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  • PANGAEA
  • 1980-1984  (160)
  • 1984  (160)
Collection
Keywords
Years
  • 1980-1984  (160)
Year
  • 1
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    PANGAEA
    In:  Supplement to: Sancetta, Constance A; Silvestri, Shaymaria (1984): Diatom stratigraphy of the late Pleistocene (Brunhes) subarctic Pacific. Marine Micropaleontology, 9(3), 263-274, https://doi.org/10.1016/0377-8398(84)90016-1
    Publication Date: 2024-05-02
    Description: Three piston cores in the subarctic region of the North Pacific show consistent changes in relative abundance of diatom species throughout the Brunhes magnetic epoch. These events can be used both as stratigraphic markers to subdivide the interval and as indicators of oceanographic conditions. The stratigraphic record shows an acme for A. ochotensis from about 625-350 Kyr (Isotope Stages 15-10); a marked increase in amplitude of abundance fluctuations for R. hebetata 300-0 Kyr (Stages 8-1), the extinction of R. curvirostris at 276 Kyr (Stage 8), and abundance fluctuations of D. seminae roughly in phase with the global oxygen isotope record from 450-0 Kyr (Stages 12-1). In the subarctic Pacific, an abrupt change in species abundance is not a reliable indicator of hiatus occurrence. Although details are not clear, there appears to have been a fundamental change of the subarctic gyre during the middle Brunhes (Stages 10-8 time), with more intense glacial intervals and stronger glacial-interglacial contrast occurring after that time. Coarse clastic detritus is not restricted to glacial intervals, suggesting that ice-rafting has occurred throughout the Brunhes interval; peak levels of ice-rafting may occur during ice-growth and decay, as well as during short intervals within a stage.
    Keywords: Age model; Calculated; DEPTH, sediment/rock; Lamont-Doherty Earth Observatory, Columbia University; LDEO; PC; Piston corer; RC10; RC10-216; Robert Conrad; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 2
    Publication Date: 2024-04-27
    Keywords: 79-544A; 96KD; Age, 40K/40Ar Potassium-Argon; Age, dated; Age, dated standard deviation; Argon-40; Argon-40, standard deviation; Charge; Deep Sea Drilling Project; Dredge, box; DRG_B; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Flame photometry; Glomar Challenger; Latitude of event; Leg79; Lithology/composition/facies; Longitude of event; Mass spectrometry; North Atlantic/PLATEAU; off West Africa; PC; Piston corer; Potassium; Potassium, standard deviation; Replicates; Sample code/label; Size fraction; V30; V30-225; VA-28/2; VA79-96KD; Valdivia (1961); Vema
    Type: Dataset
    Format: text/tab-separated-values, 194 data points
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  • 3
    Publication Date: 2024-04-27
    Keywords: 79-544A; Albite; Aluminium oxide; Anorthite; Apatite; Barium; Biotite; Calcite; Calcium oxide; Calculated; Cerium; Chromium; CIPW Norm; Cobalt; Copper; Deep Sea Drilling Project; Diopside; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epidote; Glomar Challenger; Hypersthene; Ilmenite; Iron oxide, Fe2O3; Leg79; Lithology/composition/facies; Loss on ignition; Magnesium oxide; Magnetite; Manganese oxide; Molybdenum; Muscovite; Nickel; Niobium; North Atlantic/PLATEAU; Orthoclase; Phosphorus pentoxide; Potassium oxide; Quartz; Rubidium; Sample code/label; Sample code/label 2; Silicon dioxide; Sodium oxide; Strontium; Sum; Thorium; Titanium dioxide; Total; Tungsten; Vanadium; Wollastonite; X-ray fluorescence (XRF); Yttrium; Zinc; Zircon; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Kreuzer, H; Müller, P; Wissmann, Gerd; Reinecke, T (1984): Petrography and K-Ar dating of the Mazagan granodiorite, Deep Sea Drilling Project Leg 79, Holes 544A and 547B. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 543-549, https://doi.org/10.2973/dsdp.proc.79.118.1984
    Publication Date: 2024-04-27
    Description: Gneissic granodiorite was recovered by drilling at the base of the Mazagan escarpment, 100 km west of the Casablanca, Morocco, at 4000 m water depth. Coarse, predeformative muscovite yielded dates of -515 Ma, fine-grained muscovite of -455 Ma, biotite -360 and 335 Ma, and feldspar -315 Ma. These dates are tentatively correlated with the microscopic results. We assume a minimum age of middle Cambrian for the granodiorite, an Ordovician deformation and mylonitization, and a Late Carboniferous overprint under upper greenschist facies conditions.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    Publication Date: 2024-04-16
    Keywords: Alpha spectrometry; Barium; BC; Box corer; Copper; Counting, palynology; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; Event label; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; K7905; K7905-054BC; K7905-062BC; K7905-066BC; K7905-075BC; K7905-091BC; K7905-101BC; K7905-104BC; Knorr; Manganese; MANOP; MANOP Site S, Pacific Ocean; Mass; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Radium-226; Sample surface; Size; Substrate type; Thorium-228/Thorium-232 activity ratio; Thorium-230; Thorium-232; Visual description; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 298 data points
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  • 6
    Publication Date: 2024-04-16
    Keywords: Alpha spectrometry; Barium; BC; Box corer; Copper; Deposit type; DEPTH, sediment/rock; Description; Event label; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; K7905; K7905-054BC; K7905-062BC; K7905-066BC; K7905-075BC; K7905-091BC; K7905-101BC; K7905-104BC; Knorr; Manganese; MANOP; MANOP Site S, Pacific Ocean; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Radium-226; Thorium-228/Thorium-232 activity ratio; Thorium-230; Thorium-232; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 79 data points
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  • 7
    Publication Date: 2024-04-16
    Keywords: Alpha spectrometry; BC; Box corer; Copper; Deposit type; DEPTH, sediment/rock; Description; Event label; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; K7905; K7905-054BC; K7905-062BC; K7905-075BC; K7905-101BC; K7905-106BC; Knorr; Manganese; MANOP; MANOP Site S, Pacific Ocean; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Radium-226; Thorium-228/Thorium-232 activity ratio; Thorium-230; Thorium-232; Visual description; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Moorby, S A; Cronan, David S; Glasby, Geoffrey P (1984): Geochemistry of hydrothermal Mn-oxide deposits from the S.W. Pacific island arc. Geochimica et Cosmochimica Acta, 48(3), 433-441, https://doi.org/10.1016/0016-7037(84)90272-2
    Publication Date: 2024-04-16
    Description: Hydrothermal Mn-oxide crusts have been removed from the Tonga-Kermadec Ridge, the first such hydrothermal deposits to be reported in the S.W. Pacific island arc. In several respects the deposits are similar to hydrothermal Mn-crusts from oceanic spreading centre settings. They are limited in areal extent, comprise well-crystalline birnessite and generally display extreme fractionation of Mn from Fe. They are strongly depleted in many elements compared to hydrogenous Mn deposits but are comparatively enriched in Li, Zn, Mo and Cd. The Group IA and Group IIA metals show strong intercorrelations and the behaviour of Mg in the purest samples may indicate the extent to which normal seawater has influenced the composition of the deposits. Certain aspects of the deposits are not typical of hydrothermal Mn deposits. In particular at least some of the crusts have developed on a sediment or unconsolidated talus substrate. Some crusts, or specific layers within some crusts, display a chemical composition which suggests a significant input from normal seawater.
    Keywords: Aluminium; Cadmium; Calcium; Cobalt; Copper; DISTANCE; Dredge; DRG; Event label; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Latitude of event; Lithium; Longitude of event; Magnesium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-1122; Potassium; Sample code/label; Sample comment; Silicon dioxide; Sodium; Strontium; TANG1122-U23; TANG1122-U24; Tangaroa (1960); Titanium; Tonga-Kermadec ridge; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 851 data points
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  • 9
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    PANGAEA
    In:  Supplement to: van Zinderen Bakker, Eduard M (1984): Palynological evidence for late Cenozoic arid conditions along the Namibia Coast from Holes 532 and 530A, Leg 75, Deep Sea Drilling Project. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 763-768, https://doi.org/10.2973/dsdp.proc.75.116.1984
    Publication Date: 2024-03-06
    Description: Some samples from DSDP Holes 530A and 532 were analyzed for their fossil pollen content. The sites are located in the southeastern corner of the Angola Basin, about 200 km west of the present coastline. Fossil pollen assemblages of Holocene to Miocene age were compared with present-day pollen deposition in the arid Namib sand sea. The strong resemblance of all the pollen spectra indicates that very arid conditions existed in the coastal region of Namibia in Quaternary and Pliocene times. These data are in agreement with the late Miocene origin of the coastal aridity and with the conception that upwelling of cold water was responsible for these desert conditions.
    Keywords: 75-530A; 75-532; Acacia; Acanthaceae; Acanthosicyos; Aizoaceae; Anacardiaceae; Boraginaceae; Cardiospermum; Celastraceae; Chenopodiaceae; Combretaceae; Commiphora; Compositae, pollen; Cruciferae; Cycadaceae; Cyperaceae; Deep Sea Drilling Project; Dichrostachys; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ephedripites; Epoch; Ericaceae; Euclea; Euphorbiaceae; Event label; Geranium; Glomar Challenger; Gramineae; Hypoestes; Justicia; Leg75; Leguminosae; Liliaceae; Malvaceae; Myrica; Olea; Palmae; Podocarpus; Replicates; Restionaceae; Rubiaceae; Sample, optional label/labor no; Sample code/label; see reference(s); South Atlantic; South Atlantic/RIDGE; Sparganicaeae; Spores; Tribulus, pollen; Typha; Umbelliferae; Varia
    Type: Dataset
    Format: text/tab-separated-values, 528 data points
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  • 10
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; DEPTH, sediment/rock; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-1; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; M51; Mass spectrometer Finnigan MAT 251; Meteor (1964); SL
    Type: Dataset
    Format: text/tab-separated-values, 238 data points
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  • 11
    Publication Date: 2024-02-03
    Keywords: AGE; D-Alloisoleucine; D-Alloisoleucine/L-Isoleucine ratio; DEPTH, sediment/rock; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-2; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; L-Isoleucine; M51; Meteor (1964); Sierra Leone Rise; SL
    Type: Dataset
    Format: text/tab-separated-values, 156 data points
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  • 12
    Publication Date: 2024-02-03
    Keywords: AGE; D-Alloisoleucine; D-Alloisoleucine/L-Isoleucine ratio; DEPTH, sediment/rock; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-2; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; L-Isoleucine; M51; Meteor (1964); Sierra Leone Rise; SL
    Type: Dataset
    Format: text/tab-separated-values, 279 data points
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  • 13
    Publication Date: 2024-02-03
    Keywords: AGE; D-Alloisoleucine; D-Alloisoleucine/L-Isoleucine ratio; DEPTH, sediment/rock; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-2; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; L-Isoleucine; M51; Meteor (1964); Sierra Leone Rise; SL
    Type: Dataset
    Format: text/tab-separated-values, 145 data points
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  • 14
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_2N2; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_235-2; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 15
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_EQ3; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_246-2; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 16
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_006-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 17
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_1S; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_004-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 18
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    PANGAEA
    In:  Supplement to: Sarnthein, Michael; Erlenkeuser, Helmut; von Grafenstein, Rita; Schröder, C (1984): Stable isotope stratigraphy for the last 750.000 years. Meteor core 13519 from the eastern equatorial Atlantic. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C38, 9-24
    Publication Date: 2024-02-03
    Description: From a 10.7 m long gravity core from the Sierra Leone Rise (5°39.5' N, 19°51' W) a detailed oxygen and carbon isotope record of both planktonic and benthonic foraminifera species was obtained extending from the Recent to Jaramillo event. The analysis yielded six major results. 1. Benthos oxygen isotopes varied by 1.8-2.2 per mil from interglacial to glacial times and may indicate a synglacial cooling of North Atlantic Deep Water at 2800 m depth by 1-3°C. 2. Variable anomalies between the benthos and plankton d18O record indicate a cooling of sea-surface temperatures (SST) by up to 6 °C during some glacial stages. 3. Southerly trade winds and equatorial upwelling may excert the primary control off SST variations, in particular of extremee values of cold and warm stages and of the abrupt character of climate transitions and their leads and lags, and finally, of variable sedimentation rates. 4. The benthos d13C record correlates well with the flux and preservation of organic matter. 5. A new time scale, CARPOR, was established from the assumption that terrigenous sediment supply was ± constant bit CaCO3 varied considerably. When applied to the d18O record, three major and numerous short-term variations of sedimentation rates (0.8 to 4.0 cm/kyr) can be distinguished. 6. The climatic record was modified by bioturbation much more strongly during cold than during warm stages.
    Keywords: Atlantic Ocean; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-1; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; M51; Meteor (1964); SL
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 19
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    PANGAEA
    In:  Supplement to: Müller, Peter J (1984): Isoleucine epimerization in Quaternary planktonic foraminifera: Effects of diagenetic hydrolysis and leaching, and Atlantic-Pacific intercore correlations. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C38, 25-48
    Publication Date: 2024-02-03
    Description: Panktonic foraminiferal tests of the spinose species Orbulina universa, of the non-spinose Globorotalia tumida-menardii complex, and of a mixed species assemblage (grain size fraction 200-400 µm) were isolated from Sierra Leone Rise core GIK13519-2 and analyzed for free, total, and bound (by difference) amino acids to study the isoleucine epimerization mechanism in fossil foraminiferal tests and to define empirical calibration curves for dating deep-sea sediments over the past 900,000 years. Total isoleucine epimerization curves typically separate into three "linear" segments of decreasing apparents rates with increasing time and exhibit a pronounced „species effect“. The degree of epimerization attained at time is considerably lower in O. universa than in G. tumida-menardii while the mixed species results scatter between the limits delineated by the two monospecific curves. Total allo/iso ratios are closely related to the proportion of free to total isoleucine accumulating in the tests indicating that the rate of hydrolysis of matrix proteins and peptides controls the overall epimerization reaction. The results are consistent with experimental evidenve where upon isoleucine epimerizes at a rapid rate in terminal positions but at slow rates in interior positions as well as in the free state. Notwithstanding free isoleucine exhibits the highest degree of epimerized terminal isoleucine. Species-specific hydrolysis and epimerization rates are maintained until about 50 % of bound isoleucine have been hydrolyzed to the free state corresponding to a total allo/iso ratio of about 0.5. Remaining peptide units appear to be more resistent against hydrolysis and separate species then show the same apparent epimerization rate dominantly controlled by the slow conversion rate in the free state until equilibrium is achieved in Miocene samples under deep-ocean temperature conditions. The degree of epimerization attained at comparable time in separate species will, however, remain different due to different initial rates of hydrolysis.
