Szczegóły publikacji
Opis bibliograficzny
Carbon isotopes, palynology and stratigraphy of the Santonian-Campanian boundary: the GSSP auxiliary sections, Seaford Head (England) and Bocieniec (Poland), and correlation between the Boreal and Tethyan realms / Ian Jarvis, Martin A. Pearce, Johannes Monkenbusch, Agata JURKOWSKA, Clemens V. Ullmann, Zofia Dubicka, Nicolas Thibault // Cretaceous Research ; ISSN 0195-6671. — 2023 — vol. 143 art. no. 105415, s. 1-45. — Bibliogr. s. 38-42, Abstr.
Autorzy (7)
- Jarvis Ian
- Pearce Martin A.
- Monkenbusch Johannes
- AGHJurkowska Agata
- Ullmann Clemens V.
- Dubicka Zofia
- Thibault Nicolas
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 144208 |
|---|---|
| Data dodania do BaDAP | 2022-12-21 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.cretres.2022.105415 |
| Rok publikacji | 2023 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Cretaceous Research |
Abstract
The stratigraphy and palynology of the upper Santonian–lower Campanian (Uintacrinus socialis–Gonioteuthis quadrata zones) Newhaven Chalk are described for the Campanian auxiliary GSSP section at Seaford Head, England. A new high-resolution bulk-sediment carbonate carbon stable-isotope (δ13Ccarb) curve provides the basis to refine the carbon-isotope event (CIE) stratigraphy of the section. Results are compared to a complementary palynological study of a second Campanian auxiliary GSSP section (U. socialis–O. pilula zones) at Bocieniec, Poland. Palynological assemblages are dominated by organic-walled dinoflagellate cysts (dinocysts; 208 taxa) at both sites. A stratigraphic framework is established via review of published lithostratigraphic, macrofossil, foraminifera and calcareous nannofossil records from the study sites. Carbon isotope curves with 13 major named CIEs provide a basis for correlation of Seaford Head and Bocieniec to sections at: Trunch, England; Poigny, France; Lägerdorf, Germany; and the Campanian GSSP at Gubbio, Italy. Correlations are constrained by biostratigraphic records, including dinocyst events. The Late Santonian δ13C Event (LSE, previously termed the Santonian–Campanian Boundary Event, SCBE) provides a key correlation level between Boreal and Tethyan sections and enables the placement of base Campanian markers: extinction levels of the crinoid Marsupites and the planktonic foraminifera Dicarinella asymetrica; the first appearance of the calcareous nannofossil Aspidolithus parcus parcus; and the C34n/C33r magnetozone boundary (the primary Campanian marker), in both Boreal and Tethyan sections. A holostratigraphy for the Santonian–Campanian boundary interval that integrates CIEs, macrofossils, benthic and planktonic foraminifera, calcareous nannofossils, dinocysts and magnetostratigraphy is presented. Rhynchodiniopsis juneae sp. nov. is described.
