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  • 1
    Publication Date: 2024-02-02
    Description: The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in the North. Mechanisms associated with interhemispheric heat transfer have been proposed to explain features of this event, but the response of marine biota and the carbon cycle are debated. The Southern Ocean is a key site of deep-water exchange with the atmosphere, hence deglacial changes in nutrient cycling, circulation, and productivity in this region may have global impact. Here we present a new perspective on the sequence of events in the deglacial Southern Ocean, that includes multi-faunal benthic assemblage (foraminifera and cold-water corals) and geochemical data (Ba/Ca, 14C, δ11B) from the Drake Passage. Our records feature anomalies during peak ACR conditions indicative of circulation, biogeochemistry, and regional ecosystem perturbations. Within this cold episode, peak abundances of thick-walled benthic foraminifera and cold-water corals are observed at shallow depths in the sub-Antarctic (~300 m), while coral populations at greater depths and further south diminished. Geochemical data indicate that habitat shifts were associated with enhanced primary productivity in the sub-Antarctic, a more stratified water column, and poorly oxygenated bottom water. These results are consistent with northward migration of primary production in response to Antarctic cooling and widespread biotic turnover across the Southern Ocean. We suggest that expanding sea ice, suppressed ventilation, and shifting centres of upwelling drove changes in planktic and benthic ecology, and were collectively instrumental in halting CO2 rise in the mid-deglaciation.
    Keywords: Alabaminella weddellensis; Angulogerina earlandi; Bolivina spp.; Bulimina aculeata; Bulimina sp.; Calendar age; Cassidulina carinata; Cassidulina crassa; Cibicidoides spp.; Core; DEPTH, sediment/rock; Epistominella exigua; Falkland Plateau, Southern Falkland Plateau (same site as GC526); Fissurina spp.; Foraminifera; Foraminifera, benthic agglutinated; Fursenkoina fusiformis; GC; GC528 CORE_NO 528; Globobulimina sp.; Gravity corer; Hoeglundina elegans; Hoeglundina sp.; James Clark Ross; JR20110128; JR244; JR244-GC528; Lagena spp.; Melonis barleeanus; Melonis spp.; Nonionella auris; Nonionella pulchella; Nonionella spp.; Number of taxa; Nuttallides umbonifera; Oridorsalis sp.; Oridorsalis umbonatus; Pullenia bulloides; Pullenia quinqueloba; Pyrgo spp.; Sphaeroidina bulloides; Total counts; Triloculina spp.; Uvigerina bifurcata; Uvigerina spp.; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 4995 data points
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  • 2
    Publication Date: 2024-02-02
    Description: The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in the North. Mechanisms associated with interhemispheric heat transfer have been proposed to explain features of this event, but the response of marine biota and the carbon cycle are debated. The Southern Ocean is a key site of deep-water exchange with the atmosphere, hence deglacial changes in nutrient cycling, circulation, and productivity in this region may have global impact. Here we present a new perspective on the sequence of events in the deglacial Southern Ocean, that includes multi-faunal benthic assemblage (foraminifera and cold-water corals) and geochemical data (Ba/Ca, 14C, δ11B) from the Drake Passage. Our records feature anomalies during peak ACR conditions indicative of circulation, biogeochemistry, and regional ecosystem perturbations. Within this cold episode, peak abundances of thick-walled benthic foraminifera and cold-water corals are observed at shallow depths in the sub-Antarctic (~300 m), while coral populations at greater depths and further south diminished. Geochemical data indicate that habitat shifts were associated with enhanced primary productivity in the sub-Antarctic, a more stratified water column, and poorly oxygenated bottom water. These results are consistent with northward migration of primary production in response to Antarctic cooling and widespread biotic turnover across the Southern Ocean. We suggest that expanding sea ice, suppressed ventilation, and shifting centres of upwelling drove changes in planktic and benthic ecology, and were collectively instrumental in halting CO2 rise in the mid-deglaciation.