    Keywords: FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-2; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; M51; Meteor (1964); Sierra Leone Rise; SL
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    Format: application/zip, 3 datasets
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  • 20
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_2N1; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_008-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 21
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_1N; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_007-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 22
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_EQ2; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_056-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 23
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; Current velocity, east-west; Current velocity, east-west, standard deviation; Current velocity, north-south; Current velocity, north-south, standard deviation; DEPTH, water; FGGE_3N; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_009-1; Meteor (1964); MOOR; Mooring; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 24
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    PANGAEA
    In:  Supplement to: Bauerfeind, Eduard; Brockmann, Christian; Fahrbach, Eberhard; Meincke, Jens; Panitz, Hans Jürgen; Rohardt, Gerd; Sy, Alexander (1984): A compendium of the oceanographic data obtained during FGGE-Equator '79, Cruise No. 51 of R.V. Meteor. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A/B Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A/B25, 1-108
    Publication Date: 2024-02-03
    Description: From 27 January to 23 June 1979 R.V. „Meteor“ surveyed the central equatorial Atlantic on a section along 22° W from 3° N to 2° S. During the observation period, a hydrographic section down to 600 m was repeated ten times with a continous „Howaldt-Bathysonde“ CTD and a rosette sampler. The station distance was 10 to 15 nm. The water samples were used to recalibrate salinity and to determine oxygen, nutrients and chlorophyll a. An undulating CTD system („Delphin“) was towed on 11 sections. A profiling distance of one to two nautical miles and a profile depth of 90 m was obtained. Five current meter arrys were moored along 22° W between 3° N and 1°S from January to March 1979. In May and June two moorings were installed at 2° N and at the equator. On the buoys measurements of wind speed and direction were obtained. At 43 stations a wire-guided Aanderaa profiling current meter was successfully lowered. Drifting buoy experiments were repeated three times with clusters of 5 to 10 buoys. A fourth experiment took place in 1978 in the Gulf of Guinea. On the way from and to XBT sections were carried out. The data sets obtained by these instruments are presented in this data report.
    Keywords: Atlantic Ocean; CTD/Rosette; CTD-RO; FGGE_1N; FGGE_1S; FGGE_2N1; FGGE_2N2; FGGE_3N; FGGE_ATK2N1; FGGE_ATK3N; FGGE_EQ1; FGGE_EQ2; FGGE_EQ3; FGGE_MET1N1; FGGE_MET1S; FGGE_MET2N1; FGGE_MET2N2; FGGE_MET3N; FGGE_METEQ1; FGGE_METEQ2; FGGE_METEQ3; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; HOBS; Howaldt-Bathysonde; Institute for Geosciences, Christian Albrechts University, Kiel; M51; M51_004-1; M51_006-1; M51_007-1; M51_008-1; M51_009-1; M51_010-1; M51_011-1; M51_012-1; M51_013-1; M51_014-1; M51_015-1; M51_016-1; M51_017-1; M51_018-1; M51_019-1; M51_020-1; M51_021-1; M51_022-1; M51_023-1; M51_024-1; M51_025-1; M51_026-1; M51_027-1; M51_028-1; M51_029-1; M51_030-1; M51_031-1; M51_032-1; M51_033-1; M51_034-1; M51_035-1; M51_042-1; M51_043-2; M51_044-1; M51_045-1; M51_046-1; M51_047-1; M51_048-1; M51_049-2; M51_050-1; M51_051-1; M51_052-1; M51_053-1; M51_054-1; M51_055-1; M51_056-1; M51_057-1; M51_058-1; M51_059-1; M51_060-1; M51_061-1; M51_062-1; M51_063-1; M51_064-1; M51_065-1; M51_066-1; M51_071-1; M51_072-2; M51_073-2; M51_075-1; M51_076-1; M51_077-1; M51_078-1; M51_079-1; M51_080-1; M51_081-1; M51_082-1; M51_083-1; M51_084-1; M51_085-1; M51_086-1; M51_087-1; M51_088-1; M51_090-2; M51_091-1; M51_092-1; M51_093-1; M51_094-1; M51_095-1; M51_096-1; M51_097-1; M51_098-2; M51_099-1; M51_100-1; M51_101-1; M51_102-1; M51_102-2; M51_103-1; M51_104-1; M51_105-1; M51_106-1; M51_107-1; M51_108-2; M51_109-1; M51_110-1; M51_111-1; M51_112-1; M51_113-2; M51_115-1; M51_116-2; M51_117-2; M51_122-1; M51_124-1; M51_125-1; M51_126-2; M51_127-1; M51_128-1; M51_129-1; M51_130-1; M51_131-1; M51_132-1; M51_134-2; M51_135-1; M51_136-1; M51_137-1; M51_138-1; M51_139-1; M51_140-1; M51_141-1; M51_142-1; M51_143-2; M51_144-1; M51_145-1; M51_146-1; M51_147-1; M51_148-1; M51_149-1; M51_150-2; M51_151-2; M51_152-2; M51_153-2; M51_154-2; M51_160-1; M51_161-1; M51_162-1; M51_163-1; M51_164-1; M51_165-1; M51_166-1; M51_167-1; M51_168-1; M51_169-1; M51_170-1; M51_171-1; M51_172-1; M51_173-1; M51_174-1; M51_175-1; M51_176-1; M51_177-1; M51_178-1; M51_179-1; M51_180-1; M51_181-2; M51_182-1; M51_183-1; M51_184-1; M51_185-1; M51_186-1; M51_190-1; M51_192-1; M51_197-1; M51_197-10; M51_197-11; M51_197-12; M51_197-2; M51_197-3; M51_197-4; M51_197-5; M51_197-6; M51_197-7; M51_197-8; M51_197-9; M51_199-1; M51_199-10; M51_199-11; M51_199-12; M51_199-13; M51_199-14; M51_199-15; M51_199-2; M51_199-3; M51_199-4; M51_199-5; M51_199-6; M51_199-7; M51_199-8; M51_199-9; M51_200-1; M51_201-1; M51_202-1; M51_203-1; M51_204-1; M51_205-1; M51_206-1; M51_207-1; M51_208-1; M51_209-1; M51_210-1; M51_211-1; M51_212-2; M51_213-2; M51_214-2; M51_215-2; M51_216-1; M51_217-2; M51_218-1; M51_219-1; M51_220-1; M51_221-2; M51_222-1; M51_223-1; M51_224-2; M51_225-1; M51_226-1; M51_227-1; M51_227-10; M51_227-2; M51_227-3; M51_227-4; M51_227-5; M51_227-6; M51_227-7; M51_227-8; M51_227-9; M51_229-1; M51_229-2; M51_231-2; M51_232-1; M51_233-1; M51_234-1; M51_235-1; M51_235-2; M51_236-2; M51_237-1; M51_238-2; M51_240-1; M51_241-1; M51_242-2; M51_243-1; M51_244-1; M51_245-1; M51_246-1; M51_246-2; M51_247-2; M51_248-1; M51_249-1; M51_250-1; M51_251-1; M51_252-1; M51_253-1; M51_254-1; M51_255-2; M51_256-1; M51_257-1; M51_258-2; M51_260-1; M51_261-2; M51_262-1; M51_263-1; M51_264-1; M51_265-1; M51_266-1; M51_267-2; M51_268-1; M51_269-1; M51_270-1; M51_271-1; M51_272-1; M51_273-2; M51_274-1; M51_275-1; M51_276-1; M51_277-1; M51_278-1; M51_279-1; M51_280-1; M51_286-2; M51_286-4; M51_291-1; M51_292-2; M51_293-1; M51_294-2; M51_295-1; M51_296-1; M51_297-1; M51_298-1; M51_299-1; M51_300-1; M51_301-2; M51_302-1; M51_305-1; M51_306-1; M51_307-1; M51_308-1; M51_309-2; M51_310-1; M51_311-1; M51_312-1; M51_313-1; M51_314-1; M51_315-1; M51_316-1; M51_317-1; M51_318-4; M51_320-2; M51_321-1; M51_322-1; M51_323-2; M51_324-1; M51_325-1; M51_326-1; M51_329-4; M51_330-1; M51_331-1; M51_333-2; M51_334-1; M51_335-1; M51_336-1; M51_337-1; M51_338-1; M51_339-1; M51_341-1; M51_342-1; M51_343-1; M51_344-2; M51_345-1; M51_346-1; M51_B0105N; M51_B0105S; M51_B0110N; M51_B0110S; M51_B0115N; M51_B0115S; M51_B0120N; M51_B0120S; M51_B0125N; M51_B0130N; M51_B0205N; M51_B0205S; M51_B0210N; M51_B0210S; M51_B0215N; M51_B0215S; M51_B0220N; M51_B0220S; M51_B0230N; M51_B0305N; M51_B0305S; M51_B0310N; M51_B0310S; M51_B0315N; M51_B0315S; M51_B0320N; M51_B0320S; M51_B0325N; M51_B0330N; M51_B0405N; M51_B0405S; M51_B0410N; M51_B0410S; M51_B0415N; M51_B0415S; M51_B0420N; M51_B0420S; M51_B0425N; M51_B0430N; M51_B04EQ; M51_B0505N; M51_B0505S; M51_B0510N; M51_B0510S; M51_B0515N; M51_B0515S; M51_B0520N; M51_B0520S; M51_B0525N; M51_B0530N; M51_B05EQ; M51_B0605N; M51_B0605S; M51_B0610N; M51_B0610S; M51_B0615N; M51_B0620N; M51_B0625N; M51_B0630N; M51_B06EQ; M51_B0705N; M51_B0705S; M51_B0710N; M51_B0710S; M51_B0715N; M51_B0715S; M51_B0720N; M51_B0720S; M51_B0725N; M51_B0730N; M51_B07EQ; M51_B0805N; M51_B0805S; M51_B0810N; M51_B0810S; M51_B0815N; M51_B0815S; M51_B0820N; M51_B0820S; M51_B0825N; M51_B0830N; M51_B08EQ; M51_B0905N; M51_B0905S; M51_B0910N; M51_B0910S; M51_B0915N; M51_B0915S; M51_B0920N; M51_B0920S; M51_B0925N; M51_B0930N; M51_B1005N; M51_B1005S; M51_B1010N; M51_B1010S; M51_B1015N; M51_B1015S; M51_B1020N; M51_B1025N; M51_B1030N; M51_B10EQ; M51_BFS062; M51_BFS09E; Meteor (1964); MOOR; Mooring; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 27 datasets
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  • 25
    Publication Date: 2024-02-03
    Keywords: Atlantic Ocean; DEPTH, sediment/rock; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK13519-1; GLAMAP; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; Isotope ratio mass spectrometry; M51; Meteor (1964); SL
    Type: Dataset
    Format: text/tab-separated-values, 364 data points
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  • 26
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    PANGAEA
    In:  Supplement to: Betzer, Peter R; Showers, William J; Laws, Edward A; Winn, Christopher D; DiTullio, Giacomo R; Kroopnick, Peter M (1984): Primary productivity and particle fluxes on a transect of the equator at 153°W in the Pacific Ocean. Deep-Sea Research Part A. Oceanographic Research Papers, 31(1), 1-11, https://doi.org/10.1016/0198-0149(84)90068-2
    Publication Date: 2024-02-01
    Description: Primary productivity (14C) and mass flux measurements using a free-drifting sediment trap deployed at 900 m were made at four stations in the Pacific Ocean between 12°N and 6°S at 153°W. The latitudinal variations in productivity were consistent with historical patterns showing the equator as a zone of high production and the oligotrophic waters north of the equatorial region as an area of low productivity. The correlation coefficient between the two sets of independent measurements was 0.999, indicating that in this oceanic area the activity of the primary producers was closely related to the total mass flux. A re-examination of historical data suggests that the downward flux of particulate organic carbon varies in direct proportion to the quotient of surface primary production raised to the 1.4 power and depth raised to the 0.63 power.
    Keywords: Betzer; DEPTH, water; Hawaii Ocean Time-Series; HOT; JGOFS; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; Primary production of carbon per area, yearly; Total, flux per year
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 27
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    PANGAEA
    In:  Supplement to: Sachtleben, T; Schmincke, Hans-Ulrich (1984): Metagranitic rocks from the Mazagan escarpment, Deep Sea Drilling Project Leg 79, Hole 544A. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 551-554, https://doi.org/10.2973/dsdp.proc.79.119.1984
    Publication Date: 2024-01-19
    Description: Fifty m of basement rocks underlying 185 m of Neogene and Mesozoic sediments were drilled seaward of the Mazagan Slope about 100 km west of Casablanca during Leg 79. These rocks are metagranites with mylonitic textures consisting dominantly of quartz, plagioclase, and potassium feldspar. Chemically, they are strongly peraluminous. This along with the absence of hornblende suggest that these rocks are similar to the S-type granites. Petrographic and chemical data suggest the possible existence of a former weathering surface on top of the Mazagan metagranite.
    Keywords: 79-544A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg79; North Atlantic/PLATEAU
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 28
    Publication Date: 2024-01-19
    Keywords: AGE; SPECMAP; Spectral Mapping Project (Mapping Species Variability in Global Climate); δ18O
    Type: Dataset
    Format: text/tab-separated-values, 392 data points
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  • 29
    Publication Date: 2024-01-19
    Description: Seaward of the Mazagan Escarpment and slope is a band about 50 km wide where structures interpreted as diapirs stand like columns within a pile of sediments about 5 km thick . Dredges and cores from Vema cruise 30-13 and Valdivia cruise West Africa 1979 on the slopes of the most landward of these structural highs, just 10 km from the foot of the escarpment recovered fragments of sheared granite. It was hypothesized that, if this structure were a salt diapir, it might have carried upward very old sediments, dating to the earliest stages of Atlantic evolution, in the Early Jurassic or late Triassic. DSDP Leg 79, sites 544 through 547 were closely located on the structure area.
    Keywords: 79-544A; 79-546; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg79; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/PLATEAU; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 30
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Fenton, J P G (1984): Palynological investigation of the Triassic-middle Jurassic sequences at Deep Sea Drilling Project Leg 79, Sites 545, 546, and Hole 547B, off central Morocco. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 715-718, https://doi.org/10.2973/dsdp.proc.79.129.1984
    Publication Date: 2024-01-19
    Description: Twenty-five samples from selected cored intervals of problematic Triassic-Jurassic age from Sites 545, 546, and Hole 547B have been analyzed palynologically to aid age determination. Section 545-73-1 yielded a marine palynoflora of Sinemurian-Bajocian age. A palynoflora of nonmarine origin and assigned a Rhaetian-Hettangian age was recovered from halite in Section 546-18-2. Marine palynofloras of Hettangian-early Pliensbachian age were recovered from Sample 547B-24-CC to Section 547B-14-2. Sections 547B-28-1 to 547B-25-3 yielded impoverished nonmarine palynofloras to which only a general Rhaetian-Hettangian age could be given.
    Keywords: 79-547B; Acritarcha, acanthomorph; Araucariacites australis; Botryococcus spp.; Carnisporites anreriscus; Cerebropollenites mesozoicus; Chasmatosporites spp.; Classopollis spp.; Corollina meyeriana; Crassosphaera hexagonalis; Cycadopites spp.; Deep Sea Drilling Project; Deltoidospora spp.; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Echinitosporites cf. iliacoides; Echinitosporites sp.; Foraminifera; Glomar Challenger; Kraeuselisporites reissingeri; Leg79; Leiospheres; North Atlantic/PLATEAU; Palynomorpha; Parvisaccites enigmatus; Perinopollenites elatoides; Pollen, bisaccate; Porcellispora longdonensis; Sample code/label; Tasmanites newtoni; Tasmanites suevicus
    Type: Dataset
    Format: text/tab-separated-values, 552 data points
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  • 31
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    PANGAEA
    In:  Supplement to: Schaftenaar, C H; Carlson, Richard L (1984): Acoustic properties of calcareous claystones and clay-rich chalks, Deep Sea Drilling Project, Leg 79. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 853-854, https://doi.org/10.2973/dsdp.proc.79.136.1984
    Publication Date: 2024-01-19
    Description: Laboratory measurements of the acoustic and physical properties of deep-sea sediments and rocks are important for the interpretation of seismic reflection and refraction data and estimation of in situ physical property values. Furthermore, the results of such measurements can be used to design geoacoustic models of the upper oceanic crust that can relate the physical properties of deep-sea sediments to lithology, depth of burial, and diagenetic effects (Hamilton, 1980; Milholland et al., 1980). The purpose of this paper is to report the results of laboratory measurements of wet-bulk density, compressionalwave velocity, and velocity anisotropy on sediments cored during DSDP Leg 79. The sample suite consists of 11 calcareous claystones and clay-rich chalks recovered between 370 to 720 m sub-bottom at Holes 545 and 547A.
    Keywords: 79-545; 79-547A; Calculated, see reference(s); Carbonates; Deep Sea Drilling Project; Density, wet bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Leg79; North Atlantic/PLATEAU; Porosity, fractional; Pulse transmission technique (Birch, 1960); Sample code/label; see reference(s); Velocity, compressional wave; Velocity, compressional wave anisotropy; Water in rock
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 32
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    PANGAEA
    In:  Supplement to: Schaefer, Rainer G; Leythaeuser, Detlev; Gormly, James (1984): Generation and migration of low-molecular-weight hydrocarbons in sediments of Deep Sea Drilling Project Leg 79, Sites 544, 545, and 547, offshore Morocco. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 743-773, https://doi.org/10.2973/dsdp.proc.79.131.1984
    Publication Date: 2024-01-19
    Description: A series of core samples taken during Cruise 79 of Glomar Challenger, drilling offshore Morocco (Mazagan Plateau), is analyzed for their low-molecular-weight hydrocarbon contents. Fifty-four samples from DSDP Holes 544A, 545, 547A, and 547B, deep frozen on board immediately after recovery, are studied by a hydrogen-stripping/thermovaporization technique combined with capillary gas chromatography. Thirty-eight compounds in the C2-C8 molecular range, including saturated, olefinic, and aromatic hydrocarbons, are identified. Because of large differences in organic carbon contents, the total C2-C8 hydrocarbon concentrations vary from about 20 to 1500 ng/g dry sediment weight in the whole sample series. Organic-carbon normalized values are about 3.2 x 10**4 ng/g Corg for Lithologic Subunits IIIA and IIIB at Site 545 (Cenomanian to Aptian) and 1.0 x 10**5 ng/g Corg for Unit V at Site 547 (Cenomanian to Albian) reflecting the slightly more advanced maturity stage at the latter site. Values exceeding 10**5 ng/g Corg (Site 545) and 2 x 10**5 ng/g Corg (Site 547) are associated with samples that are very lean in organic carbon and are generally rich in carbonate. These samples are enriched by small amounts of gaseous hydrocarbons. A detailed study of individual hydrocarbon concentrations, plotted against depth, reveal additional indications for migration phenomena. At Site 547, for instance, the most mobile hydrocarbons studied (e.g., ethane) appear to migrate by diffusion or a related process from more than 700 m depth toward the surface.
    Keywords: 1,cis-2-Dimethylcyclopentane per unit sediment mass; 1,cis-3-Dimethylcyclopentane per unit sediment mass; 1,trans-2,cis-3-trimethylcyclopentane per unit sediment mass; 1,trans-2,cis-4-trimethylcyclopentane per unit sediment mass; 1 trans-2-Dimethylcyclopentane per unit sediment mass; 1 trans-3-Dimethylcyclopentane per unit sediment mass; 2,2-Dimethylbutane per unit sediment mass; 2,2-Dimethylpropane per unit sediment mass; 2,3-Dimethylbutane per unit sediment mass; 2,3-Dimethylpentane per unit sediment mass; 2,4-Dimethylpentane per unit sediment mass; 2,5-Dimethylhexane per unit sediment mass; 2-Methylheptane per unit sediment mass; 2-Methylhexane per unit sediment mass; 2-Methylpentane per unit sediment mass; 3-Methylhexane per unit sediment mass; 3-Methylpentane per unit sediment mass; 79-544A; 79-545; 79-547A; 79-547B; Benzene per unit sediment mass; Carbon, organic, total; Cis-2-butene per unit sediment mass; Cyclohexane per unit sediment mass; Cyclopentane per unit sediment mass; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Ethane per unit sediment mass; Ethene per unit sediment mass; Ethylcyclopentane per unit sediment mass; Event label; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Isobutane per unit sediment mass; Isopentane per unit sediment mass; Latitude of event; Leg79; Lithology/composition/facies; Longitude of event; Methylcyclohexane per unit sediment mass; Methylcyclopentane per unit sediment mass; n-Butane per unit sediment mass; n-Heptane per unit sediment mass; n-Hexane per unit sediment mass; n-Octane per unit sediment mass; North Atlantic/PLATEAU; n-Pentane per unit sediment mass; Oxygen index, mass CO2, per unit mass total organic carbon; Propane per unit sediment mass; Propene per unit sediment mass; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label; see reference(s); Toluene per unit sediment mass; Trans-2-butene per unit sediment mass
    Type: Dataset
    Format: text/tab-separated-values, 2376 data points
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  • 33
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bate, Raymond H; Lord, Alan; Riegraf, Wolfgang (1984): Jurassic ostracoda from Leg 79, Site 547. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 703-710, https://doi.org/10.2973/dsdp.proc.79.127.1984
    Publication Date: 2024-01-19
    Description: Eighteen samples from the Early Jurassic (Hettangian to Pliensbachian) and nine from the Bajocian to Berriasian interval have been examined. The ostracode fauna has been left largely in open nomenclature pending a more detailed study. At least four new genera, listed simply as Gen. nov. A-D sp. nov. have been recognized. Although many new species are present, there is a similarity between this ostracode fauna and that of northwest Europe of comparable age. This is particularly true for the Early Jurassic from which Bairdia guttulae Herrig, 1979, Ptychobairdia cf. aselfingenensis (Lord and Moorley, 1974), Monoceratina scrobiculata Triebel and Bartenstein, 1938, Bairdia sp. 4134 Michelsen, 1975, Ogmoconcha cf. contractula Triebel, 1941, and Paracypris cf. redcarensis Blake, 1876 have been obtained. Monoceratina vulsa (Jones and Sherborn, 1888), present in the Toarcian to Callovian of Britain, is recorded here from a sample provisionally dated as Bajocian to Callovian on foraminiferal evidence. The more important species are illustrated and their distribution recorded in Table 1.
    Keywords: 79-547; Acanthocythere sp.; Bairdia cf. carinata; Bairdia guttulae; Bairdia molesta; Bairdia sp.; Bythocypris sp.; Cytherella sp.; Cytherelloidea sp.; Cytheropteron sp.; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ektyphocythere sp.; Epoch; Eucytherura sp.; Glomar Challenger; Isobythocypris cf. tatei; Isobythocypris sp.; Kinkelinella sp.; Leg79; Lutkevichinella sp.; Metacopine sp.; Monoceratina scrobiculata; Monoceratina vulsa; Monoceratins sp.; North Atlantic/PLATEAU; Ogmoconcha cf. contractula; Ogmoconcha sp.; Ogmoconchella sp.; Orthonotacythere sp.; Ostracoda; Ostracoda indeterminata; Palaeocytheridea sp.; Paracypris cf. redcarensis; Paracypris sp.; Paracytheridea sp.; Polycope cf. pelta; Polycope sp.; Procytherura sp.; Ptychobairdia cf. aselfingensis; Ptychobairdia hahni; Rutlandella sp.; Sample code/label; Stage; Tethysia sp.; Timiriasevia sp.
    Type: Dataset
    Format: text/tab-separated-values, 963 data points
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  • 34
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Kälin, Otto; Bernoulli, Daniel (1984): Schizosphaerella Deflandre and Dangeard in Jurassic deeper-water carbonate sediments, Mazagan Continental Margin (Hole 547B) and Mesozoic Tethys. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 411-435, https://doi.org/10.2973/dsdp.proc.79.112.1984
    Publication Date: 2024-01-19
    Description: The Jurassic (hemi)pelagic continental margin deposits drilled at Hole 547B, off the Moroccan coast, reveal striking Tethyan affinity. Analogies concern not only types and gross vertical evolution of facies, but also composition and textures of the fine sediment and the pattern of diagenetic alteration. In this context, the occurrence of the nanno-organism Schizosphaerella Deflandre and Dangeard (sometimes as a conspicuous portion of the fine-grained carbonate fraction) is of particular interest. Schizosphaerella, an incertae sedis taxon, has been widely recorded as a sediment contributor from Tethyan Jurassic deeper-water carbonate facies exposed on land. Because of its extremely long range (Hettangian to early Kimmeridgian), the genus Schizosphaerella (two species currently described, S. punctulata Deflandre and Dangeard and S. astrea Moshkovitz) is obviously not of great biostratigraphic interest. However, it is of interest in sedimentology and petrology. Specifically, Schizosphaerella was often the only component of the initial fine-grained fraction of a sediment that was able to resist diagenetic obliteration. However, alteration of the original skeletal structure did occur to various degrees. Crystal habit and mineralogy of the fundamental skeletal elements, as well as their mode of mutual arrangement in the test wall with the implied high initial porosity of the skeleton (60-70%), appear to be responsible for this outstanding resistance. Moreover, the ability to concentrate within and, in the case of the species S. punctulata, around the skeleton, large amounts of diagenetic calcite also contributed to the resistance. In both species of Schizosphaerella, occlusion of the original skeletal void space during diagenesis appears to have proceeded in an analogous manner, with an initial slight uniform syntaxial enlargement of the basic lamellar skeletal crystallites followed, upon mutual impingement, by uneven accretion of overgrowth cement in the remaining skeletal voids. However, distinctive fabrics are evident according to the different primary test wall architecture. In S. punctulata, intraskeletal cementation is usually followed by the growth of a radially structured crust of bladed to fibrous calcite around the valves. These crusts are interpreted as a product of aggrading neomorphism, associated with mineralogic stabilization of the original, presumably polyphase, sediment. Data from Hole 547B, along with inferences, drawn from the fabric relationships, suggest that the crusts formed and (inferentially) mineralogic stabilization occurred at a relatively early time in the diagenetic history in the shallow burial realm. An enhanced rate of lithification at relatively shallow burial depths and thus the chance for neomorphism to significantly influence the textural evolution of the buried sediment may be related to a lower Mg/Ca concentration ratio in the oceanic system and, hence, in marine pore waters in pre-Late Jurassic times.
    Keywords: 79-547B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg79; Light microscope; Method comment; North Atlantic/PLATEAU; Sample code/label; Scanning electron microscope (SEM); Schizosphaerella astraea; Schizosphaerella punctulata; Schizosphaerella spp.
    Type: Dataset
    Format: text/tab-separated-values, 278 data points
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  • 35
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    Unknown
    PANGAEA
    In:  Supplement to: Mukhopadhyay, Prasanta K; Spiro, Baruch; Rullkötter, Jürgen (1984): An inertinite-rich coal lenticle in Triassic sediment of sample 547B-35, CC, Deep Sea Drilling Project Leg 79. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 493-495, https://doi.org/10.2973/dsdp.proc.79.115.1984
    Publication Date: 2024-01-19
    Description: A lenticle of organic matter in a piece of dolomite rock embedded in Triassic sandy mudstone of Core 547B-35 (DSDP Leg 79) was identified as inertinite-rich coal by organic petrography and analytical pyrolysis. About 95% of the organic matter recognized under the microscope consists of pyrofusinite, degradofusinite, and inertodetrinite. Gaseous hydrocarbons evolved during pyrolysis are rich in methane and are characteristic of inertinitic material. The organic matter is suggested to be a piece of redeposited Permian Gondwana coal.
    Keywords: 79-547B; Carbon, organic, total; Deep Sea Drilling Project; Degradofusinite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Humic compounds; Hydrogen index, mass HC, per unit mass total organic carbon; Inertodetrinite; Leg79; Liptinite; Lithology/composition/facies; Microscopy; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrofusinite; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label; Vitrinite reflection
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 36
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Chamley, Hervè; Debrabant, Pierre (1984): Mineralogical and geochemical investigations of sediments on the Mazagan Plateau, northwestern African Margin (Leg 79, Deep Sea Drilling Project). In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 497-508, https://doi.org/10.2973/dsdp.proc.79.116.1984
    Publication Date: 2024-01-19
    Description: Detailed mineralogical and geochemical studies were performed on samples from selected time intervals recovered during Leg 79 on the Mazagan Plateau. The uppermost Albian and Cenomanian sediments of Sites 545 and 547 can be correlated on the basis of mineralogy and geochemistry; these sediments illustrate differential settling processes and the existence of hot climates with alternating humid and dry seasons in the African coastal zone. The upper Aptian to Albian black shales of Site 545 point to an irregular alternation of tectonic activity and relaxation stages, allowing different behaviors in the reworking of soils, crystalline rocks, and sediments born in peri-marine basins. The barren lower Mesozoic reddish sediments and evaporitic series of Sites 546 and 547 are characterized by a strong physical erosion of sialic landscapes, without clear evidence of post-depositional metamorphic events. At Site 546 strong early diagenetic processes in a confined evaporitic environment affect both the mineralogy and the geochemistry of pre-Miocene rocks.
