The Ornithosaurian humerus has but little in common with that of any

mammal. Most mammals have the proximal head of the bone hemispherical,

and a pit at the distal end for the olecranon process of the ulna,

while there is usually little indication of a radial crest, and the

proximal and distal ends are in the same plane. In the Bat however the

bone is twisted a little so that the slight radial crest looks in the

same direction as the distal end, here also there is no pit for the

olecranon; but the bone is sigmoid and proportionally much longer than

in Pterodactyles. In the horse, hippopotamus, &c., the radial process

becomes more developed but never resembles that of a Pterodactyle.

Among reptiles, the bone may be compared with lizards and crocodiles.

In crocodiles the proximal and distal ends are nearly in the same

plane, the distal end has two condyles, the head is convex from side to

side, and the radial crest is moderately developed and never extends so

far outward or so far proximally as in Pterodactyle. In the Chameleon

the bone is more twisted than in Crocodile, and as in Pterodactyle

the distal end is compressed on the radial side to a sharp margin.

In Iguana, Scink, and Monitor both proximal and distal ends are much

expanded, and the radial process makes no approximation to that of a

Pterodactyle.

The bird humerus does not approximate more closely in form to that

of the Pterodactyle than does the Chameleon humerus, though it has

the cardinal distinction of pneumatic foramina, and these sometimes

corresponding in position in the two groups.

The bird humerus is commonly longer, though in the parrots the

proportions and straightness are not unlike Pterodactyle. In

some respects a nearer resemblance is seen in the raptorial bird

_Gypogeranus serpentarius_, in which the radial process is rather more

developed than in the Crocodile, and extends further proximally though

still much smaller than in Pterodactyle; here too the superior surface

is concave from side to side, and the distal articulation is not unlike

that of some Pterodactyles. But no Pterodactyle has the head of the

humerus convex from the radial to the ulnar sides, and the bird is

distinctive in having the ulnar crest developed on the inferior side

of the head: a faint approximation to a similar development is seen in

Crocodile, but there is no trace of such a process in Pterodactyle. The

distal end is more Bird-like than Lacertian in form, but is twisted to

a greater angle with the proximal end than in birds.

Altogether the bone is distinctive. The points in which it is unlike

birds and reptiles are those in which Birds and Lizards resemble each

other; it would not be easy to say that in form it resembles one group

more than the other. But it is linked with birds by the pneumatic

foramina.

RADIUS AND ULNA.

Case. Comp. Tablet. Specimen.

=J= _a_ 9 5- 6

10 1-10

11 1- 7

12 1- 4

13 5- 6

Of neither of these bones has a perfect specimen been found. While

fragments of humeri are met with frequently, fragments of these bones

are rare. In accordance with the analogy with birds the Ulna might

be presumed to be the larger bone of the two. But from a study of

German specimens the larger bone is found to be the Radius, which

according to the mammalian plan is placed in front of the ulna. As a

whole, the fore-arm of Ornithosaurians is only to be compared with the

insectivorous mammal _Chrysochloris Capensis_, in which there are also

three bones in the fore-arm,--the third bone like the _Pteroid bone_

in Ornithosaurians, extending about half-way from the carpus to the

humerus, and holding, relatively, a similar position and development to

the fibula in bats.

The pteroid bone articulated with a separate carpal, and was placed

on the side of the arm, adjacent to the radius, which at the distal

end extended in German specimens more inward than the ulna. In

Chrysochloris the third bone appears to be behind the other bones, and

adjacent to the ulna[P].

[Footnote P: See D'Alton and Pander _Chiropteren und Insectivoren_,

Bonn, 1831, pl. 5, Chrysochloris.]

Among neither birds nor reptiles is any comparable modification of

the fore-arm to be found. Then by examining the proximal surface of

the proximal carpal, the characters of the distal end of the Radius

are readily discovered. The proximal carpal shows on the same surface

another articular facets with which however only one fragmentary distal

end of a bone corresponds. That accordingly is identified as the ulna.

