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An articulated specimen of the basal titanosaurian (Dinosauria: Sauropoda) Epachthosaurus sciuttoi from the early Late Cretaceous Bajo Barreal Formation of Chubut Province, Argentina

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We describe an articulated specimen of the titanosaurian sauropod Epachthosaurus sciuttoi from the early Late Cretaceous Bajo Barreal Formation of Chubut Province, central Patagonia, Argentina. The skeleton was found in tuffaceous sandstone, with its hindlimbs flexed and its forelimbs widely extended. It is slightly deformed on its left side. The skull, neck, four or five cranial dorsal vertebrae, and several distal caudals are missing. Epachthosaurus is diagnosed by the following autapomorphies: middle and caudal dorsal vertebrae with accessory articular processes extending ventrolaterally from the hyposphene, a strongly developed intraprezygapophyseal lamina, and aliform processes projecting laterally from the dorsal portion of the spinodiapophyseal lamina; hyposphene-hypantrum articulations in caudals 1–14; and a pedal phalangeal formula of 2-2-3-2-0. The genus shares the following apomorphies with various titanosaurians: caudal dorsal vertebrae with ventrally expanded posterior centrodiapophyseal laminae; six sacral vertebrae; an ossified ligament or tendon dorsal to the sacral neural spines; procoelous proximal, middle, and distal caudal centra with well-developed distal articular condyles; semilunar sternal plates with cranioventral ridges; humeri with squared proximolateral margins and proximolateral processes; unossified carpals; strongly reduced manual phalanges; craniolaterally expanded, nearly horizontal iliac preacetabular processes; pubes proximodistally longer than ischia; and transversely expanded ischia. Epachthosaurus is considered the most basal titanosaurian known with procoelous caudal vertebrae.
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107
Journal of Vertebrate Paleontology 24(1):107–120, March 2004
q
2004 by the Society of Vertebrate Paleontology
AN ARTICULATED SPECIMEN OF THE BASAL TITANOSAURIAN (DINOSAURIA:
SAUROPODA) EPACHTHOSAURUS SCIUTTOI FROM THE EARLY LATE CRETACEOUS BAJO
BARREAL FORMATION OF CHUBUT PROVINCE, ARGENTINA
RUBE
´N D. MARTI
´NEZ
1
, OLGA GIME
´NEZ
1
, JORGE RODRI
´GUEZ
1
, MARCELO LUNA
1
, and MATTHEW C. LAMANNA
2
1
Laboratorio de Paleontologia de Vertebrados, Universidad Nacional de la Patagonia ‘‘San Juan Bosco’’, C. C. 360,
(9.000) Comodoro Rivadavia, Argentina, rdfmartinez@yahoo.com;
2
Department of Earth and Environmental Science, University of Pennsylvania, 240 South 33rd Street,
Philadelphia, Pennsylvania 19104–6316, USA
ABSTRACT—We describe an articulated specimen of the titanosaurian sauropod Epachthosaurus sciuttoi from the
early Late Cretaceous Bajo Barreal Formation of Chubut Province, central Patagonia, Argentina. The skeleton was
found in tuffaceous sandstone, with its hindlimbs flexed and its forelimbs widely extended. It is slightly deformed on
its left side. The skull, neck, four or five cranial dorsal vertebrae, and several distal caudals are missing.
Epachthosaurus is diagnosed by the following autapomorphies: middle and caudal dorsal vertebrae with accessory
articular processes extending ventrolaterally from the hyposphene, a strongly developed intraprezygapophyseal lamina,
and aliform processes projecting laterally from the dorsal portion of the spinodiapophyseal lamina; hyposphene-hypan-
trum articulations in caudals 1–14; and a pedal phalangeal formula of 2-2-3-2-0. The genus shares the following
apomorphies with various titanosaurians: caudal dorsal vertebrae with ventrally expanded posterior centrodiapophyseal
laminae; six sacral vertebrae; an ossified ligament or tendon dorsal to the sacral neural spines; procoelous proximal,
middle, and distal caudal centra with well-developed distal articular condyles; semilunar sternal plates withcranioventral
ridges; humeri with squared proximolateral margins and proximolateral processes; unossified carpals; strongly reduced
manual phalanges; craniolaterally expanded, nearly horizontal iliac preacetabular processes; pubes proximodistally
longer than ischia; and transversely expanded ischia. Epachthosaurus is considered the most basal titanosaurian known
with procoelous caudal vertebrae.
RESUMEN.—Se describe un espe´cimen articulado del sauro´podo titanosaurio Epachthosaurus sciuttoi de la Formacio´n
Bajo Barreal, Creta´cico Superior temprano, de la provincia del Chubut, Patagonia central, Argentina. El esqueleto fue
hallado en un estrato de arenisca toba´cea, con sus miembros posteriores flexionados y sus miembros anteriores am-
pliamente extendidos; su costado izquierdo esta´ ligeramente deformado. El cra´neo, cuello, cuatro o cinco ve´rtebras
dorsales anteriores y varias caudales distales han desaparecido.
Epachthosaurus es diagnosticado por las siguientes autapomorfı´as: ve´rtebras dorsales medias y posteriores con pro-
cesos articulares accesorios que se extienden ventrolateralmente desde el hipo´sfeno, presencia de una la´mina interpre-
zigapofiseal fuertemente desarrollada y procesos aliformes que se proyectan lateralmente desde la porcio´n dorsal de la
la´mina espinodiapofiseal; presencia de articulaciones hipo´sfeno-hipantro en las caudales 1–14 y una fo´rmula falangeal
pedal de 2-2-3-2-0. El ge´nero comparte las siguientes apomorfı´as con otros titanosaurios: ve´rtebras dorsales posteriores
con la´minas centrodiapofisiales posteriores ventralmente expandidas; seis ve´rtebras sacras; un ligamento osificado o
tendo´n dorsal a las espinas neurales sacras; centros caudales proximales, medios y distales proce´licos con conos
articulares bien desarrollados; planchas esternales semilunares con crestas a´nteroventrales; hu´meros con ma´rgenes
pro´ximolaterales cuadrados y procesos pro´ximolaterales; carpales no osificados; falanges de la mano fuertemente re-
ducidas; procesos preacetabulares ilı´acos casi horizontales; pubis pro´ximodistalmente ma´s largos que los isquiones e
isquiones transversalmente expandidos. Epachthosaurus es considerado el titanosaurio ma´s basal conocido con ve´rtebras
caudales proce´licas.
INTRODUCTION
Titanosaurian sauropods were among the most abundant and
geographically widespread of Cretaceous herbivorous dino-
saurs. The clade was especially diverse in Europe and land-
masses derived from the supercontinent of Gondwana, partic-
ularly in South America (Bonaparte, 1986). South American
titanosaurians described to date include Aeolosaurus (Powell,
1986, 1987a; Salgado and Coria, 1993a), Andesaurus (Calvo
and Bonaparte, 1991), Antarctosaurus (Huene, 1929; Bonaparte
and Bossi, 1967; Chiappe et al., 2001), Argentinosaurus (Bo-
naparte and Coria, 1993), Argyrosaurus (Lydekker, 1893; Pow-
ell, 1986), Epachthosaurus (Powell, 1990), Gondwanatitan
(Kellner and Azevedo, 1999), Laplatasaurus (Huene, 1929),
Neuquensaurus (Lydekker, 1893; Powell, 1986), Pellegrinisau-
rus (Salgado, 1996), Rocasaurus (Salgado and Azpilicueta,
2000), Saltasaurus (Bonaparte and Powell, 1980; Powell,
1992), possibly Agustinia (Bonaparte, 1999a), and several un-
described Brazilian and Patagonian taxa (e.g., Powell, 1987b;
Calvo et al., 1997, 2001; Martı´nez, 1998; Campos and Kellner,
1999; Gonza´lez-Riga and Calvo, 1999, 2001; Chiappe et al.,
2001; Gime´nez and Apesteguia, 2001; Santucci and Bertini,
2001; Casal et al., in press). Despite this exceptional diversity,
many representatives of Titanosauria are based upon fragmen-
tary, incomplete material. Consequently, evolutionary relation-
ships within the clade remain largely unresolved.
During field research conducted as a part of the project ‘‘Los
vertebrados de la Formacio´n Bajo Barreal, Provincia de Chubut,
Patagonia, Argentina,’’ personnel from the Laboratorio de Pa-
leontologia de Vertebrados of the Universidad Nacional de la
Patagonia ‘‘San Juan Bosco’’ recovered a well preserved, artic-
ulated skeleton of a medium-sized sauropod. Martı´nez et al.
(1988, 1989) briefly described several characters of this speci-
men that indicate that it pertains to Titanosauria, including six
108 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
FIGURE 1. Geographic location and geologic context of the new
specimen of Epachthosaurus sciuttoi (UNPSJB-PV 920). The specimen
was obtained from the Lower Member of the early Late Cretaceous
(middle Cenomanian–?Coniacian) Bajo Barreal Formation, west of
Lago Musters, Estancia ‘‘Ocho Hermanos,’’ Chubut Province, Argen-
tina.
sacral vertebrae, a procoelous first caudal vertebra, and an os-
sified ligament or tendon over the sacral neural spines. They
referred the specimen, one of the most complete titanosaurian
skeletons known, to the genus Epachthosaurus. The goal of the
present work is to preliminarily describe this specimen and
identify the relationships of Epachthosaurus within Titanosau-
ria. One of us (Gime´nez) is preparing a monograph on the anat-
omy and phylogenetic position of Epachthosaurus.
