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Modern agglutinated Foraminifera from the Hovgård Ridge, Fram Strait, west of Spitsbergen: evidence for a deep bottom current

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Deep-water agglutinated foraminifera on the crest of the Hovgård Ridge, west of Spitsbergen, consist mostly of large tubular astrorhizids. At a boxcore station collected from the crest of Hovgård Ridge at a water depth of 1169 m, the sediment surface was covered with patches of large (1 mm diameter) tubular forms, belonging mostly to the species Astrorhiza crassatina Brady, with smaller numbers of Saccorhiza, Hyperammina, and Psammosiphonella. Non-tubular species consisted mainly of opportunistic forms, such as Psammosphaera and Reophax. The presence of large suspension-feeding tubular genera as well as opportunistic forms point to the presence of deep currents at this locality that are strong enough to disturb the benthic fauna. This is confirmed by data obtained from sediment echosounding, which exhibit lateral variation in relative sedimentation rates within the Pleistocene sedimentary drape covering the ridge, indicative of winnowing in a south-easterly direction.
Rocznik
Strony
309--320
Opis fizyczny
Bibliogr. 36 poz., rys., tab., wykr.
Twórcy
  • Earth Sciences Department, King Fahd University of Petroleum & Minerals, PO Box 701, Dhahran, 31261, Saudi Arabia
  • AGH University of Science & Technology, Faculty of Geology, Geophysics and Environmental Protection, Mickiewicza Ave 30, 30-059 Kraków, Poland
  • Department of Earth Sciences, University College London, Gower Street, London WCIE 6BT, U.K.
autor
  • Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Am Alten Hafen 26, 27568 Bremerhaven, Germany
Bibliografia
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  • 2. Aagaard, K., Darnall, C. & Greisman, P., 1973. Year-long current measurements in the Greenland-Spitsbergen Passage. Deep- Sea Research, 20: 743-746.
  • 3. Altenbach, A., Unsöld, G. & Walger, E., 1988. The hydrodynamic environment of Saccorhiza ramosa (Brady). Meyniana, 40: 119-132.
  • 4. Arndt, J. E., Niessen, F., Jokat, W. & Dorschel, B., 2014. Deep waler paleo-iceberg scouring on top of Hovgaard Ridge - Arctic Ocean. GeophysicalResearch Letters, 41: 5068-5074.
  • 5. Brady, H. B., 1884. Report on the foraminifera dredged by H.M.S. CHALLENGER during the years 1873-1876. In: Murray, J. (ed.), Reports of the scientific results of the voyage of the H.M.S. Challenger. Zoology, 9: 1-814.
  • 6. Cushman, J. A., 1948. Arclic Foraminifera. Contributions to the Cushman Laboratory for Foraminiferal Research Special Publication, 23: 79 pp + 8 pls.
  • 7. Eiken, O. & Hinz, K., 1993. Contourites in the Fram Strait. Sedimentary Geology, 82: 15-32.
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  • 10. Gooday, A. J., 1988. The genus Bathysiphon (Protista, Foraminiferida) in the NE Atlantic: revision of some species described by de Folin (1886). Journal of Natural History, 22: 71-93.
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  • 23. Kaminski, M. A., Silye, L. & Kender, S., 2009. Miocene deep-water agglutinated foraminifera from IODP Hole M0002a, Lomonosov Ridge: faunal constraints for the timing of the opening of the Fram Strait. Micropaleontology, 55: 117-135.
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  • 30. Schroder-Adams, C. J., Cole, F. E., Medioli, F. S., Mudie, P. J., Scott, D. B. & Dobbin, L., 1990. Recent Arctic shelf foraminifera: seasonally ice covered vs. perennially ice covered areas. Journal of Foraminiferal Research, 20: 8-36.
  • 31. Spielhagen, R., 2012. History of Atlantic water advection to the Arctic Ocean: review of 20 years of progress since the “Oden”-“Polarstern” Expedition ARCTIC 91. Polarforschung, 82: 19-36.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-7f44e72c-cee9-487d-9603-5082096026a9
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