Osteology VIII: The antorbital cavity

Digital carbon dust plate of the skull and mandibular ramus of an adult Tyrannosaurus bataar (PIN 551-3) in left lateral view © Dino Pulerà. The antorbital cavity is highlighted in color; plaster is a uniform dark gray. Among derived tyrannosauroids, the antorbital cavity of T. bataar is maximally enclosed by the surrounding subcutaneous bone and so has a reduced surface area when viewed from the side. The skull is 1130 mm long from the premaxilla to the quadrate (Maleev, 1974). Abbreviation: PIN, Palaeontological Institute, Russian Academy of Sciences, Moscow.

Introduction

In the last lecture of my Dinosaur Evolution and Extinction course, I walked the students through the Extant Phylogenetic Bracket (Witmer, 1990), and I concluded by placing a cast of an ankylosaurid skull in the middle of the table and saying (paraphrased here), “Skeletons are an illusion; bones are closer to the hole than to the donut - they are mostly shaped by the soft tissues that attach to them and permeate through their interiors. When you gaze upon bones you do not see the animal laid bare, you see a naked thing from which nearly all of the information has been stripped away.”

In this vein, my goal in this post is to draw attention to the skull as a living structure that is shaped by specific soft tissues and soft tissue systems. This will be a departure from the bone-by-bone approach that I have taken in the preceding posts, but both views are illuminating and I think this is a worthwhile change in perspective.

By the way, much of what is presented here follows the work of Dr. Lawrence M. Witmer (Ohio University, Athens), who innovated the Exant Phylogenetic Bracket (EPB) method for inferring the soft tissues that shaped the skeletons of extinct amniotes. I first saw him present his intellectually exciting research, which established the pneumatic null hypothesis for the antorbital cavity, at the 4^th Symposium of Mesozoic Terrestrial Ecosystems back in 1987 at the Tyrrell Museum of Palaeontology (Drumheller, Alberta). Ever since then I have respected and admired the innovative and illuminating work done by Larry and his students. As such, a strong EPB theme runs through the course of these posts.

A note on the illustration—The image is a digital carbon dust plate rendered by Mr. Dino Pulerà. This is our most recent collaboration; I drafted the line drawing from photographs that I took of the original specimen, when it was at the Royal Ontario Museum (ROM) as part of a temporary vertebrate fossils exhibit from Russia. I was fortunate enough to have after hours access to the exhibit  – for several nights – to take notes and measurements, and to sketch and photograph the skull. I produced the line drawing by standing directly over the skull with the photographs in hand; I was able to exactly draw all of the plaster reconstruction, foramina, sutures, and damage onto each photo. The resulting line drawing was the most exact that I could produce, under what were the best possible conditions.

By the time Dino and I agreed that we’d like to collaborate on a digital carbon dust, departing from the traditional graphite dust on illustration board, the original skull had long since been shipped to another venue. Fortunately, the ROM has a cast of the skull in its vertebrate paleontology collections (see photograph below). In 2008, Dino and I worked on the plate in the darkened collections room for several evenings over a week. Neither of us considers this work finished, but the results are promising enough to debut our new approach to illustration here.

Dino Pulerà at work on the digital carbon dust of PIN 551-3 during January, 2008. He is working from a cast in the collections room of the Department of Vertebrate Paleontology at the Royal Ontario Museum. Dino is crafting the illustration in Photoshop using a WACOM tablet.

On a less formal note, up until the ROM exhibit I had only seen the pen-and-ink illustration and the photographic plate of the skull in Maleev (1974), and the low-resolution casts of the skull in the holdings of the ROM, American Museum of Natural History, and the Canadian Museum of Nature. I have to admit that when I saw the specimen in person for the first time, it was a breath-catching moment - it is a very beautiful fossil, where the preservation has an unexpected level of anatomical detail. It is our hope to capture a sliver of that quality in the digital image.

TERMINOLOGY

The osteological terms used here follow those established by Witmer and Baumel (1993), and Witmer (1997) for archosaurian anatomy; anglicized versions of Latin terms in those sources are used when an English equivalent is not provided.

