Spiclypeus (meaning "spike shield") is an extinct genus of chasmosaurine ceratopsian dinosaur known from the Late Cretaceous Judith River Formation (late Campanian stage) of Montana, United States.

In 2000, Bill D. Shipp, a nuclear physicist, bought the Paradise Point Ranch near the town of Winifred, in Fergus County. Believing that his land contained fossils, Shipp hired the local veteran fossil collector John C. Gilpatrick to explore the terrain together. On their first trip during an afternoon in September 2005, Shipp found the Spiclypeus specimen on his land in Montana. He saw a thighbone jutting out of a hillside at the Judith River Breaks. Shipp then hired the amateur paleontologist Joe Small to excavate the fossils. At the cost of several hundred thousand dollars, a road was constructed to allow an excavator to remove the overburden covering the skull of the specimen. In 2007, Small and his team managed to secure all remaining bones. The fossils were prepared in the White River Preparium at Hill City. They were studied by Christopher Ott at the Weis Earth Science Museum in Menasha to provide a scientific description. Peter Larson of the Black Hills Institute made casts of the bones. These were used to make a complete skull reconstruction, missing parts being based on those of Triceratops. Of this reconstruction again casts were made, sold to several musea. During this time the specimen was informally called "Judith" after the Judith River Formation. In February 2015, paleontologist Jordan Mallon was asked to cooperate in writing a scientific publication naming the taxon. The specimen was sold to the Canadian Museum of Nature for $350,000, covering Shipp's expenses.

Spiclypeus contains a single species, S. shipporum, first described and named in 2016 by Jordan C. Mallon, Christopher J. Ott, Peter L. Larson, Edward M. Iuliano and David C. Evans. The generic name is derived from Latin spica, meaning "spike", and clypeus, meaning "shield", in reference to its unique frill ornamented by many large spike-like horn ossifications on its margin. The specific name shipporum honours Dr. Bill and Linda Shipp, the original owners of the type specimen, and their family.

Spiclypeus is known solely from the holotype CMN 57081 which is housed at the Canadian Museum of Nature in Ottawa, Ontario. It is represented by a partial disarticulated skull (~50% complete), as well as several postcranial elements, among them vertebrae, ribs, a left humerus, a left ilium and the left hindlimb. Missing skull elements include the skull roof, the palate, the predentary and the rear of the lower jaws. It was collected from the lower Coal Ridge Member of the Campanian Judith River Formation several meters above the mid-Judith discontinuity, which dates it to between 76.24±0.18 and 75.21±0.12 million years ago.

Spiclypeus has an estimated length of 4.5–6 metres (15–20 ft) and a weight of about three to four tonnes.

Spiclypeus is unique among Chasmosaurinae in having a wrinkled nose bone contact on the side surface of the rear projection of the premaxilla. Spiclypeus is also unique in having the trait combination of eye-socket horncores that project to above and sideways, all six epiparietals (frill horns) that are fused at their base, first two epiparietals pairs that curl down the frill surface on its front side, and third epiparietal pair that points back and towards the mid-line of the frill.

Among other chasmosaurines from the Judith River Formation, Spiclypeus can be directly distinguished from Judiceratops, Medusaceratops and Mercuriceratops. However, it is morphologically similar to the dubious ceratopsid species Ceratops montanus from the Judith River Formation and the dubious chasmosaurine species Pentaceratops aquilonius from the Dinosaur Park Formation (located just over the Canada–United States border and close in age) and in fact all three might represent a single species, which cannot be conclusively tested due to the fragmentary nature of the type specimens of these species.

The skull has a reconstructed length of 167 centimetres. The rostral bone, the core of the upper beak, is strongly hooked. The ascending branch of the praemaxilla has a very rough outer surface, with many deep pits, indicating a strong connection to the nasal bone. The depressions on the outer sides of the praemaxillae are not connected by a perforation, though the separating bone sheath is very thin at one millimetre. The triangular nose horn has a length of 166 millimetres. The maxilla has at least twenty-eight positions in the tooth battery, each featuring three to five stacked teeth. The postorbital, or brow, horns are 228 (left) and 246 (right) millimetres long. They strongly project to the side, at an angle of 50° with the midline of the skull. Their points gradually curve to below.