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+The Project Gutenberg EBook of A New Order of Fishlike Amphibia From the
+Pennsylvanian of Kansas, by Theodore H. Eaton and Peggy Lou Stewart
+
+This eBook is for the use of anyone anywhere at no cost and with
+almost no restrictions whatsoever. You may copy it, give it away or
+re-use it under the terms of the Project Gutenberg License included
+with this eBook or online at www.gutenberg.org
+
+
+Title: A New Order of Fishlike Amphibia From the Pennsylvanian of Kansas
+
+Author: Theodore H. Eaton
+ Peggy Lou Stewart
+
+Release Date: January 23, 2010 [EBook #31050]
+
+Language: English
+
+Character set encoding: ISO-8859-1
+
+*** START OF THIS PROJECT GUTENBERG EBOOK NEW ORDER OF FISHLIKE AMPHIBIA ***
+
+
+
+
+Produced by Chris Curnow, Joseph Cooper, Diane Monico, and
+the Online Distributed Proofreading Team at
+https://www.pgdp.net
+
+
+
+
+
+
+
+
+
+
+
+UNIVERSITY OF KANSAS PUBLICATIONS
+
+MUSEUM OF NATURAL HISTORY
+
+Volume 12, No. 4, pp. 217-240, 12 figs.
+May 2, 1960
+
+
+A New Order of Fishlike Amphibia
+From the Pennsylvanian of Kansas
+
+BY
+
+THEODORE H. EATON, JR., AND PEGGY LOU STEWART
+
+
+UNIVERSITY OF KANSAS
+LAWRENCE
+1960
+
+
+
+
+UNIVERSITY OF KANSAS PUBLICATIONS, MUSEUM OF NATURAL HISTORY
+
+Editors: E. Raymond Hall, Chairman, Henry S. Fitch,
+Robert W. Wilson
+
+
+Volume 12, No. 4, pp. 217-240, 12 figs.
+Published May 2, 1960
+
+
+UNIVERSITY OF KANSAS
+Lawrence, Kansas
+
+
+PRINTED IN
+THE STATE PRINTING PLANT
+TOPEKA, KANSAS
+1960
+
+28-2495
+
+
+
+
+A New Order of Fishlike Amphibia
+From the Pennsylvanian of Kansas
+
+BY
+
+THEODORE H. EATON, JR., AND PEGGY LOU STEWART
+
+INTRODUCTION
+
+
+A slab of shale obtained in 1955 by Mr. Russell R. Camp from a
+Pennsylvanian lagoon-deposit in Anderson County, Kansas, has yielded in
+the laboratory a skeleton of the small amphibian _Hesperoherpeton
+garnettense_ Peabody (1958). This skeleton provides new and surprising
+information not available from the holotype, No. 9976 K. U., which
+consisted only of a scapulocoracoid, neural arch, and rib fragment. The
+new specimen, No. 10295 K. U., is of the same size and stage of
+development as the holotype and it is thought that both individuals are
+adults.
+
+The quarry, University of Kansas Museum of Natural History Locality KAN
+1/D, is approximately six miles northwest of Garnett, Anderson County,
+Kansas, in Sec. 5, T. 19S, R. 19E, 200 yards southwest of the place
+where _Petrolacosaurus kansensis_ Lane was obtained (see Peabody,
+1952). The Rock Lake shale, deposited under alternately marine and
+freshwater lagoon conditions, is a thin member of the Stanton limestone
+formation, Lansing group, Missourian series, and thus is in the lower
+part of the Upper Pennsylvanian.
+
+Peabody (1958) placed _Hesperoherpeton_ in the order Anthracosauria,
+suborder Embolomeri, family Cricotidae. Study of the second and more
+complete specimen reveals that _Hesperoherpeton_ is unlike the known
+Embolomeri in many important features. The limbs and braincase are more
+primitive than those so far described in any amphibian. The vertebrae
+are comparable to those of Ichthyostegalia (Jarvik, 1952), as well as
+to those of Embolomeri. The forelimb is transitional between the
+pectoral fin of Rhipidistia and the limb of early Amphibia. The pattern
+of the bones of the forelimb closely resembles, but is simpler than,
+that of the hypothetical transitional type suggested by Eaton (1951).
+The foot seemingly had only four short digits. The hind limb is not
+known.
+
+The new skeleton of _Hesperoherpeton_ lies in an oblong block of limy
+shale measuring approximately 100 × 60 mm. After preparation of the
+entire lower surface, the exposed bones and matrix were embedded in
+Bioplastic, in a layer thin enough for visibility but giving firm
+support. Then the specimen was inverted and the matrix removed from the
+opposite side; this has not been covered with Bioplastic. The bones lie
+in great disorder, except that some parts of the roof of the skull are
+associated, and the middle section of the vertebral column is
+approximately in place. The bones of the left forelimb are close
+together but not in a natural position. The tail, pelvis, hind limbs
+and right forelimb are missing. Nearly all the bones present are
+broken, distorted by crushing, incomplete and scattered out of place,
+probably by the action of currents. The complete skeleton, in life,
+probably measured between 150 and 200 mm. in length.
+
+The specimen was studied at the Museum of Natural History, University
+of Kansas, with the help of a grant from the National Science
+Foundation, number NSF-G8624. The specimen was discovered in the slab
+by Miss Sharon K. Moriarty, and was further cleaned by the authors. Mr.
+Merton C. Bowman assisted with the illustrations. We are indebted to
+Dr. Robert W. Wilson for critical comments.