Institutional Abbreviations MACN-CH, Museo Argenti-
no de Ciencias Naturales -Coleccio´n Chubut, Buenos Aires;
MCT, Museu de Cieˆncias da Terra, Departamento Nacional de
Produca˜o Mineral, Rio de Janeiro; MLP, Museo de La Plata,
La Plata, Argentina; PVL, Fundacı´on-Instituto Miguel Lillo,
Tucuma´n, Argentina; SMU, Shuler Museum of Paleontology,
Southern Methodist University, Dallas; UNPSJB-PV, Univer-
sidad Nacional de la Patagonia ‘‘San Juan Bosco’’- Paleover-
tebrados, Comodoro Rivadavia, Argentina.
Anatomical Abbreviations aart, accessory articular pro-
cess; acpl, anterior centroparapophyseal lamina; al, accessory
lamina; alp, aliform process; cc, cnemial crest; cd, condyle;
cpol, centropostzygapophyseal lamina; ct, cotyle; di, diapoph-
ysis; dpc, deltopectoral crest; fhd, femoral head; fic, fibular
condyle; ft, fourth trochanter; hpa, hypantrum; hpo, hyposp-
hene; ilped, iliac peduncle; lt, lateral trochanter; mt, metatarsal;
ns, neural spine; ol, olecranon; ot, ossified tendon; pa, para-
pophysis; pc, pleurocoel; pcdl, posterior centrodiapophyseal
lamina; plb, proximolateral buttress; podl, postzygodiapophy-
seal lamina; posl, postspinal lamina; poz, postzygapophysis;
prap, preacetabular process; prsl, prespinal lamina; prz, prezy-
gapophysis; r, rib; rac, radial condyle; spc, proximolateral pro-
cess; spdl, spinodiapophyseal lamina; spol, spinopostzyga-
pophyseal lamina; sprl, spinoprezygapophyseal lamina; tic, tib-
ial condyle; tp, transverse process; tprl, intraprezygapophyseal
lamina; up, ungual phalanx; I-V, metapodials I-V; C, caudal;
D, dorsal; S, sacral. (We follow Wilson’s [1999a] nomenclature
for vertebral laminae.)
SYSTEMATIC PALEONTOLOGY
SAURISCHIA Seeley, 1887
SAUROPODOMORPHA von Huene, 1932
SAUROPODA Marsh, 1878
TITANOSAURIFORMES Salgado, Coria, and Calvo, 1997
TITANOSAURIA Bonaparte and Coria, 1993
EPACHTHOSAURUS Powell, 1990
EPACHTHOSAURUS SCIUTTOI Powell, 1990
Holotype MACN-CH 1317, an incomplete caudal dorsal
vertebra.
Paratype MACN-CH 18689, a cast, exposed in left lateral
and ventral views, of six articulated caudal dorsal vertebrae, the
partial sacrum, and a fragment of the pubic peduncle of the
right ilium. Due to its occurrence in extremely resistant matrix,
the original fossil has not yet been recovered.
Referred Specimen UNPSJB-PV 920, an articulated skel-
eton lacking the skull, neck, four or five cranial dorsal and
extreme distal caudal vertebrae.
Locality Estancia ‘‘Ocho Hermanos,’’ Sierra de San Ber-
nardo, west of Lago Musters, south-central Chubut Province,
central Patagonia, Argentina (Fig. 1).
Horizon and Age Upper portion of the Lower Member of
the Bajo Barreal Formation (Upper Cretaceous: late Cenoma-
nian-early Turonian [Archangelsky et al., 1994; Bridge et al.,
2000; Lamanna et al., 2002]) (Fig. 1). The ‘‘Ocho Hermanos’’
tetrapod assemblage, which includes the basal chelid turtles Bo-
napartemys and Prochelidella (Broin and Fuente, 2001), the
ceratosauroid theropod Xenotarsosaurus (Martı´nez et al., 1986),
a carnotaurine abelisaurid (Martı´nez et al., 1993; Lamanna et
al., 2002), the basal titanosaurian Epachthosaurus (Powell,
1990; this paper), possibly other titanosaurs, and sauropods of
unresolved affinity (Powell et al., 1989), provides further evi-
dence in support of an early Late Cretaceous age for outcrops
of the Bajo Barreal Formation on the Estancia ‘‘Ocho Herma-
nos.’’
Taphonomy Based on the sedimentology and taphonomic
characteristics of the Bajo Barreal Formation as exposed at the
Estancia ‘‘Ocho Hermanos,’’ Rodrı´guez (1993) postulated epi-
sodic deposition of large quantities of sediment, resulting in the
rapid burial of animal remains. The degree of articulation and
body position of UNPSJB-PV 920 are consistent with this hy-
pothesis (Fig. 2). When buried, the sauropod carcass was rest-
ing on its ventral surface, with the forelimbs widely extended,
both hindlimbs flexed, and the tail extended distally and curved
toward the right (Fig. 2A). It is possible that the skull and
cervical series were preserved, but have since been destroyed
by erosion, as several dorsal vertebrae and the pectoral girdle
were damaged by weathering. UNPSJB-PV 920 was probably
not transported prior to burial (Rodrı´guez, 1993).
Diagnosis Medium-sized titanosaurian sauropod diagnosed
by the following autapomorphies: middle and caudal dorsal ver-
tebrae possessing accessory articular processes extending ven-
109MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
FIGURE 2. Skeletal disposition of Epachthosaurus sciuttoi (UNPSJB-
PV920). A, dorsal view. B, cranial view of pelvis and hindlimbs. C,
lateral view of right ilium and hindlimb. Abbreviations listed in text.
Scale bar equals 1 m in A; 50 cm in B and C.
TABLE 1. Vertebral centrum lengths (mm) of UNPSJB-PV 920 (Epachthosaurus sciuttoi); *
5
element incomplete; †, vertebra without distal
articular condyle.
Dorsal vertebrae
Centrum length
Sacral vertebrae
Centrum length
Caudal vertebrae
Centrum length
Caudal vertebrae
5
300
1
150
1
130†
9
6
*2
140
2
115
10
7
*
3
*
3
125
11
8
*
4
115
4
110
12
9
240
5
125
5
*
13
10
180
6
165
6
107†
14
7
172
15
8
177
16
Centrum length
Caudal vertebrae
Centrum length
Caudal vertebrae
Centrum length
178
17
181
25
126†
162
18
175
26
138
115†
19
180
27
130
117†
20
*
28
132
270
21
135†
29
130
175
22
160
130
23
144
177
24
117†
trolaterally from the hyposphene, a strongly developed intra-
prezygapophyseal lamina, and aliform processes projecting lat-
erally from the dorsal portion of the spinodiapophyseal lamina;
hyposphene-hypantrum articulations in caudals 1–14; and a
pedal phalangeal formula of 2-2-3-2-0.
Comments Powell (1990) diagnosed the genus Epachtho-
saurus on the basis of several characters possessed by the ho-
lotype caudal dorsal vertebra (MACN-CH 1317); however, all
were subsequently shown to be ambiguous or plesiomorphic
(Salgado and Martinez, 1993; Salgado, 1996; Sanz et al., 1999).
Powell (1990) also described the occurrence of an ‘‘interprezy-
gapophyseal shelf’’ in the holotype caudal dorsal of Epacht-
hosaurus (Salgado, 1996). Salgado (1996) maintained the va-
lidity of Epachthosaurus on the basis of this character, which
he regarded as an autapomorphy of the taxon.
Powell (1990) designated MACN-CH 18689 as the ‘‘para-
plastotype’’ of Epachthosaurus, based upon its possession of
the characters listed in his diagnosis of the genus. However,
because none of these features are considered diagnostic (see
above), and MACN-CH 18689 does not appear to possess an
‘‘interprezygapophyseal shelf’’ in its caudal dorsal vertebrae,
Salgado (1996) concluded that its inclusion within Epachtho-
saurus was not justified. Bonaparte and Coria (1993) and Sal-
gado (1996) further questioned the systematic position of
MACN-CH 18689, citing the occurrence of accessory articular
processes extending ventrolaterally from the hyposphene on the
caudal dorsal vertebrae of the specimen that are not present in
the holotype of Epachthosaurus. Based upon this character, they
argued that MACN-CH 18689 pertains to a distinct genus with
affinity to the giant titanosaur Argentinosaurus, which also pos-
sesses dorsal vertebrae with accessory articulations. However,
Salgado and Martı´nez (1993) and Sanz et al. (1999) disputed
the occurrence of the hyposphene in Argentinosaurus, identi-
fying the accessory intervertebral articulations present in the
taxon as modified centropostzygapophyseal laminae. Hence, the
accessory articulations of Argentinosaurus and MACN-CH
18689 are probably not homologous, and the affinities of the
latter remain in doubt.
The articulated skeleton described here (UNPSJB-PV 920)
resolves several taxonomic issues concerning Epachthosaurus.
