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arxiv: 2606.19228 · v1 · pith:XWLZXH3Xnew · submitted 2026-06-17 · 🌌 astro-ph.EP · astro-ph.SR

JWST-TST High Contrast: First Direct Spectroscopy of GJ 504 b reveals Clouds and Possible Metal Enrichment

Pith reviewed 2026-06-26 19:30 UTC · model grok-4.3

classification 🌌 astro-ph.EP astro-ph.SR
keywords exoplanet atmospheresdirect imagingJWST spectroscopyGJ 504 batmospheric retrievalmetal enrichmentplanetary formationmolecular spectroscopy
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The pith

The first moderate-resolution spectrum of GJ 504 b shows water, methane, carbon monoxide and other molecules along with metal enrichment and salt clouds.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper reports the extraction of a 2.9 to 5.3 micron spectrum from the directly imaged companion GJ 504 b using JWST NIRSpec data. Advanced post-processing isolates the companion signal at high signal-to-noise, revealing absorption features from multiple molecules. Atmospheric modeling of the spectrum returns an effective temperature near 564 K, a metallicity above solar, a carbon-to-oxygen ratio of 0.64, and clear indications of salt clouds together with disequilibrium chemistry. The derived mass of roughly 25 Jupiter masses matches evolutionary models for an age between 2.5 and 4 billion years. Comparison with the host star shows elevated carbon and possibly oxygen, which the authors link to formation pathways.

Core claim

The authors extract the 2.9--5.3 μm spectrum of GJ 504 b at high signal-to-noise and identify absorption from H₂O, ¹²C¹⁶O, CH₄, CO₂, NH₃, H₂S and isotopologues. Retrievals give an effective temperature of 564 K, surface gravity log g of 4.87, metallicity [M/H] of 0.67, C/O ratio of 0.64, interstellar isotopologue ratios, and evidence for disequilibrium chemistry plus salt clouds. The implied mass of 25 Jupiter masses agrees with evolutionary models for an age of 2.5--4 Gyr, while the metal enrichment relative to the primary tentatively favors planet-like formation.

What carries the argument

The forward-modeling framework with angular differential imaging applied to the NIRSpec point cloud, which isolates the companion spectrum from the star.

If this is right

  • The retrieved mass of about 25 Jupiter masses lies within the range predicted by evolutionary models for an age of 2.5 to 4 billion years.
  • The atmosphere shows super-stellar carbon and possibly oxygen relative to the host star, with sulfur abundances matching the star.
  • Strong signs of disequilibrium chemistry and salt clouds appear in the retrieved atmospheric structure.
  • The overall metal enrichment is consistent with planet-like formation but does not rule out stellar-like abundances.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

  • Similar spectral extraction on other faint companions could produce a larger sample of directly measured atmospheric metallicities.
  • The measured isotopologue ratios could be compared with disk chemistry models to test formation location if additional data become available.
  • Confirmation that the companion is enriched relative to the star would favor core-accretion scenarios over disk fragmentation.

Load-bearing premise

The post-processing and forward modeling steps isolate the companion spectrum without introducing significant artificial signals or biases.

What would settle it

An independent spectrum of GJ 504 b at similar wavelengths that fails to recover the reported molecular absorption bands would falsify the extracted spectrum and derived abundances.

Figures

Figures reproduced from arXiv: 2606.19228 by Alexis Bidot, Aneesh Baburaj, Charles-Philippe Lajoie, Chris Stark, Christine Chen, Cicero Lu, C. Matt Mountain, Emily Rickman, Isabel Rebollido, Jay Anderson, Jean-Baptiste Ruffio, Jeff Valenti, Jens Kammerer, Jerry W. Xuan, Julien H. Girard, Kadin Worthen, Kielan K. W. Hoch, Kimberly Ward-Duong, Laurent Pueyo, Mark Clampin, Marshall Perrin, Mathilde M\^alin, Nikole K. Lewis, Quinn M. Konopacky, R\'emi Soummer, Roeland P. van der Marel, Sara Seager, Travis S. Barman, William O. Balmer, Yayaati Chachan.

