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Sediments in the Atlantic Corner seamounts: Control by topography,paleo-winds,and geochemically-detected modern bottom currents
Authors:Bonnie A McGregor  Peter R Betzer  Dale C Krause
Institution:1. Graduate School of Oceanography, University of Rhode Island, Kingston, R. I. U.S.A.;2. Marine Science Institute, University of South Florida, St. Petersburg, Fla. U.S.A.
Abstract:The topography in the Corner seamounts area in the western North Atlantic was studied to determine its relationship to the sedimentation pattern. The areas of anomalously thick sediment accumulation that are found on the north side of the seamounts are related to volcanic activity as well as paleocurrent and wind patterns. An irregular sediment surface has been formed by slump structures and actively eroding bottom currents, the latter as evidenced by high particulate iron concentrations in the bottom water.
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