Based upon its possession of a previously determined autapo-
morphy of the genus, a strongly developed intraprezygapophy-
seal lamina (
5
‘‘interprezygapophyseal shelf’’) on its middle
and caudal dorsal vertebrae, we refer UNPSJB-PV 920 to
Epachthosaurus. Furthermore, UNPSJB-PV 920 possesses ac-
cessory articular processes extending ventrolaterally from the
hyposphene on its caudal dorsals, as in MACN-CH 18689. This
character constitutes a synapomorphy of MACN-CH 18689 and
UNPSJB-PV 920, and therefore justifies the original assessment
of the former as the ‘‘paraplastotype’’ of Epachthosaurus (Pow-
ell, 1990). In summary, three titanosaurian specimens from the
Lower Member of the Bajo Barreal Formation exposed on the
Estancia ‘‘Ocho Hermanos’’ pertain to Epachthosaurus, and by
monotypy, E. sciuttoi (MACN-CH 1317 and 18689, and
UNPSJB-PV 920). We redesignate the ‘‘paraplastotype’’
MACN-CH 18689 as the paratype of the species, following the
International Code of Zoological Nomenclature (Fourth Edition,
Recommendation 73D).
DESCRIPTION
Axial Skeleton (Table 1)
Dorsal Vertebrae All known dorsal vertebrae in Epacht-
hosaurus are opisthocoelous. For positional assignments, we
assume the presence of ten dorsals in Epachthosaurus,ashy-
pothesized by Huene (1929) and shown in an articulated spec-
imen of an unnamed Brazilian titanosaurian (MCT 1488-R;
Powell, 1986, 1987b; Campos and Kellner, 1999). We recog-
nize, however, that our assignments may be slightly inaccurate,
as Borsuk-Bialynicka (1977) and Curry Rogers and Forster
(2001) described eleven dorsals in the titanosaurians Opistho-
coelicaudia and Rapetosaurus.
The fifth dorsal vertebra (Fig. 3A) is the cranialmost pre-
served. Although damaged by erosion, a large portion of the
centrum is present. The cranial region and portions of the neural
arch are missing. The centrum is dorsoventrally compressed
with well-developed pleurocoels extending medially nearly to
110 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
FIGURE 3. Middle dorsal vertebrae of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, fifth dorsal, caudal view; B, sixth dorsal, left lateral
view; C, sixth dorsal, cranial view. Abbreviations listed in text. Scale bars equal 10 cm.
the sagittal midline of the vertebra. The centrum displays a
deeply concave caudal cotyle. On the neural arch, ventral to
the postzygapophyses, laminae extend laterally and slightly
ventrally from the hyposphene, producing accessory interver-
tebral articular surfaces.
The sixth dorsal (Fig. 3B, C) is one of the most complete,
and has a dorsoventrally compressed, strongly opisthocoelous
centrum resembling that of the fifth dorsal. The caudally acu-
minate pleurocoels deepen towards the cranial margin of the
centrum. A weak right parapophysis and well-developed di-
apophyses are preserved. Laterally, an anterior centropara-
pophyseal lamina and two laminae of uncertain homology de-
limit a subtriangular cavity on the ventral portion of the neural
arch, caudoventral to the parapophysis. A strong, slightly ven-
trally widened posterior centrodiapophyseal lamina is present.
An accessory, caudodorsally-oriented lamina arises from the
approximate midpoint of the posterior centrodiapophyseal lam-
ina and widens dorsally before terminating between the postzy-
gapophysis and diapophysis. This lamina is distinct from the
centropostzygapophyseal lamina, which is also present (Wilson,
1999a).
Wilson (1999a) discussed the occurrence of an intraprezy-
gapophyseal lamina in sauropod cervicals and cranial dorsals,
but considered it absent caudal to dorsals 4–5. Nevertheless, a
strongly developed horizontal lamina joins the prezygapophyses
of the sixth dorsal in UNPSJB-PV 920. Curry Rogers and For-
ster (2001) listed a possibly equivalent character, a ‘‘median
interprezygapophyseal lamina’’ on the dorsal vertebrae, as an
autapomorphy of the Malagasy Late Cretaceous titanosaurian
Rapetosaurus. Similarly, Gonza´lez-Riga and Calvo (2001) men-
tioned a prezygapophyseal ‘‘platform’’ on the middle caudals
of an unnamed Upper Cretaceous titanosaurian from Neuque´n
Province in northern Patagonia. However, we maintain the dis-
tinction of these characters from that present in Epachthosau-
rus, pending further description of the Malagasy and northern
Patagonian genera. We regard a strongly developed intraprezy-
gapophyseal lamina (an ‘‘interprezygapophyseal shelf’’) on the
caudal dorsal vertebrae as an autapomorphy of Epachthosaurus
(Powell, 1990; Salgado, 1996).
Accessory hyposphenal processes on the sixth dorsal are sim-
ilar to those on the fifth. The neural spine consists of prespinal,
postspinal, and spinodiapophyseal laminae and is inclined cau-
dodorsally. The well-developed prespinal lamina bifurcates
ventrally into spinoprezygapophyseal laminae. On the right
side, at midlength, the prespinal lamina intersects a small, ro-
bust lamina that extends approximately 50 mm ventrolaterally
and delimits a pronounced cavity cranially. Subtriangular flat-
tened expansions related to the postzygapophyses, here termed
aliform processes, project laterally from the dorsal portions of
the spinodiapophyseal laminae. These structures differ from the
‘‘triangular processes’’ identified by Upchurch (1995, 1998) on
the dorsal neural spines of several macronarians, and represent
another autapomorphy of Epachthosaurus. The postspinal lam-
ina is weakly developed.
The centrum of the seventh dorsal is crushed and fractured,
revealing cancellous internal tissue. The neural spine is more
vertically inclined and craniocaudally thicker than in the fifth
and sixth dorsals. The prespinal lamina is well-developed, and
the cavity ventrolateral to it is deeper than in the previous ver-
tebra and further delimited by a secondary ramus of the spi-
nodiapophyseal lamina.
The eighth dorsal is heavily damaged by erosion. The neural
spine is completely vertical and the prespinal lamina is more
robust than in more cranial vertebrae.
The ninth dorsal (Fig. 4A, B, and C) is firmly articulated
with the tenth. The centrum is slightly dorsoventrally com-
pressed and its shape is nearly cylindrical. The neural spine is
poorly preserved. Although the prespinal lamina is missing, a
wide basal bifurcation is present, forming spinoprezygapophy-
seal laminae. A depression occurs between these laminae and
the nearly vertical spinodiapophyseal lamina.
Because the centrum of the tenth dorsal (Fig. 4) is affixed to
the ninth, many details of the cranial surface cannot be ob-
served. However, the caudal articular surface is perfectly pre-
served. The hyposphene and accessory articular processes are
well-developed. The neural arch possesses a weakly-developed
postspinal lamina and robust spinopostzygapophyseal laminae
that are separated by a wide depression. The distal end of the
neural spine is not preserved.
Dorsal Ribs Ten pairs of dorsal ribs were found, fractured,
eroded, and displaced. The cranialmost ribs are triangular in
cross-section proximally, becoming flat and wide distally. The
caudal dorsal ribs are cylindrical in cross-section. Internally,
they seem to be composed of a thin layer of spongy tissue.
Generally, the ribs seem more slender than those of most other
sauropods.
Sacrum The sacrum (Figs. 5, 11A) includes six vertebrae.
The cranial (of the 1st sacral) and caudal (of the 6th) articular
condyles are convex; however, the latter is less so than the
former. A subrectangular ossified ligament or tendon approxi-
111MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
FIGURE 4. Ninth and tenth dorsal vertebrae of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, left lateral view; B, dorsal view; C, ventral view;
D, caudal view. Abbreviations listed in text. Scale bars equal 10 cm.
mately 200 mm in transverse width, 800 mm in craniocaudal
length, and 50 mm in dorsoventral depth connects the dorsal
surfaces of all sacral neural spines. Longitudinal striations are
present along the structure. A similar feature was reported in
the specimen that the paratype of Epachthosaurus (MACN-CH
18689) was based upon (Powell, 1990; Bonaparte, 1996), and
in a titanosaurian from Peiro´polis, Brazil (MCT 1489-R, Pow-
ell, 1987b; Campos and Kellner, 1999). Although this structure
is only preserved dorsal to sacrals 2–4 in the latter, it presum-
ably connected all six (Powell, 1987b; Campos and Kellner,
1999).
The first sacral vertebra is similar in morphology to the cau-
dal dorsals. The centrum is dorsoventrally compressed, but not
as much as in the dorsal centra. In contrast with some titano-
saurians (e.g., Gondwanatitan, Kellner and Campos, 1999;
Opisthocoelicaudia, Borsuk-Bialynicka, 1977; ‘‘Titanosaurus’’
colberti, Jain and Bandyopadhyay, 1997), well-developed pleu-
rocoels are present on the first sacral. Cranially, the hypantrum
is strongly developed. The damaged parapophyses are located
directly ventral to the incomplete diapophyses. A section of the
basally bifurcate prespinal lamina is preserved. The diapophy-
ses are fused with the laterally expanded sacral ribs. Ventrally,
the sutures between the remaining sacral centra are well-de-
fined, as in MACN-CH 18689. Together with the ilium, the
caudalmost four sacral ribs contribute to the formation of the
acetabulum.
