Studying Past Deep-ocean Circulation and the Paleoclimate Record in the Gulf of Cadiz.

Mulder, L.P., Lecroart, T. P,, Voisset, M., Schönfeld, Joachim, Le Drezen, E., Gonthier, E., Hanquiez, V., Zahn, R., Faugeres, J.-C. and Hernandez-Molina, F. J. and CADISAR scientific team, IMAGES V-GINNA scientific team (2002) Studying Past Deep-ocean Circulation and the Paleoclimate Record in the Gulf of Cadiz. Open Access Eos, Transactions American Geophysical Union, 83 (43). pp. 481-488. DOI 10.1029/2002EO000337.

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Abstract

Deep marine currents are strongly influenced by climatic changes. They also deposit, rework, and sort sediment, and can generate kilometer-scale sedimentary bodies (drifts). These drifts are made of thoroughly bioturbated, stacked sedimentary sequences called contourites [Gonthier et al., 1984]. As a consequence, change in the direction or intensity of currents can be recorded in the sediments

Document Type: Article
Refereed: No
Open Access Journal?: No
Publisher: AGU (American Geophysical Union)
Date Deposited: 19 Feb 2008 14:46
Last Modified: 10 Feb 2017 14:00
URI: https://oceanrep.geomar.de/id/eprint/3907

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