Calcareous non-skeletal grains from northwestern Arabian Sea: insights into late Quaternary paleoclimate

Key Points

• Late Quaternary paleoclimate changes are evidenced by the study of calcareous grains.
• Significant shifts in oceanographic conditions were identified across multiple sediment layers.
• Sediment analysis was conducted to track climatic variations over the identified timeframe.
• Further research is needed to understand the broader implications of these findings in related regions.