Caudal Vertebrae The 29 preserved caudal vertebrae of
UNPSJB-PV 920 are all procoelous. Hyposphene-hypantrum
articulations occur in the first fourteen. These structures are
morphologically distinct from the ‘‘hyposphenal ridges’’ re-
ported in the caudal vertebrae of multiple sauropods by Up-
church (1998). Nevertheless, caudal hyposphene-hypantrum ar-
ticulations are not unique to Epachthosaurus, as similar artic-
ulations occur in proximal and middle caudal vertebrae of an
unnamed non-titanosaurian titanosauriform from the Early Cre-
taceous Paluxy Formation of Texas (SMU 61732; Langston,
112 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
FIGURE 5. Sacrum and ilia of Epachthosaurus sciuttoi (UNPSJB-PV
920) in dorsal view. Abbreviations listed in text. Scale bar equals 20
cm.
FIGURE 6. First and second caudal vertebrae of Epachthosaurus
sciuttoi (UNPSJB-PV 920). A, right lateral view; B, proximal view; C,
dorsal view. Abbreviations listed in text. Scale bars equal 10 cm.
1974; Gomani et al., 1999; Tidwell et al., 1999; Wedel et al.,
2000). Caudal hyposphene-hypantrum articulations may thus be
plesiomorphic for Epachthosaurus. However, such articulations
are not reported in the titanosaurian Andesaurus (Calvo and
Bonaparte, 1991), which probably occupies a more basal po-
sition than Epachthosaurus (Salgado and Martı´nez, 1993; Sal-
gado et al., 1997). Consequently, we consider caudal hyposp-
hene-hypantrum articulations as an autapomorphy of the latter.
We restrict our description to three general regions of the tail
that illustrate the morphological changes that occur through the
series. The somewhat deformed first caudal (Fig. 6) has a robust
centrum with a gently concave and subcircular proximal cotyle.
The centrum is also concave ventrally and laterally. The trans-
verse processes emerge from the dorsal portion of the centrum
at approximate right angles. Planar expansions on the distal
surfaces of the transverse processes may articulate with the
transverse processes of the second caudal, but this is impossible
to determine due to damage to the latter. The neural arch is
situated over the proximal half of the centrum. The neural spine
is robust and distally inclined at an angle of 50
8
from the hor-
izontal. The prespinal lamina is stout. The prezygapophyses
arise from a pair of spinoprezygapophyseal laminae that origi-
nate at the base of the neural spine. The diameter of the neural
canal is very small. The distal margin of the postspinal lamina
is poorly developed and is flanked by two strong spinopostzy-
gapophyseal laminae. The postzygapophyses are slender with
distolaterally oriented articular faces.
The centrum of the second caudal (Fig. 6A, C) remains ar-
ticulated with, and is similar to, that of the first. The articular
condyle protrudes distally nearly as far as the remainder of the
centrum is long. The transverse processes are not preserved.
The neural spine is shorter and more distally inclined than that
of the first caudal. The third caudal vertebra, damaged by ero-
sion and missing the neural arch, has a deep, concave proximal
cotyle.
The seventh caudal (Fig. 7) has a procoelous centrum with
a strongly convex distal articular condyle. The apex of the con-
dyle occurs in the dorsal half of the centrum. The stout trans-
verse processes are deflected distally. The prezygapophyses are
powerfully developed and extend far past the proximal margin
of the centrum. Hyposphene-hypantrum articular facets are
clearly present. The neural spine is proximodistally elongate
and generally transversely compressed. Nevertheless, it is
slightly transversely expanded dorsally.
Compared with the proximal caudal vertebrae, the tenth (Fig.
8A) and eleventh caudals have proportionally poorly developed
distal articular condyles. The centra are proximally concave and
possess a well-delineated longitudinal groove ventrally. The
neural arches are based within the proximal halves of the centra,
113MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
FIGURE 7. Seventh caudal vertebra of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, proximal view; B, distal view; C, right lateral view; D,
ventral view. Scale bars equal 10 cm.
but do not reach their margins, and bear short, horizontal prezy-
gapophyses with medially facing articular surfaces. The verti-
cal, plate-like neural spines are proximodistally elongate. The
transverse processes are reduced to ridges located on the dorsal
portions of the centra. The postzygapophyses are weak.
The most distal caudal vertebrae, the 27th, 28th (Fig. 8B),
and 29th, are approximately the same length as the proximal
caudals. The centra are cylindrical and retain traces of longi-
tudinal ventral sulci. The neural arches are placed on the prox-
imal halves of the centra, slightly distal to their margins. The
postzygapophyses are fused ventral to vestigial neural spines.
Haemal Arches 19 articulated haemal arches are pre-
served. The haemal canal is open dorsally and the oval articular
surfaces are directed distally and slightly medially. Haema-
pophysis two has a transversely widened, laminar spine with a
thick, round distal border and a sharp proximal margin. Haemal
arch 13 has an enlarged haemal canal and a spine less expanded
ventrally. Haemapophysis 16 has a wide canal with a reduced
spine.
Appendicular Skeleton
Pectoral Girdle The scapulae and coracoids are poorly
preserved. However, the sternal plates, although damaged, ex-
hibit the semilunar contour typical of titanosaurians. The sternal
plates have thick, rounded, and concave lateral margins. Ventral
crests that articulate with the coracoids are present craniolate-
rally.
Forelimb (Table 2) The humerus (Fig. 9A) is of typical
sauropod structure with a flat, craniocaudally compressed shaft.
The epiphyses are transversely expanded. The proximal and lat-
eral margins of the humerus meet at an approximate right angle.
As in several titanosaurs, a process is present proximolaterally
that possibly marks the insertion of the supracoracoideus mus-
cle (Borsuk-Bialynicka, 1977; Gime´nez, 1992; Upchurch,
1998). The deltopectoral crest is strongly developed, and oc-
cupies much of the proximal half of the humeral craniolateral
margin. In lateral view, the crest is convex, and its distal portion
is directed craniomedially. The edge of the crest is rugose,
marking the insertion of the pectoral muscle. The humeral head
is round, craniocaudally convex, and inclined caudally. The me-
dial projection is subtriangular and not clearly separated from
the head. The radial condyle is more strongly developed and
rounded than the ulnar.
The ulna (Fig. 9B, C) is more robust than the radius. Its
proximal end is triradiate with a prominent olecranon process,
and has three well-defined crests delimiting concave surfaces
114 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
FIGURE 8. Middle and distal caudal vertebrae of Epachthosaurus
sciuttoi (UNPSJB-PV 920) in left lateral view. A, tenth; B, 28th. Ab-
breviations listed in text. Scale bar equals 10 cm in A; 5 cm in B.
TABLE 2. Measurements (mm) of humerus, ulna, and radius of UNPSJB-PV 920 (Epachthosaurus sciuttoi).
Right humerus Left humerus Right ulna Left ulna Right radius Left radius
Proximodistal length
Proximal transverse width
Distal transverse width
Transverse width, shaft
Shaft circumference
885
300
290
165
420
935
320
290
160
425
597
255
140
105
340
613
250
145
105
335
530
165
190
80
240
550
165
160
80
240
that extend the length of the element. The radial articular sur-
face is wide, well defined throughout its proximal third, and
projects cranially toward its distal end. The flat distal articular
surface is semicircular in outline.
The radius (Fig. 9D) is slightly sigmoid. The proximal region
bears a pointed tuberosity. The distal portion of the ulnar artic-
ular surface possesses a smooth longitudinal depression, delim-
ited by two ridges. The distal ridge is the more prominent of
the two and contacts the medial protuberance of the cranial face
of the ulna. The distal articular surface is elliptical with the
long axis of the ellipse oriented mediolaterally.
The carpals are not preserved in either forelimb of UNPSJB-
PV 920, and were probably unossified. There are five metacar-
pals (Fig. 10) in each manus. All were found articulated and in
excellent condition, especially those of the right manus. When
articulated, they intersect at their distal ends, forming a verti-
cally oriented cylinder. This configuration allowed them to ef-
ficiently support the great weight they carried.
The proximal articular surfaces of the metacarpals (Table 3)
are rugose. They are subtriangular in cross-section, with the
bases of the triangles directed externally. The metacarpals be-
come subrectangular in cross-section distally. Metacarpal I is
the most robust of the series, and has a straight shaft. Metacar-
pal II is the same length as the first, but has a slightly sigmoid
shaft. The third, fourth, and fifth metacarpals show a progres-
sive decrease in length. The shaft of the fourth metacarpal is
compressed at both ends, while metacarpal V is nearly straight.
With the exception of a vestigial element fused to the distal
surface of metacarpal IV, no phalanges are present. A nearly
identical condition is present in the Mongolian titanosaurian
Opisthocoelicaudia (Borsuk-Bialynicka, 1977). This corrobo-
rates the hypothesis that the manual phalanges of titanosaurian
sauropods were strongly reduced, unossified, or absent (Gime´-
nez, 1992; Salgado et al., 1997).
Pelvic Girdle (Table 4) The pelvic elements were found
slightly displaced, but articulated. The ilium (Figs. 2, 5, 11A)
is low, elongate, and internally composed of cancellous tissue.
The preacetabular process is damaged, relatively craniocaudally
short, and expanded craniolaterally. The pubic peduncle is cra-
nially inclined and transversely elongate. The ischiadic pedun-
cle is only slightly developed, demarked by a smooth convexity
ventral to the postacetabular process.
