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Titel Orbital calibration of the late Campanian carbon isotope event in the North Sea
VerfasserIn Anastasios Perdiou, Nicolas Thibault, Kresten Anderskouv, Frans van Buchem, Govert Joan Arie Buijs, Christian J. Bjerrum
Konferenz EGU General Assembly 2016
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 18 (2016)
Datensatznummer 250121543
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2016-312.pdf
 
Zusammenfassung
A new record of carbon isotopes, nannofossil biostratigraphy, gamma-ray and Fe content variations is presented for the upper Campanian of the Adda-3 core, Danish Central Graben, North Sea. The studied interval provides a revision of previously assigned late Coniacian to early Santonian ages. New biostratigraphic data show a late Campanian age for the 60-m thick studied interval. The Late Campanian Event (LCE) is well-recorded by a 1.5‰ negative excursion in the bulk δ13C, along with two stepwise pre-excursion negative shifts (defining the pre-LCE). The amplitude of the LCE appears higher in the North Sea than in other areas as seen from the correlation to Germany, UK, and France. This correlation allows identification of a new 0.4‰ negative excursion (defined as the conica event). Fe and gamma-ray variations are used to calibrate the record with cyclostratigraphy. Fourteen 405 kyr cycles identified in the upper Campanian of Adda-3 can be correlated to North Germany. The compilation of previous results from North Germany and correlation to Adda-3 indicates that the Boreal upper Campanian spans a total of seventeen 405 cycles, i.e. 6.885 Myr. The duration of the LCE is estimated to be of ca. 1 Myr at Adda-3 and in North Germany.