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  • 1
    Publication Date: 2024-06-12
    Description: A new pyroclastic stratigraphy is presented for the island of Ischia, Italy, for the period ∼75–50 ka BP. The data indicate that this period bore witness to the largest eruptions recorded on the island and that it was considerably more volcanically active than previously thought. Numerous vents were probably active during this period. The deposits of at least 10 explosive phonolite to basaltictrachyandesite eruptions are described and interpreted. They record a diverse range of explosive volcanic activity including voluminous fountain-fed ignimbrite eruptions, fallout from sustained eruption columns, block-and-ash flows, and phreatomagmatic eruptions. Previously unknown eruptions have been recognised for the first time on the island. Several of the eruptions produced pyroclastic density currents that covered the whole island as well as the neighbouring island of Procida and parts of the mainland. The morphology of Ischia was significantly different to that seen today, with edifices to the south and west and a submerged depression in the centre. The largest volcanic event, the Monte Epomeo Green Tuff (MEGT) resulted in caldera collapse across all or part of the island. It is shown to comprise at least two thick intracaldera ignimbrite flowunits, separated by volcaniclastic sediments that were deposited during a pause in the eruption. Extracaldera deposits of the MEGT include a pumice fall deposit emplaced during the opening phases of the eruption, a widespread lithic lag breccia outcropping across much of Ischia and Procida, and a distal ignimbrite in south-west Campi Flegrei. During this period the style and magnitude of volcanism was dictated by the dynamics of a large differentiated magma chamber, which was partially destroyed during the MEGT eruption. This contrasts with the small-volume Holocene and historical effusive and explosive activity on Ischia, the timing and distribution of which has been controlled by the resurgence of the Monte Epomeo block. The new data contribute to a clearer understanding of the long-term volcanic and magmatic evolution of Ischia.
    Description: Published
    Description: 583-603
    Description: 3.5. Geologia e storia dei sistemi vulcanici
    Description: JCR Journal
    Description: reserved
    Keywords: Pyroclastic stratigraphy ; Explosive volcanism ; Caldera collapse ; Ischia ; Late Pleistocene ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
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    In:  Supplement to: Haas, Christian; Gerland, Sebastian; Eicken, Hajo; Miller, Heinz (1997): Comparison of sea-ice thickness measurements under summer and winter conditions in the Arctic using a small electromagnetic induction device. Geophysics, 62(3), 749-757, https://doi.org/10.1190/1.1444184
    Publication Date: 2024-06-12
    Description: Drillhole-determined sea-ice thickness was compared with values derived remotely using a portable small-offset loop-loop steady state electromagnetic (EM) induction device during expeditions to Fram Strait and the Siberian Arctic, under typical winter and summer conditions. Simple empirical transformation equations are derived to convert measured apparent conductivity into ice thickness. Despite the extreme seasonal differences in sea-ice properties as revealed by ice core analysis, the transformation equations vary little for winter and summer. Thus, the EM induction technique operated on the ice surface in the horizontal dipole mode yields accurate results within 5 to 10% of the drillhole determined thickness over level ice in both seasons. The robustness of the induction method with respect to seasonal extremes is attributed to the low salinity of brine or meltwater filling the extensive pore space in summer. Thus, the average bulk ice conductivity for summer multiyear sea ice derived according to Archie's law amounts to 23 mS/m compared to 3 mS/m for winter conditions. These mean conductivities cause only minor differences in the EM response, as is shown by means of 1-D modeling. However, under summer conditions the range of ice conductivities is wider. Along with the widespread occurrence of surface melt ponds and freshwater lenses underneath the ice, this causes greater scatter in the apparent conductivity/ice thickness relation. This can result in higher deviations between EM-derived and drillhole determined thicknesses in summer than in winter.