Antorbital cavity: The space ahead of the orbital fenestra, lateral to the nasal airway and medial to the external surface of the bone (Witmer, 1997). Laterally this space is enclosed by the external antorbital fenestra, and the dorsolateral surfaces of the palatine bone and the palatal process of the maxilla bound it ventromedially (Witmer, 1997). The cavity includes the external and internal antorbital fenestra, maxillary and promaxillary fenestrae, and the antorbital fossa and its subordinate openings (Witmer, 1997).

Antorbital fossa: The smooth surface that excavates the bony surfaces situated between the edges of the external and internal antorbital fenestrae (Witmer, 1997). This excavated surface (relative to the external surface of the bone) is also termed the medial lamina (Witmer, 1997).

Antorbital sinus: Term for the soft tissue structure that produced the bony antorbital cavity (Witmer, 1997).

Basal derived tyrannosauroids: This phrase refers to the Bistahiversor + Albertosaurus grade, excluding Tyrannosaurinae unless defined otherwise.

Derived tyrannosaurines: This phrase denotes the Daspletosaurus + Tyrannosaurus clade, and all descendants of their common ancestor.

Derived tyrannosauroids: This phrase refers to the Bistahieversor + Tyrannosauridae clade, which is the phylogenetic limit of content in this post unless stated otherwise.

External antorbital fenestra: The outer edge of the antorbital fossa (Witmer, 1997).

Internal antorbital fenestra: The margin of the antorbital fenestra that is separated from the external antorbital fenestra by a bony surface that is excavated by the antorbital fossa (Witmer, 1997). The fenestra is positioned lateral to the bony choana, the internal nostril (Witmer, 1997).

Lateral lamina (=lamina lateralis; Witmer, 1997): The external, subcutaneous surface of the maxilla ahead of the antorbital fossa, which may undercut the surface of the bone and extend ahead of the external antorbital fossa. In tyrannosaurids this takes the form of a strut that conceals the promaxillary fenestra from lateral view.

Maxillary antrum: The chamber within the medial half of the maxilla into which the maxillary fenestra opens; positioned caudal to the promaxillary recess (Witmer, 1997). The chamber extends ventrally between tooth root bulges as pneumatic interalveolar recesses (Witmer, 1997).

Medial lamina: See Antorbital fossa.

Promaxillary recess: The chamber ahead of the maxillary antrum into which the promaxillary fenestra opens; the recess is expressed externally as the vestibular bulla (Witmer, 1997).

Subcutaneous surface: The textured external surface of the facial and mandibular bones that was attached in life to the overlying skin.

Ventral ramus of the lacrimal (=jugal ramus; Witmer, 1997): This is the vertically oriented bar of the lacrimal that separates the orbital fenestra and the antorbital cavity from each other.

DESCRIPTION

General features of the antorbital cavity: In lateral view, the antorbital fossa is a smooth depression that is inset relative to the subcutaneous surface of the facial skeleton and surrounds the internal antorbital fenestra. The fossa is an osteological correlate the soft tissue antorbital sinus that is composed of epithelium, which removes bone (Witmer, 1987). As such, the bones that bear the fossa are described as excavated, in view of the destructive process that produced it in life (Witmer, 1987).

In terms of its relationships to bony structures, this cavity in derived tyrannosauroids extends laterally through the internal antorbital fenestra, rostrally into the maxillary antrum through the caudal fenestra of the maxillary antrum, medially through the maxillary fenestra into the maxillary antrum, and rostrally through the promaxillary fenestra into the promaxillary recess; it also extends ventromedially into the interior of the palatine bone through one or two large pneumatic recesses.

In tyrannosaurids, the fossa excavates the ventral half of the rostral ramus (the part that extends rostrally above the antorbital fenestra) of the lacrimal, the rostral surface of the ventral ramus of the lacrimal (although this cannot be seen from the side), the rostroventral quadrant of the ventral ramus of the lacrimal, the rostrodorsal quadrant of the maxillary ramus of the jugal, and the lateral surface of the maxilla that surrounds the antorbital fenestra, and extends rostrally to produce a region that is penetrated by two subordinate openings. Most of these features can be seen in Tyrannosaurus bataar, except that the cavity is enclosed rostrally and ventrally in the maxilla.

