Cenozoic continental deposits of the Bugti Hills crop out South of the Sulaiman Range in Balochistan, Pakistan, and they have been renowned since Vickary (1846) for their exceptionally rich vertebrate-bearing Miocene localities. This led G.E. Pilgrim (Geological Survey of India) then C. Foster-Cooper (University of Cambridge) to conduct expeditions in the beginning of the 20th century. More recent expeditions in the late 1990s have reported the occurrence of successive fossiliferous horizons spanning the Eocene–Pleistocene interval (Welcomme et al., 1997, 2001; Welcomme and Ginsburg, 1997). Fossil-yielding series around Dera Bugti document marine, coastal, then fluvio-lacustrine depositional environments during the Eocene, the earliest Oligocene, and the late Oligocene–Pleistocene intervals, respectively (Welcomme et al., 2001; Métais et al., 2009; Roddaz et al., 2011; Antoine et al., 2013). The most species-rich intervals, at least for mammals, are Oligocene and Miocene in age (Marivaux et al., 1999, 2001, 2002a, 2002b, 2005; Antoine and Welcomme, 2000; Antoine et al., 2003, 2004, 2010, 2013; Métais et al., 2003, 2006, 2009, 2017; Marivaux and Welcomme, 2003; Orliac et al., 2009, 2010). As for crocodylians, fossil remains were initially described from the Bugti Hills by Pilgrim (1908, 1912), but their precise stratigraphic provenance has not been recorded. Most of those fossils are quite fragmentary and they consist of large tomistomine skull fragments (Martin, 2018) formerly referred to species of Gavialis (Pilgrim, 1908, 1912). Together with these remains, Crocodilus bugtiensis Pilgrim, 1908 was erected from a left maxilla and associated skull fragments of remarkable size found at Pishi Nala. Since its formal description four years later (Pilgrim, 1912), the taxon has been briefly mentioned from several levels in the Bugti Hills (Welcomme et al., 1997) but no detailed account has been given ever since. Here, we describe partial, yet diagnostic, mandibular elements of a large crocodyloid recovered from upper Oligocene deposits of the Bugti Hills, which are morphologically compatible with the skull elements described by Pilgrim (1912). This material was collected from a well-identified Oligocene horizon within the framework of the field campaigns that took place in Baluchistan between 1995 and 2000. We also report a partial mandible collected in the 1920s from Baluchistan but with no provenance data. Finally, we mention the presence of toothmarks on associated megaherbivore remains.