1-G378; GH77-1-G379; GH77-1-G380; GH77-1-G381; GH77-1-G383; GH77-1-G384; GH77-1-G385; GH77-1-G387; GH77-1-G388; GH77-1-G389; GH77-1-G390; GH77-1-G391; GH77-1-G392; GH77-1-G393; GH77-1-G394; GH77-1-G397; GH77-1-G402; GH77-1-G403; GH77-1-G405; Hakurei-Maru (1974); Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; O70; Ocean 70 grab; Pacific Ocean; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 836 data points
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  • 54
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    PANGAEA
    In:  Supplement to: Kinoshita, Yasumasa; Moritani, Tomoyuki; Handa, Keiji (1979): Manganese nodule occurrence and benthonic activities observed from deep sea photographs, in: Deep Sea Mineral Resources Investigation in the Central-Western Part of Central Pacific Basin, January-March 1977 (GH77-1 Cruise). Geological Survey of Japan, Cruise Report, 106-130, https://www.gsj.jp/data/cruise-rep/12-08.pdf
    Publication Date: 2023-08-28
    Description: Deep sea photographs in the GH77-1 cruise were obtained by two methods, namely a one-shot 16 mm camera attached to the freefall (boomerang) type photo grab and an independent 35 mm deep sea camera.
    Keywords: Concentration; Coverage; DEPTH, sediment/rock; Elevation of event; Event label; GH77-1; GH77-1-C11; GH77-1-C12; GH77-1-FG33-1C; GH77-1-FG33-2C; GH77-1-FG34-2C; GH77-1-FG37-1C; GH77-1-FG37-2C; GH77-1-FG39-1C; GH77-1-FG39-2C; GH77-1-FG40-1C; GH77-1-FG40-2C; GH77-1-FG41-1C; GH77-1-FG41-2C; GH77-1-FG42-1C; GH77-1-FG42-2C; GH77-1-FG43-1C; GH77-1-FG43-2C; GH77-1-FG44-1C; GH77-1-FG44-2C; GH77-1-FG45-1C; GH77-1-FG45-2C; GH77-1-FG46-1C; GH77-1-FG46-2C; GH77-1-FG48-1C; GH77-1-FG48-2C; GH77-1-FG49-1C; GH77-1-FG49-2C; GH77-1-FG50-1C; GH77-1-FG50-2C; GH77-1-FG51-1C; GH77-1-FG51-2C; GH77-1-FG52-1C; GH77-1-FG52-2C; GH77-1-FG53-1C; GH77-1-FG53-2C; GH77-1-FG54-1C; GH77-1-FG54-2C; GH77-1-FG55-1C; GH77-1-FG55-2C; GH77-1-FG60-1C; GH77-1-FG61-1C; GH77-1-FG61-2C; GH77-1-FG62-1C; GH77-1-FG62-2C; GH77-1-FG64-2C; GH77-1-FG65-2C; GH77-1-FG66-1C; GH77-1-FG67-1C; GH77-1-FG67-2C; GH77-1-FG68-1C; GH77-1-FG69-1C; GH77-1-FG69-2C; GH77-1-FG70-1C; GH77-1-FG70-2C; GH77-1-FG71-2C; GH77-1-FG71-4C; GH77-1-FG71-7C; GH77-1-FG72-1C; GH77-1-FG72-2C; Hakurei-Maru (1974); Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Photo/Video; PV
    Type: Dataset
    Format: text/tab-separated-values, 177 data points
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  • 55
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    PANGAEA
    In:  Supplement to: Piper, David Z; Williamson, M E (1977): Composition of Pacific Ocean ferromanganese nodules. Marine Geology, 23(4), 285-303, https://doi.org/10.1016/0025-3227(77)90036-6
    Publication Date: 2023-08-28
    Description: Bulk composition of ferromanganese nodules from the pelagic environment of the Pacific Ocean is apparently related to nodule-growth rate, sediment-accumulation rate, and biologic productivity in the overlying seawater. Nodules with a high Mn/Fe ratio and high Ni and Cu concns tend to occur in areas where primary productivity in the surface layer of the ocean is high and the sediment accumulation rate low. They may have a Mn/Fe ratio as low as one and accrete at rates as low as 1 mm/10 M yrs. Nodules with a larger Mn/Fe ratio apparently have growth rates that are greater by as much as a factor of 10.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 56
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    In:  Supplement to: Jones, E J W; Goddard, D A (1979): Deep-sea phosphorite of tertiary age from Annan Seamount, eastern equatorial atlantic. Deep Sea Research Part A. Oceanographic Research Papers, 26(12), 1363-1379, https://doi.org/10.1016/0198-0149(79)90004-9
    Publication Date: 2023-08-28
    Description: Phosphatized bioclastic limestones of Early Tertiary age have been dredged from the crest of a seamount in the equatorial Atlantic near 9°N, 21°W. The samples were recovered from water depths of 700 to 970 m but clearly were deposited in a high-energy reefal environment, thus indicating significant Tertiary subsidence. The vertical movement is beleived to reflect reactivation of an old structural line, the Guinée Fracture Zone, which may have had important effects on the transfer of bottom waters of polar origin between the Sierra Leone and Gambia basins. Examination of foraminiferal limestone coating the shallow water material suggests that deep-water conditions were established on the seamount by Middle Miocene time. All phosphatized samples are covered with a layer of ferromanganese oxides which, from textural and faunal evidence, is Palaeocene or Eocene in age and of shallow water origin. Pervasive phosphatization of the bioclastic limestones appears to have been accomplished before the end of the Eocene while the crest of the seamount was near sea level, because Upper Eocene limestone of shallow water facies is unaffected by such radical diagenesis. Phosphatization probably was associated with vigorous upwelling near the seamount and has been taken to an unusually advanced stage, resulting in a phosphoritesof high economic grade. P2O5 contents are in the range of 37 to 41%. The purity of the phosphorites may be related to the intensity of upwelling during the Early Tertiary, but other factors such as the paucity of terrigenous detritus, frequent reworking of the sedimentary capping of the seamount, and a high primary porosity of the limestones may have been important in their information. The Early Tertiary period of phosphorite deposition on the seamount and in northwest Africa ended before the close of Eocene time in both areas, while shallow water conditions prevailed. It is argued that the cessation of phosphorite formation reflects major changes in the surface circulation of the Atlantic during the Eocene.
    Keywords: Annan Seamount, Atlantic Ocean; Atomic absorption spectrometry (Unicam SP90); Calcium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Insoluble residue; Iron; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; Sample ID; Shackleton; Shackleton75/1; Shackleton75/1_1225; Sodium; Substrate type; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 57
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1979): RISE III Expedition, Apri-May 1979, List of Dredge hauls copied from shipboard logs. Scripps Institution of Oceanography, UC San Diego, unpublished, 5 pp, https://www.ngdc.noaa.gov/mgg/curator/data/new_horizon/rise_three/15085006.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described are taken during the R/V New Horizon RISE III Expedition from April until May 1979 by the Scripps Institute of Oceanography. A total of 36 cores and dredges were recovered and are available at Scripps Institute of Oceanography for sampling and study. The goal of this expedition was to accomplish the field work of a combined field and laboratory study aimed at increasing the understanding of the origins and development of young oceanic volcanoes.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; New Horizon; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; RISE3-11D; RISE3-12D; RISE3-13D; RISE3-19D; RISE3-1D; RISE3-20D; RISE3-23D; RISE3-24D; RISE3-25D; RISE3-26D; RISE3-27D; RISE3-28D; RISE3-3D; RISE3-4D; RISE3-5D; RISE3-6D; RISE3-7D; RISE3-8D; RISE3-9D; RISEIII; RSTH; Sample ID; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 169 data points
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  • 58
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    In:  Supplement to: Fuerstenau, D W; Han, K N (1977): Extractive metallurgy (Chapter 12). in: Glasby, G.P. (Ed.), Marine Manganese Deposits. Elsevier, Amsterdam, Netherlands, 357-390, https://doi.org/10.1016/S0422-9894(08)71026-2
    Publication Date: 2023-08-28
    Description: This chapter discusses the formation and distribution of some metals in ocean-floor manganese nodules in the light of the observed data in the literature and thermodynamic and kinetic considerations of the oxidation of metal ions in the oceanic environment. There are, in general, two major schools of thought on the mechanism of incorporation of the minor elements such as nickel, copper, and cobalt with the major elements such as manganese and iron. One is the lattice substitution mechanism and the other the adsorption mechanism. If the mechanism is lattice substitution, extraction of the metal ions is not possible unless the lattice of the major elements is first broken and exchanged with other ions from the bulk solution. Consequently, the leaching behavior of minor elements should display a very close relationship with that of major elements.