    Keywords: Arctic Ocean; Ark11_203p1; Ark11_205p1; Ark11_205p2; Ark11_206p1; Ark11_207p1; Ark11_209p1; Ark11_210p1; Ark11_216p1; Ark11_219p1; Ark11_219p3; Ark11_221p1; Ark11_228p1; Ark11_229p1; Ark11_230p1; Ark11_232p1; Ark11_232p2; Ark11_233p1; Ark11_234p1; Ark11_235p1; Ark11_236p1; Ark11_237p1; Ark11_237p2; Ark11_238p1; Ark11_239p1; Ark11_240p1; Ark11_241p1; Ark11_242p1; Ark11_243p1; Ark11_247p1; Ark12_207p1; Ark12_207p2; Ark12_208p1; Ark12_209p1; Ark12_210p1; Ark12_212p1; Ark12_212p2; Ark12_213p1; Ark12_214p1; Ark12_215p1; Ark12_216p1; Ark12_218p1; Ark12_219p1; Ark12_220p1; Ark12_221p1; Ark12_222p1; Ark12_223p1; Ark12_226p1; Ark12_227p1; Ark12_229p1; Ark12_230p1; Ark12_231p1; Ark12_232p1; Ark12_232p2; Ark12_232p3; Ark12_233p1; Ark12_234p1; Ark12_236p1; Ark12_236p2; Ark12_238p1; Ark12_239p1; Ark12_240p1; Ark12_240p2; Ark12_240p3; Ark12_240p4; Ark12_240p5; Ark12_240p6; Ark12_240p7; Ark12_242p1; Ark12_243p1; Ark12_246p1; Ark12_247p1; Ark12_249p1; Ark9_4_246p1; Ark9_4_251p1; Ark9_4_253p1; Ark9_4_254p1; Ark9_4_255p1; Ark9_4_256p1; Ark9_4_257p1; Ark9_4_258p1; Ark9_4_260p1; Ark9_4_261p1; Ark9_4_264p1; ARK-IX/4; ARK-XI/1; ARK-XII; AWI_SeaIce; East Siberian Sea; FEME; ICEM; Ice measurement; Kara/Laptev Sea/Transpolar Drift; Laptev Sea; Polarstern; PS27; PS36; PS41; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: application/zip, 83 datasets
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  • 3
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    In:  Supplement to: Heinz, Petra; Hemleben, Christoph (2006): Foraminiferal response to the Northeast Monsoon in the western and southern Arabian Sea. Marine Micropaleontology, 58(2), 103-113, https://doi.org/10.1016/j.marmicro.2005.10.001
    Publication Date: 2024-06-12
    Description: Sediments from the western and southern part of the Arabian Sea were collected periodically in the spring intermonsoon between March and May 1997 and additionally at the end of the Northeast Monsoon in February 1998. Assemblages of Rose Bengal stained, living deep-sea benthic foraminifera, their densities, vertical distribution pattern, and diversity were analysed after the Northeast Monsoon and short-time changes were recorded. In the western Arabian Sea, foraminiferal numbers increased steadily between March and the beginning of May, especially in the smaller size classes (30-63 µm, 63-125 µm). At the same time, the deepening of the foraminiferal living horizon, variable diversity and rapid variations between dominant foraminiferal communities were observed. We interpret these observations as the time-dependent response of benthic foraminifera to enhanced organic carbon fluxes during and after the Northeast Monsoon. In the southern Arabian Sea, constant low foraminiferal abundances during time, no distinctive change in the vertical distribution, reduced diversity, and more stable foraminiferal communities were noticed, which indicates no or little influence of the Northeast Monsoon to benthic foraminifera in this region.
    Keywords: 19#4; 2#2; 23/25; 24/03; 32; 4#2; 7/30; 7#4; Arabian Sea; BIGSET; BIGSET-1; BIGSET-2/JGOFS-IN-4; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; JGOFS-IN-1; JGOFS-IN-2; MUC; MultiCorer; SO117; SO117_MC464; SO117_MC468; SO117_MC469; SO118; SO118_MC-02; SO118_MC-04; SO119; SO119_MC501; SO129; SO129_MC-03; SO129_MC-09; SO129_MC-14; Sonne; Southern Arabian Sediment Trap; Western Arabian Sediment Trap; Western Arabian Sediment Trap-Kuppe; Western Arabian Sediment Trap Plain; Western Arabian Sediment Trap Top
    Type: Dataset
    Format: application/zip, 52 datasets
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  • 4
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    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark11_199508212035; ARK-XI/1; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; Determined from reflected laser signal strength; FEME; Freeboard; Ice coverage, yes=1/no=0; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS36; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 444924 data points
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  • 5
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    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark11_199508231005; ARK-XI/1; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; Determined from reflected laser signal strength; FEME; Freeboard; Ice coverage, yes=1/no=0; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS36; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 416946 data points
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  • 6
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark11_199508212054; ARK-XI/1; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; Determined from reflected laser signal strength; FEME; Freeboard; Ice coverage, yes=1/no=0; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS36; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 457696 data points
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  • 7
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    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark17_200108311036; ARK-XVII/2; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; FEME; Freeboard; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS59 AMORE; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 51184 data points
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  • 8
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark17_200108311050; ARK-XVII/2; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; FEME; Freeboard; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS59 AMORE; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 41837 data points
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  • 9
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: Arctic Ocean; Ark17_200108291325; ARK-XVII/2; AWI_SeaIce; Determined by helicopter-borne laser distance measurement; FEME; Freeboard; Laser distance meter, PS100EL, IBEO; POINT DISTANCE from start; Polarstern; PS100EL; PS59 AMORE; Remote Sensing of Sea Ice Properties; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 25668 data points
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  • 10
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: ANDEEP-SYSTCO; ANT-XXIV/2; Certainty of identification; Cetacean sightings; CT; DATE/TIME; LATITUDE; LONGITUDE; MAPS; Marine Mammal Perimeter Surveillance from RV Polarstern; Number of individuals; Polarstern; PS71/2-track; PS71 ANDEEP-SYSTCO SCACE; South Atlantic Ocean; Underway cruise track measurements; Visual description; Visual observation; WALOG; Whale species
    Type: Dataset
    Format: text/tab-separated-values, 123 data points
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