Analysis reveals larger benthic foraminiferal turnover and carbon isotope shifts in carbonate platform, highlighting environmental changes during the Paleocene–Eocene Thermal Maximum.
Stable isotope datasets (δ13C and δ18O) from the Jandran and Sanjawi sections, along with supporting figures illustrating isotopic cross-plots and correlations, and tables of matrix micrite and bulk carbonate values.
No takes yet. Share an insight, caveat, or question.
Kamran et al. (2025) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: