"Historical catalogue number";"New catalogue numbers";Locality;Details
"GPIT A (Old numbers PV-10975, PV-10976 Nm. I–II, PV-10977 Nm. 1–2, PV 10977 Nm. 3)";"GPIT-PV-60296 These specimens were referred to as GPIT A, and it is unclear if this is meant to be one individual, a composite mounted to illustrate one species or several specimens collected over time that tentatively belonged to the same species.";"Found in 1864 in the localities of Jächklinge, near Pfrondorf (Quenstedt 1864: p. 308) found by Mr. Revierförster Pfizenmayer. The field designation “Gecht” could also mean “Gechtbach”, which flows into “Tiefenbach” and most likely formed the Bradklinge.";"Originally mounted (UAT 678/73, von Huene 1907: Foreword, p. III) and consisted of a complete pelvis with most of the fore- and hindlimbs, an articulated partial sacrum and the dorsal series with ribs, and as far as the eighth dorsal vertebra (Quenstedt 1867: pl. 9, fig. 4–12; Quenstedt,1882–85: 178–180, fig. 60, pl. 13, figs. 5–13). The specimen was later illustrated in detail (von Huene 1907: 29–42, figs. 17–28, pl. 10, figs. 1–5, 7, Pls. 11–16, 102)."
"Taxonomic opinions";"Quenstedt used the name Zanclodon laevis Plieninger, 1846, but was later referred to as a new species, Zanclodon quenstedti Seeley, 1892 (see Koken 1900), then referred to as Plateosaurus quenstedti von Huene, 1905. According to Galton (1999, 2001a), the lack of diagnostic characters in the sacrum and the skull material made this a nomen dubium. However, due to the uncertainty of its provenance, it is not clear whether this number refers to a specimen."
"GPIT B";GPIT-PV-60293;"Found during a construction site at Roter Graben near Bebenhausen in 1870, when Forstrat Tscherning collected and sent them for study to Quenstedt (von Huene 1907: 127).";"The material comprises several vertebrae, metacarpals, manual phalanges, a pelvis, a partial femur, a partial tibia, several metatarsals, and pedal phalanges. It was mounted as part of the same hindleg notwithstanding the correct anatomy (von Huene 1907: 127–140: figs. 120–139, pl. 53, pl. 54, fig. 4, pl. 55, pl. 56, fig. 2)"
"Taxonomic opinions";"Referred to as Gresslyosaurus robustus von Huene, 1907"
"GPIT C = GPIT VII";GPIT-PV-30790;"It was discovered in 1881 by Jacob Hildenbrand from Ohmen when doing topographic prospections in Wüstenroth, southeast from Löwenstein.";"Quenstedt acquired it for the palaeontological collection in Tübingen; it was until 1901 that the material, which Hildebrand put inside a cement block (von Huene 1907: 138, pl. 56–59). Von Huene mounted it after he prepared and isolated the elements."
"Taxonomic opinions";"von Huene (1905) made specimen GPIT C the holotype of Pachysaurus ajax von Huene, 1905."
"GPIT D (Old numbers: PV 11210–11212, 11297–11316)";"GPIT-PV-60298 third sacral vertebra (= PV 11210). GPIT-PV-60173 to 60176 left metacarpals (= PV 11300) (von Huene 1907: pl. 61, fig. 2). GPIT-PV-60182 right humerus (= PV 11212) (von Huene 1907: pl. 63, fig. 1).";"It was discovered in 1864 and given the old number PV 11297, collected from a deep rift in Brandklinge, near Jächklinge. However, von Huene (1907: p. 146) stated this finding was done in the “late 1870s”. Currently, in the collection, it is difficult to determine which material belongs to GPIT D and which belongs to GPIT A, both obtained from similar localities.";"It consists of a third sacral vertebra, ribs (old number PV 11211, lost), both pectoral girdles and humeri, parts of the radius, left metacarpus and a fragment of an ilium and a tibia (von Huene 1907: 146–153, figs. 155–159, pl. 59, fig. 7, Pls. 60–63; Galton 1999). It is impossible to distinguish between the collection sites of Brandklinge and Jächklinge, and every collection element now has independent numbers. Von Huene (1907: p. 146) described them as “a large number of worthless fragments”."
"Taxonomic opinions";"Von Huene (1905) made specimen GPIT C the holotype of Pachysaurus magnus von Huene, 1905."
"GPIT E";GPIT-PV-60234–60236;"It was collected from the upper bone bed from the Obere Mühle, an outcrop of the Trossingen Formation, where von Huene organised an expedition in 1921–1923.";"Three metatarsals (von Huene 1932: pl. 12, fig. 11). GPIT E was found as a block, catalogued as “Block 98”, and consisted of three large metatarsal bones in a relatively poor preservation state (von Huene 1932). This includes a lost bone (block 98/4) that von Huene (1932, p. 111) interpreted as a phalanx, and Galton (2001b, p. 446, fig. 4f) interpreted as a calcaneum."