    Keywords: AGE; Age, error; Benthic foraminifera; circulation; cold-water corals; DH117; DH40; DH43; DH74; DH75; DR23; DR27; DR34; DR35; DR38; DR40; Drake Passage; Dredge; DRG; Elevation of event; Event label; Genus; Latitude of event; Location; Method comment; Nathaniel B. Palmer; NBP0805; NBP0805-DR22; NBP0805-DR23; NBP0805-DR27; NBP0805-DR34; NBP0805-DR35; NBP0805-DR36; NBP0805-DR38; NBP0805-DR39; NBP0805-DR40; NBP0805-TB04; NBP0805-TB04a; NBP1103; NBP1103-DH07; NBP1103-DH09; NBP1103-DH11; NBP1103-DH112; NBP1103-DH113; NBP1103-DH115; NBP1103-DH117; NBP1103-DH120; NBP1103-DH128; NBP1103-DH129; NBP1103-DH134; NBP1103-DH138; NBP1103-DH14; NBP1103-DH140; NBP1103-DH141; NBP1103-DH143; NBP1103-DH15; NBP1103-DH16; NBP1103-DH19; NBP1103-DH22; NBP1103-DH24; NBP1103-DH36; NBP1103-DH37; NBP1103-DH38; NBP1103-DH40; NBP1103-DH43; NBP1103-DH74; NBP1103-DH75; NBP1103-DH87; NBP1103-DH88; NBP1103-DH91; NBP1103-DH95; NBP1103-DH96; NBP1103-DH97; NBP1103-TB01; NBP1103-TB02; NBP1103-TB10; NBP1103-TO104; pH; productivity; Reference/source; Sample ID; Scotia Sea; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 8524 data points
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  • 3
    Publication Date: 2024-02-02
    Description: The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in the North. Mechanisms associated with interhemispheric heat transfer have been proposed to explain features of this event, but the response of marine biota and the carbon cycle are debated. The Southern Ocean is a key site of deep-water exchange with the atmosphere, hence deglacial changes in nutrient cycling, circulation, and productivity in this region may have global impact. Here we present a new perspective on the sequence of events in the deglacial Southern Ocean, that includes multi-faunal benthic assemblage (foraminifera and cold-water corals) and geochemical data (Ba/Ca, 14C, δ11B) from the Drake Passage. Our records feature anomalies during peak ACR conditions indicative of circulation, biogeochemistry, and regional ecosystem perturbations. Within this cold episode, peak abundances of thick-walled benthic foraminifera and cold-water corals are observed at shallow depths in the sub-Antarctic (~300 m), while coral populations at greater depths and further south diminished. Geochemical data indicate that habitat shifts were associated with enhanced primary productivity in the sub-Antarctic, a more stratified water column, and poorly oxygenated bottom water. These results are consistent with northward migration of primary production in response to Antarctic cooling and widespread biotic turnover across the Southern Ocean. We suggest that expanding sea ice, suppressed ventilation, and shifting centres of upwelling drove changes in planktic and benthic ecology, and were collectively instrumental in halting CO2 rise in the mid-deglaciation.
    Keywords: AGE; Age, uncertainty; Barium/Calcium ratio; Benthic foraminifera; circulation; cold-water corals; Comment; Depth, bathymetric; DH117; DH74; DH75; DR27; DR34; DR35; DR38; DR40; Drake Passage; Dredge; DRG; Elevation of event; Event label; Genus; Latitude of event; Longitude of event; Nathaniel B. Palmer; NBP0805; NBP0805-DR27; NBP0805-DR34; NBP0805-DR35; NBP0805-DR36; NBP0805-DR38; NBP0805-DR40; NBP0805-TB04; NBP1103; NBP1103-DH07; NBP1103-DH11; NBP1103-DH112; NBP1103-DH113; NBP1103-DH117; NBP1103-DH120; NBP1103-DH14; NBP1103-DH15; NBP1103-DH16; NBP1103-DH19; NBP1103-DH74; NBP1103-DH75; pH; productivity; Reference/source; Sample ID; Site; South Pacific Ocean; δ11B, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 1741 data points
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  • 4
    ISSN: 1662-9752
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Journal of metastable and nanocrystalline materials Vol. 23 (Jan. 2005), p. 15-18 
    ISSN: 1422-6375
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Nano-scale Gd2O3:Eu phosphor powders were synthesized by combustion method. In this process, the grain sizes of nano-scale Gd2O3:Eu were controlled by changing the amount of citric acid. Compared with micro-scale powders obtained from co-precipitation process, XRD revealed that the lattice parameter of nano-scale powders Gd2O3:Eu decreased. Further detailed study show that the luminescent properties were related to the grain size of nano Gd2O3:Eu powders under UV excitation
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Advanced materials research Vol. 15-17 (Feb. 2006), p. 246-250 
    ISSN: 1662-8985
