- The paper reports that JWST NIRSpec data revealed a CO2-dominated coma with a CO2/H2O ratio of 8.0±1.0, far exceeding typical Solar System values.
- The paper details spatially resolved spectral analyses and Q-curve modeling techniques that quantified production rates and mapped dust and gas distributions in the coma.
- The paper discusses implications for interstellar planetesimal formation, proposing that unique volatile inventories and suppressed H2O sublimation signal non-traditional formation histories.
JWST NIRSpec Detection of a CO2-Dominated Gas Coma in Interstellar Object 3I/ATLAS
Introduction
The detection and characterization of interstellar objects (ISOs) traversing the Solar System provide unique constraints on the physical and chemical conditions of planetesimal formation in extrasolar environments. The third confirmed ISO, 3I/ATLAS, presents an opportunity to probe the volatile inventory of a body formed outside the Solar System. This paper reports JWST NIRSpec IFU observations of 3I/ATLAS at rH=3.32 au, revealing a coma dominated by CO2 gas, with significant implications for the understanding of volatile processing and retention in interstellar planetesimals.
Observational Strategy and Data Reduction
JWST NIRSpec IFU observations were conducted with a 3′′×3′′ field of view, providing spatially resolved spectroscopy from 0.6 to 5.3 μm at R∼30–300. The data were acquired in four dithered positions, with background subtraction performed using offset sky exposures. The resulting data cubes enabled the extraction of both spatially integrated and spatially resolved spectra, facilitating the mapping of dust and gas emission features across the coma.
Spectral Characterization of the Coma
The spatially integrated NIRSpec spectrum of 3I/ATLAS displays prominent emission features attributable to CO2, H2O, and CO, as well as solid-state absorption bands from water ice and dust scattering.
Figure 1: JWST NIRSpec prism spectrum of 3I/ATLAS, showing strong CO2 emission at 4.3~μm and additional features from H2O, CO, and water ice.
Spatially resolved flux maps reveal the distribution of dust and volatiles in the coma.



Figure 2: JWST NIRSpec flux maps for 3I/ATLAS: (a) dust-scattered light at 1.2~μm, (b) CO2 at 4.3~μm, (c) H2O at 2.7~μm, (d) CO at 4.7~μm. Insets show spatially averaged, continuum-subtracted spectra for each gas.
The dust coma exhibits a pronounced sunward enhancement, while the gas species display more symmetric distributions, with CO2 being the most spatially extended and intense. The 1/ρ-enhanced maps further highlight the anisotropy in dust and subtle asymmetries in gas emission.
Figure 3: 1/ρ-enhanced 1.2~μm dust map, emphasizing the sunward plume structure in the coma.
Quantitative Spectral Modeling
Production rates and rotational temperatures for CO2, CO, H2O, and OCS were derived using the Planetary Spectrum Generator (PSG) and optimal estimation routines. The modeling accounted for continuum contributions, line opacity, and spatial variations in the coma.


Figure 4: NIRSpec IFU spectra within a 0.625''-radius aperture centered on the nucleus, with best-fit models for continuum and gas emission components.
A Q-curve analysis was performed to extract production rates as a function of nucleocentric distance, mitigating optical depth effects near the nucleus and enabling the determination of terminal coma mixing ratios.
Figure 5: Gas production rates (Q) for CO2, CO, H2O, and OCS as a function of distance from the nucleus. CO2 dominates the volatile output at all radii.
The terminal production rates are Q(CO2)=(1.76±0.02)×1027 s−1, Q(CO)=(3.0±0.2)×1026 s−1, Q(H2O)=(2.19±0.08)×1026 s−1, and Q(OCS)=(4.3±0.9)×1024 s−1. The derived CO2/H2O mixing ratio is 8.0±1.0, a value that is 6.1σ above the trend for Solar System comets at similar heliocentric distances.
Comparative Analysis with Solar System Comets
The CO2/H2O ratio in 3I/ATLAS is anomalously high compared to the established distribution for both long-period and Jupiter-family comets.
Figure 6: CO2/H2O mixing ratios as a function of heliocentric distance for comets of various dynamical classes. 3I/ATLAS (red star) is a strong outlier, with a ratio 16× higher than the Solar System trend at rH=3.3 au.
This elevated ratio is only rivaled by the hypervolatile-rich comet C/2016 R2, but 3I/ATLAS does not exhibit a similarly extreme CO/H2O ratio. The data suggest either an intrinsically CO2-rich nucleus or suppressed H2O sublimation, potentially due to a low thermal conductivity crust or high surface albedo inhibiting heat penetration.
Coma Structure and Outgassing Morphology
The spatial analysis of the coma reveals heterogeneous outgassing patterns. The dust is strongly enhanced in the sunward direction, while the gas species show more modest asymmetries, consistent with their respective sublimation temperatures. The S/S′ ratios (sunward/antisunward) for dust, CO2, CO, and H2O are 1.37, 1.07, 1.04, and 1.20, respectively, indicating that the less volatile species (H2O) are more sensitive to solar heating.
Isotopic Constraints
A lower limit on the 12C/13C ratio in CO2 was established (>77 at 3σ), consistent with terrestrial values, but higher SNR and spectral resolution are required for a definitive measurement.
Rotational Temperatures
Rotational temperatures for CO2, CO, and H2O were retrieved as a function of nucleocentric distance, providing constraints on coma excitation conditions.
Figure 7: Rotational temperatures for CO2, CO, and H2O as a function of projected distance from the nucleus.
The observed CO2-dominated volatile inventory in 3I/ATLAS is inconsistent with the bulk ice compositions of most Solar System comets, where CO2/H2O ratios are typically ≲0.2. Theoretical models of protoplanetary disk chemistry indicate that CO2-rich ices can form in regions exposed to elevated UV/X-ray irradiation or near the CO2 ice line, especially in low-metallicity or dynamically old stellar populations. The high CO2/H2O ratio in 3I/ATLAS may thus reflect formation in such an environment, or extensive radiolytic processing during a prolonged interstellar sojourn.
Future Prospects
Further JWST and ground-based observations of 3I/ATLAS at smaller heliocentric distances are essential to determine whether the high CO2/H2O ratio persists as H2O sublimation becomes more efficient. The combined capabilities of JWST and the Vera C. Rubin Observatory will enable systematic studies of volatile inventories in both interstellar and Solar System comets, improving the statistical basis for comparative planetology.
Conclusion
JWST NIRSpec IFU observations of 3I/ATLAS reveal a coma with a CO2/H2O mixing ratio of 8.0±1.0, a value that is a significant outlier relative to Solar System comets at comparable heliocentric distances. This result suggests either an intrinsically CO2-rich nucleus or suppressed H2O outgassing, with implications for the formation and evolutionary history of interstellar planetesimals. The findings underscore the diversity of volatile compositions among ISOs and highlight the diagnostic power of high-sensitivity infrared spectroscopy for constraining the chemical evolution of small bodies beyond the Solar System.