Identifies atomic and molecular species in GJ 436 b's atmosphere, suggesting notable iron abundance.
We aim to identify the presence of atomic and molecular species in the upper atmosphere of the warm Neptune-sized transiting planet GJ,436,b, which has a radiative equilibrium temperature of 690 K and a mass of 25.4 Using the transmission spectroscopy technique, we observed two full transits of GJ,436,b with the ESPRESSO spectrograph, covering the wavelength range from 3800 to 7880 A . We searched for traces of atomic (H, i , Li, i , Na, i , Mg, i , V, i , Cr, i , Fe, i , and Fe, ii ), along with molecular (TiO, VO) species by directly detecting planetary absorption features and by cross-correlating the planetary spectrum with theoretical spectra computed for each investigated species. i signal appears in the first transit (S/N = 3.4 ± 0.2) at a wind velocity of ∼ -18.6 km,s -1 , which is unexpectedly large for a cool planet. This weak signal is not present in the second transit and combined with its low significance, this suggests an origin in noise. In the less probable scenario where the feature is suppressed during the second transit by the higher stellar activity state, the T1 tentative signal peaks at 1300 K, which is above the equilibrium temperature of GJ,436,b. Ultimately, this result would imply a neutral iron abundance comparable to or exceeding that of the host star.
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Herrero-Cisneros et al. (2026) studied this question.
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