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Commercial Y2O3 powders were subjected to high energy ball milling in a planetaryball mill using high purity alumina balls and vial. The refined Y2O3 power ,withcommercial high-purity Al2O3, Cr2O3 and Yb2O3 powders, were used as rawmaterials. Transparent ytterbium and chromium codoped yttrium aluminum garnet(Yb,Cr:YAG) ceramics were fabricated by a solid-state reaction method. TheYb,Cr:YAG ceramics exhibit a pore free structure and the average grain size is about10 micron. The strong absorptions at 940 and 968 nm of Yb3+ are suitable for InGaAsdiode laser pumping, and there is an absorption band at 1030 nm, which is suitable forpassive Q-switch laser output at 1030 nm. Transparent Yb,Cr:YAG ceramics may be apotential material for compact, efficient, high-stability diode-laser-pumped passiveQ-switched solid-state lasers
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Materials science forum Vol. 561-565 (Oct. 2007), p. 2261-2264 
    ISSN: 1662-9752
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Laser shock peening (LSP) is an innovative surface treatment technique for metal alloys,with the great improvement of their fatigue, corrosion and wear resistance performance. Finiteelement method has been widely applied to simulate the LSP to provide the theoretically predictiveassessment and optimally parametric design. In the current work, 3-D numerical modellingapproaches, combining the explicit dynamic analysis, static equilibrium analysis algorithms anddifferent plasticity models for the high strain rate exceeding 106s-1, are further developed. To verifythe proposed methods, 3-D static and dynamic FEA of AA7075-T7351 rods subject to two-sidedlaser shock peening are performed using the FEA package–ABAQUS. The dynamic and residualstress fields, shock wave propagation and surface deformation of the treated metal from differentmaterial modelling approaches have a good agreement
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Key engineering materials Vol. 403 (Dec. 2008), p. 115-116 
    ISSN: 1013-9826
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: A considerable test was made to figure out the effects of temperature and sliding conditions on the wear properties of the translucent Dy--Sialon. The friction coefficient was 0.54 at RT, 0.26 at 100 oC, and 0.81 at 600 oC respectively under an applied load of 5N. The wear rate was 6.91×10-15 at RT and 1.0×10-15 at 100 oC for the same Dy--Sialon sample. Obviously Dy-Sialon shows an excellent wear resistance under a suitable sliding condition, a load of 5N and at 100 oC. This appears attractive and important for Dy-Sialon ceramics to be used as a type of special wear resistant materials, with an optical translucence
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Key engineering materials Vol. 373-374 (Mar. 2008), p. 580-584 
    ISSN: 1013-9826
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: In the present work, surface-coated Cu nanoparticles with FCC structure and an averagesize of 40 nm were prepared by reducing reaction and surface modification technique. Themorphology and phase structure of the nano-copper were characterized by transmission electronmicroscope (TEM). The ball-on-disc tester and ring-on-block tester were performed to study thetribological properties of surface-coated Cu nanoparticles as oil additive. The tests were carried outunder the lubrication of 50CC oil alone and oil containing surface-coated nano-copper additives. Themorphologies and elementary distributions of the worn surfaces were analyzed by scanning electronmicroscope (SEM) and energy dispersive spectrometry (EDS), respectively. Results indicate thatsurface-coated nano-copper additives can significantly improve the wear resistance and load-carryingabilities of 50CC oil, as well as reduce friction coefficient. A soft copper protective film is formed onthe worn surface lubricated with oil containing nano-copper additives, which separates the wornsurfaces, avoids their direct contact and reduces friction and adhesive wear. Besides, the grooves andsmall valleys on the worn surfaces are found to be partly filled and repaired by nano-copper, as makesthe worn surface repaired and smoother
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Key engineering materials Vol. 368-372 (Feb. 2008), p. 450-452 
    ISSN: 1013-9826
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: AlON with a composition of Al23O27N5 was prepared by hot pressing at temperatures lowerthan 1900 °C. The microstructures and final properties, including both mechanical properties and opticalproperties, of the sintered specimens were studied. The results showed that sintering temperature had agreat influence on the densification of specimens and could lead to very different properties, especiallythe optical transmittance and the maximum infrared transmission
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