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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 410 (2001), S. 917-920 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Dating the onset of deep-water flow between the Arctic and North Atlantic oceans is critical for modelling climate change in the Northern Hemisphere and for explaining changes in global ocean circulation throughout the Cenozoic era (from about 65 million years ago to the present). In the early ...
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Nature 398, 57–61 (1999) In this Letter, the legend to Fig. 2 has the descriptions switched for the last two panels. The image shown in Fig. 2c is in fact of H. hauckii , with scale bar 20 µm, and that in Fig. 2d is of P. ...
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 398 (1999), S. 57-61 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The origins of sapropels (sedimentary layers rich in organic carbon) are unclear, yet they may be a key to understanding the influence of climate on ocean eutrophication, the mechanisms of sustaining biological production in stratified waters and the genesis of petroleum source rocks. Recent ...
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1573-0417
    Keywords: laminated sediments ; varves ; palaeoceanography ; palaeolimnology ; palaeoclimatology ; backscattered electron imagery
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Conventional high resolution studies of varved sediments are able to identify clastic and biogenic laminae, but are often unable to resolve the nature of fine-scale lamination contained therein. This intra-annual signal provides us with the highest potential resolution from the sedimentary record and can be resolved using scanning electron microscopy (SEM). Six case studies from lacustrine and marine settings are presented to illustrate the combination of clastic and biogenic fabric types typically found in laminated sediments. Clastic laminae fabrics include those which originate through grain settling and those which are ‘event deposits’. The correct identification of event deposits is essential if varves are to be used chronologically. SEM-based biogenic laminae fabric studies have identified seasonal faunal successions where individual laminae may be less than 100 μ thick and most recently, deep chlorophyll maxima (DCM) summer diatom floras, providing an insight into seasonal scale processes. High resolution lamina fabric studies can provide a basis for generating records of seasonal and inter-annual variability, thus contributing to our understanding of lacustrine and marine processes and palaeoenvironmental interpretation.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-02-10
    Keywords: Age model; DEPTH, sediment/rock; OMEXII-9K_2; Tropical North Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 85 data points
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  • 6
    Publication Date: 2023-02-12
    Description: This data release contains stable isotope data from benthic foraminifera isolated from sediment core OMEXII-9K off the Iberian Margin, from 0 to 204cm, and an updated age model.
    Keywords: Cibicidoides pachyderma, δ13C; Cibicidoides pachyderma, δ13C standard deviation; Cibicidoides pachyderma, δ18O; Cibicidoides pachyderma, δ18O standard deviation; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ13C, standard deviation; Cibicidoides wuellerstorfi, δ18O; Cibicidoides wuellerstorfi, δ18O standard deviation; DEPTH, sediment/rock; OMEXII-9K_2; Tropical North Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 140 data points
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  • 7
    Publication Date: 2023-05-20
    Description: The West Antarctic Peninsula (WAP) is a highly productive shelf region during austral summer, supporting a rich ecosystem that has a significant impact on carbon sequestration. This ecosystem is heterogeneous, and characterised by biological "hotspots" fuelled largely by diatom production. The specific mechanisms determining the location and extent of these hotspots are not fully understood. Sedimentary enrichment of silicic acid (DSi) relative to other nutrients along the WAP, suggest that nutrient transfer across the sediment-water interface could have an impact on algal community composition. Here we combine reaction-transport modelling with porewater profiles of DSi concentration and stable silicon isotopic composition, biogenic silica content (BSi) and diatom abundances from sediment cores collected along the WAP, to assess the DSi flux and the processes that release this key nutrient from the WAP sediment into the overlying waters. We estimate a DSi diffusive flux of 2.67- 10**10 ± 2.75- 10**9 mol/yr for the WAP continental shelf area, which is lower than that previously estimated for the open Southern Ocean. Porewater isotopic compositions suggest that DSi concentrations are supplied primarily by BSi dissolution and respond to authigenic phase formation. Reaction-transport modelling highlights the highly dynamic environment of core-top sediments and the strong impact of surface productivity on sedimentary processes and the early diagenetic release of DSi. Both observations and modelling suggest a strong pelagic influence on benthic environment with the silicon benthic fluxes highly variable on different temporal and spatial scales, and thus sensitive to sea ice dynamics and climate change.
