Dawes Review. The tidal downsizing hypothesis of planet formation
Sergei Nayakshin (U of Leicester, UK)

TL;DR
Tidal Downsizing offers a comprehensive model of planet formation that explains various exoplanet and debris disc observations, contrasting with Core Accretion, and predicts specific correlations with host star metallicity and disc properties.
Contribution
This paper summarizes detailed simulations and develops a predictive planet formation model based on Tidal Downsizing, offering new interpretations of planetary system observations.
Findings
Debris discs from Tidal Downsizing have larger inner edges (>1 au) and are less massive.
Massive cores are predicted to be rock-dominated, not ice.
Certain exoplanet and debris disc features support Tidal Downsizing over Core Accretion.
Abstract
Tidal Downsizing is the modern version of the Kuiper (1951) scenario of planet formation. Detailed simulations of self-gravitating discs, gas fragments, dust grain dynamics, and planet evolutionary calculations are summarised here and used to build a predictive planet formation model and population synthesis. A new interpretation of exoplanetary and debris disc data, the Solar System's origins, and the links between planets and brown dwarfs is offered. This interpretation is contrasted with the current observations and the predictions of the Core Accretion theory. Observations that can distinguish the two scenarios are pointed out. In particular, Tidal Downsizing predicts that presence of debris discs, sub-Neptune mass planets, planets more massive than ~Jupiter masses and brown dwarfs should not correlate strongly with the metallicity of the host. For gas giants of …
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