Even in a taxon such as T. bataar where it is partly enclosed, the cavity is extensive: rostrocaudally it occupies a third of the total skull length and over half of the length of the snout, and dorsoventrally it exceeds two-thirds of the preorbital skull height.

Antorbital fossa: In lateral view, the antorbital fossa is the smooth surface that separates the external and internal antorbital fenestrae; it is the surface that has been excavated by the epithelium of the antorbital air sac. The fossa is usually inset relative to the subcutaneous surface of the facial bones; however, in some places the surfaces grade into each other. The antorbital fossa excavates the lacrimal, jugal and maxilla as a continuous, unbroken surface that twists along its course around the internal antorbital fossa. Although most of the fossa faces laterally, in all derived tyrannosauroids it flattens the rostral surface of the ventral ramus of the lacrimal and so it is not in view.

Ontogeny of the antorbital fossa—During ontogeny, the rostral margin of the antorbital fossa becomes enclosed by the caudally extending rostrodorsal edge of the external antorbital fenestra, which conceals the promaxillary fenestra from view (Carr, 1999).

Taxonomic variation of the antorbital fossa—The fossa does not contact the nasal in Bistahieversor (Carr et Williamson, 2010) or in Daspletosaurus adults (Russell, 1970); this may also be the case in Raptorex (Sereno et al., 2009) and in juvenile T. bataar (Tsuihiji et al., 2009). The fossa has a very short contact with the nasal in Albertosaurus libratus (Carr, 1999) and juveniles of D. torosus (Currie, 2003). In contrast, the fossa has an extensive contact with the nasal in juvenile and adult T. rex (Carr, 1999; Carr et Williamson, 2004), and in adult T. bataar (Maleev, 1974).

In derived tyrannosaurines, the fossa faces ventrally along the midlength of the rostral ramus of the lacrimal such that the subcutaneous surface reaches the ventral margin of the ramus. In T. bataar, the fossa is enclosed by the subcutaneous surface of the maxilla ventrally, such that the fossa is blocked from lateral view; this condition is seen juveniles (Currie et Dong, 2001; Tsuihiji et al., 2009).

See Closure of the antorbital cavity in T. bataar, External antorbital fenestra.

Antorbital fenestra: See Internal antorbital fenestra.

Closure of the antorbital cavity in T. bataar: Arguably, T. bataar has a condition that is convergent upon what is seen in derived ornithischians, namely the external closure of the antorbital cavity. The external antorbital fenestra of T. bataar differs from that of other tyrannosauroids in that it is partly closed by the subcutaneous flange, a tall ridge that extends dorsally along the ventral margin of the fenestra (Carr, 2004). The flange blocks the ventral extent of the antorbital fossa of the maxilla from view, and entirely so below the internal antorbital fenestra.

In dorsolateral view, the flange produces a deep slot between itself and the antorbital fossa proper. This feature gives the snout of T. bataar is distinctive appearance in having what appears to be an unusually deep proximal dentigerous region, in contrast to what is seen in its closest relatives, including T. rex. Since tooth root bulges do not fill the slot, the flange is a dorsalward extension of the subcutaneous surface and is not produced by unusually deep tooth roots.

Distal accessory recess of the lacrimal—This opening occurs on the ventrolateral surface of the rostral ramus of the lacrimal at least halfway along the rostral ramus.

Taxonomic variation of the distal accessory recess of the lacrimal—This opening is seen in Alioramus, Teratophoneus, Daspletosaurus and in Tyrannosaurus Brusatte et al., 2012; Carr et Williamson, 2004, Carr et al., 2011). In Daspletosaurus, both this opening and the proximal accessory recess occur together (Carr et Williamson, 2004).

