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Mediterranean Outflow Water changes in the Gulf of Cadiz during the Mid-Pleistocene Transition – The role of insolation
Voelker, A.H.L.; Jimenez-Espejo, F.; Bahr, A.; Acton, G.D.; Rebotin, A.; Salgueiro, E.; Röhl, U.; Escutia, C. (2014). Mediterranean Outflow Water changes in the Gulf of Cadiz during the Mid-Pleistocene Transition – The role of insolation, in: Van Rooij, D. et al. (Ed.) Book of Abstracts. 2nd Deep-Water Circulation Congress: The Contourite Log-book. Ghent, Belgium, 10-12 September 2014. VLIZ Special Publication, 69: pp. 29-30
In: Van Rooij, D.; Rüggeberg, A. (Ed.) (2014). Book of Abstracts. 2nd Deep-Water Circulation Congress: The Contourite Log-book. Ghent, Belgium, 10-12 September 2014. VLIZ Special Publication, 69. Ghent University, Department of Geology and Soil Science/Flanders Marine Institute (VLIZ): Oostende. xviii, 152 pp., meer
In: VLIZ Special Publication. Vlaams Instituut voor de Zee (VLIZ): Oostende. ISSN 1377-0950, meer
Beschikbaar in  Auteurs 
Documenttype: Samenvatting
Trefwoorden
    Insolation
    Sediments > Clastics > Contourites
    Marien/Kust
Author keywords
    IODP Exp. 339; Site U1387; Mediterranean Outflow Water;
Auteurs  Top 
  • Voelker, A.H.L.
  • Jimenez-Espejo, F.
  • Bahr, A.
  • Acton, G.D.
  • Rebotin, A.
  • Salgueiro, E.
  • Röhl, U.
  • Escutia, C.
Abstract
    This multi-proxy study of IODP Site U1387 (Faro Drift) aims to reconstruct the history of the surface water and the Mediterranean Outflow Water (MOW) during the interval from 630 to 1100ka, i.e. the Mid-Pleistocene Transition. Surface and MOW experienced orbital- and millennial-scale variations. MOW related proxies show a tight coupling to insolation with poor ventilation during insolation maxima and contourite layers being formed by a faster flowing MOW during insolation minima.
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