SAUROPODOMORPHS
Sauropodomorph ancestry is close
to that of theropods; they were the first dinosaurs to become quadrupedal,
and then dramatically larger and more derived. According to Sereno (1999)
only a few synapomorphies unite sauropodomorphs; among these are enlarged
nares (= small head) and the longest pedal ungual is in the first toe (hallux).
Sauropodomorph synapomorphies
after Langer et al. (1999)
-
skull length less than 50% of length
of femur
-
lanceolate teeth
-
deltopectoral crest more than 50%
of humerus in length
-
anterior blade of ilium short and
pointed
-
deep proximal portion of pubes
-
ascending process of astragalus
broad and laterally elongated
PROSAUROPODS (TEXT,
Chapter 15)
-
Small headed, archaic saurischians
-
Tooth row often extends behind the
anterior edge of orbit
-
Gastric stones in two genera, gut
processors, no occlusal wear on teeth (characteristic of herbivores)
-
Larger size and lengthening of neck
rendered plant productivity more accessible to prosauropods than to ornithischians
-
Inhabited a variety of fluvial to
semi-arid environments of deposition (red-bed, aeolian)
Sixteen genera are known, evidently
comparable to (slightly less than) hadrosaurs in diversity. They were the
most abundant large terrestrial animals for 50 myr (through late Triassic
and early Jurassic time, Upchurch 1997).
Prosauropods are comparable to,
but somewhat smaller in size than hadrosaurs (2.5 - 11 m long, up to 2
mt)
Completely known taxa:
Plateosaurus
Massospondylus
Anchisaurus
Yunnanosaurus
Lufengosaurus
Riojasaurus
Saturnalia Carnian of
Brazil, body 1.5 m long (Langer et al. 1999)
Azendohsaurus Carnian of
western High Atlas; muzzle from skull 20 cm long, body 3 m long
Plateosaurus 4 bonebeds
(latest Triassic)
Heavy animals mired in seasonally
wet muds (juveniles spared, high weight bearing of feet, high natural selection)
Massospondylus Early-middle
Liassic, femoral rings indicate maturity in 15 years, 300 kg, rather slow
growth rate, indeterminate
Evolution in prosauropods:
-
Thecodontosaurus (Liassic
biped 2.5 m long) usually considered typical for primitive prosauropod
(chimera according to Nick Fraser)
-
see 40 primitive to derived conditions
in Galton, TEXT, p. 334-337
-
in bipedal forms the forelimbs are
as short as in Eoraptor, comparisons with Eoraptor (where
only distal part of tail is missing):
Eoraptor Prosauropods
- head large relative to neck
- head small relative to neck
- ext nares normal * external
nares enlarged
- pmx excludes maxilla from *
maxilla enters narial margin
nares
- postnarial process of mx -
postnarial process of mx
triangular triangular to narrow
and erect
- anterior teeth leaf-shaped
- posterior teeth leaf-shaped
- 4 pmx, 18 mx teeth (small size)
- 3-6 pmx, 11-30 mx teeth
- mx teeth to center orbit -
mx teeth to antorbital process
- 8 cervical vertebrae, centra
- 10 cervical verts, centra
short (no pleurocoels) long (no
pleurocoels)
- cervical ribs robust - cervical
ribs delicate
- 16 dorsal vertebrae - 15 dorsal
vertebrae
- about 45 caudals? - about 50
caudals
- manus ungual I small - manus
ungual I enlarged
- manus IV with 1 phal * manus
IV with 1-3 phal
- manus V with no phal * manus
V with 0-2 phal
- pubis broad laterally * pubis
narrow laterally
- tibia longer than femur * tibia
shorter than femur
- ischium tapers distally * ischium
expands distally
- pes V with 1 phal - pes V with
0-1 phal
In Saturnalia
-
the head is small (1/3 length of
femur) and the neck is short
-
teeth lanceolate, coarsely serrated
-
9? cervicals, 15 dorsals
-
next-to-last cervical much longer
than dorsals (sauropodomorph)
-
vertebra added to sacrum from tail
(sauropodomorph)
-
deltopectoral crest * length of
humerus (sauropodomorph)
-
pubis narrow laterally
-
femur and tibia equal in length
-
ischium expands distally
-
mtt V reduced
Which came first, Eoraptor
or prosauropods?
