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Dinosaur Monophyly and a New Class of Vertebrates

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Abstract and Figures

TRADITIONALLY dinosaurs are classified as two or three separate, independent groups of reptiles in the Subclass Archosauria. But evidence from bone histology, locomotor dynamics, and predator/prey ratios strongly suggest that dinosaurs were endotherms with high aerobic exercise metabolism, physiologically much more like birds and cursorial mammals than any living reptiles1-8. Recently Ostrom has argued forcefully that birds are direct descendants of dinosaurs and inherited high exercise metabolism from dinosaurs1,8. Here we present evidence that dinosaurs are a single, monophyletic group, and that the key advancements of endothermy and high exercise metabolism are justification for removing dinosaurs from the Reptilia and placing them with birds in a new class, the Dinosauria.
Content may be subject to copyright.
Received October 18,
1973.
LEONARD E.
KELLY
Dinosaur
Monophyly
and
a New
Class
of
Vertebrates
Nature Vol. 248 March 8
1974.
TRADmONALLY
dinosaurs are classified as
tWQ
or three separate,
independent groups
of
reptiles in the Subclass Archosauria.
But evidence from bone histology, locomotor dynamics, and
predator/prey ratios strongly suggest that dinosaurs were
endotherms with high aerobic exercise metabolism, physio-
logically much more like birds and cursorial mammals than
any liying reptiles'<". Recently Ostrom has argued forcefully
that birds are direct descendants of dinosaurs and inherited
high exercise metabolism from dinosaurs--s. Here we present
evidence that dinosaurs are a single, monophyletic group, and
that the key advancements of endothermy and high exercise
metabolism are justification for removing dinosaurs from the
Reptiffa and placing them with birds in a new class, the Dino-
sauria.
The two generally accepted orders of 4jnosaurs, the Saur-
ischia and Ornithischia, are usually interpreted as independent
derivatives of primitive thecodontian reptiles of the Triassic,
but
all known Triassic dinosaurs can be distinguished from
typical thecodontians (Fig. 1)9-23.
Most thecodontians had a wide-track sprawling gait or a
crocodile-like semi-erect gait, both requiring much multi-
directional mobility at the shoulder". The thecodontian
glenoid, or shoulder socket, was lizard or crocodile-like-
being a saddle-shaped. notch facing outward and backward,
permitting humerus rotation, abduction, and backswing.
Dinosaur glenoids were concave sockets facing mostly down
and backwards, little outwards, restricting humerus movement
severely to a fore-and-aft vertical
plane-the
'fully erect gait'",
Also, in thecodontians and reptiles, generally, the delto-
pectoral crest (dp in Fig. 1) is located close to the humerus
head, giving the pectoralis musculature good leverage for
rotating the humerus about its long axis but relatively little
leverage for a vertical humerus backswing, In dinosaurs, the
vertical backswing leverage was increased by moving the
deltopectoral crest down the humerus shaft (Figs. 1 and 2).
In thecodontians and reptiles generally, the fourth trochanter
(4t in Fig. 1) usually was located close to the femoral head,
giving the caudifemoralis brevis musculature good long-axis
rotational leverage, but little leverage for a vertical backswing.
In dinosaurs, the apex of the fourth trochanter was developed
into a distally directed flange, increasing the leverage for a
vertical backswing (Figs 1 and 2).
A sprawling or semi-erect gait directs the thrust of the femur
strongly inwards into the acetabulum, or hip socket. The
thecodontian acetabulumusually was a strong, continuous bony
'Surface
as in most living reptiles. In dinosaurs, femoral action
was more restricted to a vertical plane; the acetabulum was
perforated to allow deeper penetration of the inturned femoral
head, and the weight of the body was transmitted from the
proximal surface of the femur to the strong dorsal rim of the
acetabulum-e.
The thecodontian hand, known in phytosaurs>", aeto-
saurs1 7 25, rauisuchids-" and 'Cheirotherium'27.28, was croco-
dile-like with five long digits, the inner three subparallel, the
outer two divergent (Fig. 1). The hand of Triassic saurischian
dinosaurs is distinctive (Fig. 1) with a very short, stout meta-
carpal I; a long, strong thumb phalanx 1; a powerful, curved,
trenchant thumb claw; thumb articulations forcing the claw
to diverge and point inwards during extension, converge with
digits II and
III
and point downwards during flexion; long
digits II and III, subequal and subparallel, bearing trenchant
claws; and reduced digits IV and
V29.
The hand
of
the better
known primitive ornithischians (fabrosaurids and hypsilopho-
dontids) differed from thai of Triassic saurischians in lacking
the long thumb and having blunt hooves instead
of
claws on
digits I to
III
(ref. 30). Recently, a complete articulated
skeleton of Heterodontosaurus, a Triassic ornithischian, was
collected by A. W. Crompton, now at Harvard, for the South
African Museum. The hand is virtually identical to that of
8
a
Concentration
of
TTX
(1/g
ml-
')
100
90
8
=
Department of Zoology,
University of British Columbia,
Vancouver, B. C.
1Grigliatti, T. A., Wqliamson, R., and Suzuki, D. T., Genetics,
64, S27 (1970).
2Grigliatti, T. A., Hall, L., Rosenbluth, R., and Suzuki, D. T.,
Malec. gen. Genet., 120, 107 (1973).
3Narahashi, T.,
Moore,J.,
and Scott, W. R., J. gen. Pliueiol.,
47,965(1964).
4Hinton, C. W., Genetics, 40, 951 (1955).
16~
with~'l
Ii
min,
while no comparable effect is observed with
Oregoh-R
flies.
The converse is also true; shi'"
flies
which
are debilitated by
TTX
at 17° C are immediately paralysed
and die when shifted to 22° C. This indicates two things;
first, the debilitation induced by
TTX
is temperature rever-
sible in shi"" and secondly, the increased resistance of Ore-
gon-R and, in part, of shi'" at 17°' C is probably due to a
reduced rate of uptake of liquid in both strains. This may be
a consequence of reduced dehydration at the lower tempera-
ture. .
In conclusion, it has been shown
that
the
shi"
alleles con-
fer on Drosophila a resistance to
TTX
which, like the
paralysis of these
flies,
is temperature dependent.
It
has also
been demonstrated
that
this resistance is attributable to an
alteration in the properties of the nervous system. The
TTX
resistance results obtained for the
shi"
and
shi'"
alleles are
interpreted as resulting from alterations of different sites in
the protein molecule encoded by this gene.
It
is suggested
that
the
shi"
locus is involved in the production of some com-
ponent of the regenerative sodium channel and
that
the
presence of the
shi"
allele, as well as producing temperature-
sensitive paralysis, also reduces the affinity of this channel
for TTX.
Ithank Drs David T. Suzuki and Linda Hall for discus-
sions. This research was supported by grants from the Na-
tional Research Council of Canada and the National Cancer
Institute of Canada to Dr Suzuki.
FIG.
3 Effect of increasing concentrations of
TTX
on
u, Oreaon-R, and b, ehi" flies at 17·C. Incubation time was
48 h. Arrows marked a and b indicate LD.. for Oregon-R
and
shi"!
flies respectively.
Nature
VoZ.
248 March 8 1.974 169
Fig. 1
Skulls,
forelimbs and hindlimbs of thecodontians, dino-
saurs and birds. All
views
of right
elements
except femur.
(A)
Euparkeria,
(B)
Anchisaurus,
(G"j
Fabrosaurus, (D) Comp-
sognathus,
(E)
Archaeopteryx,
(F)
Gracilisuschus, (G) Plateo-
saurus,
(H)
Heterodontosaurus,
(I)
Halticosaurus, (J)
Ttcino-
suchus, (K) Efraaskr",
(L)
Thecodontosaurus,
(M)
Syntarsus,
(N)
Deinonychus,
(0)
Ammosaurus,
(P)
Coelophysis, (Q) an
ornithomimid and
(R)
Grus.
