Lambeia pectinatus, Mickle, 2017

Mickle, Kathryn E., 2017, The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species, Fossil Record 20 (1), pp. 47-67 : 55-62

publication ID	https://doi.org/ 10.5194/fr-20-47-2017
DOI	https://doi.org/10.5281/zenodo.13755779
persistent identifier	https://treatment.plazi.org/id/7C6F4264-FF81-9650-FCD4-FD8FA78C7856
treatment provided by	Felipe
scientific name	Lambeia pectinatus
status	gen. nov.

Treatment

Lambeia pectinatus n. gen. n. sp. ( Figs. 4–10 View Figure 4 View Figure 5 View Figure 6 View Figure 7 View Figure 8 View Figure 9 View Figure 10 )

Etymology: pectinatus in reference to the pectinations on the dorsal ridge scales and ventral and posterior margins of the scales.

Diagnosis (based on the unique combination of characters): large edentulous tuberculated ventral rostro-premaxilla; median dorsal rostral bone; maxilla with broad postorbital plate; complex ganoine ornamentation on maxilla; nasal bones with ganoine ornamentation of tubercles and short ridges ventrally, longer diagonally oriented ridges mid-bone; single rectangular-shaped supraorbital bone; numerous suborbital bones; dermopterotic as long as the parietal plus the post-parietal bones; presupracleithrum; dermohyal; series of accessory opercular bones; 12 branchiostegal rays; two lateral gular plates; six dorsal ridge scales beginning at scale row 20; first three dorsal ridge scales with pectinated posterior margins; dorsal ridge scales occupy the space of two body scale rows; body scales rows intermittently inserted between adjacent dorsal ridge scales; anal fin almost opposite dorsal fin; dorsal and anal fins posteriorly placed on the body; body depth dramatically decreases posterior to dorsal fin; large pectoral and pelvic fins; body scales with pectinated posterior margins and horizontal ganoine ridges; ventrally placed scales from scale row 5 to the end of pelvic fin have pectinated posterior and ventral margins.

Holotype and only specimen: YPM 8664 About YPM ( Figs. 4–10 View Figure 4 View Figure 5 View Figure 6 View Figure 7 View Figure 8 View Figure 9 View Figure 10 ). The holotype YPM 8664 About YPM preserves the anterior two-thirds of a rather large fish in lateral view ( Fig. 4 View Figure 4 ). The counterpart is missing. The caudal peduncle and fin are not preserved. Though the distal portion of the dorsal fin is missing, the proximal portion along the body is preserved and appears to be complete. The pectoral, pelvic, and anal fins are large and spectacularly preserved ( Fig. 4 View Figure 4 ). Though the specimen is not complete, it is a medium- to large-sized palaeoniscoid with a length of 19.5 cm, minus the caudal peduncle and fin. It is noted that this fish is preserved on a slab with the remains of three other smaller palaeoniscoids.

Type locality: Tournaisian (Lower Carboniferous) Albert Formation, New Brunswick, Canada.

4 Anatomical description

4.1 Snout

The snout is prominent and heavily tuberculated. A median dorsal rostral bone forms the anterior-most portion of the snout ( Figs. 5–6 View Figure 5 View Figure 6 ) The posterior margin of the median rostral bone contacts the parietal, whereas the ventral margin contacts the ventral rostro-premaxilla ( Figs. 5–6 View Figure 5 View Figure 6 ). The lateral margin of the median dorsal rostral is notched. This notch forms the median margin of the anterior narial opening. The median dorsal rostral bears tubercles ventrally and short ridges of ganoine dorsally. These ridges are longitudinal to diagonal in orientation ( Figs. 5–6 View Figure 5 View Figure 6 ).

A large nasal bone lies lateral to the median dorsal rostral and anterior to the orbit ( Figs. 5–6 View Figure 5 View Figure 6 ). The anterior margin of the nasal is notched. This notch forms the medial margin of the anterior narial opening. The posterior border of the nasal is also notched in two different locations. The ventralmost notch forms the anterior margin of the lateral/posterior narial opening. Dorsal to this notch, there is a protuberance that extends off the posterior margin. Dorsal to this protuberance is the second notch on the posterior margin of the nasal for the supraorbital bone ( Figs. 5–6 View Figure 5 View Figure 6 ). The nasal bears a complex pattern of ganoine. Unlike many other Carboniferous palaeoniscoids that bear long vertical ridges of ganoine, † Lambeia pectinatus has a nasal bone with tubercles and short ridges ventrally and longer diagonally oriented ridges mid-bone ( Figs. 5–6 View Figure 5 View Figure 6 ).

