Abstract

ABSTRACT Planet–planet scattering events can leave an observable trace of a planet’s migration history in the form of orbital misalignment with respect to the stellar spin axis, which is measurable from spectroscopic time-series taken during transit. We present high-resolution spectroscopic transits observed with ESPRESSO of the close-in super-Earth π Men c. The system also contains an outer giant planet on a wide, eccentric orbit, recently found to be inclined with respect to the inner planetary orbit. These characteristics are reminiscent of past dynamical interactions. We successfully retrieve the planet-occulted light during transit, and find evidence that the orbit of π Men c is moderately misaligned with the stellar spin axis with λ = − 24${_{.}^{\circ}}$0 ± 4${_{.}^{\circ}}$1 ($\psi = {26{_{.}^{\circ}} 9}^{+5{_{.}^{\circ}}8 }_{-4{_{.}^{\circ}}7 }$). This is consistent with the super-Earth π Men c having followed a high-eccentricity migration followed by tidal circularization, and hints that super-Earths can form at large distances from their star. We also detect clear signatures of solar-like oscillations within our ESPRESSO radial velocity time series, where we reach a radial velocity precision of ∼20 cm s−1. We model the oscillations using Gaussian processes (GPs) and retrieve a frequency of maximum oscillation, $\nu _\mathrm{max}{} = 2771^{+65}_{-60}\, \mu \mathrm{Hz}$. These oscillations make it challenging to detect the Rossiter–McLaughlin effect using traditional methods. We are, however, successful using the reloaded Rossiter–McLaughlin approach. Finally, in the appendix, we also present physical parameters and ephemerides for π Men c from a GP transit analysis of the full Transiting Exoplanet Survey Satellite Cycle 1 data.

Highlights

  • Perhaps one of the most surprising results from two decades of exoplanet research is that planet sizes between those of Earth and Neptune (1.5–2 R⊕) are the most likely outcome of planet formation (e.g. Borucki et al 2010; Batalha et al 2013), even when such planets are completely absent from our own Solar system

  • The paper is organized as follows: In Section 2, we present our analyses of the ESPRESSO data that include (i) modelling of the Rossiter–McLaughlin anomaly combined with a Gaussian process (GP) model for the asteroseismic activity and (ii) an independent analysis using the reloaded Rossiter–McLaughlin method

  • We show the GP-‘detrended’ π Men c transit light curve in Fig. 6, which is based on a combined fit of the six available Transiting Exoplanet Survey Satellite (TESS) sectors in Cycle 1

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Summary

Introduction

Perhaps one of the most surprising results from two decades of exoplanet research is that planet sizes between those of Earth and Neptune (1.5–2 R⊕) are the most likely outcome of planet formation (e.g. Borucki et al 2010; Batalha et al 2013), even when such planets are completely absent from our own Solar system. The currently operating Transiting Exoplanet Survey Satellite (TESS) survey (Ricker et al 2015) is expected to find ∼1000 additional super-Earths and miniNeptunes in its 2-yr nominal mission lifetime (Barclay, Pepper & Quintana 2018; Huang et al 2018a). For their abundance, there have been few observational constraints on their formation and dynamical evolution. Core accretion until isolation mass followed by a giant impact phase is unlikely to produce the observed super-Earth population (Hansen & Murray 2012; Schlichting 2014; Dawson, Lee & Chiang 2016), which points to another likely mechanism at work to explain the close-in superEarths. Due to strong gravitational perturbations produced by the binary orbital motion on to protoplanetary discs, planet formation is thought to only be possible at several au from the central binaries (e.g. Paardekooper et al 2012; Pierens, McNally & Nelson 2020) implying that the detected systems had to migrate in (Martin 2018; Pierens et al 2020)

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