Anchisaurus,
Fabrosaurus
(except
skull), Heterodontosaurus, Efraasia and Thecodontosaurus
from originalmaterial; data for the others from refs 20, 21,
26,28,36,44,53-55. (s) Scapula,(c) coracoid,(dp) deltopectoral
crest, (Ic) lunate carpal, (il) ilium, (is)
ischium,
(p)
pubis,
(a) astragalus, (ca) calcaneum,
(ft)
femorotibialis, (4t) fourth
trochanter,
(-
-
-)
long axis of
glenoid.
~C~il
~--....,
<
c~R
&2
ts :PQ
i~
E
_ A 0 p
E,
,.11
II II II
\\
~
V
V'I
~"ffi"
1"
I
III
I IV
III
I::
II QIV
IIi'
R
tv IV JJI M(embryo)
F
BeE
Right humerus
-..l
"l
11
'" 0.14
'"
"
~
:s
.0
20.10
'-
0
><
"
]0.06
a
"~f~'--'
~0.141·~.
//5.M'
L
II
9""'-/
-37'
L
~
3
21·
~~38
33~
.
IV ....31
40
.50.10 \
.11
X·I
:>1
32 .. S
~
~2
'2
~
3\'0
1
.0
18
~~.~
o • • ..
~
"'"
14 18 24 2 ...-
..
'0 0.06
\5
20/
.~,
Right
~
'
••
' femur
~
.
.s
0.24 0.32 0.40 0.48
Power index=M/L
0.13 0.21 0.29 0.37 0.45
Power index =M/L
The ankle
of
most thecodontians was complex
and
crocodile-
like: the astragalus articulated movably with the calcaneum
and tibia,
and
the calcaneum bore a 'heel' (calcaneal tuber) for
the gastrocnemius musculature-v-". In advanced thecodontians
the astragalar-calcaneal joint was a deep ball and sockets:'. In
sharp contrast, the dinosaur ankle was stiff, simple and bird-
like: the astragalus and calcaneum were rounded caps fixed
immovably on the ends
of
the tibia
and
fibula; the distal tarsals
were immovable caps on the metatarsal heads, and the tarsal
joint was a simple unidirectional hinge between astragalus-
calcaneum and distant tarsals (Fig.
1)24.28.
Saurischian diphyly
has been suggested because some theropods, such as
Allosaurus,
have deep ilia and a thin, anterior ascending process
of
the
astragalus, while prosauropods have unexpanded ilia, no
ascending process, and a peg-in-notch astragalar-tibial
joint2 2 3 4 Triassic forms, however, show how the transition
from prosauropod-grade to advanced theropod grade sauris-
chian occurred. The Triassic theropods Syntarsus and Halti-
cosaurus
had
expanded ilia but retained a pro sauropod-type
astragalar-tibial joint without an anterior ascending pro-
cess3 S 3 6 In general, the prosauropod grade
of
postcranial
anatomy seems to be the primitive dinosaur pattern. Details
of
tarsal structureare often obscured by incomplete ossification,
but
the pattern in Syntarsus is virtually identical to that
of
Heterodontosaurus
(Fig. 1). Digit I arises two-thirds down the
length of metatarsal
II
and
is reduced and slightly divergent;
digits
II
and IV are subequal; digit
III
is the longest; digit V
is reduced to a splint; distal tarsal IV is cuboid; III is rect-
angular;
II
is a thin plate and the astragalus-calcaneum are
prosauropod-like.
Fig.2
Robustnessand positionof
muscle
attachments,(a) in the
femur and, (b) in the humerus. The data are taken from
speci-
mens and refs 9, 10, 13, 15-20, 26, 28, 30, 36, 38, 39, 42, 43.
Thecodonts, e, are (1) Proterosuchus, (2) Erythrosuchus, (3)
Euparkeria, (4) Shansisuchus, (5) Fenhosuchus, (6) Wangisuchus,
(7) Argentinosuchus, (8) Neoaetosauroides, (9) Stagonolepis,
(10) Palaeorhinus,
(1)
Phytosaurus, (12) Rutiodon, (13) Mystrio-
suchus, (14) Gracilisuchus, (15) Turfanosuchus, (16)
Omitho-
suchus, (17) Riojasuchus, (18) Tictnosuchus, (19) Sphenosuchus,
(20) Pseudhesperosuchus, (21) Pedeticosaurus, (22) Triassolestes,
(23) Alligator, (24) Lagosuchus, and (25) Lagerpeton. Dinosaurs
(~,
are (26) Staurikosaurus, (27) Ischisaurus, (28) Herrera-
saurus, (29) Halticosaurus, (30) Efraasia, (31) Massospon-
dylus, (32) Teratosaurus, (33) Plateosaurus, (34) Riojasaurus,
(35) Melanorosaurus, (36) Anchisaurus, (37) Fabrosaurus, (38)
Heterodontosaurus, (39) Dysalotosaurus, and (40)Hypsilophodon.
(8)
Minimumshaft diameter,
(L)
length of femur or humerus,
(M)
distance from head to
muscle
attachment (deltopectoral
crestin humerus, fourth trochanter in
femur).
E
H
Triassic saurischians in all six
of
the features cited above.
Although specialised craniallys-,
Heterodontosaurus
probably
represents the original ornithischian hand pattern, inherited
from saurischians, where the thumb was specialised for defence
and
digits
II
and
III were used for defence, digging, and support
during slow, quadrupedal locomotion. In more advanced
ornithischian hands, the defensive function was lost, the
thumb was secondarily shortened
and
simplified, and the
claws were replaced by hooves, but in Hypsilophodon, digits
II
and III are still subequal and subparallels".
The origin of the femorotibialis, a knee extensor, in most
thecodontians
and
in reptiles generally, is on the smooth
anteriolateral surface
of
the femoral shaft. In primitive
saurischians and ornithischians, the origin was expanded by
the development of a spike-like ridge
(f.t,
in Fig. 1). In ad-
vanced saurischians
and
ornithischians, and in birds, this
spike becomes a large
crest-the
'lesser trochanter', not
homologous to the lesser trochanter
of
mammals. Increased
muscle power for knee extension probably was related to the
development
of
the fully erect gait. Ornithosuchid thecodonts
have this crest
but
differ from dinosaurs dramatically at the
ankle and forelimb'P-P.
~
-e
§
:I: IV II I
III
J
170
The radiations
of
thecodontians
and
dinosaurs were based
on different trends in locomotor anatomy, behaviour,
and
exercisemetabolism. The earliest thecodontians, the protero-
suchians!",
had
short limbs
and
a sprawling posture with a
wide range
of
movement at each joint". Stride length and power
in the sprawling gait are increased by vertebral column undula-
tions, and thecodontians generally lack adaptations for
inhibiting lateral undulation. The complex ankle
of
advanced
thecodontians was probably aresponse to selection for finer
-control of supination-pronation and greater leverage in
sprawling locomotion. Thecodontian footprlnts"? indicate
that
digit V in the
hand
and foot were strongly divergent
and
powerfully muscled, like digit 1
of
climbing mammals. Flexi-
bility at the major limb joints plus divergent digit V probably
gave thecodontians a wide locomotor repertoire, including'
some digging, climbing,
and
movement over uneven ground.
Some
of
the later Triassic thecodontians (such as aetosaurs
and
phytosaurs") retained the sprawling gait and others, such as
rauisuchids
and
ornithosuchids'v-!", developed a crocodile-
like locomotor system which make possible both sprawling
and
semierect gaits
li
, 3 7 . Inturned femoral heads indicate that a few
thecodontians such as Hal/opus and some advanced raui-
suchids and ornithosuchids!", may have
had
narrow-tracked,
fully erect hindlimbs, but even these forms retained the complex
ankle.
