A late Quaternary bio‐ and climatostratigraphy for marine sediments in the north‐central part of the North Sea

BOREAS Harland, R., Gregory, Diane M., Hughes, M. J. & Wilkinson, I. P. 1978 06 01: A late Quaternary bio‐ and climatostratigraphy for marine sediments in the north‐central part of the North Sea. Boreas, Vol. 7, pp. 91–96. Oslo. ISSN 0300–9483. Micropalaeontological studies of three boreholes in...

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Bibliographic Details
Published in:Boreas
Main Authors: HARLAND, REX, GREGORY, DIANE M., HUGHES, MURRAY J., WILKINSON, IAN P.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1978
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Online Access:http://dx.doi.org/10.1111/j.1502-3885.1978.tb00267.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00267.x
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Summary:BOREAS Harland, R., Gregory, Diane M., Hughes, M. J. & Wilkinson, I. P. 1978 06 01: A late Quaternary bio‐ and climatostratigraphy for marine sediments in the north‐central part of the North Sea. Boreas, Vol. 7, pp. 91–96. Oslo. ISSN 0300–9483. Micropalaeontological studies of three boreholes in the north‐central North Sea have led to the erection of a bio‐ and climatostratigraphy for the area. Palaeoenvironmental interpretations have depended largely upon oceanographic concepts and changes in the micropalaeontological assemblages have been related to postulated alterations in water mass regimes. The biostratigraphy can then be utilized as a climatostratigraphy since such water mass changes are most probably linked to alterations in the circulation of the North Atlantic, and in particular to the positions of the climatically important North Atlantic Current and Polar Front. The North Sea sequences are compared to similar sections in Europe and related to the commonly accepted standard chronostratigraphy.