There is a heavily tuberculated bone ventral to the median rostral and nasal bones ( Figs. 5–6 View Figure 5 View Figure 6 ). This bone is identified here as the ventral rostro-premaxilla following the terminology of Mickle (2015). The anterior tip of the maxilla is ventral to the posteroventral margin of the ventral rostro-premaxilla. The ventral rostro-premaxilla does not bear teeth, though it is possible that small teeth are obscured by the heavy amount of tuberculations. No canal is visible in this bone, but this could also be because of the heavy ganoine tuberculations. It is termed a ventral rostro-premaxilla because the only criterion that can be used to identify this bone is its placement, information on the placement of canals in any of the snout bones is lacking because of the heavy ganoine ornamentation. The bone lies anterior to the maxilla, ventral to a median rostral bone, and separate from an antorbital bone. The size of this bone and placement suggest that it is not simply a premaxillary bone. This bone is physically located in the area where premaxillary and rostral bones are found.

Posterior to the ventral rostro-premaxilla, posteroventral to the nasal and dorsal to the anterior tip of the maxilla is an antorbital bone. This bone is referred to as an antorbital because of its position and the putative canals in this bone ( Figs. 5–6 View Figure 5 View Figure 6 ). The antorbital is roughly triangular in shape and there is a row of sensory pores, illustrated with filled gray circles in Fig. 6 View Figure 6 . The antorbital forms the anteroventral margin of the orbit.

4.2 Circumorbital series

Ventral to the orbit is a thin rectangular infraorbital bone ( Figs. 5–6 View Figure 5 View Figure 6 ). This rectangular bone is large enough to bear small tubercles of ganoine. This infraorbital bone contacts the posterior margin of the antorbital bone and the anterior margin of a large crescent-shaped infraorbital bone in the posteroventral corner of the orbit ( Figs. 5–6 View Figure 5 View Figure 6 ). The crescent-shaped infraorbital bone bears tubercles of ganoine and traces of the main infraorbital canal near the anterior border of the bone. There are pore canals that branch off the main infraorbital canal preserved near the posteroventral margin of the bone. This bone is disturbed and broken in half by the inward collapse of the dorsal half, but it can be reconstructed to its original crescent shape ( Figs. 5–6 View Figure 5 View Figure 6 ).

A single dermosphenotic is located in the posterodorsal corner of the orbit ( Figs. 5–6 View Figure 5 View Figure 6 ). The anterodorsal and posteroventral margins of this bone cannot be made out with any confidence, but it appears that this bone is narrower anterodorsally than posteroventrally. There are thin short ridges of ganoine at about mid-bone and elongated tubercles anterodorsally.

4.3 Skull roof

The dermosphenotic abuts against a large dermopterotic ( Figs. 5–6 View Figure 5 View Figure 6 ). The dermopterotic is ventral to the parietal and post-parietal bones and approximately the length of these bones combined. Dorsal of the orbit and posteroventral to the nasal bone is a rectangular bone ( Figs. 5–6 View Figure 5 View Figure 6 ). This bone is not a sclerotic bone – a separate sclerotic is preserved ventral to this bone in question ( Figs. 5–6 View Figure 5 View Figure 6 ). This rectangular bone bears short ridges of ganoine that are different in orientation and size from those on the nasal. This bone fills in the space created by the dorsal-most notch on the posterior margin of the nasal bone. This bone is identified as a supraorbital. The posterior margin of the supraorbital comes in contact with the anteroventral margin of the parietal.

The margins of the parietal bones are difficult to determine. The parietal contacts the nasal, dorsal rostral, and supraorbital bones anteriorly, the dermopterotic laterally, and the post-parietal posteriorly ( Figs. 5–6 View Figure 5 View Figure 6 ). The parietal bears short ridges of ganoine along the length of the bone and a few elongated tubercles. The post-parietal is trapezoidal in shape, with the medial margin of the bone being longer than the lateral margin ( Figs. 5–6 View Figure 5 View Figure 6 ). Pit lines are not apparent because of the heavy ganoine ridges present on this bone. The post-parietal is about a third of the length of the parietal.

A thin band of bone posterior to the post-parietal and the dermopterotic is an extrascapular bone ( Figs. 5–6 View Figure 5 View Figure 6 ). There is no ganoine ornamentation on this bone, nor can it be determined if this is a series of bones or a single bone.