    Keywords: 2P-50; 2P-51; 2P-52; Date/Time of event; DEPTH, sediment/rock; DOWNWIND-H; Dredge; DRG; DWHD16; Elevation of event; Event label; Horizon; HRS1; Latitude of event; Longitude of event; Loss on drying; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63; Sample ID; SAN_JUAN_1963; SNJ-DH2; Spencer F. Baird
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 59
    Publication Date: 2023-08-28
    Description: The rate of accumulation of a ferromanganese coating on a fragment of pillow basalt was estimated using a variety of techniques. Unsupported 230 Th activity decrease in the oxide layer, K/A dating of the basalt, fission tracks dating of the glassy layer around the basalt, thickness of the palagonitization rind, and integrated 230 Th activity give ages from approximately 3 x 10-6 years to 5 x 10-3 years. Data suggest that the ferromanganese material formed rapidly (33 mm/10-6 years) and by hydrothermal or volcanic processes.
    Keywords: Alpha spectrometry; DEEPSONDE; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; DPSN02-D3; Dredge; DRG; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Substrate type; Thomas Washington; Thorium-230; Thorium-230, per area; Thorium-230, standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 228 data points
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  • 60
    Publication Date: 2023-08-28
    Keywords: Baker_B; Big-Adam_B; BLM-75; Deposit type; DEPTH, sediment/rock; Description; Dream_B; Dredge; DRG; Event label; Gulf of Mexico; Gyre; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Size; Small-Adam_B; South-Baker_B; Southern-Hospital_B; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 61
    Publication Date: 2023-08-28
    Description: During U.S. Department of Interior, Bureau of Land Management (BLM) public hearings held in 1973, 1974 and 1975 prior to Texas Outer Continental Shelf (OCS) oil and gas lease sales, concern was expressed by the National Marine Fisheries Service, scientists from Texas A&M and the University of Texas and private citizens over the possible environmental impact of oil and gas drilling and production operations on coral reefs and fishing banks in or adjacent to lease blocks to be sold. As a result, certain restrictive regulations concerning drilling operations in the vicinity of the well documented coral reefs and biostromal communities at the East and West Flower Gardens were established by BLM, and Signal Oil Company was required to provide a biological and geological baseline study of the less well known Stetson Bank before a drilling permit could be issued. Considering the almost total lack of knowledge of the geology and biotic communities associated with the South Texas OCS banks lying in or near lease blocks to be offered for sale in 1975, BLM contracted with Texas A&M University to provide the biological and geological baseline information required to facilitate judgments as to the extent and nature of restrictive regulations on drilling near these banks which might be required to insure their protection. In pursuit of this, scientists from Texas A&M University were to direct their attention toward assessments of ground fish populations, unique biological and geological features, substratum type and distribution, and the biotic and geologic relationships between these banks and those farther north.
    Keywords: Baker_B; Big-Adam_B; BLM-75; Deposit type; DEPTH, sediment/rock; Description; Dream_B; Dredge; DRG; Event label; Gulf of Mexico; Gyre; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Size; Small-Adam_B; South-Baker_B; Southern-Hospital_B; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 62
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    In:  Supplement to: Monaco, Andre; Valette, J N; Hoffert, Michel; Picot, P (1979): Héritage et néoformation dans les dépôts volcano-sédimentaires et hydrothermaux avoisinant l'île de Vulcano = Heritage and neoformation in volcanic and hydrothermal sediments surrounding Vulcano Island. Oceanologica Acta, 2(1), 75-89, https://archimer.ifremer.fr/doc/00122/23365/21192.pdf
    Publication Date: 2023-08-28
    Description: The volcanic deposits which surround Vulcano Island may be classified in four phases : a detritic phase, fed from the Island itself and from Sicily; a siliceous and carbonateous organic phase; a neogenesis mineral phase; a precipitation phase. The formation of clay and the mineralization of iron and manganese are the subject of particular study. A number of indications suggest the littoral neogenesis of kaolinite around hydrothermal issues, and the formation of smectite at greater depths. The distribution of iron mineralization in the Baie du Levant follows the physicochemical variations of the environment. Melnikovite, pyrite, marcassite and pyrrhotin are dispersed in aureoles around swallow emission points (fumaroles). Close to the hydrothermal spring, iron precipitates are found in the form of amorphous hydroxydes, while geothite and hematite characterize the deeper area as a whole. Manganese mineralizations are exclusively represented by hydroxides and oxides, locally (about - 250 m) organized as incrustations on. lapilli glasses (micronodules). These would appear to be related to the hydrothermal spring.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Visual description; Vulcano_M; Vulcano Island, Italy
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 63
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    In:  Supplement to: Turekian, Karl K; Cochran, J Kirk; Krishnaswami, Seth; Lanford, W A; Parker, P D; Bauer, K A (1979): The measurement of 10Be in manganese nodules using a tandem Van De Graaff accelerator. Geophysical Research Letters, 6(5), 417-420, https://doi.org/10.1029/GL006i005p00417
    Publication Date: 2023-08-28
    Description: The growth rate of a manganese nodule from the South Atlantic Ocean (Rio Grande Ridge) has been determined using a 10Be profile as measured with a Tandem Van de Graaff accelerator. This rate is 4.5 mm /My. A correlation may exist between the 10Be flux and the Mn flux to nodules.
    Keywords: Atlantic Ocean; Beryllium-10; Beryllium-10/Beryllium-9, standard deviation; Beryllium-10/Beryllium-9 ratio; Beryllium-10 decay; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Identification; Mass, netto; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; RC16; RC16-10RD; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 64
    Publication Date: 2023-08-28
    Keywords: Atomic absorption spectrometry (AAS); Copper; Deposit type; DEPTH, sediment/rock; Description; Event label; FFGR; Free-fall grab; Identification; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; SEAPLAD Seasonal Plankton Dynamics; Shape; VA09; VA09-LOC17; VA09-LOC2; VA09-LOC4; Valdivia (1961)
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 65
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    In:  Supplement to: Neuschütz, D; Scheffler, U; Junghauss, H (1977): Verfahren zur Aufarbeitung von Manganknollen durch Schwefelsäuredrucklaugung = Method for the processing of manganese nodules by sulfuric acid pressure leaching. Erzmetall, 30(2), 61-67, hdl:10013/epic.49444.d001
    Publication Date: 2023-08-28
    Description: A complete processing method has been experimentally developed at laboratory scale for the future extraction of metlas from manganese nodules. The digestion of the nodules is performed by pressured sulfuric acid leaching at 200° C., nickel, copper, cobalt, and zinc being selectively dissolved in solution along with iron and manganese. The subsequent separation and recovery of the valuable metals is carried out with a combination of ion exchange and precipitation processes. Estimates for this methodology based on an annual throughput of 2 million tonnes of manganese nodules should lead to the production of about 24000 tonnes of nickel, 20000 tonnes of copper, and 3000 tonnes of cobalt and zinc. The authors conclude that, despite all uncertainty regarding the metal processing costs and the future metal prices, the exploitation of manganese nodules is economically viable.
