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  • 1
    Monograph available for loan
    Monograph available for loan
    [Waterford, ME] : McIntire Publishing Services
    Call number: IASS 17.91279
    Type of Medium: Monograph available for loan
    Pages: xx, 172 Seiten , Illustrationen , 26 cm
    Edition: 5th edition
    ISBN: 0996205454 , 9780996205450
    Language: English
    Branch Library: IASS Library
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  • 2
    Call number: 9/M 07.0421(344)
    In: Geological Society special publication
    Description / Table of Contents: Fjords are glacially over-deepened, semi-enclosed marine basins, but are often neglected as a sedimentary realm. They represent the transition from the terrestrial to the marine environment and as such have the potential to preserve evidence of environmental change. Typically most fjords have been glaciated a number of times and some high-latitude fjords still possess a resident glacier. The stratigraphic record in fjords largely preserves a glacial deglacial cycle of deposition. Sheltered water and high sedimentation rates potentially make fjords ideal depositional environments for preserving continuous records of climate and environmental change with high temporal resolution. Fjords are also referred to as miniature oceans providing the unique opportunity to study marine processes in great detail. With predictions of warming climates, changing ocean circulation and rising sea levels, this volume is a timely look at these environmentally sensitive coastlines.
    Type of Medium: Monograph available for loan
    Pages: VI, 380 S. : Ill., graph. Darst., Kt.
    ISBN: 9781862393127
    Series Statement: Geological Society special publication 344
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Description / Table of Contents: Fjords are glacially over-deepened, semi-enclosed marine basins, but are often neglected as a sedimentary realm. They represent the transition from the terrestrial to the marine environment and as such have the potential to preserve evidence of environmental change. Typically most fjords have been glaciated a number of times and some high-latitude fjords still possess a resident glacier. The stratigraphic record in fjords largely preserves a glacial–deglacial cycle of deposition. Sheltered water and high sedimentation rates potentially make fjords ideal depositional environments for preserving continuous records of climate and environmental change with high temporal resolution. Fjords are also referred to as miniature oceans providing the unique opportunity to study marine processes in great detail. With predictions of warming climates, changing ocean circulation and rising sea levels, this volume is a timely look at these environmentally sensitive coastlines.
    Pages: Online-Ressource (VII, 380 Seiten)
    ISBN: 9781862393127
    Language: English
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  • 4
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    PANGAEA
    In:  Supplement to: Howe, John; Woolfe, Ken; Fielding, Christopher R (1998): Lower Miocene glacimarine gravity flows, Cape Roberts drillhole-1, Ross Sea, Antarctica. Terra Antartica, 5(3), 393-399, hdl:10013/epic.28328.d001
    Publication Date: 2023-06-27
    Description: Nineteen samples of the Cape Roberts-1 drillcore were taken from Miocene- age deposits, from 90.25 – 146.50 metres below seafloor (mbsf) for thin section and laser grain-size analysis. Using the grain-size distribution, detailed core logging, X-radiography and thin-section analysis of microstructures, coupled with a statistical grouping of the grain-size data, three main styles of gravity-flow sedimentation were revealed. Thin (centimetre-scale) muddy debris-flow deposits are the most common and are possibly tirggered by debris rain-out from sea-ice These deposits are characterised by very poorly sorted, faintly laminated muddy sandstones with coarse granules toward their base. Contacts are gradational to sharp. Variations on this style of mass-wasting deposit are rhythmically stacked sequences of pebbly-coarse sandstones representing successive thin debris-flow events. These suggest very high sedimentation rates on an unstable slope in a shallow-water proximal glacimarine environment. Sandy-silty turbidites appear more common in the lower sections of the core, below approximately 141.00 mbsf, although they occur occasionally with the debris flow deposits The turbidites are characterised by inversely to normally graded, well-laminated siltstones with occasional lonestones, and represent a more distal shallow-water glacimarine environment.