Besides these, three other articular ends of bones occur, one of which

fits on to the distal end of the femur. The remaining two are both

large bones, with epiphyses which formed portions of the articular

surfaces, and are usually wanting. One of these bones corresponds in

form with the ulna of a bird, and would fit the facet on the ulnar

side of the distal end of the Pterodactyle humerus. The other bone

is massive with a sub-quadrate articular end, and might well be the

proximal end of the radius. Some specimens are among the largest

fragments of Pterodactyle bone known. The only other bone that either

of these could be is the distal end of the tibia, a bone not yet known,

but probably not unlike that of a bird.

I. Distal End of Ulna.

Four specimens which show articular ends such as the ulna should have,

are mounted together. They are compressed bones with the section of

the fracture elongately oval; and the shaft widens from the fracture

to the articulation without increasing in thickness. The outer surface

is gently convex, becoming concave mesially near the articulation;

the inner surface has the same characters, only the concavity at the

extreme distal end reaches from side to side of the bone. The two short

sides both look outward as well as laterally; one of them flattened so

as to thicken the bone, is concave in vertical outline owing to the

extreme distal end turning suddenly outward; the other side a little

convex, compresses the bone and inflects its inner margin. The longest

specimen measures 1-5/8 inch; 5/8 inch wide at the fracture, and 1-1/8

inch wide at the distal end. The greatest thickness at the distal end

is half an inch, the thickness of the fractured shaft is 5/8 of an inch.

The articular surface appears to have an elongated sub-reniform shape,

the part at the compressed side of the bone being narrower than the

broad ovate part on the thick side of the bone, to the lateral limit

of which it extends, while the narrow part does not extend laterally

nearly so far as the inflected border, which appears to give attachment

to powerful muscles. There is also a strong muscular attachment at the

corresponding diagonal corner of the bone where the outer surface on

its right meets the side of the bone in an elevated ridge.

In its long diameter the articulation is a little convex; transversely

it is very convex in the ovate part, but more flattened in its narrower

continuation. Where widest it measures about 4/10ths of an inch.

Nos. 5 and 6 on another tablet appear to be distal ends of ulna of

another kind of Pterodactyle. They are less compressed, more quadrate

in section, and have the sides more nearly parallel The flattened

side similarly has a concave border, but instead of having its distal

termination developed laterally, has it thickened behind. The opposite

side of the bone which in the other specimens was compressed is here

thick and well rounded, and not at all inflected. There is an absence

of the concavity noticed on the outer surface of the bone in the

compressed specimens. The articular surface is much flatter, and a

little concave in length instead of being convex; as in the other

examples it looks downward. The largest fragment. No. 5, measures 1-3/8

inch long; it is 6/8 inch wide at the fracture, and 4/8 inch thick. The

sub-quadrate distal end is more than an inch long, more than 4/8ths

inch thick on the thick side, and nearly 4/8ths inch thick on the

compressed side.

II. Distal End of Radius.

The best preserved of the 10 specimens here exhibited is 3 inches long,

No. 2. The shaft is oval, flattened on one side; measuring at an inch

from the fractured end 7/10ths of an inch in the least diameter, and

one inch in the wide diameter. It widens distally at first slowly,

then rapidly, till at the articular end its greatest width is two

inches. But while expanding laterally it contracts from side to side,

the more convex side of the two at about an inch from the articular

end, beginning to approximate to the flatter side till the articular

end has a short diameter of less than half an inch.

On the left-hand corner of the convex inner side of the bone is an

elevated flattened disc for muscular attachments, fully half an inch

in diameter, there is a slight muscular attachment interior to this,

nearer the middle of the bone. The left-hand corner of the flattened

outer side of the distal end of the radius is marked by a vertical

ridge bordering a similarly elevated oval muscular attachment. Parallel

to this nearer the middle of the side is a much stronger and acutely

elevated ridge.

The articulation is made up of three distinct parts, all in a straight

line. The portion of bone adjacent to the large muscular disc is

compressed and rounded on the distal end; then first there is a rather

deep circular cup 3/8ths of an inch wide, nearer to the more convex

than to the flatter side of the bone; adjacent to this cup is a convex

ball of about the same size; while the remainder of the articulation

is concave in length, convex from side to side, and looks downward and

a little towards the inner convex side of the bone. The specimens are

arranged so as to display these characters.--The example described is

of nearly the same size as that figured for the humerus in fig. 1, T.

