Summary
Researchers combined magnetic measurements, grain‑size analysis, and accelerator mass spectrometry radiocarbon dating to reconstruct climate phases.
The record captures the Last Glacial Maximum, the warm Bølling‑Allerød, the Younger Dryas cooling, and the Holocene climatic optimum.
These long‑term data help distinguish natural climate variability from recent human‑induced changes.
The insights can improve climate models and guide water‑resource, agricultural, and flood‑management planning in the Ganga Plain.