The first well-known dinosaur is Staurikosaurus,
of
late
Middle or early Late Triassic3s.39, a long-jawed predator
with very long, gracile hindlimbs and postcranial anatomy
of
prosauropod grade (the femoral head is not as sharply in-
turned as in later dinosaurs
and
there is an oval acetabulum).
More advanced theropods, such as Ischisaurus and Herrera-
saurus,and ornithischians, such as Pisanosaurus, appear shortly
after Staurikosaurus", The original dinosaur stock were
probably predators with higher running speeds and exercise
metabolism than in thecodontians
of
comparable size. Early
dinosaurs may have been dipedal at top speed,
but
the strong
forelimb modifications for the fully erect gait and the prosauro-
pod-like
hand
indicate that quadrupedal progression was very
important. Even at the prosauropod grade, dinosaur bone
histology was identical to that
of
endothermic mammals",
Restriction
of
joint movement to a fore and aft, vertical plane
and the stiff, bird-like ankle would have made climbing difficult
for any dinosaurs". The vertebral column
of
early dinosaurs
was stiffened to inhibit lateral undulations by the development
of
extra vertebral articulations, the hyposphene-hypantra in
saurischians,
and
long ossified tendons appressed against the
neural spines in ornithischians. The locomotor repertoire
of
dinosaurs was narrow, rather restricted to moving over fairly
even terrain. Recent experimentsf! show that erect locomotion
does not require less energy for a given speed than sprawling, as
has usually been assumed",
but
erect locomotion probably
does increase manoeuvreability at very high speeds. The dino-
saur
radiation was based on a concentration
of
behavioural,
physiological, and anatomical adaptations for high, sustained
running speeds which made them irresistible predatorsand com-
petitors to contemporary thecodontians
and
the larger mammal-
like reptiles.
Could the similar postcranial adaptations
of
Triassic dino-
saurs reflect merely convergent evolution
of
the erect gait from
different thecodontians? We believe that the answer to this
question is almost certainly no. Evolution
of
erect posture
does not invariably lead to an avian-dinosaur type joint
pattern. Some thecodonts
and
many mammals, such as carni-
vores and ungulates, have a fully erect gait
but
retain complex
ankles with astragalar-calcaneal mobility
and
calcaneal 'heels'.
The very detailed similarity in all the majorjoints, especially the
hands
and
feet,
of
Triassic ornithischians
and
saurischians
makes dinosaur polyphyly exceedingly unlikely. Moreover,
the pattern
of
increasing dinosaur diversity in the Triassic
upwards from the stratigraphic level
of
Staurikosaurussuggests
one monophyletic radiation. Some
of
the little 'rabbit theco-
dontians' such as Lagosuchus
and
Lagerpeton4 2 ,4 3 , have im-
Nature Vol. 248 March
81974
mobile astragalar-calcaneal joints
and
lack calcaneal 'heels',
and
may be related in some way to dinosaur origins.
The prosauropod saurischians have a mixture
of
primitive
and
advanced features which show how ornithischians evolved
from saurischians (Fig. 1).
In
the primitive ornithischian
dentition, represented by
Fabrosaurus,
the anterior teeth were
non-serrated, pointed and slightly incurved with swollen bases
and
the cheek teeth were serrated with triangular crownst".
In some prosauropods, such as Massospondylus and probably
Anchisaurus, the basic pattern was similar: anterior, simple
teeth
and
triangular, serrated cheek teeth. In advanced pro-
sauropods, such as Plateosaurus
and
in most ornithischians,
the jaw articulation was depressed below the
tooth
row level,
but
in Fabrosaurus
and
Anchisaurus the articulation was still
on the same level as the
tooth
row4 4 The lower
jaw
of
most
ornithischians was deep and massive,
but
the fabrosaur
jaw
was slender like that
of
Anchisaurus. In early ornithischians the
origin
of
iliotibialis, a knee extensor co-inserting with the
femorotibialis, was expanded by the development
of
a long
anterioriliac prong. Such a prongis unknown in thecodontians
and
most prosauropods,
but
is present in very frabrosaur-like
configuration in Anchisaurus
and
Ammosaurus'", In ornithis-
chians the primitively broad, plate-like ventral surface
of
the
pubis and ischium were deeply excavated
and
reduced; such
excavations
had
begun in the prosauropods Anchisaurus and
Ammosaurus'",
The prosauropod grade is quite primitive,
and
herbivorous
prosauropods must have diverged very early from the basal,
predatory dinosaur stock.
It
should be noted that no theco-
dontians show trends away from carnivory towards herbivory,
except the aetosaurs, sprawling, armoured types totally unlike
ornithischians
17.
Small prosauropods with Anchisaurus-type
jaw
articulations, ilia and pubes were probably
the
immediate
ancestors
of
ornithischians. The adaptive shift probablywas an
emphasis on ultra-high speed bipedality plus adaptations for
prehension
and
cutting
of
plant fibres. Excellent fabrosaur
material collected for the South African Museum
and
now at
Harvard, shows
that
the development
of
an upper beak
had
just barely begun in
Fabrosaurus.
The fabrosaur predentary
was small, sharply pointed,
and
movably articulated with the
dentary; the dentary symphysis was mobile. The predentary
beak could serve as a gouge for digging into plant stems and
as a cutting edge occluding with the arcade
of
premaxillary
teeth, much like the incisors
of
kangarooss", while the mobile
symphysis permitted the retention
of
independent control
of
each
jaw
ramus, important for tooth-to-tooth shearing on
one side
of
the
mouth
at a time. Excavations in the maxilla
and
dentary, for cheek pouches to retain the cut ends
of
plant
material?",
had
begun in
Fabrosaurus.
All known Triassic
ornithischians
had
very long hind limbs with elongate distal
extremities indicatingvery high speeds. A short
trunk
facilitates
the maintainance
of
balance in a highly bipedal animal,
but
herbivory demands a long, bulky gut. Ornithischians solved
the balance problem by rotating the pubis posteriorly so that
the distal end, marking the end
of
the gut, lay far posterior
to the acetabulum. Thus, the gut was extended between the
hindlimbs
and
the pre-acetabular
trunk
section could be
abbreviateds",
Although Walker49has cited some resemblances between
living birds
and
crocodile-like thecodontians (sphenosuchids),
we believe that Ostrom has shown that the similarities between
Archaeopteryx
and
small theropods are so detailed
and
comprehensive
that
the immediate ancestor
of
birds must have
been a saurischian dinosaurl.s,5o. Some
of
the features cited
by Walker as evidence
of
crocodile-bird relationships are
actually widespread among tetrapods: cranial salt glands are
developed in lizards, especially in Amblyrhynchus51 ;forearm
articulations which force the radius distally during forearm
flexion are present in salamanders, Sphenodon,
and
lizards.
Although details are obscure, the Archaeopteryx skull seems
much more like the light, kinetic skulls
of
small theropods than
the solidly braced sphenosuchid structure'
2.
Archaeopteryx
'
..
Nature Vol. 248 March
81974
has the complete suite of seven features listed above as diag-
nostic of the primitive dinosaur erect gait. _In flying birds, bats
and pterosaurs the glenoid faces strongly outwards to make
possible the abduction of the humerus necessary for gliding
and powered flight. Significantly,
Archaeopteryx
retained the
typical, downward-facing dinosaur glenoid; it is difficult to
imagine how this joint would have made either flight or gliding
possible. The initial evolution of feathers probably was not
associated with flight, a- hypothesis developed at length by
Ostrom'.
Ostrom has shown that the hands and feet of
Archaeopteryx
are identical in detail to certain Jurassic/Cretaceous theropods,
and differ only in being larger relative to the body size (Fig.
3)1,50,53-55.
Feathers may have been widespread in bird-like
theropods.
