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Article Reference Biostratigraphy of the Danian/Selandian transition in the southern Tethys. Special reference to the Lowest Occurrence of planktic foraminifera Igorina albeari.
Located in Library / RBINS Staff Publications
Article Reference Reconstruction of a latest Paleocene shallow-marine eutrophic paleoenvironment at Sidi Nasseur (Central Tunisia) based on foraminifera, ostracoda, calcareous nannofossils and stable isotopes (δ13 C, δ18 O).
Located in Library / RBINS Staff Publications
Article Reference Shallow marine ostracode turnover in response to environmental changes during the Paleocene-Eocene thermal maximum in northwest Tunisia.
Located in Library / RBINS Staff Publications
Article Reference Assessing paleotemperature and seasonality during the early Eocene climatic optimum (EECO) in the Belgian Basin by means of fish otolith stable O and C isotopes.
Located in Library / RBINS Staff Publications
Article Reference A multi-proxy record of the Latest Danian Event at Gebel Qreiya, Eastern Desert, Egypt.
Located in Library / RBINS Staff Publications
Article Reference The global stratotype sections and points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain.
Located in Library / RBINS Staff Publications
Article Reference Latest Danian carbon isotope anomaly and associated environmental change in the southern Tethys (Nile Basin, Egypt).
Located in Library / RBINS Staff Publications
Article Reference Early Paleogene δ 13C and δ 18O records based on marine ostracodes: implications for the Upper Danian succession at Sidi Naseur (Tunisia) and their application value in paleoceanography
Located in Library / RBINS Staff Publications
Article Reference Reconstruction of a latest Paleocene shallow-marine eutrophic paleoenvironment at Sidi Nasseur (Central Tunisia) based on foraminifera, ostracoda, calcareous nannofossils and stable isotopes (δ13 C, δ18 O).
Located in Library / RBINS Staff Publications
Article Reference The Aktulagay section, west Kazakhstan: a key site for northern mid-latitude Early Eocene stratigraphy.
A section at Aktulagay (west Kazakhstan), in the Peri-Tethys realm, exposes mid-neritic to upper bathyal Ypresian marls, clays and silts. These range from Zone NP10 to early Zone NP14, with abundant and diverse microfossil assemblages. Multidisciplinary analysis has identified dinoflagellate cyst, calcareous nannofossil, planktonic and benthic foraminiferid and pteropod zones and events. Calibration of a key interval in the evolution of the shark Otodus has been possible for the first time. Episodic low-oxygen facies, including sapropelic clays widely distributed in Peri-Tethys, are represented here and can be placed within a detailed biostratigraphic framework. The current lithostratigraphic terminology is modified, with the introduction of the Aktulagay Formation. Paleoenvironmental aspects are discussed; five depositional sequences are tentatively identified. This section can be correlated in detail with the succession in the North Sea Basin, with implications for paleogeographic reconstructions. High-resolution biostratigraphic calibration between disparate fossil groups makes this a key reference section for northern mid-latitude Ypresian biostratigraphy.
Located in Library / RBINS Staff Publications