Eoraptor apomorphies:
-
large skull
-
jugal forked posteriorly
-
robust cervical ribs
-
loss of phalanges in external manal
digits
Prosauropod apomorphies
-
long neck
-
large body, enlarged external nares
-
manus ungual I enlarged (support
against trees; cf. sauropods, Upchurch 1993 Gaia 10: 161-171).
Three major varieties (TEXT, Upchurch
1997. Enc. Din.)
Thecodontosauridae (small)
Plateosauridae (medium)
Melanorosauridae (large)
Melanorosaurids parallel the
later sauropods in:
-
large body size
-
quadrupedal stance
-
straight femur shaft
-
increase in body size through time
Riojasaurus 2-7 m long, Norian
melanorosaur (Bonaparte 1995, Ameghiniana 32: 341-349; Upchurch 1997)
-
lacrimal vertical, does not overhang
antorb fen
-
5 pmx, 24 mx, teeth, carinae finely
serrate
-
mx teeth extend back to beneath
center of the orbit
-
craniomandibular articulation in
alveolar plane
-
posterior "cervicals" taller, shorter
than in Plateosaurus
-
hindlimb shorter relative to trunk
than in Plateosaurus
Why prosauropods are sister group,
not ancestors, of sauropods; apomorphic characers:
-
in prosauropods the dorsal process
of the maxilla is distinct, its base is in the anterior half of the bone
(usually anterior third), and never on the posterior half (Gauffre 1993,
Palaeontology 36: 897-908)
-
also in Eoraptor,
displacement posteriorly due to derived enlargement of sauropod nares
-
in sauropods the mt V is unreduced,
and hence cannot be derived from that of prosauropods (Galton TEXT, p.
334)
-
note more massive, abbreviated
sauropod pes
Prosauropod apomorphies barring
them from ancestry of sauropods (Upchurch 1997)
-
keratinous beak and fleshy cheek
-
tall and dorsally directed maxillary
acending process
-
twisted pollex (thumb) tipped by
large, inwardly pointing claw (see also Sereno 1999), could be elevated
while walking quadrupedally
-
triangular cross section through
distal end of ischium (apparently present in Herrerasaurus)
-
reduction of fifth metatarsal
Benton et al. 2000 (JVP 20 (1):
77-108) regard prosauropods as a clade rather within, rather than a series
of outgroups of the sauropoda.
The Oldest Sauropod?
(Buffetaut et al. 2000. Nature 407: 72-74)
Isanosaurus: one cervical,
one dorsal and 6 caudals, neural spine of one posterior dorsal, two chevrons,
one scapula and one sternal plate, and one femur ? latest Triassic of Thailand.
-
cervical opisthocoelous; amphiplatyan
in prosauropods
-
isolated neural spine is taller
than in prosauropods, with incippient posterior lamina not seen in prosauropods
-
femur 76 cm long, straight shaft,
flattened anteroposteriorly, sigmoid 4th trochanter
Peculiarities include the very short
vertebrae, upwardly oriented femoral head and expanded distal end of femur
There are no skeletal parts preserved
which would show prosauropod apomorphies. But it does look like an archaic,
abbarent sauropd.
SAUROPODS Quadrupedality
is achieved with increase in size, cf. from prosauropods weighing 300 kg
at the base of the Jurassic to animals weighing on the order of 50 mt within
25 myr.
A small sauropod is 15 m long
and weighs 12 mt; few dinosaurs are larger.
