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  • 1985-1989  (1,263,373)
  • 1975-1979  (865,643)
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Year
  • 1
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    Drilling in a high temperature and overpressured area Sunda Straits, Indonesia (1977)
    IPA
    Details
    Publication Date: 2024-05-08
    Description: The Aminoil Group drilled a 10,000 ft - well a few kilometers off the Krakatau volcano in 1973. The well bottomed in Pliocene sediments after penetrating a more than 8,000 ft thick Upper Pliocene section of mainly claystones with interbedded sand-, siltstones and pyroclastics. On the basis of temperature surveys and BHT's measured during logging, a static formation temperature in excess of 450° F was extrapolated for the bottom of the hole. Tue high temperatures caused some deterioration in the mud properties, but otherwise no serious drilling problems. Owing to overpressures a high salinity oil mud and controlled drilling had to be employed. The well was P&A because no economic hydrocarbon accumulations could be expected in the high temperature regimes.
    Type: Conference or Workshop Item , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 2
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    Modelluntersuchungen zur Dynamik des Oder-Mündungsgebietes (1988)
    Details
    Publication Date: 2024-05-06
    Description: Das Stettiner Haff ist von großer wirtschaftlicher Bedeutung, dabei jedoch auch Gegenstand wissenschaftlicher Untersuchungen. Die Verbindung zwischen Szczecin, Polens größtem Ostseehafen, und der Ostsee bedeutet einerseits die wirtschaftliche Anbindung an die Handelsrouten durch die Ostsee und nach Übersee, andererseits besteht ein großes wissenschaftliches Interesse an den hydrographischen Verhältnissen, besonders in bezug auf die Dynamik und den Massenaufbau eines Gebietes, in dem salzreiche und salzarme Wasserkörper aufeinandertreffen. So gibt es bereits seit Beginn des vorigen Jahrhunderts Pegelregistrierungen (Swinoujscie 1810, Wolgast 1848, Szczecin 1851 nach Majewski [28]). Die fischereiwirtschaftliche Nutzung, die auch heute noch intensiv betrieben wird, macht eine Überwachung und Vorhersage der chemischen und biologischen Entwicklung des Gewässers notwendig. Dabei spielen einerseits der Einfluß der Ostsee, andererseits die zunehmende Verschmutzung der Gewässer im Einzugsbereich der Oder eine wesentliche Rolle. In der hier vorgestellten Arbeit sollen die Bewegungs- und Transportvorgänge dieses Gebietes, welches das Stettiner Haff sowie die Mündungsarme von Peene, Swina und Dziwna umfaßt, mit Hilfe eines numerischen Modells simuliert werden. Mit der erfolgreichen Anpassung wird das Modell die Vorhersage von Wasserstandsänderungen, insbesondere die Überschwemmungsgefahr bei Sturmfluten, sowie von Geschwindigkeitsverteilungen und Massenaufbau ermöglichen können.
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 3
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    Comparison of glacial/interglacial carbonate concentrations in Atlantic sediments (1987)
    PANGAEA
    In:  Supplement to: Balsam, William L; McCoy, F M J (1987): Atlantic sediments: glacial/interglacial comparisons. Paleoceanography, 2(5), 531-542, https://doi.org/10.1029/PA002i005p00531
    Details
    Publication Date: 2024-05-02
    Description: To assess the regional effects of glaciation on sedimentation in the Atlantic Ocean we compare sediment types, distributions, and rates between Recent (core top) and last glacial maximum (LGM: ~18,000 years B.P.) stratigraphic levels. Based upon smear slides and carbonate analyses in 178 cores we find that glacial age carbonate content is generally lower than Recent. During both the Recent and LGM, carbonate content shows an east/west asymmetry with western basins exhibiting lower carbonate values. Input of ice-rafted detritus into the North Atlantic during LGM time interrupts this topographic control on carbonate distribution considerably farther south than at present; in the South Atlantic this effect is minor. Comparison of LGM and Recent sediment distributions indicates that the LGM seafloor was dominated by biogenic oozes, calcareous clays, and clays, while the Recent is dominated by biogenic oozes and marls. Coarse-grained detritus is much more prevalent in LGM sediments, derived not only from glacial input but also from fluvial and aeolian sources. Sedimentation rates, calculated from LGM to Recent sediment thickness in cores, are 〈4 cm/1000 yr for most of the ocean. Higher rates are typical of the continental margin off the Amazon River, the North American Basin, and a small region off west equatorial Africa.
