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Dr Bertram Bitsch (University College Cork, Ireland)25/03/2026, 10:10Oral contribution
Planets form in protoplanetary discs surrounding newly formed stars, where dust
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grains clump and form km-sized planetesimals. As the dust grains start to grow to mm-cm
sized pebbles, they drift inwards very rapidly due to the gas drag within the disc. As the
pebbles drift inwards towards the hotter disc regions, they can evaporate and enrich the
inner disc with their vapor to largely... -
Claudia Danti (Center for Star and Planet Formation, University of Copenhagen, Denmark)25/03/2026, 10:40Oral contribution
Exoplanetary demographic statistics shows that super-Earths are the most
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abundant exoplanets, orbiting approximately every other solar-like star. In our own solar system, however, the inner terrestrial planets did not grow beyond Earth in mass. A possible explanation could be provided by the presence of gas giants in our own system, that might have influenced the growth of the inner... -
Matthew Doty (Rice University, USA)25/03/2026, 11:30Oral contribution
Understanding and testing possible formation mechanisms is crucial to
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understanding the history of planetary systems. While observationally there is a prevalence of evenly sized and spaced systems (“peas-in-a-pod” - Weiss et. al 2018), there is also an observational trend between the presence of a Cold Jupiter and inner system non-uniformity (He et. al 2023). Recent work explored in Best et.... -
Dr Keming Zhang (Massachusetts Institute of Technology)25/03/2026, 11:45Oral contribution
I make the case for q < 0.02 as a working definition for giant planets based on their formation via core accretion. Analyzing microlensing surveys sensitive to giant planets on 1–10 au orbits, my recent work (Zhang 2025; ApJL 995, L55) showed that the giant-planet mass-ratio distribution follows a power law that is sharply truncated at q = 0.017–0.02 (95% CI). Similar mass-ratio boundaries are...
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