Dorsal fossa of the lateral interfenestral strut (=pneumatic excavation of the ascending ramus; Witmer, 1997): The rationale for the name change from Witmer (1997) is to express the exact topological position of this structure. This fossa is absent or shallow in relatively immature derived tyrannosauroids, whereas it is deep in adults (Carr, 1999; Carr et Williamson, 2004).

External antorbital fenestra: This feature corresponds to the edge of the antorbital fossa along the subcutaneous surface of the facial skeleton. It may seem to be a subtle distinction from the antorbital fossa, but the difference becomes clear in mature tyrannosaurids, where the subcutaneous surface becomes strutlike – especially rostrally – and partly encloses the perimeter of the antorbital fossa.

This rim extends along the lateral surface of the maxilla, jugal, and lacrimal, In some taxa, including T. rex and T. bataar, it extends along the ventrolateral edge of the nasal bone. Over much of its course the fenestra is a distinct rim, but in some taxa (e.g., Tyrannosaurus) it is only a subtle demarcation between the coarse subcutaneous surface and the smooth antorbital fossa in several regions, such as on the maxilla along the ascending ramus, the lacrimal at the lacrimal pneumatic recess, and the jugal on either side of the jugal pneumatic recess.

On the lacrimal, the rim occurs on the lateral surface of the bone at the angle between the ventral and rostral rami. The caudodorsal edge of the rim forms the external margin of the lacrimal pneumatic recess. The entire rim may be undercut by the antorbital fossa, or the subcutaneous and fossa surfaces might not be separated from each other (Carr, 1999).

The rim usually extends along the lateral surface of the rostral ramus; it may also extend along the ventrolateral edge of the ramus. As such, in some tyrannosauroids (Bistahieversor, Albertosaurus spp.), the antorbital fossa is widely exposed on the ramus in lateral view, whereas it faces largely or entirely ventrally in others (T. bataar, Daspletosaurus).

The rim extends along the leading edge of the ventral ramus of the lacrimal, before extending caudoventrally toward the jugal. In this region, the antorbital fossa returns to view on the lateral surface of a small flange, the rostroventral ala. As it extends from the lacrimal to the jugal, the rim may be distinct, where the antorbital fossa undercuts the subcutaneous surface of the lacrimal and jugal (Albertosaurus spp.) or it might be indistinct (Tyrannosaurinae), where the undercut is absent.

The rim of the fenestra extends around the rostrodorsal corner of the jugal, extending between the lacrimal dorsally and the maxilla rostrally. The rim forms the distinct caudoventral edge of the jugal pneumatic recess, which is undercut by an invasive sinus that inflates the body of the jugal bone.

Ontogeny of the external antorbital fenestra—In small juveniles of A. libratus, the rostroventral margin of the fenestra is distinct, whereas in more mature specimens it is indistinct and the subcutaneous surface and the antorbital fossa grade into each other. Also, in A. libratus juveniles, the rostral margin of the ventral ramus of the lacrimal is convex along its course; in contrast, the rostrodorsal margin is distinctly concave in subadults and adults (Carr, 1999).

See also Antorbital fossa.

Internal antorbital fenestra: This is the conventional ‘antorbital fenestra’ of most workers, which is usually not distinguished from the external antorbital fenestra. The internal fenestra is a large aperture that is enclosed by the maxilla rostrally, the lacrimal caudodorsally and caudally, and by the jugal caudoventrally. In some taxa the contribution of the jugal may be very short. Of these bones, the maxilla has the greatest contribution to the fenestra, followed by the lacrimal, and then the jugal.

Ontogeny of the internal antorbital fenestra—In tyrannosaurids the general trend is for the fenestra to deepen, increasing the ratio of its height to length (Carr, 1999; Currie, 2003). This trend pertains to all tyrannosaurids, including tyrannosaurines (Tsuihiji et al., 2009).

Taxonomic variation of the internal antorbital fenestra—The fenestra of basal derived tyrannosauroids is longer than tall, whereas among tyrannosaurines the fenestra is as long as tall, or taller than long (Carr, 1999). In contrast to other derived tyrannosauroids, the contribution of the jugal to the margin of the fenestra is greatly reduced – nearly excluded by the lacrimal and maxilla - in T. rex (Carr, 1999).