"Taxonomic opinions";"The large size of the metatarsals (mt. II being 52 cm long) was used as a condition to erect the species Pachysaurus giganteus von Huene, 1932."
"GPIT I (mounted individual)";GPIT-PV-30784;"Collected from the lower dinosaur bed, Obere Mühle.";"Complete skeleton with few elements missing (von Huene 1926: pl. 5, fig. 9, text-fig. 4; von Huene 1928: pl. 10, von Huene 1932: 141–160, pl. 24, fig. 1, 2, text-fig. 53)."
"Taxonomic opinions";"Von Huene (1932) referred the specimen to Plateosaurus quenstedti von Huene, 1905. Galton (2001b) placed it along with AMNH FARB 6810 as part of Plateosaurus longiceps Jaekel, 1913."
"GPIT I (stored skull)";GPIT-PV-30784;"Collected from the lower dinosaur bed, Obere Mühle";"The skull is not mounted but stored in the basement collection. It is partially articulated, but the skull roof collapsed over the left side (von Huene 1932: pl. 25). The mounted skulls are casts of SMNS 13200 and is used in GPIT-PV-30784 and GPIT-PV-30785."
"Taxonomic opinions";"Von Huene (1932) referred the specimen to Plateosaurus quenstedti. Galton (2001b) placed it along with AMNH FARB 6810 as part of Plateosaurus longiceps."
"GPIT II (composite of several individuals)";GPIT-PV-30785;"Collected from the lower dinosaur bed, Obere Mühle";"GPIT IIe.i refers to the dorsal 13–15, the sacrum, caudal vertebrae 1–42, pelvis with a closed obturator foramen), hindlimbs of mounted skeleton GPIT II (von Huene 1932: 166–174, fig. 14, pl. 25; fig. 15). GPIT IIq refers to some dorsal vertebrae mounted in the exhibit (von Huene 1932; fig. 14, pl. 5; Weishampel and Westphal 1986: fig. 3)."
"Taxonomic opinions";"GPIT II.e.i. was referred to P. erlenbergiensis von Huene, 1905 (von Huene 1932). GPIT IIq was referred to P. quenstedti (von Huene 1932). Galton (2001b) considered both species nomina dubia and does not give an opinion on the taxonomic placement for GPIT II. Nevertheless, in the literature, this composite is considered part of P. ‘engelhardti’."
"GPIT III";GPIT-PV-30786;"Collected from upper dinosaur bed, Obere Mühle";"Both ischia, a complete right hindlimb (von Huene 1932: pl. 41)."
"Taxonomic opinions";"The specimen was referred to as G. ‘robustus’, the same species given to GPIT B. The species was considered a junior synonym of P. ‘engelhardti’."
"GPIT IV";GPIT-PV-30787;"Collected from lower dinosaur bed, Obere Mühle";"The specimen includes a pelvis with the sacrum, part of the tail, left hindlimb, right fibula, partial foot, all articulated, and a partial forelimb with a mandible."
"Taxonomic opinions";"Von Huene (1932) referred it to as P. ‘plieningeri’ von Huene, 1905, whose holotype (SMNS 80664) was collected from the Knollenmergel of Degerloch in Stuttgart. A recent morphological study placed the specimen from Degerloch within the range of variability for P. trossingensis, which includes some elements of GPIT II (Lefevbre et al. 2020), GPIT I and SMNS 13200. Galton (2001b) considered P. ‘plieningeri’ as a nomen dubium. Here, we consider the elements found in articulation as the holotype of Tuebingosaurus n. gen."
"GPIT V";GPIT-PV-30788;"Collected from upper dinosaur bed, Obere Mühle";"Eight dorsals, incomplete third sacral vertebra, 13 caudal vertebrae, the distal two-thirds of the left humerus, the ventral half of the left ilium, both ischia and pubes, an almost complete left hindlimb (von Huene 1932: 105–111, pl. 12; Galton 2011: fig. 4e, 10e)."
;"Taxonomic opinions";"The specimen was made the holotype of Pachysaurus wetzelianus von Huene, 1932, and considered as a junior synonym of P. ‘engelhardti’ by Galton (1985c, 1990, 1992), but made a nomen dubium in Galton (2001b) due to the apparent poor preservation. The humerus is currently missing. GPIT V is also the largest specimen in the collection, with the hindlimb measuring about 3 meters long."
"GPIT VI";GPIT-PV-30789;"Collected from the lower dinosaur bed, Obere Mühle";"A left hindlimb with femur, tibia, fibula, distal tarsals, metatarsals and pedal phalanges."
"Taxonomic opinions";"It was referred to as P. ‘quenstedti’ in an unpublished drawing by von Huene."
"GPIT VII = GPIT C";"See GPIT C";"See GPIT C";"See GPIT C"