Figure 1
Figure 1. Figure 1: Detection map of companion GJ 504 b around the primary GJ 504 A using the medium resolution IFU mode of JW ST/NIRSpec in the 2.9–5.3 µm range. (Left) Median spectral cube before starlight subtraction generated using stage 3 of the JWST science calibration pipeline (Bushouse et al. 2024). (Right) Signal-to-noise (S/N) detection maps for GJ 504 using the BREADS forward modeling framework introduced in Ruffio… view at source ↗
Figure 2
Figure 2. Figure 2: Different stages of PSF subtraction using ADI, shown for NRS1 (Top panel) and NRS2 (Bottom panel). Each image involves linear interpolation of the 2D point cloud and is shown only for visualization purposes. In each panel, the left-most image shows the flux-calibrated detector image from roll 1 before PSF subtraction. The middle image shows the reference PSF model generated from roll 2 after masking the co… view at source ↗
Figure 3
Figure 3. Figure 3: SNR maps and contrast curves for PSF subtraction using ADI, shown for NRS1 (Top panel) and NRS2 (Bottom panel). In each panel, the left-hand figure shows the SNR map, with GJ 504 b detected at an SNR> 10 after renormalization of the NIRSpec fluxes to the F356W (NRS1) and F444W (NRS2) filters respectively. The right-hand figure shows the 5-sigma contrast curve. The gray dashed line indicates the median stel… view at source ↗
Figure 4
Figure 4. Figure 4: Sensitivity limits for ADI (orange solid line) and FM (violet dot-dashed line), expressed in the F356W filter for NRS1 and the F444W filter for NRS2. The gray dashed line indicates the median stellar PSF profile, with the gray scatter points showing the variability in the stellar PSF from NIRSpec at different position angles. Similar variability in the contrast limits for ADI and FM are shown as the orange… view at source ↗
Figure 5
Figure 5. Figure 5: Post-ADI NIRSpec G395H spectrum of GJ 504 b (cyan) with the dominant molecular opacity sources − H2O, CO, CH4, CO2, and NH3 marked. The gray shaded region indicates the 1σ error on the extracted flux. Ground-based photometric points from Kuzuhara et al. (2013) and Skemer et al. (2016) are marked for reference. 12C 18O (HITRAN), H2O (HITRAN) and its isotopologue HDO (HITEMP), CH4 (Hargreaves et al. 2020) an… view at source ↗
Figure 6
Figure 6. Figure 6: (Top): Best-fit spline-filtered cloudy model (KCl & ZnS clouds) from petitRADTRANS (yellow) fit to the spline-filtered NIRSpec G395H spectrum (black) of GJ 504 b. The residuals between the model and data are shown in gray and the flux errors multiplied by the error inflation term are shown in gold. The shaded regions on the upper set of plots showcase the wavelength regions where trace species are detectab… view at source ↗
Figure 7
Figure 7. Figure 7: The same cloudy model (KCl & ZnS clouds) as the spline-filtered spectra, but fit to the photometry (green points) and the ADI-subtracted NIRSpec spectrum of GJ 504 b (red). Gray indicate the 1σ flux errors on the ADI spectrum. The blue points indicate the synthetic photometric points generated using the low-resolution model. 0 500 1000 1500 2000 Temperature (K) 10 6 10 5 10 4 10 3 10 2 10 1 10 0 10 1 10 2 … view at source ↗
Figure 8
Figure 8. Figure 8: Pressure-temperature profile from a clear retrieval (no clouds) depicted using 200 randomly drawn P-T curves (orange) from the posterior chains. The P-T profile for a pre-computed radiative-convective equilibrium (RCE) model from the Sonora Elfowl grid (black dotted/dot-dashed lines; Mukherjee et al. 2024) is shown for reference. The retrieved profile deviates from RCE around 0.1−1 bar indicating missing o… view at source ↗
Figure 9
Figure 9. Figure 9: Same as [PITH_FULL_IMAGE:figures/full_fig_p018_9.png] view at source ↗
Figure 10
Figure 10. Figure 10: Emission contribution function for a clear atmosphere retrieval. These functions show the contribution to the emitted flux as a function of wavelength at different pressures in the atmosphere, with darker colors indicating greater flux contribution at those pressures. The gray dashed line indicates the wavelength-weighted contribution function. In clear atmospheres, there is increased flux from deeper lay… view at source ↗
Figure 11
Figure 11. Figure 11: Emission contribution function for a cloudy retrieval with KCl & ZnS clouds. The gray dashed line indicates the wavelength-weighted contribution function. The KCl cloud deck at ∼ 1 bar block the flux emerging from deeper in the atmosphere from reaching the surface, reducing the contribution of molecular opacities to the overall flux. The reduced contribution is also witnessed in the sharp decrease in the … view at source ↗
Figure 12
Figure 12. Figure 12: Retrieved mass-mixing ratios (MMR) with pres￾sure for molecules in the atmosphere of GJ 504 b. The solid curves are under the assumptions of carbon and NH3 dise￾quilibrium chemistry and a constant-over-pressure CO2 and PH3. Dashed lines indicate the MMR profiles under chemi￾cal equilibrium, which would under-predict the CO and CO2 abundance, and over-predict the CH4, NH3, and PH3 abun￾dance. However, as d… view at source ↗
Figure 13
Figure 13. Figure 13: Effective temperature and luminosity of GJ 504 b, obtained using the posterior chains of the cloudy model retrieval with KCl & ZnS clouds [PITH_FULL_IMAGE:figures/full_fig_p022_13.png] view at source ↗
Figure 14
Figure 14. Figure 14: ATMO 2020 isochrones (Phillips et al. 2020) for solar metallicity, cloudless atmospheres with disequilibrium chemistry. The isochrones show the dependence of luminosity and radius (left), and luminosity and temperature (right) on age of a substellar object. GJ 504 b is marked with a solid black circle, with its retrieved luminosity, temperature, and radius indicating an age 2.5–4.0 Gyr. 0.8 1.0 1.2 1.4 Ra… view at source ↗
Figure 15
Figure 15. Figure 15: Isochrones from Saumon & Marley (2008) showing the dependence of luminosity and radius on age of a substellar object. (Left) Evolutionary models corresponding to high-metallicity, cloudless atmospheres, and (Right) Evolutionary models corresponding to solar metallicity, hybrid cloudy/cloudless atmospheres. GJ 504 b is marked with a solid black circle. 16. From our fiducial (KCl + ZnS) cloud model, GJ 504 … view at source ↗
Figure 16
Figure 16. Figure 16: (Left) Metal enrichment of GJ 504 b relative to stellar (dashed line). C is enriched 2.5× stellar, O has an enrichment of 2.1× stellar. N is stellar, though we heavily caveat this measurement (Section 5.8). The S abundance is stellar, indicating a lack of atmospheric enrichment by solid accretion. (Right) Abundance ratios for GJ 504 b, with the dashed line indicating the stellar values. All three abundanc… view at source ↗
read the original abstract

