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  • PANGAEA  (437)
  • Springer  (4)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 9 (1989), S. 135-144 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In the deepest parts of Bute and Knight Inlets, British Columbia, unusual blocky mounds of sediment rise abruptly from the otherwise smooth sea floor. The mounds (up to 28 m high, 80 m wide, and 150 m long) display bioturbated surfaces with transverse fractures and elongate depressions. The origin of the mounds and sediment blocks, which contrast with the otherwise flat-lying fjord-bottom strata, remains unknown. Two mechanisms for their formation are considered: (1) subsidence associated with earthquake-induced liquefaction; and (2) uplift driven by the growth of localized gas hydrates in the near-surface sediments.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 2 (1982), S. 117-122 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A submarine sediment instability event (landslide) occurred at Kitimat, British Columbia, in 1975. Recent high-resolution surveys provide details of the resulting seafloor morphology. The effects of the slide include modification of the fjord head delta-front slopes, transport of delta sediments into deep water and mixing with deep water, fjord bottom clays. Distinctive features include the results of shallow rotational sliding, tearing and shearing, compressional folding and long distance block gliding at the downslope slide terminus.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 14 (1994), S. 238-243 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The frequency of turbidity currents in Bute Inlet and Knight Inlet (British Columbia, Canada) was monitored. A prototype instrument (turbidity event detector) was deployed adjacent to prominent incised sea-floor channels. Approximately 25–30 turbidity currents occur annually. They appear closely correlated to periods of higher river discharge into the heads of the fjords. Two peaks in both discharge and turbidity current fequency occur, one in response to snow melt in late June–early July, the other to glacier melt in August. Virtually no turbidity currents were observed in winter. River mouth bars, channel deposits, and other deltaic sediments build up during lower discharge periods and are swept onto the steep delta front and into subaqueous channels, along with bedload, during floods.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 5 (1986), S. 217-224 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A high-resolution acoustic survey over a fjord side fan delta revealed distinctive bottom features resulting from slope instability processes. Delta-front chutes occurring on slopes of l3° are partially filled with radiating splays of coarse-grained sediment, apparently transported downslope by coarse-grained debris flows that originated on the subaerial slopes above the fan. Arcuate scarp patterns represent shallow successive, rotational slides, with numcrous small displacements of individual blocks and slabs of sediment. Blocky, ridged depositional areas occur at the base of the fan delta, but there is no evidence of long-distance mass movement farther downfjord.
    Type of Medium: Electronic Resource
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Bornhold, Brian D (1983): Ice-rafted debris in sediments from Leg 71, Southwest Atlantic Ocean. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 307-316, https://doi.org/10.2973/dsdp.proc.71.110.1983
    Publication Date: 2023-06-27
    Description: The surficial few meters of sediment at Sites 511 and 512 on Maurice Ewing Bank consist of a lag deposit of icerafted sands and gravels ranging from lower Pliocene to Quaternary in age. The sediments contain up to 62% angular to subangular gravel of mixed lithology. Significant volumes of sand- and gravel-sized ice-rafted detritus (IRD) first reached the Falkland (Malvinas) Plateau and southeasternmost Argentine Basin in the late Miocene (6.9 Ma) in response to the rapid buildup and grounding of the ice sheet in West Antarctica. IRD accumulation rates remained relatively low until 4.15 Ma, after which they increased markedly. Peaks of IRD accumulation at Sites 513 and 514 can, in most instances, be correlated directly with colder climates in Antarctica and southern Patagonia.
    Keywords: 71-513; 71-513A; 71-514; Counting 〉250 µm fraction; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Feldspar; Glomar Challenger; Identification; Latitude of event; Leg71; Longitude of event; Minerals; Quartz; Rock fragments; Sample code/label; South Atlantic; South Atlantic/FLANK
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Bornhold, Brian D (1983): Appendix I. Detailed textural analyses of Miocene to Quaternary sediments, Leg 71. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 1183-1184, https://doi.org/10.2973/dsdp.proc.71.app1.1983
    Publication Date: 2023-06-27
    Description: In conjunction with a study of ice-rafted detritus (IRD), textural analyses were carried out on Miocene to Quaternary sediments at Sites 511, 512, 513, and 514. Grain-size statistics were computed for the 〈62.5 µm fraction in order to identify changes in current velocity; the sand fraction was omitted from these determinations because it consists primarily of ice-raft and biogenic components. The contributions by terrigenous sediment in the 62.5-250 µm and the 〉250 µm fractions were determined.
