Anand, A.; Spitzer, F.; Hopp, T.; Windmill, R.; Kruttasch, P.; Burkhardt, C.; Dauphas, N.; Greenwood, R.; Hofmann, B.; Mezger, K.et al.; Kleine, T.: Isotopic evidence for a common parent body of IIG and IIAB iron meteorites. Geochimica et Cosmochimica Acta 382, pp. 118 - 127 (2024)
Pape, J.; Zhang, B.; Spitzer, F.; Rubin, A. E.; Kleine, T.: Isotopic constraints on genetic relationships among group IIIF iron meteorites, Fitzwater Pass, and the Zinder pallasite. Meteoritics and Planetary Science 59, pp. 778 - 788 (2024)
Pape, J.; Zhang, B.; Spitzer, F.; Rubin, A. E.; Kleine, T.: Isotopic constraints on genetic relationships among group IIIF iron meteorites, Fitzwater Pass, and the Zinder pallasite. Meteoritics & Planetary Science, pp. 1 - 11 (2023)
Windmill, R. J.; Franchi, I. A.; Hellmann, J. L.; Schneider, J. M.; Fridolin, S.; Kleine, T.; Greenwood, R. C.; Anand, M.: Isotopic evidence for pallasite formation by impact mixing of olivine and metal during the first 10 million years of the Solar System. PNAS Nexus 1 (1) (2022)
Fridolin, S.; Burkhardt, C.; Pape, J.; Kleine, T.: Collisional mixing between inner and outer solar system planetesimals inferred from the Nedagolla iron meteorite. Meteoritics and Planetary Science 57, pp. 261 - 276 (2022)
The Uranian magnetic field is more expansive than previously thought, according to newly analyzed data from Voyager 2, making it easier to search for moons with oceans.
The Planetary Plasma Environments group (PPE) has a strong heritage in the exploration of planetary magnetospheres and space plasma interactions throughout the solar system. It has contributed instruments to several past missions that flew-by or orbited Jupiter (Galileo, Cassini, Ulysses). The PPE participates in the JUICE mission by contributing hardware and scientific expertise to the Particle Environment Package (PEP).