The pubis (Fig. 11B) is heavily damaged caudally, but ap-
pears to be a long, flattened element with expanded proximal
and distal ends. The lateral margin of the pubis is concave ven-
trally. On the lateral surface, at the approximate proximodistal
midpoint of the element, there is a process for muscular inser-
tion. In both pubes, the middle region of the shaft and the me-
dial process that articulates with the corresponding pubis are
deformed. The pubes are strongly thickened distally.
The ischium (Fig. 11C), although badly damaged, appears
flattened and shorter than the pubis. It is expanded proximally
at the iliac peduncle. The left ischium preserves the pubic and
iliac articular surfaces. In dorsomedial view, the ischium dis-
plays a pronounced lateral thickness that thins distally and me-
dially.
Hindlimb (Table 5) The left femur is deformed proximal-
ly. For this reason, our description is based principally on the
right (Fig. 12A). The right femur is a long and straight bone,
damaged in the region of the femoral head. The femoral head
extends further dorsally than the greater trochanter and does not
project strongly medially. A proximolateral buttress is present,
as in most titanosauriforms. Caudomedially, the fourth trochan-
ter emerges as a well-developed ridge approximately halfway
down the shaft. Distally, the fibular condyle is divided into me-
dial and lateral portions by a marked subvertical sulcus, and
separated from the strongly developed tibial condyle by a poor-
ly defined depression. The tibial condyle articulates with a me-
dian concavity on the proximal surface of the tibia.
The tibia (Fig. 12B) is slender and more expanded proxi-
mally than distally. The most elevated region of the tibia is
laterally positioned and articulates with the intercondylar de-
pression of the femur, between the tibial and fibular condyles.
The transversely narrow, proximodistally lengthened, and cra-
niocaudally deep cnemial crest is craniolaterally directed and
delineated laterally by a cavity. The proximal tibial surface is
rugose but relatively flat, whereas the distal surface possesses
a strong, ventrally directed process for articulation with the as-
tragalus.
The fibula (Fig. 12C) is slender with a slightly craniocaudally
expanded proximal end. It is ovoid in cross-section distally. The
lateral surface of the fibula is convex while its medial surface
is flat. Its most notable character is the presence of a prominent
115MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
FIGURE 9. Right forelimb elements of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, humerus, cranial view; B, ulna, cranial view; C, ulna,
lateral view; D, radius, craniolateral view. Abbreviations listed in text. Scale bars equal 20 cm.
FIGURE 10. Right metacarpus of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, cranial view; B, proximal view. Scale bar equals 10 cm in A;
5cminB.
116 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
TABLE 3. Proximodistal lengths (mm) of metacarpals of UNPSJB-
PV 920 (Epachthosaurus sciuttoi).
Right I II III IV V
Length 305 303 295 275 268
Left I II III IV V
Length 288 297 297 284 270
TABLE 4. Lengths (mm) of right ilium, pubis, and ischium of
UNPSJB-PV 920 (Epachthosaurus sciuttoi); *
5
element incomplete.
Ilium Pubis Ischium
Length 770 670 440*
FIGURE 11. Pelvis and reconstructed right pubis and ischium of
Epachthosaurus sciuttoi (UNPSJB-PV 920). A, sacrum and ilia, cranial
view; B, pubis, dorsal view; C, ischium, ventral view. Scale bars equal
20 cm.
dual tuberosity at midshaft on its lateral surface. This structure,
the lateral trochanter, is slightly obliquely directed with respect
to the long axis of the shaft.
Articulated astragali (Fig. 12D) were recovered for both
hindlimbs. Each is subtriangular, robust, and has a proximodis-
tally elevated and thick lateral portion that gradually decreases
in height and thickness medially. The ascending process artic-
ulates with a depression in the craniodistal portion of the tibia.
The proximal portion of the ascending process is wide and pos-
sesses a facet that articulates with the distomedial margin of
the fibula. The craniodistal face is elliptical and slightly medio-
laterally convex. This grades into a rounded surface that artic-
ulates with the proximal ends of metatarsals I, II, and III. The
entire astragalar surface displays rugosities typical of cartilag-
inous insertion. There is no ossified calcaneum in Epachtho-
saurus.
The pedes are complete and articulated in both hindlimbs of
UNPSJB-PV920 (Table 6; Fig. 13). Epachthosaurus is thus the
first South American titanosaurian for which pedal morphology
is completely known. The foot is of graviportal structure and
retains five radially arranged digits. The foot is wide, with short
metatarsals with expanded proximal ends. The metatarsopha-
langeal articular surfaces are well-developed, and suggest con-
siderable mobility at the majority of the joints. Proximally, the
five metatarsals are closely abutted, forming a wide articular
surface for the astragalus. The first metatarsal is the most ro-
bust. Metatarsals I–IV gradually increase in length sequentially,
but metatarsal V is slightly shorter than metatarsal IV.
A possible autapomorphy of Epachthosaurus is the reduction
of its pedal phalangeal formula to 2-2-3-2-0. The first three
digits possess claws. Those of digits I and II are nearly iden-
tical, but that of digit III is smaller. The articular surfaces of
the ungual phalanges are inclined, suggesting mobility in hor-
izontal and vertical planes, as in an unnamed titanosauriform
from the Early Cretaceous of Texas (Gallup, 1989). A kerati-
nous sheath probably covered the claws in life.
Dermal Skeleton No osteoderms were recovered with
UNPSJB-PV 920, and we consequently assume that Epacht-
hosaurus was unarmored.
Weight of Epachthosaurus T. Galarza and J. Gallegos
(pers. comm., 1998) attempted to determine the live weight of
UNPSJB-PV 920. They made a scale model of this individual
of Epachthosaurus and followed the method outlined by Al-
exander (1989), obtaining a weight estimate of 11,290 kg.
COMPARISONS
We compared UNPSJB-PV 920 to several Cretaceous South
American titanosaurian genera, including the plesiomorphic An-
desaurus and the more derived Argentinosaurus,Argyrosaurus,
and Saltasaurus. Epachthosaurus was also compared to the
Late Cretaceous Mongolian sauropod Opisthocoelicaudia,
which has been recently recognized as a titanosaurian (Gime´-
nez, 1992; Salgado and Coria, 1993b; Upchurch, 1995, 1998;
Salgado et al., 1997; Calvo et al., 1998; Wilson, 1999b).
Andesaurus delgadoi (Calvo and Bonaparte, 1991) The
caudal dorsal centra of Andesaurus are weakly opisthocoelous
and their neural arches and spines are more dorsally elevated
than in Epachthosaurus.Andesaurus has hyposphene-hypan-
trum articulations in its caudal dorsal vertebrae, as in Epacht-
hosaurus, but the hyposphene of the latter is apomorphically
developed, with accessory articular processes extending ventro-
laterally. The taxa share several titanosaurian plesiomorphies
such as dorsal neural spines with well-developed prespinal lam-
inae that bifurcate ventrally into spinoprezygapophyseal lami-
nae, and reduced postspinal laminae. Unlike Epachthosaurus,
Andesaurus has amphiplatyan caudal vertebrae. The retention
of this plesiomorphic character, among others, relegates Ande-
saurus to a basal position within Titanosauria (Salgado and
Martı´nez, 1993; Salgado et al., 1997; Upchurch, 1998).
Argentinosaurus huinculensis (Bonaparte and Coria,
1993) Although the extremely large titanosaurian Argentino-
saurus possesses accessory intervertebral articulations in its
dorsal column, they are anatomically distinct from those of
Epachthosaurus (Salgado and Martı´nez, 1993; Sanz et al.,
1999). Moreover, Argentinosaurus possesses reduced, non-bi-
furcate prespinal laminae, implying that this taxon may be more
highly derived than Epachthosaurus (Salgado et al., 1997).
Contrary to the condition in Epachthosaurus, sutures between
the fused sacral vertebrae of Argentinosaurus are indistinct in
ventral view (Powell, 1990; Bonaparte and Coria, 1993), al-
though this could be of ontogenetic rather than phylogenetic
significance. The fibula of Argentinosaurus, originally consid-
ered a tibia, (Wilson and Sereno, 1998, contra Bonaparte and
Coria, 1993) differs from that of Epachthosaurus because it
lacks a dual tuberosity in its proximal half.
Argyrosaurus superbus (Lydekker, 1893; Bonaparte and
Gasparini, 1979; Powell, 1986) Argyrosaurus is a large ti-
tanosaurian originally based upon a left forelimb, MLP 77-V-
117MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
TABLE 5. Measurements (mm) of femur, tibia, and fibula of UNPSJB-PV 920 (Epachthosaurus sciuttoi); *
5
element incomplete.
Right femur Right tibia Left tibia* Right fibula Left fibula
Proximodistal length
Proximal transverse width
Distal transverse width
Shaft transverse width
Shaft circumference
1095
340
310
230
550
700
210
185
130
335
662
730
150
110
80
220
725
155
110
80
215
FIGURE 12. Right hindlimb elements of Epachthosaurus sciuttoi
(UNPSJB-PV 920). A, femur, caudal view; B, tibia, craniolateral view;
C, fibula, lateral view; D, astragalus, cranial view. Scale bar equals 20
cm in A-C; 5 cm in D.
TABLE 6. Proximodistal lengths (mm) of right metatarsals of
UNPSJB-PV 920 (Epachthosaurus sciuttoi).