    Keywords: A150/180; A152-118; A156-3; A156-4; A164-24; A164-5; A164-6; A164-61; A167-13; A167-14; A173-13; A173-4; A179-15; A180-15; A180-16; A180-32; A180-39; A180-47PC; A180-48PC; A180-56; A180-72; A180-73; A180-74; A180-76; A180-9; Atlantic Ocean; Barcelona Coast; Cork Harbour; Guadiana Estuary; Himmerfjarden; Lamont-Doherty Earth Observatory, Columbia University; LDEO; Limfjorden; Oder Estuary; PC; Pertuis Charentais; Piston corer; Quaternary Environment of the Eurasian North; QUEEN; RC08; RC08-145; RC08-18; RC09; RC09-225; RC09-49; RC10; RC10-288; RC10-289; RC11; RC1112; RC11-21; RC11-26; RC11-86; RC12; RC12-234; RC12-241; RC12-267; RC12-291; RC12-294; RC13; RC13-189; RC13-205; RC13-210; RC13-227; RC13-229; RC15; RC15-94; RE5-034; RE5-036; RE5-054; Robert Conrad; Scheldt Delta Estuary; SP008-004; Taranto Mare Piccolo; TC; Thau Lagoon; Trigger corer; V04; V04-1; V04-32; V04-8; V15; V15-157; V15-168; V16; V16-205; V16-25; V16-36; V17; V17-165; V17-178; V18; V18-110; V19; V19-240; V19-248; V19-281; V19-282; V19-283; V19-291; V19-309; V20; V20-212; V20-227; V20-228; V20-241; V20-242; V22; V22-168; V22-171; V22-172; V22-174; V22-177; V22-182; V22-186; V22-188; V22-196; V22-197; V22-219; V22-222; V22-234; V22-26; V22-38; V22-83; V22-86; V23; V23-100; V23-145; V23-23; V23-42; V23-58; V23-59; V23-60; V23-74; V23-81; V23-82; V23-83; V23-84; V23-91; V23-98; V24; V24-1; V24-221; V24-229; V24-235; V24-237; V24-240; V25; V25-21; V25-42; V25-44; V25-56; V25-59; V25-60; V26; V26-104; V26-175; V26-176; V26-177; V26-37; V26-41; V26-46; V26-63; V26-82; V27; V27-110; V27-116; V27-17; V27-171; V27-175; V27-178; V27-19; V27-20; V27-228; V27-232; V27-238; V27-239; V27-240; V27-248; V27-263; V27-264; V27-265; V27-267; V27-269; V27-46; V27-47; V27-60; V27-84; V27-85; V27-86; V28; V28-108; V28-14; V28-35; V28-38; V28-56; V28-59; V28-89; V29; V29-144; V29-153; V29-173; V29-174; V29-177; V29-178; V29-179; V29-180; V29-206; V29-210; V29-219; V30; V30-100; V30-101; V30-36; V30-40; V30-41; V30-49; V30-51; V30-96; V30-97; V30-99; V31; V31-166; V31-178; Vema
    Type: Dataset
    Format: application/zip, 2 datasets
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    DATA PANGAEA
  • 4
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    Estimates of annual mean surface temperatures in the late Quaternary of the tropical Atlantic (1986)
    PANGAEA
    In:  Supplement to: Mix, Alan C; Ruddiman, William F; McIntyre, Andrew (1986): Late Quaternary paleoceanography of the Tropical Atlantic, 1: spatial variability of annual mean sea-surface temperatures, 0-20,000 years B.P. Paleoceanography, 1(1), 43-66, https://doi.org/10.1029/PA001i001p00043
    Details
    Publication Date: 2024-05-02
    Description: At least two modes of glacial-interglacial climate change have existed within the tropical Atlantic Ocean during the last 20,000 years. The first mode (defined by cold glacial and warm interglacial conditions) occurred symmetrically north and south of the equator and dominated the eastern boundary currents and tropical upwelling areas. This pattern suggests that mode 1 is driven by a glacial modification of surface winds in both hemispheres. The second mode of oceanic climate change, defined by temperature extremes centered on the deglaciation, was hemispherically asymmetrical, with the northern tropical Atlantic relatively cold and the southern tropical Atlantic relatively warm during deglaciation. A likely cause for this pattern of variation is a reduction of the presently northward cross-equatorial heat flux during deglaciation. No single mechanism accounts for all the data. Potential contributors to oceanic climate changes are linkage to high-latitude climates, modification of monsoonal winds by ice sheet and/or insolation changes, atmospheric CO2 and greenhouse effects, indirect effects of glacial meltwater, and variations in thermohaline overturn of the oceans.