+
+
+SKULL
+
+_Dorsal Aspect_ (Figs. 1, 2)
+
+In reconstruction, the skull measures approximately 8.0 mm.
+dorsoventrally at the posterior end. The height diminishes anteriorly
+to about 1.5 mm. at the premaxillary. The length is about 15.5 mm. in
+the median line, or 24.0 mm. to the tip of the tabular, and the width
+about 16.0 mm. posteriorly. The snout is blunt, continuing about 1-2
+mm. anterior to the external nares. Each of the tabulars has a slender
+posterior process 5.0 mm. long, which probably met the supracleithrum;
+the intertabular space is about 8.5 mm. wide. The orbits are
+approximately 5.5 mm. in diameter and extend from the maxillary to
+within about 3.0 mm. of the midline dorsally. The pineal opening is 1.8
+mm. anterior to the occipital margin of the skull.
+
+Reduction of bones at the back of the skull seems to have eliminated
+any dermal elements posterior to the squamosal, while enlargement of
+the orbit has removed most of the postorbital series, leaving the
+squamosal as the only cheekbone. There is apparently no jugal or
+postfrontal.
+
+The squamosal of _Acanthostega_ (Jarvik, 1952) is articulated under the
+tabular and reaches forward and down, much as if it were an opercular
+in reversed position. Internally, it must lie against the otic capsule
+below the tabular, partially concealing the stapes. The bone that we
+suppose to be the squamosal of _H. garnettense_ is of similar shape, of
+about the same size and has internally an articular surface at one
+corner, bounded by a pair of ridges in the shape of a V. This articular
+surface probably fitted on a lateral process extending from the roof of
+the neurocranium, over the front of the otic capsule.
+
+The premaxillary extends posterolaterally to a distance 5.5 mm. from
+the midline and attains a width at its broadest point of about 1.5 mm.
+The posterior edge is slightly concave and in part forms the anterior
+border of the naris.
+
+[Illustration: FIG. 1. _Hesperoherpeton garnettense_ Peabody. Skull,
+dorsal view. Postorbital processes of the neurocranium are shown in
+dotted outline. KU 10295, × 4.]
+
+The nasal is triangular and, with the lacrimal, forms the medial border
+of the naris. The length of the medial side of the nasal bone is
+approximately 5.0 mm., the transverse width is 3.8 mm., and the extent
+of the posterolateral border is 5.5 mm.
+
+The maxillary meets the premaxillary lateral to the naris, borders the
+naris posteroventrally, and continues posteriorly beneath the orbit, of
+which it forms the external border. The maxillary is about 8.5 mm.
+long, and immediately anterior to the orbit has a maximum width of 1.3
+mm.
+
+The lacrimal fills the remaining rim of the narial opening between the
+nasal and maxillary, and extends to the anterior edge of the orbit. The
+length, from naris to orbit, is 4.2 mm.; the width ranges from 1.0 mm.
+anteriorly to 2.5 mm. posteriorly.
+
+[Illustration: FIG. 2. _Hesperoherpeton garnettense_ Peabody. Skull,
+lateral view, showing relatively large orbit and absence of smaller
+circumorbital bones. KU 10295, × 4.]
+
+The external naris is approximately 1.0 mm. in diameter. It is slightly
+anterodorsal to the internal naris and 4.0 mm. lateral to the midline.
+
+The dorsal margin of the orbit appears to be formed by the frontal. The
+anterior part of this margin, however, may be formed by a prefrontal,
+which is not clearly set off by a suture. The frontal extends 3.8 mm.
+in the midline, and anteriorly and laterally borders the nasal and
+lacrimal, respectively. A faint pattern of pitting radiates on the
+surface from the center of ossification of the frontal. There is also a
+pit indicating the presence of a supraorbital sensory pore.
+
+The parietal bones enclose the pineal opening, approximately 2.5 mm.
+posterior to the suture with the frontal. The foramen is about 0.5 mm.
+in diameter. Laterally the parietal meets the medial angle of the
+postorbital and the medial border of the supratemporal. No bone of this
+animal shows the deep pitting and heavy ornamentation characteristic of
+many primitive Amphibia.
+
+The postorbital meets the anterolateral corner of the parietal for a
+distance of 0.5 mm., the anterior edge bordering the frontal bone and
+the orbit for a combined distance of about 3.0 mm. The lateral margin
+is slightly convex, and is probably interrupted behind by the anterior
+point of the tabular. Medially, the concave margin of the postorbital
+meets the supratemporal for about 3.5 mm.
+
+The supratemporal is thus wedge-shaped and located between the parietal
+and the postorbital. The posterior edge of the supratemporal protrudes
+as a convex border slightly behind the end of the parietal, and
+measures 3.0 mm. around the curve to the parietal suture.
+
+[Illustration: FIG. 3. _Hesperoherpeton garnettense_ Peabody. A, left
+squamosal, internal surface. B, left squamosal, external surface. C,
+right tabular internal surface. D, right tabular, external surface. KU
+10295, all × 4.]
+
+The squamosal (Fig. 3 A, B) is a large, somewhat rectangular bone
+extending from the back of the orbit to the posterior extremity of the
+cheek. It outlines almost entirely the posterior border of the orbit,
+the ventrolateral portion of the cheek region, and the lateral border
+of the top of the skull behind the orbit. Dorsally, the squamosal meets
+the anterior half of the tabular and the lateral border of the
+supratemporal. Near the anteroventral edge of the squamosal there is a
+small pit, probably related to a postorbital sensory pore in the skin.
