REVIEW 4 major objections 5 minor 2 cited by
exoALMA. X. channel maps reveal complex $^{12}$CO abundance distributions and a variety of kinematic structures with evidence for embedded planets
T0 review · 4 major / 5 minor · reviewed 2026-08-16 · deepseek-v4-flash
Pith's one-line read Six of 15 planet-forming disks show gas kinks consistent with embedded giant planets, and seven show only partial CO freeze-out.
desk verdict A solid survey-level census of kinematic deviations in 15 disks with carefully hedged planet candidates; the CO midplane detection is the sturdiest new result. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The workhorse is the velocity channel map: a single-velocity image of the line emission, with isovelocity curves showing where the projected Keplerian velocity equals that channel. A 'velocity kink' is a localized distortion of an isovelocity curve, and the paper uses the result that each time a planet's wake crosses an isovelocity curve it creates a kink, so multiple kinks across channels do not rule out a single planet. To turn kinks into planet properties, the paper runs gas-only smoothed-particle hydrodynamics simulations post-processed with 3D radiative transfer to produce synthetic channel maps for planets of 1, 2, 5, and 10 $M_\mathrm{Jup}$, comparing shapes and amplitudes by eye. For the chemistry, a CO abundance prescription with freeze-out below 20 K, photodissociation, and photodesorption is used to model the midplane depletion and outer-disk desorption.
What would settle it
A high-contrast image at the deprojected kink locations in AA Tau, SY Cha, J1842, J1615, LkCa 15, or HD 143006 that shows no companion, combined with a non-planet hydrodynamic simulation that reproduces the same kinks, would falsify the planet interpretation; a resolved line-ratio measurement of midplane CO in one of the seven disks implying depletion below $10^{-3}$ of the warm-layer value would falsify the partial freeze-out claim.
Extended reading notes
Core claim
The central claim is that individual channel maps of $^{12}$CO $J=3-2$ in the 15-disk sample reveal a rich zoo of kinematic deviations from Keplerian rotation, and that in six of those disks the deviations take the form of velocity kinks consistent with the wakes of embedded planets. Comparing the data to gas-only hydrodynamical plus radiative-transfer models with a single planet, the paper infers planet masses of about 1 to 5 $M_\mathrm{Jup}$ at orbital radii of 80 to 310 au. A separate but equally central discovery is that in every disk where the upper and lower emission surfaces can be separated (seven disks), there is non-zero emission between the surfaces, implying the vertical CO snowline is present but freeze-out is partial: the midplane $^{12}$CO abundance is only $10^{-3}$ to $10^{-2}$ of the warm-layer value, and CO desorbs in the outer disk. Both results are presented as preliminary, with the planet masses limited by the simplicity of the model grid.
Load-bearing premise
The argument rests on assuming each velocity kink is the wake of a single embedded planet rather than another disk motion (instability, thermal wave, or companion), and that the planet masses come out right from a simplified gas-only, vertically isothermal, single-planet model with a fixed viscosity and a chosen CO abundance.
Editorial extensions
If this is right
- If the six planet candidates are real, wide-orbit giant planets (1–5 $M_\mathrm{Jup}$ at 80–310 au) are present in 6 of 15 large, bright disks, suggesting such planets are not rare when the disk is big enough.
- The candidate planets sit just outside the dust continuum emission, which would mean they are truncating the dusty disk at large radii.
- Partial midplane freeze-out ($10^{-3}$–$10^{-2}$ depletion) and outer-disk desorption must be built into disk chemical models, and CO-based gas mass estimates that assume full freeze-out may need revision.
- The background of other kinematic deviations sets the current detection floor at about 1 $M_\mathrm{Jup}$, so lower-mass planets could be hidden in the noise.
- Additional physics (vertical temperature gradients, multiple planets, or disk instabilities) is likely needed to explain all observed deviations, especially the filamentary structures.
Reading between the lines
- If midplane CO is only partially depleted in a wide range of disks, then CO snowline positions derived from emission gaps may overestimate the true freeze-out radius; mapping midplane emission at higher resolution could test this.
