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Sordes

Sordes is a genus of small, non-pterodactyloid pterosaur that lived during the Late Jurassic period, approximately 164–155 million years ago, in what is now Kazakhstan. The type and only species, Sordes pilosus, was a primitive rhamphorhynchoid with a wingspan of about 0.6 meters, slender pointed jaws, a long tail, and notably, the first documented evidence of pycnofibers—a fur-like covering—on a pterosaur, suggesting possible insulation or sensory functions; recent studies (as of 2022) indicate these filamentous structures may have had melanosomes for coloration and signaling. Named by Soviet paleontologist Aleksandr Grigorevich Sharov in 1971 from fossils found in the Karabastau Formation, the genus name derives from Latin for "filth" or "scum," while the specific epithet "pilosus" means "hairy" in Latin, reflecting the preserved soft tissues that initially appeared as hair but are now understood as filamentous structures unique to pterosaurs. The specimen (PIN 2585/3) and additional material exhibit exceptional preservation of , revealing a bat-like flight apparatus where the wings extended from the ankles, including a uropatagium () supported by an elongated fifth on the hind foot. This configuration indicates that Sordes had a structurally heterogeneous flight surface, with a stiff outer section for aerodynamic efficiency and a more flexible inner region for maneuverability, challenging earlier models of locomotion. As a basal member of the Pterosauria, Sordes provides key insights into the early evolution of soft tissues and flight adaptations, bridging gaps between reptilian ancestors and more derived flying reptiles. Fossils of Sordes pilosus come exclusively from the Oxfordian–Kimmeridgian stages of the Karabastau Svita, a known for its fine-grained limestones that preserve delicate structures, alongside other small vertebrates like early mammals and . Its diet likely consisted of small or soft prey, inferred from the crushing-adapted posterior teeth and overall size, positioning it as an agile hunter, possibly nocturnal or crepuscular, in a diverse ecosystem. Ongoing studies continue to refine its phylogenetic position within , emphasizing its role in debates over and .

Discovery and Naming

Discovery

The specimen of Sordes pilosus (PIN 2585/3), consisting of a nearly complete but crushed preserved on a slab, was discovered in the in the foothills of the Karatau Mountains, southern , within the Karabastau Formation of the . This locality, part of a known for exceptional fossil preservation, dates to the Oxfordian–Kimmeridgian stages, approximately 155.7 million years ago. The specimen was formally named and described in 1971 by Soviet paleontologist Aleksandr Grigorevich Sharov in the Russian journal Priroda (Sharov, A.G. 1971. Novye letayushchie reptilii iz mezozoya Kazakhstana i Kirgizii. Priroda 4: 81-87.), marking one of the earliest reports of a with preserved structures. Sharov simultaneously designated a (PIN 2470/1), another slab-mounted skeleton that provided complementary details on cranial despite similar compression. At least six additional specimens are known from the same formation, enhancing understanding of and preservation quality among these small-bodied pterosaurs (Bakhurina & Unwin 1995). Early excavations proved challenging due to the fragile, dorsoventrally crushed state of the fossils, which complicated preparation, as well as the remote desert setting of the , limiting access and logistical support during fieldwork in the .

Etymology

The name Sordes derives from the Latin noun sordēs, meaning "filth," "dirt," or "scum." However, Aleksandr Grigorevich Sharov, who established the in , intended Sordes to correspond to the Russian word nechistʹ ("нечисть"), signifying "," "evil spirit," or "unclean spirit," thereby evoking the image of a "hairy " due to the fossil's preserved integumentary filaments. This nominative choice highlighted the specimen's eerie, fur-like appearance, which Sharov emphasized in his original description from the Karabastau Formation in . The specific epithet pilosus originates from the Latin adjective pilosus, meaning "hairy" or "shaggy," alluding directly to the dense covering of pycnofibers on the specimen that Sharov interpreted as hair. Consequently, the full Sordes pilosus translates literally to "hairy filth" or "hairy scum" in Latin, though Sharov's conceptual intent rendered it as "hairy demon" or "hairy " to capture the fossil's otherworldly preservation. This naming occurred in Sharov's seminal 1971 paper, where the extraordinary soft-tissue details justified the evocative terminology.

Description

Overall Anatomy

Sordes pilosus was a small , one of the smaller members of the group. The overall body was compact with a short and robust that contributed to its slender, agile build. This , devoid of cranial or other prominent ornamentation, emphasized functional adaptations over structures. The wings of Sordes were proportionally short, with the primary support provided by an elongated fourth finger that extended to form the structural basis of the wing membrane, or . A distinctive feature was the long tail, which exceeded half the length of the body and terminated in an elongated vane, likely aiding in aerodynamic stability during flight. The skeletal proportions, including the integration of hind limbs into the flight apparatus, further highlight its specialized aerial adaptations.

Skull and Dentition

The skull of Sordes pilosus is slender, featuring a narrow rostrum and large orbits. The basic rhamphorhynchoid cranial plan is evident, with an unreduced lacking the modifications seen in more derived pterosaurs such as pterodactyloids. Dentition in S. pilosus includes prominent, pointed teeth concentrated at the anterior portion of both upper and lower jaws, while the posterior regions bear smaller, more numerous teeth. These teeth exhibit a circular cross-section rather than the labiolingual compression typical of many other non-pterodactyloid pterosaurs. Preserved cranial elements reveal a robust articulation.