    Keywords: Aluminium; Calcium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Grab; GRAB; Identification; Iron; Location 10; Location 6; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample code/label; Sodium; VA-05/1; VA-05/1_06; VA-05/1_10; VA-08/1; VA-08/1-51GB; Valdivia (1961); Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 66
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    In:  Supplement to: Margolis, Stanley V (1975): Manganese Deposits Encountered during Deep Sea Drilling Project, Leg 29, in Subantarctic Waters. In: Kennett, J.P.; Houtz, R.E.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXIX, 1083-1091, https://doi.org/10.2973/dsdp.proc.29.135.1975
    Publication Date: 2023-08-28
    Description: Manganese nodules, micronodules, and crusts were encountered in surface sediments, and at depth, in 6 of the 10 sites drilled during DSDP Leg 29 south of New Zealand and Tasmania. Major concentrations of surface nodule pavements occur on and adjacent to the Campbell Plateau south of New Zealand, south of the Tasman Rise, and in the South Tasman Sea. These deposits are found on top of erosional unconformities, which span tens of millions of years and reflect scouring by strong bottom currents. Micronodules were also found at depth throughout most of these cores. Their occurrence apparently is dependent upon a number of environmental factors.
    Keywords: 29-275; 29-276; 29-277; 29-278; 29-280; 29-280A; 29-281; 29-282; 29-283; 29-283A; 29-284; Antarctic Ocean; Antarctic Ocean/BASIN; Antarctic Ocean/CONT RISE; Antarctic Ocean/PLATEAU; Antarctic Ocean/Tasman Sea; Antarctic Ocean/Tasman Sea/CONT RISE; Antarctic Ocean/Tasman Sea/PLATEAU; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Identification; Latitude of event; Leg29; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 437 data points
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  • 67
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    In:  Supplement to: Ingle, James C; Karig, Daniel E; Bouma, D E; Ellis, C Howard; Haile, N S; Koizumi, I; Moore, J Casey; Ujiie, H; Watanabe, T; White, S M; Yasuii, M; Ling, Hsin Yi (1975): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXI, 927 pp, https://doi.org/10.2973/dsdp.proc.31.1975
    Publication Date: 2023-08-28
    Description: The major purpose of Leg 31 was the scrutiny of tectonic, sedimentologic, volcanic, paleontologic, and paleooceanographic processes operative in arc-marginal basin complexes along with a deciphering of basin history. The 12 sites ultimately occupied during Leg 31 all yielded significant new data bearing on the nature and evolution of the West Philippine Basin, Shikoku Basin, and Sea of Japan. The major objective at sites 290 through 292 was to test the mode and age of origin of the West Philippine Sea with emphasis on the nature of the Central Basin Fault. Sites 294/295 were drilled far to the east of the Central Basin Fault zone in the thin sediment blanket covering deeper portions of the northeastern West Philippine Basin. The other sites were situated in the Sea of Japan.
    Keywords: 31-290; 31-291; 31-294; 31-295; 31-297; 31-299; 31-300; 31-301; 31-302; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg31; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/Japan Sea; North Pacific/Japan Sea/BASIN; North Pacific/Japan Sea/CONT RISE; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/RIDGE; North Pacific/Philippine Sea/TRENCH; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 199 data points
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  • 68
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    In:  Supplement to: Larson, Roger L; Moberly, Ralph; Bukry, David; Foreman, H P; Gardner, James V; Keene, John B; Lancelot, Yves; Luterbacher, Hanspeter; Marshall, M C; Matter, A (1975): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXII, 980 pp, https://doi.org/10.2973/dsdp.proc.32.1975
    Publication Date: 2023-08-28
    Description: The northwestern Pacific Ocean is the largest expanse of old oceanic lithosphere, and so the principal theme of Leg 32 set by the Pacific Advisory Panel was the late Mesozoic history of the Pacific Ocean. The main scientific goals originally set for the leg were to: 1) Determine the development of the very deep sea floor of the western Pacific, including the nature of its basement rocks and the age, lithology, and fossil content of the sedimentary rocks overlying acoustic basement. 2) Establish standard mid-Mesozoic to Recent paleontological-biostratigraphic reference sections for the (present-day) northwest Pacific. 3) Determine the paleolatitude for a specific period of volcanicity on Koko Guyot of the Emperor Seamount Chain.
    Keywords: 32-303; 32-303A; 32-304; 32-306; 32-307; 32-310; 32-310A; 32-311; 32-313; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg32; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; North Pacific/BASIN; North Pacific/CONT RISE; North Pacific/SEAMOUNT; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 216 data points
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  • 69
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    In:  Supplement to: Heirtzler, James R; Taylor, P T; Ballard, R D; Houghton, R L (1977): A Visit to the New England Seamounts: Seamounts, one of the largest topographic features of the ocean floor are largely volcanic, yet their origin is obscure. American Scientist, 65(4), 466-472, http://www.jstor.org/stable/27847969
    Publication Date: 2023-08-28
    Description: In the summer of 1974, upon returning to Woods Hole from the Azores, the submersible Alvin had the opportunity to make brief dives on Corner Rise and the New England seamount chain. This was the first time man had directly viewed the expanse of the Earth between the Mid-Atlantic Ridge and the North of the American continent. Single dives were made on seven seamounts: Corner Rise and Nashville, Gilliss, Rehoboth, Manning, Balanus, and Mytilus.
    Keywords: ALV-518; ALV-519; ALV-520; ALV-521; ALV-522; ALV-523; ALV-524; ALV-525; ALV-526; ALV-527; ALV-528; ALV-529; ALV-530; ALV-532; ALV-533; ALV-534; ALV-537; ALV-538; ALV-539; ALV-540; ALV-541; ALV-542; ALV-543; ALV74; Alvin; Atlantic Ocean; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Grab; GRAB; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
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  • 70
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    In:  Supplement to: Jenkyns, Hugh C (1976): Sediments and Sedimentary History, Manihiki Plateau, South Pacific Ocean. In: Schlanger, S.O.; Jackson, E.D.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIII, 873-890, https://doi.org/10.2973/dsdp.proc.33.134.1976
    Publication Date: 2023-08-28
    Description: The Manihiki Plateau is an elevated area of shallow oceanic crust in the South Pacific; it was formed during Early Cretaceous time by profuse outpourings of basalt. DSDP Holes 317, 317A, and 317B, on which this account is based, are situated in a basinal area on the so called High Plateau, the shallowest part of the volcanic edifice, where depths range between 2000 and 3000 meters. The oldest sediments cored are Lower Cretaceous greenish-black volcaniclastics traversed by reddish-purple clay seams; these deposits commonly show evidence of redeposition, but the only possible shallow-water remains found are very rare bryozoan and echinoderm fragments.