- The prevalence of wide-orbit planet candidates in this sample could connect to direct-imaging surveys: many of these planets would be directly imageable with next-generation instruments if they are real companions.
- Comparing these channel maps with non-planet simulations (e.g., vertical shear instability or buoyancy spirals) at the same resolution would separate planet wakes from other velocity perturbations; the paper's public data products make such a comparison possible.
Signed reviews
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. This paper analyzes 12CO J=3-2 channel maps of the 15 exoALMA protoplanetary disks. The authors report kinematic deviations from Keplerian rotation in 13 of 15 disks, classifying them as large-scale arcs, localized velocity kinks, and filamentary structures. For six disks (AA Tau, SY Cha, J1842, J1615, LkCa 15, HD 143006) they interpret the kinks as planet wakes, and for five of them they run phantom/mcfost single-planet simulations, concluding that planet masses of 1-5 MJup at orbital radii of 80-310 au best match the observations. In the seven disks with favorable inclination for separating the upper and lower emitting surfaces, they consistently detect midplane CO emission and infer a partial freeze-out depletion factor of roughly 10^-3 to 10^-2 relative to the warm molecular layer, together with CO desorption in the outer regions. The paper explicitly acknowledges that the morphological classification is subjective and that the modeling is a restricted, preliminary exploration.
Significance. The observational catalog of kinematic substructures and the systematic detection of midplane CO emission are valuable contributions, and the paper strengthens them with concrete cross-checks: reimaging without continuum subtraction, regularized maximum likelihood imaging, and consistency checks against dynamite and discminer surface parameters. The public release of synthetic models and data products through the cited Dataverse is a further strength that supports reproducibility. The wake-location overlay in Figure 5 provides a falsifiable prediction that can be tested with deeper or higher-resolution data. If the planetary interpretation is confirmed by a dedicated test against non-planet mechanisms, the inferred population of 1-5 MJup planets at large orbital radii would be an important result for planet formation. As it stands, the robust claims are the qualitative detections of kinematic deviations and midplane CO; the quantitative mass and depletion values are model-dependent and require stronger support.
major comments (4)
- [4.2, Fig. 7] The planet mass estimates are based on a by-eye comparison to a grid of 1, 2, 5, and 10 MJup at fixed disk parameters, with no quantitative goodness-of-fit metric or uncertainty budget. The abstract and conclusions present 'masses between 1 and 5 MJup' as a result, but this range is not demonstrably constrained: the paper does not explore variations in disk scale height, viscosity, CO abundance, or planet accretion radius. Either a quantitative fitting procedure over a denser grid should be added, or the mass range should be explicitly described as illustrative rather than as an estimate.
- [4.1, 5, Fig. 3] The attribution of the velocity kinks to embedded planets is not tested against the main non-planet alternatives. All new hydrodynamic runs adopt a locally isothermal equation of state and contain exactly one planet, while the observed filamentary structures in SY Cha, J1615, LkCa 15, J1852, DM Tau, and HD 34282 are said to resemble VSI/MRI predictions, as the authors themselves note. A no-planet, vertically stratified or MHD simulation should be compared to the same channel maps to show that instabilities such as VSI cannot produce the observed kink morphology; without such a control, the planetary interpretation is one viable hypothesis rather than a demonstrated detection. I would caution against phrasing the issue as 'vertical isothermality removes VSI', since locally isothermal baroclinic disks can in fact host VSI; the real gap is the absence of a no-planet comparison run.
- [3.2, 4.2, Fig. 8] The depletion factor of 10^-3 to 10^-2 is derived from only two disks (LkCa 15 and J1615) and from a single hydrodynamic realization, with no exploration of correlations with disk density, thermal structure, or UV radiation, yet the abstract applies this range to all seven disks where midplane CO is detected. The qualitative conclusion that CO is not fully frozen out in the midplane is well supported, but the quantitative depletion range should either be restricted to the two modeled sources or be supported by similar fits to the other five disks.
