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  • 1985-1989  (24)
  • 1989  (24)
Document type
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  • 1985-1989  (24)
Year
  • 1
    Keywords: Dust-Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Research Workshop, Oracle, AZ, U.S.A., November 17-19, 1987.
    Type of Medium: Online Resource
    Pages: 1 online resource (904 pages)
    Edition: 1st ed.
    ISBN: 9789400909953
    Series Statement: Nato Science Series C: Series ; v.282
    DDC: 551.6
    Language: English
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  • 2
    Keywords: Reisebericht ; Atlantischer Ozean ; Geologie ; Expedition
    Type of Medium: Book
    Pages: 40, [29] S , Ill., graph. Darst., Kt , 29 cm
    Series Statement: Berichte / Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität Kiel, BR Deutschland Nr. 36
    Language: German
    Note: Beitr. teilw. dt., teilw. engl
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  • 3
    Publication Date: 2018-10-02
    Description: Near-surface sediments from the equatorial east Atlantic and the Norwegian Sea exhibit pronounced shear strength maxima in profiles from the peak Holocene and Pleistocene. These semi-indurated layers start to occur at 8–102 cm below the sediment surface and can be explained neither by the modal composition nor by the effective overburden pressure of the sediments. However, scanning electron microscope and microprobe data exhibit micritic crusts and crystal carpets, which are clearly restricted to (undisturbed) samples from indurated layers and form a manifest explanation for their origin. The minerals precipitated comprise calcite, aragonite, and in samples more proximal to the African continent SiO2 needles, and needles of as yet unidentified K-Mg-Fe-Al silicates, crusts of which dominate the indurated layers in the Norwegian Sea. By their stratigraphic position in deep-sea sediments the carbonate-based shear strength maxima are tentatively ascribed to dissolved adjacent pteropod layers from the early Holocene and hence to short-lived no-analogue events of early diagenesis. Possibly, they have been controlled by a reduced organic carbon flux, leading to increased aragonite preservation in the deep sea.
    Type: Article , PeerReviewed
    Format: text
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  • 4
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    PANGAEA
    In:  Supplement to: Sarnthein, Michael; Tiedemann, Ralf (1989): Toward a high-resolution stable isotope stratigraphy of the last 3.4 million years: Sites 658 and 659 off Northwest Africa. In: Ruddiman, W; Sarnthein, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 108, 167-185, https://doi.org/10.2973/odp.proc.sr.108.159.1989
    Publication Date: 2024-01-09
    Description: Ocean Drilling Program Site 658, cored below a major upwelling cell offshore Cap Blanc, contains a largely undisturbed hemipelagic sediment section spanning the Brunhes Chron and the early Quaternary and late Pliocene. The companion Site 659 recovered a complete and undisturbed Neogene profile further offshore that serves as a nonupwelling pelagic reference section. Oxygen and carbon isotope ratios in benthic (C. wuellerstorfi and in part Uvigerina sp.) and planktonic foraminifers (G. inflata) provide a climatic record of high resolution for the Brunhes Chron. At Site 658 the record extends back to the early Pleistocene and late Pliocene. The standard oxygen isotope record of the last 730,000 yr is markedly refined by a well-documented high-frequency variation (e.g., by a new "aborted" ice age at stage 13.2 and by Younger-Dryas style climatic setbacks during most terminations). In the late Pliocene, the numerical oxygen isotope stage taxonomy was extended back to stage 137 about 3.3 Ma ago. In comparison with published records, stage 114 at 2.7 Ma represents the first major glaciation event, when 18O was short-term enriched up to a middle Pleistocene glacial d18O level. About 3.17 Ma ago (stage 133), the interglacial oxygen isotope values of C. wuellerstorfi started to increase by 0.5 per mil until 2.7 Ma and then remained largely constant until the Holocene. Based on the d13C difference between C. wuellerstorfi and G. inflata, the dissolved CO2 in the ambient bottom water of Site 658 was dominated by the flux of particulate carbon from the overlying upwelling cell during the last 630,000 yr. In contrast, the advection of (upper) North Atlantic Bottom Water dominated in the control of the local CO2 content during the early Pleistocene and late Pliocene.