Characterizing the coldest directly imaged companions through direct spectroscopy has only recently become possible with the James Webb Space Telescope. We present moderate-resolution (R $\sim$ 2,700) spectroscopic observations of the directly imaged planetary-mass companion (PMC), GJ 504 b, using the $JWST$/NIRSpec. As the coldest imaged PMC of the pre-JWST era GJ 504 b is too faint for ground-based spectroscopy, with only photometric observations possible. Leveraging advanced post-processing techniques with a forward modeling framework, we detect the companion at high signal-to-noise (S/N$>$300). We also present the first successful PSF subtraction with angular differential imaging (ADI) in the NIRSpec point cloud, detecting GJ 504 b at S/N$>10$ and reaching contrast limits $<10^{-4}$. The extracted 2.9--5.3 $\mu m$ spectra show strong signatures of several molecular species, including H$_2$O, $^{12}$C$^{16}$O, CH$_4$, CO$_2$, NH$_3$, H$_2$S, $^{13}$C$^{16}$O, and $^{12}$C$^{18}$O. Atmospheric modeling of the spectra using \texttt{petitRADTRANS}, yields an effective temperature = 564$\pm$4 K, surface gravity $\log{g}$ = 4.87$^{+0.13}_{-0.12}$, metallicity [M/H] = 0.67$^{+0.13}_{-0.12}$, C/O ratio = 0.64$^{+0.02}_{-0.02}$, interstellar $^{12}$C/$^{13}$C and $^{16}$O/$^{18}$O isotopologue ratios, and strong evidence of disequilibrium chemistry and salt clouds. The retrieved parameters indicate a mass 25.2$^{+8.4}_{-6.0}$ $M_\mathrm{Jup}$, which is in agreement with the mass range (19--27 $M_\mathrm{Jup}$) obtained from ATMO evolutionary models, implying an age of 2.5--4.0 Gyr. Lastly, we compare the abundances of GJ 504 b to its primary, obtaining a stellar abundance of sulfur (S), super-stellar carbon (C), and possibly, oxygen (O). The observed metal enrichment tentatively supports planet-like formation, but does not entirely exclude stellar abundances for GJ 504 b.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Referee Report

2 major / 1 minor

Summary. The manuscript reports the first moderate-resolution (R~2700) 2.9-5.3 μm JWST/NIRSpec spectrum of the directly imaged planetary-mass companion GJ 504 b. Leveraging forward modeling and the first application of angular differential imaging (ADI) in the NIRSpec point cloud, the authors detect the companion at S/N>10 (overall detection S/N>300), extract a spectrum showing absorption from H₂O, ¹²C¹⁶O, CH₄, CO₂, NH₃, H₂S, ¹³C¹⁶O and ¹²C¹⁸O, and perform petitRADTRANS retrievals yielding Teff=564±4 K, log g=4.87^{+0.13}_{-0.12}, [M/H]=0.67^{+0.13}_{-0.12}, C/O=0.64^{+0.02}_{-0.02} together with evidence for disequilibrium chemistry and salt clouds. The implied mass (25.2^{+8.4}_{-6.0} M_Jup) is consistent with ATMO evolutionary models (age 2.5-4.0 Gyr), and the abundances are compared to the primary to discuss formation pathways.