Archaeopteryx
strongly resemblessmall theropods
in general body plan with a short trunk, thin, flexible neck,
very long hindlimbs and long fingers bearing trenchant claws
for snagging prey. Sphenosuchid thecodontians were quite
different (Fig. 3) with a long trunk, thick neck and long fore-
limbswith short digits adapted for running and not prehension.
Near bird-lower cretaceous theropod Microvenator
Archaeopteryx
~
Crocodyloid thecodont (sphenosuchid) Pseudhesperosuchus
Fig.3 Bodyform in a small theropod dinosaur, the firstknown
bird and a crocodyloid thecodontian. Microvenator hand and
skull restored after Ornitholestes. Data from refs 10, 53-55.
Endothermy and high aerobic exercisemetabolism are
suffi-
cient justification for separating birds into a class distinct from
other living sauropsid tetrapods. But endothermy and high
exercise metabolism were probably already present in the
dinosaur ancestors of birds and are the key features differen-
tiating dinosaurs from crocodilians and the other extinct
archosaurs. The bird radiation has produced many species,
but the structural diversity is not more striking than that
within the Ornithischia or Saurischia. Bird physiology is also
rather stereotyped. The avian radiationisan aerial exploitation
of basic dinosaur physiology and structure, much as the bat
radiation is an aerial exploitation of basic, primitive mammal
171
physiology. Bats are not separated into an independent class
merely because they fly. We believe that neither flight nor the
species, diversity of birds merits separation from dinosaurs on
a class level. Among all amniotes, the most profound adaptive
shift was from ectothermy to endothermy, which occurred
during the origin of mammals and dinosaurs. Therefore we
propose the erection of a Class Dinosauria, to include as
subclasses the Saurischia, Aves and Ornithischia. The cur-
rently recognised suborders of dinosaurs would be elevated to
orders (Fig. 4). Thecodontians, crocodilians, and pterosaurids
Cu
~oou~
S~bc""
omitbitcbia:
.~~,
r
Subcu
lauriacbia
r;,:;::
Order
On!«
Ordet.l:1lliial
Order '/ Order I
S~~u
I~
otDIllio-
An~YJo,
-.
Sau"ropodOmorpba
Theropoda Aves
~.
f
...../
..... / .....
/'-1/'-"
I
If
If
~
I
Fig. 4 Suggested phylogeny and classification of dinosaurs.
Position of Lagosuchus and Lagerpeton is very uncertain.
Within orders, ancestor-descendentrelationship is not necessarily
indicated by stratigraphic levelof known specimens,for example,
Pisanosaurus
is earlier than, but in some ways more advanced
than the earliest known Fabrosaurus. (1) Proterosuchus, (2)
Euparkeria, (3) Ticinosuchus, (4) Gracilisuchus, (5) Spheno-
suchus, (6) Pseudhesperosuchus, (7) Lagerpeton, (8) Lagosuchus,
(9) Staurikosaurus, (10) Ischisaurus, (11) Herrerasaurus, (12)
Coelophysis, (13) Syntarsus, (14) Halticosaurus, (15) Coelurus,
(16) Ornitholestes, (17) Compsognathus, (18) Archaeopteryx,
(19) Microvenator, (20) Deinonychus, (21) Thecodontosaurus,
(22) Efraasia, (23) Plateosaurus, (24) Ammosaurus, (25)
Anchisaurus, (26) Pisanosaurus, (27) Fabrosaurus and (28)
Heterodontosaurus.
would remain in the reptilian subclass Archosauria, which
would stand to Dinosauria much as the reptilian subclass
Synapsida (the mammal-like reptiles) stands to Mammalia.
This new classification, we believe, reflects more faithfully the
major evolutionary steps. Ectotherms and forms transitional
to endotherms are retained in the Reptilia and the two highly
successful endothermic groups, mammals and dinosaurs, are
given separate class status.
172
We
thank
J. Ostrom for
data
on
Archaeopteryx
and
A. W.
Crompton for access to fabrosaurid
and
heterodontosaurid
material. Supported in
part
by the National Science Founda-
tion. ROBERT T. BAKKER
Department
of
Vertebrate Paleontology,
Museum
of
Comparative
Zoology,
Harvard
University,
Cambridge,
Massachussetts
02138
PETER
M.
GALTON
Department
of
Biology,
University
of
Bridgeport,
Bridgepor~
Connecticut 06602
Received
June 25;
revised
October8, 1973.
1Ostrom,J. H., Q. Rev. Bioi. (in the press, 1974).
2. Bakker, R. T., in Perspectives
of
Biophysical Ecology (edit. by
Gates, D., and
Schmerl,
R. B.) (New York, in the press).
3Enlow,D. H., and Brown,S.
0.,
Tex. J.
s«,
2, 186 (1957).
4Currey, J. D., Palaeontology, 5, 238 (1962).
5Ricqles,
A,
Annis. Paleont., 54, 9 (1968).
6Bakker, R. T., Evolution, 25, 363 (1971).
7Bakker, R. T., Nature, 238, 81 (1972).
8Ostrom,
I.
0.,
Nature, 242, 136(1973).
1I Bonaparte, I. F., Proc. Pap. 2nd Gond. Symp, S. Afr., 665
(Council for
Scientific
and Industrial Research, Pretoria, 1972).
10
Bonaparte, I. F., Op, lilloana, 22, 183 (1971).
11 Casamiquela, R. M., Ameghiniana, 4, 47 (1967).
12. Reig, O. A., Ameghiniana, 3, 3 (1963).
13
Romer, A. S.,
Breviora,
389,1
(1972).
14
Thulbom, R.
A,
Nature, 234, 75 (1971).
15
Cruickshank, A. R., in Studies in Vertebrate Evolution (edit. by
Joysey, K.
A,
and Kemp, T. S.)(Oliverand Boyd,Edinburgh,
1972).
16
Young,C.C., Mem. Inst,
vertebr,
Paleont,Peking,
10,15
(1973).
17
Walker,A. D., Phil. Trans. R. Soc., B,
244,
103 (1961).
18
Walker, A. D., Phil. Trans. R. Soc., B, 248, 53 (1964).
ill
Walker, A. D., Phil. Trans. R. Soc., B, 257, 323 (1970).
2.0
Kuhn,
0.,
in Die Saurier der Deutschen Trias (Verglag Oeben,
Munchen, 1971).
2.1 Romer, A. S., in Vertebrate Paleontology (University of Chicago
Press,Chicago, 1967).
2.2. Charig, A. I., Attridge,
I.,
and Crompton, A. W., Proc. Linn.
Soc. Lond.,
176,197
(1965).
23
Romer,
AS.,
Breviora;395, 1 (1972).
24
Charig, A J., in Studies in Vertebrate Evolution (edit. by Joysey,
K., and Kemp, T.) (Oliverand Boyd, Edinburgh,1972).
25
Sawin,H. I.,J. Paleont.,21, 201 (1947).
26
Huene, F., von, in Die fossilen Reptilien des Siidamerikanischen
Gondwanalandes
(C. H. Beck'sche VerlagsbuchhandIang,
Milnchen,1935-1942).
27
Soergel,
W., in Die Fahrten der Chirotheria (lena, 1926).
28
Krebs, B., Schweiz. Palaeont. Abh., 81, 1 (1965).
211 Galton, P. M., Arnoldia, 15, 1(1971).
30
Galton, P. M., Lethaia, 4, 453 (1971).
31
Charig, A.
I.,
and Crompton, A. W., Boonstra Commemorative
Vol. (CapeTown, in thepress).
32. Hughes,B., S. Afr. J. Sci., 59, 221 (1963).
33
Sill,W., Bull. Mus.
Compo
Zool. Harv, (in the press).
34
Bonaparte,I. F., Zoo. J. Linn. Soc., 48, 471 (1969).
