Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation

Comparison of marine, lacustrine, and terrestrial records from twenty-four sites suggests the existence of a 'Younger Dryas'-type climate oscillation just prior to the Oxygen Isotope Stage 6/5e boundary. These records include results from biostratigraphic, pedostratigraphic, and speleothem...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Seidenkrantz, MS, Bornmalm, L, Johnsen, SJ, Knudsen, KL, Kuijpers, A, Lauritzen, SE, Leroy, SAG., Mergeai, I, Schweger, C, Vanvlietlanoe, B.
Other Authors: UCL
Format: Article in Journal/Newspaper
Language:English
Published: Pergamon-elsevier Science Ltd 1996
Subjects:
Online Access:http://hdl.handle.net/2078.1/47120
https://doi.org/10.1016/0277-3791(95)00086-0