Gigantic sauropods (Paul 1997,
Dinofest International Proceedings, Acad. Nat. Sci. Philadelphia):
-
cf. Supersaurus (diplodocid)
scap-cor: 35-45 m, 40-50 mt
-
Amphicoelias (diplodocid)
dorsal neural arch: 40-60 m, 100-150 mt
-
Argentinosaurus (titanosaur)
dorsals: 80-100 mt
Anderson et al. 1985 (J. Zool.,
London 207: 53-61), Monbaron et al. 1999 (C. R. Acad. Sci. Paris 329: 519-526),
Rich et al. 1999 (Natl. Sci. Mus. Tokyo Monographs 15: 61-84), McIntosh
et al. 1996 (Bull. Gunma Mus. N. H. 1)
Brachiosaurus: 29 mt
Cf = 730 mm, Ch = 654 mm; ratio
= 1.1162
Opisthocoelicaudia: 22
mt
Cf = 680 mm, Ch = 565 mm; ratio
= 1.2035
Atlasaurus: 22.5 mt (Bathonian-Callovian)
Cf = 690 mm, Ch = 565 mm; ratio
= 1.2212
Tehuelchesaurus: 31.5 mt
(Callovian or earlier)
Cf = @805 mm, Ch = 615 mm; ratio
= 1.3089
Apatosaurus: 35 mt
Cf = 845 mm, Ch = 629 mm; ratio
= 1.3434
Camarasaurus: 19.5 mt
(CM 11393)
Cf = @689 mm, Ch = 502; ratio
= 1.3725
Av. Cf/Ch = 1.26, sd = 0.0973
Camarasaurus: 1.6 mt
Cf = @268 mm, Ch = @207.5; ratio
= 1.2916
Camarasaurus: 9.3 mt
Cf = 514 mm, Ch = 394; ratio
= 1.3046
Camarasaurus: 15.7
mt
Cf = 630 mm, Ch = 472; ratio
= 1.3347
Camarasaurus: 19.5
mt (CM 11393)
Cf = @689 mm, Ch = 502; ratio
= 1.3725
Camarasaurus alenquerensis:
26
mt
Cf = 785 mm, Ch = 547 mm; ratio
= 1.4351
Av. Cf/Ch = 1.35, sd = 0.0579
Wq = 0.078 Ch+Cf exponent 2.73
+/- 0.09
Wb = 0.16 Cf exponent 2.73
Gara Samani humerus 96 cm + in
length, Ch = 716 mm
Cf = Ch x 1.27 (Anderson et al.
1985, table IV)
Cf = 911 mm
Largest sauropod Cf:
-
Antarctosaurus ? 820, measurement
by D.A.R. ? 34.2 mt
-
Camarasaurus ? 826, measurement
by D.A.R. (identification by J. S. McIntosh, personal communication 1997)
? 35 mt
-
Gara Samani sauropod ? 45.6 mt
Sauropod eye: sclerotic plates -
Brachiosaurus
70 mm, Diplodocus 55 mm, Nemegtosaurus 73 mm - only hadrosaurs
have larger eyes.
The name Brontosaurus -
first restoration by Marsh (1883), first mount in AMNH (1905), a primary
effect was an enlargement of Museum galleries
Completely known taxa:
Camarasaurus
Shunosaurus
Diplodocus
Apatosaurus
Brachiosaurus - east African
specimens not fully mature
Comparison of Diplodocus,
TEXT: fig. on p. 346, with Plateosaurus TEXT, fig. on p. 321 (*
= weight related character):
-
*shorter skull
-
reduction in number of teeth
-
nares displaced posteriorly
-
small jugal, large quadratojugal
-
cervicalization of dorsals (from
10 cervicals in prosauropods to 19 in one Chinese sauropod)
-
*pneumatization (pleurocoely)
from anterior part of neck posteriorly
-
*enlarged zygosphene-zygantra
-
*increase in number of sacrals (1
from dorsal, 1 from caudal)
-
*broadening of lower scapula, ilium
-
*solid, column-like limb bones
-
metacarpals longer than metatarsals
-
*reduction in number of phalanges
-
remaining claws narrow and deep
"Elephant analogues" or "Parelephants"
Definition of Sauropods:
Combination of Upchurch 1998. (Zool. J. Linn. Soc. 124: 43-103), and Wilson
and Sereno 1998. (JVP 18, suppl. No. 2, SVP Mem 5, 68 p.):
-
4th (caudal) vertebra
incorporated into sacrum
-
caudal ribs disappear on caudal
16, or more anteriorly
-
obligatory quadrupedal posture with
columnar limbs, fore/hind limb length ratio 0.66 or more
-
deltopectoral crest of humerus low
-
olecranon process on ulna ("crazy
bone") reduced or absent
-
proximal end of ulna triradiate,
deep radial fossa
-
distal end radius subrectangular,
flat articulation for ulna
-
ilium with low ischial peduncle
-
ischial shaft equal to or longer
than pubic shaft
-
ischial shaft with dorsoventrally
flattened distal end
-
femoral shaft straight, anteroposteriorly
compressed, lesser trochanter reduced
-
tibia/femur less than 0.65
-
distal tarsals fail to ossify
-
mtt V enlarged (reversal analgous
to mtt I contacting ankle in therizinosaurs)
No information in the diagnosis
pertains to the skull, neck, back or shoulder girdle. These parts are not
preserved in type skeleton of the heretofore most primitive sauropod, Vulcanodon,
from the early Jurassic of South Africa, which has (Upchurch 1995):
-
4 sacrals
-
long forelimbs (0.75 hind limbs)
-
reduced lesser trochanter (absent
in all other sauropods)
-
distal "roller" on astrag
-
no distal tarsals
-
length of mtt V 75% length of mtt
IV
Tooth to tooth occlusion, as evidenced
by flat wear facets on the teeth, is also diagnostic of early sauropods
(Barrett 1999, JVP 19 (4): 785-787).