4.4 Cheek

Posterior to the circumorbital bones lies a series of suborbital bones ( Figs. 5–6 View Figure 5 View Figure 6 ). Though this region is disturbed by the inward collapse of the infraorbitals and suborbitals, it is clear that there are numerous suborbital bones. The suborbitals are roughly arranged in vertical rows – the first row is posterior to the circumorbital bones, the second is between the first and third rows of suborbital bones, and the third row contacts the anterior margin of the preoperculum ( Figs. 5–6 View Figure 5 View Figure 6 ). The third row of suborbitals is composed of two large bones ( Figs. 5–6 View Figure 5 View Figure 6 ). The dorsal-most of the two large suborbitals has a rounded convex anterior margin. Ventral to this is a triangular suborbital bone with rounded corners. The anterior border of this suborbital bone is slightly concave. Both of these suborbital bones bear fine diagonal ridges of ganoine.

The second row of suborbitals is also composed of large bones. Two large bones with fine ganoine ridges are present and overlain in sections by the suborbital bones in rows 3 and 1 ( Figs. 5–6 View Figure 5 View Figure 6 ). The first row of suborbital bones is the area with the most disturbance. It seems that multiple smaller suborbital bones are located posterior to the dermosphenotic and infraorbital three ( Figs. 5–6 View Figure 5 View Figure 6 ).

The maxilla is a large bone with a deep and broad postorbital plate ( Figs. 5–6 View Figure 5 View Figure 6 ). A posteroventral process off the postorbital plate overlaps the posterodorsal margin of the lower jaw. The maxilla tapers to a narrow arm that extends anterior to the orbit. This narrow arm terminates ventral to the heavily tuberculated ventro–rostro-premaxilla. There are fine, minute, needle-like teeth on the oral margin of this portion of the maxilla. Large conical teeth are seen on the oral rim ventral to the postorbital plate, with small conical teeth inserted between the large ones.

The ganoine ornamentation of the maxilla is complex ( Figs. 5–6 View Figure 5 View Figure 6 ). The anterior-most portion of the maxilla, up to the anterior-most corner of the infraorbital in the posteroventral corner of the orbit, is heavily tuberculated with closely set tubercles. Below the crescent-shaped infraorbital, the maxilla bears short diagonal ridges of ganoine. The pattern of ganoine on the maxilla then changes to fine, faint, and more horizontally oriented ridges along the postorbital plate. Fine vertical ridges are present along the posteroventral process of the maxilla. Though the anteroventral margin of this process is disturbed, it appears that these vertical ridges of ganoine break down to fine tubercles at this margin. The ventral margin of the postorbital plate has its own ganoine pattern – here ornamentation consists of short, closely set, vermiform ridges that are horizontal to vertical in orientation. Directly ventral and posteroventral to the orbit, there is a narrow band along the dorsal-most border of the maxilla that is smooth and does not bear any ganoine ornamentation. This is an area of articulation between the maxilla and the overlying infraorbitals.

The preoperculum is hatchet shaped, anteriorly inclined, and contacts the dorsal and posterior margins of the postorbital plate of the maxilla ( Figs. 5–6 View Figure 5 View Figure 6 ). Dorsal to the maxilla, the preoperculum is expanded, whereas posterior to the maxilla, the preoperculum is a tall, narrow arm arched around the posterior margin of the maxilla. The anterior margin of the preoperculum sutures with two suborbitals. These suborbitals are situated within a concavity made by the arms of the expanded region of the preoperculum. There are short ganoine ridges along the posterior margin of the preoperculum and fine horizontal ridges on the expanded region of the preoperculum, dorsal to the maxilla.

Posterior to the preoperculum and anterior to the operculum is a tall and narrow wedge-shaped dermohyal ( Figs. 5– 6 View Figure 5 View Figure 6 ). The dermohyal extends from the anterodorsal corner of the operculum to about half the depth of this bone. The dermohyal bears short ridges of ganoine parallel with the anteroventral and posterodorsal margins of the bone. These ridges are similar to those found on the expanded region of the preoperculum. Posterior to the preoperculum, ventral to the dermohyal, and along the anterior border of the operculum is a series of accessory opercular bones. The largest bone of the series is found near the anteroventral corner of the operculum. This bone is wider ventrally than dorsally and bears diagonal ridges of ganoine. There are three accessory opercular bones dorsal to the expanded ventral bone. The dorsal accessory opercular bones are small and rhombic and bear faint ridges of ganoine.