35 Huene, F. von, Paldont, Z., 16, 145 (1942).
36
Raath, M.
A,
Amoldia, 28, 1 (1969).
37
Cott, H. B., Trans. zool. Soc. Lond., 29,211 (1961).
38
Colbert, E. H., Amer. Mus. Novitates,2405, 1 (1970).
311 Galton, P. M., Paldont,
Z.,
47, 229 (1973).
40
Galton, P. M., Bull. Br. Mus. nat. HiM., A, 25, 1 (1974).
41
Bakker,R. T., Physiologist, Lond., 15, 3 (1972).
42. Romer, A. S., Breviora, 378, 1 (1971).
43
Romer, A. S., Breviora, 394, 1
(972).
44
Thulbom, R.
A,
Palaeontology, 13, 414 (1970).
45
Galton, P. M.,J. Paleont., 45, 781 (1971).
46
Ride,W. D., Syst, Ass. Pub., 3, 33 (1959).
47
Galton, P. M., Lethaia, 6, 67 (1973).
48
Galton, P. M., Evolution, 24, 448 (1970).
411 Walker,A D., Nature, 237, 257 (1972).
50
Ostrom, I. H., K. ned.
Akad.
v. Wet., B, 75, 289 (1972).
51 Dunson, W. A., Am. J. Physiol., 216, 995 (1965).
52. De Beer, G., in Archaeopteryx lithographica (British Museum
(Natural History), London, 1954).
53 Heilmann,G., in The Origin
of
Birds (D.Appleton and Co.,New
York, 1927).
54
Ostrom,I. H., Bull. Peabody Mus. nat.
Hlst.,
35 (1970).
55
Ostrom, I. H., Bull. Peabody Mus. nat.
si«,
30 (1969).
Nature Vol. 248 March
81974
Viroids and viral hepatitis in
marmosets
DIENER
land Zuckerman- have recently speculated
that
hepatitis A and B, respectively, may be caused by infective
naked nucleic acids or viroids.
In
response to their hy-
potheses, we felt it would be of interest to investigate
the
nature of an agent known to cause hepatitis in marmoset
monkeys. We reasoned
that
if the aetiologic agent of
hepatitis found in serum is a free, or naked, nucleic acid in
this system, then its infectivity should be destroyed by the
action of a specific endonuclease.
For
example, a free viral
DNA
would be rendered uninfective after treatment with
pancreatic DNase.
The
virus used in our
study
was the
'Barker' agent, originally recovered by Deinhardt et ol.
from acute phase sera of marmosets inoculated with serum
from ahuman case of viral hepatitis", This virus consistently
induces hepatitis in such animals, although its pedigree as
ahuman hepatitis agent has been asubject of controversys.
As many animal sera contain RNase activity,
but
not
DNase activity, we assumed the postulated viroid for Barker-
induced marmoset hepatitis, if it existed, would most likely
be anaked DNA. To test this assumption, we divided a
pool of infective acute-phase marmoset serum into two
equal aliquots. One aliquot was treated with pancreatic
DNase
(EC
3.1.4.5) at 20
p.g
ml" for 1h at 37° C; the
other aliquot was heated to 37° C for 1 h without any other
treatment. Three S. nigricoUis marmosets were inoculated
intravenously (i.v.) with treated serum (0.25 ml
each);
three other S. nigricollis marmosets were inoculated i.v. with
untreated serum. The course of infection in each marmoset
was monitored by measuring serum glutamic pyruvic trans-
aminase (SOPT) and serum isocitric dehydrogenase (SICD)
activities as indicator enzymes for liver damage.
All six marmosets demonstrated elevated
SOPT
and
SICD
activities by. the fourth or fifth week after inoculation, in-
dicating liver damages had been sustained in each animal.
Clearly, then,
the
marmoset hepatitis agent cannot be a
DNA viroid as all three animals receiving DNase treated
serum showed convincing enzymatic evidence of viral hep-
atitis.
The
results of our preliminary study
are
consistent
with the tentative finding by Deinhardt et al.5
that
the
Barker hepatitis agent bands in CsCI
at
abuoyant density
of 1.2. Viruses usually band around p=1.2-1.4, whereas
free viral
DNA
bands at about p=1.7.
While the possibility still exists
that
the
marmoset hep-
atitis agent is another
type
of viroid,
that
is, a unique
double-stranded
RNA
(or
RNA:DNA
hybridr-protein
con-
jugate which bands in CsCI
at
p=1.2, our experimental
evidence at least rules out the presence of a simple DNA
viroid in serum containing the marmoset agent.
D. W. BRADLEY
D. H.
KRUSHAK
J. E.
MAYNARD
Phoenix Laboratories,
Bureau of Epidemiology,
Center for Disease Control,
4402
North
Seventh Street,
Phoenix, Arizona 85014
Received November 29,1973.
1Diener, T. 0., Agric. Res. USDA, February (1972).
2Zuckerman,A.J., Lancet, 1, 1468 (1973).
3Deinhardt, F., Holmes, A., Capps, R., and Popper, H., J.
expo Med., 125, 673(1967).
Parks, W., and Melnick, J., J. inject.
DiB.,
120,539
(1969).
5Deinhardt, F., Wolfe, L., Junge, U., and Holmes, A., C.M.A.
J., 106, 468
(1972).
... (2) Second, there was a revolution in systematics that led to greater rigour. Cladistics had emerged in the 1960s as an objective, testable way to discover phylogenetic trees, and it quickly became apparent that Dinosauria was a clade, as suggested by Bakker and Galton (1974), although they had not constructed a cladogram. Bakker and Galton (1974) recognised that all dinosaurs shared unique features of the skeleton and skull, and these and other characters were deployed by Benton (1984aBenton ( ,b, 1985, Gauthier (1984Gauthier ( , 1986, and Sereno (1984Sereno ( , 1986 in the first independently analysed cladograms of dinosaurs. ...
... Cladistics had emerged in the 1960s as an objective, testable way to discover phylogenetic trees, and it quickly became apparent that Dinosauria was a clade, as suggested by Bakker and Galton (1974), although they had not constructed a cladogram. Bakker and Galton (1974) recognised that all dinosaurs shared unique features of the skeleton and skull, and these and other characters were deployed by Benton (1984aBenton ( ,b, 1985, Gauthier (1984Gauthier ( , 1986, and Sereno (1984Sereno ( , 1986 in the first independently analysed cladograms of dinosaurs. The diagnostic characters provided a yardstick for the first time that enabled palaeontologists to identify which taxa were inside the clade Dinosauria, and which outside. ...
... Ostrom, 1973Ostrom, , 1974 he showed powerfully that Huxley had been right and that birds were dinosaurs. This provided evidence for Bakker and Galton (1974) to name Dinosauria as a clade comprising dinosaurs and birds, as noted earlier (Section 2), and also provided the basis for Robert Bakker's arguments that dinosaurs had been endothermic. Further, as noted earlier (Section 2), the first cladograms in the 1980s showed that Dinosauria was indeed a clade, that birds were theropod dinosaurs (Gauthier, 1986), and that pterosaurs were a close sister group of Dinosauria. ...
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... The acetabular region of the archosaur ilium has been subject of discussion, since the presence of a partially to totally perforate acetabulum was accepted as a diagnostic character for Dinosauria (Bakker & Galton 1974;Gauthier 1986;Novas 1996;Benton 1999;Fraser et al. 2002). A more recent definition of this character deals with the ventral margin of the acetabular wall, which is regarded as concave in most dinosaurs, and more commonly convex to straight in non-dinosaur archosaurs (see Langer & Benton 2006). ...