EUSAUROPODA ("TRUE SAUROPODS")
fide Upchurch 1995 (Phil. Trans. Roy. Soc. London, Ser. B, 349:365-390),
see Sereno 1998, Upchurch 1998 for more details
Characters known to be advanced
over basal sauropods (Upchurch 1998):
-
loss of denticles on tooth crowns
-
transverse processes of dorsal vertebrae
directed dorsolaterally
-
fourth trochanter reduced to a low
rounded ridge (ridge longer and more acute in Isanosaurus)
-
length of mtt V 85% or more that
of mtt IV
Cranial characters which
may be present in basal sauropods:
-
retraction of external nares
-
snout with stepped, "shelf-like"
subnarial margin
-
ascending process of maxilla meets
lacrimal
-
short skull roof and temporal region
-
anterior lower temporal opening
extends beneath orbits
-
external mandibular fenestra reduced
-
teeth procumbant
-
teeth anterior to or below antorborbital
fenestra
Postcranial characters which
may be present in basal sauropods:
-
two additional cervicals (total
of 12, or more)
-
metacarpals arranged in a semicircular
collonade
-
manus 2-2-2-2-1 or less
-
pubis short, robust, not twisted
-
pedal digit IV with 3 phalanges
-
metatarsal I short, robust
-
loss of ligament pits on pedal phalanges
CLASSIFICATION OF SAUROPOD SUBGROUPS
HAS BEEN VERY UNCERTAIN
-
incompleteness of material
-
homoplasy
Incompleteness of material:
about as much morphology as a mouse skeleton, but takes years to collect
and prepare
Skeletal problems
-
skull loosely attached, easily detached
-
neck pneumatised, easily displaced
-
posterior dorsals, base of tail,
appendicular elements heavy, displaced with difficulty
Sedimentological problems (Hunt
et al. 1994, Gaia 10: 261-279)
-
large carcasses hard to move
-
skeleton much "thicker" than annual
rate of sedimentation
Resulting record (see also Hunt
et al.):
-
very few complete skeletons:
Shunosaurus 5 skeletons with
skulls
Camarasaurus 5 skeletons
with skulls
Apatosaurus 1 skeleton
with skull
-
5 of 90 genera completely known
osteologically
-
reasonably complete skulls for 11
genera
Homoplasy:
-
elevation of nostrils
-
pneumatization of vertebrae front
to back
-
split cervical spines
-
increase in neck length
-
procoelous caudals
-
divided chevrons
-
tail clubs
Russell and Zheng 1993 (Can. J.
Earth Sci.) 9 taxa, 21 characters, consistency index 0.59, 6% matrix question
marks
Calvo and Salgado 1995 (Gaia
11: 13-33) 15 taxa, 49 characters
consistency index 0.66, 21% matrix
question marks
Upchurch 1994 (Gaia 10: 249-260)
32 taxa, 174 characters
consistency index 0.63
Wilson and Sereno 1998: 10 taxa,
109 characters
consistency index 0.81, 22% matrix
question marks
Upchurch 1998: 26 taxa, 205 characters
consistency index 0.55, 46% matrix
question marks
Differences between Wilson
and Sereno (WS), and Upchurch (U):
Euhelopus
-
with Chinese Euhelopodids (U)
-
at base of titanosaurs (WS)
Haplocanthosaurus
-
sister group of diplodocoids (U)
-
sister group of brachiosaurs (WS)
Similarities between Wilson and
Sereno and Upchurch:
Sauropods are divided into two
major groups: Diplocomorphs and camarasauromorphs; titanosauromorphs are
now recognized as camarasaur derivatives by both Wilson and Sereno, and
by Upchurch.