+
+The tabular (Fig. 3 C, D) is pointed anteriorly, where it probably fits
+against the lateroposterior edge of the postorbital. The dorsal part of
+the bone flares out and down, forming a small otic notch at a point
+halfway back. Posteriorly, the flange attains a dorsoventral width of
+2.0 mm. at the edge of the notch. The slender posterior process of the
+tabular which continues beyond the flange is approximately 0.5 mm. in
+diameter and 5.0 mm. long.
+
+_Ventral Aspect_ (Fig. 4)
+
+The palatal view of the skull shows the paired premaxillary, maxillary,
+palatine, pterygoid, and quadrate bones. The openings for the internal
+nares, the ventral orbital fenestrae, and the subtemporal fossae are
+readily recognized. The quadrate processes extend posteriorly leaving a
+large gap medially at the posterior end of the skull.
+
+[Illustration: FIG. 4. _Hesperoherpeton garnettense_ Peabody. Palate
+reconstructed; ventral aspect at left, showing teeth, dorsal aspect at
+right. KU 10295, × 4.]
+
+The left quadrate appears to be in place on the posterior prong of the
+pterygoid. The dorsal side of the quadrate is grooved between two
+anterolaterally directed ridges. The groove, which probably held the
+end of the stapes, extends about half the width of the quadrate itself.
+The width of the quadrate is 4.0 mm., the length is 4.5 mm. medially
+and about 2.0 mm. laterally. In ventral view the quadrate appears to
+project laterally, but is incomplete and its shape uncertain. The
+distance from the posterior end of the quadrate to the visible
+posterior edge of the orbital fenestra, which opens ventrally, is 10.0
+mm.
+
+This region between the quadrate and the orbit is occupied by a
+pterygoid with three projections. Anteriorly, the pterygoid outlines
+most of the posterior edge of the orbit (a distance of about 6.5 mm.).
+A lateral process separates the orbit from the subtemporal fossa. A
+posteriorly directed edge defines the fossa, which extends about 6.5
+mm. anteroposteriorly. The lateral process of the pterygoid terminates
+10.0 mm. from the midline. Both the lateral and posterior pterygoid
+processes are approximately 2.0 mm. wide. The greatest width of the
+subtemporal fossa is about 2.0 mm. The medial border of the orbital
+fenestra is missing, but apparently consisted of the pterygoid for at
+least the posterior half.
+
+Along the posterior edge of the orbital fenestra, there is a narrow,
+dorsally projecting flange of the pterygoid. The lateral opening of the
+orbit is approximately 7.5 mm. wide.
+
+The remaining border of the orbital fenestra on the anterior and medial
+sides is formed by a bone occupying the position of palatine and vomer;
+for convenience we designate this as palatine. When reconstructed in
+its probable position in relation to the pterygoid, the left palatine
+lacks a section, on its medial and posterior edges, measuring about 2.5
+mm. by 9.0 mm. The lateral margin of the palatine is convex; about 5.5
+mm. anterior to the orbit this margin curves into a strong anteriorly
+pointing projection, medial to which is seen the internal narial
+opening. The remaining anterior edge is slightly convex, smoothly
+rounded, and meets the midline about 9.0 mm. anterior to the pterygoid.
+
+The void area medial to the palatine and anterior to the pterygoid does
+not fit any bone which we can recognize as the parasphenoid. It is thus
+suspected that this area is covered in part by the missing edge of the
+palatine and partly by an anteromedial extension of the pterygoid. Of
+course a parasphenoid may also have been present.
+
+The position, length, and shape of the premaxillary shown in palatal
+view (Fig. 4) are primarily based upon the dorsal appearance since
+ventrally most of it cannot be seen. At the point where it forms the
+anterior border of the internal naris, the premaxillary is slightly
+wider than the maxillary and seems to become narrower as it approaches
+the midline.
+
+The ethmosphenoid, which we cannot identify, may have been exposed in a
+gap between the premaxillary and the palatine. The gap measures
+approximately 8.0 mm. wide and ranges up to 1.0 mm. anteroposteriorly.
+
+The maxillary begins at a suture with the premaxillary lateral to the
+naris and continues posteriorly, bordering the orbit with a width of
+about 1.2 mm. It then tapers to a point approximately 2.0 mm. anterior
+to the lateral projection of the pterygoid. The width of the maxillary
+at this point is 0.8 mm. and the posterior end is broken; probably when
+complete it approached the pterygoid, and either met the latter or had
+a ligamentous connection with it. As nearly as can be determined, the
+total length of the maxillary is approximately 12.0 mm.
+
+The teeth on the maxillary are small and seem to be in two longitudinal
+rows. The palatine bears two large, grooved teeth anteriorly; the first
+is approximately 1.0 mm. posteromedial to the naris and the second is
+about 3.0 mm. posterior and slightly lateral to the naris. The flat
+ventral surfaces of the palatine and pterygoid bear numerous small
+teeth distributed as shown in Fig. 4.
+
+_Braincase and Occipital Region_ (Fig. 5)
+
+The parts of the neurocranium are scattered, disconnected and
+incomplete, but it is possible to make out a number of features of the
+otico-occipital section with fair assurance. In posterior view the
+notochordal canal and foramen magnum are confluent with each other, and
+of great size relative to the skull as a whole. The notochordal canal
+measures 2.8 mm. in diameter, and the foramen magnum about 4.0 mm. The
+crescent-shaped supraoccipital rests on the upright ends of the
+exoccipitals, but between the latter and the basioccipital no sutures
+can be seen. Probably the whole posterior surface of the braincase
+slanted posteroventrally; consequently the rim of the notochordal canal
+was about 3.0 mm. behind the margin of the parietals.
