No. 5 — Triassic Reptile Footprint Faunules from Milford, New Jersey By Donald Baied CONTENTS Page FOREWORD 449 GEOLOGICAL OCCURRENCE 451 SYSTEMATIC DESCRIPTIONS 452 THEROPODA Grallator sulcatus Baird, n. sp 453 Anchisauripus milfordetisis (Bock) 462 Anchisauriprts parallelus (Hitchcock) 464 Genus incertum 465 Taxonomy of theropod footprints 467 PSEUDOSUCHIA Chirotherium parvum (G. H. Hitchcock) 473 Chirotherium ey.ermani Baird, n. sp. 479 PHYTOSAURIA Apatopus lineatus (Bock), n. gen. 486 LACERTOIDEA INCERTAE SEDIS Rhynchosauroides hyperiates Baird, n. sp 494 Rhynchosauroides sp. 497 CORRELATIVE AGE OF THE MILFORD FAUNULES 501 REPTILES OF THE BRUNSWICK FORMATION 503 APPENDIX I : The nature of Otouphepm 507 APPENDIX II : Brontozoum 509 SUMMARY 511 REFERENCES 514 FOREWORD In a recent paper Wilhelm Bock (1952) has described a num-ber of important faunules of fossil footprints from various horizons and localities in the Upper Triassic (Middle Keuper) of the Newark Basin. One of these faunules, found in a gray sandstone layer of the upper Brunswick formation near Milford, New Jersey, had been discussed in the literature as early as 1886 ; but until 1952 only its dominant species, Chirotherium parvum, had been adequately described. In the same paper
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