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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 295 (1982), S. 105-110 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In an East Mediterranean marine core, the upper sapropel begins soon after the start of a global event—a very heavy precipitation which occurred in the equatorial latitudes during the late Glacial–early Holocene. This heavy precipitation in Africa, channelled by the Nile River across ...
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2016-08-02
    Description: This study documents the biological signatures impressed upon the sedimentary record underlying both the 5°N upwelling system of the Somali Current and the equatorial area of the Somali Basin out of the upwelling influence. The evolution of these two distinct hydrographic systems is compared for the last 160 kyr. Correspondence and cluster analyses are performed on combined radiolarian and planktonic foraminiferal quantitative data in order to study the changes of the planktonic assemblages through time and space. The Upwelling Radiolarian Index (URI) is used as a productivity proxy. The water temperature and hydrographic structure of the upper water masses appear to be the major factors controlling the distribution patterns of the fauna. The relative abundances of three groups of foraminifera, cold water form (dextral N. pachyderma), mixed layer dwellers (G. trilobus, G. ruber, G. sacculifer, G. conglobatus, and G. glutinata), and thermocline dwellers (G. menardii, G. tumida, N. dutertrei, G. crassaformis, and P. obliquiloculata), follow distinct evolutionary patterns at the two sites during the last 160 kyr. At the equatorial site (core MD 85668), downcore fluctuations in the relative abundances of the three groups are closely related to the glacial/interglacial cyclicity and provide some insights into the interpretation of hydrographic changes. The dominance of the mixed layer foraminifera at the transition intervals between isotope stages 6/5 and 2/1, combined with weak URI values, is thought to reflect the reorganization of the oceanographic circulation. These short-term events (with a duration of 〈 5000 year) could be related to the rapid inflow of oxygen-depleted water through the Indonesian straits as a result of sea level rise during deglaciation. Underneath the 5°N gyre (core MD 85674), the response to global climatic changes is overprinted by the regional effect of the Somalian upwelling, which has been persistent over the last 160 kyr.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    PANGAEA
    In:  Supplement to: Vergnaud-Grazzini, Colette; Saliège, Jean Francois (1985): Pleistocene climatic changes in surface waters of the northeastern Atlantic: Oxygen and carbon isotopic compositions of planktonic foraminifers at Deep Sea Drilling Project Sites 548 and 549. In: De Graciansky, PC; Poag, CW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Gov. Printing Office), 80, 793-803, https://doi.org/10.2973/dsdp.proc.80.130.1985
    Publication Date: 2023-05-12
    Description: Oxygen- and carbon-isotope analyses have been performed on the Quaternary planktonic foraminifers of Sites 548 and 549 (DSDP Leg 80) to investigate major water mass changes that occurred in the northeastern Atlantic at different glacial-interglacial cycles and to compare them with the well-defined picture of 18,000 yr. ago. Oxygen-isotope stratigraphy also provides a chronological framework for the more important data on the fauna and flora. Although bioturbation and sedimentary gaps obliterate the climatic and stratigraphic record, general trends in the oceanographic history can be deduced from the isotopic data. Isotopic stratigraphy has tentatively been delineated down to isotopic Stage 16 at Site 548 and in Hole 549A. This stratigraphy fits well with that deduced from benthic foraminiferal d18O changes and with bioclimatic zonations based on foraminiferal associations at Site 549. Variations in the geographic extension and in the flux of the Gulf Stream subtropical waters are inferred from both d18O and d13C changes. Maximal fluxes occurred during the late Pliocene. Northward extension of subtropical waters increased through the various interglacial phases of the early Pleistocene and decreased through the late Pleistocene interglacial phases. Conversely, glacial maxima were more intense after Stage 16. Isotopic Stages 12 and 16 mark times of important change in water mass circulation. Oxygen- and carbon-isotope analyses have been performed on the Quaternary planktonic foraminifers of Sites 548 and 549 (DSDP Leg 80) to investigate major water mass changes that occurred in the northeastern Atlantic at different glacial-interglacial cycles and to compare them with the well-defined picture of 18,000 yr. ago. Oxygen-isotope stratigraphy also provides a chronological framework for the more important data on the fauna and flora. Although bioturbation and sedimentary gaps obliterate the climatic and stratigraphic record, general trends in the oceanographic history can be deduced from the isotopic data. Isotopic stratigraphy has tentatively been delineated down to isotopic Stage 16 at Site 548 and in Hole 549A. This stratigraphy fits well with that deduced from benthic foraminiferal d18O changes and with bioclimatic zonations based on foraminiferal associations at Site 549. Variations in the geographic extension and in the flux of the Gulf Stream subtropical waters are inferred from both d18O and d13C changes. Maximal fluxes occurred during the late Pliocene. Northward extension of subtropical waters increased through the various interglacial phases of the early Pleistocene and decreased through the late Pleistocene interglacial phases. Conversely, glacial maxima were more intense after Stage 16. Isotopic Stages 12 and 16 mark times of important change in water mass circulation.