    Keywords: 108-658; 108-659; Canarias Sea; COMPCORE; Composite Core; Joides Resolution; Leg108; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Tiedemann, Ralf; Sarnthein, Michael; Stein, Ruediger (1989): Climatic changes in the western Sahara: aeolo-marine sediment record of the last 8 million years (Sites 657-661). In: Ruddiman, W; Sarnthein, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 108, 241-277, https://doi.org/10.2973/odp.proc.sr.108.169.1989
    Publication Date: 2024-01-09
    Description: Five Ocean Drilling Program sites (657-661), which form a north-south transect off the western periphery of the Sahara, were selected to measure the long-term history of Saharan/Sahelian dust flux and fluvial sediment discharge and the fluxes of marine CaCO3 and opal over the last 8 m.y. Sites 658 and 659 served for high-resolution studies, and Sites 657, 660, and 661 for insights into the spatial patterns of dust flux. The nearshore mean flux of opal off Cap Blanc (21 °N) showed an abrupt increase about 3 Ma that appears to reflect the main onset of coastal upwelling fertility and enhanced trade winds. At the same time, the input of river-borne clay strongly decreased, suggesting a dry up of the central Saharan rivers. Later, marked short-lived spikes of clay and opal may indicate ongoing ephemeral pulses of fluvial runoff linked to peak interglacial stages. Given the zonal dust discharge centered near 18 °N at Site 659, the aridification of the south Sahara and Sahel increased in several steps: at 4.6, 4.3, and especially at 4.0, 3.6, and 2.1 Ma, and again, at 0.8 Ma. The late Miocene and earliest Pliocene were humid. Although the central and north Saharan climate appears to be linked to the glaciation history of the Northern Hemisphere, the long-term aridification further south followed a different schedule. The spatial distribution of quartz accumulation suggests that the dust outbreaks linked to the Intertropical Convergence Zone during summer did not shift in latitude back to 4.0 Ma, at least. The short-term variations of dust output over the last 0.5 m.y. followed orbital scale pulses with a strong precessional signal, showing a link of Sahelian humidity changes to the variation of sea-surface temperature and evaporation in the tropical Atlantic.
    Keywords: 108-657; 108-658; 108-658A; 108-659; 108-660; 108-661; Canarias Sea; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg108; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 6
    Publication Date: 2024-02-02
    Keywords: Calculated; Carbon, organic, total; Density, wet bulk; DEPTH, sediment/rock; Element analyser CHN, LECO; Giant box corer; GIK23055-2; GKG; Grain size, SEDIGRAPH 5000; Grain size, sieving; M2/2; Meteor (1986); Norwegian Sea; Overburden pressure; Quaternary Environment of the Eurasian North; QUEEN; Sand; Sensitivity; Silt; Size fraction 〈 0.002 mm, clay
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 7
    Publication Date: 2024-02-02
    Keywords: Calculated; Carbon, organic, total; Density, wet bulk; DEPTH, sediment/rock; Element analyser CHN, LECO; Giant box corer; GIK23059-2; GKG; Grain size, SEDIGRAPH 5000; Grain size, sieving; M2/2; Meteor (1986); Norwegian Sea; Overburden pressure; Quaternary Environment of the Eurasian North; QUEEN; Sand; Sensitivity; Silt; Size fraction 〈 0.002 mm, clay
    Type: Dataset
    Format: text/tab-separated-values, 101 data points
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  • 8
    Publication Date: 2024-02-02
    Keywords: 377; AGE; Age, maximum/old; Age, minimum/young; ANT-IV/1c; Atlantic Ocean; BC; Box corer; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Equatorial Atlantic; Event label; GC; GEOTROPEX 83, NOAMP I; Giant box corer; GIK16402-1; GIK16403-1; GIK16404-1; GIK16405-1; GIK16407-1; GIK16408-1; GIK16410-1; GIK16413-1; GIK16415-1; GIK16416-1; GIK16417-1; GIK16426-1; GIK16453-2; GIK16455-1; GIK16457-1; GIK16458-2; GIK23055-2; GIK23056-2; GIK23057-1; GIK23059-2; GIK23062-3; GIK23063-2; GIK23064-2; GIK23065-2; GIK23068-3; GIK23070-2; GIK23071-3; GIK23072-2; GIK23074-1; GKG; Gravity corer; KAL; Kasten corer; Latitude of event; Longitude of event; M2/2; M65; Meteor (1964); Meteor (1986); Norwegian Sea; Polarstern; PS08; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 108-657; AGE; Calcium carbonate; Canarias Sea; COMPCORE; Composite Core; Density, dry bulk; DEPTH, sediment/rock; Joides Resolution; Leg108; Ocean Drilling Program; ODP; Quartz; Siliciclastics; Weighted; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 224 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 108-660; AGE; Calcium carbonate; COMPCORE; Composite Core; Density, dry bulk; DEPTH, sediment/rock; Joides Resolution; Leg108; Ocean Drilling Program; ODP; Quartz; Siliciclastics; South Atlantic Ocean; Weighted; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 390 data points
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