Planet Formation Solar System Protoplanetary Disks Exoplanets Beta Pictoris Stability Multi-Planetary Systems Protoplanetary Discs Planetary Formation Star Characteristics Orbital Dynamics Gas Giants Red Dwarf Stars Magnetosphere Multi-Planet Systems Super-Earths L 98-59 System Planetary Distances G-type Stars Super-Neptune Planets Planetary Characteristics Extrasolar Planets Binary Objects Binary Star Systems Habitable Zone Orbital Patterns HD 110067 Solar Systems Multiplanet system Planet Consumption Water Vapor Exoplanetary Atmospheres Metal Accretion Instability Consequences of Planetary Ingestion Ingestion Factors Dynamics Life Gas Dispersal Inner Planets Outer Planets Orbiting Planets Diversity Diverse Compositions Planetary Devouring Circumbinary Planets Formation Theories Kepler-725 System Kepler Space Telescope 14 Herculis System Development Satellite Dynamics Planetary Discovery Debris Discs Mutual Inclination TRAPPIST-1 Formation Small Bodies Habitability Moon Formation Moons Uranus Ring Systems Solar System Formation Young Stars Ejection Processes Star Systems Formation of Comets Rocky Planets Formation of Planets Planetary Evolution Planet Population Synthesis Planetary Nebulae Orbital Mechanics Kuiper Belt Objects 40 Eridani A System Atmosphere Orbit Red Giant Stars Resonance Epsilon Indi System Epsilon Indi Planetary Remnants Multiplanet Systems Red Dwarfs Formation Mechanisms Planet-Planet Occultations
Refractory sulfur provides a solid-growth tracer, pushing core-accretion models to higher masses at wider orbits.