XXIV. of the Cretaceous Reptilia. The less well preserved bone in that

figure exhibits the Ulna in its true position behind the Radius.

III. Proximal End of Ulna.

This bone has much the proportions of the Ulna in birds, the smaller

specimens nearly resembling the ulna of the Heron. The specimen (No.

1) with the shaft best preserved is 2-1/4 inches long, cylindrical at

the fracture, where it measures in diameter 3/16ths of an inch. It

gradually enlarges proximally widening to about 7/10ths of an inch;

near the proximal end it is a little curved, the side which is concave

in length being a little flattened, while there is a lateral elevation

on the opposite side, apparently corresponding to the quill-ridge on

the convex side of the bird-ulna. There is a separate ossification for

the olecranon, which is an irregular sub-oblong bone forming the outer

part of the articulation; it is only preserved in No. 1. Nos. 4, 5 and

6 show the concave transverse groove from which it has come away.

The articular surface looks upward and forward, in which aspect it has

a trapezoidal form. Sometimes, as in No. 2, the great sigmoid area is

divided into two parts by a vertical ridge, the more elevated part

of the articulation on the radial side of the bone being concave,

while the outer part, as in the heron, besides being concave, has its

border on the concave side of the bone produced and rounded. There is

a small triangular elevation on the radial aspect of the proximal end

like that on the corresponding part of the ulna of the heron. On this

aspect the bone is flattened, on the opposite and outward aspect it is

compressed and produced as in the bird. No. 2 measures 1-1/8 inch over

the articular end. The series includes 6 specimens.

IV. Proximal End of Radius.

This bone terminated in an epiphysis which formed part of the articular

surface, and has disappeared from all the 7 specimens mounted. So much

of the articulation as remains does not oppose the idea of its having

been attached to the humerus, while the large size of the example No.

7, which could not have measured less than 2-1/2 inches from side to

side over the articulation, is more in accordance with what is at

present known of the dimensions attained by the distal end of the

humerus than with the size that would be expected in the distal end

of the tibia, which is the only other unknown bone to which these

specimens could be referred.

The longest specimen, No. 3, is 3 inches long; broadly ovate at the

fracture, measuring in the long diameter 1 inch, and in the short

diameter more than 3/4ths of an inch. Nearer the articular end the bone

becomes in section sub-quadrate or rather sub-rhomboid. No. 1 shows

these terminal characters extremely well. On the posterior aspect of

the specimen the surface is divided into two flattened slightly convex

parts by a median vertical well-rounded angular bend. In front the side

is similarly divided into two parts, both of them a little concave

proximally, by a sharp median vertical ridge, which does not reach to

the articulation by a varying distance, never so long as the bone is

wide. The ridge terminates in, and is pierced by, a vertical groove

apparently for a nutritive vessel. Where the anterior and posterior

aspects of the bone converge laterally the sides are well rounded.

Only a small part of the articular surface is preserved, looking upward

and a little forward; it terminates the wider of the halves of the

bone laterally and in front. The remainder of the articular surface,

from which the epiphysis has come away, may be divided principally in

the majority of specimens into a posterior flattened median rhomboid

space and an oblong cup-shaped anterior space divided from it by an

elevated ridge. The extreme lateral termination appears to have been a

ball-shaped convexity.

The great length of the fore-arm relatively to the humerus,

characteristic of German Ornithosaurians, from the fragmentary

condition of Cambridge specimens is not seen.

Although the fore-arm resembles Chrysochloris in _plan_ the

resemblance is not close in the details of form. In many Mammals it is

characteristic for the radius to be the principal bone of the fore-arm,

and among Ruminants in which this is especially the case the radius is

altogether in front and the ulna behind as is the position with Birds

and Crocodiles. And among mammals with claws, as in the Lion, Bear,

&c., and in the Chameleon, it is characteristic, for the radius also to

be on the inside of the limb at the distal end, as in Ornithosaurians.