... Thulborn 1975;Thulborn 2006), there is little consensus as to how this clade can be diagnosed. Previous studies have proposed a set of dinosaurian synapomorphies (Bakker & Galton 1974;Gauthier 1986;Novas 1989Novas , 1992Novas , 1996Sereno 1999), and recent reviews have regarded some of these characters as valid (Benton 1990(Benton , 1999(Benton , 2004Langer 2004;Langer & Benton 2006;Irmis et al. 2007a;Nesbitt et al. 2007). However, Fraser et al. (2002: 87) claimed that Rauhut (2003) ?????????? ?????????? ?????????? ?????????? ?????????? ?????????? ?????????? ??0??0?0?? ? ...
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We redescribe the holotype of the saurischian dinosaur Staurikosaurus pricei Colbert, 1970 from Late Triassic Santa Maria Formation (southern Brazil), following additional preparation that revealed new anatomical features. A revised diagnosis is proposed and the published synapomorphies for Dinosauria and less inclusive clades (e.g. Saurischia) are evaluated for this species. Some characters previously identified as present in the holotype, including the intramandibular joint, hyposphene-hypantrum articulations in dorsal vertebrae, and a cranial trochanter and trochanteric shelf on the femur, cannot be confirmed due to poor preservation or are absent in the available material. In addition, postcranial characters support a close relationship between S. pricei and Herrerasaurus ischigualastensis Reig, 1963 (Late Triassic, Argentina), forming the clade Herrerasauridae. Several pelvic and vertebral characters support the placement of S. pricei as a saurischian dinosaur. Within Saurischia, characters observed in the holotype, including the anatomy of the dentition and caudal vertebrae, support theropod affinities. However, the absence of some characters observed in the clades Theropoda and Sauropodomorpha suggests that S. pricei is not a member of Eusaurischia. Most morphological characters discussed in previous phylogenetic studies cannot be assessed for S. pricei because of the incompleteness of the holotype and only known specimen. The phylogenetic position of S. pricei is constrained by that of its sister taxon H. ischigualastensis, which is known from much more complete material.
... (3) If birds are derived from dinosaurian stock, as is now largely accepted (Bakker and Galton 1974, Paul 2002, Currie 2004, the fact that they survived and their larger cousins did not can be attributed to their early adoption of smaller size and feathers as physiological aids to exploiting an aerial niche. Body temperatures of birds in general are higher than those of mammals, and might in part be linked to their affinity with the reptilian version of endothermy and its evolutionary limitations within a nonequilibrial atmosphere. ...
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Biogeography has always been recognized as an interdisciplinary subject, but the relations involved are often referred to particular traditions of research only, and not to unifying principles that might cross such boundaries. Thus, historical biogeographers tend to emphasize the way past geographic relationships might influence species dispersal and divergence in a deterministic, black box fashion that neglects the ecological roles of the actors, whereas ecological biogeographers have often explained presence or absence on the basis of conditions of the immediate environment that are poorly linked to longer term, evolutionary, history. Through the use of the concept of final causes an attempt is made here to steer thinking toward population, community and ecosystem integration models that are less divisive in this regard. Applications to the study of mass extinctions, ten-year cycles in northern wildlife populations, and natural biogeographic range change are briefly described.
... Although there were fundamental disagreements concerning the monophyly or (Seeley's preference) diphyly and even polyphyly of dinosaurs with respect to their origin from archosaurian predecessors (e.g. Romer, 1933Romer, , 1968Charig et al., 1965;Bakker & Galton, 1974;Charig, 1982), Seeley's fundamental classificatory scheme proved robust in the face of continuous discoveries of new dinosaur taxa. In a major cladistic review of the Archosauria, Gauthier (1986) finally established a consensus over the matter of the monophyly of the Dinosauria and one that incorporated Seeley's two principal taxa as sister-taxa. ...
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... (3) If birds are derived from dinosaurian stock, as is now largely accepted (Bakker and Galton 1974, Paul 2002, Currie 2004, the fact that they survived and their larger cousins did not can be attributed to their early adoption of smaller size and feathers as physiological aids to exploiting an aerial niche. Body temperatures of birds in general are higher than those of mammals, and might in part be linked to their affinity with the reptilian version of endothermy and its evolutionary limitations within a nonequilibrial atmosphere. ...
Article
Biogeography has always been recognized as an interdisciplinary subject, but the relations involved are often referred to particular traditions of research only, and not to unifying principles that might cross such boundaries. Thus, historical biogeographers tend to emphasize the way past geographic relationships might influence species dispersal and divergence in a deterministic, black box fashion that neglects the ecological roles of the actors, whereas ecological biogeographers have often explained presence or absence on the basis of conditions of the immediate environment that are poorly linked to longer term, evolutionary, history. Through the use of the concept of final causes an attempt is made here to steer thinking toward population, community and ecosystem integration models that are less divisive in this regard. Applications to the study of mass extinctions, ten-year cycles in northern wildlife populations, and natural biogeographic range change are briefly described.
... Additionally, the ilium has an anteriorly pointing preacetabular process, so that the pelvis appears four-pronged in lateral view. Basal ornithischians are poorly documented by scarce fossils; consequently, their origin and phylogenetic relationships with saurischians and silesaurids have long been, and are still discussed (Galton 1970;Bakker and Galton 1974;Gauthier 1986;Langer and Benton 2006;Langer and Ferigolo 2013;Padian 2013;; ; . Researches dating back from the very first numerical phylogenetic analyses profoundly changed our conception of ornithischian relationships. ...
Article
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... Ostrom 1976;Gauthier 1986), leading to speculation that the most talismanic of avian features, feathers, would eventually be discovered in their non-avian relatives (e.g. Bakker and Galton 1974;Paul 1988). Spectacular discoveries of exquisitely preserved non-avian theropods from the Early Cretaceous Jehol Biota of China confirmed this prediction (Chen et al. 1998), and numerous subsequent finds showed that feathers and other feather-like structures were widespread amongst coelurosaurs and potentially primitive for theropods as a whole (e.g. ...
Chapter
Over the last two decades, the dinosaur fossil record has revealed much about the nature of their epidermal structures. These data challenged long-standing hypotheses of widespread reptile-like scalation in dinosaurs and provided additional evidence that supported the deeply nested position of birds within the clade. Moreover, in recent years, the discovery of filamentous structures in numerous species across the dinosaurian evolutionary tree suggests a model of deep feather homology within dinosaurs, with the appearance of feathers hypothesised to coincide with the dinosaur origin. Thanks to phylogenetic comparative methods, these homologies can now be tested empirically and form the basis of this study. Based on a dataset of 77 dinosaur species that preserve integumentary structures, we undertake a series of model-fitting and ancestral state reconstruction analyses to interpret the evolutionary history and ancestral integumentary condition in dinosaurs. Our results provide the first empirical support for the evolution of feathers in an ordered fashion, but reveal that these evolutionary trends were not always towards ‘more complex’ conditions. Ancestral state reconstructions demonstrate that irrespective of the preferred phylogenetic framework, the ancestral pterosaur condition or whether any one major dinosaur lineage had a Late Triassic-feathered representative, support values for a filamentous/feathered dinosaur ancestor are low. More examples of feathered taxa from across the dinosaur tree, and in particular the discovery of as yet unknown feathered Triassic taxa, will be needed in order to overturn current support for a scaly dinosaurian ancestor.
... This observation suggests that enlargements of the inner acetabular foramen occurred in parallel in the dinosaurian clades. Bakker & Galton (1974) suggested that the perforate acetabulum is a mechanical consequence during the evolution of adducted hip posture in archosaurs, such that the decrease in medially directed ground reaction forces favors the reduction, and eventual loss, of bony inner acetabular walls. Egawa et al (2018) further investigated the developmental mechanism of acetabular perforation in the avian hip joint, and proposed that the evolution of a membranous inner acetabular wall in dinosaurs resulted from the loss of cartilaginous anlagen at the inner acetabular wall during embryogenesis. ...
