Where Did Earth Get Its Oceans? Maybe It Made Them Itself
Scientists are reconsidering the origin of Earth's oceans, moving beyond the long-held theories that water was delivered by comets or asteroids. While early evidence favored comets, their distinct deuterium-to-hydrogen (D/H) ratios mismatched Earth's water, leading researchers to favor asteroids, whose water chemistry aligns more closely. However, discrepancies in noble gas levels and questions about late bombardment timing have fueled a radical new hypothesis: Earth may have generated much of its water internally. Recent experiments show that high-pressure reactions between hydrogen in the early atmosphere and oxygen-rich magma could have produced vast amounts of water rapidly, suggesting planets like Earth might naturally become water-rich. While uncertainties remain about whether Earth had enough hydrogen for this process, increasing evidence—including renewed support for cometary contributions—points to a complex, mixed origin where indigenous production, asteroids, and comets all played a role.
