Jugal pneumatic recess: This recess penetrates the caudoventral corner of the antorbital fossa, ahead of or slightly below the ventral ramus of the lacrimal and caudal to the division between the lateral and medial maxillary processes of the jugal (Carr, 1999). The jugal pneumatic recess leads into an extensive chamber that hollows the body of the bone below the orbital fenestra and in some cases extends a short distance up into the postorbital process of the jugal.

Lacrimal antorbital fossa: The antorbital fossa covers the ventral region of the rostral ramus of the lacrimal, which is continuous rostrally with that of the maxilla. The antorbital fossa of the lacrimal is penetrated by up to three pneumatic foramina, in addition to the lacrimal pneumatic recess (Carr et Williamson, 2004).

Ontogeny of the lacrimal antorbital fossa—In juvenile A. libratus, the antorbital fossa on the rostral ramus is widely exposed to lateral view, whereas in subadults and adults, it is nearly excluded by the ventrally extending subcutaneous surface (Carr, 1999). In A. libratus, the antorbital fossa of the lacrimal is not undercut where it extends along the subcutaneous surface of the ventral ramus in juveniles; in contrast, the fossa is deeply excavated in this region (Carr, 1999).

Lacrimal pneumatic recess (=dorsolateral lacrimal fossa; Witmer, 1997): This opening occurs at the caudodorsal corner of the antorbital fossa, where it pierces the crux between the ventral and rostral rami of the lacrimal. The chamber it opens into hollows the supraorbital region of the bone and extends a short distance into the ventral ramus.

Ontogeny of the lacrimal pneumatic recess—In derived tyrannosaurines, the opening is large in juveniles; in contrast, in adults it is reduced in size in part by the inflation of surrounding pneumatic sinuses within the bone.

Taxonomic variation of the lacrimal pneumatic recess—In basal derived tyrannosauroids (Apalachiosaurus, Bistahieversor) and in derived tyrannosaurines (Daspletosaurus, Tyrannosaurus), the opening is small. In contrast, the opening is large in Albertosaurus, Alioramus, and Teratophoneus.

Lateral casement of the antorbital sinus: In modern birds, the facial skin covers the antorbital sinus (Witmer, 1997); based on recent common ancestry, there is no reason to think that this condition was not also in extinct archosaurs. This drum-skin arrangement was vulnerable to injury - I have seen many tyrannosaurids with extensive lesions on the antorbital fossa; some of these penetrate through the maxillary bone (Peterson et al., 2009). To my mind, it is notable that tyrannosaurids survived direct injuries (that presumably were open to the outside) to this part of their respiratory airway.

Maxillary fenestra: This opening is seen in all tyrannosaurids, and is the second largest opening in the antorbital fossa. The maxillary fenestra is the largest of the subordinate openings that can be seen in lateral view. It is a window that opens into the maxillary antrium, a box enclosed medially by thin bone that is penetrated by three additional medial openings.

The fenestra in tyrannosaurids has a distinct shape, where the caudodorsal and caudoventral margins are nearly straight and converge caudally, producing a caudally pointing V (Brochu, 1993). It is this V-shaped margin that defines the dorsal and ventral limits of the lateral interfenestral strut; ergo, the dorsoventral height of the fenestra is equivalent to that of the strut. The caudal extreme of the ‘v’ represents the narrowest point of the interfenestral strut. The rostroventral margin usually curves rostrodorsally along a steep angle to the convex rostrodorsal margin.

Ontogeny of the maxillary fenestra—In most derived tyrannosauroids the fenestra is small in juveniles, where it is located centrally in the antorbital fossa and does not approach the rostrodorsal, rostral, or ventral margins of the depression (Carr, 1999). In A. libratus the fenestra enlarges, where it extends rostrally, but without closely approaching the rostral margin of the antorbital fossa (Carr, 1999). In contrast, the opening is large in juveniles of Raptorex and T. bataar (Sereno et al., 2009; Tsuihiji et al., 2009).

