Planktonic foraminifera and stable isotopes of the upper Cenomanian–middle Turonian in central Tunisia: Implications for bioevents synchronicity and paleoenvironmental turnover

Author:

Salhi Idris,Elamri Zaineb,Bazeen Youssef S.ORCID,Ahmad Fayez,Mahmoudi Salah,Farouk Sherif

Publisher

Elsevier BV

Subject

Paleontology

Reference66 articles.

1. Response of calcareous nannoplankton to the Late Cretaceous Oceanic Anoxic Event 2 at Oued Bahloul (central Tunisia);Aguado;Palaeogeography, Palaeoclimatology, Palaeoecology,2016

2. Isotope signatures associated with early meteoric diagenesis;Allan;Sedimentology,1982

3. Zonation by ammonites and foraminifers of the Vraconnian-Turonian interval: a comparison of the Boreal and Tethyan domains (NW Europe/Central Tunisia);Amédro;Carnets de Géologie - Notebooks on Geology,2008

4. Position de la limite Cénomanien-Turonien dans la Formation Bahloul de Tunisie centrale: apports intégrés des ammonites et des isotopes du carbone (δ 13 C);Amédro;Eclogae Geologicae Helvetiae,2005

5. Stable isotopes of oxygen and carbon and their application to sedimentologic and environmental problems;Anderson,1983

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