+
+The U-shaped border of the notochordal canal is a thick, rounded bone,
+comparable in appearance to the U-shaped intercentra of the vertebrae.
+This bone apparently rested upon a thinner, troughlike piece (Fig. 5 B)
+forming the floor of the braincase. The latter is broad, shallow,
+concave, open midventrally and narrowing anteriorly to form a pair of
+articular processes. Since no sutures can be seen in this structure, it
+probably is the ventral, ossified portion of the basioccipital. Watson
+(1926, Fig. 4 B) illustrates the floor of the braincase in
+_Eusthenopteron_, with its more lateral, anterior portion labelled
+prootic, but in our specimen the corresponding part could scarcely have
+formed the anterior wall of the otic capsule, being entirely in the
+plane of the floor. The two articular surfaces anteriorly near the
+midline suggest that a movable joint existed between the
+otico-occipital part of the braincase and the ethmosphenoid part, as in
+Rhipidistia (Romer, 1937). We have found nothing in the specimen that
+could be referred to the ethmosphenoid; it may have been unossified.
+
+[Illustration: FIG. 5. _Hesperoherpeton garnettense_ Peabody, KU 10295,
+× 4. A, occipital view of skull; B, basioccipital bone in dorsal
+(internal) view.]
+
+The otic capsules appear to have rested against lateral projections of
+the basioccipital. The single otic capsule that can be seen (the
+right) is massively built, apparently ossified in one piece, with a
+shallow dorsomedial excavation, probably the vestige of a supratemporal
+fossa. On the lateral face is a broad, shallow depression dorsally, and
+a narrower, deeper one anteroventrally; these we suppose to have
+received the broader and narrower heads of the stapes, respectively.
+The posterior wall of the otic capsule we have designated opisthotic in
+the figure. Anterior to the otic capsule the lateral wall of the
+braincase cannot be seen, and may not have been ossified.
+
+The roof of the braincase is visible in its ventral aspect, extending
+from approximately the occipital margin to a broken edge in front of
+the parietal foramen, and laterally to paired processes which overlie
+the otic capsules directly behind the orbits (see dotted outlines in
+Fig. 1). Each of these postorbital processes, seen from beneath,
+appears to be the lateral extension of a shallow groove beginning near
+the midline. Presumably this section of the roof is an ossification of
+the synotic tectum. It should be noted that the roof of the braincase
+proper is perfectly distinct from the overlying series of dermal bones,
+and that the parietal foramen can be seen in both. The roof of the
+braincase in our specimen seems to have been detached from the
+underlying otic capsules and the occipital wall.
+
+The bone that we take to be the stapes is blunt, flattened (perhaps by
+crushing), 5.0 mm. in length, and has two unequal heads; its width
+across both of these is 4.0 mm. The length is appropriate to fit
+between the lateral face of the otic capsule and the dorsal edge of the
+quadrate; the wider head rests on a posterodorsal concavity on the otic
+capsule, and the smaller fits a lower, more anterior pit. Laterally the
+stapes carries a short, broad process that probably made contact with a
+dorsally placed tympanic membrane. Thus the bone was a hyomandibular in
+the sense that it articulated with the quadrate, but it may also have
+served as a stapes in sound-transmission. It contains no visible canal
+or foramen.
+
+_Mandible_ (Fig. 6)
+
+The crushed inner surface of the posterior part of the left mandible
+and most of the external surface of the right mandible are preserved in
+close proximity. Although the whole length of the tooth-bearing margins
+is missing, some parts of six elements of the right mandible can be
+seen. The pattern of sutures and the general contour closely resemble
+those of _Megalichthys_ (Watson, 1926, Figs. 37, 38) and other known
+Rhipidistia.
+
+The anteroposterior length of the mandible is about 23.8 mm., and the
+depth is 3.8 mm. The dentary extends approximately 17.6 mm. back from
+the symphysis, and its greatest width is probably 2.0 mm. Its lower
+edge meets all the other lateral bones of the jaw. The splenial and
+postsplenial form the curved anteroventral half of the jaw for a
+distance of about 9.0 mm. The fragmented articular, on the posterior
+end of the jaw, is 4.0 mm. long and 2.0 mm. deep, exhibiting a broken
+upper edge; presumably the surface for articulation with the quadrate
+was a shallow concavity, above the end of the articular.
+
+[Illustration: FIG. 6. _Hesperoherpeton garnettense_ Peabody. Right
+mandible, lateral view, KU 10295, × 4. External surfaces are pitted;
+broken surfaces are coarsely stippled.]
+
+
+VERTEBRAE (Fig. 7)
+
+The vertebrae that are visible from a lateral view are crushed and
+difficult to interpret. It is possible, nevertheless, to see that the
+trunk vertebrae resemble those of Ichthyostegalia (Jarvik, 1952, Fig.
+13 A, B), except that the pleurocentra are much larger. A few parts of
+additional vertebrae can be seen, but they are so scattered that it is
+impossible to be sure of their original location. Therefore comparisons
+between different regions cannot yet be made.
+
+The U-shaped intercentrum encloses the notochord and occupies an
+anteroventral position in the vertebra. Anteriorly, each intercentrum
+articulates with the pleurocentra of the next preceding vertebra by
+slightly concave surfaces. Dorsolaterally there is an articular surface
+for the capitulum of the rib.
