Strontium and sulfur isotope constraints on climate fluctuations and marine incursions in the lacustrine Subei Basin during the late Paleocene

Key Points

• Climate fluctuations appear evident in the Subei Basin during the late Paleocene, indicating significant environmental changes.
• Strontium and sulfur isotopes demonstrate clear variations related to marine incursions across different strata.
• The analysis of isotopes provides insights into lacustrine environments and their response to past climatic conditions.
• Findings may highlight the intricate relationships between marine events and terrestrial climate shifts in historical contexts.