In form, ridges, and muscular attachments (see pl. 3) the distal end of

the radius approximates closely to the Bear and the Lion, and may also

be compared with the Bats and Birds, though with Birds it is a small

bone. From the epiphysis of the proximal end apparently being wanting

it would be difficult to compare closely. But though not like any

particular mammal, it might have pertained to a mammal since it has the

large perforation for the nutritive vessel near to the proximal end as

in the Camel and many of the mammalia.

The ulna of the Pterodactyles is at the proximal end altogether

distinguished from mammals by the slight development of the olecranon,

nor can the distal end, especially in its relation to the carpus, be

paralleled.

Among birds and reptiles the ulna is the large bone, and here a

general resemblance in form to the ulna of Pterodactyles is seen at

the proximal end. It is not compressed from side to side as in the

Crocodile, Iguana, Monitor, &c., but from back to fronts in this

rather resembling Birds than the Chameleon. It however at the distal

end is more crocodilian.

The fore-arm in plan is mammalian. The Pteroid bone is mammalian, the

Radius is mammalian and avian; the Ulna is avian, and crocodilian in

form, but mammalian in proportion. The pneumatic foramen of the ulna is

peculiarly avian.

CARPUS.

Pl. 5.

Case. Comp. Tablet. Specimen.

=J= _b_ 1 1-13

2 1-18

3 1- 4

4 1- 8

The pterodactyle wrist is made up of three bones, arranged as a

proximal carpal, a distal carpal, and a lateral carpal. Two of them

are figured by Professor Owen, who regarded the distal carpal of

this description as the scapho-cuneiform; while A very imperfect

example of the proximal carpal is named the unciform: neither of these

determinations, the reverse of those which follow, were given as more

than probable guesses.

I. Proximal Carpal.

No. 10 shows the proximal surface well; portions of it are seen in

Nos. 4, 5, 6, 8, 9, 11, and 12. The distal surface is best exhibited

in No. 1; portions of it are shown in Nos. 2, 3, 5, 7, 8. No. 13 is an

impression taken from the proximal sur&ce of a distal carpal to show

its correspondence with distal surface of the proximal carpal. The

bone is proximally of an irregular oblong form, being five sided, and

much broader towards the inner end than towards the outer end. The two

ends are sub-parallel, and rather obliquely connected on one side by

a nearly straight border more than twice as long as the shorter end.

The other limits of the sub-parallel ends are connected by two concave

borders meeting in a well rounded convexity, which is near to the

broader inner end.

The proximal surface of the bone is flattened, and may be divided into

a sub-rhomboid space, adjacent to the shorter of the sub-parallel ends,

which is moderately concave in the long axis of the bone and slightly

convex transversely, and an oblong space adjacent to the longer of

the two ends. This is separated from the sub-rhomboid space, toward

the straight side of the bone, by an elevated ridge sub-parallel

with the ends. It is directed towards the convexity on the opposite

side, in which the long and short concave parts meet, but after half

crossing the bone it becomes forked in a U shape, and less elevated;

the smooth unarticular included space shows an oval pneumatic foramen,

which varies in size with the different species. The region between

this Y-shaped ridge and the longer of the two ends, is sub-reniform,

slightly concave in its long diameter, and deeply concave in the short

diameter, exactly corresponding in form with the articular surface

already described as the distal end of the ulna. Also parallel with

the long end of the bone are marks of an articular surface exactly

corresponding with those described as the distal end of the radius;

that is, at the convex angle of the angulated side is placed a

hemispherical boss,' interior to which is a hemispherical concavity,

and extending toward the straight side is the oblique smooth border

of the sub-rhomboid area described. There still remains a space to be

accounted for. This consists of a sub-quadrate area forming the corner

of the bone made by the concave side and the shorter outer end; it is

made up of an inner concave part separated from the radial articulation

by a ridge, and an outer convex part constituting the shorter end of

the bone.

This carpal is moderately compressed from the proximal to the distal

side, except towards the shorter end of the bone, being there prolonged

distally into a wedge-shaped process, showing at its termination marks

of a powerful muscular attachment.

The outer lateral surface is of variable antero-posterior extent.