    Keywords: 79-545; 79-546; 79-547A; 79-547B; Aluminium oxide; Atomic absorption spectrometry (AAS); Calcium oxide; Chromium; Cobalt; Colorimetry; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Iron oxide, Fe2O3; Latitude of event; Lead; Leg79; Lithium; Longitude of event; Magnesium oxide; Manganese; Nickel; North Atlantic/PLATEAU; Phosphorus pentoxide; Potassium oxide; Sample code/label; see reference(s); Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 1250 data points
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  • 37
    Publication Date: 2024-01-19
    Keywords: 79-547B; Buliminacea; Cassidulinacea; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Foraminifera, benthic; Glomar Challenger; Leg79; Miliolacea; Nodosariacea; North Atlantic/PLATEAU; Preservation; Robertinacea; Sample code/label; Spirillinacea; Textulariina
    Type: Dataset
    Format: text/tab-separated-values, 422 data points
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  • 38
    Publication Date: 2024-01-19
    Keywords: 79-546; Bromine; Carnallite; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg79; Magnesium; North Atlantic/PLATEAU; Potassium; Ratio; Sample code/label; see reference(s); Soluble residue; Sylvite
    Type: Dataset
    Format: text/tab-separated-values, 628 data points
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  • 39
    Publication Date: 2024-01-19
    Keywords: 79-546; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg79; Lithology/composition/facies; North Atlantic/PLATEAU; Sample code/label; see reference(s); δ18O; δ18O, standard deviation; δ34S
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 40
    Publication Date: 2024-01-19
    Keywords: 79-544A; Aluminium oxide; Barium; Calcium oxide; Carbon dioxide; Chlorine; Chromium; Cobalt; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron oxide, Fe2O3; Iron oxide, FeO; Leg79; Magnesium oxide; Manganese oxide; Nickel; Niobium; North Atlantic/PLATEAU; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Silicon dioxide; Sodium oxide; Strontium; Sulfur, total; Titanium dioxide; Total; Water in rock; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 140 data points
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  • 41
    Publication Date: 2024-01-19
    Keywords: 79-544A; Albite; Anorthite; Apatite; Calcite; CIPW Norm; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Enstatite; Ferrosilite; Glomar Challenger; Halite; Ilmenite; Leg79; Magnetite; North Atlantic/PLATEAU; Orthoclase; Pyrophyllite; Quartz; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 42
    Publication Date: 2024-01-19
    Keywords: 79-545; Calpionella alpina; Calpionellids; Crassicollaria brevis; Crassiocollaria intermedia; Crassiocollaria parvula; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg79; North Atlantic/PLATEAU; Sample code/label; Tintinnopsis carpathica
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 43
    Publication Date: 2024-01-19
    Keywords: 79-547B; Calpionella alpina; Calpionellids; Crassicollaria sp.; Crassiocollaria intermedia; Crassiocollaria parvula; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg79; North Atlantic/PLATEAU; Remaniella ferasini; Sample code/label; Tintinnopsis carpathica
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 44
    Publication Date: 2024-01-19
    Keywords: 79-544A; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; Discorhabdus sp.; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ellipsagelosphaera britannica; Ellipsagelosphaera sp.; Glomar Challenger; Leg79; Nannofossil abundance; Nannofossils preservation; North Atlantic/PLATEAU; Period; Sample code/label; Smear slide analysis
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 45
    Publication Date: 2024-01-19
    Keywords: 79-545; Axopodorhabdus cylindratus; Bidiscus ignotus; Carinolithus sp.; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; Discorhabdus sp.; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ellipsagelosphaera crucicentralis; Ellipsagelosphaera sp.; Glomar Challenger; Leg79; Nannofossil abundance; Nannofossils preservation; North Atlantic/PLATEAU; Paleopontosphaera sp.; Sample code/label; Smear slide analysis; Stage; Staurorhabdus quadriacullus; Tubirhabdus patulus; Tubirhabdus sp.; Zeugrhabdotus erectus
    Type: Dataset
    Format: text/tab-separated-values, 331 data points
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  • 46
    Publication Date: 2024-01-19
    Keywords: 79-545; 79-547A; 79-547B; Calcium carbonate; Carbon, organic, fraction; Carbon, organic, total; Carbon/Nitrogen ratio; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN; Elevation of event; Epoch; Event label; Glomar Challenger; Latitude of event; Leg79; Lithologic unit/sequence; Lithology/composition/facies; Longitude of event; Nitrogen, organic; Nitrogen, organic, fraction; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 193 data points
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  • 47
    Publication Date: 2024-01-19
    Keywords: 79-547B; Ageprofile Datum Description; Bidiscus ignotus; Calcivascularis jansae; Comment; Crepidolithus crassus; Crepidolithus crucifer; Crepidolithus sp.; Crucirhabdus primulus; Cyclagelosphaera deflandrei; Cyclagelosphaera margerelii; Deep Sea Drilling Project; DEPTH, sediment/rock; Discorhabdus sp.; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ellipsagelosphaera britannica; Ellipsagelosphaera crucicentralis; Ellipsagelosphaera keftalrempti; Ellipsagelosphaera sp.; Glomar Challenger; Hexalithus sp.; Leg79; Nannofossil abundance; Nannofossils preservation; Nannofossil zone; North Atlantic/PLATEAU; Orthogonoides hamiltoniae; Paleopontosphaera dubia; Paleopontosphaera sp.; Parhabdolithus liasicus; Parhabdolithus marthae; Sample code/label; Schizosphaerella punctulata; Smear slide analysis; Stage; Staurorhabdus quadriacullus; Stephanolithion bigotii; Tubirhabdus patulus; Tubirhabdus sp.; Watznaueria barnesae; Zeugrhabdotus erectus
    Type: Dataset
    Format: text/tab-separated-values, 2629 data points
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  • 48
    Publication Date: 2024-01-19
    Keywords: -; 79-545; 79-547A; 79-547B; Bituminosity coefficient; Carbon, organic, total; Carbon Preference Index, n-Alkanes; Color description; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN; Elevation of event; Event label; Gas chromatography/mass spectrometry (GF/C filtered); Glomar Challenger; Hydrocarbon yield; Latitude of event; Leg79; Longitude of event; n-Alkane, carbon maximum number; North Atlantic/PLATEAU; Pristane/Phytane ratio; Ratio; Sample code/label; Sample mass; see reference(s); Yield
    Type: Dataset
    Format: text/tab-separated-values, 221 data points
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  • 49
    Publication Date: 2024-01-19
    Keywords: 79-547A; 79-547B; Carbon, organic, total; Carbon dioxide yield, S3 per unit sediment mass; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN; Epoch; Event label; Gas chromatography/mass spectrometry (GF/C filtered); Glomar Challenger; Hydrocarbon yield, S1 per unit sediment mass; Hydrocarbon yield, S2 per unit sediment mass; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Lithologic unit/sequence; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
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  • 50
    Publication Date: 2024-01-19
    Keywords: 79-545; 79-547A; 79-547B; Aromatic hydrocarbon fraction; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Epoch; Event label; Extract; Glomar Challenger; Hydrocarbons; Hydrogen index, mass HC, per unit mass total organic carbon; Latitude of event; Leg79; Liquid chromatography; Lithology/composition/facies; Longitude of event; Nonaromatic hydrocarbon fraction; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 174 data points
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  • 51
    Publication Date: 2024-01-19
    Keywords: 79-547B; Aromatic hydrocarbon fraction; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Extract; Glomar Challenger; Hydrocarbons; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Liquid chromatography; Lithology/composition/facies; Nonaromatic hydrocarbon fraction; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 111 data points
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  • 52
    Publication Date: 2024-01-19
    Keywords: 79-544; 79-544A; 79-545; 79-546; 79-547A; Alkalinity, total; Ammonium; Calcium; Chlorine; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg79; Lithium; Longitude of event; Magnesium; North Atlantic/PLATEAU; pH; Potassium; Salinity; Sample code/label; see reference(s); Silicon; Strontium; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 437 data points
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  • 53
    Publication Date: 2024-01-19
    Keywords: 79-547B; Alginite; Bituminite; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Inertinite; Kerogen microscopy; Leg79; Liptinite; North Atlantic/PLATEAU; Relative fluorescence intensity, ratio; Sample code/label; Vitrinite; Vitrinite reflection; Vitrinite reflection, standard deviation; Wavelength of highest fluorescence intensity
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 54
    Publication Date: 2024-01-19
    Keywords: 79-544A; 79-544B; Carbon, organic, fraction; Carbon, pyrolysis mineral; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Event label; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Lithologic unit/sequence; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Petroleum potential; Production index, S1/(S1+S2); Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 341 data points
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  • 55
    Publication Date: 2024-01-19
    Keywords: 79-545; Carbon, organic, fraction; Carbon, pyrolysis mineral; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Lithologic unit/sequence; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Petroleum potential; Production index, S1/(S1+S2); Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 666 data points
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  • 56
    Publication Date: 2024-01-19
    Keywords: 79-544A; 79-545; 79-546; 79-547A; 79-547B; Calcium; Chlorine; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg79; Longitude of event; Magnesium; North Atlantic/PLATEAU; Salinity; Sample code/label; see reference(s)
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
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  • 57
    Publication Date: 2024-01-19
    Keywords: 79-546; Carbon, organic, fraction; Carbon, pyrolysis mineral; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Lithologic unit/sequence; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Petroleum potential; Production index, S1/(S1+S2); Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 333 data points
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  • 58
    Publication Date: 2024-01-19
    Keywords: 79-547; 79-547A; 79-547B; Carbon, organic, fraction; Carbon, pyrolysis mineral; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Event label; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Leg79; Lithologic unit/sequence; North Atlantic/PLATEAU; Oxygen index, mass CO2, per unit mass total organic carbon; Petroleum potential; Production index, S1/(S1+S2); Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 1358 data points
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  • 59
    Publication Date: 2024-01-19
    Keywords: 79-545; Aromatics; Chloroform extract; Comment; Compounds; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Extract; Glomar Challenger; Leg79; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 61 data points
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  • 60
    Publication Date: 2024-01-19
    Keywords: 79-545; 79-547A; 79-547B; Ash; Carbon; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Event label; Glomar Challenger; Hydrogen; Hydrogen/Carbon ratio; Iron; Latitude of event; Leg79; Longitude of event; Nitrogen, organic; North Atlantic/PLATEAU; Oxygen; Oxygen/Carbon ratio; Sample code/label; Sulfur, organic
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
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  • 61
    Publication Date: 2024-01-19
    Keywords: 79-547A; 79-547B; Aromatics; Chloroform extract; Comment; Compounds; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Extract; Glomar Challenger; Leg79; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 64 data points
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  • 62
    Publication Date: 2024-01-19
    Keywords: 79-547A; 79-547B; Calcispheres; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Echinoid debris; Event label; Fish remains; Foraminifera; Glauconite; Glomar Challenger; Iron oxide; Leg79; Mica; North Atlantic/PLATEAU; Ostracoda; Preservation; Pyrite; Quartz; Radiolarians abundance; Sample code/label; Shell debris; Sponge spiculae
    Type: Dataset
    Format: text/tab-separated-values, 1712 data points
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  • 63
    Publication Date: 2024-01-19
    Keywords: 79-545; Calcispheres; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Echinoid debris; Fish remains; Foraminifera; Glauconite; Glomar Challenger; Iron oxide; Leg79; Mica; North Atlantic/PLATEAU; Ostracoda; Preservation; Pyrite; Quartz; Radiolarians abundance; Sample code/label; Shell debris; Sponge spiculae
    Type: Dataset
    Format: text/tab-separated-values, 1504 data points
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  • 64
    Publication Date: 2024-01-19