- [Table 2, 4.1] Several quoted quantities are fitted parameters rather than independent measurements: the planet orbital radii are set by the visually identified kink locations, the disk masses are tuned to reproduce the separation between emitting layers, and the CO depletion factor is adjusted to match the observed brightness. This fitting procedure is appropriate for testing a hypothesis, but the paper should consistently label the resulting masses, radii, and abundances as model-inferred values, not as free derivations from the data, to avoid giving the impression of independent predictions.
minor comments (5)
- [Fig. 7 caption] The caption lists the synthetic model grid as '1, 2, 3 and 5 M Jup', while the text in §4.1 states masses of 1, 2, 5, or 10 MJup; please reconcile this inconsistency.
- [3.1] The word 'corrresponds' should be corrected to 'corresponds'.
- [Fig. 5 caption] The abbreviation 'SPHERE DPI' is not expanded at first use; please define 'DPI' (dual-polarization imaging) in the caption or in the text.
- [Table 1 and text] Velocity units appear inconsistently as 'km/s', 'm/s', and 'm s^-1' across Table 1 and the text; please adopt one consistent notation, preferably 'm s^-1' for channel offsets and 'km s^-1' for systemic velocities.
- [3.2] The sentence noting that 'the majority of disks exhibiting evidence of desorption also show potential signs of planets' and calling this 'likely a coincidence' would benefit from either a brief statistical argument or removal, as presented it is an unsupported aside.
Circularity Check
No significant circularity: the kinematic detections and model comparisons are self-contained, and fitted parameters are transparently labeled as estimates rather than predictions.
full rationale
The paper's central empirical content is an observational detection: velocity kinks and midplane 12CO emission are identified directly in channel maps, with robustness checks that include no-continuum-subtraction imaging and regularized maximum likelihood imaging. The planet interpretation is a forward-model consistency test: a planet is placed at the observed kink position, the mass is stepped over a discrete grid, and synthetic cubes are compared with the data. The paper explicitly states that the goal is to test 'whether a single planet can reasonably explain the observed channel maps,' and the mass constraints are called 'preliminary' and the freeze-out range 'only indicative.' These are model fits, not predictions produced by construction. The orbital radii are taken from the deprojected kink locations, so reporting them as 'suggested' by the simulations is loose wording, but the radii are not derived from the simulations themselves and the paper does not claim they are independently predicted. Self-citations appear (dynamite, the CO abundance prescription, the phantom/mcfost benchmark, and the Bollati et al. kink-crossing result), but none is load-bearing in a circular way: they are methodological tools or external theoretical results whose assumptions do not include the target detections, and they are not invoked as uniqueness theorems. The lack of a no-planet, VSI-capable comparison is a genuine model-selection limitation, not a circular step; the paper itself flags vertical isothermality and instabilities as limitations. Under the standard that circularity requires a specific reduction of a claimed derivation to its inputs, no such reduction is present here.
Assumptions & free parameters
free parameters (4)
- Planet masses (AA Tau, J1615, J1842, LkCa 15, SY Cha) =
2, 2, 1, 5, 5 Jupiter masses
- Planet orbital radii =
80, 310, 105, 240, 140 au
- CO freeze-out depletion factor =
10^-3 to 10^-2
- Model disk masses =
5e-3 to 1e-2 solar masses
assumptions (5)
- domain assumption Velocity kinks trace planet wakes crossing isovelocity curves (Rafikov 2002; Bollati et al. 2021).
- domain assumption A single embedded planet in a vertically isothermal, gas-only, non-self-gravitating SPH disk captures the observed kinks.
- domain assumption The CO abundance prescription of Pinte et al. (2018a) (freeze-out, photodissociation, photodesorption) applies, with warm-layer abundance 1e-4 relative to H.
- domain assumption CO J=3-2 emission is thermalized (LTE) with Tgas = Tdust and no turbulent broadening.
- domain assumption Disk geometries and stellar masses from dynamite (Keplerian fits) are correct.
