Abstract
An event stratigraphy for the Last Termination, based on the stratotype of the GRIP ice-core record, has been outlined for the North Atlantic region. It is suggested that such an approach to stratigraphic subdivision may o!er a more satisfactory alternative to conventional stratigraphical procedures for those parts of the recent Quaternary record that are characterised by rapid and/or short-term climatic #uctuations. ( 1999 Elsevier Science Ltd. All rights reserved.
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