    Keywords: 16 km ENE Cape Roberts; Cape Roberts Project; Comment; Core wireline system; CRP; CRP-1; CWS; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Interpretation; Lithologic unit/sequence; Lithology/composition/facies; off Cape Roberts, Ross Sea, Antarctica; Sampling/drilling ice
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: Area/locality; Bioturbation; Burrows; Depth, bottom/max; Description; Grain size description; Mounds; Number of stations; Occurrence; Sediment type; Station label; Surface description; Tubes
    Type: Dataset
    Format: text/tab-separated-values, 270 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Agassiz Trawl; AGT; ANT-XIX/3; ANT-XIX/4; ANT-XXII/3; Date/Time of event; Date/Time of event 2; EBS; Epibenthic sledge; Event label; Expected number of species; Haul length; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; MOOR; Mooring; Polarstern; PS61/041-3; PS61/042-2; PS61/043-8; PS61/046-7; PS61/099-4; PS61/105-7; PS61/114-4; PS61/129-2; PS61/131-3; PS61/132-2; PS61/133-3; PS61/134-3; PS61/135-4; PS61/136-4; PS61/137-4; PS61/138-6; PS61/139-6; PS61/140-8; PS61/141-10; PS61/142-6; PS61/143-1; PS61 ANDEEP 1; PS61 ANDEEP 2; PS67/016-10; PS67/021-7; PS67/059-5; PS67/074-6; PS67/078-9; PS67/080-9; PS67/081-8; PS67/088-8; PS67/094-14; PS67/102-3; PS67/110-8; PS67/121-10; PS67/133-2; PS67/142-5; PS67/150-6; PS67/151-7; PS67/152-6; PS67/153-7; PS67/154-9; PS67 ANDEEP 3; Sample elevation; Scotia Sea, southwest Atlantic; South Atlantic Ocean; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 7
    Publication Date: 2023-06-27
    Description: Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed uncomplicated by ACC axis migration. We outline Holocene and Last Glacial Maximum (LGM) current-controlled sedimentation using data from 3.5-kHz profiles, cores and current meter moorings. Geophysical surveys show areas of erosion and deposition controlled by Neogene basement topography. Deposition occurs in mounded sediment drifts or flatter areas, where 500-1000 m of sediment overlies acoustic basement. 3.5-kHz profiles show parallel, continuous sub-bottom reflectors with highest sedimentation rates in the centre of the drifts, and reflectors converging towards marginal zones of non-deposition. Locally, on the flanks of continental blocks (e.g. South Georgia), downslope processes are dominant. The absence of mudwaves on the sediment drifts may result from the unsteadiness of ACC flow. A core transect from the ACC axis south to the boundary with the Weddell Gyre shows a southward decrease in biogenic content, controlled by the Polar Front and the spring sea-ice edge. Both these features lay farther north at LGM. The cores have been dated by relative abundance of the radiolarian Cycladophora davisiana, and by changes in the biogenic Ba content, a palaeoproductivity indicator. Sedimentation rates range from 3 to 17 cm/ka. The grain size of Holocene sediments shows a coarsening trend from south to north, consistent with strongest bottom-current flow near the ACC axis, though interpretation is complicated by the presence of biogenic grains. Year-long current meter records indicate mean speeds from 7 cm/s in the south to 12 cm/s in the north, with benthic storm frequency increasing northwards. LGM sediments are predominantly terrigenous and show a clearer northward-coarsening trend, with well-sorted silts in the northern Scotia Sea. Assuming a constant terrigenous source, this implies stronger ACC flow at the LGM, contrasting with weaker Weddell Gyre flow deduced from earlier work.