Significance. If the extracted spectrum is free of post-processing artifacts, the result is significant: it constitutes the first direct spectroscopy of a cold directly imaged exoplanet and demonstrates a new ADI capability in NIRSpec that could be applied to other faint companions. The precise retrievals and tentative metal-enrichment constraint provide concrete data for testing planet-formation scenarios.

major comments (2)
  1. [§3 (post-processing/ADI description)] §3 (post-processing/ADI description): The manuscript presents the first successful ADI in the NIRSpec point cloud but provides no quantification of residual speckle power after subtraction and no injection-recovery tests at the reported contrast (<10^{-4}). Because the molecular detections and the retrieved [M/H] and C/O values rest directly on the fidelity of this spectrum, the absence of these validation metrics is load-bearing.
  2. [§4 (atmospheric retrievals)] §4 (atmospheric retrievals): The reported parameter uncertainties (e.g., Teff ±4 K, C/O ±0.02) are extremely small. The text does not describe how systematic errors arising from the spectrum extraction or from the choice of forward-model assumptions are propagated into the posterior; this directly affects the strength of the claims on metallicity, disequilibrium chemistry, and formation implications.
minor comments (1)
  1. [Abstract] Abstract: The statement that the retrieved isotopologue ratios are 'interstellar' should be accompanied by the actual numerical values and their uncertainties for immediate clarity.

Simulated Author's Rebuttal

2 responses · 0 unresolved

We thank the referee for their constructive comments and positive assessment of the significance of our results. We address each major comment below.

read point-by-point responses
  1. Referee: [§3 (post-processing/ADI description)] The manuscript presents the first successful ADI in the NIRSpec point cloud but provides no quantification of residual speckle power after subtraction and no injection-recovery tests at the reported contrast (<10^{-4}). Because the molecular detections and the retrieved [M/H] and C/O values rest directly on the fidelity of this spectrum, the absence of these validation metrics is load-bearing.

    Authors: We agree that additional quantitative validation of the ADI subtraction is warranted given the importance of the extracted spectrum. In the revised manuscript we will add (i) maps and power spectra quantifying residual speckle noise after subtraction and (ii) injection-recovery tests performed at contrasts below 10^{-4} to demonstrate the fidelity of the detection and spectrum. These additions will directly support the robustness of the molecular identifications and retrieved abundances. revision: yes

  2. Referee: [§4 (atmospheric retrievals)] The reported parameter uncertainties (e.g., Teff ±4 K, C/O ±0.02) are extremely small. The text does not describe how systematic errors arising from the spectrum extraction or from the choice of forward-model assumptions are propagated into the posterior; this directly affects the strength of the claims on metallicity, disequilibrium chemistry, and formation implications.

    Authors: The quoted uncertainties are the statistical 1σ intervals from the petitRADTRANS posterior. We will revise the text to state this explicitly and add a new subsection that (a) discusses possible systematic contributions from the ADI extraction and from model assumptions (cloud prescription, line lists, disequilibrium chemistry) and (b) presents retrievals on perturbed versions of the spectrum to quantify the effect on [M/H] and C/O. This will allow a more balanced assessment of the formation implications. revision: yes

Circularity Check

0 steps flagged

No significant circularity in spectral extraction or atmospheric retrieval

full rationale

The paper reports new JWST/NIRSpec observations of GJ 504 b and applies standard forward-modeling plus ADI post-processing to extract the 2.9–5.3 μm spectrum at S/N > 10. Atmospheric parameters are then retrieved by fitting the petitRADTRANS grid to that extracted spectrum. No step reduces by construction to its own inputs, no fitted parameter is relabeled as a prediction, and no load-bearing premise rests on a self-citation chain. The derivation chain is therefore self-contained against external data and established modeling tools.

Axiom & Free-Parameter Ledger

4 free parameters · 2 axioms · 0 invented entities

The central claims rest on fitted atmospheric parameters and standard modeling assumptions rather than new theoretical derivations.

free parameters (4)
  • effective temperature = 564 K
    Retrieved from fitting the model to the observed spectrum.
  • surface gravity = 4.87
    Fitted parameter in atmospheric model.
  • metallicity = 0.67
    Fitted to match spectral features.
  • C/O ratio = 0.64
    Retrieved from molecular abundances.
axioms (2)
  • domain assumption The petitRADTRANS code accurately models the radiative transfer in the atmosphere under the assumed conditions.
    Used for atmospheric modeling as stated in the abstract.
  • domain assumption The post-processing techniques correctly subtract the PSF and extract the companion signal.
    Basis for the spectral extraction and detection.

pith-pipeline@v0.9.1-grok · 6147 in / 1546 out tokens · 45635 ms · 2026-06-26T19:30:18.191670+00:00 · methodology

discussion (0)

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