Acta Geologica Polonica, Vol. 54 (2004), No. 4, pp. 639-656 20 years of event stratigraphy in NW Germany; advances and open questions FRANK WIESE1, CHRISTOPHER J. WOOD2 & ULRICH KAPLAN3 1Fachrichtung Paläontologie, Institut für Geologische Wissenschaften der FU Berlin, Malteserstr. 74-100, D-12249 Berlin, Germany. Email:
[email protected] 2Scops Geological Services Ltd., 31 Periton Lane, Minehead Somerset, TA24 8AQ, UK. Email:
[email protected] 1Eichenalle 141, D-33332 Gütersloh, Germany. Email:
[email protected] “The being determines consciousness” (Karl Marx) For Gundolf ABSTRACT: WIESE, F., WOOD, C.J. & KAPLAN, U. 2004. 20 years of event stratigraphy in NW Germany; advances and open ques- tions. Acta Geologica Polonica, 54 (4), 639-656. Warszawa. The application of event stratigraphy in the Cenomanian to Lower Coniacian (Upper Cretaceous) Plänerkalk Gruppe of northwestern Germany has advanced stratigraphic resolution considerably. For a short interval in the Upper Turonian, various genetically variable events (bioevents, tephroevents, stable isotope marker, eustatoevents) are reviewed and new data are partly added. In addition, the lateral litho and biofacies changes within individual events are discussed and provide a basis for a tentative high-resolution correlation between distal and proximal settings. The dense sequence of events permits a stratigraphic resolution of 50 – 100ky for some intervals. Beyond stratigraphic purposes, the alternation of fossil barren intervals with thin fossil beds still demands explanations. As taphonomic processes are considered to be play only a minor role, other explanations are required. It appears that trophic aspects and a calibra- tion of planktic and benthic faunal assemblages may result in a better understanding of this biosedimentary system and its faunal characteristics.