    Keywords: 79-547B; Achomosphaera ramulifera; Achomosphaera triangulata; Aptea eisenackii; Callaiosphaeridium trycherium; Canningia ringnesiorum; Cassiculosphaeridia reticulata; Chlamydophorella discreta; Chlamydophorella nyei; Cleistosphaeridium clavulum; Cleistosphaeridium multispinosum; Codoniella campanulata; Cometodinium whitei; Coronifera oceanica; Coronifera tubulosa; Cribroperidinium cooksoniae; Cribroperidinium orthoceras; Cribroperidinium tensiftense; Cyclonephelium brevispinatum; Cyclonephelium cf. membraniphorum; Cyclonephelium compactum; Cyclonephelium distinctum; Cyclonephelium paucimarginatum; Deep Sea Drilling Project; Dissiliodinium globulum; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Exochosphaeridium bifidum; Exochosphaeridium phragmites; Eyrea nebulosa; Florentinia berran; Florentinia mantellii; Florentinia radiculata; Florentinia resex; Florentinia stellata; Fromea amphora; Glomar Challenger; Gonyaulacysta cretacea; Gonyaulacysta helicoidea; Hapsocysta dictyota; Hapsocysta peridictya; Hexagonifera cf. chlamydata; Hystrichodinium pulchrum; Hystrichosphaeridium arundum; Hystrichosphaeridium atlasiense; Hystrichosphaeridium cf. arundum; Kiokansium corollum; Kiokansium polypes; Leg79; Lithosphaeridium siphoniphorum; Litosphaeridium conispinum; Maghrebinia chleuh; Maghrebinia perforata; Maghrebinia perforata perforata; Muderongia perforata; North Atlantic/PLATEAU; Occisucysta coummia; Occisucysta mazaganensis; Occisucysta sousensis; Odontochitina cribropoda; Odontochitina operculata; Oligosphaeridium albertense; Oligosphaeridium asterigerum; Oligosphaeridium complex; Oligosphaeridium irregulare; Oligosphaeridium poculum; Oligosphaeridium pulcherrimum; Oligosphaeridium totum minor; Oligosphaeridium totum totum; Oodnadattia alata; Oodnadattia tuberculata; Ovoidinium diversum; Ovoidinium scabrosum; Palaeoperidinium cretaceum; Pervosphaeridium pseudhystrichodinium; Pervosphaeridium truncatum; Polysphaeridium sp.; Polysphaeridium warrenii; Prolixosphaeridium conulum; Prolixosphaeridium parvispinum; Pterodinium cingulatum cingulatum; Pterodinium cornutum; Sample code/label; Sample ID; Spiniferites ancoriferum ancoriferum; Spiniferites cf. wetzelii; Spiniferites lenzii; Spiniferites multibrevis ghiran; Spiniferites multibrevis multibrevis; Spiniferites multibrevis seghiris; Spiniferites ramosus ramosus; Stage; Subtilisphaera cheit; Subtilisphaera scabrata; Surculosphaeridium trunculum; Systematophora silyba; Tanyosphaeridium regulare; Trabeculodinium quinquetrum; Trichodinium castanea
    Type: Dataset
    Format: text/tab-separated-values, 1134 data points
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  • 65
    Publication Date: 2024-01-19
    Keywords: 79-545; Achomosphaera neptuni; Achomosphaera ramulifera; Achomosphaera sagena; Achomosphaera triangulata; Achomosphaera verdieri; Aptea almohadensis; Aptea eisenackii; Aptea polymorpha; Apteodinium maculatum; Batiacasphaera saidensis; Callaiosphaeridium trycherium; Canningia cf. reticulata; Canningia ringnesiorum; Carpodinium granulatum; Cassiculosphaeridia reticulata; Cassiculosphaeridia tazadensis; Cerbia aucda; Cerbia tabulata; Chlamydophorella discreta; Chlamydophorella nyei; Cleistosphaeridium clavulum; Cleistosphaeridium huguoniotii; Codoniella campanulata; Codoniella psygma; Cometodinium whitei; Coronifera oceanica; Coronifera tubulosa; Cribrodinium edwardsii; Cribroperidinium cf. diaphane; Cribroperidinium cf. orthoceras; Cribroperidinium cooksoniae; Cribroperidinium diaphane; Cribroperidinium orthoceras; Cribroperidinium tensiftense; Cyclonephelium brevispinatum; Cyclonephelium cf. membraniphorum; Cyclonephelium cf. vannophorum; Cyclonephelium chabaca; Cyclonephelium distinctum; Cyclonephelium hystrix; Cyclonephelium maugaad; Cyclonephelium paucimarginatum; Cyclonephelium vannophorum; Danea chibanis; Deep Sea Drilling Project; Dingodinium albertii; Dissiliodinium globulum; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ellipsoidictyum imperfectum; Endoscrinium campanula nichan; Epelidosphaeridia spinosa; Exochosphaeridium bifidum; Exochosphaeridium phragmites; Eyrea nebulosa; Florentinia laciniata laciniata; Florentinia laciniata seghiris; Florentinia mantellii; Florentinia radiculata; Florentinia resex; Florentinia stellata; Fromea amphora; Glomar Challenger; Gonyaulacysta cassidata; Gonyaulacysta cretacea; Gonyaulacysta helicoidea; Hapsocysta peridictya; Heterosphaeridium heteracanthum; Hexagonifera cf. chlamydata; Histiocysta outananensis; Hystrichodinium compactum; Hystrichodinium pulchrum; Hystrichosphaeridium arundum; Hystrichosphaeridium bowerbankii; Hystrichosphaerina schindewolfii; Keithriasphaeridium sarmentum; Kiokansium corollum; Kiokansium hydra; Kiokansium polypes; Kleithriasphaeridium eoinodes; Leg79; Lithosphaeridium siphoniphorum; Litosphaeridium conispinum; Maghrebinia chleuh; Maghrebinia perforata mirabilis; Maghrebinia perforata perforata; Meiourogonyaulax cf. bulloidea; Meiourogonyaulax stoveri; Muderongia perforata; Nematosphaeropsis singularis; North Atlantic/PLATEAU; Occisucysta cf. tenuiceras; Occisucysta hinzii; Occisucysta mazaganensis; Occisucysta sousensis; Occisucysta tentoria; Occisucysta tenuiceras; Odontochitina operculata; Oligosphaeridium albertense; Oligosphaeridium asterigerum; Oligosphaeridium complex; Oligosphaeridium dividuum; Oligosphaeridium djenn; Oligosphaeridium irregulare; Oligosphaeridium poculum; Oligosphaeridium porosum; Oligosphaeridium pulcherrimum; Oligosphaeridium totum minor; Oligosphaeridium totum totum; Oligosphaeridium verrucosum; Oodnadattia alata; Oodnadattia tuberculata; Operculodinium hirsutum; Ovidinium scabrosum; Ovoidinium verrucosum; Palaeohystrichophora infusorioides; Palaeoperidinium cretaceum; Pervosphaeridium truncatum; Phoberocysta neocomica; Polysphaeridium duma; Polysphaeridium flexuosum; Polysphaeridium sp.; Polysphaeridium warrenii; Prolixosphaeridium conulum; Prolixosphaeridium parvispinum; Prolixosphaeridium parvispinum deirense; Protoellipsodinium spinosum; Protoellipsodinium touile touile; Protoellipsoidinium seghire seghire; Pseudoceratium gochtii; Pterodinium agadirense; Pterodinium aliferum; Pterodinium bab; Pterodinium cingulatum cingulatum; Pterodinium cornutum; Pterodinium mamounia; Rhynchodiniopsis aptiana; Sample code/label; Sample ID; Spiniferites ancoriferum ancoriferum; Spiniferites ancoriferum ghiran; Spiniferites cf. wetzelii; Spiniferites cornutus cornutus; Spiniferites dentatus; Spiniferites hyperacanthus; Spiniferites lenzii; Spiniferites magnoserratus; Spiniferites multibrevis ghiran; Spiniferites multibrevis multibrevis; Spiniferites multibrevis seghiris; Spiniferites ramosus ramosus; Spiniferites ramosus reticulatus; Stage; Subtilisphaera cheit; Subtilisphaera deformans; Subtilisphaera scabrata; Subtilisphaera senegalensis; Surculosphaeridium trunculum; Systematophora complicata; Systematophora cretacea; Systematophora silyba; Systematophora sp.; Tanyosphaeridium boletus; Tanyosphaeridium regulare; Trichodinium castanea; Wallodinium luna; Xenascus ceratioides; Xenascus plotei
    Type: Dataset
    Format: text/tab-separated-values, 6356 data points
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  • 66
    Publication Date: 2024-01-19
    Keywords: 79-547B; Achistrum issleri; Akidocheilus transiens; Biologic remains; Bivalvia; Brachiopoda; Bryozoa; Deep Sea Drilling Project; Dictyomitra cf. duodecimcostata; DRILL; Drilling/drill rig; DSDP; Echinoid debris; Emiluvia sp.; Eocaudina mortenseni; Fish remains; Fusinite; Gastropoda; Glomar Challenger; Hadrocheilus liasinus; Hemisphaeranthos cf. carpenteri; Lamellaptychi; Leg79; Mortensenites; North Atlantic/PLATEAU; Ophiuridea; Ostracoda; Paronaella sp.; Podobursa cf. pantanellii; Radiolarians indeterminata; Sample code/label; Theelia mesolissica; Triactinosphaera sp.; Triactoma cf. blakei
    Type: Dataset
    Format: text/tab-separated-values, 572 data points
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  • 67
    Publication Date: 2024-01-19
    Keywords: 79-547A; Achomosphaera ramulifera; Achomosphaera sagena; Achomosphaera triangulata; Aptea eisenackii; Canningia ringnesiorum; Cassiculosphaeridia magna; Cassiculosphaeridia reticulata; Chlamydophorella discreta; Chlamydophorella nyei; Cleistosphaeridium clavulum; Codoniella campanulata; Cometodinium whitei; Coronifera oceanica; Cribroperidinium cooksoniae; Cribroperidinium orthoceras; Cribroperidinium tensiftense; Cyclonephelium brevispinatum; Cyclonephelium cf. chabaca; Cyclonephelium cf. membraniphorum; Cyclonephelium chabaca; Cyclonephelium distinctum; Cyclonephelium paucimarginatum; Cyclonephelium vannophorum; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Endoscrinium ludbrookii; Exochosphaeridium phragmites; Eyrea nebulosa; Florentinia berran; Florentinia laciniata laciniata; Florentinia mantellii; Florentinia radiculata; Florentinia resex; Florentinia stellata; Glomar Challenger; Gonyaulacysta cassidata; Gonyaulacysta cretacea; Gonyaulacysta helicoidea; Hapsocysta dictyota; Heterosphaeridium heteracanthum; Hexagonifera cf. chlamydata; Hystrichodinium pulchrum; Hystrichosphaeridium bowerbankii; Kiokansium corollum; Leg79; Lithosphaeridium siphoniphorum; Litosphaeridium conispinum; Maghrebinia chleuh; Maghrebinia perforata mirabilis; Maghrebinia perforata perforata; North Atlantic/PLATEAU; Occisucysta coummia; Odontochitina operculata; Oligosphaeridium asterigerum; Oligosphaeridium complex; Oligosphaeridium dividuum; Oligosphaeridium irregulare; Oligosphaeridium poculum; Oligosphaeridium porosum; Oligosphaeridium pulcherrimum; Oligosphaeridium totum minor; Oligosphaeridium totum totum; Oodnadattia alata; Oodnadattia tuberculata; Ovoidinium implanum; Ovoidinium scabrosum; Ovoidinium verrucosum; Palaeoperidinium cretaceum; Pervosphaeridium pseudhystrichodinium; Pervosphaeridium truncatum; Polysphaeridium warrenii; Prolixosphaeridium conulum; Prolixosphaeridium parvispinum; Pterodinium cingulatum cingulatum; Pterodinium cornutum; Sample code/label; Sample ID; Spiniferites ancoriferum; Spiniferites cornutus cornutus; Spiniferites hyperacanthus; Spiniferites lenzii; Spiniferites multibrevis ghiran; Spiniferites multibrevis multibrevis; Spiniferites multibrevis seghiris; Spiniferites ramosus ramosus; Spiniferites ramosus reticulatus; Stage; Subtilisphaera cheit; Subtilisphaera scabrata; Subtilisphaera senegalensis; Surculosphaeridium trunculum; Systematophora sp.; Tanyosphaeridium boletus; Tanyosphaeridium regulare; Trabeculodinium quinquetrum; Trichodinium castanea; Xenascus ceratioides; Xenascus plotei
    Type: Dataset
    Format: text/tab-separated-values, 3478 data points
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  • 68
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Holser, William T; Saltzman, Eric S; Brookins, Douglas G (1984): Geochemistry and petrology of evaporites cored from a deep-sea diapir at Site 546 offshore Morocco. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 509-540, https://doi.org/10.2973/dsdp.proc.79.117.1984
    Publication Date: 2024-01-19
    Description: At Site 546, below the Mazagan Escarpment at a water depth of 4 km, 36 m of salt rock was cored from the top of one of a field of salt domes. The core was studied by thin section and a variety of geochemical procedures. The salt rock contains 0.1 to 3% carnallite and lesser amounts of sylvite and polyhalite, which with the corresponding high level of bromide place it within the potash evaporite facies. The bromide profile is of a dominantly marine evaporite deposited in moderately shallow brine which, however, was not repeatedly desiccated. A mineralogical argument suggests that the brine surface was not below sea level. An average of about 5% elastics, with dispersed anhydrite, darken the salt rock to deep shades of red, brown, and gray green. Most of the included materials are in highly deformed boudins or dispersions in the salt rock that has also undergone cataclasis in a subsequent, probably tectonic, deformation. The salt rock is slightly deficient in anhydrite, and the usual separate beds and laminae of anhydrite are virtually absent. Stable isotope ratios of sulfur and oxygen in the sulfate are clearly derived from sea water of Permian to Scythian age, in contrast to the late Triassic or Early Jurassic age of evaporites onshore in Morocco and Portugal and the corresponding evaporites offshore Maritime Canada. In contrast to those evaporites off the axis of Atlantic rifting, the salt at Site 546 may have been deposited in a very early central rift fed by marine waters from Tethys through the Gibraltar or South Atlas fracture zones.
    Keywords: 79-546; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg79; North Atlantic/PLATEAU
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 69
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Riegraf, Wolfgang; Luterbacher, Hanspeter; Leckie, R Mark (1984): Jurassic foraminifers from the Mazagan Plateau, Deep Sea Drilling Project Site 547, Leg 79, off Morocco. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 671-702, https://doi.org/10.2973/dsdp.proc.79.126.1984
    Publication Date: 2024-01-19
    Description: The first marine incursion of the incipient North Atlantic Ocean is recorded in the uppermost Triassic to Lower Jurassic sequence of DSDP Site 547 off central Morocco. A lithologic change from continental red beds below to slope breccias and hemipelagic carbonates above indicates that a carbonate ramp was probably established by Sinemurian time along the Moroccan continental margin and that subsidence in the adjacent basin was rapid in the early phases of continental rift. Foraminifers recovered from the Liassic (Sinemurian-Pliensbachian) basinal deposits are diverse and well preserved. The faunas are compositionally similar to contemporaneous neritic assemblages of Europe and the Grand Banks of Newfoundland. The Middle Jurassic in Hole 547B is characterized by regressive deposits that are poor in foraminifers. The major Late Jurassic "Atlantic" transgression is again represented by basinal deposits consisting of limestone breccias and pelagic carbonates. Foraminifers recovered from this interval are transitional between Late Jurassic assemblages reported from deep-sea deposits in the North Atlantic and typical Late Jurassic neritic assemblages of Europe. The Late Jurassic assemblages of Hole 547B are primarily dominated by nodosariids and spirillinids with moderate abundances of simple arenaceous forms. Nonreticulate epistominids occur very rarely in the Upper Jurassic of Hole 547B. It is tentatively suggested that these represent upper bathyal assemblages.