    Keywords: Benthic flux; Campaign; continental shelf; DATE/TIME; DEPTH, sediment/rock; early diagenesis; Event label; James Clark Ross; JR15003; JR15003_1; JR15003_2; JR15003_3; Latitude of event; Longitude of event; MULT; Multiple investigations; Opal, biogenic silica; Silicate; Silicon cyle; Station label; West Antarctic Peninsula; δ30Si, silicic acid; δ30Si, silicic acid, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 259 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Seeberg-Elverfeldt, Ismene A; Lange, Carina Beatriz; Arz, Helge Wolfgang; Pätzold, Jürgen; Pike, Jennifer (2004): The significance of diatoms in the formation of laminated sediments of the Shaban Deep, Northern Red Sea. Marine Geology, 209(1-4), 279-301, https://doi.org/10.1016/j.margeo.2004.05.019
    Publication Date: 2023-06-27
    Description: Laminated sediments spanning the last 20,000 years (though not continuously) in the Shaban Deep, a brine-filled basin in the northern Red Sea, were analyzed microscopically and with backscattered electron imagery in order to determine laminae composition with emphasis on the diatomaceous component. Based on this detailed study, we present schematic models to propose paleoflux scenarios for laminae formation at different time-slices. The investigated core (GeoB 5836-2; 26°12.61'N, 35°21.56'E; water depth 1475 m) shows light and dark alternating laminae that are easily distinguishable in the mid-Holocene and at the end of the deglaciation (13-15 ka) period. Light layers are mainly composed of coccoliths, terrigenous material and diatom fragments, while dark layers consist almost exclusively of diatom frustules (monospecific or mixed assemblages). The regularity in the occurrence of coccolith/diatom couplets points to an annual deposition cycle where contrasting seasons and associated plankton blooms are represented (diatoms-fall/winter deposition, coccoliths-summer signal). We propose that, for the past ~15,000 years, the laminations represent two-season annual varves. Strong dissolution of carbonate, with the concomitant loss of the coccolith-rich layer in sediments older than 15 ka, prevents us from presenting a schematic model of annual deposition. However, the diatomaceous component reveals a marked switch in species composition between Last Glacial Maximum (LGM) sediments (dominated by Chaetoceros resting spores) and sediments somewhat younger (18-19 ka; dominated by Rhizosolenia). We propose that different diatom assemblages reflect changing conditions in stratification in the northern Red Sea: Strong stratification conditions, such as during two meltwater pulses at 14.5 and 11.4 ka, are reflected in the sediment by Rhizosolenia layers, while Chaetoceros-dominated assemblages represent deep convection conditions.
    Keywords: Center for Marine Environmental Sciences; Color description; Comment; DEPTH, sediment/rock; GeoB5836-2; Gravity corer (Kiel type); M44/3; MARUM; Meteor (1986); Northern Red Sea; SL; Texture
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Allen, Claire Susannah; Pike, Jennifer; Pudsey, Carol J; Leventer, Amy (2005): Submillennial variations in ocean conditions during deglaciation based on diatom assemblages from the southwest Atlantic. Paleoceanography, 20(2), PA2012, https://doi.org/10.1029/2004PA001055
    Publication Date: 2023-06-27
    Description: We present a high-resolution paleoceanographic record of deglaciation based on diatom assemblages from a core located just south of the Polar Front in the southwest Atlantic. Core KC073 is from a sediment drift at the mouth of the Falkland Trough and contains sediments from the Last Glacial Maximum (LGM) to present, dated using radiocarbon dates on bulk organic matter and radiolarian stratigraphy. The site lies along the path of the Antarctic Circumpolar Current (ACC) and immediately downstream of where North Atlantic Deep Water (NADW) is entrained into the ACC. Significant variations in ocean conditions are reflected in high-amplitude changes in diatom concentrations and assemblage composition. The diatom assemblage at the LGM indicates that winter sea ice extent was at least 5° farther north than present until at least 19.0 ka (calendar years) and summer sea ice may have occasionally extended over the site, but for the most part it lay to the south. During deglaciation, Chaetoceros resting spores (CRS) dominate the diatom assemblage with valve concentrations in excess of 500 * 10**6 valves per gram. Submillennial-scale variations in the numbers of CRS and Thalassiosira antarctica occur throughout the late deglacial and dominate the changes in diatom concentration. We propose that the influx of CRS is controlled by the flow of NADW over the Falkland Plateau. As such our data provide unique evidence that NADW impacted on this sector of the Southern Ocean during deglaciation. During the Holocene the sedimentation rate dramatically reduced. We suggest that the ACC flow increased over the site and inhibited settling and winnowed the surface sediments.
    Keywords: Age, 14C AMS; Age, 14C calibrated, CALIB 4.4 (Stuiver et al., 2003); Age, dated; Age, dated standard deviation; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Calendar age, standard deviation; Carbon; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; KAL; Kasten corer; KC073; Laboratory code/label
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Hendry, Katharine R; Gong, Xun; Knorr, Gregor; Pike, Jennifer; Hall, Ian R (2016): Deglacial diatom production in the tropical North Atlantic driven by enhanced silicic acid supply. Earth and Planetary Science Letters, 438, 122-129, https://doi.org/10.1016/j.epsl.2016.01.016
    Publication Date: 2023-06-27
    Description: This data release contains stable silicon isotope data from sponge spicules isolated from sediment core RAPiD15-4P off Iceland, from 10 to 18 ka.
    Keywords: AGE; CD159; CD159-15; Charles Darwin; DEPTH, sediment/rock; PC; Piston corer; RAPiD-15-4P; South of Iceland; δ30Si, biogenic silica; δ30Si, error
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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