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Download fileGeochemical and radiogenic isotope records of the Weissert Event in south Tethyan sediments
journal contribution
posted on 2022-12-06, 12:01 authored by M. Shmeit, C. Chauvel, F. Giraud, E. Jaillard, S. Reboulet, M. Masrour, J. E. Spangenberg, A. El-SamraniFig. S2. Location of selected samples (arrows) in Zalidou and DSDP Hole 416A; colors correspond to the pre-Weissert Event (blue), Weissert Event (green) and post-Weissert Event intervals (orange), following Shmeit et al. (2022). In Zalidou, the recognized stages are plotted with, the ammonite biostratigraphy (zones/subzones), calcareous nannofossil biostratigraphy (zones/subzones), sedimentary discontinuities (D0 to D8) and lithology (Reboulet et al. 2022; Shmeit et al. 2022). In Hole 416A, the recognized stages are plotted with, the calcareous nannofossil biostratigraphy (zones/subzones) same as for Zalidou, the lithological units, magnetic anomalies and lithology. Also, in Hole 416A, the Berriasian/Valanginian boundary is fixed following Čepek and Gartner (1980), and the top of the Valanginian stage is fixed following Shmeit et al. (2022). Abbreviations: Berr., Berriasian; Haut., Hauterivian; T. pertra., T. pertransiens; N. prem., N. premolicus; N. neocomiensi., N. neocomiensiformis; B. camp., B. campylotoxus; K. i., K. inostranzewi; S. ver., S. verrucosum; K. pro.; K. pronecostatum; T. c., Tescheniceras callidiscum and magnetic anom., magnetic anomalies.
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radiogenic isotope recordsfixed following čepekhaut ., hauteriviancalcareous nannofossil biostratigraphyweissert event intervalsfixed following shmeitet al .dsdp hole 416aprem ., nneocomiensi ., ncamp ., bberr ., berriasianweissert eventhole 416aet alver .,pertra .,ammonite biostratigraphy., kvalanginian stagevalanginian boundaryselected samplesrecognized stagesmagnetic anomalieslithological unitscolors correspond1980 ),