CAMARASAUROMORPHS (Camarasaurus
+ Titanosauriformes of Wilson and Sereno, Brachiosaria of Upchurch), characters
selected from both references
-
external nares larger than orbits,
greatest diameter equal to 40% length of skull
-
quadrate fossa deep
-
posterior dorsals opisthocoelous
-
forelimb:hindlimb ratio > 75%
-
metacarpal one subequal to metacarpal
IV
TITANOSAUROMORPHS (Somphospondyli
of Wilson and Sereno, Titanosauroidea of Upchurch), characters selected
from both references
-
presacrals fiilled with spongy bone
-
anterior dorsal pleurocoels with
acute margins
-
anterior and mid dorsal spines posteriorly
inclined
-
six sacral vertebrae
-
scapular glenoid medially inclined
-
ischium length/pubis length = 0.90
or less
DIPLODOCOMORPHS (Diplodocoidea of
Wilson and Sereno, Upchurch)
-
dentary with angular "chin"
-
external nares face dorsally, behind
antorbital fenestra
-
premaxilla narrow anteriorly, elongate
posteriorly
-
internarial bar absent
-
lateral temporal fenestrae narrow
-
basipterygoid processes long, project
anteriorly
-
peg teeth, tooth row terminates
in front antorbital fenestra
-
cervical ribs shorter than associated
centra
-
forelimbs secondarily reduced; front/hind
limb ratio 0.67-0.70 (less than 0.75)
-
whiplash tail (30 or more elongate
boconvex posterior caudals)
CAMARASAUROMORPHS
Giraffe sauropods, morphology
closer to that of Plateosaurus than in case of diplodocomorphs;
bush, tree browsers, riparian habitats
Includes Euhelopodidae, Brachiosauridae,
Camarasauridae, example Brachiosaurus
-
large, spoon-shaped teeth, primitively
with denticles
-
nares elevated, medially bridged
-
premaxillary-maxillary shelf on
muzzle
-
pocket in back of quadrate
-
elongated cervical ribs
-
elongated forelimbs, metacarpals
Atlasaurus ? a primitive
brachiosaur-like camarasauromorph from the middle Jurassic of Morocco (Monbaron
et al. 1999. C. R. Acad. Sci. Paris 329: 519-526).
Joberia ? a primitive
camarasaur-like camarasauromorph from the early Cretaceous of Niger (Sereno
et al. 1999. Science 286: 1342-1347)
Also Sauroposeidon, from
the middle Cretaceous of Oklahoma, based on elongated neck vertebrae of
a giant, late brachiosaur (Wedel et al. JVP 20 (1): 109-114).
Euhelopodidae (formerly thought
to be restricted to middle Jurassic-early Cretaceous of Central Asia, now
with a possible record in Argentina ? see Rich et al. 1999)
-
possess a quadrate pocket and very
long cervical ribs
-
lack maxillary shelf
-
possess forked chevrons (diplodocoid)
-
in spite of previous reports, none
are known to possess tail club (Upchurch 1998, p. 80)
DIPLODOCOMORPHS (whip tailed
sauropods)
Most derived sauropods, easy
to identify, vacuum-cleaners, pivoting on hind limbs, fern browsers
Includes Diplodocidae, Nemegtosauridae,
Dicraeosauridae (for details see Upchurch 1995, 1998)
-
nares on top of skull, above orbits,
no internarial bar
-
mandible rectangular anteriorly,
teeth limited to anterior part of jaws
Basal diplodocoid(?): Shunosaurus
(restricted to middle Jurassic of China)
-
very archaic sauropod (cf. skull,
TEXT fig. 16.2 p. 355)
-
maxillary bridge under vomer (personal
observation)
-
teeth lanceolate, closer to peg
than spatulate
-
vertical lamina present on lateral
surface dorsal spines
-
has a tail club (cf. titanosaurids)
DICRAEOSAURIDAE
-
long, subparallel bpt processes
-
supratemporal fenestra face laterally
-
extreme elongation of deeply split
cervical spines
-
sacral spines four times height
of centra
-
Dicraeosaurus lacks pleurocoels
-
short neck of 12 vertebrae
-
short forelimbs
-
whiplash tail
Apatosaurus grew to large
sub-adults in about 10 years (Curry 1999 JVP 19 (4): 654-669); Janenschia
(a late Jurassic putative titanosaur ancestor) became reproductively adult
at ll years ? Sander 2000. Paleobilogy 26(3): 466-488) ? the animal has
recently been redescribed by Bonaparte in Palaeontographica.