In adults of basal derived tyrannosauroids (Bistahieversor, Albertosaurus) the fenestra is larger than the condition seen in juveniles, but it is still centrally located in the antorbital fossa and does not approach the rostral margin of the fossa. In tyrannosaurine adults, the fenestra closely approaches (Daspletosaurus) or extends ahead (Tyrannosaurus) of the rostral and rostrodorsal margins of the external antorbital fenestra.

Taxonomic variation of the maxillary fenestra—In basal derived tyrannosauroids (Appalachiosaurus, Bistahieversor, Albertosaurus, Teratophoneus), the fenestra is small. In contrast, the fenestra is large in derived tyrannosaurines,where the fenestra closely approaches. (Daspletosaurus) or extends medially past the rostral margin of the antorbital fossa (Tyrannosaurus; Carr, 1999).

The condition seen in Zhuchengtyrannus is unusual, where the enlarged fenestra reaches the rostral margin of the fossa by a notch (Hone et al., 2011). The fenestra is long in Alioramus, but it is centrally located within the antorbital fossa without closely approaching its rostral margin (Brusatte et al., 2012). In fact, it is situated closer to the rostrla margin of the internal antorbital fenestra than to the external antorbital fenestra Brusatte et al., 2012).

Promaxillary fenestra: In lateral view, this opening cannot be seen in T. bataar or T. rex adults owing to the rostrally extended maxillary fenestra. However, in less mature individuals and other tyrannosaurids, the dorsal and ventral margins of the fenestra can usually be seen, as well as a shallow fossa that extends between them into the opening.

Ontogeny of the promaxillary fenestra—In juveniles of A. libratus and T. rex, the promaxillary fenestra is a narrow slit that is not recessed dorsally (Carr, 1999). In contrast, the dorsal margin of the fenestra is recessed in subadults of A. libratus, whereas in adult T. rex the opening is modified into a round foramen (Carr, 1999). The fenestra is recessed in the holotype of Alioramus altai, where its dorsal margin has the form of a distinct ridge, which is consistent with its subadult relative maturity (Brusatte et al., 2012).

Taxonomic variation of the promaxillary fenestra—In Bistahieversor, Albertosaurus, Alioramus, and Teratophoneus, this opening is a narrow teardrop shaped slit. This condition is also seen in juveniles of Tyrannosaurus, whereas it is a round foramen in adults (Carr, 1999).

The dorsoventral position of the fenestra relative to the ventral margin of the maxillary fenestra is taxonomically informative, where the opening in A. libratus and Bistahieversor is positioned dorsal to the ventral margin of the maxillary fenestra (Holtz, 2001; Carr et Williamson, 2010).

Promaxillary pillar (=pila promaxillaris; Witmer, 1997): The region of the antorbital fossa that separates the promaxillary and maxillary fenestrae (Witmer, 1997).

Ontogenetic & taxonomic variation of the promaxillary pillar—In basal derived tyrannosauroids, excluding tyrannosaurines more derived that Teratophoneus, the pillar is rostrocaudally long and widely separates the promaxillary and maxillary fenestra. This is also seen in juvenile derived tyrannosaurines, whereas in adults the pillar is nearly eliminated (Daspletosaurus) or eliminated (Zhuchengtyrannus, Tyrannosaurus) by the rostrally extended maxillary fenestra.

Proximal accessory recess of the lacrimal: This recess occurs ahead of the lacrimal pneumatic recess and they are separated by a septum that may be short or long.

Taxonomic variation of the proximal accessory recess of the lacrimal: The proximal recess is seen in A. libratus (Carr, 1999), A. sarcophagus (Carr et Williamson, 2004), Daspletosaurus (Carr et Williamson, 2004), and in T. bataar (Carr et Williamson, 2004).

Rostrodorsal recess of the maxilla: This recess is seen in Alioramus altai (Brusatte et al., 2010), Raptorex (Sereno et al., 2009), and juvenile T. bataar (Tsuihiji et al., 2009).