Article
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Article
Full-text available
Triassic beds from Argentina and Brazil provide the most relevant fossil record of early dinosauriforms in terms of numerical abundance and taxonomic diversity. This record currently represents the best source to understand the origin and early evolutionary radiation of dinosaurs. In the present paper we offer an updated review focused on the available evidence of Carnian dinosaurs from this continent, but we also discuss the record of Triassic dinosaur precursors and the evolution of Triassic dinosaurs in other continents. It is clear that, aside the agreed taxonomic composition of some particular dinosaurian subclades (e.g., Herrerasauridae, Neotheropoda), there is no consensus about early dinosaur phylogeny, and our paper is not the exception. Recent years witnessed the discovery of several new early dinosaurian taxa, as well as reviews of the taxonomic allocation of several renowned forms such as Lagerpeton, Lewisuchus, Pisanosaurus, and Eoraptor. New analyses demonstrate that evidence supporting the taxonomic referrals of pre-Norian dinosaurs to Theropoda, Sauropodomorpha and Ornithischia are tenuous, at best. Here we present new anatomical observations and comparisons for each of these South American early dinosauriforms with the aim to test previous phylogenetic interpretations. Evidence from South America allows reviewing the phylogenetic relationships of taxa from other continents, including Tawa, Chindesaurus, and Daemonosaurus, which are here suggested to nest within Herrerasauria. Evidence at hand indicates that herrerasaurs were a successful clade of archaic predatory saurischians that inhabited both South and North America, and probably also India and Europe.
Article
Pterosaurs, which lived during the Mesozoic, were the first known vertebrates to evolve powered flight.¹,² Arboreal locomotion has been proposed for some taxa,³,⁴ and even considered to have played a role in the origin of pterosaur flight.⁵,⁶ Even so, there is still need for comprehensive quantitative ecomorphological analyses.³,⁴ Furthermore, skeletal adaptations correlated to specialized lifestyles are often difficult to recognize and interpret in fossils. Here we report on a new darwinopteran pterosaur that inhabited a unique forest ecosystem from the Jurassic of China. The new species exhibits the oldest record of palmar (or true) opposition of the pollex, which is unprecedented for pterosaurs and represents a sophisticated adaptation related to arboreal locomotion. Principal-coordinate analyses suggest an arboreal lifestyle for the new species but not for other closely related species from the same locality, implying a possible case of ecological niche partitioning. The discovery adds to the known array of pterosaur adaptations and the history of arborealism in vertebrates. It also adds to the impressive early bloom of arboreal communities in the Jurassic of China, shedding light on the history of forest environments.
Article
Locomotion, activity patterns, and thermoregulation were closely related in the evolution of tetrapods. The short, stocky limbs of the first Carboniferous reptiles suggest that they were not heliophilic and were active in the shaded areas of the coal forests. The first archosaurs retained the sprawling locomotion and possibly the thermal preferences of primitive reptiles. However, by the Mid Triassic large, predatory archosaurs with more erect posture and very gracile, quick-action limbs appeared, and in these animals the metabolic scope and endogenous heat production during activity may have exceeded that of large living monitor lizards. Fully Erect Posture, permitting support of the body free of the ground for long periods of time, appeared in dinosaurs at the end of the Triassic. Dinosaurs probably combined large body size, high body temperature, large hatchling size, and continuous high levels of activity with an efficient aviantype air-sac system for loss of excess heat. Thus dinosaurs could achieve homeothermy in the warm Mesozoic climates. Birds were derived from dinosaurs, and, with the development of feathered insulation, could apply the dinosaurian mechanisms for homeothermy to small body size. Advanced mammal-like reptiles may not have been heliophilic, but specialized in reducing surface area to volume ratios, possibly to conserve heat. In the competition with Triassic archosaurs, the retention of sprawling locomotion and possibly the lack of efficient heat-loss mechanisms in therapsids caused their extinction. However, with the development of superficial insulation of hair and high endogenous heat production, the first mammals could maintain their activity temperatures all through the night and could exploit nocturnality more extensively than nocturnal lizards, while avoiding activity during the day and thus reducing the dangers of overheating and of contact with the large predatory diurnal lizards and dinosaurs. Mesozoic mammals were restricted to small body size partly because of the difficulty of losing excess body heat in a large mammal lacking efficient evaporative cooling, but mostly because mammals were competitively inferior to dinosaurs during the day and were forced to seek secure diurnal shelters in trees and burrows to escape the great reptiles.
Article
The postpubic rod of ornithischians is homologous with the pubis of birds and other reptiles and the prepubic process, that was not specifically developed for abdominal support, was probably formed after the main part of the pubis came to lie parallel and close to the ischium. This change in position of the pubis of ornithischians and birds resulted in a posterior shift of the center of gravity that was advantageous to a bipedal animal. The change was possible once the musculature on the pubis was no longer necessary for protracting the femur because it was functionally replaced by the musculature on the anterior process of the ilium. The posterior reorientation of the pubis may only have occurred once but birds cannot be derived from any known ornithischian. The common ancestor of ornithischians and birds may have been a cursorial biped of the Middle Triassic with a long anterior process to the ilium and a backwardly directed pubis. The lack of similarity between the two groups is attributed to the specializations of ornithischians associated with the great adaptive shift to a herbivorous diet. Several features of birds, including the backwardly directed hallux, were probably developed during a cursorial "Preproavis" stage that subsequently took to the trees to give the arboreal "Proavis" that gave rise to Archaeopteryx and the other birds.
Article
The osteology of Ornithosuchus is described in some detail. This study is largely based on material discussed by previous workers, but also takes into account specimens hitherto undescribed. It is considered that the species O. taylori Broom 1913 is invalid, being based on larger individuals of the form previously named O. woodwardi by Newton (1894). Furthermore, evidence is presented to show that specimens previously described by Huxley (1877) and Walker (1961) as Dasygnathus longidens are also referable to Ornithosuchus. It is concluded that but one species is present in the material, the correct name for which is Ornithosuchus longidens (Huxley). At least eleven individuals are present with skulls ranging from about 50 to 450 mm in length. Observations on the smaller members of this series suggest that changes in the shape and proportions of the skull took place with growth in a similar manner to those seen in living crocodiles. In the light of new information concerning the osteology of Ornithosuchus it is considered that this reptile is a primitive carnosaur, occupying a position very close to the ancestry of the Jurassic and Cretaceous members of this group. An examination of descriptions and figures of Triassic reptiles referred by von Huene (1932) and later authors to the Carnosauria has led to the conclusion that the great bulk of this material is more properly allocated to the Prosauropoda, and that the only Triassic carnosaurs known at the present time, apart from Ornithosuchus, are Teratosaurus and Sinosaurus, these two names being here used in a restricted sense. It is suggested that Ornithosuchus is close to the common ancestry of both the Megalosauridae and the Tyrannosauridae, and the derivation of the skull patterns of these forms from that of Ornithosuchus is discussed. Additional fenestrations marginal to the preorbital fossa and in the surangular of advanced carnosaurs are held to be related to the development of the pterygoid musculature rather than to the need to lighten the skull. In the course of a brief review of the Carnosauria the view is put forward that Acrocanthosaurus is a Lower Cretaceous representative of the tyrannosaur group, using this term in a broad sense, and is perhaps related to the Cenomanian Spinosaurus and the Wealden Altispinax. As a result of examination of English megalosaurian material, the name Eustreptospondylus oxoniensis gen. et sp.nov. is proposed for the Oxford specimen previously known as `Streptospondylus' cuvieri, and Metriacanthosaurus gen.nov. for Megalosaurus parkeri. The incomplete cranium from Dives figured by Piveteau (1923) is made the type of a new species, E. divesensis, to which certain other carnosaurian material from Normandy is provisionally allocated. Following Chakravarti (1935), the endoskeletal elements included by Matley (1923) in the type material of the Indian nodosaur Lametasaurus are held to belong to one or other of the two carnosaurs Indosuchus and Indosaurus, but the numerous scutes are not thought to be carnosaurian and the name Lametasaurus is here restricted to them. It is suggested that Indosuchus from the? Turonian is a tyrannosaurid. On the other hand Ceratosaurus and Proceratosaurus are regarded as coelurosaurs. A modified classification of the Infra-order Carnosauria is given, in which two main groups are recognized; Superfamily Megalosauroidea to include the Megalosauridae, and Superfamily Tyrannosauroidea to include the Ornithosuchidae (restricted), Spinosauridae and Tyrannosauridae.
