A temperate Earth-sized planet with tidal heating transiting an M6 star.
Merrin S PetersonBjörn BennekeKaren CollinsCaroline PiauletIan J M CrossfieldMohamad Ali-DibJessie L ChristiansenJonathan GagnéJackie FahertyEdwin S KiteCourtney DressingDavid CharbonneauFelipe MurgasMarion CointepasJose Manuel AlmenaraXavier BonfilsStephen KaneMichael W WernerVaroujan GorjianPierre-Alexis RoyAvi ShporerFrancisco J PozuelosQuentin Jay SociaRyan CloutierJeremy DietrichJonathan IrwinLauren WeissWilliam WaalkesZach Berta-ThomsonThomas M Evans-SomaDaniel ApaiHannu ParviainenEnric PalleNorio NaritaAndrew W HowardDiana DragomirKhalid BarkaouiMichaël GillonEmmanuel JehinElsa DucrotZouhair BenkhaldounAkihiko FukuiMayuko MoriTaku NishiumiKiyoe KawauchiGeorge R RickerDavid W LathamJoshua N WinnSara SeagerHoward IsaacsonAlex BixelAidan GibbsJon M JenkinsJeffrey C SmithJose Perez ChavezBenjamin V RackhamThomas K HenningPaul GaborWen-Ping ChenNestor EspinozaEric L N JensenKevin I CollinsRichard P SchwarzDennis M ContiGavin WangJohn F KielkopfShude MaoKeith HorneRamotholo SefakoSamuel N QuinnDan MoldovanMichael FausnaughGábor FűűrészThomas BarclayPublished in: Nature (2023)
Temperate Earth-sized exoplanets around late-M dwarfs offer a rare opportunity to explore under which conditions planets can develop hospitable climate conditions. The small stellar radius amplifies the atmospheric transit signature, making even compact secondary atmospheres dominated by N 2 or CO 2 amenable to characterization with existing instrumentation 1 . Yet, despite large planet search efforts 2 , detection of low-temperature Earth-sized planets around late-M dwarfs has remained rare and the TRAPPIST-1 system, a resonance chain of rocky planets with seemingly identical compositions, has not yet shown any evidence of volatiles in the system 3 . Here we report the discovery of a temperate Earth-sized planet orbiting the cool M6 dwarf LP 791-18. The newly discovered planet, LP 791-18d, has a radius of 1.03 ± 0.04 R ⊕ and an equilibrium temperature of 300-400 K, with the permanent night side plausibly allowing for water condensation. LP 791-18d is part of a coplanar system 4 and provides a so-far unique opportunity to investigate a temperate exo-Earth in a system with a sub-Neptune that retained its gas or volatile envelope. On the basis of observations of transit timing variations, we find a mass of 7.1 ± 0.7 M ⊕ for the sub-Neptune LP 791-18c and a mass of [Formula: see text] for the exo-Earth LP 791-18d. The gravitational interaction with the sub-Neptune prevents the complete circularization of LP 791-18d's orbit, resulting in continued tidal heating of LP 791-18d's interior and probably strong volcanic activity at the surface 5,6 .