Diplodocus, 23 m 16 mt
-
maxillary bridge under vomer
-
elongated basipterygoid processes
on basiphenoid
-
short cervical ribs
-
vertical ridge on dorsal and basal
caudal neural spines
-
very tall sacral spines
-
wing-like basal caudal transverse
processes
-
whip-lash distal caudals
-
biramate chevrons
Seismosaurus (Gilette 1991,
J. Vert. Paleo 11: 417-433)
-
up to 40-50 m long
-
caudal centra longer than in other
diplodocids, spines more erect
-
pubis, ischium more massive than
in other diplodocids
Amphicoelias (Wilson 1996,
J. Vert. Paleo. 16(3): 73A)
-
giant, primitive diplodocoid
Cretaceous diplodocoids:
Dicraeosauridae
Amargasaurus cazui
(L. Salgado and J. Bonaparte 1991. Ameghiniana 28(3-4): 333-346; L. Salgado
and J. Calvo 1992. Ameghiniana 29(4): 337-346); very close to Dicraeosaurus,
Late Neocomian of Argentina, cervical spine from Morocco.
-
fontanelle separating parietals,
bridged in Dicraeosaurus
-
supratemporal fenestrae very narrow
-
broad postorbital-squamosal suture
-
deeply elongated, cleft cervical
spines
-
no pleurocoels
Rebbachisauridae (see Sereno
et al. 1999. Science 286: 1342-1347).
Rayosaurus agriensis,
represented by a superb skeleton described by Calvo and Salgado 1995 Gaia
11: 13-33, Albian-Cenomanian, Argentina (see also Calvo 1999, Natl. Sci.
Mus. Tokyo Monogr. 15: 13-45, where it is referred to Rebbachisaurus
tessonei, and another specimen as Rayosaurus agriensis, Bonaparte
1996. Dinosaurios de America del Sur, Graficas Sagitaro Iturri, Buenos
Aires, 174 p., see p. 108)
-
nares above orbit (diplodocoid,
not camarasauroid)
-
supratemporal, infratemporal fenestrae
nearly closed(slit-like, cf. ornithomimids)
-
quadratojugal greatly expanded in
front of orbit (quasi-diplodocid)
-
pocket on posterior surface of quadrate
(camarasauroid, titanosauroid)
-
short basipterygoid processes (camarasauroid)
-
undivided cervical neural spines
(not diplodocoid)
-
cervical ribs short but slender
(quasi-diplodocoid)
-
pleurocoels on all dorsals
-
anterior caudals amphiplatyan (not
diplodocoid, not titanosauroid)
-
whiplash tail (diplodocoid)
-
distal ends ischia elongated (not
titanosauroid), flat (not diplodocoid)
-
forelimb/hindlimb 0.80 (not diplodocoid)
Antarctosaurus wichmannianus
(Huene 1929. Ann. Mus. La Plata 2(3): 1-196 - see plates 28-29), a primitive
member of the Rebbachisauridae, Sereno et al. 1999.