    Keywords: 79-547B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg79; North Atlantic/PLATEAU
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 70
    Publication Date: 2024-01-19
    Keywords: 79-547B; Ammodiscus glumaceus; Ammodiscus siliceus asper; Ammovertella plicata; Astacolus carinocostata; Astacolus cf. turgidus; Astacolus deformis; Astacolus semiincisus; Astacolus spongiphilis; Astacolus stillus; Astacolus turgidus; Astacolus varians; Bigenerina arcuata; Bigenerina jurassica; Brizalina liasica; Citharina colliezi; Citharina inconstans; Deep Sea Drilling Project; Dentalina aff. pseudoarcuata; Dentalina alternans; Dentalina biloculina; Dentalina cf. terquemi; Dentalina crenata; Dentalina cushmani; Dentalina digitalis; Dentalina glandulinoides; Dentalina gyrosa; Dentalina haeusleri; Dentalina integra; Dentalina jurensis; Dentalina nodigera; Dentalina plebeia; Dentalina sculpta; Dentalina sp.; Dentalina suboligostegia; Dentalina subsiliqua; Dentalina subulata; Dentalina teutoburgensis; Dentalina torta; Dentalina turgida; Dentalina vetustissima; Dorothia dumortieri; DRILL; Drilling/drill rig; DSDP; Eoguttulina bilocularis; Eoguttulina laevis; Eoguttulina liassica; Eoguttulina metensis; Eoguttulina oolithica; Eoguttulina subrhomboidalis; Eoguttulina ventricosa; Epistomina sp.; Foraminifera, benthic porcelaneous indeterminata; Frondicularia major; Frondicularia paradoxa; Frondicularia sacculus; Frondicularia squamosa; Frondicularia terquemi dubia; Frondicularia terquemi terquemi; Glomar Challenger; Glomospira pattoni; Glomospira variabilis; Glomospira virgula; Haplophragmoides barrowensis; Haplophragmoides globigerinoides; Haplophragmoides hyalinus; Haplophragmoides kingakensis; Haplophragmoides pictonicum; Hyperammina liasina; Hyperammina sp.; Jaculella anulata; Lagenammina jurassica; Leg79; Lenticulina gottingensis; Lenticulina hebetata; Lenticulina inermis; Lenticulina oolithica; Lenticulina polygonata; Lenticulina pusilla; Lenticulina quenstedti; Lingulina acuformis; Lingulina aff. tenera; Lingulina affinis; Lingulina cf. dentaliniformis; Lingulina costata; Lingulina dentaliniformis; Lingulina esseyana; Lingulina franconica; Lingulina gottingensis; Lingulina laevissima; Lingulina lingula; Lingulina nodosaria; Lingulina sp.; Lingulina taenioides; Lingulina tenera carinata; Lingulina tenera praepupa; Lingulina tenera tenera; Lingulina tenera tenuistriata; Marginulina brunsvigensis; Marginulina dentaliniformis; Marginulina oolithica; Marginulina paulinae; Marginulina porrecta; Marginulina prima; Marginulina spinata; Marginulina variabilis; Marginulinopsis baccularis; Marginulinopsis matutina matutina; Marginulinopsis matutina terquemi; Marginulinopsis matutina vetusta; Nodosaria alemannica; Nodosaria apheilolocula; Nodosaria caudata; Nodosaria claviformis; Nodosaria clavula; Nodosaria geniculata; Nodosaria incongrua; Nodosaria kunzi; Nodosaria lagenoides; Nodosaria lamellosa; Nodosaria multicostata; Nodosaria ornata; Nodosaria perlata; Nodosaria regularis; Nodosaria sexcostata; Nodosaria simplex; North Atlantic/PLATEAU; Ophthalmidium baccularis; Ophthalmidium carinatum; Ophthalmidium liasicum; Ophthalmidium sp.; Ophthalmidium strumosum; Palmula anceps; Palmula filosa; Palmula gyrata; Palmula hybrida; Palmula irregularis; Palmula nucleata; Palmula pikettyi; Palmula plebeia; Palmula primaria; Palmula primordialis; Palmula semiinvoluta; Palmula triquetra; Patellinella poddari; Pseudonodosaria dubia; Pseudonodosaria metensis; Pseudonodosaria nitidana; Pseudonodosaria sexcostata; Pseudonodosaria turbiniformis; Pseudonodosaria vulgata; Ramulina cf. spandeli; Reophax helveticus; Reophax imperspicuus; Sample code/label; Saracenaria obesa; Spirillina concava; Spirillina gracilis; Spirillina numismalis; Stage; Tolypammina jurensis; Tolypammina sp.; Triloculina meotica; Trochammina canningensis; Trochammina pulchra; Trocholina umbo; Vaginulina aff. jurassica; Vaginulina anomala; Vaginulina contracta; Vaginulina implicata; Vaginulina parva; Vaginulina perfoliata; Vaginulina sp.; Vaginulina triangula; Verneuilinoides tryphera
    Type: Dataset
    Format: text/tab-separated-values, 3360 data points
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  • 71
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schumann, Dieter (1984): Mineralogy of Cenozoic sediments cored during Deep Sea Drilling Project Leg 79 as determined by X-ray diffraction. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Gov. Printing Office), 79, 395-398, https://doi.org/10.2973/dsdp.proc.79.110.1984
    Publication Date: 2024-01-19
    Description: Four sites in the region of the Mazagan Plateau off northwest Africa were drilled during Leg 79 of the Deep Sea Drilling Project. Bulk mineralogy and clay mineralogy were analyzed from the Cenozoic sediments recovered from the four sites.
    Keywords: 79-544A; 79-544B; 79-545; 79-546; 79-547; 79-547A; Apatite; Calcite; Chlorite; Clay minerals; Deep Sea Drilling Project; Dolomite; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Feldspar; Glomar Challenger; Gypsum; Halite; Illite; Kaolinite; Kaolinite+Chlorite; Latitude of event; Leg79; Lithologic unit/sequence; Longitude of event; Mixed layer clay minerals; North Atlantic/PLATEAU; Opal-CT; Palygorskite; Pyrite, FeS2; Quartz; Sample code/label; Sepiolite; Smectite; X-ray diffraction (XRD); X-ray diffraction TEXTUR, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 1735 data points
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  • 72
    facet.materialart.
    Unknown
    PANGAEA
    In:  Deutscher Wetterdienst/Seewetteramt, Offenbach/Hamburg
    Publication Date: 2024-01-19
    Keywords: Characteristic of barometric tendency; Cloud base height; CT; DATE/TIME; Dew/frost point; Direction of first swell waves; Height of first swell waves; Height of waves; High cloud; Horizontal visibility; Humidity, relative; Indicator for inclusion or ommission of precipitation data; Indicator for source and units of wind speed; LATITUDE; LONGITUDE; Low/middle cloud amount; Low cloud; M67; M67-track; Mean ships course; Mean ships speed; Meteor (1964); Middle cloud; Past weather1; Past weather2; Periode of first swell waves; Present weather; Pressure, atmospheric; Quality control indicator for (a); Quality control indicator for (clouds); Quality control indicator for (dd); Quality control indicator for (Ds); Quality control indicator for (ff); Quality control indicator for (h); Quality control indicator for (HwHw); Quality control indicator for (iR,RRR,tR); Quality control indicator for (ppp); Quality control indicator for (PPPP); Quality control indicator for (PwPw); Quality control indicator for (swell); Quality control indicator for (tbtbtb); Quality control indicator for (TdTdTd); Quality control indicator for (TTT); Quality control indicator for (TwTwTw); Quality control indicator for (Vs); Quality control indicator for (VV); Quality control indicator for (weather); Temperature, air; Temperature, air, wet bulb; Temperature, water; Total cloud amount; Underway cruise track measurements; Wave period; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 16128 data points
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  • 73
    Publication Date: 2024-01-19
    Keywords: 79-547A; 79-547B; Biticinella breggiensis; Clavihedbergella moremani; Clavihedbergella simplex; Clavihedbergella subcretacea; Counting 〉63 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Globigerinelloides bentonensis; Globigerinelloides gyroidinaeformis; Globigerinelloides ultramicrus; Glomar Challenger; Gubkinella graysonensis; Guembelitria cenomana; Hedbergella aff. trocoidea; Hedbergella cf. rischi; Hedbergella delrioensis; Hedbergella libyca; Hedbergella paradubia; Hedbergella planispira; Hedbergella simplicissima; Hedbergella sp.; Heterohelix moremani; Leg79; Loeblichella sp.; North Atlantic/PLATEAU; Planktic foraminifera zone; Planomalina buxtorfi; Planomalina praebuxtorfi; Praeglobotruncana delrioensis; Praeglobotruncana stephani; Rotalipora aff. cushmani; Rotalipora appenninica; Rotalipora cushmani; Rotalipora gandolfii; Rotalipora greenhornensis; Rotalipora micheli; Rotalipora montsalvensis; Rotalipora praebalernaensis; Rotalipora reicheli; Rotalipora subticinensis; Rotalipora ticinensis; Sample code/label; Schackoina bicornis; Schackoina cenomana; Schackoina moliniensis; Schackoina multispinata; Ticinella madecassiana; Ticinella praeticinensis; Ticinella primula; Ticinella raynaudi; Ticinella roberti
    Type: Dataset
    Format: text/tab-separated-values, 4863 data points
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  • 74
    Publication Date: 2024-01-19
    Keywords: 79-545; Biticinella breggiensis; Clavihedbergella moremani; Clavihedbergella simplex; Clavihedbergella subcretacea; Comment; Counting 〉63 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, planktic indeterminata; Globigerinelloides algerianus; Globigerinelloides aptiense; Globigerinelloides bentonensis; Globigerinelloides blowi; Globigerinelloides cf. barri; Globigerinelloides cf. saundersi; Globigerinelloides ferreolensis; Globigerinelloides gyroidinaeformis; Globigerinelloides sp.; Globigerinelloides ultramicrus; Glomar Challenger; Gubkinella graysonensis; Guembelitria cenomana; Hedbergella aff. sigali; Hedbergella aff. trocoidea; Hedbergella cf. rischi; Hedbergella delrioensis; Hedbergella gorbachikae; Hedbergella libyca; Hedbergella paradubia; Hedbergella planispira; Hedbergella simplicissima; Hedbergella sp.; Hedbergella trocoidea; Heterohelix moremani; Leg79; Loeblichella sp.; North Atlantic/PLATEAU; Planktic foraminifera zone; Planomalina buxtorfi; Planomalina cheniourensis; Planomalina praebuxtorfi; Praeglobotruncana delrioensis; Praeglobotruncana stephani; Rotalipora aff. cushmani; Rotalipora appenninica; Rotalipora gandolfii; Rotalipora greenhornensis; Rotalipora micheli; Rotalipora praebalernaensis; Rotalipora reicheli; Rotalipora subticinensis; Rotalipora ticinensis; Sample code/label; Schackoina bicornis; Schackoina cenomana; Schackoina moliniensis; Schackoina multispinata; Ticinella madecassiana; Ticinella praeticinensis; Ticinella primula; Ticinella raynaudi; Ticinella roberti
    Type: Dataset
    Format: text/tab-separated-values, 5208 data points
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  • 75
    Publication Date: 2024-01-09
    Keywords: 81-552A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Globigerina atlantica, δ13C; Globigerina atlantica, δ18O; Glomar Challenger; Leg81; Mass spectrometer VG Isogas 903; North Atlantic/PLATEAU; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 312 data points
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  • 76
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    PANGAEA
    In:  Supplement to: Baker, Earl W; Louda, William (1984): Highly deaikylated copper and nickel etioporphyrins in marine sediments. Organic Geochemistry, 6, 183-192, https://doi.org/10.1016/0146-6380(84)90040-8
    Publication Date: 2023-12-07
    Description: Copper porphyrins have been recognized as natural constituents of marine sediments only within the past 5 years (Palmer and Baker, 1978, Science201, 49–51). In that report it was suggested that these pigments may derive from and be markers for oxidized terrestrial organic matter redeposited in the marine environment. In the present study we describe the distribution of copper porphyrins in sediments from several north Pacific and Gulf of California DSDP/IPQD sites (Legs 56,63,64). These allochthonous pigments have now been found to be accompanied by identical arrays of highly dealkylated nickel etioporphyrins. Evaluation of data from this and past studies clearly reveals that there is a strong carbon-number distribution similarity betweeen coincident Cu and Ni etioporphyrins. This homology match is taken as reflecting a common source for the tetrapyrrole ligands of this population of Cu and Ni chelates. Predepositional generation of these highly dealkylated etioporphyrins is concluded from the occurrence of these pigments in sediments continuing essentially all stages of in situ chlorophyll diagenesis (cf. Baker and Louda, 1983). That is, their presence is not regulated by the in situ diagenetic continuum. Thus, the highly dealkylated Cu and Ni etioporphyrins represent an 'allochthonous' background over which 'autochthonous' (viz. marine produced) chlorophyll derivatives are deposited and are undergoing in situ diagenesis.
    Keywords: 42-380A; 42-381; 43-387; 44-391A; 44-391C; 47-397; 47-397A; 47-398D; 57-440B; 63-467; 63-471; 64-474; 64-474A; 64-479; 64-481A; Black Sea; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg42; Leg43; Leg44; Leg47; Leg57; Leg63; Leg64; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/SEAMOUNT; North Pacific/FAN; North Pacific/GAP; North Pacific/Gulf of California/BASIN; North Pacific/TRENCH
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 77
    Publication Date: 2023-12-07
    Keywords: 42-380A; 42-381; 43-387; 44-391A; 44-391C; 47-397; 47-397A; 47-398D; 57-440B; 63-467; 63-471; 64-474; 64-474A; 64-479; 64-481A; Black Sea; C22 carbon number; C23 carbon number; C24 carbon number; C25 carbon number; C26 carbon number; C27 carbon number; C28 carbon number; C29 carbon number; C30 carbon number; C31 carbon number; C32 carbon number; C33 carbon number; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Leg42; Leg43; Leg44; Leg47; Leg57; Leg63; Leg64; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/SEAMOUNT; North Pacific/FAN; North Pacific/GAP; North Pacific/Gulf of California/BASIN; North Pacific/TRENCH; Reference/source; Sample code/label; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 792 data points
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  • 78
    Publication Date: 2023-11-28
    Keywords: Akademik Vernadsky; Archive of Ocean Data; ARCOD; AV19; AV19_2163; AV19_2164; AV19_2166; AV19_2168/2; AV19_2170; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Equator Seamount; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Size fraction 〈 0.100 mm; Size fraction 〉 1 mm, gravel; Size fraction 0.100-0.010 mm; Size fraction 0.250-0.100 mm; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand; Somali Basin; Sum
    Type: Dataset
    Format: text/tab-separated-values, 378 data points
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  • 79
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    PANGAEA
    In:  Supplement to: Shnyukov, Evgeny F; Starostenko, V I; Belevtsev, R Ya; Gozhik, Piotr F; Kalyaev, G I; Koptyukh, Yu M; Overchuk, V O; Slipchenko, V V; Sobotovich, Emlen V; Sobolevsky, Yu V; Chugunny, YuG; Shcherbakov, I B (1984): Geology and Metallogeny of the Northern and Equatorial Indian Ocean. Kiev, Naukova Dumka (E.F. Shnyukov, Ed.), 168 pp
    Publication Date: 2023-11-28
    Description: The monograph has been written on the base of data obtained from samples and materials collected during the 19-th cruise of RV ''Akademik Vernadsky'' to the Northern and Equatorial Indian Ocean. Geological features of the region (stratigraphy, tectonic structure, lithology, distribution of ore-forming components in bottom sediments, petrography of igneous rocks, etc.) are under consideration. Regularities of trace element concentration in Fe-Mn nodules, nodule distribution in bottom sediments, and engineering-geological properties of sediments within the nodule fields have been studied. Much attention is paid to ocean crust rocks. The wide range of ore mineralization (magnetite, chromite, chalcopyrite, pyrite, pentlandite, and other minerals) has been ascertained.
