Late Cretaceous to Palaeogene carbon isotope, calcareous nannofossil and foraminifera stratigraphy of the Chalk Group, Central North Sea. (February 2021)

• Record Type: Journal Article
• Authors: Eldrett, James S.; Vieira, Manuel; Gallagher, Liam; Hampton, Matthew; Blaauw, Maarten; Swart, Peter K.
• Is Part Of: Marine and petroleum geology. Volume 124(2021)
• Publication Date: 2021-02
• Subjects: Late cretaceous -- Chalk -- Calcareous nannofossils -- Carbon isotope stratigraphy -- Micropalaeontology; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2020.104789
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: A highly resolved record of stable carbon isotope values (δ 13 C) of the Late Cretaceous to Palaeogene (Cenomanian – Danian) was generated from ditch-cuttings material recovered from the Shearwater A9 hydrocarbon production well, Shearwater Field, Central North Sea. The profile of δ 13 C values was integrated with calcareous nannofossil and foraminifera biostratigraphy to provide an integrated stratigraphy for the Late Cretaceous Chalk Group. Detailed correlation between Shearwater A9 carbon isotope stratigraphy and associated biostratigraphic events with other similar records from both the Boreal and Tethyan Realms, including several proposed and/or ratified Global Boundary Stratotype Sections and Points had enabled the identification of major Stage and sub-Stage boundaries. This study provides a long-term and near-continuous stratigraphic record of the Late Cretaceous and earliest Palaeogene from more basinal facies of the Central North Sea. The record is punctuated with several short duration hiatal intervals, and a longer hiatus is identified whereby most of the Cenomanian is missing at this location. Highlights: A 37 Myr-long Late Cretaceous to Paleogene stratigraphy generated for the North Sea Chalk Group. Stable isotope values generated from ditch-cuttings material. Diagenetic alteration of the primary depositional signal was evaluated. Integrated with nannofossil and foraminifera biostratigraphy. Precise correlations between the Shearwater Field and other published Boreal and Tethyan sections.