    Keywords: A150/180; A179-15; East Atlantic; EN06601; EN066-10GGC; Endeavor; GC; GIK12392-1; Gravity corer; KAL; Kasten corer; Lamont-Doherty Earth Observatory, Columbia University; LDEO; M12392-1; M25; Meteor (1964); PC; Piston corer; RC09; RC09-49; RC13; RC13-184; RC13-189; RC24; RC24-1; RC24-16; RC24-27; RC24-7; Robert Conrad; TC; Trigger corer; V15; V15-168; V22; V22-174; V22-177; V22-182; V22-222; V22-38; V23; V23-110; V25; V25-56; V25-59; V25-60; V25-75; V29; V29-144; V30; V30-36; V30-40; V30-41k; V30-49; V30-51k; V32; V32-8; Vema
    Type: Dataset
    Format: application/zip, 34 datasets
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  • 5
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    Estimates of sea surface temperatures in the Coral Sea (1989)
    PANGAEA
    In:  Supplement to: Anderson, David M; Prell, Warren L; Barratt, N J (1989): Estimates of sea surface temperature in the Coral Sea at the last glacial Maximum. Paleoceanography, 4(6), 615-627, https://doi.org/10.1029/PA004i006p00615
    Details
    Publication Date: 2024-05-02
    Description: The CLIMAP [1981] reconstruction of the Coral Sea found relatively little cooling (2°C) in the low latitudes (10°S) but a warming off Australia at about 25°S. The small low-latitude changes are of interest because terrestrial pollen and snowline data from the New Guinea highlands imply that surface temperatures may have been 6° to 9°C colder at the last glacial maximum (LGM). The purpose of this paper is to evaluate these conclusions on the basis of additional core sites, new oxygen isotope stratigraphy, and new sea surface temperature (SST) estimates using the modern analog technique (MAT). In the northern Coral Sea, planktonic foraminifer assemblages consist of tropical-subtropical species that show little change over the past 20 kyr. Quantitative estimates of SST using the modern analog technique (MAT) confirm the CLIMAP [1981] conclusion that little or no temperature change occurred in this tropical region at the LGM, thus reinforcing the conflict with terrestrial evidence. In the southern region (25°S), two cores indicate that foraminifer faunas became more subtropical at the LGM. The MAT estimates for the LGM are 3° to 4°C colder than modern, producing a steeper thermal gradient in the southern Coral Sea. These data remove the warm SST anomaly along the eastern coast of Australia and indicate that during the LGM, cool high- latitude waters were displaced northward along the coast of Australia into the southern Coral Sea.
    Keywords: Lamont-Doherty Earth Observatory, Columbia University; LDEO; PC; Piston corer; RC09; RC09-124; RC09-126; RC10; RC10-131; RC12; RC12-107; RC12-109; RC12-113; Robert Conrad; V24; V24-157; V24-161; V24-166; V24-170; V24-184; Vema
    Type: Dataset
    Format: application/zip, 22 datasets
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  • 6
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    (Table 3) Stable oxygen isotope ratios of Globigerinoides ruber from sediment core A179-015 (1986)
    PANGAEA
    Details
    Publication Date: 2024-05-02
    Keywords: A150/180; A179-15; DEPTH, sediment/rock; Globigerinoides ruber white, δ18O; Lamont-Doherty Earth Observatory, Columbia University; LDEO; TC; Trigger corer
    Type: Dataset
    Format: text/tab-separated-values, 22 data points
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  • 7
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    Distribution of calcium carbonate in Atlantic sediments from the last glacial (18 kyr) (1987)
    PANGAEA
    Details
    Publication Date: 2024-05-02