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
    Publication Date: 2023-05-12
    Keywords: Calculated; Depth, bathymetric; DEPTH, sediment/rock; LATITUDE; LONGITUDE; Mass spectrometer VG SIRA 9; Sample code/label; Uvigerina spp., δ13C; Uvigerina spp., δ18O; Δδ13C; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 117 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: Depth, bottom/max; Depth, top/min; Ficarazzi; Isotopic event; Italy; OUTCROP; Outcrop sample; SECTION, height
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Ficarazzi; Globigerinoides ruber, δ18O; Italy; OUTCROP; Outcrop sample; SECTION, height; Uvigerina peregrina, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 164 data points
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Bonneau, M-C; Vergnaud-Grazzini, Colette; Berger, Wolfgang H (1980): Stable isotope fractionation and differential dissolution in recent planktonic foraminifera from Pacific box-cores. Oceanologica Acta, 3(3), 377-381
    Publication Date: 2023-05-12
    Description: Stable isotope analyses and scanning electron micrographs have been carried out on six planktonic forminifera species, Pulleniatina obliquiloculata, Globorotalia tumida, Sphaeroidinella dehiscens, Globigerinoides ruber, Globigerinoides sacculifer and Globigerinoides quadrilobatus from eleven box-cores taken at increasing depths in the equatorial Ontong-Java Plateau (Pacific). This allows us to describe the way dissolution affects the microstructures of the tests of the different species and to quantify the changes of isotopic composition. We may conclude that: 1) dissolution effects on test morphology and stable isotope compositions are species dependent, species with a similar habitat showing a similar trend; 2) the shallow water, thin-shelled species are the first to disappear: scanning electron microscope (SEM) work shows alteration of outer layers. Deep water, thick-shelled species are present in all samples: SEM work shows breakdown and disparition of inner layers; 3) for all species there is a similar trend towards increasing delta18O values with increasing water depths and increasing dissolution. This effect may be as high as 0.6 ‰ per thousand meters for Globorotalia tumida; 4) below the lysocline, around 3500 m, it appears that 13C/12C ratios slightly increase towards equilibrium values for thick shelled species: G. tumida, P. obliquiloculata and S. dehiscens. 14C dates and isotope stratigraphy of two box-cores show that all samples are recent in age, and exclude upward mixing of glacial deposits as an important factor.
    Keywords: BC; Box corer; DEPTH, sediment/rock; Elevation of event; ERDC; ERDC-079BX; ERDC-088BX; ERDC-092BX; ERDC-120BX; ERDC-123BX; ERDC-125BX; ERDC-128BX; ERDC-129BX; ERDC-131BX; ERDC-136BX; ERDC-141BX; Event label; Globigerinoides quadrilobatus, δ13C; Globigerinoides quadrilobatus, δ18O; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Globorotalia tumida, δ13C; Globorotalia tumida, δ18O; Isotope ratio mass spectrometry; Latitude of event; Longitude of event; Pulleniatina obliquiloculata, δ13C; Pulleniatina obliquiloculata, δ18O; Sphaeroidinella dehiscens, δ13C; Sphaeroidinella dehiscens, δ18O; Thomas Washington
    Type: Dataset
    Format: text/tab-separated-values, 92 data points
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  • 8
    Publication Date: 2023-05-12
    Keywords: AC85-4; Age model; Age model, stable isotope stratigraphy; DEPTH, sediment/rock; FAEGAS_IV; Le Noroit; Mass spectrometer VG SIRA 9; Mediterranean Sea; PC; Piston corer; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 111 data points
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  • 9
    Publication Date: 2023-05-12
    Keywords: Age model; Age model, stable isotope stratigraphy; DEPTH, sediment/rock; FAEGAS_IV; KC82-21; Le Noroit; Mass spectrometer VG SIRA 9; Mediterranean Sea; PC; Piston corer; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 93 data points
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  • 10
    Publication Date: 2023-05-12
    Keywords: Age model; Age model, stable isotope stratigraphy; DEPTH, sediment/rock; FAEGAS_IV; KC82-26; Le Noroit; Mass spectrometer VG SIRA 9; Mediterranean Sea; PC; Piston corer; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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