Cite this review
Pith. "Pith review of exoALMA. X. channel maps reveal complex $^{12}$CO abundance distributions and a variety of kinematic structures with evidence for embedded planets." pith.science (2026). https://pith.science/paper/5GSO74CJ
@misc{pith2026250418717,
author = {Pith},
title = {Pith review of: exoALMA. X. channel maps reveal complex $^12$CO abundance distributions and a variety of kinematic structures with evidence for embedded planets},
year = {2026},
howpublished = {\url{https://pith.science/paper/5GSO74CJ}},
note = {Machine review of arXiv:2504.18717}
}
abstract
We analyze the $^{12}$CO $J=3-2$ data cubes of the disks in the exoALMA program. 13/15 disks reveal a variety of kinematic substructures in individual channels: large-scale arcs or spiral arms, localized velocity kinks, and/or multiple faints arcs that appear like filamentary structures on the disk surface. We find kinematic signatures that are consistent with planet wakes in six disks: AA Tau, SY Cha, J1842, J1615, LkCa 15 and HD 143006. Comparison with hydrodynamical and radiative transfer simulations suggests planets with orbital radii between 80 and 310\,au and masses between 1 and 5 M$_\mathrm{Jup}$. Additional kinematic substructures limit our ability to place tight constraints on the planet masses. When the inclination is favorable to separate the upper and lower surfaces (near 45$^\mathrm{o}$, i.e. in 7/15 disks), we always detect the vertical CO snowline and find that the $^{12}$CO freeze-out is partial in the disk midplane, with a depletion factor of $\approx 10^{-3}$ - $10^{-2}$ compared to the warm molecular layer. In these same seven disks, we also systematically detect evidence of CO desorption in the outer regions.
Figures
Figures from the paper (5 more)
Forward citations
Cited by 2 Pith papers
-
exoALMA VII: Benchmarking Hydrodynamics and Radiative Transfer Codes
Five hydrodynamics codes and two radiative transfer codes produce consistent planet-driven kinematic signatures in synthetic observations, allowing reliable planet location retrieval.
-
Extending dynamical mass measurements: probing GI as a possible origin of mm-dust spirals
Dynamical rotation-curve fits give M_disk ≈ 0.30 M_sun for HD 97048 and ≈ 0.21 M_sun for WaOph 6, and indicate disks with mm-dust spirals have systematically lower Toomre Q.
Reference graph
Works this paper leans on
-
[1]
Allard, F., Homeier, D., & Freytag, B. 2012, Phil. Trans. Roy. Soc. A, 370, 2765, doi: 10.1098/rsta.2011.0269
arXiv 2012
-
[2]
Avenhaus, H., Quanz, S. P., Garufi, A., et al. 2018, ApJ, 863, 44, doi: 10.3847/1538-4357/aab846
- [3]
-
[4]
2021, ApJ, 912, 56, doi: 10.3847/1538-4357/abe45e
Bae, J., Teague, R., & Zhu, Z. 2021, ApJ, 912, 56, doi: 10.3847/1538-4357/abe45e
-
[5]
Ballabio, G., Nealon, R., Alexander, R. D., et al. 2021, MNRAS, 504, 888, doi: 10.1093/mnras/stab922
- [6]
-
[7]