    Keywords: Akademik Vernadsky; Arabian-Indian Ridge; Arabian Sea; Archive of Ocean Data; ARCOD; Argo Fault Zone; AV19; AV19_1484; AV19_1487; AV19_1492; AV19_1493; AV19_1498; AV19_1500; AV19_1516; AV19_1517; AV19_1534; AV19_1544; AV19_1545; AV19_2159; AV19_2161/1,2; AV19_2162; AV19_2163; AV19_2164; AV19_2166; AV19_2168/2; AV19_2170; AV19_2171/2; AV19_2172/1; AV19_2173/3; AV19_2174; AV19_2177/3; AV19_2178; AV19_2180; AV19_2181; AV19_2182/1; AV19_2184; AV19_2185; AV19_2188; AV19_2189/1; AV19_2190/2; AV19_2190/3; AV19_2191/1; AV19_2191/2; AV19_2193/1; AV19_2195/1; AV19_2197/1; Bay of Bengal; Central Basin, Indian Ocean; Continental slope of the Arabian Peninsula; Dredge; DRG; Equator Seamount; GC; Grab; GRAB; Gravity corer; Indostan shelf; Karlsberg Ridge; Maria Celeste Fault Zone; Owen Fault Zone; Shelf of the Arabian Peninsula; Shelf of the Socotra Island; Somali Basin
    Type: Dataset
    Format: application/zip, 15 datasets
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  • 80
    Publication Date: 2023-09-12
    Keywords: 77-540; Amphizygus brooksii; Axopodorhabdus albianus; Axopodorhabdus dietzmannii; Bidiscus ignotus; Biscutum ellipticum; Braarudosphaera primula; Braarudosphaera regularis; Braarudosphaera stenorhetha; Broinsonia signata; Chiastozygus litterarius; Chiastozygus platyrhethus; Corollithion achylosum; Corollithion signum; Cretarhabdus conicus; Cretarhabdus crenulatus; Cretarhabdus loriei; Cribrosphaerella ehrenbergii; Crucicribrum anglicum; Crucicribrum striatum; Cruciellipsis chiastia; Cyclagelosphaera margerelii; Cylindralithus sp.; Darwinulithus pentarhethum; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eiffellithus sp.; Eiffellithus turriseiffelii; Eprolithus floralis; Flabellites biforaminis; Gartnerago nanum; Glomar Challenger; Grantarhabdus coronadventis; Gulf of Mexico; Haqius circumradiatus; Hayesites albiensis; Lapideacassis mariae; Leg77; Lithraphidites acutum spp. eccentricum; Lithraphidites alatus; Lithraphidites carniolensis; Manivitella pemmatoidea; Micrantholithus hockwoldensis; Nannoconus elongatus; Nannoconus spp.; Nannoconus truitti; Nannofossil abundance; Nannofossils preservation; Nannofossil zone; Octocyclus reinhardtii; Ontogenetic stage; Parhabdolithus achylostaurion; Parhabdolithus embergeri; Parhabdolithus infinitus; Prediscosphaera columnata; Prediscosphaera sp.; Prediscosphaera spinosa; Reinhardtites elegans; Reinhardtites fenestratus; Retecapsa angustiforata; Rhagodiscus angustus; Rhagodiscus asper; Rucinolithus irregularis; Sample code/label; Scapholithus fossilis; Stephanolithion laffittei; Tegumentum stradneri; Tetrapodorhabdus coptensis; Tetrapodorhabdus decorus; Tranolithus gabalus; Tranolithus orionatus; Vagalapilla matalosa; Vekshinella angusta; Vekshinella quadriarculla; Vekshinella stradneri; Watznaueria barnesae; Watznaueria biporta; Watznaueria britannica; Watznaueria supracretacea; Zeugrhabdotus erectus; Zeugrhabdotus salillum; Zygodiscus diplogrammus; Zygodiscus spp.; Zygodiscus theta
    Type: Dataset
    Format: text/tab-separated-values, 4106 data points
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  • 81
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    PANGAEA
    In:  Supplement to: Boyce, Robert E (1984): Laboratory-determined sound velocity, porosity, wet-bulk density, acoustic impedance, acoustic anisotropy, and reflection coefficients for Cretaceous-Jurassic turbidite sequences at Deep Sea Drilling Project Sites 370 and 416 off the Coast of Morocco. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 1229-1244, https://doi.org/10.2973/dsdp.proc.75.148.1984
    Publication Date: 2023-09-07
    Description: From 661 to 880 m beneath the seafloor at DSDP Sites 370 and 416 are Albian to Barremian claystone with some limestone, sandstone, and siltstone. Compressional-wave velocities ranged from 1.70 to 4.37 km/s, with an average in situ vertical velocity of 1.93 km/s. From 880 to 1430 m are Hauterivian to Valanginian turbidites of alternating graded calcareous and quartzose cycles from siltstone or fine sandstone to mudstone. Compressional-wave velocities range from 1.80 to 4.96 km/s with an average in situ velocity of 2.61 km/s. From 1430 to 1624 m are early Valanginian to Tithonian (Kimmeridgian?) turbidites, with alternating quartzose siltstone grading to mudstone cycles with hard micritic limestone and calcarenite (calciturbidites). Compressional-wave velocities range from 2.26 to 5.7 km/s, with an average in situ vertical velocity of 3.25 km/s. Acoustic anisotropy is 0 to 30% faster parallel to bedding in Cretaceous to Tithonian sandstone-siltstone turbidites in mudstone and minor limestone from 661 to 1624 m below the seafloor. Between 2.0(?) km/s and 4.2(?) km/s, anisotropy becomes particularly significant (below 1178 m), where the anisotropy is about + 0.4 km/s or greater. The mudstone, softer sandstone, and softer siltstone tend to have velocities around 2.0 to 2.5 km/s; the cemented sandstone and limestone cluster around 2.5 km/s to 4.2 km/s; thus the relative percentage anisotropy is greater for lower-velocity lithologies. Above 4.2(?) km/s, the well-cemented sandstone and limestone tend to have a smaller (less than + 0.4 km/s) absolute anisotropy, and many samples are nearly isotropic. These physical property data are separated into depth plots for (1) mudstone, (2) siltstone (3) sandstone, (4) marlstone, and (5) limestone. The mudstone's porosity and wet-bulk density curves versus depth are slightly higher and lower, respectively, than similar porosity and wet-bulk density curves summarized in Hamilton (1976). These differences could be some combination of (1) differences in laboratory methods; (2) age, lithologic, and cementation differences; or (3) overconsolidation created by a geological sequence which has been eroded away. If the average in situ vertical velocities calculated by Boyce (1980b) for Hole 416A are correct, then the 1.43-s (round-trip) reflector (blue) discussed by Lancelot and Winterer (1980) and Lancelot, Winterer et al. (1980b), would correlate to about 1500 m in Hole 416A, and not below 1624 m as suggested by Lancelot and Winterer. There appears to be a significant change in the acoustic character at or around that depth (1500 m) to a more lithified, calcareous, and cemented lithology. This does not prove Lancelot and Winterer (1980) and Lancelot, Winterer et al. (1980b) to be incorrect, but only suggests another possible interpretation.
    Keywords: 50-416A; Calculated, see reference(s); CFA; Color description; Comment; Continuous Flow Analysis; Deep Sea Drilling Project; Density, wet bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Gamma-ray attenuation porosity evaluator (GRAPE); Glomar Challenger; Impedance, specific; Leg50; Lithology/composition/facies; North Atlantic; Porosity; Sample code/label; Sonic velocity; Temperature, technical; Velocity, compressional wave anisotropy; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 2563 data points
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  • 82
    Publication Date: 2023-09-06
    Keywords: 75-530B; 75-532; Alcohols, n-C26/n-C16 ratio; Alkanes, n-C29/n-C17 ratio; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Gas-liquid chromatography; Glomar Challenger; Leg75; n-C26/n-C16 alkanoic acids ratio; Pristane/n-heptadecane ratio; Pristane/Phytane ratio; Sample code/label; South Atlantic; South Atlantic/RIDGE; Stenols, n-C29/n-C27 ratio; Sum even numbered/sum odd numbered alkanoic acids ratio; Sum even numbered/sum odd numbered n-alkanols ratio; Sum odd numbered/sum even numbered n-alkanes ratio
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
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  • 83
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    PANGAEA
    In:  Supplement to: Cortelezzi, CR; Espósito, G; Iasi, R (1984): Study of manganese nodules from the Malvinas (Falkland) Plateau, South Atlantic Ocean. In: Arndt Wauschkuhn, Cornelia Kluth & Richard A. Zimmermann (eds) Syngenesis and Epigenesis in the Formation of Mineral Deposits, Springer Berlin Heidelberg, 653 pp, 221-227, https://doi.org/10.1007/978-3-642-70074-3_21
    Publication Date: 2023-08-28
    Description: Manganese nodules occurring within marine sediments of presumably Upper Miocene-Lower Pliocene age from cores obtained by the Argentine oceanographic vessel ARA Islas Orcadas in 1977 on the Malvinas (Falkland) Plateau and neighbouring Scotia Sea were studied with the aim of comparing them with other fossil nodules found on the mainland of Argentina that were also ascribed to the marine environment. After optical mineralogical, chemical, X-ray and trace element analysis, the studied "nodules" proved to be actually wacke clasts cemented by manganese oxides with a high Fe/Mn ratio corresponding to a continental environment. The studied "nodules" thus differ from the Argentine mainland nodules and are supposed to have been transported from continental environments and then deposited in the marine realms. The wacke clasts became then nuclei for the deposition of the marine manganese oxides of the coatings. The proportion of trace elements, which is high, suggests the growth of the nodules in the marine environment.
    Keywords: IO13-1477; IO13-1477.001-PC; IO13-1477.006-PC; Islas Orcadas; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 84
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    PANGAEA
    In:  Supplement to: Frazer, Jane Z; Fisk, Mary B; Fitzgerald, R; Guy, J (1976): Chemical analyses of manganese nodules, 1975-1976. Scripps Institution of Oceanography, UC San Diego Report, unpublished
    Publication Date: 2023-08-28
    Description: Manganese nodules have been analysed at the Scripps Institution of Oceanography after having been ground to to a diameter less than 74 microns. Some analysises were performed on pellets by X-ray Emission Spectroscopy for 1000 Seconds. All concentrations have been corrected to 110 degrees Celsius drying conditions (see: https://doi.pangaea.de/10.1594/PANGAEA.854202).
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 85
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    PANGAEA
    In:  Supplement to: Ridout, Paul; Carpenter, M S N; Morris, R J (1984): Analysis of a metalliferous encrustation from a seamount in the Gulf of Guinea. Chemical Geology, 42(1-4), 219-225, https://doi.org/10.1016/0009-2541(84)90016-0
    Publication Date: 2023-08-28
    Description: Morphological, mineralogical and chemical analysis are reported for a metalliferous encrustation from a seamount in the Gulf of Guinea, South Atlantic. The results are compared with published data on encrustation from similar environments. The morphology and mineralogy indicate a crust formed on the exposed rock surface with some agglutination of foram debris. Comparison of the abundance patterns for transition elements with that of known data suggests that some enrichment had resulted from the high primary productivity at this site.
    Keywords: Aluminium; Atlantic Ocean; BC; Box corer; Calcium; Cobalt; Copper; D10516; DEPTH, sediment/rock; Description; Elevation of event; Iron; Latitude of event; Longitude of event; Loss on ignition; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Sample ID; Silicon; Titanium; Wet chemistry; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 86
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    PANGAEA
    In:  Supplement to: Sliter, William V; Premoli Silva, Isabella (1984): Autochthonous and displaced (allochthonous) Cretaceous benthic foraminifers from Deep Sea Drilling Project Leg 77, Sites 535, 536, 537, 538, and 540, Gulf of Mexico. In: Buffler, R.T; Schlager, W.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VXXII, 593-627, https://doi.org/10.2973/dsdp.proc.77.125.1984
    Publication Date: 2023-08-28
    Description: Mesozoic benthic foraminifers, recovered from five single-bit holes drilled in the southern Gulf of Mexico on Deep Sea Drilling Project Leg 77 are rare, poorly preserved, and scattered throughout the dominantly redeposited sediments. The Mesozoic sequence at basin Sites 535 and 540 consists largely of laminated limestone with smaller amounts of skeletal limestone and pure pelagic limestone, whereas the Mesozoic sediments at basement Sites 536, 537, and 538 (Hole 538A) consist largely of oolitic-oncolitic limestone.
    Keywords: 77-536; 77-537; 77-538A; 77-540; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Gulf of Mexico; Gulf of Mexico/KNOLL; Gulf of Mexico/SLOPE; Identification; Leg77; 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, 105 data points
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  • 87
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; ELT07; ELT07.012-PC; ELT12; ELT12.006-PC; Eltanin; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 88
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    PANGAEA
    In:  Institute of Oceanographic Sciences, Wormley
    Publication Date: 2023-08-28
    Description: The main objective of the cruise was to study the sediments and sedimentary processes in an area known as Great Meteor East (GME) - part of a feasibility study into the ocean disposal of high-level radioactive waste commissioned by the Department of the Environment. Previous cruises (Discovery 118, 126, 134 and Farnella 3/81) had done much of the ground work, consequently the area was already well known but not necessarily well understood for the purposes of our investigation.
    Keywords: Atlantic Ocean; D144; D1979; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 89
    Publication Date: 2023-08-28
    Description: The drilling plan for Leg 74 of the Deep Sea Drilling Project was designed to address three main scientific topics: (1) the history of the deep-water circulation in the southeastern Atlantic, (2) the nature and geologic evolution of the Walvis Ridge, and (3) the biostratigraphy and magnetic stratigraphy of this region. In order to study these subjects, a suite of five sites was drilled on the Walvis Ridge that extended from its crest (near 1000 m water depth) down its northwest flank into the Angola Basin to a depth of 4400 m.
    Keywords: 74-527; 74-528; 74-528A; 74-529; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; Event label; Glomar Challenger; Identification; Leg74; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Atlantic; South Atlantic/RIDGE; South Atlantic/SLOPE; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 74 data points
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  • 90
    Publication Date: 2023-08-28
    Description: Leg 73 was the middle of five legs on South Atlantic paleoenvironments planned by the JOIDES Ocean Paleoenvironment (OP) Panel during the years from 1975 to 1980. The idea of drilling a transect of holes across the 30°S parallel was entertained soon after the drilling on Leg 3, during the first phase of the Deep Sea Drilling Project (1968/69), when the surprising discovery was made that the middle Miocene sediments of the South Atlantic were largely marls and red clays. The deposition of the red clays was obviously related to the intense dissolution of calcite during the middle Miocene, when the calcite-compensation level was elevated. The objectives and tactical planning for a transect across the east flank of the Mid-Atlantic Ridge just north of 30°S were outlined by the OP Panel more fully to the Planning Committee in July of 1978. After a piston core containing Paleocene sediments was taken in 1979 at the site in the Cape Basin at the foot of the Walvis Ridge this area was designated for DSDP Leg 73 and 74.
    Keywords: 73-519A; 73-520; 73-521; 73-522; 73-522A; 73-522B; 73-523; 73-524; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; Elevation of event; Event label; File name; Glomar Challenger; Identification; Latitude of event; Leg73; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Atlantic/CANYON; South Atlantic/HILL; South Atlantic/PLATEAU; South Atlantic/RIDGE; South Atlantic/VALLEY; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 385 data points
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  • 91
    Publication Date: 2023-08-28
    Description: Site 530 is located in the southeastern corner of the Angola Basin, about 20 km north of the Walvis Escarpment, near the eastern end of the easternmost (or Frio) segment of the Walvis Ridge. It lies on the abyssal floor of the Angola Basin and exhibits a seismic stratigraphic sequence typical for the entire deep part of the basin. It was selected because it appears to have the oldest strata in the region preserved in a sediment pond between low basement rises.