    Keywords: 71-511; 71-512; 71-513; 71-513A; 71-514; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Grain size, mean; Latitude of event; Leg71; Longitude of event; Sample code/label; Sand; see reference(s); Silt; Size fraction 〈 0.002 mm, clay; Size fraction 〉 0.250 mm; Size fraction 0.250-0.0625 mm; Skewness; Sorting in phi; South Atlantic; South Atlantic/BANK; South Atlantic/FLANK; South Atlantic/PLATEAU
    Type: Dataset
    Format: text/tab-separated-values, 2182 data points
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  • 7
    Publication Date: 2023-11-25
    Keywords: AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; DEPTH, sediment/rock; GEOMAR; Globigerina bulloides, δ13C; Globigerina bulloides, δ18O; Gyroidinoides spp., δ13C; Gyroidinoides spp., δ18O; Helmholtz Centre for Ocean Research Kiel; Isotope ratio mass spectrometry; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; North Pacific; PAR87A-02; PC; Piston corer; Uvigerina spp., δ13C; Uvigerina spp., δ18O
    Type: Dataset
    Format: text/tab-separated-values, 262 data points
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  • 8
    Publication Date: 2023-11-25
    Keywords: AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; DEPTH, sediment/rock; GEOMAR; Globigerina bulloides, δ13C; Globigerina bulloides, δ18O; Gyroidinoides spp., δ13C; Gyroidinoides spp., δ18O; Helmholtz Centre for Ocean Research Kiel; Isotope ratio mass spectrometry; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; North Pacific; PAR87A-10; PC; Piston corer; Uvigerina spp., δ13C; Uvigerina spp., δ18O
    Type: Dataset
    Format: text/tab-separated-values, 204 data points
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  • 9
    Publication Date: 2023-11-25
    Keywords: Age, 14C AMS; Age, 14C milieu/reservoir corrected; Age, calibrated; Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, dated material; DEPTH, sediment/rock; GEOMAR; Helmholtz Centre for Ocean Research Kiel; North Pacific; PAR87A-10; PC; Piston corer
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 10
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    Unknown
    PANGAEA
    In:  Supplement to: Zahn, Rainer; Pedersen, Thomas F; Bornhold, Brian D; Mix, Alan C (1991): Water mass conversion in the glacial subarctic Pacific (54°N, 148°W): physical constraints and the benthic-planktonic stable isotope record. Paleoceanography, 6(5), 543-560, https://doi.org/10.1029/91PA01327
    Publication Date: 2023-11-25
    Description: Benthic (Uvigerina spp., Cibicidoides spp., Gyroidinoides spp.) and planktonic (N. pachyderma sinistral, G. bulloides) stable isotope records from three core sites in the central Gulf of Alaska are used to infer mixed-layer and deepwater properties of the late glacial Subarctic Pacific. Glacial-interglacial amplitudes of the planktonic delta18O records are 1.1-1.3 per mil, less than half the amplitude observed at core sites at similar latitudes in the North Atlantic; these data imply that a strong, negative deltaw anomaly existed in the glacial Subarctic mixed layer during the summer, which points to a much stronger low-salinity anomaly than exists today. If true, the upper water column in the North Pacific would have been statically more stable than today, thus suppressing convection even more efficiently. This scenario is further supported by vertical (i.e., planktic versus benthic) delta18O and delta13C gradients of 〉1 per mil, which suggest that a thermohaline link between Pacific deep waters and the Subarctic Pacific mixed layer did not exist during the late glacial. Epibenthic delta13C in the Subarctic Pacific is more negative than at tropical-subtropical Pacific sites but similar to that recorded at Southern Ocean sites, suggesting ventilation of the deep central Pacific from mid-latitude sources, e.g., from the Sea of Japan and Sea of Okhotsk. Still, convection to intermediate depths could have occurred in the Subarctic during the winter months when heat loss to the atmosphere, sea ice formation, and wind-driven upwelling of saline deep waters would have been most intense. This would be beyond the grasp of our planktonic records which only document mixed-layer temperature-salinity fields extant during the warmer seasons. Also we do not have benthic isotope records from true intermediate water depths of the Subarctic Pacific.
    Keywords: GEOMAR; Helmholtz Centre for Ocean Research Kiel; North Pacific; PAR87A-01; PAR87A-02; PAR87A-10; PC; Piston corer
    Type: Dataset
    Format: application/zip, 4 datasets
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