    Keywords: 33-314; 33-315A; 33-317A; 33-318; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg33; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/FAN; North Pacific/TROUGH; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Pacific/PLATEAU; South Pacific/RIDGE; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 71
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    In:  Supplement to: Natland, James H (1976): Petrology of Volcanic Rocks Dredged from Seamounts in the Line Islands. In: Schlanger, S.O.; Jackson, E.D.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIII, 749-777, https://doi.org/10.2973/dsdp.proc.33.126.1976
    Publication Date: 2023-08-28
    Description: Volcanic rocks dredged from the tops of seamounts in the Line Islands and cored from their flanks demonstrate that this is a region of extreme petrologic diversity. Tholeiitic and alkalic basalts were obtained in a single dredge haul and a wide spectrum of alkalic differentiates, including quartz trachytes, and phonolites were dredged or cored elsewhere. Four dredge stations on widely scattered seamounts recovered potassic nephelinites, unlike any other volcanic rocks heretofore found in the ocean basins. These rocks include amphibole and biotite-bearing varieties, some of which are leucite normative.
    Keywords: 7TOW_6; 7TOW06WT; 7TOW06WT-129D; 7TOW-129D; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSDP; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Size; Substrate type; Thomas Washington; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 72
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    In:  Supplement to: Clague, David A (1976): Petrology of Basaltic and Gabbroic Rocks Dredged from the Danger Islands Troughs, Manihiki Plateau. In: Schlanger, S.O.; Jackson, E.D.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIII, 891-911, https://doi.org/10.2973/dsdp.proc.33.135.1976
    Publication Date: 2023-08-28
    Description: Dredging in the Danger Island Troughs, which divide the High and Western parts of the Manihiki Plateau, recovered several fresh pebbles of olivine tholeiite and tholeiite, a single pebble of highly altered gabbroic cumulate, and several dozen pebbles of altered variolitic basalt. Troughs suggests that at one time the troughs were the site of active faulting. A tectonic model for the evolution of the plateau, consistent with a fracture zone origin for the Danger Island Troughs, requires the formation of the Manihiki Plateau at a triple junction of the Pacific, Farallon, and Antarctic plates.
    Keywords: Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSDP; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; SOTW11WT-068D; SOTW-68D; SOUTHTOW; Substrate type; Thomas Washington; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 73
    Publication Date: 2023-08-28
    Description: This DSDP leg was originally conceived by the Antarctic Advisory Panel in order to investigate the geologic histories of the Scotia Arc and of the Argentine Basin. Site 326 (Drake Passage) was drilled in 3812 meters of water about 150 km southeast of Cape Horn. The main objective was to check the magnetic-reversal dating of the opening of Drake Passage by determining basement age. Site 327 is in 2400 meters of water on the western nose of the elevated eastern part of the Falkland Plateau, the Maurice Ewing Bank and was chosen to examine Southern Ocean shallow-water pre-Neogene biostratigraphy. Site 328, in 5103 meters of water in the Malvinas Outer Basin immediately to the east of the Falkland Plateau and to the south of the Falkland Fracture Zone, was chosen to examine correlatives of Argentine Basin acoustic reflectors, to obtain a deep-water southerly biostratigraphic section, and if possible, to date the underlying oceanic basement. Site 330, in 2626 meters of water at the western end of the elongate rise forming the eastern end of the Falkland Plateau, the Maurice Ewing Bank, was selected to elucidate the pre-Aptian history of the Falkland Plateau and to obtain a biostratigraphic section older than that cored at Sites 327 and 329.
    Keywords: 36-326; 36-327; 36-327A; 36-328; 36-328A; 36-328B; 36-330A; Antarctic Ocean/SEDIMENT POND; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg36; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Atlantic/BASIN; South Atlantic/CONT RISE; South Atlantic/PLATEAU; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 320 data points
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  • 74
    Publication Date: 2023-08-28
    Description: DSDP Leg 337 was planned as an attemp at deep penetration of the igneous section of the oceanic crust on the western flank of the FAMOUS (Franco- American Mid-Ocean Undersea Study) area of the Mid-Atlantic Ridge at 36°N. Site 332 is located in Deep Drill Valley approximately 30 km west of the axis of the Mid-Atlantic Ridge at 36°52'N latitude. The principal goal at this site was deep penetration into layer 2 of the ocean crust by multiple re-entry. Site 334 was drilled on a steep east-facing slope in a small, deep basin near the middle of magnetic anomaly 5. In this area, breccias with gabbro and peridotite clasts in a nannofossil-foram ooze matrix are interlayered with the plutonic rocks and may reflect exposure of a melange in or near the Median Valley of the Mid- Atlantic Ridge prior to burial by later basaltic extrusions.
    Keywords: 37-332B; 37-334; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg37; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/BASIN; North Atlantic/VALLEY; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 75
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    In:  Supplement to: Vallier, Tracy L; Salisbury, Matthew H; Sachs, H; Quilty, Patrick G; Hart, Roger A; Benson, William E; Bass, Manuel N; Ade-Hall, James M; Yeats, Robert S; Hart, Stanley R (1976): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIV, 814 pp, https://doi.org/10.2973/dsdp.proc.34.1976
    Publication Date: 2023-08-28
    Description: The Bauer Deep is the depression between the active East Pacific Rise on the west and the extinct Galapagos Rise on the east. The selection of Site 319 was based on a detailed survey of the Bauer Basin during Yaloc-13, Leg 3. Leg 3. It is in a basin about 8 km wide (east-west) at 13°OO.8'S, which is part of a broadly faulted zone on the low western flank of the Galapagos Rise. Site 320 and 321 where located in order to survey the Nazca plate. The objectives for Site 320 were (1) to core basalt continuously as deep as possible, with one and possibly two re-entries; (2) to determine the history of the eastern Nazca plate for the last 30 to 40 m.y., (3) to determine the effectiveness of the Peru-Chile Trench as a barrier to turbidity current dispersal. Site 321 is located on the eastern edge of the Nazca plate immediately south of the Mendafia Fracture Zone. The objectives for Site 321 were similar as those for Site 320.
    Keywords: 34-319; 34-319A; 34-320; 34-320B; 34-321; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg34; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Pacific/BASIN; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 137 data points
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  • 76
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    In:  Supplement to: White, Stan; Warnke, Detlef A; Nilsen, T H; Müller, Carla; Morris, D A; Kharin, Gennady S; Faas, Richard W; Caston, V S D; Bjorklund, Kjell R; Talwani, Manik; Udintsev, Gleb B (1976): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXVIII, 1256 pp, https://doi.org/10.2973/dsdp.proc.38.1976
    Publication Date: 2023-08-28
    Description: Because of its position between the North Atlantic and the Arctic oceans, its young age, small size, and diversity of geological structures, the Norwegian-Greenland Sea provided a unique target for deep drilling on Leg 38 of the Glomar Challenger. From studies of the sediments and basement rocks it was expected to gain insight particularly as to the following: 1) The tectonic framework and evolution of this area with special emphasis on the continental margins and on questions concerned with shifts of spreading axis and existence of foundered continental areas. 2) The youngest times of existence of land bridges between Eurasia and North America and the effect these land bridges had on water circulation and paleoclimates. 3) The date of the initiation of glaciation and dates of glacial advances and retreats. 4) Description of the Tertiary marine microfauna and microflora of the Norwegian-Greenland Sea, which are essentially unknown at present, and investigation of their similarity with microfauna and microflora from other areas.
