dc.contributor
Balduin, Alexander
dc.creator
Kruijer, Thomas S.
dc.creator
Burkhardt, Christoph
dc.creator
Thorsten Kleine
dc.date.accessioned
2023-10-18T09:02:05Z
dc.date.available
2023-10-18T09:02:05Z
dc.identifier
https://doi.org/10.35003/LDLIYX
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/41171
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-40892
dc.description
Jupiter is the most massive planet of the Solar System and its presence had an immense effect on the dynamics of the solar accretion disk. Knowing the age of Jupiter, therefore, is key for understanding how the Solar System evolved toward its present-day architecture. However, although models predict that Jupiter formed relatively early, until now, its formation has never been dated. Here we show through isotope analyses of meteorites that Jupiter’s solid core formed within only ∼1 My after the start of Solar System history, making it the oldest planet. Through its rapid formation, Jupiter acted as an effective barrier against inward transport of material across the disk, potentially explaining why our Solar System lacks any super-Earths.
dc.subject
Earth and Environmental Sciences
dc.title
Replication Data for: Age of Jupiter inferred from the distinct genetics and formation times of meteorites.
dcterms.accessRights.openaire
metadata only access