Article
The unique holotype of Hallopus victor (Marsh), from the Upper Jurassic of Garden Park, Colorado, is redescribed. The bones previously identified as pubes (Marsh 1890) or ischia (von Huene 1914) are regarded here as the left radius and ulna, and the 'ulna' and 'radius' of previous workers are considered to be the left radiale and ulnare. Marsh's identification (1890) of the ischium and his orientation of the scapula and femur (1896) are upheld. The presence of a humerus on the larger slab is confirmed. Hallopus is interpreted as a highly specialized, cursorial crocodilian, with slender, hollow bones, a greatly elongated radiale and ulnare, and a roller-like joint between these and the metacarpals. The manus is pentadactyl with a symmetrical distribution of lengths about the central axis and some proximal wedging-out of the metacarpals. The iliac blade is elongated and resembles that of Orthosuchus, the ischium is reminiscent of that of Protosuchus. The femur has a lesser trochanter, a fourth trochanter and a 'pseudointernal' trochanter, but no greater trochanter. The tibia is longer than the femur. The tarsus is basically crocodilian in pattern, but greatly compressed and specialized. The first metatarsal is reduced to an elongated splint, permanently recessed into metatarsal II. Metatarsals II to IV are symmetrical in length with III longest, metatarsal V is reduced, pointed, and lacks phalanges. The interpretation put forward provides a consistent explanation of the peculiarities of the skeleton of Hallopus as a variant on the basic crocodilian plan. The details of the articulation of the carpal and tarsal joints are described as far as preservation permits, and possible movements are considered. The carpometacarpal and tarsal joints are simple hinges, but the proximal carpal joint appears to have been relatively immobile and the elongation of the radiale and ulnare is viewed as a device to compensate for the increase in length of the tibia. The femur has an off-set, ball-like head and evidently moved essentially in a parasagittal plane. The pes is functionally tridactyl, with the metatarsals locked together proximally. It is concluded that both fore- and hind-feet were digitigrade during movement, although in a stationary pose the metatarsus may have been in contact with the ground. Some aspects of the pelvic and hind-limb musculature are briefly discussed. Functional analogies from the locomotory point of view are limited by the lack of cursorial quadrupedal archosaurs for comparison. It is concluded that a hare-like bounding gallop was the most probable type of fast locomotion in Hallopus. Although no skull bones have been identified, evidence from the postcranial skeleton is adduced to show that Hallopus is of pedeticosaurid descent. The relationships of early crocodilomorphs are discussed, and it is deduced that two basic stocks diverged from a common ancestry during the middle part of the Trias. These two groups are included in an expanded Order Crocodylomorpha. The Suborder Crocodylia has the Triassic Stegomosuchidae as its radicle and contains 'normal' crocodiles (including the Sebecosuchia but not the Baurusuchidae). The suborder Paracrocodylia is proposed for mainly cursorial forms, to include the infraorders Pedeticosauria, Baurusuchia and Hallopoda. Diagnoses for these groupings are presented. An origin for both stocks from a form close to Cerritosaurus is postulated. Erpetosuchus and Dyoplax are not now regarded as crocodilomorphs. The possibility of an early cursorial phase in crocodilian evolution is briefly discussed, and it is tentatively suggested that the gallop occasionally observed in young crocodiles (Cott 1961) may be a relic of a primitive type of locomotion in the group. The significance of this to the emergence of the crocodilian type of shoulder-girdle is considered.
Article
The maxilla named by T. H. Huxley Dasygnathus longidens, from the Trias of Findrassie near Elgin, is re-described. A pterygoid from the same locality is referred to this species and described for the first time. These two bones indicate a large, carnivorous pseudosuchian apparently allied to Erythrosuchus. A detailed description is given of the osteology of the pseudosuchian Stagonolepis, amplified by a large number of hitherto undescribed specimens. The material (considered to represent at least twenty-one individuals) shows an almost complete segregation into two size-groups, distinguished by only a few minor morphological differences of the postcranial skeleton. The larger and small individuals are considered to be males and females respectively, of the one species S. robertsoni Agassiz. Study of Stagonolepis has demonstrated its close relationship to Aetosaurus from the Stubensandstein (Keuper) of Stuttgart. The latter genus, however, was in urgent need of revision. Accordingly a brief account is included of the principal respects in which previous descriptions of this form require modification. Specimens referred by von Huene (1921) to A. crassicauda are shown to have been misidentified in many cases; this material is a composite of a small coelurosaur and a true aetosaurid. Some modifications are also suggested to previous accounts of Typothorax and Desmatosuchus from the Trias of North America, and new restorations are given of the skulls of these forms. The extremely close relationship between Stagonolepis and Aetosaurus, perhaps even indicating generic identity, makes unavoidable the merging of the two families previously founded on these genera. On grounds of priority the name Aetosauridae is retained for the taxonomic unit which includes Aetosaurus, Stagonolepis, Typothorax and Desmatosuchus as principal members. A restricted diagnosis of the family Aetosauridae is given, based on the above four forms, and this is followed by a review of the genera which have from time to time been included in the former families Stagonolepidae and Aetosauridae. The great majority of these genera are excluded from the group as now defined. Possible evolutionary trends within the family are briefly outlined; the sequence of increase of specialization appears to be Aetosaurus, Stagonolepis, Typothorax, Desmatosuchus. The conclusions of Dollo (1884), Adams (1919) and others concerning the function of the preorbital fossa in archosaurian reptiles are endorsed, and it is suggested that a trend towards the reduction of the anterior pterygoid muscle took place in aetosaurids, in parallel with a similar trend in ornithischian dinosaurs. Many features of the skeleton of aetosaurids recall the Ornithischia. These include the elongate naris, reduced dentition, vertical or forwardly inclined quadrate, slipper-shaped jaw, small skull and well-developed dermal armour. However, a direct ancestor-descendant relationship appears to be ruled out by the position of the supratemporal fossa, reduction of the infratemporal opening, probable loss of the coronoid and typically pseudosuchian pubis, although the aetosaurids may well lie close to the root-stock of the Ornithischia. The mode of life of the aetosaurids is considered, and it is concluded that these animals were herbivorous, or possibly feeders upon invertebrates obtained, in the case of Stagonolepis at least, by digging with the peculiar expanded snout-tip and dentary rostrum. A simple muscular mechanism is postulated whereby this could be effected. The stratigraphical implications of these studies are briefly examined and the suggestion, based primarily on the close relationship between Stagonolepis and Aetosaurus, is put forward that the Triassic sandstone of Elgin occupies a higher horizon than has previously been considered.
Article
Detailed evidence from the skull of Sphenosuchus, and from embryological and other resemblances between birds and crocodiles, suggests that these two groups are much more closely related than has been realized
Article
WALKER1 has restated the long-held belief that both birds and crocodiles evolved from thecodont ancestors, but he added the novel suggestion that these two groups arose from a common thecodont ancestor and thus are much more closely related than has been previously realized. Inasmuch as the Thecodontia include the most primitive as well as the most ancient archosaurs known, it is highly probable that all subsequent archosaurs (including birds) were derived from members of this order. Although Walker may be correct, I do not think that the evidence cited indicates such a close relationship between birds and crocodiles as he proposes.