    Keywords: 38-337; 38-345; 38-347; 38-349; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg38; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/Norwegian Sea/BASIN; North Atlantic/Norwegian Sea/RIDGE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 81 data points
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  • 77
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    In:  Supplement to: Heirtzler, James R (1976): Submersible studies of the Cayman Trough. In: Geodynamics Project U.S. Progress Report - 1976. National Academy of Sciences, Washington D.C., USA; https://catalog.hathitrust.org/Record/007158946, 11-17, https://store.pangaea.de/Projects/NOAA-MMS/Heirtzler_1976_Cayman.pdf
    Publication Date: 2023-08-28
    Description: Scientists from the Woods Hole Oceanographic Institution, the U.S. Navy, the State University of New York at Albany, Wesleyan University, Oregon State University, Dalhousie University, and the Scripps Institution of Oceanography participated in the Cayman Trough expedition durieng 15 ALVIN dives in January and February 1976. The survey focused on a spreading center is a 150-km section of the plate boundary running across the floor of the Cayman Trough, where two tectonic plates are actually moving apart.
    Keywords: AL61100; AL61200; AL61300; AL61500; AL61600; AL61700; AL61900; AL62000; AL62100; AL62200; AL62300; AL62400; AL62500; ALV611; ALV-611; ALV612; ALV-612; ALV613; ALV-613; ALV615; ALV-615; ALV616; ALV-616; ALV617; ALV-617; ALV619; ALV-619; ALV620; ALV-620; ALV621; ALV-621; ALV622; ALV-622; ALV623; ALV-623; ALV624; ALV-624; ALV625; ALV-625; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Grab; GRAB; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 78
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    In:  Supplement to: Perch-Nielsen, Katharina; Supko, Peter R; Boersma, Anne; Bonatti, Enrico; Carlson, Richard L; McCoy, Floyd W; Neprochnov, Yuri P; Zimmerman, H B (1977): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXIX, 1139 pp, https://doi.org/10.2973/dsdp.proc.39.1977
    Publication Date: 2023-08-28
    Description: Unlike most previous Deep Sea Drilling Project cruises, Leg 39 was not scientifically planned as a "theme" cruise, on which a number of sites are drilled to address a single scientific problem area, namely, to improve our knowledge of paleocirculation changes and the overall geologic history of the South Atlantic Ocean. This would be done along more specific objectives: 1) collect a biostratigraphic section on the Ceará Rise (Site 354), determine the nature and age of a prominent reflector there, and determine the nature and age of basement; 2) date basement between magnetic anomalies 32 and 33 in the Argentine Basin (Site 358), and 33 and 34 in the Brazil Basin (Site 355); obtain as complete sedimentary sections as time would permit at the Ceará Rise, Brazil Basin, the Argentine Basin and Sào Paulo Plateau (Site 356).
    Keywords: 39-354; 39-355; 39-356; 39-358; 39-359; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg39; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; South Atlantic/BASIN; South Atlantic/PLATEAU; South Atlantic/SEAMOUNT; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 79
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    In:  Supplement to: Malcolm, Frieda L (1979): Petrography, mineral chemistry and microstructures of gabbros from the Mid-Cayman Rise Spreading Center. Master thesis, University of Albany, 121 pp, https://scholarsarchive.library.albany.edu/cas_daes_geology_etd/56/
    Publication Date: 2023-08-28
    Description: The suite of gabbroic rocks collected by the DSRV ALVIN in 1976 and 1977 from the walls of the Mid-Cayman Rise spreading center were studied in detail to provide the best available data on plutonic rocks sampled directly from the ocean floor. The rock types studied include variably deformed and altered gabbros, orthopyroxene gabbros, olivine gabbros and troctolites, and a few amphibolites. Mineral chemical analyses suggest that the various rock types are representative of a fractionation trend from magnesian troctolites through olivine and clinopyroxene gabbros to iron-enriched orthopyroxene gabbros. Within many individual samples, the primary mineral phases are apparently chemically homogeneous despite sometimes considerable alteration, which suggests reequilibration after original crystallization. Variation in mineral-chemistry across the suite is larger than previously reported for ocean-floor gabbros; this may be due to the larger population of this study. The primary or secondary nature of plagioclase and amphibole must be distinguished in discussions of the igneous processes involved in the genesis of these rocks. In this suite, textural evidence is often inconclusive, and although sodic chemistry is assumed to indicate a secondary origin for plagioclase, no chemical indicator was found to apply to amphiboles. Many different deformation textures are observed in the samples, indicating considerable variation in the conditions of deformation within this slowly accreting ridge environment. Ductile features range from mechanical twins and bent crystals (low strain) to complete recrystallization with a well-developed foliation (high strain). Textures suggestive of cataclasis include zones .1-10 mm wide containing very fine, irregular grains; kinked and cracked grains, usually very undulose; and crosscutting fractures. These textures may occur separately, or next to or overprinting each other. Of the variables controlling the formation of deformation features, temperature and water pressure are most easily estimated. Minimum temperature during deformation is suggested by minimum temperature of formation of mineral assemblages unaffected by this deformation. This temperature is greater than 550°C (epidote-amphibolite facies) for the majority of features observed, although sampling may have introduced a bias away from lower temperature features. Observations suggest enhanced recrystallization where the primary mineralogy has been hydrated to a greater extent. Theoretically, confining pressure for the gabbroic rocks in this suite may have varied from about .3-.9kb; fluid pressure should have been within these limits. Based on mineralogical evidence, cataclastic and ductile textures developed at both high and moderate temperatures. This suggests that strain rates and/or pressure vary considerably within regions where rocks are hot as well as where rocks are cooler, and that after high-temperature deformation some rocks cooled quickly enough to prevent significant recrystallization while others cooled more slowly. These interpretations indicate that the Cayman plutonics were raised to their present position by motions which varied from place to place and time to time, and suggests that the structural history of plutonic.rocks formed at slowly accreting plate boundaries is highly variable and complex.
    Keywords: AL73700; AL73800; AL73900; AL74000; AL74100; AL74200; ALV737; ALV-737; ALV738; ALV-738; ALV739; ALV-739; ALV740; ALV-740; ALV741; ALV-741; ALV742; ALV-742; Alvin; Deposit type; DEPTH, sediment/rock; Description; Event label; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 80
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    In:  Supplement to: Hollister, Charles D; Craddock, Campbell; Bogdanov, Yury A; Edgar, N Terry; Gieskes, Joris M; Haq, Bilal U; Lawrence, James R; Rögl, F; Schrader, Hans-Jürgen; Tucholke, Brian E; Weaver, Fred M; Zhivago, V N (1976): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXV, 999 pp, https://doi.org/10.2973/dsdp.proc.35.1976
    Publication Date: 2023-08-28
    Description: The sites drilled on Leg 35 were selected to study the tectonic relationships and interactions between the Antarctic plate and the Antarctic Peninsula, the Scotia Arc, the southern Andes, and the Chile Ridge. Site 322 was drilled on the eastern end of the Bellingshausen Abyssal Plain where it is bounded by the Hero Fracture Zone to the northeast and the continental rise of Antarctica to the south. Site 323 was centrally located on the abyssal plain, about 30 miles west of the Eltanin Fracture Zone and about 150 miles north of the Antarctic continental rise. Site 324 was located on the gently sloping lower continental rise of Antarctica about 160 miles north of Thurston Island, the closest exposed land.
