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  • 1
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    PANGAEA
    In:  Supplement to: Moore, J A; Vecchione, M; Hartel, K E; Collette, B B; Galbraight, J K; Gibbons, R; Turnipseed, M; Southworth, M; Watkins, E (2001): Biodiversity of Bear Seamount, New England Seamount Chain: Results of Exploratory Trawling. Northwest Atlantic Fisheries Organization, Scientific Council Meeting - September 2001 (Deep-sea Fisheries Symposium - Oral) NAFO SCR Doc. 01/155, Serial No. N4549, 1-8, https://doi.org/10.2960/J.v31.a28
    Publication Date: 2023-11-14
    Description: Bear Seamount (39° 55'N, 67° 30'W) is an extinct undersea volcano located inside the U.S. Exclusive Economic Zone south of Georges Bank. The fauna associated with the seamount was little known until twenty trawl stations were made 2-7 December 2000, by the NOAA ship Delaware II. The objective of the cruise was to begin to document the biodiversity on and over the seamount, particularly of fishes, cephalopods, and crustaceans. Representatives of most species were preserved as vouchers and for subsequent definitive identification. Preliminary identifications indicate the capture of 115 fish species. Among these were a number of new fish records for the area or rare species, including Acromycter pertubator (Congridae), Alepocephalus bairdii (Alepocephalidae), Mirognathus normani (Alepocephalidae), Bathygadus favosus (Bathygadidae), Nezumia longebarbata (Macrouridae), Gaidropsarus argentatus (Phycidae), and Dibranchus tremendus (Ogcocephalidae). Only two fish species of potential commercial importance were encountered: Coryphaenoides rupestris and Macrourus berglax. Cephalopods comprised 26 species in 15 families, including one new distributional record and several rarelycollected species. The crustacean fauna was diverse with at least 46 species. Totals for other invertebrate species are pending laboratory identification, but number at least 113 species in 10 phyla. This includes a number of new distributional records and a new species of gorgonian.
    Keywords: 2754; ALV286; ALV-286; Alvin; AT281; AT281-17; AT281-19; Atlantis (1931); Balanus Seamount, Atlantic Ocean; Bear Seamount, Atlantic Ocean; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 308 (1984), S. 527-531 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] To check the fanning of transform fault directions, the Institute of Oceanographie Sciences organized a Gloria8 long-range sidescan sonar survey in autumn 1981 onboard MV Farnella. The survey covered the active sections of all major fracture zones (Oceanographer, Hay es, Atlantis, Kane and Fifteen ...
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 205 (1965), S. 688-689 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The preliminary results are listed in Table 1. Table 1 Velocity Thickness Depth 1,500 m/sec 40m 40m 1-85 km/sec 2-2 km 2-2km 3-0 km/sec 1-0 km 3-2 km 6-15 km/sec 26-5 km 30km 8-3 km/sec Velocity-depth profile at 54 40' N, 3 20' E. The ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 1 (1970), S. 46-60 
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract First conclusions of a study of the fault pattern in the North Atlantic ocean are briefly outlined. Correlation of fracture zones in deep ocean basins, even over short distances (30 miles) is difficult when using only topographic and seismic profiler data, and requires the additional criterion that the magnetic pattern is shifted along the fracture zones. This implies that each track must be paralleled by at least one more track at close distance to detect breaks in the magnetic pattern. Transform faults are regarded as complementary to the median rift, which, as a tension fault, should be normal to the direction of maximum strain according to laboratory experiments by Gramberg. Median rift segments and transform faults together form an orthogonal system approximating an originally irregular but continuous fissure. Mantle convection currents are thought to be the agents of continental drift. In view of the dimensions of convection cells, a direct coupling between ridges (or ridge segments) and the upwelling branch of a convection current seems impossible. Thus the known bifurcations of mid-ocean ridges in the Indian and in the Pacific Ocean may be interpreted as the result of a divergence of the horizontal branch of a convection cell or a divergence of the movements of crustal plates through collision of continents. Secondary fissures would lead to the development of secondary ridges that cannot be distinguished from primary ridges. In this concept mid-ocean ridges can partake in the horizontal movement by asymmetrical spreading. This might explain the disappearance of the East Pacific Rise under the North American continent. The resulting convection current system is simple: one upwelling and one downgoing current as two complementary helices winding round the earth. Ways are indicated to check several aspects of the proposed hypotheses.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 1 (1970), S. 104-107 
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 1 (1972), S. 361-361 
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 13 (1991), S. 81-103 
    ISSN: 1573-0581
    Keywords: Magnetic anomalies ; African plate sea floor spreading ; plate reconstructions
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This paper describes a compilation of magnetic data collected off West Africa during the period 1961–1988. The internal accuracy of the total data set was assessed using a crossover analysis and the cleaned profile data were gridded to produce, among other things, a colour display of the magnetic anomalies which is presented here. The magnetic anomalies were differentially reduced to the pole using a technique that takes into account variations in the directions of the geomagnetic field and of the magnetization over a study area. A brief description of the magnetic field and its relation to bathymetric features is given. Several sea floor spreading anomalies and fracture zones were identified from the magnetic data and a general flowline pattern of the region is presented.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 14 (1992), S. 163-163 
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-0581
    Keywords: Sea floor spreading ; North Atlantic ; Mesozoic magnetic anomalies ; plate kinematics ; fracture zones
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The data from a recent magnetic compilation by Verhoefet al. (1991) off west Africa were used in combination with data in the western Atlantic to review the Mesozoic plate kinematic evolution of the central North Atlantic. The magnetic profile data were analyzed to identify the M-series sea floor spreading anomalies on the African plate. Oceanic fracture zones were identified from magnetic anomalies and seismic and gravity measurements. The identified sea floor spreading anomalies on the African plate were combined with those on the North American plate to calculate reconstruction poles for this part of the central Atlantic. The total separation poles derived in this paper describe a smooth curve, suggesting that the motion of the pole through time was continuous. Although the new sea floor spreading history differs only slightly from the one presented by Klitgord and Schouten (1986), it predicts smoother flowlines. On the other hand, the sea floor spreading history as depicted by the flowlines for the eastern central Atlantic deviates substantially from that of Sundvik and Larson (1988). A revised spreading history is also presented for the Cretaceous Magnetic Quiet Zone, where large changes in spreading direction occurred, that can not be resolved when fitting magnetic isochrons only, but which are evident from fracture zone traces and directions of sea floor spreading topography.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 6 (1984), S. 383-394 
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The basement topography and the free-air gravity along two profiles in the central North Atlantic between 16° and 25° N, crossing a number of fracture zones, were divided in three wavelength intervals. Two-dimensional modelling shows that the short wavelength (〉50 km) gravity is well explained by uncompensated topography (mainly spreading topography). For the long wavelengths (〉200 km) there is no correlation of topography and gravity. In principle this topography is compensated. Residual anomalies comprise the Ridge effect as well as regional anomalies related to depth anomalies. The 50 to 200km band-pass filtered topography and gravity contain relevant information on fracture zones. Models require a base of the crust that parallels the topography rather than a form of regional compensation. For an explanation of this crustal model that has the appearance of ‘frozen in’ normal faults we have to consider the typical morphology as created in the transform domain. The geophysical processes that cause this morphology are still an object of study.
    Type of Medium: Electronic Resource
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