Ontogeny of the rostrodorsal recess of the maxilla—In juvenile T. bataar this recess is a shallow fossa (Tsuihiji et al., 2009); it culminates in adults (PIN 551-1) as a penetrating recess (Maleev, 1974).

Taxonomic variation of the rostrodorsal recess of the maxilla—This recess is seen in Alioramus, Raptorex, and T. bataar, whereas it is not seen in other derived tyrannosauroids.

Rostroventral ala of the lacrimal (=ventrolateral lacrimal fossa; Witmer, 1997): This structure is a short triangular surface that is deeply excavated by the antorbital fossa such that it is separated from the subcutaneous surface of the ventral ramus by a deep slot. The lateral surface of the ala is concave, indicating an indistinct fossa.

Secondary fossa of the jugal: This structure is a synapomorphy of Tyrannosauridae, which is not seen in Bistahieversor or less derived tyrannosauroids (Carr et Williamson, 2010). This is a discrete fossa positioned medial to the jugal pneumatic recess that has a distinctly inset dorsal margin; in contrast, the corresponding surface in Bistahieversor is flat. The secondary fossa is widely exposed to lateral view in adult tyrannosaurines, such as T. bataar, whereas in juveniles and in nontyrannosaurines, the fossa is only marginally exposed to view (Carr, 1999).

Ontogeny of the secondary fossa—In tyrannosaurine juveniles, the secondary fossa is marginally exposed to lateral view; in contrast, it is widely exposed to view, where it extends far above the lateral edge of the jugal pneumatic recess (Carr, 1999; Currie, 2003). This exposure is almost certainly the result of absorption of bone along the lateral edge of the jugal pneumatic recess.

Taxonomic variation of the secondary fossa —In nontyrannosaurines, the secondary fossa is marginally exposed above the lateral edge of the jugal pneumatic recess. In contrast, the fossa is widely exposed in tyrannosaurines, such that it is nearly circular in outline (Carr, 1999; Currie, 2003).

Subordinate fossae: In lateral view, several nonpenetrating fossae are seen within the boundaries of the antorbital fossa. These occur with regularity in tyrannosaurids, although they may vary ontogenetically and phylogenetically. These include the proximal and distal pneumatic recesses of the lacrimal, the secondary fossa of the jugal, the rostrodorsal recess on the maxilla, and the dorsal and ventral fossae of the lateral interfenestral strut.

See Dorsal fossa of the lateral interfenestral strut, Rostrodorsal recess of the maxilla, Secondary fossa, Ventral fossa of the lateral interfenestral strut.

Subordinate penetrating recesses: The antorbital fossa has several subordinate recesses; these are openings that are larger than neurovascular foramina, which lead into sinuses that hollow out the interior of bones. Tyrannosaurids have a relatively fixed set of penetrating recesses, namely the lacrimal pneumatic recess, the jugal pneumatic recess, the maxillary fenestra, and the promaxillary fenestra. In addition to these, most tyrannosaurids have one or two accessory recesses ahead of the lacrimal pneumatic recess.

The maxilla has a set of subordinate recesses; these include a recess that occurs rostrodorsal to the maxillary fenestra (Alioramus altai, Raptorex, T. bataar), another in the dorsal half of the lateral interfenestral strut, and one in the base of the interfenestral strut. The recesses of the interfenestral strut become more deeply excavated during ontogeny (Carr, 1999), until – in Tyrannosaurus – they penetrate through the basal part of the strut (Maleev, 1974; Carr et Williamson, 2004).

See Rostrodorsal recess of the maxilla, Ventral fossa of the lateral interfenestral strut.

Ventral fossa of the lateral interfenestral strut—This fossa is an ontogentically controlled feature, where it is absent from juveniles, but present in subadults and adults (Carr, 1999). In some taxa (Zhuchengtyrannus, T. bataar, T. rex) it becomes a penetrating recess late in adulthood, where it opens into the maxillary antrum (Carr et Williamson, 2004). This fossa is not connected to the dorsal fossa of the interfenestral strut.