I II III IV V
Length 125 153 177 185 153
29-1, possibly from the Bajo Barreal Formation (Lydekker,
1893; Huene, 1929; Bonaparte, 1996). PVL 4628, a titanosau-
rian partial skeleton, also probably from the Bajo Barreal For-
mation, has been tentatively referred to Argyrosaurus (Powell,
1986; Bonaparte, 1996). As in Epachthosaurus, the middle dor-
sal vertebra of PVL 4628 possesses a lamina that arises from
the ventral region of the posterior centrodiapophyseal lamina
and terminates between the postzygapophysis and diapophysis
(Bonaparte, 1999b). Nevertheless, the dorsal pleurocoels of
PVL 4628 are less extensive than in Epachthosaurus, and its
neural arches and spines are dorsally elevated. Moreover, the
preserved caudal dorsal of PVL 4628 is only weakly opistho-
coelous. Appendicular elements of MLP 77-V-29-1 and PVL
4628 are similar to those of Epachthosaurus. Further study of
MLP 77-V-29-1 and PVL 4628 is needed to clarify the status
of the genus Argyrosaurus, and its possible affinity to Epacht-
hosaurus.
Saltasaurus loricatus (Bonaparte and Powell, 1980; Pow-
ell, 1992) The dorsal neural arches of Saltasaurus are dorsally
elevated, transversely narrow, and have dorsally deflected di-
apophyses, characters absent in Epachthosaurus. The dorsal
vertebrae of Saltasaurus also differ from those of Epachtho-
saurus in their possession of reduced, undivided prespinal lam-
inae and weakly developed pleurocoels, and their lack of
hyposphene-hypantrum articulations. The caudal vertebrae of
Saltasaurus have proximally-placed neural arches, similar to
the condition in Epachthosaurus. Appendicular elements of Sal-
tasaurus are similar to those of UNPSJB-PV 920.
Opisthocoelicaudia skarzynskii (Borsuk-Bialynika, 1977)
The Mongolian titanosaur Opisthocoelicaudia shares many an-
atomical characters with Epachthosaurus, including opisthocoe-
lous dorsal vertebrae with caudally acuminate pleurocoels, low
neural arches, and centroparapophyseal laminae; six sacral ver-
tebrae; laterally concave sternal plates; metacarpals with nearly
flat articular surfaces; metacarpals I and II subequal in length
with symmetrical distal ends; one rudimentary manual phalanx;
and a reduced pedal phalangeal formula. All of these characters
appear to be synapomorphies of Titanosauria or more inclusive
sauropod clades and probably are not reflective of particularly
close relationships between Opisthocoelicaudia and Epachtho-
saurus within Titanosauria (Gime´nez, 1992; Salgado et al.,
1997). Differences between Opisthocoelicaudia and Epacht-
hosaurus include bifurcate neural spines in the cranial dorsal
vertebrae and opisthocoelous proximal caudal vertebrae in the
former.
DISCUSSION
Titanosauria, a term first proposed by Bonaparte and Coria
(1993), includes all somphospondylian sauropod dinosaurs
more closely related to Saltasaurus than to Euhelopus (Sereno,
1998). Titanosaurians were initially known principally from
fragmentary remains; however, several relatively complete
specimens have been identified in recent years (e.g., Powell,
1992; Jain and Bandyopadhyay, 1997; Curry Rogers and For-
ster, 2001). Epachthosaurus sciuttoi is clearly titanosaurian, as
it possesses multiple proposed synapomorphies of the clade and
subclades nested within it, including caudal dorsal vertebrae
with ventrally expanded posterior centrodiapophyseal laminae;
six sacral vertebrae; procoelous proximal, middle, and distal
caudal centra with well-developed distal articular condyles;
semilunar sternal plates with cranioventral ridges; humeri with
squared proximolateral margins and proximolateral processes;
unossified carpals; strongly reduced manual phalanges; cranio-
laterally expanded, nearly horizontal iliac preacetabular pro-
cesses; pubes longer than ischia; and transversely expanded is-
chia (Gime´nez, 1992; Salgado and Coria, 1993b; Salgado et al.,
1997; Upchurch, 1995, 1998; Wilson and Sereno, 1998; Sanz
et al., 1999; Wilson, 1999b; Curry Rogers and Forster, 2001).
Epachthosaurus is the probably the most basal titanosaurian
known that possesses the derived character of procoelous cau-
118 JOURNAL OF VERTEBRATE PALEONTOLOGY, VOL. 24, NO. 1, 2004
FIGURE 13. Right pes of Epachthosaurus sciuttoi (UNPSJB-PV 920). A, proximal view; B, cranial view. Scale bar equals 10 cm.
dal vertebrae. It is intermediate in phylogenetic position be-
tween Andesaurus, in which all known caudals are amphiplat-
yan, and most remaining titanosaurians. A forthcoming titano-
saurian cladistic analysis that includes Epachthosaurus prom-
ises to more accurately determine its phylogenetic position
(Gime´nez, unpubl. data).
Epachthosaurus is now among the most completely known
titanosaurian genera, and provides insight into several issues
concerning the anatomy and evolutionary history of the clade.
The sacral vertebrae in Epachthosaurus are dorsally united by
an ossified ligament or tendon, otherwise described only in an
unnamed titanosaurian from the Late Cretaceous of Brazil
(Powell, 1987b; Campos and Kellner, 1999). This character
may reflect close affinity between these taxa; alternately, it may
eventually be found to be synapomorphic of a more inclusive
subclade within Titanosauria. Additionally, ossified ligaments
or tendons probably developed in several regions of the tita-
nosaurian skeleton, as they were reported associated with the
cervical vertebrae of a probable new titanosauriform from the
Bajo Barreal Formation (Martı´nez, 1998), the caudal dorsal
neural spines of the specimen upon which the paratype of
Epachthosaurus (MACH-CH 18689) is based (Powell, 1990;
Bonaparte, 1996), and the iliac preacetabular processes of the
titanosaurian ‘‘Titanosaurus’’ colberti (Jain and Bandyopadh-
yay, 1997). Sanz et al. (1999) hypothesized that similar struc-
tures were connected to the planar dorsal surfaces of the caudal
dorsal diapophyses in several titanosaurians, including Lirai-
nosaurus,Saltasaurus, and an unnamed genus from Peiro´polis,
Brazil.
Epachthosaurus possesses apomorphically developed
hyposphene-hypantrum articulations in its dorsal, sacral, and
proximal to middle caudal vertebrae. This contrasts with the
condition in Andesaurus, in which hyposphene-hypantrum ar-
ticulations are limited to the dorsal vertebrae, and most remain-
ing titanosaurians, in which these structures are absent. Acces-
sory intervertebral articulations, along with ossified ligaments
or tendons associated with the caudal dorsal and sacral verte-
brae, probably would have greatly increased the rigidity of the
axial skeleton in Epachthosaurus relative to other sauropods.
The functional significance of this situation requires further re-
search.
Several titanosaurians, including Aeolosaurus (Salgado and
Coria, 1993a), Ampelosaurus (Le Loeuff et al., 1994; Le
Loeuff, 1995), Laplatasaurus (Huene, 1929; Powell, 1980), Li-
rainosaurus (Sanz et al., 1999), Malawisaurus (Jacobs et al.,
1993; Gomani, 1999), Neuquensaurus (Huene, 1929; Powell,
119MARTI
´NEZ ET AL.—ARTICULATED TITANOSAURIAN SAUROPOD EPACHTHOSAURUS
1980), and Saltasaurus (Bonaparte and Powell, 1980; Powell,
1980, 1992), and the possible titanosaurian Agustinia (Bonaparte,
1999a) are reported to possess osteoderms. Moreover, reports of
isolated osteoderms associated with or attributed to titanosaurians
are numerous and geographically widespread (e.g., Depe´ret,
1896; Sanz and Buscalioni, 1987; Chatterjee and Rudra, 1996;
Azevedo and Kellner, 1998; Dodson et al., 1998; Csiki, 1999).
Nevertheless, UNPSJB-PV 920, a largely complete, articulated
skeleton, lacks a dermal skeleton; thus, armor was probably ab-
sent in Epachthosaurus. Whether this character represents the
retention of a plesiomorphic state or constitutes a reversal is un-
resolved. Interestingly, the extreme development of hyposphene-
hypantrum articulations and absence of dermal elements in
Epachthosaurus is consistent with Le Loeuff et al.’s (1994) hy-
pothesis that osteoderms may have served to limit dorsal mobil-
ity in titanosaurians, most of which lack these articulations.
ACKNOWLEDGMENTS
We are deeply indebted to John McIntosh, LeonardoSalgado,
and Jerry Harris for constructive comments on this work. Peter
Dodson and David Gillette provided helpful reviews of the
manuscript. We thank Gabriel Casal for his fine illustrations.
We also thank Jaime Powell for technical comments and assis-
tance with fieldwork and Pamela Balzi for her kind help in the
preparation of the manuscript. Our thanks to all who helped
accomplish the difficult fieldwork required to recover this spec-
imen. Finally, we are grateful to the Valbuena family for their
hospitality at the Estancia ‘‘Ocho Hermanos.’