2015, A&A, 578, L6, doi: 10.1051/0004-6361/201526011
Benisty, M., Juhasz, A., Boccaletti, A., et al. 2015, A&A, 578, L6, doi: 10.1051/0004-6361/201526011
-
[8]
2017, ApJ, 840, 60, doi: 10.3847/1538-4357/aa696c
Boehler, Y., et al. 2017, ApJ, 840, 60, doi: 10.3847/1538-4357/aa696c
Show all 65 references
-
[9]
J., & Pinte, C
Bollati, F., Lodato, G., Price, D. J., & Pinte, C. 2021, MNRAS, 504, 5444, doi: 10.1093/mnras/stab1145
2021 doi
-
[10]
F., Doty, S
Bruderer, S., van Dishoeck, E. F., Doty, S. D., & Herczeg, G. J. 2012, A&A, 541, A91, doi: 10.1051/0004-6361/201118218
2012 doi
-
[11]
Byrne, P. B. 1986, Irish Astronomical Journal, 17, 294
1986
-
[12]
J., Pinte, C., et al
Calcino, J., Price, D. J., Pinte, C., et al. 2023, MNRAS, 523, 5763, doi: 10.1093/mnras/stad1798
2023 doi
-
[13]
2022, ApJL, 929, L25, doi: 10.3847/2041-8213/ac64a7
Calcino, J., et al. 2022, ApJL, 929, L25, doi: 10.3847/2041-8213/ac64a7
2022 doi
-
[14]
J., Price, D
Calcino, J., Norfolk, B. J., Price, D. J., et al. 2024, MNRAS, 534, 2904, doi: 10.1093/mnras/stae2233 CASA Team, Bean, B., Bhatnagar, S., et al. 2022, PASP, 134, 114501, doi: 10.1088/1538-3873/ac9642
2024 doi
-
[15]
2019, ApJL, 883, L41, doi: 10.3847/2041-8213/ab4425
Casassus, S., & P´ erez, S. 2019, ApJL, 883, L41, doi: 10.3847/2041-8213/ab4425
2019 doi
-
[16]
2020, MNRAS, 491, 504, doi: 10.1093/mnras/stz2938
Cuello, N., Louvet, F., Mentiplay, D., et al. 2020, MNRAS, 491, 504, doi: 10.1093/mnras/stz2938
2020 doi
-
[17]
M., & Testi, L
Curone, P., Facchini, S., Andrews, S. M., & Testi, L. 2025, ApJL, exoALMA D’Alessio, P., Cant´ o, J., Hartmann, L., Calvet, N., &
2025
-
[18]
1999, ApJ, 511, 896, doi: 10.1086/306704 de Boer, J., Salter, G., Benisty, M., et al
Lizano, S. 1999, ApJ, 511, 896, doi: 10.1086/306704 de Boer, J., Salter, G., Benisty, M., et al. 2016, A&A, 595, A114, doi: 10.1051/0004-6361/201629267 de Gregorio-Monsalvo, I., M´ enard, F., Dent, W., et al. 2013, A&A, 557, A133
1999 doi
-
[19]
P., Isella, A., Andrews, S
Dullemond, C. P., Isella, A., Andrews, S. M., Skobleva, I., & Dzyurkevich, N. 2020, A&A, 633, A137
2020
-
[20]
M., Simon, J
Flaherty, K., Hughes, A. M., Simon, J. B., et al. 2020, ApJ, 895, 109, doi: 10.3847/1538-4357/ab8cc5
2020 doi
-
[21]
2025, ApJL, exoALMA
Galloway-Sprietsma, M., Bae, J., & Izquierdo, A. 2025, ApJL, exoALMA
2025
-
[22]
2025, ApJL, exoALMA
Gardner, C., Isella, A., Hui, L., & Shengtai, L. 2025, ApJL, exoALMA
2025
-
[23]
2021, MNRAS, 504, 782, doi: 10.1093/mnras/stab800
Garg, H., Pinte, C., Christiaens, V., et al. 2021, MNRAS, 504, 782, doi: 10.1093/mnras/stab800
2021 doi
-
[24]
2024, A&A, 685, A52, doi: 10.1051/0004-6361/202244005
Ginski, C., Garufi, A., Benisty, M., et al. 2024, A&A, 685, A52, doi: 10.1051/0004-6361/202244005
2024 doi
-
[25]
2020, ApJ, 904, 148, doi: 10.3847/1538-4357/abac17
Hall, C., Dong, R., Teague, R., et al. 2020, ApJ, 904, 148, doi: 10.3847/1538-4357/abac17
2020 doi
-
[26]
J., et al
