A primordial heavy water reservoir in the outer solar systemOPEN ACCESS
Lindsay P. Keller, Christopher J. Snead, Ming-Chang Liu, and Kevin D. McKeegan
Science Advances
11 Nov 2026
Vol 12, Issue 46
LINK (OPEN ACCESS)
PDF (OPEN ACCESS)
“The oxygen (O) isotopic composition of outer solar system ices is believed to be enriched in heavy O isotopes owing to photochemical processes, but evidence for this O reservoir is exceedingly rare in meteorites. Hydrated interplanetary dust particles (IDPs) collected in Earth’s stratosphere that display high densities of solar energetic particle tracks originate from Edgeworth-Kuiper belt objects. Their mineralogy is dominated by hydrated minerals that formed by alteration of anhydrous precursor minerals at low temperatures through reactions with water (H2O)–carbon dioxide fluids. The O isotopic compositions of track-rich hydrated IDPs implicate 17,18O-rich ices as the source of H2O involved in their alteration, providing compelling evidence for the presence of a major heavy water reservoir beyond the orbits of the gas giant planets that was largely isolated from inner solar system materials.”


