Pycnofibers and Integument

Sordes pilosus represents the first pterosaur genus in which pycnofibers—filamentous ary structures—were definitively identified, with preservation evident in the specimen (PIN 2585/3) from the Karabastau Formation of . These structures appear as impressions on the , , and portions of the wings, extending from the head to the ankles in the preserved material. Additional specimens further documented pycnofibers across similar regions of the , confirming their widespread occurrence in this species. The pycnofibers of S. pilosus consist of simple, unbranched, hair-like filaments that vary in length up to several centimeters, forming a dense covering over the body and a sparser distribution along the wing membranes. Unlike the uniform keratinous shafts of mammalian hair, these multicellular filaments exhibit a central canal and lack true scales or vanes, distinguishing them as a unique pterosaurian feature rather than true fur. In the original 1971 description, the pycnofibers were misinterpreted as a fur-like pelage, inspiring the species epithet pilosus (Latin for "hairy"). This interpretation was later refined through studies of the and paratypes, reclassifying the structures as pycnofibers—proto-feather-like filaments endemic to pterosaurs—and ruling out with mammalian based on their histological composition and distribution.

Classification

Taxonomic History

Sordes pilosus was originally described by Aleksandr G. Sharov in 1971 and assigned to the family Rhamphorhynchidae, primarily due to its elongate tail supported by elongated chevrons and a featuring multicusped teeth typical of that group. This placement within Rhamphorhynchidae was reaffirmed in subsequent reviews, emphasizing the shared long-tailed morphology and cranial features with other members of the family. Subsequent analyses refined this classification further; David M. Unwin proposed assigning Sordes to the subfamily Scaphognathinae within Rhamphorhynchidae, citing similarities in wing proportions, such as a relatively short relative to body size, and tail vane structure with . During the , several additional specimens from the Karabastau Formation were referred to Sordes pilosus and retained within the species due to consistent skeletal features aligning with the .

Phylogenetic Position

Sordes pilosus is recognized as a basal member of the non-pterodactyloid pterosaurs, specifically within the family Rhamphorhynchidae, where it occupies an early position in the radiation of the group following its Late origins. Traditional cladistic analyses place Sordes in the Scaphognathinae as the to more derived forms such as crassirostris, supported by shared derived traits including a reduced with no more than nine pairs of straight or slightly recurved rostral teeth and six vertically oriented mandibular teeth, as well as an angular flexure (40–45°) in the mid-length of pedal V 2. In the broader pterosaur tree, Sordes represents an early-diverging taxon among the basally branching non-pterodactyloids, characterized by synapomorphies of Rhamphorhynchidae such as a long, slender tail with a distal vane, metacarpals I–III of subequal length and shorter than metacarpal IV (which is ≥80% humerus length), and the presence of pycnofibers—filamentous integumentary structures—that reinforce the monophyly of a "fuzzy" subclade of long-tailed pterosaurs. Phylogenetic studies from the 2010s onward, including those incorporating expanded matrices of early taxa, have upheld Sordes' basal status within non-pterodactyloids but challenged its Scaphognathinae placement due to autapomorphic featuring robust, conical teeth lacking the labiolingual compression typical of related rhamphorhynchids, often resolving it instead as sister to the monofenestratan (Rhamphorhynchidae + ). More recent analyses (as of 2024) continue to support its basal position within Rhamphorhynchidae without conclusively resolving subfamily placement.

Paleobiology

Diet and Feeding

Sordes pilosus is inferred to have been primarily insectivorous or piscivorous, with its adapted for capturing small or arthropods from the water surface or in mid-air. The are larger, recurved, and pointed, facilitating the snatching and secure holding of evasive prey, while the posterior teeth are smaller, robust, and suited for crushing the exoskeletons of hard-bodied . This dental configuration indicates an opportunistic diet focused on soft-bodied and shelled , consistent with the insect-rich lacustrine of the Karabastau Formation where the fossils were found. Jaw mechanics in basal rhamphorhynchoids like S. pilosus suggest a relatively strong bite force for its small size, with the stocky providing resistance to bending stresses during feeding. This would have enabled the capture and processing of small prey, comparable to the capabilities of modern small insectivorous or piscivorous . The robust posterior further supports durophagous tendencies, allowing for the breakdown of tougher prey. Tooth morphology shows no adaptations for herbivory, such as grinding surfaces or shearing edges for plant material, nor for scavenging, like bone-crushing features seen in some theropods. Instead, the pointed, grasping and crushing posterior ones align exclusively with a carnivorous or insectivorous lifestyle targeting live, mobile prey.

Habitat and Ecology

Sordes fossils are preserved in the Karabastau Formation of the Karatau Mountains in southern , a Middle to Late Jurassic (Oxfordian–Kimmeridgian) consisting of thin-bedded, fine-grained limestones formed in a lacustrine . These sediments indicate low-oxygen, reducing conditions with high and limited decomposers, which facilitated exceptional preservation of soft tissues by delaying organic decay. The paleoenvironment around the Karatau region was characterized by a warm, humid climate that supported lush vegetation and a rich , including abundant —over 18,000 specimens representing diverse orders—and small-bodied such as teleosts and semionotids. This ecosystem also featured early avialans like Praeornis and Ambiortus, relatives of Archaeopteryx, alongside fragmentary remains of dinosaurs and other reptiles, reflecting a continental setting with freshwater to brackish influences. As a small-bodied rhamphorhynchid with a of approximately 0.6 meters, Sordes likely filled an as a low-altitude flier foraging over lacustrine and coastal habitats, exploiting its size to minimize with larger pterosaurs such as anurognathids and early pterodactyloids present in the formation. Its appears restricted to , with no isotopic or faunal evidence suggesting long-distance migration, and it may have engaged in predator-prey interactions with aquatic vertebrates like and amphibians in the shallow waters.

References

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