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... We assign FSAC-KK 7000 to a central position in the middle caudal series, given that the new vertebra lacks transverse processes but preserves feeble protuberances, and the neural spine is a simple, laterally compressed blade that is not yet low and directed posteriorly as is typical of more posterior caudals. Based on comparisons to titanosaurians with well represented anterior and middle caudal sequences (e.g., Alamosaurus sanjuanensis [Gilmore, 1946], Baurutitan britoi [Kellner et al., 2005], Dreadnoughtus schrani , Epachthosaurus sciuttoi [Martínez et al., 2004], Overosaurus paradasorum [Coria et al., 2013], Pellegrinisaurus powelli [Salgado, 1996], MPCA 1501 [a caudal sequence of an unidentified lithostrotian; Powell, 2003; Gallina and Otero, 2015]), the new Kem Kem vertebra probably pertains to a position between caudals 11 and 15. Moreover, in FSAC-KK 7000, the zygapophyses remain well developed, and some laminae, other than those connected to the neural spine, are present but reduced (Fig. 2). ...
... 13–15, 19–23). These structures are also similar to those in anterior caudal vertebrae of several Late Cretaceous titanosauriforms from Argentina, including the Cenomanian–Turonian Epachthosaurus sciuttoi (Martínez et al., 2004, fig. 7), the Coniacian Malarguesaurus florenciae (González Riga et al., 2009, fig. ...
... In caudals 10–12 of Baurutitan britoi, by contrast, the neural spine to prezygapophyseal length ratios are approximately 0.75 for spine length and 0.50 for spine height. In Epachthosaurus sciuttoi, the spine to prezygapophyseal length ratio does not exceed 1.0 for both length and height (Martínez et al., 2004, figs. 7–8). ...
Article
Full-text available
A well preserved middle caudal vertebra from middle Cretaceous (?Albian–lower Cenomanian) deposits informally known as the “Kem Kem beds” exposed in the Gara Sbaa region of Morocco is attributed to a large-bodied titanosaurian sauropod dinosaur. It represents one of the best-preserved and most complete skeletal elements reported for this sauropod group from the Kem Kem sequence. The vertebra is generally similar to middle caudals of the lithostrotian titanosaur Baurutitan britoi from the Upper Cretaceous Bauru Group of Brazil, but differs in several respects, such as: (1) a transversely compressed (as opposed to more square in posterior view) centrum; (2) a taller, anteroposteriorly longer, and more anteriorly positioned neural spine; and (3) prezygapophyses that are subtriangular in lateral view. It represents an animal that likely attained a very large body size (possibly over 25 m in total length), considerably larger than the diplodocoid Rebbachisaurus garasbae, the only named sauropod from the Kem Kem assemblage. Additional, selected specimens from the Kem Kem beds are described, with some probably referable to Titanosauria. In the Kem Kem sequence, sauropod fossils are far less common than those of predatory dinosaurs, which include several coeval, multi-ton taxa. This was likely due to an abundance of potential aquatic prey as well as complex niche partitioning among sympatric theropods, pterosaurs, and crocodyliforms. Nevertheless, some predators, such as the giant theropod Carcharodontosaurus saharicus, likely preyed on sauropods. The taxon represented by the new vertebra (and possibly other isolated remains from the Kem Kem region) and the giant Egyptian titanosaurian Paralititan stromeri rank among the largest known sauropods. Most other North African Cretaceous sauropods appear to have reached only modest adult body sizes; this could, however, be an artifact of the limited number of fossils and uncertainty in the ontogenetic stages represented by most specimens. The morphology of the Kem Kem vertebra suggests that the taxon it represents may have been more closely related to South American and/or European titanosaurians than to other members of this clade from sub-Saharan Africa.
... However, as exemplified by Astrophocaudia (D'Emic, 2012a), Malarguesaurus (Gonz alez Riga et al., 2009) and Phuwiangosaurus (Suteethorn et al., 2010 ), basal titanosauriforms tend to have relatively tall and craniocaudally reduced neural arches, with zygapophyses distant from the centra. We found stronger similarities to MSNM V7157 in the Titanosauria, beginning with basal representatives (Rukwatitan, ), and especially in the lithostrotians Adamantisaurus (Santucci and Bertini, 2006), Epachtosaurus (Martinez et al., 2004), Lirainosaurus (Diaz et al., 2013), Malawisaurus (Gomani 1999Gomani , 2005), Normanniasaurus (Le Loeuff et al., 2013), Paludititan (Csiki et al., 2010), including Alamosaurus (Gilmore, 1946) and other more derived forms, such as Pitekunsaurus from the Campanian of Argentina (Filippi and Garrido, 2008) and Trigonosaurus from the Maastrichtian of Brasil (Campos et al., 2005), In these taxa, the neural arch becomes " lowered " , as it is attached to the anterior half of the centrum by shorter pedicles. This also occurs in the incertae sedis titanosaur Baurutitan (Kellner et al., 2005). ...
... This character, associated to short neural spines, is recovered by our analysis as a synapomorphy of the titanosauriform clade including Atlasaurus and more derived taxa. This morphology is found in some European titanosaurs, such as Ampelosaurus (Le Loeuff, 2005), Normanniasaurus (Le Loeuff et al., 2013), and Paludititan (Csiki et al., 2010), and it is present also in the African basal lithostrotian Malawisaurus (Gomani, 1999Gomani, , 2005), and in the relatively derived lithostrotian Epachtosaurus (Martinez et al., 2004). Trigonosaurus (Campos et al., 2005) and many derived titanosaurs possess neural spines more or less angled anteriorly. ...
... However, the degree of elongation of the prezygapophyseal rami shown by the Italian vertebra e about 40% of the centrum length e is typical of the anterior caudal vertebrae of basal titanosaurs (e.g. Rukwatitan, Gorscak et al., 2014 ), and some members of Lithostrotia , such as Malawisaurus (Gomani, 1999Gomani, , 2005), Lirainosaurus (Diez-Diaz et al., 2013), Alamosaurus (Gilmore, 1946), Epachtosaurus (Martinez et al., 2004). By contrast, very long prezygapophyses (i.e., more than 50% of the centrum length) are found in derived titanosaurs , such as the aeolosaurines (Martinelli et al., 2011; Santucci and Arruda-Campos, 2011). ...
Article
Here we describe the first sauropod skeletal remains from the Italian peninsula that also represent the earliest record of titanosaurs in Southern Europe. Scattered bones, including an almost complete anterior caudal vertebra, were found in Cretaceous (AptianeAlbian) marine deposits, some 50 km East of Rome. The vertebra shows a bizarre and perhaps unique orientation of the zygapophyseal articular facets that renders their interpretation problematic. Phylogenetic retrofitting tests support the placement of the Italian titanosaur among basal lithostrotians. Palaeobiogeographic analysis based on the resulting phyletic relationships suggests an Afro-Eurasian route for the ancestors of the Italian titanosaur, a scenario compatible with the palaeogeographic evolution of the Italian microplates during the Cretaceous. Together with previously recorded titanosaurian-like ichnites from a Cenomanian locality in Latium, this new find suggests a quite long emersion for the Apenninic carbonate platform. We suggest that the Italian titanosaur was member of a population that crossed the western Tethys Sea through a “filtering bridge” composed of a chain of ephemeral islands and peninsulae, known as Periadriatic (Adria) carbonate platforms, that connected sporadically Africa and Europe since the Early Cretaceous.
... In The neural spine seems to be short. There is a prominent, thick and rugose prespinal lamina (prsl) on its anterior surface, with striations and grooves running dorsoventrally (Fig. 7); the spinoprezygapophyseal laminae (sprl) follow a trajectory parallel to the prsl on the neural spine, until they disappear dorsally, as occurs in Trigonosaurus and Rapetosaurus and other titanosauriforms (Powell, 1987;Martínez et al., 2004;Campos et al., 2005;Curry Rogers, 2009). There are anterior and posterior spinodiapophyseal laminae (aspdl and pspdl) crossing the lateral surface of the neural spine (Figs. 6 and 7) and delimit an interlaminar fossa that we propose to be named spdl-f, Fig. 7D. ...
... There are anterior and posterior spinodiapophyseal laminae (aspdl and pspdl) crossing the lateral surface of the neural spine (Figs. 6 and 7) and delimit an interlaminar fossa that we propose to be named spdl-f, Fig. 7D. These two laminae are present in the dicraeosaurid Brachytrachelopan and in titanosaurians (González Riga, 2003;Martínez et al., 2004;Rauhut et al., 2005;Salgado & Coria, 2009;Salgado & Powell, 2010). The right aspdl and pspdl laminae are in contact with one another by means of an accessory lamina that divides the fossa situated between the two spinodiapophyseal laminae (spdl), (Figs. ...
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The sauropod of El Oterillo II is a specimen that was excavated from the Castrillo de la Reina Formation (Burgos, Spain), late Barremian–early Aptian, in the 2000s but initially remained undescribed. A tooth and elements of the axial skeleton, and the scapular and pelvic girdle, represent it. It is one of the most complete titanosauriform sauropods from the Early Cretaceous of Europe and presents an opportunity to deepen our understanding of the radiation of this clade in the Early Cretaceous and study the paleobiogeographical relationships of Iberia with Gondwana and with other parts of Laurasia. The late Barremian–early Aptian is the time interval in the Cretaceous with the greatest diversity of sauropod taxa described in Iberia: two titanosauriforms, Tastavinsaurus and Europatitan; and a rebbachisaurid, Demandasaurus. The new sauropod Europatitan eastwoodi n. gen. n. sp. presents a series of autapomorphic characters in the presacral vertebrae and scapula that distinguish it from the other sauropods of the Early Cretaceous of Iberia. Our phylogenetic study locates Europatitan as the basalmost member of the Somphospondyli, clearly differentiated from other clades such as Brachiosauridae and Titanosauria, and distantly related to the contemporaneous Tastavinsaurus. Europatitan could be a representative of a Eurogondwanan fauna like Demandasaurus, the other sauropod described from the Castrillo de la Reina Formation. The presence of a sauropod fauna with marked Gondwananan affinities in the Aptian of Iberia reinforces the idea of faunal exchanges between this continental masses during the Early Cretaceous. Further specimens and more detailed analysis are needed to elucidate if this Aptian fauna is caused by the presence of previously unnoticed Aptian land bridges, or it represents a relict fauna from an earlier dispersal event.
