Two related studies report JWST/MIRI spectroscopy of protoplanetary disks in the Upper Scorpius association, which is older than many previous JWST/MIRI targets. One analysis observes 14 disks in Upper Scorpius (about 5–10 million years) and models their inner-disk gas with slab emission under local thermal equilibrium. It finds that roughly half show detectable molecular emission beyond H2 (including H2O, CO2, HCN, C2H2 and H2), while the other half are molecular-poor and show no molecular lines other than H2. When combined with additional Upper Scorpius data from the AGE-PRO program, the studies find lower detection rates and systematically lower line luminosities for major molecular species than in younger (about 1–3 million years) comparison disks, with different scaling against accretion luminosity. The second study presents JWST/MIRI MRS results for 10 disks aged about 2–6 million years, finding large diversity in chemical compositions and a strong reduction in water: water luminosities are lower by factors of about 10 to 1000. Both works interpret the trends as evidence for chemical evolution in the inner disk, with cooler emitting layers, reduced inner-disk molecular gas masses, and indications of elevated inner-disk C/O in older systems.
JWST/MIRI finds declining molecular gas and water in older Upper Scorpius disks
Two related studies report JWST/MIRI spectroscopy of protoplanetary disks in the Upper Scorpius association, which is older than many previous JWST/MIRI targets. One analysis observes 14 disks in Uppe...
- JWST/MIRI spectroscopy targets disks in Upper Scorpius (ages roughly 2–10 million years) and compares them with younger (~1–3 million year) systems.
- Older Upper Scorpius disks show reduced detection rates and systematically lower line luminosities for major molecular species compared with younger disks.
- Water emission weakens substantially in older disks, with water luminosities reported as lower by factors of about 10–1000.
- Some older disks are molecular-poor, showing little or no molecular emission other than H2.
- Models and comparisons suggest inner-disk chemical evolution, including cooler emitting molecular gas and possible increases in inner C/O ratios in older systems.
arXiv:2606.27477v1 Announce Type: new Abstract: We present JWST/MIRI spectroscopy of 14 disks in the older (~5-10 Myr) Upper Scorpius (USco) association and use slab of gas in local thermal equilibrium to infer basic gas properties. We find that half of these disks are molecular rich, with detections of H$_2$O, CO$_2$, HCN, C$_2$H$_2$, and H$_2$, while the other half are molecular poor, showing no molecular emission other than H$_2$. We further combine this sample with 10 other USco disks from the AGE-PRO program and compare the combined older sample to young (~1-3 Myr) JDISCS Cycle~1 systems, which are analyzed in a similar manner. We find that USco disks have lower detection rates of major molecular species but a significantly higher detection rate of rarer C-bearing molecules such as C$_4$H$_2$. At a given accretion luminosity, molecular line luminosities are systematically lower in USco than in young disks, and the scaling relations with accretion luminosity differ between the two populations. Moreover, we find that about half of the older disks, preferentially the millimeter faint, and likely more compact disks, have observable mass ratios of C- to O-bearing molecules that are higher than the maximum values in the young sample. These results point to reduced inner-disk molecular gas masses, cooler emitting layers, and higher inner gas C/O ratios in older disks, the latter being consistent with pebble drift. Taken together, our findings provide evidence for chemical evolution of inner disk gas from young to older systems, with important implications for the accretion of primordial planetary atmospheres.
2 hours agoarXiv:2606.27476v1 Announce Type: new Abstract: Tracing the chemical evolution of protoplanetary disks over time requires observations of disks at different ages. However, most JWST/MIRI surveys published to date have targeted younger ($\sim$1-3 Myr) rather than older systems. We present the results of a JWST/MIRI MRS survey of the inner regions of 10 protoplanetary disks (ages $\sim$2-6 Myr, spectral types M0-M4.5) in the Upper Scorpius region previously characterized by the ALMA AGE-PRO large program. Using MCMC slab modeling, we fit to a wide variety of detected molecules, including H$_2$O, CO, C$_2$H$_2$, $^{13}$CCH$_2$, HCN, HC$_3$N, CO$_2$, $^{13}$CO$_2$, C$_2$H$_6$, C$_4$H$_2$, and OH, as well as C$_6$H$_6$, CH$_3$, and H$_2$ visually. We classify each disk along two independent axes-a Water Classification based on H$_2$O line luminosity (Water-Rich, Water-Poor, or Water-Absent) and a Chemotype based on the dominant non-water chemistry (Organic-Rich, CO$_2$-Dominated, or Molecule-Absent)-and find an unexpectedly high diversity of distinct chemical compositions within our population. We leverage the heterogeneity of detected molecules in our sample to present new characteristic "diagnostic" wavelength regions for most species. We find that carbon-based molecules consistently exhibit markedly lower excitation temperatures ($\lesssim$300 K) compared to younger ($\sim$1-3 Myr) star-forming regions ($\sim$600-1000 K), hinting at relatively colder molecular reservoirs. We also determine that Upper Scorpius disks show systematically lower water luminosities by factors of 10-1000. In particular, disks with strong carbon-based molecular features but no observed H$_2$O defy expectations of an inner-disk dust cavity or a low ($\lesssim3$) $R_{\rm gas}/R_{\rm dust}$ ratio, instead suggesting that the presence of a strong outer-disk dust trap largely controls the chemical outcome of the terrestrial planet-forming region.
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