-
termed diplodocoid by Upchurch 1995,
Campanian-Maastrichtian
-
angled dentary
-
frontal much shorter than in "Rebbachisaurus",
-
STF more closed
-
posterior aspect of braincase more
massive
-
huge orbit
-
short basipterygoid processes, ventrally
directed, widely divergent
Antarctosaurus septentrionalis
braincase (Chatterjee and Rudra 1996, Mem. Queensland Mus. 39: 489-532),
recently named Jainosaurus (Hunt et al. 1994)
-
paroccipital processes narrow, L-shaped
-
long basipterygoid processes
-
looks diplodocoid, although Hunt
et al. 1994 say the type braincase is different from the diplodocoid braincase
of Antarctosaurus (from Argentina)
Nigersaurus dentary with
600 teeth highly derived, expanded into a broad, squared-off muzzle, diplodocoid
position of external nares, scaupula resembles that of Rebbachisaurus
(Sereno et al. 1999)
Nemegtosauridae
Nemegtosaurus, skull,
Mongolia (Upchurch 1995)
-
squamosal excluded from lat temp
fen
-
anterior process qj deflected anteriorly
Quaesitosaurus, isolated
skull from Mongolia, has quadrate pocket
Both genera are referred to Nemegtosauridae
of the Diplodocoidea, Upchurch 1999 JVP 19 (1): 106-125.
TITANOSAUROMORPHS ("bird"
sauropods)
Includes Titanosauridae, Andesauridae
(and Opisthocoelicaudia fide Wilson and Sereno, Upchurch)
-
teeth with small, lenticular crowns
-
"cellular" (not cavernous) pneumatization
of vertebrae
-
cervical neural spines low, unsplit
-
"eye-shaped" presacral pleurocoels
-
six sacral vertebrae
-
caudal neural arches placed anteriorly
on centrum
-
elevated caudal zygapophyses
-
squared, ventrodistally expanded
coracoid
-
robust ulna, hollowed proximally
-
claw absent on first manus digit,
manal phalanges absent
-
ilium everted anteriorly
-
pubis much larger than ischium
-
ischium very short and broad distally,
relative to symphyseal region
-
dermal armour, tail clubs
Argentinosaurus truly titanic
Saltasaurus neck vertebrae
like hadrosaurs
Titanosaurs reviewed by Salgado
et al. (1997, Ameghiniana 34: 3-32, 33-48)
Pleurocoelus caudals andesaurian,
manus lacks claws
[Antarctosaurus, Nemegtosaurus,
Quaesitosaurus all considered titanosaurs; since referred to the Diplodocoidea
by Sereno et al.
1999, Upchurch 1999]
Recent Papers on Titanosaurs:
- Argentinosaurus huinculensis,
J. Bonaparte and R. Coria 1993. Ameghiniana 30(3): 271-282: giant dorsals
with huge zygosphene-zygantra, sacrals and tibia 155 cm long, dorsals 1
m+ high, 50 cm long, huge pleurocoels (Andesauridae with hyp artics; Titanosauridae
without hyp artics)
- Ampelosaurus atacis,
J. Le Loeuff 1995: C.R. Acad. Sci. (Paris) 321, série IIa, p. 693-699.
bone bed occurrence (vertebrae and limb bones, osteoderms) from early Maastrichtian
fluviatile sediments, in a vinyard in the Aude Valley of southern France.
Animal estimated to be 15 m long
Titanosaurus indicus,
Chatterjee and Rudra 1996, Mem. Queensland Mus. 39: 489-532. braincase,
parocc proc broad, recurved, basipterygoid processes short
Titanosaurus colberti,
Jain and Bandyopadhyay 1997, JVP 17: 114-136. articulated/associated skeleton,
no skull parts - a medium-sized animal
-
"inflated" appearance of vertebrae
-
short cervical vertebrae
-
short cervical ribs, fused to centra
-
dorsals with pleurocoels, without
zygosphene-zygantrum
-
max length dorsal = 24 cm
-
all dorsals opisthocoelous
-
6 sacrals
-
titanosaur tail, procoelous, high
zygs and neural arches, neural arches anterior in position
-
short, broad scap-cor
-
recognize 4 sp, based on caudal
verts
Malawisaurus dixei, PhD thesis,
Elizabeth Gomani, rhino sized
-
skull large compared to cervicals
-
anteriorly placed nares (!)
-
huge "pocket" in quadrate
-
dentary with curved symphyseal ramus
-
simple, peg-like teeth
-
single cervical spines
-
long cervical ribs
-
basal caudal with simple, "bipronged"
ala
-
procoelous caudals
-
distal caudals amphiplatyan
Return
to main page Continue
on to lecture 8