| Description: |
Sea-level change over Earth's history reflects the interplay of water volume and the ever-shifting architecture of ocean basins. While short-term fluctuations (103–105 yr) often trace the advance and retreat of glaciers and ice caps, multi-million-year trends (107–109 yr) arise from deep-Earth processes – seafloor spreading, subduction, intraplate deformation, mantle plume upwelling, and the emplacement of large igneous provinces – that remodel basin volume and modulate the ocean's water budget. New geodynamic models now discard the assumption of steady-state mantle regassing and degassing, showing instead that persistent imbalances can lock water into the interior or release it back to the surface, sculpting long-term sea-level trajectories. Recent advances in seismic and tomographic imaging, coupled with high-resolution numerical simulations, have fostered an emerging convergence between geodynamic theory and stratigraphic records of Phanerozoic sea-level curves – particularly for second-order (multi-million years) Meso-Cenozoic variations. These efforts also cast doubt on earlier reconstructions based solely on continental flooding metrics without accounting for evolving hypsometries. Superimposed on these tectonic signals are third-order cycles driven largely by Earth's orbital rhythms: long-period Milankovitch modulations (∼1.2 Myr obliquity, especially common during refrigerations, and ∼2.4 Myr eccentricity, recurrent during warm intervals) leave clear imprints in sequence stratigraphic, deep-sea hiatuses, fossil diversity patterns, and stable-isotopic records. Meanwhile, the capacity of small, hydrous mantle plumes to shuttle water across the core-mantle boundary – and the topographic uplift associated with flood basalt provinces – emerges as an underappreciated influence on regional sea-level anomalies. Despite these advances, reconstructing pre-Cretaceous sea-level history remains hampered by scant constraints on ancient spreading and subduction systems. Addressing these gaps and achieving further ... |