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A cold and distant origin for the interstellar object 3I/ATLAS
I/ATLAS, the third-known interstellar visitor to pass through our Solar System, may have formed in an ancient planetary system around 12 billion years ago. Isotopic evidence, presented in Nature this week, reveals that the object has a composition unlike anything else in the Solar System.
3I/ATLAS, discovered in July 2025, is the third confirmed interstellar object to pass through our inner Solar System. Despite detailed observations of this object, the precise age, origin, and path of 3I/ATLAS have been uncertain. Estimates of its age have ranged from 3–10 billion years old based on its velocity. Measurements of the ratio of isotopes (different versions of chemical elements) can offer clues about the physical and chemical conditions where 3I/ATLAS formed.
Martin Cordiner and colleagues report isotopic measurements of 3I/ATLAS obtained from observations from JWST and the ALMA observatory. Ratios of hydrogen isotopes provide insights into the temperature and radiation in the environment in which 3I/ATLAS formed, while carbon isotope ratios can help to locate the object’s home interstellar gas cloud. The water in 3I/ATLAS contains 10 times more deuterium (a hydrogen isotope) than other known comets, and the carbon ratios exceed typical values found in the Solar System, as well as nearby interstellar clouds and protoplanetary disks. The authors propose that the observed values indicate that 3I/ATLAS formed in a cold environment, less than 30 K (roughly –243 °C). The carbon composition implies that 3I/ATLAS may have formed 12 billion years ago, following a period of intense, early star formation in its host environment.
These findings suggest that 3I/ATLAS came from a primordial ancient planetary system, the authors conclude.