    Keywords: 75-530; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg75; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Atlantic/RIDGE; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 92
    Publication Date: 2023-08-28
    Description: The drilling of Leg 77 is part of an overall program by the JOIDES Passive Margin Panel to study the evolution of the western North Atlantic passive margin. The history of the central North Atlantic is probably the best known of all ocean basins, but the origin and history of the neighboring Gulf of Mexico are very much uncertain. Some geologists consider it the oldest ocean basin still in existence (Paleozoic), but others doubt the existence of "true" oceanic crust under the central Gulf. The nature and origin of the transitional crust and the overlying Mesozoic sedimentary sequences in the southeastern Gulf, therefore, was the main objective of Leg 77.
    Keywords: 77-535; 77-536; 77-537; 77-538A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Gulf of Mexico/BASIN; Gulf of Mexico/KNOLL; Gulf of Mexico/SLOPE; Identification; Leg77; 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, 130 data points
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  • 93
    Publication Date: 2023-08-28
    Description: The principal goal of Site 543 was definition of an oceanic reference section. One of the specific objectives was to provide a physical-property profile through the undisturbed oceanplate section and thereby a basis for measuring the tectonic consolidation of any offscraped rocks of similar lithology in the area of the Tiburon and Barracuda rises which constitute prominent highs emerging from the Atlantic abyssal plain and presently intersecting the deformation front of the Barbados Ridge complex.
    Keywords: 78-543; 78-543A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg78; Leg78AB; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 94
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Piper, David Z; Basler, J R; Bischoff, James L (1984): Oxidation state of marine manganese nodules. Geochimica et Cosmochimica Acta, 48(11), 2347-2355, https://doi.org/10.1016/0016-7037(84)90230-8
    Publication Date: 2023-08-28
    Description: Analyses of the bulk oxidation state of marine manganese nodules indicates that more than 98% of the Mn in deep ocean nodules is present as Mn(IV). The samples were collected from three quite different areas: the hemipelagic environment of the Guatemala Basin, the pelagic area of the North Pacific, and seamounts in the central Pacific. Results of the study suggest that todorokite in marine nodules is fully oxidized and has the following stoichiometry: (K, Na, Ca, Ba)0.33 (Mg, Cu, Ni)0.76 Mn5 O22 (H2O)3.2.
    Keywords: Atomic absorption spectrometry (AAS); BC; Box corer; Cobalt; Copper; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DMSA-DJ18; DMSA-DJ2; DMSA-DJ39; DNWB0ABD; DOMES Site A, Pacific Ocean; DOMES Site C, Pacific Ocean; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD4; DWHD16; Elevation of event; Event label; Horizon; Insoluble residue; Iron; Latitude of event; Longitude of event; Magnesium; Manganese; MANOP Site H, Pacific Ocean; MDPC02HO-MP-025F-1; MDPC02HO-MP-025F-2; MDPC03HO-MP-043C; Melville; MIDPAC; MPC-25F-1; MPC-25F-2; MPC-43C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; RP23OC77; RP-23-OC77; RP8OC76; RP-8-OC-76; RP8OC76-10-15; RP8OC76-11-16; RP8OC76-12-18; RP8OC76-13-19; RP8OC76-14-20; RP8OC76-15-21; RP8OC76-1-6; RP8OC76-16-22; RP8OC76-17-23; RP8OC76-18-24; RP8OC76-21-27; RP8OC76-4-9; RP8OC76-6-11; RP8OC76-8-13; RP8OC76-9-14; Sample ID; Spencer F. Baird; VLCN-1; VLCN-1-68BX; VULCAN Leg 1; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 269 data points
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  • 95
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Calvert, Stephen E; Piper, David Z (1984): Geochemistry of ferromanganese nodules from DOMES site a, Northern Equatorial Pacific: Multiple diagenetic metal sources in the deep sea. Geochimica et Cosmochimica Acta, 48(10), 1913-1928, https://doi.org/10.1016/0016-7037(84)90374-0
    Publication Date: 2023-08-28
    Description: The major and minor element composition of ferromanganese nodules from DOMES Site A has been determined by X-ray fluorescence methods. Three phases appear to control the bulk compositions: Mn and Fe oxyhydroxides and aluminosilicates. Relatively wide compositional variations are evident throughout the area. Nodules with high Mn/Fe ratios, high Cu, Mg, Mo, Ni and Zn concentrations and high todorokite/-MnO2 ratios have gritty surface textures and are confined to an east-west trending depression with thin Quaternary sediment cover. Nodules with low Mn/Fe ratios, high concentrations of As, Ca, Ce, Co, La, P, Sr, Ti, V, Y and Zr and low todorokite/-MnO2 ratios have smooth surfaces and are confined to shallower areas with relatively thick Quaternary sediment to the north and south of the depression. All nodules in the area have compositions which are influenced by diagenesis, but those with the most marked diagenetic signature (high Mn/Fe and Cu/Ni ratios, low Ce/La ratios and more todorokite) are found in areas of very slow or non-existent sedimentation; many of these nodules are actually in contact with outcropping Tertiary sediment. This paradox may be resolved by postulating, by analogy with some shallow-water occurrences, that the nodules accrete from bottom waters which have enhanced particulate and dissolved metal contents derived from diagenetic reaction in areas remote from the site of nodule formation. The metals are supplied in a bottom flow (probably Antarctic Bottom Water) which also erodes, or prevents modern sedimentation in, the depression. Nodules on the flanks of the depression are not evidently affected by this flow and derive at least pan of their constituent metals from diagenetic reaction in the underlying Quaternary sediment. Apparently, abyssal diagenetic nodules can have an immediate and a remote diagenetic metal source. Metal fluxes derived from pore water dissolved metal gradients may not be relevant to particular accreting nodules if a significant fraction of their metals is derived from outside the area in which they form.
    Keywords: Aluminium; Arsenic; Barium; BC; Box corer; Calcium; Cerium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DMSA-DJ1; DMSA-DJ10; DMSA-DJ11; DMSA-DJ12; DMSA-DJ13; DMSA-DJ14; DMSA-DJ15; DMSA-DJ16; DMSA-DJ17; DMSA-DJ18; DMSA-DJ19; DMSA-DJ2; DMSA-DJ20; DMSA-DJ21; DMSA-DJ22; DMSA-DJ23; DMSA-DJ24; DMSA-DJ25; DMSA-DJ27; DMSA-DJ28; DMSA-DJ29; DMSA-DJ3; DMSA-DJ30; DMSA-DJ32; DMSA-DJ34; DMSA-DJ36; DMSA-DJ39; DMSA-DJ4; DMSA-DJ40; DMSA-DJ41; DMSA-DJ42; DMSA-DJ44; DMSA-DJ46; DMSA-DJ47; DMSA-DJ48; DMSA-DJ49; DMSA-DJ50; DMSA-DJ52; DMSA-DJ59; DMSA-DJ6; DMSA-DJ63; DMSA-DJ65; DMSA-DJ66; DMSA-DJ69; DMSA-DJ7; DMSA-DJ70; DMSA-DJ72; DMSA-DJ73; DMSA-DJ8; DMSA-DJ9; DMSA-DJA3; DOMES Site A, Pacific Ocean; Elevation of event; Environment; Event label; Identification; Iron; Lanthanum; Latitude of event; Lead; Longitude of event; Loss on ignition; Magnesium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Phosphorus; Potassium; RP23OC77; RP-23-OC77; Rubidium; Sample code/label; Silicon; Sodium; Strontium; Texture; Titanium; Todorokite/MnO2 peak ratio; Vanadium; Wet chemistry; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 2507 data points
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  • 96
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Smith, J N; Schafer, C T (1984): Bioturbation processes in continental slope and rise sediments delineated by Pb?210, microfossil and textural indicators. Journal of Marine Research, 42(4), 1117-1145, https://doi.org/10.1357/002224084788520738
    Publication Date: 2023-08-28
    Description: Measurements of Pb-210 activities, in conjunction with micropaleontological, geotechnical and sedimentological observations, on sediment cores have been used to characterize two distinctive bioturbation regimes on the continental slope and rise east of Newfoundland. On the rise (2600 m), excess Pb-210 is confined to the upper few centimeters of the coarser-grained sediments underlying the axis of the Western Boundary Undercurrent. The geological and geochemical evidence for a low rate of bioturbation in this high bottom current regime is consistent with a reduced population of deeper burrowing macrofauna, particularly the species Maldane sarsi. In contrast, a higher flux of organic-rich, fine-grained particulate material to the middle slope (1500 m water depth), and the comparatively stable sedimentological conditions that prevail in this low bottom current regime, have led to the active colonization of the sediment substrate by bioturbating organisms. Enhanced mixing of middle slope deposits is reflected by comparatively lower shear strengths within the upper 30 cm of the sediment column, and by the reduced variability of the sediment-depth distribution of the most abundant species of foraminifera. Excess Pb-210 has been transported downward from the sediment-water interface to depths greater than 12 cm. Some Pb-210 profiles from the middle slope can be interpreted in terms of a diffusion mixing model for which the biological mixing coefficients are of the order of 0.10-1.0 cm2/yr.Measurements of the two and three dimensional distribution of excess Pb-210 in one middle slope box core indicate that the mixing process in these sediments has a pronounced heterogeneous component on time scales of the same order as the half life of Pb-210 (22.3 yr). Spatial correlations between Pb-210 anomalies and artifacts of bioturbation observed in x-radiographs of the core suggest that Pb-210 maxima observed at depth may be the result of an inclined orientation of burrow structures which have introduced a significant lateral component to the downward transport of surficial sediments.
    Keywords: Comment; Dawson; Deposit type; DEPTH, sediment/rock; Description; DW77-034; DW77-034-12C; DW77-034-16C; Elevation of event; Event label; File name; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic; 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
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Moore, Willard S (1984): Thorium and radium isotopic relationships in manganese nodules and sediments at MANOP Site S. Geochimica et Cosmochimica Acta, 48(5), 987-992, https://doi.org/10.1016/0016-7037(84)90190-X
    Publication Date: 2023-08-28
    Description: Relationships among Th and Ra isotopes in nodule, sediment and water phases at MANOP Site S establish the most likely source for Th in the nodules, the frequency of nodule turning, and the similarity of micro and macro nodules. Manganese nodules and bottom waters have 230Th/232Th activity ratios considerably higher than other phases at this site suggesting that sea water is the likely source of Th for the nodules. Similar 230Th/232Th activity ratios in nodule tops and bottoms and in certain cases departure from expected 226Ra/230Th activity ratios in nodule tops and bottoms indicate that the nodules rotate every one to ten thousand years. The micro nodules have diffusion coefficients of Ra similar to macro nodule bottoms. I suggest that they may act as a carrier phase for transporting metals through oxic sediments to nodules.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 98
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Poppe, L J; Commeau, R F; Commeau, J A; Manheim, Frank T; Aruscavage, P J (1984): Ferromanganese micronodules from the surficial sediments of Georges Bank. Journal of Marine Research, 42(2), 463-472, https://doi.org/10.1357/002224084788502765
    Publication Date: 2023-08-28
    Description: Ferromanganese micronodules have been found on Georges Bank, off the U.S. northeast coast, distributed throughout the surficial sediments within an area about 125 km long and at least 12 km wide. These coarse, sand-sized concretions have precipitated from metal-rich interstitial waters and contain many of the textural and structural features common to other neritic nodules. Most of the nodules have accreted around detrital grains, and X-ray powder diffraction analyses indicate the presence of geothite and vernadite ( delta -MnO sub(2)) in the ferromanganese layers. Chemical analyses of the micronodules, when compared with similar data on deep-sea manganese nodules, reveal lower Mn/Fe ratios, significantly higher concentrations of V and As, comparable values of Mo, and an order of magnitude less of Co, Ni, Ce and most other, metals.
    Keywords: AB3_101; AB3101-W167; AB3101-W169; AB3101-W180; AB4_11; AB411-2545K; Albatross III (1948-1959); Albatross IV (1963); Atlantic Ocean; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GOS22; GOS22-1114; GOS22-1123; Gosnold; 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; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 99
    Publication Date: 2023-08-28
    Description: The cores and dredges described at this site were taken on the RIDA cruise from 1 May until 25 May 1984 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 45 cores and dredges were recovered along with underwater camera runs. They are available at MNHN for sampling and study.
    Keywords: Comment; CS840027; CS840029; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DR840026; DR840031; DR840033; DR840036; Dredge; DRG; Elevation of event; Event label; GS840583; GS840584; GS840585; GS840587; GS840590; GS840593; GS840596; GS840597; Identification; Indian Ocean; Latitude of event; Longitude of event; Marion Dufresne (1972); MD39; MD39-08; MD39-12; MD39-12d; MD39-17; MD39-17d; MD39-18a; MD39-18b; MD39-19; MD39-22; MD39-24; MD39-24c; MD39-25; MD39-26; MD39-29; MD39-30; MD39-34; MD-DR840026; MD-DR840028; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; RIDA - Ride de Davie; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
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  • 100
    Publication Date: 2023-08-28
    Keywords: 7TOW_1; 7TOW01WT; BC; Box corer; Calcium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DOMES Site C, Pacific Ocean; Dredge; DRG; Elevation of event; Event label; FFGR; Free-fall grab; Identification; Iron; KEN-1-10FF; KEN-1-6FF; KEN-1-7FF; Latitude of event; Lead; Longitude of event; Manganese; Method/Device of event; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; RP6OC75; RP6OC75-24B-29; SCR-MR-1; SCR-MR-10; SCR-MR-11; SCR-MR-13; SCR-MR-14; SCR-MR-15; SCR-MR-16; SCR-MR-17; SCR-MR-18; SCR-MR-19; SCR-MR-2; SCR-MR-21; SCR-MR-22; SCR-MR-23; SCR-MR-25; SCR-MR-26; SCR-MR-27; SCR-MR-29; SCR-MR-3; SCR-MR-30; SCR-MR-31; SCR-MR-32; SCR-MR-33; SCR-MR-34; SCR-MR-35; SCR-MR-36; SCR-MR-38; SCR-MR-39; SCR-MR-4; SCR-MR-40; SCR-MR-41; SCR-MR-42; SCR-MR-43; SCR-MR-45; SCR-MR-46; SCR-MR-47; SCR-MR-48; SCR-MR-49; SCR-MR-5; SCR-MR-50; SCR-MR-51; SCR-MR-52; SCR-MR-53; SCR-MR-54; SCR-MR-55; SCR-MR-56; SCR-MR-57; SCR-MR-59; SCR-MR-6; SCR-MR-61; SCR-MR-62; SCR-MR-63; SCR-MR-64; SCR-MR-65; SCR-MR-66; SCR-MR-67; SCR-MR-68; SCR-MR-69; SCR-MR-7; SCR-MR-70; SCR-MR-71; SCR-MR-72; SCR-MR-73; SCR-MR-74; SCR-MR-75; SCR-MR-9; Shape; Size; Thomas Washington; X-ray emission spectroscopy (XES)
    Type: Dataset
    Format: text/tab-separated-values, 1183 data points
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