Procompsognathus triassicus E. Fraas, 1913

Sues, Hans-Dieter & Schoch, Rainer R., 2025, Synopsis of the Triassic reptiles from Germany, Fossil Record 28 (2), pp. 411-483 : 411-483

publication ID

https://doi.org/10.3897/fr.28.164405

publication LSID

lsid:zoobank.org:pub:E2366C87-D1C3-4F5A-A21D-1A7A5D49BB8F

DOI

https://doi.org/10.5281/zenodo.17824187

persistent identifier

https://treatment.plazi.org/id/3D65E7E6-3D84-5767-89D5-4F1295624B59

treatment provided by

by Pensoft

scientific name

Procompsognathus triassicus E. Fraas, 1913
status

 

Procompsognathus triassicus E. Fraas, 1913

Holotype.

SMNS 12591 , partial postcranial skeleton comprising 14 dorsal and 13 caudal vertebrae, rib fragments, right scapula and coracoid, left radius, ulna, and three incomplete metacarpals, parts of both pubes, left femur, fragment of left tibia, and right hindlimb (Fig. 19 C View Figure 19 ). None of the cranial material historically assigned to Procompsognathus triassicus belongs to this taxon ( Sereno and Wild 1992; Spiekman 2023).

Type locality.

“ Weisser Steinbruch ” near Pfaffenhofen, Heilbronn district, Baden-Württemberg.

Type horizon.

Middle Stubensandstein (S 2), Löwenstein Formation. Age: Late Triassic (Norian: Lacian-Alaunian).

Diagnosis.

Distinguished by the following combination of features: sigmoidal trochanteric shelf (shared with Coelophysis bauri ); preacetabular process of ilium deep dorsoventrally; prominent supraacetabular crest; and pubis flat anteroposteriorly and lacking distinct ‘ foot’ ( Ostrom 1981; Sereno and Wild 1992).

Comments.

Procompsognathus triassicus is closely related to Coelophysis bauri from Upper Triassic (Rhaetian) Chinle Formation of New Mexico and Segisaurus halli from the Lower Jurassic (Pliensbachian-Toarcian) Navajo Sandstone of Arizona ( Sereno and Wild 1992).

References.

E. Fraas (1913), F. Huene (1921 b, 1932 b), Ostrom (1981), Sereno and Wild (1992), Rauhut and Hungerbühler (2000), Spiekman (2023).

SMNS

Staatliches Museum fuer Naturkund Stuttgart