Upper ocean temperature change caused by the closing of the Indonesian Seaway from the late Miocene to early Pliocene

Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1. 1Gradual Warming of Western Pacific Warm Pool Due To Weakening of Indonesian Throughflow During the Late Mid‐Pleistocene Transition2025 · 2 citations
2. 2Changes in the Indonesian Throughflow Since the Late Miocene Based on Radiolarian Assemblages From ODP Site 710 in the Western Tropical Indian Ocean: Implications of the Indo‐Pacific Gateway (Indonesian Seaway)2026
3. 3Migrations of the Indo-Pacific Warm Pool through the past eight glacial cycles2024
4. 4Impact of tropical seaways closure on ENSO variability during the Middle Miocene Climatic Optimum2026
5. 5Seasonal Response of the Miocene Indonesian Throughflow to Orbital Forcing Buffered by an Open Seaway2026