    Keywords: A150/180; A152-118; A156-3; A156-4; A164-24; A164-5; A164-6; A164-61; A167-13; A167-14; A173-13; A173-4; A179-15; A180-15; A180-16; A180-32; A180-39; A180-47PC; A180-48PC; A180-56; A180-72; A180-73; A180-74; A180-76; A180-9; Atlantic Ocean; Barcelona Coast; Calcium carbonate; Cork Harbour; DEPTH, sediment/rock; Element analysis, Vacuum-gasometric (Jones & Kaiteris, 1983); Elevation of event; Event label; Guadiana Estuary; Himmerfjarden; Lamont-Doherty Earth Observatory, Columbia University; LATITUDE; LDEO; Limfjorden; LONGITUDE; Oder Estuary; PC; Pertuis Charentais; Piston corer; Quaternary Environment of the Eurasian North; QUEEN; RC08; RC08-145; RC08-18; RC09; RC09-225; RC09-49; RC10; RC10-288; RC10-289; RC11; RC1112; RC11-21; RC11-26; RC11-86; RC12; RC12-234; RC12-241; RC12-267; RC12-291; RC12-294; RC13; RC13-189; RC13-205; RC13-210; RC13-227; RC13-229; RC15; RC15-94; RE5-034; RE5-036; RE5-054; Robert Conrad; Scheldt Delta Estuary; SP008-004; Taranto Mare Piccolo; TC; Thau Lagoon; Trigger corer; V04; V04-1; V04-32; V04-8; V15; V15-157; V15-168; V16; V16-205; V16-25; V16-36; V17; V17-165; V17-178; V18; V18-110; V19; V19-240; V19-248; V19-281; V19-282; V19-283; V19-291; V19-309; V20; V20-212; V20-227; V20-228; V20-241; V20-242; V22; V22-168; V22-171; V22-172; V22-174; V22-177; V22-182; V22-186; V22-188; V22-196; V22-197; V22-219; V22-222; V22-234; V22-26; V22-38; V22-83; V22-86; V23; V23-100; V23-145; V23-23; V23-42; V23-58; V23-59; V23-60; V23-74; V23-81; V23-82; V23-83; V23-84; V23-91; V23-98; V24; V24-1; V24-221; V24-229; V24-235; V24-237; V24-240; V25; V25-21; V25-42; V25-44; V25-56; V25-59; V25-60; V26; V26-104; V26-175; V26-176; V26-177; V26-37; V26-41; V26-46; V26-63; V26-82; V27; V27-110; V27-116; V27-17; V27-171; V27-175; V27-178; V27-19; V27-20; V27-228; V27-232; V27-238; V27-239; V27-240; V27-248; V27-263; V27-264; V27-265; V27-267; V27-269; V27-46; V27-47; V27-60; V27-84; V27-85; V27-86; V28; V28-108; V28-14; V28-35; V28-38; V28-56; V28-59; V28-89; V29; V29-144; V29-153; V29-173; V29-174; V29-177; V29-178; V29-179; V29-180; V29-206; V29-210; V29-219; V30; V30-100; V30-101; V30-36; V30-40; V30-41; V30-49; V30-51; V30-96; V30-97; V30-99; V31; V31-166; V31-178; Vema
    Type: Dataset
    Format: text/tab-separated-values, 178 data points
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  • 8
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    (Table 2) Age model of sediment core RC24-27 (1986)
    PANGAEA
    Details
    Publication Date: 2024-05-02
    Keywords: Age model; DEPTH, sediment/rock; Lamont-Doherty Earth Observatory, Columbia University; LDEO; PC; Piston corer; RC24; RC24-27; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 4 data points
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  • 9
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    (Table 4) Ge/Si ratio, Si, opal, and age model of Site ELT17.009-PC (1989)
    PANGAEA
    Details
    Publication Date: 2024-05-02
    Keywords: Age model; Age model, biostratigraphy; DEPTH, sediment/rock; ELT17; ELT17.009-PC; Eltanin; Germanium/Silica, biogenous opal ratio; Graphite furnace atomic absorption spectrometer (GF-AAS); Lamont-Doherty Earth Observatory, Columbia University; LDEO; Opal, biogenic silica; Opal, extraction; Mortlock & Froelich, 1989; PC; Piston corer; Silicon; Silicon Cycling in the World Ocean; SINOPS
    Type: Dataset
    Format: text/tab-separated-values, 74 data points
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  • 10
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    (Table 2) Stable isotope analysis on planktonic foraminifer G. sacculifer from sediment core RC12-109 (1989)
    PANGAEA
    Details
    Publication Date: 2024-05-02
    Keywords: DEPTH, sediment/rock; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Lamont-Doherty Earth Observatory, Columbia University; LDEO; Mass spectrometer VG SIRA 24; PC; Piston corer; RC12; RC12-109; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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