    Keywords: 35-322; 35-323; 35-324; Antarctic Ocean/CONT RISE; Antarctic Ocean/PLAIN; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg35; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 75 data points
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  • 81
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    In:  Marine Institute, University of Texas, Galvestone
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Event label; Gulf of Mexico; Ida Green; Identification; IG19-3; IG19-3-13; IG19-3-15; IG19-3-41; IG19-3-42; IG19-3-45; IG19-3-46; IG19-3-47; IG19-3-48; IG19-4; IG19-4-54; IG19-4-55; IG19-4-56; IG19-4-57; IG19-4-58; IG19-4-68; IG19-4-72; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
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  • 82
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    In:  Supplement to: Williams, David L; Green, K; van Andel, Tjeerd H; von Herzen, Richard P; Dymond, Jack R; Crane, Kathleen (1979): The hydrothermal mounds of the Galapagos Rift: Observations with DSRV Alvin and detailed heat flow studies. Journal of Geophysical Research: Solid Earth, 84(B13), 7467-7484, https://doi.org/10.1029/JB084iB13p07467
    Publication Date: 2023-08-28
    Description: Ranging in height from gentle hills of less than a meter to steep-sided giants of more than 20 m, the mounds of the Galapagos Rift are spectacular hydrothermal features. Their internal temperatures have been measured at up to 13°C above the bottom water temperature, and total heat flow (conducted plus convected) can be several hundred to several thousand times the normal oceanic values. Fluids, when they discharge from the mound, do so at a very slow rate and at temperatures probably quite near the bottom water temperature. The mounds are principally composed of iron silicates intermixed and incrusted with lesser amounts of manganese oxides. They are generally found in rows, in a uniformly sedimented area above faults or fractures in the crustal rocks which permit fluids to escape from a deep hydrothermal aquifer. The sediment blanket in some way alters the chemistry of the ascending thermal fluids and leads to the development of mounds. The mounds field, covering an area of at least 200 km2 and consisting of thousands of individual mounds, is probably less than 300,000 years old; and many of the mounds may be only a few tens of thousands of years old or less.
    Keywords: AL72500; AL72900; AL73100; AL73400; ALV725; ALV-725; ALV729; ALV-729; ALV731; ALV-731; ALV734; ALV-734; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; SMC; Submersible mounted corer; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 83
    Publication Date: 2023-08-28
    Keywords: Atlantic Ocean; Comment; Core; CORE; D84; D9564; D9566; D9567; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 84
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    In:  Supplement to: Bolli, Hans M; Ryan, William B F; Foresman, J B; Hottman, W E; Kagami, H; Longoria, J F; McKnight, B K; Melguen, M; Natland, J; Proto-Decima, F; Siesser, W G (1978): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XL, 1079 pp, https://doi.org/10.2973/dsdp.proc.40.1978
    Publication Date: 2023-08-28
    Description: From a structural and morphological point of view, the continental margin of southwestern Africa is a middle-aged "pull-apart" or "passive-type" margin which was initially created during the breakup of the supercontinent of Gondwanaland in the Mesozoic. The most important objective of the Leg 40 expedition was the attainment of strata laid down when the newly formed ocean was very young and only a few hundred kilometers wide. Site 361 was drilled at the fall of continental platform into the Cape Basin, to a sub-sea floor depth of 1314 meters and yielded sediments that range in age from upper Eocene to lower Aptian and possibly slightly older.
    Keywords: 40-361; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; File name; Glomar Challenger; Identification; Leg40; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Atlantic; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 85
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    In:  Supplement to: Lancelot, Yves; Seibold, Eugen; Cepek, Pavel; Dean, Walter E; Eremeev, V V; Gardner, J; Jansa, Lubomir F; Johnson, D; Krasheninnikov, Valery A; Pflaumann, Uwe; Rankin, J G; Trabant, P; Bukry, David (1978): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, XLI, 1259 pp, https://doi.org/10.2973/dsdp.proc.41.1978
    Publication Date: 2023-08-28
    Description: he forty-first cruise of Glomar Challenger was devoted to the study of the evolution of the eastern basins of the North Atlantic, off the continental margin of West Africa. As the available data a the time was showing that most litho-stratigraphic units in the deep basins of the Atlantic had enough lateral extension, the drilling of a limited number of sites in key areas would allow for large-scale regional interpretation. One of the sites was loacted in the Cape Verde deep Basin (Site 367) while others were located in shallower waters such as, the Sierra Leone Rise (Site 366), the Cape Verde Rise (Site 368) or the Continental Slope off Spanish Sahara (Site 369).
    Keywords: 41-366; 41-366A; 41-367; 41-368; 41-369; 41-369A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg41; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/CONT SLOPE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 526 data points
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  • 86
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    In:  Supplement to: Udintsev, Gleb B; Kharin, Gennady S (1978): Sedimentary Rocks of the Jan-Mayen Ridge. In: Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, Supl., U.S. Government Printing Office, 38/39/40/41, 21-161, https://doi.org/10.2973/dsdp.proc.38394041s.109.1978
    Publication Date: 2023-08-28
    Description: On cruises 10 and 15 of Academic Kurchatov (1971, 1973) at the Jan-Mayen Ridge, a large number of samples was obtained. Most of them contained sedimentary rocks. From their study, it is safe to assume that the rocks of the Jan-Mayen Ridge were, at first, subjected to subsidence to a considerable depth, and then uplifted to their contemporary position, by the ascending tectonic movements. Thus, the Jan-Mayen Ridge is in contrast to other Atlantic submarine ridges, not only in the sedimentary rock composition, but in the character of the tectonic movements.
    Keywords: AK10-794-3B; AK10-794-3C; AK10-799-1; AK10-799-2; AK10-800; AK10-801; Akademik Kurchatov; AKU10; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Identification; Jan Mayen Ridge; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 64 data points
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  • 87
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    In:  Supplement to: McCave, I Nick; Demars, Kenneth R; Kendrick, J W; Okada, Hisatake; McNulty, C L; Kaneps, Ansis G; Galehouse, J S; Houghton, R L; Rothe, Peter; Murdmaa, Ivar O; Tucholke, Brian E; Vogt, Peter R (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIII, 1115 pp, https://doi.org/10.2973/dsdp.proc.43.1979
    Publication Date: 2023-08-28
    Description: Leg 43 was planned to examine a wide variety of geological problems at numerous sites in the deep western North Atlantic basin. A variety of objectives were to be addressed on Leg 43,among these: 1) to investigate the sedimentary development of the North American basin, 2) to recover sediments containing late Mesozoic and Cenozoic fossils for biostratigraphic, paleobiogeographic, and paleoceanographic studies 3) to recover samples of basaltic basement from the smooth crest of the basement ridge associated with the northern part of the New England seamounts, 4) To examine the age and nature of volcanism on Bermuda and along the New England seamount chain, in order to test ideas on volcanic* origin such as the "hotspot" hypothesis, and to examine volcaniclastic lithofacies and assess the role of volcanic sources for certain North Atlantic sediments.
    Keywords: 43-384; 43-385; 43-386; 43-387; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg43; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; North Atlantic/RIDGE; North Atlantic/SEAMOUNT; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 88
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    In:  Supplement to: Worstell, Paula J; Mélières, Frédéric; Bernoulli, Daniel; Erickson, A J; Wright, Ramil; Bizon, G; Cita, Maria Bianca; Müller, Carla; Kidd, Robert B; Fabricius, F H; Garrison, Robert E; Hsü, Kenneth J; Montadert, Lucien (1978): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLII Pt. 1, 1249 pp + 1244 pp, https://doi.org/10.2973/dsdp.proc.42-1.1978
    Publication Date: 2023-08-28
    Description: Leg 42, Part 1 of the Deep Sea Drilling Project was scheduled to continue the geological exploration of the Mediterranean. The strategy was to search for areas where the Mediterranean Evaporite formation had been largely or completely removed by erosion, such is the case for Site 372. For Leg 42, Part 2, the project entered the Black Sea. In particular, Site 379 was located the central portion of the Black Sea.
