[MIS14-02] Myr-scale monsoon records paced with Milankovitch cycles during Triassic-Jurassic
Earth’s orbital variations on timescales of 104-105 years, known as Milankovitch cycles, have played a critical role in pacing climate change and ecosystem dynamics, through glacial and/or monsoon dynamics. However, the climatic and biotic consequences of these cycles on much longer (~107 years) timescales remain unclear, due to a lack of long proxy records with precise age constraints. Here, we show ~10-Myr scale variations in early Mesozoic (250-180 Ma) records of pelagic biogenic-silica burial flux, atmospheric pCO2, and sea-surface-temperature (SST). Their phase relationships, coupled with carbon cycle modeling results, suggest that orbitally-paced summer monsoon dynamics modulates changes in global weatherability, affecting changes in pCO2 and SST.