Kryptops (meaning "covered face") is an extinct genus of abelisaurid theropod dinosaurs from the Early Cretaceous of Niger. It is known from a partial maxilla (upper jaw bone) found at the Gadoufaoua locality in the western Ténéré Desert, in rocks of the Aptian–Albian-age Elrhaz Formation. The fossils were collected in 2000 by a University of Chicago expedition to Niger led by American paleontologist Paul Sereno. They were then described in 2008 by Sereno and Steve Brusatte. The genus contains a single species, Kryptops palaios. Sereno and Brusatte referred several postcranial remains to Kryptops, but later studies have shown that these elements belong to an allosauroid theropod, leaving Kryptops to be only known from the incomplete maxilla.

Kryptops is one of the oldest known members of the Abelisauridae, making it vital to understanding this family's evolution. Its length is estimated to be around 6–7 m (19.7–23.0 ft), making it smaller than later genera such as Carnotaurus. Nevertheless, Kryptops is a large, carnivorous dinosaur with highly serrated teeth (bearing many denticles) and robust upper jaws. The outer surface of its maxilla features deep striations, grooves, and rugosities, indicating it was covered in a tightly adhering integumentary structure like keratin.

In 2000, an expedition conducted by the University of Chicago led by American paleontologist Paul Sereno and funded by the National Geographic Society explored fossiliferous sandstone outcrops in a site known as Gadoufaoua on the western edge of the Ténéré Desert of Niger. These layers belong to the Elrhaz Formation, which dates to the Aptian and Albian ages of the Early Cretaceous, around 112 million years ago. During the expedition, a maxilla (main tooth-bearing bone of the upper jaw) of a theropod was collected 15 m (49 ft) away from a set of postcranial elements consisting of three dorsal (back) vertebrae, two ribs, the sacrum, and the pelvis. These remains were then transported to the University of Chicago for study and preparation before being returned to the Musee National du Niger and deposited under the catalog number MNN GAD1. The maxilla was cataloged as MNN GAD1-1, whereas the postcranial fossils were assigned MNN GAD1-2 through MNN GAD1-8.

These theropod remains were believed to belong to the same individual by Paul Sereno, who, with Jeffrey Wilson and Jack Conrad, later mentioned them in a 2004 paper as an undescribed abelisaurid. Sereno and Steve Brusatte described the fossils as the holotype (name-bearing) specimen of a new genus and species of abelisaurid in 2008, named Kryptops palaios. The generic name derives from the Ancient Greek words krypto, meaning 'covered', and ops, meaning 'face', referencing the unique anatomy of the maxilla. The specific name, palaios, is a Greek term meaning "old", in reference to the age of the fossils compared to related taxa.

Sereno and Brusatte assigned the postcranial material to the same individual as the maxilla based on their close association and alleged basal abelisaurid features in the vertebrae and pelvis. Kryptops is not the only theropod known from the Elrhaz Formation; other genera include Eocarcharia, Suchomimus, and Afromimus. In 2012, Matthew Carrano and colleagues considered Kryptops palaios to be a chimera (specimen composed of multiple species), and stated that its postcranial remains, especially the pelvis and sacrum, may actually belong to a carcharodontosaurid, possibly Eocarcharia. However, these bones do not overlap with the Eocarcharia holotype, which consists only of an isolated skull element. This hypothesis was supported by later studies, who agreed that the postcranial remains belonged to an allosauroid, or more specifically, a carcharodontosaurid. In 2018, paleontologist Rafael Delcourt questioned the validity of Kryptops, suggesting that, due to the presence of only one autapomorphy (unique feature) of the maxilla, Kryptops may be a nomen dubium.

In 2025, researchers Andrea Cau and Alessandro Paterna agreed with allosauroid affinities for the postcranium. However, their phylogenetic analysis placed this material in the family Metriacanthosauridae, rather than Carcharodontosauridae. Based on these results, they further suggested that metriacanthosaurids radiated across the world during the Early Cretaceous, as demonstrated by the roughly simultaneous presence of Erectopus in Europe, the "Kryptops" postcrania in Africa, and Siamotyrannus in Asia.

The holotype individual is large for an abelisaurid, belonging to an adult about 6–7 m (19.7–23.0 ft) in length. Like other abelisaurids, Kryptops has a short, deep skull and a long, slender body. The maxilla has a preserved tooth row length of 15 cm (5.9 in) and is missing its tip, some of the alveolar margin (the upper edge of the maxilla that supports the tooth sockets), and the tooth crowns. The left maxilla preserves 11 alveoli (tooth positions) but likely bore 17 or 18 alveoli when complete, based on the related genus Rugops. There is a row of neurovascular foramina above the alveolar margin, a characteristic of abelisauroids.

The exterior face of the maxilla is extremely rugose, with pits and short vascular grooves adorning the surfaces. This condition is similar to that of other abelisaurids and some carcharodontosaurids. This may imply a keratinous integument on the maxillae instead of scales, giving the genus its name, though the skull of Carnotaurus was scaly. Sereno and Brusatte (2008) interpreted the external texture of the maxilla, with its short linear grooves, as a diagnostic characteristic of Kryptops, distinguishes it from other abelisaurids. However, Delcourt (2018) noted that this same condition is observable in Rugops and Majungasaurus, and therefore is not unique to Kryptops.