+
+The two pleurocentra of each vertebra are separate ventrally as well as
+dorsally, but form thin, broad plates of about the same height as the
+notochord. The lateral surface appears to be depressed, allowing,
+perhaps, for movement of the rib. Above each pleurocentrum, on the
+lateral surface of the neural arch, there is a short diapophysis for
+articulation with the tuberculum of the rib.
+
+The margin of the neural spine is convex anteriorly and concave
+posteriorly, the tip reaching a point vertically above the
+postzygapophysis. The prezygapophysis of each vertebra articulates
+with the preceding postzygapophysis by a smooth dorsal surface. One
+nearly complete neural arch shows (Fig. 7 B) a pit above the neural
+canal, clearly corresponding to the canal for a dorsal ligament shown
+by Jarvik in _Ichthyostega_. Indeed this view of the neural arch and
+intercentrum together brings out the striking resemblance between the
+vertebrae of _Hesperoherpeton_ and those of the Ichthyostegids. The
+rounded intercentrum in both is an incomplete ring enclosing the
+notochordal canal.
+
+[Illustration: FIG. 7. _Hesperoherpeton garnettense_ Peabody. A, End
+view of incomplete vertebra, probably near anterior end of column. B,
+Neural arch and intercentrum in end view, showing probable association.
+C, Left lateral view of trunk vertebra. All figures: KU 10295, × 4.]
+
+TABLE 1.--AVERAGE MEASUREMENTS OF THE TRUNK VERTEBRAE (in mm.).
+NUMBERS IN PARENTHESES INDICATE THE NUMBER OF PIECES AVAILABLE FOR
+MEASURING
+
+----------------------------+------------+-------------+---------------
+ PARTS | Ant.-post. | Dors.-vent. | Transv. width
+----------------------------+------------+-------------+---------------
+Neural spine | 1.5 (3) | 3.0 (3) | --
+----------------------------+------------+-------------+---------------
+Neural spine and arch | 2.0 (4) | 4.5? (4) | --
+----------------------------+------------+-------------+---------------
+Neural canal | 2.0 (4) | 2.0 (1) | 1.0 (1)
+----------------------------+------------+-------------+---------------
+Intercentrum | 1.5 (5) | 3.5 (4) | 3.0 (1)
+----------------------------+------------+-------------+---------------
+Pleurocentrum | 1.5 (3) | 3.0 (2) | --
+----------------------------+------------+-------------+---------------
+
+The shape, in end view, of a partly preserved neural arch (Fig. 7 A)
+seems to account for the incompleteness of the intercentrum just
+mentioned; the ventral edge of the arch is emarginate in such a way as
+to fit the dorsal surface of the notochord. The dorsal portion of this
+neural arch is not present (either broken or not yet ossified), but
+the opening of the neural canal is comparable in width to the foramen
+magnum. Hence this vertebra may be one of the most anterior in the
+column. In comparison with the trunk vertebrae seen farther posteriorly
+it appears that there may be a progressive ossification of neural
+arches toward their dorsal ends, and of intercentra around the
+notochord, with probable fusion of the intercentra and neural arches in
+the posterior part of the trunk. The notochord seems to have been
+slightly constricted by the intercentra, but not interrupted.
+
+
+RIBS
+
+The proximal ends of the ribs expand dorsoventrally to a width
+approximately four times that of their slender shafts. The tuberculum
+and capitulum on each of the trunk ribs are separated only by a shallow
+concavity. These two articular surfaces are so situated that the rib
+must tilt downward from the horizontal plane. The shaft flares
+terminally in some ribs, and the distal end is convex. Ribs in the
+trunk region differ little if any in size. Five that can be measured
+vary in length from 5.0 to 7.0 mm. One short, bent rib 3.5 mm. long
+perhaps is sacral or caudal.
+
+
+PECTORAL GIRDLE (Figs. 8, 9, 10)
+
+The right scapulocoracoid is almost complete, and the left one is
+present but partly broken into three pieces, somewhat pushed out of
+position. With the advantage of this new material, we may comment on
+the scapulocoracoid of _H. garnettense_ as described by Peabody (1958).
+In size and contour, the slight differences between the type (KU 9976)
+and the new skeleton (KU 10295) are considered to be no more than
+individual variation. We have redrawn the type (Fig. 8) in order to
+show the resemblances more clearly.
+
+The small sections that were missing from the type are present in KU
+10295. The jagged edge directly posterior to the area occupied by the
+neural arch in the type extends 0.5 mm. farther back in our specimen.
+The angle formed between the recurved dorsal ramus and the edge of the
+ventral flange is seen in our specimen to be less than 90°. The glenoid
+fossa, appearing as a concave articular surface for the cap of the
+humerus, was in part covered by cartilage and shows as "unfinished"
+bone (Peabody, 1958, p. 572); this area is more oval than triangular,
+as Peabody thought. The obstruction of a clear view of this part of the
+type is the result of the accidental position of a neural arch. The
+raised portion immediately dorsal to the glenoid fossa exhibits an
+unfinished surface, suggesting the presence of either cartilage or a
+ligament.
+
+[Illustration: FIG. 8. _Hesperoherpeton garnettense_ Peabody. Type
+specimen redrawn. Right scapulocoracoid in external view (at left), and
+internal view (at right). KU 9976, × 4.]
+
+
+[Illustration: FIG. 9. _Hesperoherpeton garnettense_ Peabody. Right
+scapulocoracoid in external view, showing part of interclavicle, and
+position occupied by clavicle. The specimen is flattened and lies
+entirely in one plane. KU 10295, × 4.]
+
+
+[Illustration: FIG. 10. _Hesperoherpeton garnettense_ Peabody. Right
+clavicle in external view. Anterior edge to right. KU 10295, × 4.]
