Similar mean orbital elements led the discoverers to postulate a common origin for the group in a break up of a larger body.[1]
The diagram illustrates the Gallic group in relation to other irregular satellites of Saturn. The eccentricity of the orbits is represented by the yellow segments (extending from the pericentre to the apocentre) with the inclination represented on Y axis.
The four members of the group are (in order of increasing distance from Saturn):
The group was later found to be physically homogenous, all satellites displaying light-red colour (colour indices B − V = 0.91 and V − R = 0.48)[2]
and similar infrared indices [3]
Remarkably, recent observations revealed that the largest member of the group, Albiorix, displays actually two different colours: one compatible with Eriapo and Tarvos, and another less red. Instead of the common progenitor, it was postulated that Tarvos and Erriapus could be fragments of Albiorix, leaving a large, less red crater.[4]
Such an impact would require a body with the diameter in excess of 1 km and relative velocity close to 5 km/s, resulting in a large crater with the radius of 12 km. Numerous, very large craters observed on Phoebe, prove the existence of such collisions in the Saturnian system's past.
↑B. Gladman, P. Nicholson, J. Burns, JJ Kavelaars, B. G. Marsden, M. Holman, T. Grav et al.. Discovery of 12 satellites of Saturn exhibiting orbital clustering., Nature, 412 (2001), p. 163
↑ Grav, Tommy; Holman, Matthew J.; Gladman, Brett J.; Aksnes, Kaare Photometric survey of the irregular satellites, Icarus, 166,(2003), pp. 33-45. Preprint
↑
Tommy Grav and Matthew J. HolmanNear-Infrared Photometry of the Irregular Satellites of Jupiter and Saturn,The Astrophysical Journal, 605, (2004), pp. L141–L144 Preprint
↑
Tommy Grav and James Bauer
A deeper look at the colors of Saturnian irregular satellites, Preprint