4.5 Lower jaw

Individual bones that make up the lower jaw cannot be distinguished. Overall, the lower jaw is a large bone that is longer than the maxilla ( Figs. 5–6 View Figure 5 View Figure 6 ). The lower jaw extends slightly anterior to the ventral rostro-premaxilla. Vertically oriented conical teeth are along the oral rim of about the anterior half of the lower jaw. In between these teeth are smaller conical teeth. There are also teeth medial to this series of conical teeth. The medially placed teeth are conical, short, and closely set. Anteriorly, the lower jaw bears ganoine tuberculations. These tubercles are present until about the posterior margin of the ventral rostro-premaxilla. Posterior to the ventral rostro-premaxilla to the posterior margin of the median gular, the lower jaw is ornamented with short diagonal ridges. At the posterior-lateral margin of the median gular, there is a change in ganoine ornamentation on the lower jaw to fine and long horizontal ridges. Near the posterior margin of the lower jaw, these horizontal ridges curve dorsally towards the posteroventral process of the maxilla.

4.6 Operculo-gular apparatus

The operculum is a rectangular bone that is anteriorly inclined and about twice the depth of the suboperculum ( Figs. 5–6 View Figure 5 View Figure 6 ). The operculum bears fine diagonal ridges of ganoine that are not as closely packed as the ganoine ornamentation on other bones. The suboperculum is vertically oriented and rhombic in shape ( Figs. 5–6 View Figure 5 View Figure 6 ). There are short diagonal and vertical ganoine ridges on this bone. The suboperculum is taller posterodorsally than anterodorsally.

Gulars and branchiostegal rays are visible in lateral view ( Figs. 5–6 View Figure 5 View Figure 6 ). The proximal portion of the median gular closest to the lower jaw is missing so that only the distal tip of this bone can be commented upon. The distal portion of the median gular bears short ridges of ganoine and a few tubercles. Posterior to the median gular lies the first of two lateral gulars. Both lateral gulars are teardrop shaped and bear short ridges of ganoine. When seen in lateral view, these ridges are diagonal on the first lateral gular but more horizontally oriented on the second lateral gular. The second lateral gular bears a prominent pit line. Posterior to the lateral gulars follows a series of branchiostegal rays ( Figs. 5–6 View Figure 5 View Figure 6 ). The branchiostegals are obscured just anterior to the posteroventral corner of the lower jaw, making determinations of their number and shape difficult. Anterior to this point, there are two branchiostegal rays. Posterior to this point, there are seven rays. If the size of the branchiostegal rays anterior to the posteroventral corner of the lower jaw are consistent with those directly anterior and posterior to this area of ambiguity, the total number of branchiostegal rays is estimated to be around 12.

4.7 Pectoral girdle

The posttemporal is a large bone with a rounded posterior margin ( Figs. 5–6 View Figure 5 View Figure 6 ). The posttemporal bears prominent ridges of ganoine that extend to the posterior border of the bone to form a serrated posterior margin. The posttemporal overlaps the dorsal border of the ventrally located supracleithrum.

A rounded presupracleithrum is situated near the posterodorsal corner of the operculum, ventral to the posttemporal and overlapping the anterior margin of the supracleithrum ( Figs. 5–6 View Figure 5 View Figure 6 ). The presupracleithrum bears diagonal ridges of ganoine that extend to the posterior end of the bone, giving the presupracleithrum a serrated posterior margin. The supracleithrum lies posterior to the operculum, overlapped by the presupracleithrum and posttemporal. The supracleithrum is about the same depth as the operculum ( Figs. 5–6 View Figure 5 View Figure 6 ). At about two-thirds down the depth of the bone, the posterior margin of the supracleithrum is concave. The posterodorsal and posteroventral margins of the supracleithrum are convex. The supracleithrum bears strong ridges of ganoine. The ridges in the posterodorsal portion of the bone are curved, whereas the ornamentation on the anterodorsal portion of the bone consists of straight diagonal ridges. These ridges are more vertically oriented near the anterior border of the bone. The ridges in the ventral portion of the supracleithrum are slightly diagonal to vertical in orientation.