REFERENCES CITED

Brochu, C.A. 2003. Osteology of Tyrannosaurus rex: insights from a nearly complete skeleton and high-resolution computed tomographic analysis of the skull. Society of Vertebrate Paleontology Memoir 7: 1-138.

Carr, T.D.  1999.  Craniofacial ontogeny in Tyrannosauridae (Dinosauria, Theropoda). Journal of Vertebrate Paleontology 19: 497-520.

Carr, T.D. 2004. Phylogeny of Tyrannosauroidea (Dinosauria: Coelurosauria) with special reference

            to North American Forms. Unpublished PhD Dissertation, University of Toronto, 1270 pp.

Carr, T.D., and Williamson, T.E. 2004. Diversity of Late Maastrichtian Tyrannosauridae (Dinosauria: Theropoda) from western North America. Zoological Journal of the Linnean Society 142: 419-523.

Carr, T. D., T. E. Williamson, B. B. Britt, and K. Stadtman. 2011. Evidence for high taxonomic and morphologic tyrannosauroid diversity in the Late Cretaceous (Late Campanian) of the American Southwest and a new short-skulled tyrannosaurid from the Kaiparowits Formation of Utah. Naturwissenschaften 98: 241–246.

Currie, P.J. 2003. Cranial anatomy of tyrannosaurid dinosaurs from the Late Cretaceous of Alberta, Canada. Acta Palaeontologica Polonica 48(2): 191-226.

Holtz, T.R. 2001. The phylogeny and taxonomy of the Tyrannosauridae. In D.H. Tanke and K. Carpenter (editors), Mesozoic Vertebrate Life: 64–83. Bloomington: Indiana University Press.

Hone, D.W.E., Wang, K., Sullivan, C., Zhao, X., Chen, Shuqing, Li, D., Ji, S., Ji, Q., and X. Xu. 2011. A new, large tyrannosaurine theropod from the Upper Cretaceous of China. Cretaceous Research 32:495-503.

Maleev, E.A. (1974). [Gigantic carnosaurs of the family Tyrannosauridae.]  Joint Soviet-Mongolian Palaeontological Expedition, Transactions 1, 132-191. (In Russian with English summary)

Peterson, J.E., Henderson, M.D., Scherer, R.P., and C.P. Vittore. 2009. Face-biting on a juvenile tyrannosaurid and behavioral implications. Palaios 24, 780-784.

Russell, D.A.  1970.  Tyrannosaurs from the Late Cretaceous of western Canada. National Museum of Natural Science Publications in Palaeontology 1: 1-34.

Tsuihiji T, M. Watabe, K. Togtbaatar, T. Tsubamoto, R. Barsbold, S. Suzuki, A. H. Lee, R. C. Ridgely, Y. Kawahara, and L. M. Witmer. 2011. Cranial osteology of a juvenile specimen of Tarbosaurus bataar (Theropoda, Tyrannosauridae) from the Nemegt Formation (Upper Cretaceous) of Bugin Tsav, Mongolia. Journal of Vertebrate Paleontology 31: 497–517.

Witmer, L.M. 1990. The extant phylogenetic bracket and the importance of reconstructing soft tissues. In Functional Morphology in Vertebrate Paleontology. Edited by J.J. Thomason. Cambridge University Process. pp. 19-33.

Witmer, L.M., and Baumel, J.J. 1993. Osteologia. In Handbook of Avian Anatomy: Nomina Anatomica Avium, Second Edition. Edited by J.J. Baumel, A.S. King, J.E. Breazile, H.E. Evans, and J.C. Vanden Berge. Publications of the Nuttall Ornithological Club. Cambridge, Massachusetts. pp. 44-132

Witmer, L.M.  1997.  The evolution of the antorbital cavity of archosaurs: a study in soft-tissue reconstruction in the fossil record with an analysis of the function of pneumaticity. Journal of Vertebrate Paleontology 17 (Suppl. to No. 1): 1-73.