Ichnospecies: pandemicus LOCKLEY, 1989
Etymology:
Type: CU-MWC 186.5
Locality: Moab megastracksite site E, west side of Arches National Monument, Eastern Utah.
Horizon:
Biostratigraphy: Entrada-Summerville Transition zone.
Age: Oxfordian-Lower Kimmeridgian Stage, Lower-Middle Malm Epoch, Early Late Jurassic.
Material: Rubber mold and fiberglass replica of 5 consecutive footprints, and intervening rock surface from a single trackway of 13 consecutive steps.
Topotype: CU-MWC 186.2: From same surface at adjacent site G.
Paratypes:
Locality: Del Monte mines locality, north of Bullfrog, Utah.
Horizon: Upper part of the Summerville Formation.
Biostratigraphy:
Age: Late Jurassic.
Material:
CU-MWC 188.10, 188.13: natural casts of 3 tracks.
CU-MWC 188.14: Replica of a natural cast.
Referred material:
Locality: Cactus Park, Mesa County, Colorado.
Horizon: Upper Summerville Formation.
Biostratigraphy:
Age: Late Jurassic.
Material:
CU-MWC 188.24: Impression of theropod tracks.
CU-MWC 188.63: Impression of theropod tracks.
Locality: Northwestern Oklahoma.Horizon: ?Bell Ranch Formation.
Biostratigraphy:
Age: Late Jurassic.
Material:
Number: Not given:
Locality: Fuentesalvo, north of Soria, La Rioja Province, Cameros Basin, Spain.Horizon: Oncala Group.
Biostratigraphy:
Age: ?Late Jurassic – Early Cretaceous.
Material:
Number: Not given:
Locality: Kugitang Suite, Khodja-Pil Ata, Turkmenistan.Horizon:
Biostratigraphy:
Age: Oxfordian-Kimmeridgian Stage, Lower-Middle Malm Epoch, Early Late Jurassic.
Material:
Number: Not given:
= cf. Therangospodus pandemicus PAZOS, LAZO, TUNIK, MARSICANO, FERNANDEZ, & AGUIRRE-URRETA, 2012
Locality: Neuquen Basin, Patagonia, Argentina.
Horizon: Agrio Formation.
Biostratigraphy:
Age: Early Cretaceous.
Material:
In situ:
Tracksite I (Mina la Continental): Trackways.
Tracksite II (Cerro Rayoso): Tracks.
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