Supplemental Material: Early to middle Eocene (50–43 Ma) Xianqian Basin in central Tibet: Archives of arid paleoenvironments and a southward plateau uplift trend

The research highlights a trend of plateau uplift during the Eocene, impacting climate and ecosystems.
Analysis of paleoenvironments in the Xianqian Basin indicates significant aridity around 50–43 Ma.
Findings contribute to understanding the geological history of central Tibet and its climatic evolution.
Understanding these trends is essential for insights into past environmental conditions and landscape evolution.

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