Ventral to the supracleithrum is a tall but narrow crescent-shaped postcleithrum ( Figs. 5–6 View Figure 5 View Figure 6 ). The postcleithrum bears short diagonal ridges on the dorsal half of the bone and vertical ridges down the ventral half. In the dorsal half of the bone, these ridges extend to the posterior margin, giving the bone a pectinated posterior margin. The smooth area anterior to the postcleithrum and posterior to the suboperculum is the cleithrum, but the shape of this bone cannot be determined.

4.8 Squamation

There is a series of large dorsal ridge scales anterior to the origin of the dorsal fin ( Figs. 4 View Figure 4 , 7 View Figure 7 ). The dorsal ridge scales are not continuous to the occiput; rather, they begin at scale row 20. The dorsal ridge scale series consists of six large scales. The posterior border of the preceding scale overlaps the anterior margin of the subsequent scale. The first dorsal ridge scale has more of an acuminate posterior margin compared to the subsequent scales with blunt and rounded posterior borders ( Fig. 7 View Figure 7 ). The first three dorsal ridge scales have serrated posterior margins ( Fig. 7 View Figure 7 ). These pectinations are formed by ridges of ganoine that run down the center of the ridge scales. The ganoine ridges on the lateral margin of these ridge scales are curved to follow the convex lateral margin of the scale.

The first and second dorsal ridge scales correspond to two ventrally placed rows of body scales ( Fig. 7 View Figure 7 ). Because of the overlap of the dorsal ridge scales, the second body scale row that is ventral to the posteroventral margin of the first dorsal ridge scale also overlaps the posterior margin of the second dorsal ridge scale. This gives the appearance of the body scale rows being inserted between the dorsal ridge scales ( Fig. 7 View Figure 7 ). This pattern is seen between dorsal ridge scale one and two, as well as two and three. This may indicate that the two vertical scale rows correspond to one myomere rather than a 1: 1 ratio of scale rows to myomeres. The third dorsal ridge scale is unique in that it is the only one of the six to correspond to just one body scale row. Dorsal ridge scales four through six all correspond to two body scale rows ( Fig. 7 View Figure 7 ). There are no pectinations on the posterior edges of dorsal ridge scales four through six. These ridge scales also differ in shape from the anterior three ridge scales. Ridge scales four through six do not have the same rounded appearance as the first three, and they have more pronounced convex posterior margins ( Fig. 7 View Figure 7 ).

It is questionable whether ridge scales are present between the pectoral and pelvic fins. Between the pectoral and pelvic fins there is an area of ambiguity caused by the body of a smaller palaeoniscoid overlapping the ventral margin of the larger specimen in YPM 8664. Partially visible are two rounded structures that do not bear pectinated posterior margins or ganoine ornamentation. These could potentially be ventral ridge scales between the pectoral and pelvic fins. There are enlarged scales anterior to the anal fin and potentially the vent of the fish.

In order to describe the body scales, the body has been broken down into different regions. These regions are detailed and illustrated in Fig. 8 View Figure 8 . In YPM 8664, scales in region A1 (dorsally placed scales posterior to the skull roof) are heavily ornamented with ridges of ganoine and have strongly pectinated posterior margins. Posterior to the posttemporal, the posteroventral margins of the scales have four to five serrations, but at the level of the supracleithrum, there is a change so that the entire posterior margin is pectinated. In region A2 (mid-body scales posterior to the pectoral girdle), scales are generally pectinated and bear diagonal ridges of closely set ganoine. These scales are rhombic at the level of the supracleithrum. At the level of the supracleithrum, at scale rows 1 through 3, there are diagonal ridges of ganoine dorsally and curved ridges of ganoine near the ventral border of the scale. Scales ventral to the supracleithrum at about the level of the postcleithrum are taller, rectangular, and narrower. These scales only bear diagonal ridges of ganoine. The scales bearing the lateral line are notched posteriorly. The notch is more superiorly placed in this region then in regions B2 or B3. The lateral-line-bearing scales are pectinated.

In region A3 (ventrally placed scales posterior to the pectoral girdle), the scales are rhombic, but there is a trend of the scales being narrower and more rectangular in shape the more ventral they are on the body. Regardless of their placement, all of the scales in the A3 region bear close-set diagonal ridges of ganoine.

Scales in region B commence at scale row 6. Scales in region B2 (mid-body scales from scale rows 6–12) are tall, narrow, and rectangular in shape. The posterior margins are pectinated; the pectinations are formed by the closely set diagonal ridges of ganoine that ornament the scales. The lateral-line-bearing scales are notched posteriorly.