+
+The right clavicle is complete, and resembles a spoon having a slender
+handle. The dorsal tip of the handle is L-shaped. The expanded ventral
+part is convex externally, and rested upon the anteroventral surface of
+the scapulocoracoid. The lateral edge next to the "stem" is distinctly
+concave, abruptly becoming similar in contour to the opposite edge, and
+giving the impression of an unsymmetrical spoon. The left clavicle is
+present in scattered fragments, its dorsal hooklike end being intact.
+
+The posterior end of the interclavicle lies in contact with the right
+scapulocoracoid. There are short lateral processes at the point where
+the interclavicle was overlapped by the clavicles, but we cannot be
+sure of the extent of this bone anteriorly or posteriorly.
+
+The presumed left cleithrum, a long rectangle, is approximately equal
+in length to the rodlike stem of the clavicle, and is about as wide as
+the dorsal L-shaped tip of the clavicle. The posterior end of the
+cleithrum presumably met the tip of the clavicle, while the rest of it
+was directed anteriorly and a little dorsally. There seems to be a
+small articular surface near the anterior extremity which suggests the
+presence of a supracleithrum. The upper border of the cleithrum is
+slightly convex and the lower concave.
+
+
+FORELIMB (Fig. 11)
+
+The left forelimb is the only one present and appears to be nearly
+complete, although the elements are scattered almost at random. The
+only parts of the forelimb known to be missing are two subterminal and
+two terminal phalanges, probably of the first and third digits, and the
+proximal end of the second metacarpal. The smooth and relatively flat
+surfaces suggest an aquatic rather than terrestrial limb; only the
+proximal half of the humerus bears any conspicuous ridges or
+depressions. As we restore the skeleton of the limb, several features
+are remarkable: The humerus, ulna, and ulnare align themselves as the
+major axis of the limb, each carrying on its posterior edge a process
+or flange comparable to those in the axial series of a rhipidistian
+fin. The remaining elements take positions comparable to the diagonally
+placed preaxial radials in such a fin. The digits appear to have been
+short, perhaps with no more than two phalanges. There is only one row
+of carpals present (the proximal row of other tetrapods). A second and
+third row would be expected in primitive Amphibia; if they existed in
+_Hesperoherpeton_ they must either have been wholly cartilaginous or
+washed away from the specimen. Neither of these alternatives seems at
+all likely to us in view of the well-ossified condition of the elements
+that are present, and the occurrence of both the proximal carpals and
+the metacarpals. The space available for metacarpals probably could not
+have contained more than the four that are recognized.
+
+[Illustration: FIG. 11. _Hesperoherpeton garnettense_ Peabody. Left
+forelimb, showing characters of both a crossopterygian fin and an
+amphibian foot. KU 10295, × 4.]
+
+The proximal end of the humerus is more rounded anteriorly than
+posteriorly, and has a thin articular border that bore a cartilaginous
+cap as the primary surface for articulation with the scapulocoracoid.
+Although the unfinished surface of the head extends down the anterior
+margin about a third the length of the humerus, the shaft has been
+broken and so twisted that the distal part is not in the same plane as
+the proximal. Immediately posterior to the cartilaginous cap is a
+round, deep notch bordered posteriorly by the dorsal process of the
+head.
+
+The shaft is longer and narrower than would be anticipated in a
+primitive amphibian limb (cf. Romer, 1947). The distal end bears two
+surfaces for articulation with the radius and ulna. The full extent of
+the former surface was not determined because the more anterior part of
+the expanded end is represented only by an impression. The surface
+nearest the ulna was partially rounded for articulation with that
+element, the remaining posterior edge being broadly concave. The most
+striking feature of the humerus is a slender hooklike process on the
+posterior edge near the distal end, probably homologous with (1) the
+posterior flange on the "humerus" in Rhipidistia, and (2) the
+entepicondyle of the humerus in _Archeria_ (Romer, 1957) and other
+tetrapods.
+
+The radius is about the same width proximally as distally. The
+curvature of the shaft is approximately alike on both sides. Distally
+the surface is rounded for articulation with the radiale and perhaps
+the intermedium.
+
+The proximal end of the ulna is similar to that of the radius but is
+slightly larger. Posteriorly, there is a short, broad expansion
+resembling the entepicondyle of the humerus, and even more nearly like
+the postaxial flanges in a crossopterygian fin.
+
+The ends of the radiale are expanded and rounded, the entire bone being
+approximately twice as long as wide. The three sides of the intermedium
+are similarly convex. The surface of this bone is unfinished, showing
+that it must have been embedded in cartilage. The ulnare is
+conspicuously similar to the ulna in bearing a posterior hooklike
+expansion, and is larger than the radiale.
+
+The four metacarpals are slightly expanded proximally and distally.
+Although measurements of length and width are tabulated below (Table
+2), we are not certain of the sequence of these bones in the row.
+
+The dimensions of the two proximal phalanges are alike. The shape of
+these elements is similar to that of the metacarpals. The two terminal
+phalanges are somewhat triangular in shape, the lateral edges being
+concave and the proximal convex.
+
+TABLE 2.--APPROXIMATE MEASUREMENTS OF THE FORELIMB (in mm.)
+
+--------------------------+-------------------------------------------
+ | Dimensions
+ +----------+--------------------------------
+ ELEMENT | | Width
+ | Length +----------+----------+----------
+ | | Proximal | Midway | Distal
+--------------------------+----------+----------+----------+----------
+Humerus | 16.0 | 5.0 | 2.0 | 7.5?