    Keywords: 42-372; 42-379A; Black Sea; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg42; Mediterranean Sea/BASIN; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 89
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    PANGAEA
    In:  Supplement to: Bryan, Wilfred B; Sargent, John R (1979): Basalt from 22°23°N, Mid-Atlantic Ridge Median Valley. In: Melson, W.G.; Rabinowitz, P.D.; et al., Initial Reports of the Deep Sea Drilling Project, 45, U.S. Government Printing Office, 45, 653-655, https://doi.org/10.2973/dsdp.proc.45.140.1979
    Publication Date: 2023-08-28
    Description: This paper summarizes the petrography and major element chemistry of basalt collected by R/V Atlantis II at 23 °N, and compare these data with published data for 22 °N and with the preliminary shipboard data for DSDP Sites 395 and 396, in order to define the regional petrologic setting of the Leg 45 basalts.
    Keywords: A209201; AII-92-1PC; AII-92-1PG; AII-92-4PC; AII-92-4PG; AII-92-4RD; AII-92-5PC; AII-92-5RD; AII-92-6RD; AII-92-7PC; AII-92-7RD; ATII92; Atlantic Ocean; Atlantis II (1963); Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 146 data points
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  • 90
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    In:  Supplement to: Honnorez, Jose J; Böhlke, John Karl; Honnorez-Guerstein, B-M (1979): Petrographical and Geochemical Study of the Low Temperature Submarine Alteration of Basalt from Hole 396B, Leg 46. In: Dmitriev, L.; Heirtzler, J.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLVI, 299-329, https://doi.org/10.2973/dsdp.proc.46.120.1979
    Publication Date: 2023-08-28
    Description: A combined mineralogical, petrological, and geochemical study of altered basaltic rock samples of the upper oceanic crust from Hole 396B IPOD Leg 46. The hole was drilled on the west flank of the Mid-Atlantic Ridge, in anomaly 5 at about 23°N. The site is located in a sediment pond at a water depth of 4450 meters; 205 meters of pillow lavas intercalated with indurated ooze and one exceptionally thick lava unit (sill or flow?) were drilled.
    Keywords: 46-396B; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; File name; Glomar Challenger; Identification; Leg46; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 81 data points
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  • 91
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    PANGAEA
    In:  Supplement to: Zolotarev, Boris P; Rhodes, M; Prosser, Egfrid; Natland, James H; Lawrence, James R; Johnson, Harlan; Graham, Andrew L; Fujii, Toshitsugu; Bougault, Henri; Melson, William G; Rabinowitz, Philip D (1979): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLV, 717 pp, https://doi.org/10.2973/dsdp.proc.45.1979
    Publication Date: 2023-08-28
    Description: Leg 45 of the Deep Sea Drilling Project was the inaugural cruise of the International Phase of Ocean Drilling. Its primary scientific objective was to develop an understanding of the composition, structure, and origin of oceanic crust by drilling as deeply into it as technology would permit. The feasibility of drilling deep into the oceanic crust was demonstrated during Leg 37 when one hole was drilled 586 meters into basaltic volcanic rocks near the crest of the Mid-Atlantic Ridge at about 37 °N. The areas of principal interest for Leg 45 were survey areas AT-5, situated near 23 °N, 46 °W and AT-6 near 23 °N, 43°W. The two survey areas are on opposite sides of the Mid-Atlantic Ridge, south of the Kane fracture zone. During Leg 45, Holes 395 and 395A were drilled in survey area AT-5 and Hole 396, was drilled in survey area AT-6.
    Keywords: 45-395; 45-395A; 45-396; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg45; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/SEDIMENT POND; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 125 data points
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  • 92
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    PANGAEA
    In:  Supplement to: Benson, William E; Enos, Paul; Freeman, Tom; Gradstein, Felix M; Murdmaa, Ivar O; Pastouret, L; Schmidt, Ronald R; Sheridan, Robert E; Stuermer, D H; Weaver, Fred M; Worstell, Paula J (1978): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIV, 1005 pp, https://doi.org/10.2973/dsdp.proc.44.1978
    Publication Date: 2023-08-28
    Description: The western part of the North Atlantic Ocean holds clues to some of the most intriguing questions in marine geology. But because the geologic problems are many and varied, the sites of Leg 44 were multipurpose in nature. In particular, some of the targets were : 1) the Blake Nose, a spur of the Blake Plateau, to determine the nature, age, and origin of reef-like structures recognized on seismic profiles and 2) the Blake Outer Ridge, a long low ridge of sediments that forms the eastern boundary of the Blake-Bahama Basin, where we hoped to study the stratigraphy and sample supposed clathrates.
    Keywords: 44-389; 44-390; 44-390A; 44-392; 44-392A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg44; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 188 data points
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  • 93
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    PANGAEA
    In:  Supplement to: Montadert, Lucien; Roberts, David G; Auffret, Gérard A; Bock, W D; Dupeuble, P A; Hailwood, Ernie A; Harrison, William E; Kagami, H; Lumsden, D N; Müller, C M; Schnitker, Detmar; Thompson, T L; Timofeev, Pyotr P (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLVIII, 1183 pp, https://doi.org/10.2973/dsdp.proc.48.1979
    Publication Date: 2023-08-28
    Description: Unlike many cruises of the Deep Sea Drilling Project, Leg 48 was scientifically planned to drill a number of sites to systematically address the problems of passive margin evolution. Site 400 was drilled at the foot of the Meriadzek Escarpment of North Biscay in 4399 meters depth. The site was located in a half-graben forming part of a succession of tilted and rotated fault blocks near the continent/ocean boundary. Site 401 was situated on the planated edge of a tilted fault-block underlying the southern edge of the Meriadzek Terrace on the north Biscay margin. Site 402 was located on the upper slope of the northern continental margin of the Bay of Biscay. The main objectives were to establish the presence or absence of shallow water Upper Cretaceous beds, and to penetrate pre-Aptian synrift sediments and the upslope equivalent of the deep water Albian-Aptian carbonaceous mudstones penetrated at Hole 400A.
    Keywords: 48-400A; 48-401; 48-402; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg48; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/BASIN; North Atlantic/SLOPE; North Atlantic/TERRACE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 67 data points
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  • 94
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    In:  Supplement to: Luyendyk, Bruce P; Cann, Joe R; Sharman, G; Roberts, W P; Shor, A N; Duffield, W A; Varet, J; Zolotarev, Boris P; Poore, Richard Z; Steinmetz, J C; Kobayashi, Kazuo; Vennum, W; Wood, D A; Steiner, M (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIX, 1020 pp, https://doi.org/10.2973/dsdp.proc.49.1979
    Publication Date: 2023-08-28
    Description: Leg 49 of the International Phase of Ocean Drilling (IPOD) was designed with a wide spectrum of problems in mind. Topics investigated were (1) variation with time of mantle sources of spreading-center magmas, (2) aging of the volcanic layer, (3) degree of hydrothermal alteration and metamorphism of the volcanic layer, (4) lateral and vertical variation of the petrochemistry, magnetic properties, and structure of the volcanic layer, (5) north-south variability of spreading-center magmas through the North Atlantic, (6) initiation of glaciation during the late Pliocene, and (7) the influence of bottom currents originating at the Iceland-Faeroes Ridge on sediments of the ridge flank province of the western North Atlantic.