Hammond, I., Christiaens, V., Price, D. J., et al. 2022, MNRAS, 515, 6109, doi: 10.1093/mnras/stac2119 exoALMA channel maps 15
2022 doi
-
[27]
2025, ApJL, exoALMA
Hardiman, C., Price, D., & Pinte, C. 2025, ApJL, exoALMA
2025
-
[28]
Izquierdo, A. F. 2025, ApJL, exoALMA
2025
-
[29]
F., Stadler, J., Bae, J., et al
Izquierdo, A. F., Stadler, J., Bae, J., et al. 2025, ApJL, exoALMA
2025
-
[30]
J., Teague, R., Loomis, R
Law, C. J., Teague, R., Loomis, R. A., et al. 2021, ApJS, 257, 4, doi: 10.3847/1538-4365/ac1439
2021 doi
-
[31]
J., Crystian, S., Teague, R., et al
Law, C. J., Crystian, S., Teague, R., et al. 2022, ApJ, 932, 114
2022
-
[32]
2023, MNRAS, 518, 4481, doi: 10.1093/mnras/stac3223
Lodato, G., Rampinelli, L., Viscardi, E., et al. 2023, MNRAS, 518, 4481, doi: 10.1093/mnras/stac3223
2023 doi
-
[33]
2025, ApJL, exoALMA
Longarini, C., Lodato, G., Rosotti, G., & Andrews, S. 2025, ApJL, exoALMA
2025
-
[34]
2021, ApJL, 920, L41, doi: 10.3847/2041-8213/ac2df6
Longarini, C., Lodato, G., Toci, C., et al. 2021, ApJL, 920, L41, doi: 10.3847/2041-8213/ac2df6
2021 doi
-
[35]
2025, ApJL, exoALMA
Loomis, R., & exoALMA. 2025, ApJL, exoALMA
2025
-
[36]
2022, MNRAS, 510, 1248, doi: 10.1093/mnras/stab3440
Martinez-Brunner, R., Casassus, S., P´ erez, S., et al. 2022, MNRAS, 510, 1248, doi: 10.1093/mnras/stab3440
2022 doi
-
[37]
A., Hashimoto, J., et al
Muto, T., Grady, C. A., Hashimoto, J., et al. 2012, ApJL, 748, L22, doi: 10.1088/2041-8205/748/2/L22
2012 doi
-
[38]
J., Pinte, C., Calcino, J., et al
Norfolk, B. J., Pinte, C., Calcino, J., et al. 2022, ApJL, 936, L4, doi: 10.3847/2041-8213/ac85ed ¨Oberg, K. I., Facchini, S., & Anderson, D. E. 2023, ARA&A, 61, 287 Paneque-Carre˜ no, T., Miotello, A., van Dishoeck, E. F., et al. 2023, A&A, 669, A126, doi: 10.1051/0004-6361/2...
2022 doi
-
[39]
2025, exoALMA X
Pinte, C. 2025, exoALMA X. Data Products, V1, Harvard Dataverse, doi: 10.7910/DVN/H5QUQT
2025 doi
-
[40]
2006, A&A, 459, 797, doi: 10.1051/0004-6361:20053275
Pinte, C., M´ enard, F., Duchˆ ene, G., & Bastien, P. 2006, A&A, 459, 797, doi: 10.1051/0004-6361:20053275
2006 doi
-
[41]
2023a, in Astronomical Society of the Pacific Conference Series, Vol
Pinte, C., Teague, R., Flaherty, K., et al. 2023a, in Astronomical Society of the Pacific Conference Series, Vol. 534, Protostars and Planets VII, ed. S. Inutsuka, Y. Aikawa, T. Muto, K. Tomida, & M. Tamura, 645, doi: 10.48550/arXiv.2203.09528
-
[42]
2009, A&A, 498, 967, doi: 10.1051/0004-6361/200811555
Pinte, C., et al. 2009, A&A, 498, 967, doi: 10.1051/0004-6361/200811555
2009 doi
-
[43]
J., M´ enard, F., et al
Pinte, C., Price, D. J., M´ enard, F., et al. 2018b, ApJL, 860, L13, doi: 10.3847/2041-8213/aac6dc
-
[44]
2019, Nature Astronomy, 3, 1109, doi: 10.1038/s41550-019-0852-6
Pinte, C., van der Plas, G., M´ enard, F., et al. 2019, Nature Astronomy, 3, 1109, doi: 10.1038/s41550-019-0852-6
2019 doi
-
[45]