The distal articular surface is placed entirely toward the narrow

end of the bone, leaving at the proximal end a large smooth rhomboid

unarticular area, of which every side is a little concave: it connects

obliquely the proximal with the distal articular surfaces. The distal

articular area is divided by a diagonal ridge into a long oblong area

of which the inner and outer sides are sub-parallel and the ends

rounded: it is slightly concave in length as well as transversely, and

is slightly twisted like the flukes of a screw. Adjacent to this region

laterally is the other and sub-triangular part of the articulation.

The broad end of the triangle is toward the broad end of the bone; it

is concave in length and flattened transversely. The two parts of the

articulation are inclined to each other at a large angle, both looking

downward and outward, but on opposite sides of the bone.

II. Distal Carpal.

The tablets of this bone comprise 22 specimens. Nos. 2, 3, 4, 5, 6,

8, 9, 10, 15, 16, 19 and 22 are so mounted as to exhibit the proximal

surface. Nos. 7, 11, 12, 13, 14, 15, 16, 20 and 21 show the distal

surface of the bone. No. 17 is a cast from the distal sur&ce of a

proximal carpal for comparison with the proximal surface of the distal

carpal. No. 16 is a cast from the proximal end of the wing-metacarpal

for comparison with the distal surface of the distal carpal. No. 20

is a distal carpal of unusual type, 19 is a cast from its proximal

surface, and 21 is a cast from the distal surface of the same specimen.

The proximal aspect of this bone is rather narrower than the distal

aspect; each is sub-triangular in outline, the sides being convexly

curved. In the long axis from the apex on the inside to the short

outer[Q] side the bone is convex proximally with an oblique transverse

depression; in the short axis, that is, between the two longer sides,

the middle of the bone is hollow, but the oblique transverse depression

makes both sides of the hollow convex,--so that excepting the smooth

unarticular triangular area adjacent to the apex, the sub-quadrate

articular surface is shaped somewhat like two cones put side by side

in such manner that the apex of each touches the base of the other:

the apex of that cone which should touch the short side or base of

the triangle formed by the bone, is truncated by a depression which

exhibits an oval pneumatic foramen. Towards the apex, on the same side

as the pneumatic foramen, the margin of the bone is rounded for a small

terminal oval articulation which looks outward and upward.

[Footnote Q: Outer and inner are here used in accordance with the usual

interpretation, and the better to compare with birds.]

The lateral aspects of the bone are at right angles to the proximal and

distal surfaces. They are smooth, a little concave in antero-posterior

extent, and convex in the opposite direction. That one on to which

the marginal articular surface impinges is except for that surface

sub-quadrate in outline; the opposite side has a slightly crescentic

form, the flattened outline being distal. They show several small

foramina.

The distal aspect of the bone is comparatively flat. The distal surface

consists of a smooth unarticular part adjacent to the apex, rather

smaller than the corresponding area on the proximal aspect of the bone.

Between this part and the sub-crescentic articular surface, which

occupies the remainder of the distal area, is a large circular pit,

furthest removed from the side of the bone which forms the sub-apical

marginal articulation. The pit on the apical side shows several small

foramina; on the outer side of the bone the roughened articular

surface extends down the pit side. The articulation is flattened from

side to side of the bone. Its outer margin is slightly prominent, and

the margin of the pit is slightly convex and prominent, so that the

intervening articular surface in the direction between these limits

is concave. It is commonly divided into two parts by a median band

limiting a depressed half, which is in a slightly different plane

from the other half of the articulation. Where the depressed part

terminates towards the marginal articulation, which does not extend

so far distally, there is between the two a small step-like roughened

articular portion.

The large crescentic articulation described gave attachment to the

wing-metacarpal bone; if there was a second metacarpal terminating

in a claw, it must have been attached to the small articulation last

referred to. In No. 20 the pit is extremely small, the impressed part

of the articulation is small and deeply sunk, while the apicular

articulation is widened and shortened so as to make the outline of the

bone quadrate.

III. Lateral Carpal.

The Ornithosauria An elementary study of the bones of Pterodactyles made from fossil remains found in the Cambridge Upper Greensand, and arranged in the Woodwardian Museum of the University of Cambridge · 第 4 / 13 段