... La fauna de vertebrados fósiles del Grupo Chubut, específicamente la procedente de las areniscas verdes presentes en la parte alta del Miembro Inferior de la Formación Bajo Barreal, ha brindado información desde el punto de vista morfológico, sistemático, evolutivo, paleoecológico, paleoambiental, paleobiogeográfico y tafonómico (Rodríguez, 1993; Martínez et al., 2004; Martínez y Novas, 2006; Casal et al., 2006; Casal et al., 2007; Casal e Ibiricu, 2010; Ibiricu et al., 2012; Ibiricu et al., 2013a Ibiricu et al., , 2013b Casal et al., 2013). Esto permite considerarla una de las faunas de vertebrados más importantes de Argentina, particularmente por la abundancia y diversidad de dinosaurios cretácicos registrados (Martínez et al., 2001; Casal et al., 2009). ...
... La fracturación y humedad presente en los restos recuperados provocó la pérdida de fragmentos óseos durante la extracción, fundamentalmente en la hemapófisis. Martínez et al., 2004; Calvo et al., 2007; Filippi et al., 2011; Casal et al., 2013, entre muchos otros) y en menor medida en facies lacustres (González Riga et al., 2008, entre Behrensmeyer, 1988; Behrensmeyer y Hook, 1992) en los que los factores sedimentológicos son decisivos en la preservación de los fósiles. Por ejemplo, el titanosaurio Mendozasaurus neguyelap (González Riga, 2003) fue hallado en facies de crevasse splay, y vinculado a un modo tafonómico denominado " asociación ósea de desbordamiento (overbank) " (González Riga y Astini, 2007). ...
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Rests of Aeolosaurus colhuehuapensis, a titanosaur from the Colhue Huapi lake, in the southern Chubut Province, Argentina, were analyzed. The materials under study include twenty one caudal vertebrae and seven haemal arches. They were recovered articulated in overbank facies related to deposits of multi-channel fluvial systems of high sinuosity in the informally called "strata of the Colhue Huapi lake" of Campanian-Maastricthian age. These systems displayed important seasonal fluctuations in the paleodischarge and they were encompassed in a semi-arid climate. The taphonomic history was inferred from the analysis of several taphonomic characteristics present in the bones and macro- and micro-scopic sedimentologic observations. The presence of tenuous longitudinal striation, the absence of bone exfoliation, the articulate condition of the materials and the dorsal bow of the caudal series, support a short period of subaerial exposure with a rapid burial episode. The absence of abrasion marks in the materials indicates that they had scarce or null transport; therefore, they could be considered as autochthonous. The dorsal bow of the tail shows an opisthotonus posture, also exhibited by some theropod and sauropod dinosaurs, but undocumented in the Chubut Group. The recent fluctuant climatic conditions, with variations of extreme humidity and drought, strongly affected the preservation of the materials. The present work is the first detailed taphonomic study of a dinosaur preserved in proximal floodplain facies for the Chubut Group. Finally, the preservation of sauropod bones in those facies is relevant because this type of sub-environment possess a high rate of sediment input as well as scarce or null re-working of the skeletal remains, which favor the conservation of articulated skeletal elements. These findings are very important for the taphonomic and phylogenetic analysis of the titanosaur clade, in which the majority of the taxa are represented by isolated and unarticulated remains.
... Nevertheless, bones of sauropods are extremely rare at Dzharakuduk and similar localities (Nesov, 1995: p. 20), and titanosaurian osteoderms are generally scarcely found (D'Emic, Wilson & Chatterjee, 2009), even in sites in which these sauropods are common (see e.g., Bellevue in France, Le Loeuff et al., 1994, andLo Hueco in Spain, Vidal, Ortega & Sanz, 2014). More importantly, the possession of osteoderms is at best an ambiguous synapomorphy of Lithostrotia (see e.g., D'Emic, 2012: table 5) and, very probably, not all members of this clade bore such bony structures (see Martínez et al., 2004). Averianov & Sues (2017: p. 192) noted that the Dzharakuduk sauropod presents similarities to Dongyangosaurus sinensis and Baotianmansaurus henanensis. ...
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Despite continuous improvements, our knowledge of the palaeoneurology of sauropod dinosaurs is still deficient. This holds true even for Titanosauria, which is a particularly speciose clade of sauropods with representatives known from numerous Cretaceous sites in many countries on all continents. The data currently available regarding the palaeoneurology of titanosaurs is strongly biased towards Gondwanan forms (Argentina above all, but also India, Malawi and Australia). In contrast, the palaeoneurology of Laurasian titanosaurs is known only from a few taxa from Spain and Uzbekistan, despite the discovery in other countries of Laurasia of a number of neurocranial remains that would lend themselves well to investigations of this kind. To fill in this gap in our knowledge, we subjected a titanosaurian braincase from the uppermost Upper Cretaceous of southern France to X-ray computed tomographic scanning, allowing the generation of 3D renderings of the endocranial cavity enclosing the brain, cranial nerves and blood vessels, as well as the labyrinth of the inner ear. These reconstructions are used to clarify the phylogenetic position of the specimen from the Fox-Amphoux-Métisson site. A combination of characters, including the presence of two hypoglossal rami on the endocast, the average degree of development of the dorsal-head/ caudal-middle-cerebral vein system and the relatively short and subequal lengths of the ipsilateral semicircular canals of the labyrinth, are particularly revealing in this respect. They suggest that, compared with the few other Laurasian titanosaurs for which in-depth palaeoneurological data are available, the French taxon is more derived than the distinctly more ancient, possibly non-lithostrotian titanosaur from the Uzbek site of Dzharakuduk but more basal than derived saltasaurids, such as the coeval or slightly more recent forms from the Spanish locality of Lo Hueco.
... The titanosaur fossil record includes several articulated specimens that do not have associated osteoderms (e.g., Epachthosaurus, Martínez et al., 2004;Opisthocoelicaudia, Borsuk-Bialynicka, 1977;Alamosaurus, Gilmore, 1946;Phuwiangosaurus, Martin et al., 1994). These unarmored titanosaurs are widely distributed in time and space, a pattern that suggests that taphonomic biases may not have substantially filtered the titanosaur osteoderm record. ...
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Here we describe a new record of a sauropod dinosaur from the Lower Cretaceous (Hauterivian-Barremian) Rio Piranhas Formation, Sousa Basin, NE Brazil. Dinosaur fossil bones from this deposit were unknown until now. Thus, the discovery of a sauropod fibula from this locality is highly significant. Our discovery represents an indeterminate titanosaur and the earliest stratigraphic occurrence of this group in central Gondwana. When compared to chronocorrelate titanosaur trackmakers of this geological unit, this fossil specimen appears substantially smaller. Histological analysis of the fibula suggests that this is a relatively young individual (approximately 40-50% adult body size) that had passed its most rapid phase of early juvenile growth, but had not yet attained somatic maturity. Thus, the fibula recovered is from a young individual rather than from a small-bodied adult titanosaur.
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Titanosauria is an exceptionally diverse, globally-distributed clade of sauropod dinosaurs that includes the largest known land animals. Knowledge of titanosaurian pedal structure is critical to understanding the stance and locomotion of these enormous herbivores and, by extension, gigantic terrestrial vertebrates as a whole. However, completely preserved pedes are extremely rare among Titanosauria, especially as regards the truly giant members of the group. Here we describe Notocolossus gonzalezparejasi gen. et sp. nov. from the Upper Cretaceous of Mendoza Province, Argentina. With a powerfully-constructed humerus 1.76 m in length, Notocolossus is one of the largest known dinosaurs. Furthermore, the complete pes of the new taxon exhibits a strikingly compact, homogeneous metatarsus-seemingly adapted for bearing extraordinary weight-and truncated unguals, morphologies that are otherwise unknown in Sauropoda. The pes underwent a near-progressive reduction in the number of phalanges along the line to derived titanosaurs, eventually resulting in the reduced hind foot of these sauropods.
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Studies of a complete left pes of the Texas Lower Cretaceous sauropod, Pleurocoelus sp. indet., show-on the basis of the form and size of the elements, particularly the claws-some adaptations for scratch-digging. Four distinct claws are associated with the pedal skeleton, supporting the view that this species was at least one of the Glen Rose trackmakers. Evidence presented here allies Pleurocoelus with the brachiosaurids.
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Remains assigned to Aeolosaurus Powell, 1986 from the Allen Formation are described. The specimen differs from the holotype of Aeolosaurus rionegrinus Powell, 1986 in the length of the prezigapophyses, relative position of the postzigapophyses, and radius and ischium morphology. Considerations on a specimen tentatively assigned to the type species, and modified diagnosis of genus are included. Association of dermal plates to the specimen here described is commented. -English summary