In 1974, Canadian amateur paleontologist Irene Vanderloh discovered the skeleton of a small theropod near
Steveville in Alberta. She showed it to
John Storer of the
Provincial Museum of Alberta, who brought it to the attention of
Hans-Dieter Sues. In 1978, Sues named and described the specimen as the type species
Saurornitholestes langstoni. The generic name is in reference to the
Saurornithoididae, due to the resemblance with this group that is today seen as part of the
Troodontidae, and combines their name with a Greek
lestes, "thief". The
specific name honours
Wann Langston, Jr.
Additional specimens Two more complete and larger partial skeletons (RTMP 88.121.39 and MOR 660), dozens of isolated bones, and scores of teeth are known from the badlands of
Dinosaur Provincial Park in Alberta; most of these are housed at the
Royal Tyrrell Museum of Palaeontology, in
Drumheller,
Alberta and remain undescribed. The Alberta and Montana remains are usually attributed to the single species
Saurornitholestes langstoni, though they come from a variety of rock formations indicating a wide span of time; for example, the
Oldman Formation (dated to about 77 million years ago but whether they represent
S. langstoni or a different, related species is unknown. Neonate-sized
Saurornitholestes fossils have been reported in the
scientific literature.
Saurornitholestes sullivani is known from the Hunter Wash fauna of the
Kirtland Formation in New Mexico, based on the frontal SMP VP-1270. It differs from
S. langstoni in the characters of the frontal. A well-preserved skeleton of
Saurornitholestes (specimen UALVP 55700) discovered in 2014 is currently under preparation by
University of Alberta paleontologists working in Japan. After examining the skull of that specimen, Currie and Evans announced in 2019 that the
Zapsalis teeth from the Dinosaur Park Formation represented the second premaxillary tooth of
S. langstoni.
Formerly assigned species In 2006,
Robert Sullivan named and described a second nominal species,
Saurornitholestes robustus, based on holotype SMP VP-1955, a left frontal. The specific name refers to the great thickness of this bone, the only trait in which the species is known to differ from
S. langstoni. The holotype was found in the Willow Wash fauna of the
Kirtland Formation in New Mexico, dated to about 73 million years ago. and a study published in 2014 took the conclusion a step further by demonstrating that
S. robustus was assignable to
Troodontidae based on similarities with troodontids. In 2026, Rivera-Sylva and colleagues tentatively assigned
S. robustus to their new genus
Xenovenator based on shared cranial anatomy, a conclusion supported by their
phylogenetic analyses. Possible indeterminate fossils are known from the
Hell Creek Formation in
Montana,
North Dakota, and
South Dakota, dated to about 66 million years ago. ==Description==