Joint Program In Ocea~ography, Massa~usetts John D~lliman
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joint program in ocea~ography, massa~usetts john d~lliman-3MODERN SEDIMENTATION IN THE NORTHERN BARENTS SEA: INPUT, DISPERSAL, AND DEPOSITION OF SUSPENDED SEDIMENTS FROM GLACIAL MELTWATER by STEPHANIE LOUISE PFIRMAN Submitted to the Department of Earth and Planetary Sciences on August 3, 1984 in partial fulfillment of the requirements for the degree of Doctor of Philosophy ABSTRACT The modern depositional environment of the northern epicontinental Barents Sea varies from proximal to distal glaciomarine. The regional surface sediment distribution is controlled by erosion of shallow banks of the Pleistocene glaciated surface, with the fine material deposited in the deep basins.