J., M´ enard, F., et al
Pinte, C., Price, D. J., M´ enard, F., et al. 2020, ApJL, 890, L9, doi: 10.3847/2041-8213/ab6dda
2020 doi
-
[46]
J., et al
Pinte, C., Hammond, I., Price, D. J., et al. 2023b, MNRAS, 526, L41, doi: 10.1093/mnrasl/slad010
-
[47]
J., Wurster, J., Tricco, T
Price, D. J., Wurster, J., Tricco, T. S., et al. 2018, PASA, 35, e031, doi: 10.1017/pasa.2018.25
2018 doi
-
[48]
Qi, C., & Wilner, D. J. 2024, ApJ, 977, 60, doi: 10.3847/1538-4357/ad8d55
2024 doi
-
[49]
Rafikov, R. R. 2002, ApJ, 569, 997, doi: 10.1086/339399
2002 doi
-
[50]
2024, A&A, 686, A264, doi: 10.1051/0004-6361/202449583
Ragusa, E., Lynch, E., Laibe, G., Longarini, C., & Ceppi, S. 2024, A&A, 686, A264, doi: 10.1051/0004-6361/202449583
2024 doi
-
[51]
2018, A&A, 611, A74, doi: 10.1051/0004-6361/201732016
Reggiani, M., Christiaens, V., Absil, O., et al. 2018, A&A, 611, A74, doi: 10.1051/0004-6361/201732016
2018 doi
-
[52]
B., Benisty, M., Ginski, C., et al
Ren, B. B., Benisty, M., Ginski, C., et al. 2023, A&A, 680, A114, doi: 10.1051/0004-6361/202347353
2023 doi
-
[53]
A., Andrews, S
Rosenfeld, K. A., Andrews, S. M., Hughes, A. M., Wilner, D. J., & Qi, C. 2013, ApJ, 774, 16
2013
-
[54]
2020, ApJL, 904, L18, doi: 10.3847/2041-8213/abc704
Pinte, C. 2020, ApJL, 904, L18, doi: 10.3847/2041-8213/abc704
2020 doi
- [55]
-
[56]
Stadler, J., Benisty, M., & Winter, A. J. 2025, ApJL, exoALMA
2025
-
[57]
2023, A&A, 670, L1, doi: 10.1051/0004-6361/202245381
Stadler, J., Benisty, M., Izquierdo, A., et al. 2023, A&A, 670, L1, doi: 10.1051/0004-6361/202245381
2023 doi
-
[58]
C., & Gahm, G
Stempels, H. C., & Gahm, G. F. 2004, A&A, 421, 1159, doi: 10.1051/0004-6361:20034502
2004 doi
-
[59]
2021, ApJS, 257, 18, doi: 10.3847/1538-4365/ac1438
Teague, R., et al. 2021, ApJS, 257, 18, doi: 10.3847/1538-4365/ac1438
2021 doi
-
[60]
J., Price, D
Verrios, H. J., Price, D. J., Pinte, C., Hilder, T., & Calcino, J. 2022, ApJL, 934, L11, doi: 10.3847/2041-8213/ac7f44
2022 doi
-
[61]
C., & Draine, B
Weingartner, J. C., & Draine, B. T. 2001, ApJ, 548, 296, doi: 10.1086/318651
2001 doi
-
[62]
Woitke, P., Kamp, I., & Thi, W. F. 2009, A&A, 501, 383, doi: 10.1051/0004-6361/200911821
2009 doi
-
[63]
Yoshida, C. T. 2025, ApJL, exoALMA
2025
-
[64]
2025, ApJL, exoALMA 16 Pinte et al
Zawadzki, B., & Czekala, I. 2025, ApJL, exoALMA 16 Pinte et al. ACKNOWLEDGMENTS This paper makes use of the following ALMA data: ADS/JAO.ALMA#2021.1.01123.L. ALMA is a partnership of ESO (representing its member states), NSF (USA) and NINS (Japan), together with NRC (Canada), ...
2025
-
[65]
101002188)
DF, JS have received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (PROTOPLANETS, grant agreement No. 101002188). Computations by JS have been performed on the ‘Mesocentre SIGAMM’ machine, hosted by O...
2020
Reviewed August 16, 2026 · model on record in the stance chip above.
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