    Keywords: Calculated from radiolarians; Drake Passage; Event label; GC; GC027; GC037; Gravity corer; KAL; Kasten corer; KC064; KC081; KC083; PC; PC029; PC031; PC063; PC077; PC078; PC079; Piston corer; Sedimentation rate; TC; TC032; Trigger corer
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Brandt, Angelika; Gooday, Andrew J; Brandão, Simone N; Brix, Saskia; Brökeland, Wiebke; Cedhagen, Tomas; Choudhury, Madhumita; Cornelius, Nils; Danis, Bruno; De Mesel, Ilse; Diaz, Robert; Gillan, David C; Ebbe, Brigitte; Howe, John; Janussen, Dorte; Kaiser, Stefanie; Linse, Katrin; Malyutina, Marina; Pawlowski, Jan; Raupach, Michael R; Vanreusel, Ann (2007): First insights into the biodiversity and biogeography of the Southern Ocean deep sea. Nature, 447(7142), 307-311, https://doi.org/10.1038/nature05827
    Publication Date: 2023-10-28
    Description: Shallow marine benthic communities around Antarctica show high levels of endemism, gigantism, slow growth, longevity and late maturity, as well as adaptive radiations that have generated considerable biodiversity in some taxa1. The deeper parts of the Southern Ocean exhibit some unique environmental features, including a very deep continental shelf2 and a weakly stratified water column, and are the source for much of the deep water in the world ocean. These features suggest that deep-sea faunas around the Antarctic may be related both to adjacent shelf communities and to those in other oceans. Unlike shallow-water Antarctic benthic communities, however, little is known about life in this vast deep-sea region2, 3. Here, we report new data from recent sampling expeditions in the deep Weddell Sea and adjacent areas (748-6,348 m water depth) that reveal high levels of new biodiversity; for example, 674 isopods species, of which 585 were new to science. Bathymetric and biogeographic trends varied between taxa. In groups such as the isopods and polychaetes, slope assemblages included species that have invaded from the shelf. In other taxa, the shelf and slope assemblages were more distinct. Abyssal faunas tended to have stronger links to other oceans, particularly the Atlantic, but mainly in taxa with good dispersal capabilities, such as the Foraminifera. The isopods, ostracods and nematodes, which are poor dispersers, include many species currently known only from the Southern Ocean. Our findings challenge suggestions that deep-sea diversity is depressed in the Southern Ocean and provide a basis for exploring the evolutionary significance of the varied biogeographic patterns observed in this remote environment.
    Keywords: AWI; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Fielding, Christopher R; Baker, Julian C; Woolfe, Ken; Howe, John; Lavelle, Mark (1998): Reassessment of the Miocene-Quaternary boundary in CRP-1, Cape Roberts Project, Antarctica. Terra Antartica, 5(3), 425-426, hdl:10013/epic.28334.d001
    Publication Date: 2023-07-10
    Description: During the course of the 1997 drilling campaign, lithostratigraphic boundaries were assigned to the CRP-l core on the basis of perceived changes in lithology. The geologically most important boundary in the core, between the Miocene and overlying Quaternary sections, was placed at 43.55 mbsf. This horizon was described in the core logs (Cape Roberts Science Team, 1998) as a contact between muddy, finegrained sandstone (which were assigned a Lower Miocene age based on diatom biostratigsaphy) and overlying diamictons containing Quaternary diatoms. This boundary is a major unconformity, recognisable on seismic reflection records. As such, it has considerable significance in the ongoing scientific analysis of the drillcore. During a re-examination of the core, focusing on the archive half held at the Antarctic Geology Research Facility of the Florida State University at Tallahassee; the authors noted that the core across the published boundary (43.55 mbsf) did not show any lithological change, but logged a sharp contact between dark olive grey, muddy sandstone and overlying diamicton at 43.15 mbsf (Fig. l). We suggest, therefore, that the core log in appendix l of Cape Roberts Science Team (1998) is misleading over this interval. In order to test the veracity of the suggested boundary revision, a series of thin-sections was examined and point-counted for framework grain abundances.
    Keywords: 16 km ENE Cape Roberts; Calcite; Cape Roberts Project; Chert; Claystone; Core wireline system; CRP; CRP-1; CWS; DEPTH, sediment/rock; Epoch; Grain size, mean radius; Kalifeldspar; Micrite; off Cape Roberts, Ross Sea, Antarctica; Opaque minerals; Plagioclase; Porosity; Pyroxene; Quartz; Sampling/drilling ice; Sorting description; Thin section analysis/measurements; Volcanic glass; Volcanite
    Type: Dataset
    Format: text/tab-separated-values, 75 data points
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  • 10
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Journal of the American Chemical Society 57 (1935), S. 1262-1265 
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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