+Radius | 9.0 | 4.0 | 1.5 | 3.5
+Ulna | 8.5 | 4.5 | 1.5 | 3.5
+Radiale | 3.0 | 2.0 | 1.5 | 2.0
+Intermedium | 1.5 | -- | 2.0 | --
+Ulnare | 3.5 | 2.0 | 2.0 | 2.5
+Metacarpal A | 4.5 | 2.5 | 1.0 | 2.0
+Metacarpal B | 4.5 | 3.0? | 1.5 | 2.5
+Metacarpal C | 4.0 | 2.0 | 1.5 | 2.0
+Metacarpal D | 3.5 | 2.5 | 1.0 | 1.5
+Proximal Phalanx A | 2.0 | 1.5 | 1.0 | 1.5
+Proximal Phalanx B | 2.0 | 1.5 | 1.0 | 1.5
+Terminal Phalanx A | 1.5 | 1.5 | 1.0 | 1.0
+Terminal Phalanx B | 1.5 | 1.5 | 1.0 | 1.0
+--------------------------+----------+----------+----------+----------
+
+
+COMPARISONS AND DISCUSSION
+
+Apparently primitive rhipidistian characters in _Hesperoherpeton_ are:
+Braincase in two sections, posterior one containing an expanded
+notochordal canal; lateral series of mandibular bones closely
+resembling that of _Megalichthys_, as figured by Watson (1926); tabular
+having long process probably articulating with pectoral girdle; lack of
+movement between head and trunk correlated with absence of occipital
+condyle; sensory pits present on frontal and squamosal.
+
+Although we are unable to separate, by sutures, the vomers from the
+palatines, the palatal surface of these bones and of the pterygoids is
+studded by numerous small teeth, as in Rhipidistia (Jarvik, 1954) and
+some of the early Amphibia (Romer, 1947). The stapes apparently reaches
+the quadrate, and could therefore serve in hyostylic suspension of the
+upper jaw.
+
+The pectoral limb has an axial series of bones carrying hooklike
+flanges on their posterior edges. The other bones of the limb show
+little modification of form beyond the nearly flat, aquatic type seen
+in Rhipidistia. No distinct elbow or wrist joints are developed.
+
+Characters of _Hesperoherpeton_ common to most primitive Amphibia, in
+contrast with Crossopterygii, are: Nares separated from edge of jaw;
+stapes having external process that may have met a tympanic membrane,
+thus giving the bone a sound-transmitting function. Apparently none of
+the opercular series was present.
+
+There are two large palatal teeth, slightly labyrinthine in character,
+adjacent to each internal naris. The scapulocoracoid, as shown by
+Peabody (1958), is Anthracosaurian in structure, as are the
+long-stemmed clavicles. The limbs have digits rather than fin-lobes,
+although the digital number apparently is four and the number of bones
+in the manus is less than would be expected in a primitive amphibian.
+The vertebrae are similar to those of Ichthyostegids, as described by
+Jarvik (1952), except that the pleurocentra are much larger.
+
+In addition to this remarkable combination of crossopterygian and
+amphibian characters, _Hesperoherpeton_ is specialized in certain
+features of the skull. The orbits are much enlarged, probably in
+correlation with the diminutive size of the animal, and this has been
+accompanied by loss of several bones. The frontal and squamosal nearly
+meet each other, and both form part of the rim of the orbit. The bones
+of the posterior part of the dermal roof are greatly reduced, and there
+is none behind the squamosal except the projecting tabular; there is no
+indication of quadratojugal, jugal, intertemporal or postparietal. The
+foramen magnum is enormous. The external surfaces of the bones of the
+skull are nearly smooth.
+
+Is it possible that the "primitive" and "specialized" features of this
+animal are actually larval? Are they not just the kind of characters
+that would be expected in an immature, aquatic embolomere of
+Pennsylvanian time? For several reasons we do not think this is the
+case. Except for the anterior part of the braincase, there is no
+indication that the skeleton was not well ossified. The postaxial
+processes on the humerus, ulna and ulnare could scarcely have been
+larval features only, since they are so clearly homologous with those
+in adult Rhipidistia; a larval limb should indeed be simple, but its
+simplicity is unlikely to involve paleotelic adult characters. The
+scapulocoracoid of our specimen is of practically the same shape and
+size as that in the only other known individual, the type; this would
+be probable if both were adults, but somewhat less likely if they were
+larvae of a much larger animal. The form of the stapes, tabular and
+otic notch suggest a functional tympanic membrane, which could not have
+occurred in a gill-breathing larva. On the other hand, an adult animal
+of pigmy size might be expected to have large orbits, large otic
+capsules and a large foramen magnum.
+
+We conclude that _Hesperoherpeton_ lived and sought food in the weedy
+shallows at the margin of a pond or lagoon, and that for much of the
+time its head was partly out of water (Fig. 12). The animal could
+either steady itself or crawl around by means of the paddlelike limbs,
+but these probably could not be used in effective locomotion on land.
+Like the Ichthyostegids, it probably swam by means of a fishlike tail.
+
+[Illustration: FIG. 12. _Hesperoherpeton garnettense_ Peabody. Probable
+appearance in life. × 0.5.]