Scales in region B3 (ventrally placed scales from scale rows 6–12) are very unique. Here, the ventral margins of the scales, as well as the posterior margins, are pectinated ( Fig. 9 View Figure 9 ). These scales also bear ridges of ganoine.

Scale region C starts at scale row 13. Scales in region C1 (dorsally placed scales from scale row 13 to origin of dorsal fin) are more teardrop shaped in appearance as compared to the anteriorly placed rhombic and rectangular scales. These scales bear diagonal ridges of ganoine. The posterior edges are sometimes pectinated with five to six serrations.

The posterior borders of scales in region C2 (mid-body scales from scale row 13 to origin of dorsal fin) are pectinated with closely packed fine serrations. The exact number is hard to determine because of how close the serrations are, but there are at least a dozen serrations per scale. The scales that are located at the level of the ventral portion of the supracleithrum are more rectangular in shape than the rhombic scales above and below this point. The lateral-line-bearing scales are noticeably notched posteriorly. This notch is located mid-scale.

Like the scales in region B3, the scales in region C3 (ventrally placed scales from row 13 to origin of dorsal fin) are serrated on both the posterior and ventral borders. These scales are ornamented with fine diagonal ridges of ganoine. The more ventrally placed scales are shorter and more rectangular in shape than the more dorsally placed rhombic scales in this region.

Scale region D begins at the origin of the dorsal fin. The scales in region D1 (dorsally placed scales from origin of dorsal fin to preserved end of specimen), are short but rectangular in shape. They are closely packed and overlapping. There are faint signs of horizontal ridges of ganoine. The first four scales ventral to the dorsal fin are slightly different – these scales are about 2 times the depth of the others and rhombic in shape.

Scales in region D2 (mid-body scales from origin of dorsal fin to preserved end of specimen) are rhombic and not as tall as the more anteriorly placed scales. The posterior edges of scales in region D2 are pectinated with six to seven serrations. The ganoine ornamentation is not as dramatic as that of the more anteriorly placed scales but there are faint horizontal to diagonal ridges. Scales in the region D3 (ventrally placed scales from origin of dorsal fin to preserved end of specimen) are similar to those described for region C3, but the scales in D3 lack the serrations on the ventral margin. There are a few scales in D3 that have serrations on the posterior margin.

4.9 Fins

The pectoral fin is large, fan-shaped, and formed by highly bifurcated and closely packed fin rays ( Fig. 10 View Figure 10 ). Fringing fulcra line the leading edge of the pectoral fin. The fulcra are thicker and longer proximally and decrease in size down the height of the fin so that the distal-most fringing fulcra are fine and short. Proximally, the fringing fulcra from the opposite side of the fin are seen. The two sides of the fulcra meet in midline to form a V-shaped unit.

All of the fin rays that make up the pectoral fin are segmented. The fin rays are bifurcated numerous times. The first bifurcation occurs in the proximal quarter of the fin. The fin rays bifurcate at least one more time distally so that the distal-most portion of the fin is made up of fine delicate fin rays. This makes determining how many times the fin rays bifurcate and detailed illustrations of the distal portion of the fin difficult. The first two fin rays do not extend down the entire depth of the fin to contribute to the distal margin, instead, the highly bifurcated fin rays posterior to the first two fin rays fill in and form the distal margin of the fin.

There is a large triangular pelvic fin that spans four scale rows and contains 25 fin rays ( Fig. 10 View Figure 10 ). The pelvic fin originates at scale row 12. Like the pectoral fin, the fin rays that form the pelvic fin are highly bifurcated. The first bifurcation occurs close to the proximal margin of the fin at about the second or third segment. At about mid-depth of the pelvic fin, the fin rays bifurcate again. Because of all the bifurcations, the distal region of the pelvic fin is made of very fine closely packed fin rays. There are fringing fulcra along the leading edge of the pelvic fin, but the fulcra are not as large or dramatic as that of the pectoral fin. The most proximal structure on the leading edge of the pelvic fin is different from the distal fringing fulcra – it is a single median structure that looks more like a ridge scale than the start of the fringing fulcra series.

The triangular anal fin originates posterior to the origin of the dorsal. The anal fin is large – spanning about 12 scale rows and containing 42 fin rays ( Fig. 10 View Figure 10 ). Like the other fins, the anal fin has highly bifurcated fin rays and fringing fulcra. The fringing fulcra are clearest on the leading edge of the distal portion of the fin, though it is presumed to be continuous along the entire anterior margin. The caudal fin is not preserved.