    Keywords: 49-407; 49-408; 49-410; 49-412; 49-412A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg49; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/FRACTURE ZONE; North Atlantic/RIDGE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 99 data points
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  • 95
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    In:  Supplement to: Lonsdale, Peter (1976): Abyssal circulation of the southeastern Pacific and some geological implications. Journal of Geophysical Research, 81(6), 1163-1176, https://doi.org/10.1029/JC081i006p01163
    Publication Date: 2023-08-28
    Description: The abyssal circulation of the Pacific Ocean east of the East Pacific Rise is deduced from hydrographic data, supported by a few direct current measurements. Two main flow paths are recognized: across the Chile Rise into the Chile Basin, and thence northward into the Peru Basin and Panama Basin; and eastward across the East Pacific Rise into the Guatemala Basin and into Bauer Basin. Transform fault troughs are important passages allowing flow across the rises, and the Peru-Chile Trench is the principal channel for inflow to the Peru and Panama basins. The deep water that flows across the East Pacific Rise near the equator has a similar temperature structure to that in the southern Chile Basin, but it is less saline and has lower oxygen concentrations. Along both flow paths the bottom waters become warmer, less saline, and less oxygenated as a result of vertical mixing (intensified near sills), geothermal heating (concentrated at active spreading centers) and in situ decay of organic matter (especially beneath productive surface waters). The regional pattern of abyssal circulation may partly control the distribution of metalliferous pelagic sediments (including both fine-grained precipitates and manganese nodules) and the rates of dissolution of calcareous sediments. Where the deep thermohaline flow is accelerated in narrow passages between basins it has deeply eroded the sea floor and transports sediment as bed load. Steady currents measured in one of these passages exceeded 30 cm/s.
    Keywords: CCTW-03D; COCOTOW; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; East Pacific Ocean; File name; Identification; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 96
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    PANGAEA
    In:  Supplement to: Lonsdale, Peter; Spiess, Fred N (1979): A pair of young cratered volcanoes on the East Pacific Rise. The Journal of Geology, 87(2), 157-173, http://www.jstor.org/stable/30060250
    Publication Date: 2023-08-28
    Description: 35 km either side of the Pacific-Cocos spreading axis at 846'N, on crust 0.6 x 10SUP-6 years old, a pair of small seamounts rises 1.4 km above the faulted terrain of young abyssal hills. A high-resolution traverse made with the sonars and cameras of a deeply towed vehicle shows that the seamounts are inactive volcanoes, with concave side slopes that steepen upwards to 30, and then abruptly flatten at 2-4 km wide summits. Ledges of pillow basalt outcrop on the lower slopes, and form some talus slopes, but the superficial rock of the upper slopes appear to be mainly hyaloclastite. A transponder-navigated deep-tow survey at the summit area of the eastern seamount mapped an asymmetric caldera containing 3 pit craters, which have vertical walls and flat floors. Dredging across the caldera floor recovered hyaloclastite, angular fragments of primitive tholeiite, and manganese nodules. The paired seamounts probably had a common origin at a 'hot spot' on the spreading axis; continued to grow after they were split by sea-floor spreading; and became extinct and suffered summit collapse after they spread too far from their magma source.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; East Pacific Ocean; File name; Identification; Indomed_leg_1; INMD-1-4C; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 21 data points
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  • 97
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    PANGAEA
    In:  Supplement to: LaRock, P A; Ehrlich, H L (1975): Observations of bacterial microcolonies on the surface of ferromanganese nodules from blake plateau by scanning electron microscopy. Microbial Ecology, 2(1), 84-96, https://doi.org/10.1007/BF02010383
    Publication Date: 2023-08-28
    Description: Examination of the surface of freshly collected ferromanganese nodules by scanning electron microscopy revealed the presence of microcolonies of rod- and coccus-shaped bacteria which appeared to be anchored to the nodule surface by slime. The attachment of microcolonies by slime to the surface of freshly collected nodules argues against their being contaminants introduced during nodule collection or processing. These results corroborate cultural and biochemical detection of bacteria on ferromanganese nodules.
    Keywords: Blake Plateau, Atlantic Ocean; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; E-9-73; EASTW-973-D1; EASTW-973-D2; Eastward; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Expected Availability
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  • 98
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    PANGAEA
    In:  Supplement to: Hekinian, Roger; Hoffert, Michel (1975): Rate of palagonitization and manganese coating on basaltic rocks from the Rift Valley in the Atlantic Ocean near 36°50′N. Marine Geology, 19(2), 91-109, https://doi.org/10.1016/0025-3227(75)90056-0
    Publication Date: 2023-08-28
    Description: Various types of rocks consisting of plagioclase basalts, olivine basalts, pyroxene basalts, picritic basalts and volcanoclastics were found in the Rift Valley between 36°52'N and 36°47'N in the Atlantic Ocean. Palagonite and manganese are the main coating materials encountered on the chilled margins of the pillow-lava fragments. Palagonite is often associated with montmorillonite and chlorite. The thickness of palagonite coating the chilled margins increases in the fragments found from the innerfloor axis towards the walls of the Rift Valley. There is a linear correlation between the thickness of palagonite and that of the manganese encrustation. Considering a rate of manganese and palagonite accumulation of about 3my/10**3 year it is speculated that the age of a hill located near the axis of the inner floor near 36°50'N is between 3,000 and 12,000 years. The relative age of the inner floor near the intersection of the Rift Valley walls is less than 120,000 years. The specimens having a thicker manganese and palagonite crust located at 4-6 km away from the inner floor axis are 130,000–482,000 years old.
    Keywords: Archimède (Submersible); CHAR31-DR10; CHAR31-DR11; CHAR31-DR2; CHAR31-DR3; CHAR31-DR6; CHAR31-DR7; CHAR31-DR9; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; FAM73-07-01; FAM73-10-02; FAM73-10-03; FAM73-13-04; FAMOUS73; Identification; Jean Charcot; MIDLANTE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Rift Valley, Atlantic Ocean; ROCK; Rock sample; Sediment type; Size; Substrate type; Thickness; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 187 data points
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  • 99
    Publication Date: 2023-08-28
    Description: The 286 site is located in the gap between the North and South New Hebrides trenches near the foot of the slope down from Malekula (100 km west of the island) and 370 km north of Mare in the Loyalty Island. The main objectives at the site were: 1) To determine when detritus was first shed into this basin from Malekula and thereby determine when the trench was destroyed and whether the island has moved into its present position in relatively recent time. 2) To determine the time of generation of the sea floor and compare it with that of the South Fiji Basin The Ontong-Java Plateau is underlain by a region of unusual oceanic crust that has an estimated maximum thickness of 40 km. Site 288 was located on the eastern flank of the plateau with the hope that the nature of the basement of the plateau could be determined.
    Keywords: 30-285; 30-286; 30-288A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg30; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; South Pacific; South Pacific/BASIN; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 216 data points
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  • 100
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    PANGAEA
    In:  Supplement to: Kuypers, E P; Denyer, P C (1979): Volcanic exhalative manganese deposits of the Nicoya ophiolite complex, Costa Rica. Economic Geology, 74(3), 672-678, https://doi.org/10.2113/gsecongeo.74.3.672
    Publication Date: 2023-08-28
    Description: In Costa Rica the manganese deposits are an integral part of the Nicoya ophiolite complex. They contain both primary mineralization and, due to weathering, small residual concentrations. The most common manganese minerals in surface outcrops are psilomelane and pyrolusite. Most of them exist in jasper bodies often in a form of breccia in contact with underlaying basalt. In some instances stratiform manganese-oxide crusts and nodule deposits cap jasper bodies and stratabound deposits being overlain by radiolarites.
    Keywords: Conchal, Costa Rica; Curiol_K; Deposit type; DEPTH, sediment/rock; Description; Event label; File name; Huacas, Costa Rica; Identification; Los_Limones_K; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pavones_K; Playa_Real_K; Position; Quantity of deposit; San Pablo, Costa Rica; Santa Rosa,Costa Rica; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
    Location Call Number Expected Availability
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