+
+
+TAXONOMY
+
+Evidently _Hesperoherpeton_ is a small, lagoon-dwelling survivor of
+the Devonian forms that initiated the change from Crossopterygii to
+Amphibia (Jarvik, 1955). It shows, however, that this transition did
+not affect all structures at the same time, for some, as the braincase
+with its notochordal canal, the mandibular bones and axial limb bones,
+are unchanged from the condition normal for the Rhipidistia, but most
+other characters are of amphibian grade. To express these facts
+taxonomically requires that _Hesperoherpeton_ be removed from the
+family Cricotidae, suborder Embolomeri, order Anthracosauria, and
+placed in a new order and family of labyrinthodont Amphibia.
+
+ Order PLESIOPODA
+
+ (_plesios_, Gr., near, almost; _podos_, Gr., foot)
+
+ Labyrinthodontia having limbs provided with digits, but
+ retaining posterior flanges on axial bones as in
+ Rhipidistia, without joint-structure at elbow and wrist
+ essential for terrestrial locomotion; neurocranium having
+ separate otico-occipital section, large notochordal canal,
+ no occipital condyle, as in Rhipidistia; nares separate from
+ rim of mouth; pectoral girdle anthracosaurian; vertebrae
+ having U-shaped intercentrum and paired, but large,
+ pleurocentra.
+
+Probably associated with the characters of the order, as given above,
+are the connection of pectoral girdle with skull, and the presence of a
+tympanic membrane, the stapes functioning in both sound-transmission
+and palatoquadrate suspension.
+
+ Family HESPEROHERPETONIDAE
+
+ Orbits and foramen magnum unusually large in correlation
+ with reduced size of animal; squamosal forming posterior
+ margin of orbit; circumorbital series absent (except for
+ postorbital); sensory pits on squamosal and frontal.
+
+Characters defining the family are evidently the more specialized
+cranial features, which probably evolved during Mississippian and early
+Pennsylvanian times.
+
+The definition of the genus and species may be left to rest upon
+Peabody's (1958) original description and the present account, until
+the discovery of other members of the family gives reason for making
+further distinctions.
+
+
+SUMMARY
+
+_Hesperoherpeton garnettense_ Peabody (1958), based on a
+scapulocoracoid and part of a vertebra, was originally placed in the
+order Anthracosauria, suborder Embolomeri, family Cricotidae. A new
+skeleton from the type locality near Garnett, Kansas (Rock Lake shale,
+Stanton formation, Upper Pennsylvanian), shows that the animal has the
+following rhipidistian characters: Large notochordal canal below
+foramen magnum, otico-occipital block separate from ethmosphenoid,
+postaxial processes on three axial bones of forelimb, pectoral girdle
+(probably) articulated with tabular. Nevertheless, _Hesperoherpeton_
+has short digits, an anthracosaurian type of pectoral girdle, an otic
+rather than spiracular notch, nostrils separate from the mouth, and
+vertebrae in which the intercentrum is U-shaped and the pleurocentra
+large but paired. The stapes reaches the quadrate.
+
+_Hesperoherpeton_ is placed in a new order, PLESIOPODA, on the basis of
+the characters stated above, and a new family, HESPEROHERPETONIDAE.
+Specialized characters of the family include: Reduction of
+circumorbital bones, bringing the squamosal to the edge of the orbit,
+loss of certain bones of the temporal region, and relative enlargement
+of the orbits and foramen magnum, in correlation with the diminutive
+size of the animal. The structural characters of _Hesperoherpeton_
+suggest to us that it lived in the shallow, weedy margins of lagoons,
+rested with its head partly out of water, and normally did not walk on
+land.
+
+
+LITERATURE CITED
+
+EATON, T. H., JR.
+ 1951. Origin of tetrapod limbs. Amer. Midl. Nat., 46: 245-251.
+
+JARVIK, E.
+ 1952. On the fish-like tail in the ichthyostegid stegocephalians.
+ Meddel. om Grønland, 114: 1-90.
+ 1954. On the visceral skeleton in _Eusthenopteron_ with a discussion
+ of the parasphenoid and palatoquadrate in fishes. Kgl. Svenska
+ Vetenskapsakad. Handl., 5: 1-104.
+ 1955. The oldest tetrapods and their forerunners. Sci. Monthly,
+ 80: 141-154.
+
+MOORE, R. C., FRYE, J. C., and JEWETT, J. M.
+ 1944. Tabular description of outcropping rocks in Kansas. Kansas
+ State Geol. Surv. Bull., 52: 137-212.
+
+PEABODY, F. E.
+ 1952. _Petrolacosaurus kansensis_ Lane, a Pennsylvanian reptile
+ from Kansas. Univ. Kansas Paleont. Contrib., Vertebrata,
+ Art. 1: 1-41.
+ 1958. An embolomerous amphibian in the Garnett fauna (Pennsylvanian)
+ of Kansas. Jour. Paleont., 32: 571-573.
+
+ROMER, A. S.
+ 1937. The braincase of the Carboniferous crossopterygian
+ _Megalichthys nitidus_. Mus. Comp. Zool. Bull., 82: 1-73.
+ 1947. Review of the Labyrinthodontia. Mus. Comp. Zool. Bull.,
+ 99: 1-368.
+ 1957. The appendicular skeleton of the Permian embolomerous
+ amphibian _Archeria_. Univ. Michigan Contrib. Mus. Paleont.,
+ 13: 103-159.
+
+WATSON, D. M. S.
+ 1926. The evolution and origin of the Amphibia. Phil. Trans. Roy.
+ Soc. London, (B) 214: 189-257.
+
+_Transmitted January 13, 1960._
+
+
+28-2495
+
+
+
+
+
+End of the Project Gutenberg EBook of A New Order of Fishlike Amphibia From
+the Pennsylvanian of Kansas, by Theodore H. Eaton and Peggy Lou Stewart
+
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